View source for Earth:Grand Canyon

{{short description|Steep-sided canyon carved by the Colorado River in Arizona, United States }}
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{{Infobox valley
|name = Grand Canyon
|length = {{convert|277|mi|km}}
|width = {{convert|4|to|18|mi|km}}
|elevation = Approx. {{convert|2600|ft|m|-2}}
|location = Arizona
|age = 5–6 million years<ref name=Karlstrom>{{cite journal|title=Formation of the Grand Canyon 5 to 6 million years ago through integration of older palaeocanyons|journal=Nature Geoscience|first1=Karl E.|last1=Karlstrom|first2=John P.|last2=Lee|first3=Shari A.|last3=Kelley|first4=Ryan S.|last4=Crow|first5=Laura J.|last5=Crossey|display-authors=4|doi =10.1038/ngeo2065|volume = 7|issue=3| pages = 239–244| year=2014|bibcode=2014NatGe...7..239K}}</ref>
|photo = Canyon_River_Tree_(165872763).jpeg
|photo_caption = The [[Earth:Colorado River|Colorado River]] flowing through the Grand Canyon in Arizona
|photo_size = 400
|label = 
|label_position = right
|coordinates = {{Coord|36.3|N|112.6|W|type:landmark_region:US-AZ_scale:300000|format=dms|display=inline,title}}
|watercourses=[[Earth:Colorado River|Colorado River]]
|map=Arizona#USA#North America
|map_caption=Location within Arizona##Location within the United States##Location within North America
|country=United States}}

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The '''Grand Canyon''' ({{Lang-hop|Öngtupqa}},<ref name="nameinHopi">{{cite web | url=http://navajotimes.com/opinion/pueblos-join-forces-to-oppose-grand-canyon-escalade-project/ | title=Pueblos join forces to oppose Grand Canyon Escalade Project | publisher=Navajo Times | date=September 11, 2014 | access-date=April 20, 2016 | url-status=live | archive-url=https://web.archive.org/web/20160601164359/http://navajotimes.com/opinion/pueblos-join-forces-to-oppose-grand-canyon-escalade-project/ | archive-date=June 1, 2016 | df=mdy-all }}</ref> {{lang-yuf-x-yav|Wi:kaʼi:la}}, {{Lang-nv|Bidááʼ Haʼaztʼiʼ Tsékooh}},<ref>Linford, Laurence D. ''Navajo Places. History, Legend, Landscape.'' University of Utah Press. Salt Lake City, UT: 2000.</ref><ref>Wilson, Alan with Gene Dennison. ''Navajo Place Names. An observer's guide.'' Jeffrey Norton Publishers. Guilford, CT: 1995.</ref> Southern Paiute language: Paxa’uipi,<ref>Yanawant Paiute Places and Landscapes in the Arizona Strip: Volume Two of the Arizona Strip Landscapes and Place Name Study, Part 2, p. 69 [http://npshistory.com/publications/para/yanawant-2.pdf Link]</ref> {{Lang-es|Gran Cañón or Gran Cañón del Colorado}}) is a steep-sided [[Earth:Canyon|canyon]] carved by the [[Earth:Colorado River|Colorado River]] in Arizona, United States. The Grand Canyon is {{convert|277|mi|km}} long, up to {{convert|18|mi|km}} wide and attains a depth of over a mile ({{convert|6093|ft|m|disp=or|sp=us}}).<ref name="Kiver"/>{{rp|902}}

The canyon and adjacent rim are contained within Grand Canyon National Park, the Kaibab National Forest, Grand Canyon–Parashant National Monument, the Hualapai Indian Reservation, the Havasupai Indian Reservation and the Navajo Nation. The surrounding area is contained within the Baaj Nwaavjo I'tah Kukveni – Ancestral Footprints of the Grand Canyon National Monument. President [[Biography:Theodore Roosevelt|Theodore Roosevelt]] was a major proponent of the preservation of the Grand Canyon area and visited it on numerous occasions to hunt and enjoy the scenery.

Nearly two billion years of Earth's geological history have been exposed as the Colorado River and its tributaries cut their channels through layer after layer of rock while the [[Earth:Colorado Plateau|Colorado Plateau]] was [[Earth:Tectonic uplift|uplifted]].<ref name="Witze">{{cite journal |last1=Witze |first1=Alexandra |title=A deeper understanding of the Grand Canyon |journal=Knowable Magazine |date=26 February 2019 |doi=10.1146/knowable-022619-1|doi-access=free |url=https://knowablemagazine.org/article/physical-world/2019/deeper-understanding-grand-canyon |access-date=23 June 2022}}</ref><ref name=npsgeol>[http://www.nps.gov/grca/naturescience/geologicformations.htm Geologic Formations of the Grand Canyon] {{webarchive|url=https://web.archive.org/web/20070403022128/http://www.nps.gov/grca/naturescience/geologicformations.htm |date=April 3, 2007 }} National Park Service Retrieved November 17, 2009</ref> While some aspects about the history of incision of the canyon are debated by geologists,<ref name="Witze"/><ref name=carvingGC>{{cite book|title=Carving Grand Canyon: Evidence, Theories, and Mystery|first=Wayne|last=Ranney|publisher=Grand Canyon Association|year=2005|isbn=978-0938216827}}</ref> several recent studies support the hypothesis that the Colorado River established its course through the area about 5 to 6 million years ago.<ref name="Witze"/><ref name=Karlstrom/><ref>{{Cite journal|title = Geomorphic constraints on the age of the western Grand Canyon|journal = Geosphere|pages = 958–976|volume = 11|issue = 4|doi = 10.1130/ges01131.1|first1 = Andrew|last1 = Darling|first2 = Kelin|last2 = Whipple|year = 2015|bibcode = 2015Geosp..11..958D|df = mdy-all|doi-access = free}}</ref><ref>{{Cite journal|title = Review and analysis of the age and origin of the Pliocene Bouse Formation, lower Colorado River Valley, southwestern USA|journal = Geosphere|pages = 444–459|volume = 9|issue = 3|doi = 10.1130/ges00896.1|first1 = J.E.|last1 = Spencer|first2 = P.J.|last2 = Patchett|first3 = P.A.|last3 = Pearthree|first4 = P.K.|last4 = House|first5 = A.M.|last5 = Sarna-Wojcicki|first6 = E.|last6 = Wan|first7 = J.A.|last7 = Roskowski|first8 = J.E.|last8 = Faulds|year = 2013|df = mdy-all|bibcode = 2013Geosp...9..444S|doi-access = free}}</ref> Since that time, the Colorado River has driven the down-cutting of the tributaries and retreat of the cliffs, simultaneously deepening and widening the canyon.

For thousands of years, the area has been continuously inhabited by Native Americans, who built settlements within the canyon and its many caves. The Pueblo people considered the Grand Canyon a holy site, and made pilgrimages to it.<ref>{{cite book|last1=Mitchell|first1=Douglas R.|last2=Lippert|first2=Dorothy|first3=Judy L.|last3=Brunson-Hadley|title=Ancient Burial Practices in the American Southwest|publisher=UNM Press|location=Albuquerque, NM|edition=reprint, illustrated|isbn=978-0826334619|url=https://books.google.com/books?id=T7VBVRMFJiAC&q=Ongtupqa&pg=PA11|page=11|year=2004|url-status=live|archive-url=https://web.archive.org/web/20160517041227/https://books.google.com/books?id=T7VBVRMFJiAC&pg=PA11&dq=Ongtupqa|archive-date=May 17, 2016|df=mdy-all}}</ref> The first European known to have viewed the Grand Canyon was García López de Cárdenas from Spain, who arrived in 1540.<ref>{{cite encyclopedia|url=http://www.uen.org/utah_history_encyclopedia/c/COLORADO_PLATEAU.html|title=History of the Colorado Plateau|encyclopedia=Utah History Encyclopedia|access-date=October 22, 2010|url-status=dead|archive-url=https://web.archive.org/web/20130109223648/http://www.uen.org/utah_history_encyclopedia/c/COLORADO_PLATEAU.html|archive-date=January 9, 2013}}</ref>

==Geography==
[[File:GrandCanyon.NASA.2014.jpg|thumb|Image of the Grand Canyon and surrounding area taken from the [[Astronomy:International Space Station|International Space Station]]]]
[[File:Grand Canyon from air.JPG|thumb|upright|The Grand Canyon from an airplane, with the Colorado River visible]]
[[File:GrandCanyon27June2017.tif|thumb|Grand Canyon, Arizona, Nevada, Lake Powell to Lake Mead, June 27, 2017, Sentinel-2 true-color satellite image.  Scale 1:450,000.]]

The Grand Canyon is a river valley in the [[Earth:Colorado Plateau|Colorado Plateau]] that exposes uplifted [[Earth:Proterozoic|Proterozoic]] and [[Earth:Paleozoic|Paleozoic]] strata,<ref name="Ranney">{{cite journal |last1=Ranney |first1=Wayne |title=A pre–21st century history of ideas on the origin of the Grand Canyon |journal=Geosphere |date=April 2014 |volume=10 |issue=2 |pages=233–242 |doi=10.1130/GES00960.1 |bibcode=2014Geosp..10..233R |language=en |issn=1553-040X|doi-access=free }}</ref> and it is also one of the six distinct physiographic sections of the Colorado Plateau province.<ref name="Leydsman McGinty">{{cite book |last1=Leydsman McGinty |first1=Ellie I. |last2=McGinty |first2=Christopher M. |editor-last1=Banner |editor-first1=R. E. |editor-last2=Baldwin |editor-first2=B. D. |editor-last3=Leydsman McGinty |editor-first3=Ellie I. |title=Rangelands resources of Utah|chapter=Physiography of Utah |date=2009 |publisher=Utah State University Cooperative Extension Service |location=Logan, Utah, USA |pages=24–28 |url=https://extension.usu.edu/rangelands/ou-files/RRU_Section_Three.pdf |archive-url=https://web.archive.org/web/20220826162151/https://extension.usu.edu/rangelands/ou-files/RRU_Section_Three.pdf |archive-date=2022-08-26 |url-status=live |access-date=23 June 2022}}</ref> Even though it is not the deepest canyon in the world (Kali Gandaki Gorge in Nepal is much deeper<ref>{{cite web |last1=Montmoli |first1=C |title=A geological journey through the deepest gorge on Earth: the Kali Gandaki valley section, west-central Nepal|url=https://www.researchgate.net/publication/264996830 |website=ResearchGate.net |access-date=27 July 2021}}</ref>), the Grand Canyon is known for its visually overwhelming size and its intricate and colorful landscape. Geologically, it is significant because of the thick sequence of ancient rocks that are well preserved and exposed in the walls of the canyon. These rock layers record much of the early geologic history of the North American continent.<ref name="Witze"/>

Uplift associated with mountain formation later moved these sediments thousands of feet upward and created the Colorado Plateau. The higher elevation has also resulted in greater precipitation in the Colorado River drainage area, but not enough to change the Grand Canyon area from being semi-arid.<ref>{{cite journal |last1=Marlatt |first1=William |last2=Riehl |first2=Herbert |title=Precipitation regimes over the upper Colorado River |journal=Journal of Geophysical Research |date=15 December 1963 |volume=68 |issue=24 |pages=6447–6458 |doi=10.1029/JZ068i024p06447 |bibcode=1963JGR....68.6447M }}</ref> The uplift of the Colorado Plateau is uneven, and the [[Earth:Kaibab Plateau|Kaibab Plateau]] that the Grand Canyon bisects is over {{convert|1000|ft|m|spell=in}} higher at the North Rim than at the South Rim. Almost all runoff from the North Rim (which also gets more rain and snow) flows toward the Grand Canyon, while much of the runoff on the plateau behind the South Rim flows away from the canyon (following the general tilt).<ref name="Witze"/> The result is deeper and longer tributary washes and canyons on the north side and shorter and steeper side canyons on the south side.<ref name="Kiver">{{cite book |last1=Kiver |first1=Eugene P. |last2=Harris |first2=David V. |title=Geology of U.S. Parklands |date=15 June 1999 |publisher=John Wiley & Sons |isbn=978-0-471-33218-3 |url=https://books.google.com/books?id=S0zDQWiFuvkC&pg=PA406 |access-date=23 June 2022 |language=en}}</ref>{{rp|406}}

Temperatures on the North Rim are generally lower than those on the South Rim because of the greater elevation (averaging {{convert|8,000|ft|m|disp=or|sp=us}} above sea level).<ref name=NPSnatsci/> Heavy rains are common on both rims during the summer months. Access to the North Rim via the primary route leading to the canyon (State Route 67) is limited during the winter season due to road closures.<ref name=off-season(jump-link)>{{cite web|title=Winter on the North Rim (off-season)|url=http://www.nps.gov/grca/planyourvisit/hours.htm#CP_JUMP_538881|work=Operating Hours & Seasons|publisher=National Park Service; US Dept. of Interior|access-date=January 21, 2013|url-status=live|archive-url=https://web.archive.org/web/20110303012942/http://www.nps.gov/grca/planyourvisit/hours.htm#CP_JUMP_538881|archive-date=March 3, 2011|df=mdy-all}}</ref>

==Geology==
[[File:Stratigraphy of the Grand Canyon.png|thumb|upright=1.4|Diagram showing the placement, age and thickness of the rock units exposed in the Grand Canyon]]
[[Image:GCRockfall.JPG|thumb|Rockfalls in recent times, along with other [[Earth:Mass wasting|mass wasting]], have further widened the canyon]]

The Grand Canyon is part of the Colorado River basin, which has developed over the past 70{{nbsp}}million years.<ref name="Witze"/><ref>{{cite Q|Q56082876}}</ref> Over more than 150 years, scientists have gathered data, proposed new ideas, and debated sometimes contentious theories about the geologic origins of the Grand Canyon and the Colorado River. Formation of the Grand Canyon and the Colorado River may involve a complex history in which multiple factors and geologic processes have interacted over time and in different locations.<ref name="Ranney"/>

In the most recent round of "old river" vs. "young river" controversy, researchers have challenged estimates that had placed the age of the canyon at 5–6{{nbsp}}million years. The research has aroused considerable controversy because it suggests a substantial departure from prior widely supported scientific consensus.<ref name="Johnson1">{{cite web |first1=Joshua |last1=Johnson |date=2013 |title=Western U.S. Tectonics: The Origin of the Grand Canyon – Controversy and Tectonic Implications – Intro page |url=http://cires1.colorado.edu/people/jones.craig/WUStectonics/grand_canyon/ |website=cires1.colorado.edu |access-date=23 June 2022}}</ref><ref name="Johnson2">{{cite web |first1=Joshua  |last1= Johnson |date=2013 |title=Western U.S. Tectonics: The Origin of the Grand Canyon – Controversy and Tectonic Implications – SYNTHESIS AND TECTONIC IMPLICATIONS |url=http://cires1.colorado.edu/people/jones.craig/WUStectonics/grand_canyon/ |website=cires1.colorado.edu |access-date=23 June 2022}}</ref><ref name="Witze"/>

In a 2008 study, Victor Polyak examined caves near the Grand Canyon and placed their origins about 17{{nbsp}}million years ago. The study, which was published in the journal ''Science'' in 2008, used uranium-lead dating to analyze [[Chemistry:Calcite|calcite]] deposits found on the walls of nine caves throughout the canyon.<ref name="UNM Study">{{cite news | last = Wilford | first = John | title = Study Says Grand Canyon Older Than Thought | newspaper = New York Times | date = February 6, 2008 | url = https://www.nytimes.com/2008/03/06/science/06cnd-canyon.html?_r=2&hp&oref=slogin&oref=slogin | access-date = February 6, 2008 | url-status=live | archive-url = https://web.archive.org/web/20130517190314/http://www.nytimes.com/2008/03/06/science/06cnd-canyon.html?_r=2&hp&oref=slogin&oref=slogin | archive-date = May 17, 2013 | df = mdy-all }}</ref><ref name="NPR2008">{{cite news |title=How Old Is the Grand Canyon? |url=https://www.npr.org/2008/03/07/87984356/how-old-is-the-grand-canyon |access-date=23 June 2022 |work=NPR.org |date=March 7, 2008 |language=en}}</ref><ref name="Polyak">{{cite journal |last1=Polyak |first1=Victor |last2=Hill |first2=Carol |last3=Asmerom |first3=Yemane |title=Age and evolution of the Grand Canyon revealed by U-Pb dating of water table-type speleothems |journal=Science |date=7 March 2008 |volume=319 |issue=5868 |pages=1377–1380 |doi=10.1126/science.1151248 |pmid=18323451 |bibcode=2008Sci...319.1377P |s2cid=206509716 |url=https://pubmed.ncbi.nlm.nih.gov/18323451/ |access-date=23 June 2022 |issn=1095-9203}}</ref>

In another 2008 study, Rebecca Flowers reported on [[Chemistry:Apatite|apatite]] (U-Th)/He [[Physics:Thermochronology|thermochronometry]] results suggesting that parts of the Grand Canyon had reached a depth near to the modern depth around 20{{nbsp}}million years ago.<ref name=NYT-29-Nov-2012/><ref name="Flowers">{{cite journal |last1=Flowers |first1=R.&nbsp;M. |last2=Wernicke |first2=B.&nbsp;P. |last3=Farley |first3=K.&nbsp;A. |title=Unroofing, incision, and uplift history of the southwestern Colorado Plateau from apatite (U-Th)/He thermochronometry |journal=GSA Bulletin |date=1 May 2008 |volume=120 |issue=5–6 |pages=571–587 |doi=10.1130/B26231.1 |bibcode=2008GSAB..120..571F |url=https://pubs.geoscienceworld.org/gsa/gsabulletin/article-abstract/120/5-6/571/2275/Unroofing-incision-and-uplift-history-of-the |access-date=23 June 2022 |language=en |issn=0016-7606}}</ref>
In a subsequent study published in the journal ''Science''  in 2012, she suggested that the western part of the Grand Canyon could be as old as 70{{nbsp}}million years.<ref name="Achenbach">{{cite news |last1=Achenbach |first1=Joel |title=New research revives debate over Grand Canyon's age |url=https://www.washingtonpost.com/national/health-science/new-research-revives-debate-over-grand-canyons-age/2014/01/26/6da35f32-8539-11e3-9dd4-e7278db80d86_story.html |access-date=23 June 2022 |newspaper=Washington Post |date=26 January 2014}}</ref><ref name=NYT-29-Nov-2012>{{cite news|last=Wilford|first=John Noble|title=60-Million-Year Debate on Grand Canyon's Age|url=https://www.nytimes.com/2012/11/30/science/earth/study-sees-older-grand-canyon-stirring-controversy.html?_r=0|access-date=January 22, 2013|newspaper=New York Times|date=November 29, 2012|url-status=live|archive-url=https://web.archive.org/web/20130121222602/http://www.nytimes.com/2012/11/30/science/earth/study-sees-older-grand-canyon-stirring-controversy.html?_r=0|archive-date=January 21, 2013|df=mdy-all}}</ref><ref>{{Cite journal|last1=Flowers|first1=R.&nbsp;M.|last2=Farley|first2=K.&nbsp;A.|date=2012-12-21|title=Apatite 4He/3He and (U-Th)/He Evidence for an Ancient Grand Canyon|journal=Science|language=en|volume=338|issue=6114|pages=1616–1619|doi=10.1126/science.1229390|issn=0036-8075|pmid=23196906|bibcode=2012Sci...338.1616F|s2cid=32277486|doi-access=free}}</ref><ref>{{cite news| url= http://www.3news.co.nz/Debate-rages-over-Grand-Canyons-origins/tabid/1160/articleID/278924/Default.aspx| work= 3 News NZ| title= Grand Canyon as old as the dinosaurs?| date= December 3, 2012| url-status= dead| archive-url= https://web.archive.org/web/20131031192424/http://www.3news.co.nz/Debate-rages-over-Grand-Canyons-origins/tabid/1160/articleID/278924/Default.aspx| archive-date= October 31, 2013| df= mdy-all| access-date= December 2, 2012}}</ref>

The emerging scientific consensus is that the canyon is made up of multiple segments which formed at different times and eventually connected to become the waterway now traversed by the Colorado River.  Of the three central segments, the "Hurricane" was formed 50–70{{nbsp}}million years ago, and the "Eastern Grand Canyon" was cut 15–25{{nbsp}}million years ago. In contrast, the "Marble Canyon" and "Westernmost Grand Canyon" segments at the ends of the canyon were carved in the last five to six million years.<ref>{{cite news |last1=Amos |first1=Jonathan |title=Grand Canyon 'formed recently' |url=https://www.bbc.com/news/science-environment-25881953 |access-date=11 July 2022 |work=BBC News |date=26 January 2014}}</ref><ref>{{cite news |last1=Bush |first1=Mike |title=Debate over the origins of the Grand Canyon - Albuquerque Journal |url=https://www.abqjournal.com/346998/origins-of-the-grand-canyon.html |access-date=11 July 2022 |work=www.abqjournal.com |date=February 3, 2014}}</ref>

The major geologic exposures in the Grand Canyon range in age from the two-billion-year-old Vishnu Schist at the bottom of the Inner Gorge to the 270-million-year-old [[Earth:Kaibab Limestone|Kaibab Limestone]] on the Rim. There is a gap of about a billion years between 1.75{{nbsp}}billion and 1.25{{nbsp}}billion years ago. This large [[Earth:Unconformity|unconformity]] indicates a long period for which no deposits are present.<ref name="Witze"/>

Then, between 1.25{{nbsp}}billion and 730{{nbsp}}million years ago, intermittent sediments began to form the Grand Canyon Supergroup.<ref name="Witze"/> Many of the formations were deposited in warm shallow seas, near-shore environments (such as beaches), and swamps as the seashore repeatedly advanced and retreated over the edge of a proto-North America. Major exceptions include the Permian [[Earth:Coconino Sandstone|Coconino Sandstone]], which contains abundant geological evidence of [[Earth:Aeolian processes|aeolian]] sand dune deposition. Several parts of the Supai Group also were deposited in non-marine environments.

The great depth of the Grand Canyon and especially the height of its strata (most of which formed below sea level) can be attributed to {{convert|5000|-|10000|ft|m}} of uplift of the Colorado Plateau, starting about 65{{nbsp}}million years ago (during the [[Earth:Laramide orogeny|Laramide orogeny]]). This uplift has steepened the [[Stream gradient|stream gradient]] of the Colorado River and its tributaries, which in turn has increased their speed and thus their ability to cut through rock (see the [[Earth:Colorado River#Elevation summary|elevation summary]] of the Colorado River for present conditions).

Weather conditions during the [[Earth:Quaternary glaciation|ice ages]] also increased the amount of water in the Colorado River drainage system. The ancestral Colorado River responded by cutting its channel faster and deeper.

The base level and course of the Colorado River (or its ancestral equivalent) changed 5.3{{nbsp}}million years ago when the Gulf of California opened and lowered the river's base level (its lowest point). This increased the rate of erosion and cut nearly all of the Grand Canyon's current depth by 1.2{{nbsp}}million years ago. The terraced walls of the canyon were created by differential erosion.<ref>{{cite web|url=http://academic.brooklyn.cuny.edu/geology/leveson/core/graphics/nyc_mins2/hyp_test_diff_erode.html|title=The Hypothesis of Differential Erosion|first=David|last=Leveson|access-date=October 22, 2010|url-status=live|archive-url=https://web.archive.org/web/20110622085241/http://academic.brooklyn.cuny.edu/geology/leveson/core/graphics/nyc_mins2/hyp_test_diff_erode.html|archive-date=June 22, 2011|df=mdy-all}}</ref>

Between 100,000 and 3{{nbsp}}million years ago, volcanic activity deposited ash and lava over the area, which at times completely obstructed the river. These volcanic rocks are the youngest in the canyon.

==Hydrology==
[[File:Grand Canyon National Park Ribbon Falls 0913e (6687267983).jpg|thumb|upright| Ribbon Falls, near the North Kaibab Trail, represents ground water reaching the surface.]]
Groundwater flow in the Grand Canyon region is an active area of study.  
[[Earth:Groundwater|Groundwater]] forms when rain soaks down into the earth and reaches the [[Earth:Water table|water table]]. The composition of the earth in a given area determines its [[Earth:Permeability (earth sciences)|permeability]], the ease with which water flows through it. Sand is more permeable than clay.  Less permeable rock layers composed of clay can block the passage of water and are known as  aquitards.  More permeable areas of rock that hold and transport groundwater underground are known as aquifers.  An area of water bounded by two aquitards is called a confined aquifer, while water below the surface and above an aquitard is called an unconfined aquifer.<ref name="Wesoloski">{{cite web |last1=Wesoloski |first1=Catherine |title=The Pressure on Groundwater in the Grand Canyon |url=https://watershed.ucdavis.edu/education/classes/files/content/flogs/Wesoloski_blogging_Tanner_groundwater.pdf |archive-url=https://web.archive.org/web/20220826162140/https://watershed.ucdavis.edu/education/classes/files/content/flogs/Wesoloski_blogging_Tanner_groundwater.pdf |archive-date=2022-08-26 |url-status=live |website=UC Davis Center for Watershed Sciences |access-date=30 June 2022}}</ref>

The different geologic levels of the Grand Canyon have created two major aquifers where groundwater collects.  The higher C-aquifer is an unconfined aquifer.  It collects groundwater that seeps through the Kaibab and Toroweap Formations into the Coconino Sandstone. Below it, the Permian Hermit Formation and Supai Group provide a dense barrier. Groundwater from the C-acquifer can flow laterally, appearing as seeps along the canyon walls at the base of the Coconino Sandstone but can also descend vertically through fault zones to recharge the underlying confined R-aquifer.  The R-aquifer, also known as the Red Wall Muav aquifer, is a [[Earth:Karst|karst]] aquifer.  It involves an area of substantial fracturing through the Redwall Limestone, Temple Butte Formation and Cambrian Muav Limestone of the Tonto Group.  Five individual systems flow through the R-aquifer and compose the regional groundwater-flow system which drains into the Grand Canyon: Kaibab, Uinkaret-Kanab, Marble-Shinumo, Cataract, and Blue Spring.<ref name="Knight">{{cite book |last1=Knight |first1=Jacob E. |last2=Huntoon |first2=Peter W. |title=Conceptual models of groundwater flow in the Grand Canyon region, Arizona: U.S. Geological Survey Scientific Investigation Report 2022–5037 |date=2022 |publisher=U.S. Department of the Interior U.S. Geological Survey |url=https://pubs.usgs.gov/sir/2022/5037/sir20225037.pdf |archive-url=https://web.archive.org/web/20220419115410/https://pubs.usgs.gov/sir/2022/5037/sir20225037.pdf |archive-date=2022-04-19 |url-status=live |access-date=30 June 2022 |language=en}}</ref>

The flow of groundwater in the Grand Canyon region is influenced in multiple ways by [[Earth:Fault (geology)|geologic faults]] and [[Earth:Fold (geology)|folds]]. Discharge from the R-aquifer appears as springs and seeps in both the Grand Canyon  and tributary canyons.  Springs discharge to the Grand Canyon in areas of lower Paleozoic carbonates, and are associated with geologic faults and fractures. Fractures are believed to provide dominant pathways both for vertical circulation in the Paleozoic section, and for lateral collection and transport of water to springs deep in the canyons. The largest springs discharge from the R-aquifer. A smaller number of springs discharge at lower rates from the C-aquifer.  Much of the water that could potentially recharge the aquifers is likely released as springs rather than reaching the aquifers.<ref name="Knight"/>

Studies of the chemical composition of groundwater at sites across the Grand Canyon region indicate that groundwater contains a fraction of modern water (post-1950), and that many springs have a mix of modern water and older groundwater. Estimated mean ages for South Rim groundwater range from 6 years old (San Francisco Peaks) to nearly 20,000 years old (Bar Four well, Blue Spring). Groundwater age in the South Rim groundwater system also correlates to longitude, with age increasing from east to west from Red Canyon to Boucher springs. Surprisingly, the Canyon Mine Observation well is more similar to Redwall-Muav aquifer wells (R-aquifer) than to the Coconino C-aquifer. This suggests the possibility of a hydrologic connection or similar recharge sources for that hydrologic position. Old groundwater from Havasupai well may have a similar source to the Havasu Spring upwelling from the Redwall-Muav aquifer. Sites with younger estimated mean ages tend to be associated with the unconfined Coconino aquifer. They may recharge quickly as a result of snowmelt, run-off and local precipitation. It is likely that the deeper confined R-aquifer relies primarily on snowmelt from the San Francisco Peaks to recharge.<ref name="Solder">{{cite journal |last1=Solder |first1=John E. |last2=Beisner |first2=Kimberly R. |last3=Anderson |first3=Jessica |last4=Bills |first4=Don J. |title=Rethinking groundwater flow on the South Rim of the Grand Canyon, USA: characterizing recharge sources and flow paths with environmental tracers |journal=Hydrogeology Journal |date=1 August 2020 |volume=28 |issue=5 |pages=1593–1613 |doi=10.1007/s10040-020-02193-z |bibcode=2020HydJ...28.1593S |s2cid=220260022 |language=en |issn=1435-0157|doi-access=free }}</ref>

Other research has tried to relate groundwater flow paths to possible levels of risk for contamination and identify vulnerability regions for the underlying aquifers.  Almost half of the Kaibab plateau's surface was associated with high to very high vulnerability of the unconfined Coconino aquifer (C-aquifer), while about a fifth of the Kaibab Plateau was estimated to be an area of high vulnerability for the Redwall-Muav aquifer (R-aquifer).<ref>{{cite news |title=Mystery of Grand Canyon's water supply |work=ScienceDaily |date=January 23, 2020 |url=https://www.sciencedaily.com/releases/2020/01/200123170622.htm |access-date=1 July 2022 |language=en}}</ref><ref name="Jones">{{cite journal |last1=Jones |first1=Natalie A. |last2=Hansen |first2=Jered |last3=Springer |first3=Abraham E. |last4=Valle |first4=Cynthia |last5=Tobin |first5=Benjamin W. |title=Modeling intrinsic vulnerability of complex karst aquifers: modifying the COP method to account for sinkhole density and fault location |journal=Hydrogeology Journal |date=December 2019 |volume=27 |issue=8 |pages=2857–2868 |doi=10.1007/s10040-019-02056-2 |bibcode=2019HydJ...27.2857J |s2cid=207990859 |url=https://link.springer.com/article/10.1007/s10040-019-02056-2 |access-date=1 July 2022}}</ref>

==History==
[[File:Nankoweap.JPG|thumb|Ancestral Puebloan granaries at Nankoweap Creek]]

===Native Americans===
The Ancestral Puebloans were a Native American culture centered on the present-day [[Earth:Four Corners|Four Corners]] area of the United States. They were the first people known to live in the Grand Canyon area. The cultural group has often been referred to in archaeology as the Anasazi, although the term is not preferred by the modern Puebloan peoples.<ref>{{Cite web|last=Congress|first=The Library of|title=LC Linked Data Service: Authorities and Vocabularies (Library of Congress)|url=https://id.loc.gov/authorities/subjects/sh2014001391.html|access-date=2020-12-25|website=id.loc.gov}}</ref> The word "Anasazi" is [[Social:Navajo language|Navajo]] for "enemy ancestors" or "alien ancestors".<ref>{{oed|Anasazi}}</ref>

Archaeologists still debate when this distinct culture emerged. The current consensus, based on terminology defined by the Pecos Classification, suggests their emergence was around 1200&nbsp;{{small|[[History:Before Common Era|BCE]]}} during the Basketmaker II Era. Beginning with the earliest explorations and excavations, researchers have believed that the Ancestral Puebloans are ancestors of the modern Pueblo peoples.<ref name="UNCO">{{cite web|url=http://hewit.unco.edu/DOHIST/puebloan/begin.htm|title=Getting Started|work=The Ancestral Puebloans|publisher=Hewit Institute, University of Northern Colorado|access-date=October 22, 2010|url-status=dead|archive-url=https://web.archive.org/web/20100709073248/http://hewit.unco.edu/dohist/puebloan/begin.htm|archive-date=July 9, 2010|df=mdy-all}}</ref>

In addition to the Ancestral Puebloans, a number of distinct cultures have inhabited the Grand Canyon area. The Cohonina lived to the west of the Grand Canyon, between 500 and 1200&nbsp;{{small|CE}}.<ref name=Tufts/><ref>{{cite web | title = Kaibab National Forest | publisher = USDA Forest Service | url = http://www.fs.fed.us/r3/kai/recreation/historic/tusayan.shtml | archive-url = https://web.archive.org/web/20090210165142/http://www.fs.fed.us/r3/kai/recreation/historic/tusayan.shtml | archive-date = February 10, 2009 | access-date = January 4, 2007}}</ref> The Cohonina were ancestors of the Yuman, Havasupai, and Hualapai peoples who inhabit the area today.<ref name="McGregor1951">{{cite book|last=McGregor|first=John Charles|title=The Cohonina culture of northwestern Arizona|url=https://archive.org/details/cohoninacultureo0000mcgr_x1r5|url-access=registration|year=1951|publisher=University of Illinois Press|pages=[https://archive.org/details/cohoninacultureo0000mcgr_x1r5/page/1 1–7]}}</ref>

The Sinagua were a cultural group occupying an area to the southeast of the Grand Canyon, between the Little Colorado River and the Salt River, between approximately 500 and 1425 {{small|CE}}. The Sinagua may have been ancestors of several Hopi clans.

By the time of the arrival of Europeans in the 16th{{nbsp}}century, newer cultures had evolved. The Hualapai inhabit a {{convert|100|mi|km|adj=on}} stretch along the pine-clad southern side of the Grand Canyon. The Havasupai have been living in the area near Cataract Canyon since the beginning of the 13th{{nbsp}}century, occupying an area the size of Delaware.<ref name="Whiting">{{cite book|last=Whiting|first=A.F.|title=Havasupai Habitat|url=https://archive.org/details/havasupaihabitat0000whit|url-access=registration|location=Tucson, Arizona|publisher=University of Arizona Press|year=1985|isbn=978-0816508662}}</ref> The Southern Paiutes live in what is now southern Utah and northern Arizona. The Navajo, or Diné, live in a wide area stretching from the [[Earth:San Francisco Peaks|San Francisco Peaks]] eastwards towards the Four Corners. Archaeological and linguistic evidence suggests the Navajo descended from the Athabaskan people near Great Slave Lake, Canada, who migrated after the 11th{{nbsp}}century.<ref>{{cite web | title=Discovery of the Athabascan Origin of the Apache and Navajo Language | publisher=Watkins, Thayer – San Jose State University | url=http://www.sjsu.edu/faculty/watkins/navajo.htm | access-date=July 30, 2014 | url-status=live | archive-url=https://web.archive.org/web/20141112211856/http://www.sjsu.edu/faculty/watkins/navajo.htm | archive-date=November 12, 2014 | df=mdy-all }}</ref> In the mythology of some Third Mesa Hopi communities, the Grand Canyon was the location humankind arose out of the [[Religion:Hopi mythology#Four Worlds|Third World]] from a sipapu.<ref>{{cite book |last1=Courlander |first1=Harold |last2=Harmon |first2=Daniel |title=The Fourth World of the Hopis |url=https://books.google.com/books?id=dgcUguU8ajwC&q=grand+canyon+hopi+fourth+world&pg=PA214 |publisher=UNM Press |year=1971 |page=214|isbn=978-0826310118 }}</ref>

===European arrival and settlement===

====Spanish explorers====
[[File:La conquista del Colorado.jpg|thumb|''La conquista del Colorado'' (2017), by Augusto Ferrer-Dalmau, depicts Francisco Vázquez de Coronado's 1540–1542 expedition. García López de Cárdenas can be seen overlooking the Grand Canyon.]]

In September 1540, under orders from the conquistador Francisco Vázquez de Coronado to search for the fabled Seven Cities of Cibola, Captain García López de Cárdenas, along with Hopi guides and a small group of Spanish soldiers, traveled to the south rim of the Grand Canyon between Desert View and Moran Point. Pablo de Melgrossa, Juan Galeras, and a third soldier descended some one third of the way into the canyon until they were forced to return because of lack of water. In their report, they noted that some of the rocks in the canyon were "bigger than the great tower of Seville, Giralda".<ref name="greatabyss">{{cite book |first=Page|last=Stegner |title=Grand Canyon, The Great Abyss|url=https://archive.org/details/grandcanyongreat00steg|url-access=registration|year= 1994|publisher= HarperCollins|isbn=978-0062585646| page=[https://archive.org/details/grandcanyongreat00steg/page/25 25]}}</ref> It is speculated that their Hopi guides likely knew routes to the canyon floor, but may have been reluctant to lead the Spanish to the river. No Europeans visited the canyon again for more than two hundred years.

Fathers Francisco Atanasio Domínguez and Silvestre Vélez de Escalante were two Spanish priests who, with a group of Spanish soldiers, explored southern Utah and traveled along the north rim of the canyon in Glen and Marble Canyons in search of a route from Santa Fe to California in 1776. They eventually found a crossing, formerly known as the "Crossing of the Fathers", that today lies under Lake Powell.

Also in 1776, Fray Francisco Garces, a Franciscan missionary, spent a week near Havasupai unsuccessfully attempting to convert a band of Native Americans to Christianity. He described the canyon as "profound".<ref name="greatabyss"/>

====American exploration====
James Ohio Pattie, along with a group of American trappers and mountain men, may have been the next European to reach the canyon, in 1826.<ref>{{cite journal |last1=Kroeber |first1=A. L. |last2=Kroeber |first2=Clifton B. |last3=Euler |first3=R. C. |last4=Schreoder |first4=A. H. |title=The Route of James O. Pattie on the Colorado in 1826: A Reappraisal by A. L. Kroeber |journal=Arizona and the West |date=1964 |volume=6 |issue=2 |pages=119–136 |jstor=40167806 |url=https://www.jstor.org/stable/40167806 |access-date=21 June 2022 |language=en}}</ref><ref>{{cite journal|url=https://books.google.com/books?id=Xm5IAAAAYAAJ&pg=PA243 |title=New light on Pattie and the southwestern fur trade|first=Joseph J.|last=Hill|journal=Southwestern Historical Quarterly|volume=26|issue=4|year=1923}}</ref>

Jacob Hamblin, a Mormon missionary, was sent by Brigham Young in the 1850s to locate suitable river crossing sites in the canyon. Building good relations with local Hualapai and white settlers, he reached the Crossing of the Fathers,<ref>{{cite web |title=Canyon Club hosts presentation on Crossing of the Fathers |url=https://lakepowellchronicle.com/article/canyon-club-hosts-presentation-on-crossing-of-the-fathers |website=Lake Powell Chronicle |access-date=21 June 2022}}</ref> crossed the location that would become Lees Ferry on a raft in 1858<ref name="Lee">{{cite web |title=Lee's Ferry Historic Site |url=https://pagelakepowellhub.com/historic-sites/ |website=The Page-Lake Powell Hub |access-date=21 June 2022}}</ref> and Pearce Ferry (later operated by, and named for, [[Biography:Joseph Pearce|Harrison Pearce]]).<ref>{{cite web |title=Pearce Ferry |url=https://www.westernriver.com/grand-canyon-river-trip/mile-by-mile-280-pearce-ferry |website=Western River Expeditions |access-date=21 June 2022 |language=en}}</ref> He also acted as an advisor to John Wesley Powell, before his second expedition to the Grand Canyon, serving as a diplomat between Powell and the local native tribes to ensure the safety of his party.<ref name="Lee"/>

[[File:GRAND CANYON OF THE COLORADO, MOUTH OF PARIA CREEK, LOOKING WEST FROM PLATUEAU - NARA - 524227.tif|left|thumb|upright|William Bell's photograph of the Grand Canyon, taken in 1872 as part of the Wheeler expedition]]

In 1857, Edward Fitzgerald Beale was superintendent of an expedition to survey a wagon road along the 35th parallel from Fort Defiance, Arizona to the Colorado River. He led a small party of men in search of water on the [[Earth:Coconino Plateau|Coconino Plateau]] near the canyon's south rim. On September 19, near present-day National Canyon, they came upon what May Humphreys Stacey described in his journal as "a wonderful canyon; four thousand feet deep. Everybody in the party admitted that he never before saw anything to match or equal this astonishing natural curiosity."<ref>{{cite book |last1=Stacey |first1=May Humphreys |title=Uncle Sam's camels; the journal of May Humphreys Stacey supplemented by the report of Edward Fitzgerald Beale (1857–1858) edited by Lewis Burt Lesley |date=1929 |publisher=Harvard University Press |location=Cambridge |page=100 |url=https://babel.hathitrust.org/cgi/pt?id=uva.x000664200&view=1up&seq=122&skin=2021&q1=%22wonderful%20canyon%22 |access-date=21 June 2022 |language=en}}</ref>

Also in 1857, the U.S. War Department asked Lieutenant Joseph Ives to lead an expedition to assess the feasibility of an up-river navigation from the Gulf of California. On December 31, 1857, Ives embarked from the mouth of the Colorado  in the [[Engineering:Paddle steamer|stern wheeler steamboat]] ''Explorer''. His party reached the lower end of Black Canyon on March 8, 1858, then continued on by rowboat past the mouth of the Virgin River after the ''Explorer'' struck a rock.<ref>{{cite book |last1=Tabor |first1=C C |title=The Ives Expedition of 1858 |url=https://cawaterlibrary.net/wp-content/uploads/2019/10/The-Ives-Expedition-of-1858.pdf |archive-url=https://web.archive.org/web/20220826162102/https://cawaterlibrary.net/wp-content/uploads/2019/10/The-Ives-Expedition-of-1858.pdf |archive-date=2022-08-26 |url-status=live |location=El Centro, Calif. |publisher= Imperial Irrigation District |date=1968  |access-date=21 June 2022}}</ref><ref>{{cite web |title=The Colorado Exploring Expedition (Ives Expedition) (1857–1858) |url=https://www.si.edu/object/auth_exp_fbr_EACE0014 |website=Smithsonian Institution |access-date=8 July 2022 |language=en}}</ref><!-- some two months after George Johnson. who? --> Ives led his party east into the canyon&nbsp;– they may have been the first Europeans to travel the Diamond Creek drainage.<ref>{{cite web |last1=Anderson |first1=Michael F. |title=Rim to River and Inner Canyon Trails – Nature, Culture and History at the Grand Canyon |url=https://grcahistory.org/sites/rim-to-river-and-inner-canyon-trails/ |website=Grand Canyon History |publisher=Arizona State University |access-date=8 July 2022}}</ref> In his "Report Upon the Colorado River of the West" to the Senate in 1861 Ives states that "The marvellous story of Cardinas, that had formed for so long a time the only record concerning this rather mythical locality, was rather magnified than detracted from by the accounts of one or two trappers, who professed to have seen the cañon".<ref>{{cite book |last1=Ives |first1=Joseph C. |title=Report Upon the Colorado River of the West |date=1861 |publisher=U.S. Government Printing Office |url=https://books.google.com/books?id=1xIOAAAAQAAJ&pg=PA21 |language=en}}</ref>

[[File:'Noon Day Rest in Marble Canyon' from the second Powell Expedition 1872.jpg|thumb|upright|Noon rest in Marble Canyon, second Powell Expedition, 1872]]
According to the ''San Francisco Herald'', in a series of articles run in 1853, Captain Joseph R. Walker in January 1851 with his nephew James T. Walker and six men, traveled up the Colorado River to a point where it joined the Virgin River and continued east into Arizona, traveling along the Grand Canyon and making short exploratory side trips along the way. Walker is reported to have said he wanted to visit the "Moqui" (Hopi) Indians. who he had met briefly before and found exceptionally interesting.<ref name="Gilbert">{{cite book |last1=Gilbert |first1=Bil |title=Westering Man: The Life of Joseph Walker |date=1985 |publisher=University of Oklahoma Press |isbn=978-0806119342 |pages=236–238 |url=https://books.google.com/books?id=h7BQjaTxHy8C&q=Moqui |access-date=8 July 2022 |language=en}}</ref>

In 1858, John Strong Newberry became probably the first geologist to visit the Grand Canyon.<ref>{{Cite book|url=https://books.google.com/books?id=cmEgAAAAIAAJ&q=In+1858,+John+Strong+Newberry+became+the+first+geologist+to+visit+the+Grand+Canyon|title=Geomorphology before Davis|last=Chorley|first=Richard J.|year=1984|publisher=Methuen|language=en}}</ref>

In 1869, Major John Wesley Powell set out to explore the Colorado River and the Grand Canyon in the first expedition down the canyon. Powell ordered a shipwright to build four reinforced Whitewall rowboats from Chicago and had them shipped west on the newly completed Continental railroad.<ref name="Stojka">{{cite web |last1=Stojka |first1=Andre |title=Shipping a boat over land west in 1869 |url=https://listen2read.com/getting-boat-west-1869/ |website=Listen2Read|date=October 7, 2015 |access-date=21 June 2022 }}</ref> He hired nine men, including his brother Walter, and collected provisions for ten months. They set out from Green River, Wyoming, on May 24.<ref name="Utah">{{cite web |title=Powell's 1869 Journey Down the Green and Colorado Rivers – Utah Geological Survey |url=https://geology.utah.gov/map-pub/survey-notes/powell-1869-river-journey/ |website=Utah Geological Survey |date=August 29, 2019 |access-date=21 June 2022}}</ref> On June 7, they lost one of their boats, 1/3 of their food, and other badly-needed supplies: as a result the team eventually had to subsist on starvation rations.<ref name="Howland"/>  Passing through (or portaging around) a series of dangerous rapids, the group passed down the [[Earth:Green River (Colorado River tributary)|Green River]], reaching its [[Earth:Confluence|confluence]] with the Colorado River, near present-day Moab, Utah, on July 17. Continuing on down the Colorado River, the party encountered more rapids and falls.<ref name="Ribokas">{{cite web |last1=Ribokas |first1=Bob |title=The Powell Expedition |url=https://www.kaibab.org/kaibab.org/powell/powexp.htm |website=Grand Canyon Explorer |access-date=21 June 2022}}</ref> On August 28, 1869, faced with what some felt to be impassable rapids, three men left the expedition on foot in an attempt to reach a settlement {{convert|75|mile}} away. Ironically, the remaining members went safely through the rapids on August 29, 1869, while Seneca Howland, Oramel Howland, and William H. Dunn were murdered.<ref name="Howland"/> The area through which the three men traveled was marked by tensions between farming and hunting Shivwits and incoming Mormon settlers. Which group was responsible for killing the three men has been hotly debated.<ref name="Waterman">{{cite web |last1=Waterman |first1=Jonathan |title=Seeking Hard Desert Truth |url=https://jonathanwaterman.com/media/2020/7/johnwesleypowell-expedition.pdf |archive-url=https://web.archive.org/web/20200926233347/https://jonathanwaterman.com/media/2020/7/johnwesleypowell-expedition.pdf |archive-date=2020-09-26 |url-status=live |website=jonathanwaterman.com |access-date=21 June 2022}}</ref> Powell himself visited the area the following year, and was told (through a Mormon interpreter) that the Shivwits had mistakenly killed the men, believing them to be prospectors who had murdered an Indian woman. He choose to smoke a peace pipe with them.<ref name="Howland">{{cite news |title=Oramel G. Howland (1833–1869) Seneca B. Howland (1843–1869) William Dunn (? – 1869) |url=http://www.shoppbs.pbs.org/wgbh/amex/canyon/peopleevents/pandeAMEX02.html |access-date=21 June 2022 |work=American Experience |agency=PBS}}</ref><ref>{{cite news |title=John Wesley Powell's Undertakings |url=https://www.pbs.org/wgbh/americanexperience/features/john-wesley-powell-undertakings/ |access-date=21 June 2022 |work=American Experience |agency=PBS |language=en}}</ref>
Powell went on to become  the first Director of the U.S. Bureau of Ethnology of the Smithsonian Institution (1879–1902) and the second Director  of the US Geological Survey (1881–1894).<ref>{{cite web |title=John Wesley Powell |url=https://www.usgs.gov/staff-profiles/john-wesley-powell |website=U.S. Geological Survey |access-date=21 June 2022}}</ref>  He was the first to use the term "Grand Canyon", in 1871; previously it had been called the "Big Canyon".<ref>[http://www.etymonline.com/index.php?term=grand&allowed_in_frame=0 ''Grand''] {{webarchive|url=https://web.archive.org/web/20160304110153/http://www.etymonline.com/index.php?term=grand&allowed_in_frame=0 |date=March 4, 2016 }}, Etymonline.com</ref>

In 1889, Frank M. Brown wanted to build a railroad along the Colorado River to carry coal. He, his chief engineer Robert Brewster Stanton, and 14 others started to explore the Grand Canyon in poorly designed cedar wood boats, with no life preservers. Brown drowned in an accident near Marble Canyon: Stanton made new boats and proceeded to explore the Colorado all of the way to the Gulf of California.<ref>{{cite web|url=http://www.nps.gov/history/history/online_books/geology/publications/bul/1508/sec4.htm |archive-url=https://web.archive.org/web/20121106185414/http://www.nps.gov/history/history/online_books/geology/publications/bul/1508/sec4.htm |archive-date=November 6, 2012 |work=The Geologic Story of Colorado National Monument |title=Late Arrivals |publisher=United States Geological Survey |id=Geological Survey Bulletin 1508 |access-date=November 7, 2010 |url-status=dead }}</ref>

The Grand Canyon became an official national monument in 1908 and a national park in 1919.<ref>{{cite web|url=http://explorethecanyon.com/explore-learn/grand-canyon-facts/|title=Grand Canyon Facts|work=National Geographic Visitor Center, Arizona|url-status=live|archive-url=https://web.archive.org/web/20160219170547/http://explorethecanyon.com/explore-learn/grand-canyon-facts/|archive-date=February 19, 2016|df=mdy-all}}</ref>

====Settlers in and near the canyon====
[[File:15742 Grand Canyon Historic - David Rust Tipoff c. 1910 (4738929263).jpg | thumb | right | David Rust, {{c.|1910}}]]
* Miners: "Captain" John Hance,<ref>{{cite journal |last1=Billingsley |first1=George |last2=Spamer |first2=Earle |title=Quest for the pillar of gold : The mines and miners of the Grand Canyon |journal=Grand Canyon Association (Monograph No. 10) |date=1 January 1997 |url=https://www.academia.edu/36778125}}</ref> William W. Bass,<ref>{{cite web |title=William Wallace Bass Collection |url=http://www.azarchivesonline.org/xtf/view?docId=ead/nau/ahs_bass.xml&doc.view=print;chunk.id=0 |website=Arizona Historical Society |access-date=8 July 2022}}</ref> Louis Boucher "The Hermit",<ref>{{cite news |last1=Drew |first1=Dr Daryl |title=Louis Boucher: Canadian Guide of the Grand Canyon {{!}} Canadian Cowboy Country Magazine |url=https://cowboycountrymagazine.com/2016/02/louis-boucher-canadian-guide-of-the-grand-canyon/ |access-date=8 July 2022 |work=Cowboy Country Magazine.com |date=1 February 2016}}</ref> Seth Tanner,<ref>{{cite web |title=Seth Tanner |url=http://www.allhikers.com/History/Seth-Tanner.htm |website=All Hikers |access-date=8 July 2022}}</ref> Charles Spencer,<ref>{{cite web |title=Charles Spencer collection, 1910–1920 Spencer (Charles) collection |url=http://www.azarchivesonline.org/xtf/view?docId=ead/mna/MNA_MS023_Spencer.xml;query=ms-023;brand=default |website=Arizona Archives Online |access-date=8 July 2022}}</ref> D.W. "James" Mooney<ref>{{cite web |title=The Tunnels In Mooney Falls, Havasu Canyon |url=http://tchester.org/znet/grand_canyon/mooney.html |website=tchester.org |access-date=8 July 2022}}</ref>
* Lees Ferry: John Doyle Lee, Emma Lee French (17th of John Lee's 19 wives),<ref>{{cite web |title=Lees Ferry History |url=https://www.nps.gov/glca/learn/historyculture/leesferryhistory.htm |website=Glen Canyon National Recreation Area (U.S. National Park Service) |access-date=8 July 2022 |language=en}}</ref> James Simpson Emmett<ref>{{cite journal |last1=St. John Stott |first1=Graham |title=Zane Grey and James Simpson Emmett |journal=Brigham Young University Studies |date=1978 |volume=18 |issue=4 |pages=491–503 |jstor=43040779 |url=https://www.jstor.org/stable/43040779 |access-date=8 July 2022 |issn=0007-0106}}</ref>
* Phantom Ranch: David Rust,<ref>{{cite book |last1=Swanson |first1=Frederick H. |title=Dave Rust : a life in the canyons |date=2007 |publisher=University of Utah Press |location=Salt Lake City |isbn=978-0874809152}}</ref> Mary Colter<ref name="Berke">{{cite book |last1=Berke |first1=Arnold |title=Mary Colter, architect of the Southwest |date=2002 |publisher=Princeton Architectural Press |location=New York |isbn=978-1568983455}}</ref><ref name="Grattan">{{cite book |last1=Grattan |first1=Virginia L. |title=Mary Colter, builder upon the red earth |date=1992 |publisher=Northland Press |location=Grand Canyon, Arizona |isbn=978-0938216452}}</ref>
* Grand Canyon Village: Ralph H. Cameron,<ref>{{cite news |last1=Sowards |first1=Adam M. |title=The Man Who Tried to Claim the Grand Canyon |url=https://daily.jstor.org/the-man-who-tried-to-claim-the-grand-canyon/ |access-date=8 July 2022 |work=JSTOR Daily |date=31 July 2019}}</ref> Emery & Ellsworth Kolb<ref name="Kolb">{{cite web |title=The Kolb Brothers |url=https://library.nau.edu/speccoll/exhibits/daysofarchives/film.html |website=Northern Arizona University Library |access-date=8 July 2022}}</ref>

====Federal protection: National Monument and Park====
[[File:RAILWAY STATION AND EL TOVAR HOTEL, FACING WNW Grand Canyon Village. 1994, HAER.jpg|thumb|Railway Station and El Tovar Hotel, Facing WNW, Grand Canyon Village. 1994 photo, HAER ]]
[[File:Grand Canyon National Park, Fred Harvey, The Towering Cliffs above Hermit Camp (NBY 20816).jpg|thumb|Fred Harvey postcard, The Towering Cliffs above Hermit Camp ]]
U.S. President Theodore Roosevelt visited the Grand Canyon in 1903.  An avid outdoorsman and staunch conservationist, Roosevelt established the Grand Canyon Game Preserve on November 28, 1906. Livestock grazing was reduced, but predators such as mountain lions, eagles, and wolves were eradicated. Roosevelt along with other members of his conservation group, the Boone and Crockett Club helped form the National Parks Association, which in turn lobbied for the Antiquities Act of 1906 which gave Roosevelt the power to create national monuments. Once the act was passed, Roosevelt immediately added adjacent national forest lands and redesignated the preserve a U.S. National Monument on January 11, 1908.<ref>{{cite web|last1=Sheldon|first1=Charles|title=History of the Boone and Crockett Club|url=http://scholarworks.umt.edu/cgi/viewcontent.cgi?article=1000&context=sheldon|website=University of Montana Mansfield Library|publisher=Boone and Crockett Club|access-date=February 24, 2017|ref=Pgs 15–57|url-status=live|archive-url=https://web.archive.org/web/20170225133129/http://scholarworks.umt.edu/cgi/viewcontent.cgi?article=1000&context=sheldon|archive-date=February 25, 2017|df=mdy-all}}</ref> Opponents such as land and mining claim holders blocked efforts to reclassify the monument as a U.S. National Park for 11 years. Grand Canyon National Park was finally established as the 17th U.S. National Park by an Act of Congress signed into law by President [[Biography:Woodrow Wilson|Woodrow Wilson]] on February 26, 1919.<ref name=Tufts>{{cite book|title=Secrets in The Grand Canyon, Zion and Bryce Canyon National Parks|edition=Third|first=Lorraine Salem|last=Tufts|location=North Palm Beach, Florida|publisher=National Photographic Collections|year=1998|pages=12–13|isbn=978-0962025532}}</ref>

The federal government administrators who manage park resources face many challenges. These include issues related to the recent reintroduction into the wild of the highly endangered [[Biology:California condor|California condor]], air tour overflight noise levels, water rights<ref name="Denetclaw">{{cite news |last1=Denetclaw |first1=Pauly |title=Colorado River, stolen by law |url=https://www.hcn.org/issues/54.3/indigenous-affairs-colorado-river-stolen-by-law |access-date=1 July 2022 |work=High Country News |date=March 1, 2022}}</ref> and management disputes, and forest fire management.

The canyon's ecosystem was permanently changed after the construction of the Glen Canyon Dam in 1963. Average flood levels dropped from 85,000 to 8,000 cubic ft/sec.  In the absence of natural flooding, sandbars and beaches eroded and invasive species  began to displace native species. Federal officials started releasing floods in the Grand Canyon in hopes of restoring its [[Earth:Ecosystem|ecosystem]] beginning with 1996, 2004, and 2008.<ref name="Witze"/><ref>{{cite news | first = A.L. | last = Myers | title = Three-Day Grand Canyon Flood Aims to Restore Ecosystem | agency = Associated Press | url = http://news.nationalgeographic.com/news/2008/03/080306-AP-grand-canyo.html | date = March 6, 2008 | url-status=dead | archive-url = https://web.archive.org/web/20160304080434/http://news.nationalgeographic.com/news/2008/03/080306-AP-grand-canyo.html | archive-date = March 4, 2016 | df = mdy-all }}</ref> 
In 2018, the Department of Interior started experimenting with “adaptive management” of the Glen Canyon Dam, using a High-Flow Experiment (HFE) water release to shift volumes of sand and monitoring effects such as the dispersal of invasive tamarisk seeds.<ref>{{cite web |title=On-going experiment in high-volume CO River releases from Glen Canyon Dam set {{!}} Arizona Department of Water Resources |url=https://new.azwater.gov/news/articles/2018-01-11 |website=Arizona Department of Water Resources |access-date=24 June 2022|date=November 1, 2018}}</ref>
However, as of 2022, extreme drought has caused water levels in Lake Powell to drop so much that a planned release of water has been delayed, to ensure that the Glen Canyon Dam can continue to generate hydropower.<ref name="Hager">{{cite news |last1=Hager |first1=Alex |title=Lake Powell water level: Feds announce measures to help Glen Canyon Dam hydropower |url=https://cronkitenews.azpbs.org/2022/05/04/lake-powell-water-level-feds-announce-help-glen-canyon-dam-hydropower/ |access-date=23 June 2022 |work=Cronkite News – Arizona PBS |date=4 May 2022}}</ref>

Between 2003 and 2011, 2,215 mining claims had been requested that are adjacent to the canyon, including claims for uranium mines.<ref name="Carus"/> Critics of uranium mining are concerned that uranium will leach into the aquifers feeding the Colorado River and contaminate the water supply for up to 18 million people.<ref name="Carus">{{cite news|title=Demand for uranium threatens Grand Canyon biodiversity|url=https://www.theguardian.com/environment/2011/feb/17/uranium-demand-grand-canyon-biodiversity|newspaper=The Guardian|first=Felicity|last=Carus|date=February 17, 2011|url-status=live|archive-url=https://web.archive.org/web/20170226013923/https://www.theguardian.com/environment/2011/feb/17/uranium-demand-grand-canyon-biodiversity|archive-date=February 26, 2017|df=mdy-all}}</ref>  In 2009, U.S. Interior Secretary Ken Salazar  published a Notice of Intent to suspend approvals for new uranium mining in the area.<ref name="Zinke">{{cite web |title=United States Court of Appeals for the Ninth Circuit No. 14-17350 |url=https://cdn.ca9.uscourts.gov/datastore/opinions/2017/12/12/14-17350.pdf |archive-url=https://web.archive.org/web/20180728102945/http://cdn.ca9.uscourts.gov/datastore/opinions/2017/12/12/14-17350.pdf |archive-date=2018-07-28 |url-status=live |website=United States Courts for the Ninth Circuit |access-date=30 June 2022}}</ref>  In 2012, Salazar established a 20-year moratorium (known as the "Northern Arizona Withdrawal") withdrawing {{convert|1|e6acre|km2}} from the permitting process for uranium and hardrock mining, stating "People from all over the country and around the world come to visit the Grand Canyon. Numerous American Indian tribes regard this magnificent icon as a sacred place and millions of people in the Colorado River Basin depend on the river for drinking water, irrigation, industrial and environmental use."<ref name="Salazar">{{cite news |title=Secretary Salazar Announces Decision to Withdraw Public Lands near Grand Canyon from New Mining Claims |url=https://www.doi.gov/news/pressreleases/Secretary-Salazar-Announces-Decision-to-Withdraw-Public-Lands-near-Grand-Canyon-from-New-Mining-Claims |access-date=30 June 2022 |work=United States Department of the Interior |date=9 January 2012 |language=en}}</ref>  However, Salazar's 20-year moratorium on new mines still allows mines with previous authorization to operate.<ref name="Salazar"/>

Multiple challenges have been brought into court both against the moratorium and against the operation of uranium mines in the area.<ref name="Clark">{{cite news |last1=Clark |first1=Roger |title=Grand Canyon Uranium Decisions Loom Large in 2017 |url=https://www.grandcanyontrust.org/blog/grand-canyon-uranium-decisions-loom-large-2017 |access-date=30 June 2022 |work=Grand Canyon Trust |date=6 January 2017 |language=en}}</ref>  The federal government's 2012 moratorium was upheld by the U.S. District Court for Arizona in 2014, but appealed in November 2014 as  ''National Mining Association v. Jewell'' (No. 14-17350).<ref>{{cite news|author1=Curtis Spicer|title=Arizona continues to push for new uranium mines near Grand Canyon|url=https://www.azcentral.com/story/news/local/arizona/2015/09/24/arizona-uranium-mines-grand-canyon/72741520/|access-date=January 7, 2016|work=The Arizona Republic|agency=Cronkite News Service|date=September 24, 2015}}</ref> The 9th Circuit Court of Appeals again upheld the moratorium in 2017, stating that the Secretary of the Interior held valid withdrawal authority.<ref name="Zinke"/>

''Havasupai Tribe v. Provencio''  was also argued at multiple court levels based on multiple grounds.  The Havasupai people and the Grand Canyon Trust sought to block the reopening of the Pinyon Plain Mine (formerly Canyon Uranium Mine). Activity at the mine had ceased in 1992, ten years prior to the moratorium on new development in 2012. Appellants challenged the U.S. Forest Service's consultation process for approving reopening of the mine. As of February 22, 2022, the 9th U.S. Circuit Court of Appeals rejected the arguments in No. 20-16401, concluding that the Forest Service had not acted arbitrarily in making its decision.<ref name="Crane">{{cite news |last1=Crane |first1=Steve |title=Uranium mine near Grand Canyon permitted by court, despite mining ban |url=https://cronkitenews.azpbs.org/2022/02/22/uranium-mine-near-grand-canyon-permitted-by-court-despite-mining-ban/ |access-date=30 June 2022 |work=Cronkite News – Arizona PBS |date=23 February 2022}}</ref><ref name="Grzincic">{{cite news |last1=Grzincic |first1=Barbara |title=Court greenlights uranium mine in national forest |url=https://www.reuters.com/legal/litigation/court-greenlights-uranium-mine-national-forest-2022-02-23/ |access-date=30 June 2022 |work=Reuters |date=23 February 2022 |language=en}}</ref>

A study examining samples of groundwater from 180 spring sites and 26 wells in the Grand Canyon region has assessed the presence of uranium in groundwater from September 1, 1981, to October 7, 2020. The goal of the study was  to establish a baseline assessment of groundwater conditions in the Grand Canyon region. At 95% of sites, maximum observed uranium concentrations were below the EPA{{’}}s Maximum Contaminant Level for drinking water, 30&nbsp;µg/L. At 86% of sites, uranium concentrations were below the Canadian level for protection of freshwater aquatic life, 15&nbsp;µg/L.<ref name="Tillman">{{cite journal |last1=Tillman |first1=Fred D. |last2=Beisner |first2=Kimberly R. |last3=Anderson |first3=Jessica R. |last4=Unema |first4=Joel A. |title=An assessment of uranium in groundwater in the Grand Canyon region |journal=Scientific Reports |date=16 November 2021 |volume=11 |issue=1 |pages=22157 |doi=10.1038/s41598-021-01621-8 |pmid=34785687 |pmc=8595346 |bibcode=2021NatSR..1122157T |language=en |issn=2045-2322}}</ref>

On August 8, 2023, it was announced that U.S. President Joe Biden will designate Baaj Nwaavjo I’tah Kukveni – Ancestral Footprints of the Grand Canyon National Monument, a move aimed at conserving nearly 1 million acres of greater Grand Canyon landscape.<ref>{{Cite web |last= |first= |date=2023-08-08 |title=Biden designates new national monument surrounding the Grand Canyon, blocking mining {{!}} CNN Politics |url=https://www.cnn.com/2023/08/08/politics/joe-biden-national-monument-grand-canyon/index.html |access-date=2023-08-10 |website=CNN |language=en}}</ref>

==South Rim buildings==
There are several historic buildings located along the South Rim with most in the vicinity of Grand Canyon Village.
[[Image:Yavapai Observation Station.jpg|thumb|upright|Desert View Watchtower in 2004|right]]
* Buckey O'Neill Cabin was built during the 1890s by William Owen "Buckey" O'Neill. He built the cabin because of a copper deposit that was nearby. He had several occupations such as miner, judge, politician, author and tour guide. This cabin is the longest continually standing structure on the South Rim.<ref>{{cite book |last1=Moore |first1=Randy |last2=Witt |first2=Kara Felicia |title=The Grand Canyon: An Encyclopedia of Geography, History, and Culture |year=2018 |publisher=ABC-CLIO |isbn=978-1610698405 |url=https://books.google.com/books?id=ngldDwAAQBAJ&pg=PA279 |language=en}}</ref>  It is currently used as a guest house; booking is required well in advance.
* Kolb Studio was built in 1904 by brothers Ellsworth and Emery Kolb. They were photographers who made a living by photographing visitors walking down the Bright Angel Trail. In 1911, the Kolb brothers filmed their journey down the Green and [[Earth:Colorado River|Colorado River]]s. Emery Kolb showed this movie regularly in his studio until 1976 when he died at the age of 95. Today the building serves as an art gallery and exhibit.<ref name="Kolb"/>
* The El Tovar Hotel was built in 1905 as a luxury hotel for the Atchison, Topeka, and Santa Fe Railway, on the South Rim near the railway's main line. It was designed by Charles Whittlesley, a staff architect for the railway. The hotel is reminiscent of a Swiss chalet or Norwegian villa, combined with local materials for a rustic appearance<ref name="Harrison">{{cite book |last1=Harrison |first1=Laura Soulliere |title=Architecture in the Parks: National Historic Landmark Theme Study |date=1986 |publisher=Department of the Interior |location=Washington, D.C. |isbn=978-0365027799 |edition=1st |url=http://www.npshistory.com/publications/architecture-in-the-parks.pdf |archive-url=https://web.archive.org/web/20170113052001/http://npshistory.com/publications/architecture-in-the-parks.pdf |archive-date=2017-01-13 |url-status=live |access-date=8 July 2022}}</ref>  sometimes called "National Park Service rustic."<ref>{{cite web |title=National Park Service: Rustic Architecture 1916–1942 |url=https://www.nps.gov/parkhistory/online_books/rusticarch/introduction.htm |website=National Park Service |access-date=8 July 2022}}</ref><ref name="Glick">{{cite book |last1=Glick |first1=Marshall |title=National Park Service Rustic: Historic Architecture of California |date=2015 }}</ref> It consists of 4 stories, with a gift shop and restaurant located inside the hotel.
* Hopi House was built by Mary Jane Colter in 1905. It is based on structures that were built in an ancient Hopi settlement called Old Oraibi, located on the Third Mesa in eastern Arizona. It served as a residence for the Hopi Indians who sold arts and crafts to South Rim visitors.<ref name="Grattan"/><ref name="Berke"/>
* Verkamp's Curios, which stands next to the Hopi House, was built by John Verkamp in 1905. He sold arts and crafts as well as souvenirs. Until September 2008, it was run by his descendants;<ref>{{cite book |last1=Stampoulos |first1=Linda L. |title=Visiting the Grand Canyon: Views of Early Tourism |date=2004 |publisher=Arcadia Publishing |location=Charleston, South Carolina |isbn=978-1439649886 |url=https://books.google.com/books?id=--zBCQAAQBAJ&pg=PA53 |access-date=8 July 2022 |language=en}}</ref> in November 2008, the building reopened as a visitor center focusing on the history of the Grand Canyon Village community.<ref>{{cite news |title=Verkamp's building reopens with exhibits on community |url=https://www.williamsnews.com/news/2008/nov/25/verkamps-building-reopens-with-exhibits-on-commun/ |access-date=8 July 2022 |work=Grand Canyon News |date=November 25, 2008 |language=en}}</ref>

[[File:Grandcanyon railroad.jpg|thumb|1923-built [[Engineering:Steam locomotive|steam locomotive]] No. 4960 at the Grand Canyon Depot]]
* Grand Canyon Railway Depot was completed in 1910 and contains 2 levels. Gordon Chappell, Regional Historian for the Park Service, claims that this depot building is one of only three log-cabin-style train stations currently standing, out of fourteen ever built in the U.S.<ref>{{cite book|first=Gordon|last=Chappell|title=Statements on Architectural and Historical Significance|year=1985|publisher=National Park Service, Western Regional Office}}</ref> The depot is the northern terminus of the Grand Canyon Railway which begins in Williams, Arizona.<ref>{{cite web |last1=Wadzinski |first1=Gloria |title=Ride the Train to the Grand Canyon |url=https://www.mygrandcanyonpark.com/things-to-do/guided-tours/grand-canyon-railway-train/ |website=Grand Canyon National Park Trips |access-date=8 July 2022 |language=en |date=2 August 2021}}</ref><ref>{{cite web |title=History of the Grand Canyon Railway |url=https://www.canyontours.com/guides/history-of-the-grand-canyon-railway/ |website=Canyon Tours |access-date=8 July 2022 |date=4 May 2018}}</ref>
* Lookout Studio, another Mary Colter design, was built in 1914. Photography, artwork, books, souvenirs, and rock and fossil specimens are sold here. A great view of Bright Angel Trail can be seen here.<ref name="Grattan"/><ref name="Berke"/>
* Desert View Watchtower, one of Mary Colter's best-known works, was built in 1932. Situated at the far eastern end of the South Rim, {{convert|27|mile|km}} from Grand Canyon Village, the tower stands {{convert|70|ft|m}} tall. The top of the tower is {{convert|7522|ft|m}} above sea level, the highest point on the South Rim. It offers one of the few full views of the bottom of the canyon and the Colorado River. It was designed to mimic Ancestral Puebloans watchtowers, though, with four levels, it is significantly taller than historical towers.<ref>{{cite web | url=http://www.scienceviews.com/parks/watchtower.html | title=Grand Canyon Desert View Watchtower | url-status=live | archive-url=https://web.archive.org/web/20160210175238/http://scienceviews.com/parks/watchtower.html | archive-date=February 10, 2016 | df=mdy-all }}</ref><ref name="Grattan"/><ref name="Berke"/>
* Bright Angel Lodge was built of logs and stone in 1935. Mary Colter designed the lodge and it was built by the Fred Harvey Company. Inside the lodge is a small museum honoring Fred Harvey (1835–1901), who played a major role in popularizing the Grand Canyon. In the History Room is a stone fireplace layered in the same sequence as those in the canyon.<ref name="Grattan"/><ref name="Berke"/>

==Weather==
Weather in the Grand Canyon varies according to elevation. The forested rims are high enough to receive winter snowfall, but along the Colorado River in the Inner Gorge, temperatures are similar to those found in Tucson and other low elevation desert locations in Arizona. Conditions in the Grand Canyon region are generally dry, but substantial precipitation occurs twice annually, during seasonal pattern shifts in winter (when Pacific storms usually deliver widespread, moderate rain and high-elevation snow to the region from the west) and in late summer (due to the North American Monsoon, which delivers waves of moisture from the southeast, causing dramatic, localized thunderstorms fueled by the heat of the day).<ref name="gcweather">{{cite web|title=Grand Canyon National Park Weather |url=http://www.grand.canyon.national-park.com/weather.htm |archive-url=https://web.archive.org/web/20121005051849/http://www.grand.canyon.national-park.com/weather.htm |archive-date=October 5, 2012 |url-status=dead |date=2016-04-27 }}</ref> Average annual precipitation on the South Rim is less than {{convert|16|in|cm}}, with {{convert|60|in|cm}} of snow; the higher North Rim usually receives {{convert|27|in|cm}} of moisture, with a typical snowfall of {{convert|144|in|cm}}; and Phantom Ranch, far below the canyon's rims along the Colorado River at {{Convert|2500|feet|m}} gets just {{convert|8|in|cm}} of rain, and snow is a rarity.[[Image:GrandCanyonWinter2008.JPG|thumb|left|Grand Canyon covered with snow]]

Temperatures vary wildly throughout the year, with summer highs within the Inner Gorge commonly exceeding {{Convert|100|F}} and winter minimum temperatures sometimes falling below {{Convert|0|F|abbr=out|spell=in}} along the canyon's rims.<ref name="gcweather"/> Visitors are often surprised by these potentially extreme conditions, and this, along with the high altitude of the canyon's rims, can lead to unpleasant side effects such as [[Medicine:Dehydration|dehydration]], sunburn, and [[Physics:Hypothermia|hypothermia]].

Weather conditions can greatly affect hiking and canyon exploration, and visitors should obtain accurate forecasts because of hazards posed by exposure to extreme temperatures, winter storms and late summer monsoons. While the park service posts weather information at gates and visitor centers, this is a rough approximation only, and should not be relied upon for trip planning. For accurate weather in the canyon, hikers should consult the [[Earth:National Weather Service|National Weather Service]]'s NOAA weather radio or the official National Weather Service website.<ref>{{cite web | title = Flagstaff Weather Forecast Office | publisher = National Weather Service | url = http://www.wrh.noaa.gov/fgz/ | access-date = January 4, 2007}}</ref>

The National Weather Service has had a cooperative station on the South Rim since 1903. The record high temperature on the South Rim was {{Convert|105|F}} on June 26, 1974, and the record low temperature was {{Convert|-20|F}} on January 1, 1919, February 1, 1985, and December 23, 1990.<ref>{{cite web|url=http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?az3591|title=Grand Canyon National Park Climate Summary|publisher=Western Regional Climate Center|access-date=October 22, 2010|url-status=live|archive-url=https://web.archive.org/web/20120902033052/http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?az3591|archive-date=September 2, 2012|df=mdy-all}}</ref><ref>{{cite web|url=http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?az3595|title=Grand Canyon National Park Climate Summary|publisher=Western Regional Climate Center|access-date=October 22, 2010|url-status=live|archive-url=https://web.archive.org/web/20120902033151/http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?az3595|archive-date=September 2, 2012|df=mdy-all}}</ref><ref>{{cite web|url=http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?az3596|title=Grand Canyon National Park Climate Summary|publisher=Western Regional Climate Center|access-date=October 22, 2010|url-status=live|archive-url=https://web.archive.org/web/20100726054625/http://www.wrcc.dri.edu/cgi-bin/cliMAIN.pl?az3596|archive-date=July 26, 2010|df=mdy-all}}</ref>

===Air quality===
[[File:Grand Canyon NP-Arizona-USA.jpg|thumb|Smoke from prescribed fires on the South Rim, as seen from Yavapai Point, April 2007.<ref>{{cite web |url=http://www.nps.gov/grca/parknews/upload/3.08.07%20Grand%20Canyon%202007%20Prescribed%20Fire%20Plans.pdf |title=Grand Canyon News Release – Fire Managers Prepare to Implement Several Prescribed Fires |date=March 8, 2007 |access-date=April 11, 2012 |url-status=live |archive-url=https://web.archive.org/web/20100529105618/http://www.nps.gov/grca/parknews/upload/3.08.07%20Grand%20Canyon%202007%20Prescribed%20Fire%20Plans.pdf |archive-date=May 29, 2010 |df=mdy-all }}</ref>]]
{{As of|1999}} the Grand Canyon area had some of the cleanest air in the United States.<ref name="Project MOHAVE Final Report">
{{cite web
 |title=Project MOHAVE (Measurement of Haze and Visual Effects) Final Report
 |date=March 19, 1999
 |publisher=Interagency Monitoring of Protected Visual Environments (IMPROVE)
 |url=http://vista.cira.colostate.edu/improve/Studies/MOHAVE/Reports/FinalReport/mosec05.pdf
 |access-date=April 16, 2012
 |url-status=dead
 |archive-url=https://web.archive.org/web/20060919062308/http://vista.cira.colostate.edu/IMPROVE/Studies/MOHAVE/Reports/FinalReport/mosec05.pdf
 |archive-date=September 19, 2006
}}</ref>{{rp|p.5-2}}<ref name="IMPROVE viewer">
{{cite web
 |title=US Annual Spatial and Seasonal Patterns of PM2.5, Light Extinction and Contributions of Major Aerosol Types, 1996 – 1998
 |publisher=Interagency Monitoring of Protected Visual Environments (IMPROVE)
 |url=http://vista.cira.colostate.edu/improve/Data/Graphic_Viewer/seasonal.htm
 |access-date=June 27, 2011
 |url-status=dead
 |archive-url=https://web.archive.org/web/20100801171200/http://vista.cira.colostate.edu/improve/Data/Graphic_Viewer/seasonal.htm
 |archive-date=August 1, 2010
}} Note: Air quality as represented by PM-2.5 is shown by clicking the canyon's location on the map and selecting 'Fine Mass' from dropdown box above the map. Visibility is shown by selecting 'Deciview' from the dropdown box.</ref>
However,  air quality in the area can be affected by air pollution from coal-fired power plants, mining, oil and gas, vehicles, and urban and industrial pollution from nearby states, California and Mexico.<ref>{{cite web |title=Air Quality at Grand Canyon National |url=https://www.nps.gov/grca/learn/nature/airquality.htm |website=National Park Service |access-date=24 June 2022 |language=en}}</ref><ref>{{cite web |title=Park Air Profiles – Grand Canyon National Park |url=https://www.nps.gov/articles/airprofiles-grca.htm |website=National Park Service |access-date=24 June 2022 |language=en}}</ref><ref name="Nicla">{{cite news |last1=Nicla |first1=Andrew |title=Will power plant's closure help clear the air, restore the view of Grand Canyon? |url=https://www.azcentral.com/story/news/local/arizona-environment/2019/10/16/closure-navajo-generating-station-clear-air-over-grand-canyon/1710330001/ |access-date=24 June 2022 |work=The Arizona Republic |date=October 18, 2019}}</ref> Events such as forest fires and [[Earth:Dust storm|dust storm]]s in the Southwest can have a considerable impact.<ref name="Brewer">{{cite journal |last1=Brewer |first1=Patricia |last2=Moore |first2=Tom |title=Source Contributions to Visibility Impairment in the Southeastern and Western United States |journal=Journal of the Air & Waste Management Association |date=September 2009 |volume=59 |issue=9 |pages=1070–1081 |doi=10.3155/1047-3289.59.9.1070 |pmid=19785274 |bibcode=2009JAWMA..59.1070B |s2cid=42362472 |url=https://www.tandfonline.com/doi/pdf/10.3155/1047-3289.59.9.1070 |access-date=24 June 2022 |language=en |issn=1096-2247}}</ref>

Differences in visibility tend to be seasonal: best during the winter and poorest during the summer.<ref name="AQ2002">{{cite book |title=Air Quality in the National Parks |date=2002 |publisher=National Park Service Air Resources Division |location=Lakewood, Colorado |edition=2nd |url=http://npshistory.com/publications/air-quality/aqnps-2002.pdf |archive-url=https://web.archive.org/web/20190116050611/http://npshistory.com/publications/air-quality/aqnps-2002.pdf |archive-date=2019-01-16 |url-status=live |access-date=24 June 2022}}</ref>  
Winter cold fronts tend to carry clean, crisp air from the northwest, a less populated area. However they can also carry pollution from nearby mines and power plants. The average visibility during the winter is 160 miles, with the potential to reach 210 miles under ideal conditions. In the summer, prevailing winds from the southwest carry pollution from major urban and industrial centers, and visibility on average is only 100 miles. Within the canyon itself, smog can be trapped.<ref>{{cite web |title=Grand Canyon Breathtaking views |url=http://npshistory.com/brochures/grca/breathtaking-views.pdf |archive-url=https://web.archive.org/web/20220624204910/http://npshistory.com/brochures/grca/breathtaking-views.pdf |archive-date=2022-06-24 |url-status=live |website=National Park Service |access-date=24 June 2022}}</ref>

Air quality and visibility in the canyon are affected mainly by sulfates, soils, and organics. The sulfates largely result from urban emissions in southern California, borne on the prevailing [[Earth:Westerlies|westerly winds]] throughout much of the year, and emissions from Arizona's copper smelter region, borne on southerly or southeasterly winds during the monsoon. Airborne soils originate with windy conditions and road dust. Organic particles result from vehicle emissions, long-range transport from urban areas, and forest fires, as well as from [[Earth:Volatile organic compound|VOCs]] emitted by vegetation in the surrounding forests. Nitrates, carried in from urban areas, stationary sources, and vehicle emissions; as well as [[Earth:Black carbon|black carbon]] from forest fires and vehicle emissions, also contribute to a lesser extent.<ref name="IMPROVE viewer" /><ref name="intro vis">{{cite web
 |title=Introduction to Visibility
 |date=May 1999
 |author=((William C. Malm, Air Resources Division, National Park Service))
 |publisher=Cooperative Institute for Research in the Atmosphere (CIRA), Colorado State University
 |url=http://vista.cira.colostate.edu/improve/Education/intro_to_visibility.pdf
 |access-date=May 28, 2011
 |url-status=dead
 |archive-url=https://web.archive.org/web/20120211100049/http://vista.cira.colostate.edu/improve/Education/intro_to_visibility.pdf
 |archive-date=February 11, 2012
}}</ref>{{rp|26, 49–51}}

A number of actions have been taken to preserve and further improve air quality and visibility at the canyon.
In 1990, amendments to the Clean Air Act established the Grand Canyon Visibility Transport Commission (GCVTC) to advise the US EPA on strategies for protecting visual air quality on the [[Earth:Colorado Plateau|Colorado Plateau]]. The GCVTC released its final report in 1996 and initiated the Western Regional Air Partnership (WRAP), a partnership of state, tribal and federal agencies to help coordinate the implementation of the commission's recommendations.<ref>{{cite web
 |title       = Recommendations for Improving Western Vistas, Report of the Grand Canyon Visibility Transport Commission to the United States Environmental Protection Agency
 |date        = June 10, 1996
 |publisher   = Western Regional Air Partnership
 |url         = http://www.wrapair.org/WRAP/reports/GCVTCFinal.PDF
 |access-date  = May 17, 2012
 |url-status=live
 |archive-url  = https://web.archive.org/web/20120517110032/http://www.wrapair.org/WRAP/reports/GCVTCFinal.PDF
 |archive-date = May 17, 2012
 |df          = mdy-all
}}</ref><ref>{{cite web
 |title       = Western Regional Air Partnership
 |url         = http://www.wrapair2.org/
 |access-date  = April 19, 2012
 |url-status=live
 |archive-url  = https://web.archive.org/web/20120501112240/http://www.wrapair2.org/
 |archive-date = May 1, 2012
 |df          = mdy-all
}}</ref>

In 1999, the Regional Haze Rule established a goal of restoring visibility in national parks and wilderness areas (Class 1 areas), such as the Grand Canyon, to natural background levels by 2064. Subsequent revisions to the rule provide specific requirements for making reasonable progress toward that goal.<ref>
{{cite web
 |title       = Federal Register 40 CFR Part 51: Regional Haze Regulations and Guidelines for Best Available Retrofit Technology (BART) Determinations
 |date        = July 6, 2005
 |publisher   = United States Environmental Protection Agency
 |url         = http://www.gpo.gov/fdsys/pkg/FR-2005-07-06/pdf/05-12526.pdf
 |access-date  = July 26, 2012
 |url-status=live
 |archive-url  = https://web.archive.org/web/20140826202038/http://www.gpo.gov/fdsys/pkg/FR-2005-07-06/pdf/05-12526.pdf
 |archive-date = August 26, 2014
 |df          = mdy-all
}}</ref>
[[File:Grand Canyon in fog.jpg|thumb|left|350px|Natural fog sometimes fills the canyon, during temperature inversions]]
In the early 1990s, studies indicated that emissions of SO<sub>2</sub>, a sulfate precursor, from the Navajo Generating Station affected visibility in the canyon, mainly in the winter.<ref name="NGS SO2 visibility history">{{cite web
 |title       = RA BART (Reasonably Attributable Best Available Retrofit Technology) Case Study, Navajo Generating Station, Appendix C
 |author      = Mike Sundblom, Arizona Department of Environmental Quality
 |publisher   = Western Regional Air Partnership
 |url         = http://www.wrapair.org/forums/amc/projects/ra_bart_case/Navajo-C.doc
 |access-date  = August 22, 2011
 |url-status=live
 |archive-url  = https://web.archive.org/web/20120331095521/http://www.wrapair.org/forums/amc/projects/ra_bart_case/Navajo-C.doc
 |archive-date = March 31, 2012
 |df          = mdy-all
}}</ref>{{rp|p.C-2,C-6}}
As a result, scrubbers were added to the plant's three units in 1997 through 1999 to reduce SO2 emissions by 90% on an annual average.<ref name="Reitze">{{cite book |last1=Reitze |first1=Arnold W. Jr. |title=2019 Visibility Protection Under the Clean Air Act |date=2019 |publisher=SJ Quinney College of Law, University of Utah |url=https://dc.law.utah.edu/cgi/viewcontent.cgi?article=1177&context=scholarship |access-date=24 June 2022}}</ref> Before and after observations showed a wintertime decrease of 33% for particulate sulfur (Sp), improving visibility.<ref name="Green">{{cite journal |last1=Green |first1=Mark |last2=Farber |first2=Rob |last3=Lien |first3=Nghi |last4=Gebhart |first4=Kristi |last5=Molenar |first5=John |last6=Iyer |first6=Hari |last7=Eatough |first7=Delbert |title=The Effects of Scrubber Installation at the Navajo Generating Station on Particulate Sulfur and Visibility Levels in the Grand Canyon |journal=Journal of the Air & Waste Management Association |date=1 November 2005 |volume=55 |issue=11 |pages=1675–1682 |doi=10.1080/10473289.2005.10464759 |pmid=16350365 |bibcode=2005JAWMA..55.1675G |s2cid=31615461 |url=http://dx.doi.org/10.1080/10473289.2005.10464759 |access-date=24 June 2022 |issn=1096-2247}}</ref> The plant also installed low-NO<sub>x</sub> SOFA burners in 2009–2011, reducing emissions of NO<sub>x</sub>, a nitrate precursor, by 40%<ref name="Hurlbut">{{cite book |last1=Hurlbut |first1=David J. |last2=Haase |first2=Scott |last3=Brinkman |first3=Gregory |last4=Funk |first4=Kip |last5=Gelman |first5=Rachel |last6=Lantz |first6=Eric |last7=Larney |first7=Christina |last8=Peterson |first8=David |last9=Worley |first9=Christopher |last10=Liebsch |first10=Ed |title=Navajo Generating Station and Air Visibility Regulations: Alternatives and Impacts: Technical Report NREL/TP-6A20-53024 |date=2012 |publisher=U.S. Department of Energy |url=https://www.nrel.gov/docs/fy12osti/53024.pdf |archive-url=https://web.archive.org/web/20120925134528/http://www.nrel.gov/docs/fy12osti/53024.pdf |archive-date=2012-09-25 |url-status=live |access-date=24 June 2022}}</ref>
The plant shut down completely in 2019.<ref name="Nicla"/>
Emissions from the Mohave Generating Station to the west were similarly found to affect visibility in the canyon. The plant was required to have installed SO<sub>2</sub> scrubbers, but was instead shut down in 2005, completely eliminating its emissions.<ref>
{{cite web
 |title       = Revision of the Visibility FIP (Federal Implementation Plan) for Nevada (to include emissions reduction requirements for the Mohave Generating Station): Final Rule Fact Sheet
 |date        = June 6, 2001
 |publisher   = United States Environmental Protection Agency
 |url         = http://www.epa.gov/region9/air/mohave/pdf/nevadafipfact0202.pdf
 |access-date  = July 26, 2012
 |url-status=live
 |archive-url  = https://web.archive.org/web/20170118032153/https://www3.epa.gov/region9/air/mohave/pdf/nevadafipfact0202.pdf
 |archive-date = January 18, 2017
 |df          = mdy-all
}}</ref>

[[Biology:Controlled burn|Prescribed fires]] are typically conducted in the spring and fall in the forests adjacent to the canyon to reduce the potential for severe forest fires and resulting smoke conditions. Although prescribed fires also affect air quality, the controlled conditions allow the use of management techniques to minimize their impact.<ref>{{cite web
 |title       = Kaibab National Forest Fire Management Plan
 |date        = January 31, 2011
 |publisher   = U.S. Forest Service
 |url         = http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5298050.pdf
 |access-date  = July 30, 2012
 |url-status=live
 |archive-url  = https://web.archive.org/web/20140327212521/http://www.fs.usda.gov/Internet/FSE_DOCUMENTS/stelprdb5298050.pdf
 |archive-date = March 27, 2014
 |df          = mdy-all
}}</ref><ref>{{cite web
 |title       = Grand Canyon National Park Fire Management Plan
 |date        = March 2012
 |publisher   = U.S. National Park Service
 |url         = http://parkplanning.nps.gov/document.cfm?parkID=65&projectID=10959&documentID=46754
 |access-date  = July 30, 2012
 |url-status  = dead
 |archive-url  = https://web.archive.org/web/20130301120900/http://parkplanning.nps.gov/document.cfm?parkID=65&projectID=10959&documentID=46754
 |archive-date = March 1, 2013
 |df          = mdy-all
}}</ref>{{rp|p.86,93}}
{{clear}}

==Climate change==
[[File:Grand Canyon high climate.png|thumb|Grand Canyon Climate Summary Chart (NPS)]]

Due to the increase of greenhouse gases, temperatures have steadily risen making recent years the warmest in the century-long record.<ref name=":0">{{Cite web |title=Grand Canyon National Park Climate Action Plan |url=https://www.nps.gov/subjects/climatechange/upload/GRCA-CFP-Action-Plan-508compliant.pdf |archive-url=https://web.archive.org/web/20190611114928/https://www.nps.gov/subjects/climatechange/upload/GRCA-CFP-Action-Plan-508compliant.pdf |archive-date=2019-06-11 |url-status=live |website=National Park Service}}</ref> Temperatures have increased in Arizona by 2.1 degrees Fahrenheit since 1895.<ref>{{Cite web |title=State of the Earth in Numbers |url=https://usafacts.org/earth-day-facts/environment-climate/ |access-date=2022-03-06 |website=USAFacts |language=en}}</ref> From 1916 to 2014, naturalized streamflow in the Upper Colorado River Basin decreased by 16.5%, in spite of a slight increase of +1.4% in annual precipitation over the same period.<ref name="Xiao">{{cite journal |last1=Xiao |first1=Mu |last2=Udall |first2=Bradley |last3=Lettenmaier |first3=Dennis P. |title=On the Causes of Declining Colorado River Streamflows |journal=Water Resources Research |date=September 2018 |volume=54 |issue=9 |pages=6739–6756 |doi=10.1029/2018WR023153 |bibcode=2018WRR....54.6739X |s2cid=133694146 |language=en|doi-access=free }}</ref>
Increases in temperature correlate to increased evaporation, loss of reflective snow, and decreases in snowpack,  reducing available water in the Colorado River by an estimated 9.3% per degree Celsius of warming.<ref name="Childs">{{cite news |last1=Childs |first1=Jan Wesner |title=Climate Change Threatens Colorado River And the Water Supply for 40 Million People |url=https://weather.com/news/news/2020-02-21-colorado-river-drying-up-drought-climate-change |access-date=24 June 2022 |work=The Weather Channel |date=March 17, 2020}}</ref><ref name="Milly">{{cite journal |last1=Milly |first1=P. C. D. |last2=Dunne |first2=K. A. |title=Colorado River flow dwindles as warming-driven loss of reflective snow energizes evaporation |journal=Science |date=13 March 2020 |volume=367 |issue=6483 |pages=1252–1255 |doi=10.1126/science.aay9187 |pmid=32079679 |bibcode=2020Sci...367.1252M |s2cid=211233121 |language=en |issn=0036-8075|doi-access=free }}</ref>

Over the last 30 years, the South Rim of the Grand Canyon has averaged 13.4 inches of rainfall per year, while the North Rim has averaged 24 inches.<ref>{{Cite web |location=Grand Canyon National Park, AZ  |title=Park Statistics – Grand Canyon National Park (U.S. National Park Service) |url=https://www.nps.gov/grca/learn/management/statistics.htm |access-date=2022-03-06 |website=www.nps.gov |language=en}}</ref>  The first dual distribution water system in the United States was built on the South Rim, treating and reclaiming wastewater for nonpotable reuse as early as 1926.  Early on, water for human use was brought in by tankers, and pumped up from a spring deeper in the canyon.<ref name="Okun">{{cite journal |last1=Okun |first1=Daniel A. |title=Water Reclamation and Unrestricted Nonpotable Reuse: A New Tool in Urban Water Management |journal=Annual Review of Public Health |date=May 2000 |volume=21 |issue=1 |pages=223–245 |doi=10.1146/annurev.publhealth.21.1.223 |pmid=10884953 |language=en |issn=0163-7525|doi-access=free }}</ref> In the 1960s, the Transcanyon Pipeline was built to carry water from the North Rim down into the canyon and back up to the South Rim.<ref name="Repanshek">{{cite news |last1=Repanshek |first1=Kurt |title=Grand Canyon National Park Settles On Plan To Replace Transcanyon Water Pipeline |url=https://www.nationalparkstraveler.org/2019/05/grand-canyon-national-park-settles-plan-replace-transcanyon-water-pipeline |access-date=1 July 2022 |work=www.nationalparkstraveler.org |date=May 9, 2019 |language=en}}</ref>
Every day 500,000 gallons of water are pumped from underground springs on the North Rim through the pipeline to supply the more heavily developed South Rim with water.<ref name="Witze"/><ref name="O'Sullivan"/>

As water consumption continues to soar due to increasing visitation in the park, both the sustainability of the water supply and the condition of the pipeline are in question.<ref name="Witze"/><ref name="O'Sullivan">{{cite news |last1=O'Sullivan |first1=Serena |title=Grand Canyon restricts water use after water pipeline damaged again |url=https://www.azcentral.com/story/news/local/arizona/2019/05/23/grand-canyon-national-park-north-rim-water-pipeline-issues/1209384001/ |access-date=24 June 2022 |work=The Arizona Republic |date=May 23, 2019}}</ref> As of 2019, plans to replace the aging 16-mile aluminum pipeline were proposed.<ref name="Repanshek"/> Another proposal, from the Bureau of Reclamation, recommended that the park drill a well into the Redwall-Muav aquifer to meet the increasing water consumption. However, the aquifer's recharge rate stands to decline over time due to decreases in precipitation and snowpack.<ref>{{Cite web |last=Markovich |first=Katie |title=Climate Change, Development, and Groundwater-Surface Water Interactions in Grand Canyon National Park |date=2015 |url=https://watershed.ucdavis.edu/education/classes/files/content/page/markovich_report.pdf |archive-url=https://web.archive.org/web/20220227163705/https://watershed.ucdavis.edu/education/classes/files/content/page/markovich_report.pdf |archive-date=2022-02-27 |url-status=live |website=University of California, Davis}}</ref> Some effects of over pumping aquifers include land subsidence, reduction in rivers and lakes, disrupted riparian systems, and poor water quality.<ref>{{Cite web |title=Groundwater Decline and Depletion {{!}} U.S. Geological Survey |url=https://www.usgs.gov/special-topics/water-science-school/science/groundwater-decline-and-depletion |access-date=2022-03-25 |website=www.usgs.gov}}</ref>

In the National Park Service's "Climate Action Plan," goals were set to reduce greenhouse gases 30 percent below 2008 levels by 2020 and plan and implement measures that best allow the park to adapt to the impacts of climate change. Strategies to accomplish these goals included: "reduce [greenhouse gases] emissions resulting from activities within and by the park, developing and implementing a plan to adapt to current and future impacts of climate change, increase climate change education and outreach, and monitor progress and identify areas for improvement".<ref name=":0" />

==Biology and ecology==

===Plants===
There are approximately 1,737 known species of [[Biology:Vascular plant|vascular plant]]s, 167 species of [[Biology:Fungus|fungi]], 64 species of [[Biology:Moss|moss]], and 195 species of [[Biology:Lichen|lichen]] found in Grand Canyon National Park.<ref name=NPSplants>{{NPS|url=http://www.nps.gov/grca/naturescience/plants.htm|work=Grand Canyon National Park|title=Plants|accessdate=October 22, 2010}}</ref> This variety is largely due to the {{convert|8,000|foot}} elevation change from the Colorado River up to the highest point on the North Rim.<ref name=NPSplants/> Grand Canyon boasts a dozen endemic plants (known only within the Park's boundaries) while only ten percent of the Park's flora is exotic.<ref name=NPSplants/> Sixty-three plants found here have been given special status by the U.S. Fish and Wildlife Service.<ref name=NPSplants/>
[[File:Grand Canyon Clouds time lapse VP8.webm|thumb|left|Grand Canyon Clouds time lapse VP8]]
The Mojave Desert influences the western sections of the canyon, Sonoran Desert vegetation covers the eastern sections, and [[Biology:Pinus ponderosa|ponderosa]] and [[Biology:Pinyon pine|pinyon pine]] forests grow on both rims.<ref name=NPSanimals>{{NPS|url=http://www.nps.gov/grca/naturescience/animals.htm|work=Grand Canyon National Park|title=Animals|accessdate=October 22, 2010}}</ref>

Natural seeps and springs percolating out of the canyon walls are home to 11% of all the plant species found in the Grand Canyon.<ref name=NPSanimals/> The canyon itself can act as a connection between the east and the west by providing corridors of appropriate habitat along its length.<ref name=NPSanimals/> The canyon can also be a genetic barrier to some species, like the [[Biology:Abert's squirrel|tassel-eared squirrel]].<ref name=NPSanimals/>

The aspect, or direction a slope faces, also plays a major role in adding diversity to the Grand Canyon. North-facing slopes receive about one-third the normal amount of sunlight, so plants growing there are similar to plants found at higher elevations, or in more northern latitudes.<ref name=NPSanimals/> The south-facing slopes receive the full amount of sunlight and are covered in vegetation typical of the Sonoran Desert.<ref name=NPSanimals/>

===Animals===
[[File:Bighorn sheep grand canyon.jpg|thumb|A [[Biology:Bighorn sheep|bighorn ram]] perched on a cliff in the Grand Canyon]]
Of the 90 [[Biology:Mammal|mammal]] species found along the Colorado River corridor, 18 are [[Biology:Rodent|rodent]]s and 22 are [[Biology:Bat|bat]]s.<ref name=NPSmammals>{{NPS|url=http://www.nps.gov/grca/naturescience/mammals.htm|work=Grand Canyon National Park|title=Mammals|accessdate=October 22, 2010}}</ref>

===Life zones and communities===
The Park contains several major ecosystems.<ref name=NPSnatsci>{{NPS|url=http://www.nps.gov/grca/naturescience/index.htm|work=Grand Canyon National Park|title=Nature and Science}}</ref> Its great biological diversity can be attributed to the presence of five of the seven [[Biology:Life zone|life zone]]s and three of the four desert types in North America.<ref name=NPSnatsci/> The five life zones represented are the Lower Sonoran, Upper Sonoran, Transition, Canadian, and Hudsonian.<ref name=NPSnatsci/> This is equivalent to traveling from Mexico to Canada. Differences in elevation and the resulting variations in climate are the major factors that form the various life zones and communities in and around the canyon. Grand Canyon National Park contains 129 vegetation communities, and the composition and distribution of plant species are influenced by climate, geomorphology and geology.<ref name=NPSplants/>

====Lower Sonoran====
The Lower Sonoran life zone spans from the Colorado River up to {{convert|3500|ft}}. Along the Colorado River and its perennial tributaries, a riparian community exists.<ref name=NPSplants/> [[Biology:Salix exigua|Coyote willow]], [[Biology:Pluchea sericea|arrowweed]], [[Biology:Baccharis salicifolia|seep-willow]], [[Biology:Prosopis glandulosa|western honey mesquite]], [[Biology:Senegalia greggii|catclaw acacia]], and exotic [[Biology:Tamarix|tamarisk]] (saltcedar) are the predominant species.<ref name=NPSplants/> Hanging gardens, seeps and springs often contain rare plants such as the white-flowering western [[Biology:Cercis occidentalis|redbud]], [[Biology:Epipactis gigantea|stream orchid]], and ''Flaveria mcdougallii''.<ref name=NPSplants/> Endangered fish in the river include the [[Biology:Humpback chub|humpback chub]] and the [[Biology:Razorback sucker|razorback sucker]].<ref name=NPSfish>{{NPS|url=https://web.archive.org/web/20101022/http://www.nps.gov/grca/naturescience/endangeredfish.htm|work=Grand Canyon National Park|title=Endangered Fish|accessdate=October 22, 2010}}</ref>
[[File:Bighorn, Grand Canyon.jpg|thumb|left|upright|A [[Biology:Bighorn sheep|bighorn ewe]] at the Grand Canyon, 2008]]
The three most common amphibians in these riparian communities are the [[Biology:Canyon tree frog|canyon tree frog]], [[Biology:Red-spotted toad|red-spotted toad]], and Woodhouse's Rocky Mountain toad.<ref name=NPSamphib>{{NPS|url=http://www.nps.gov/grca/naturescience/amphibians.htm|work=Grand Canyon National Park|title= Amphibians|accessdate=October 22, 2010}}</ref> [[Biology:Leopard frog|Leopard frog]]s are very rare in the Colorado River corridor; they have undergone major declines and have not been seen in the Canyon in several years.<ref name=NPSamphib/> There are 33 crustacean species found in the Colorado River and its tributaries within Grand Canyon National Park. Of these 33, 16 are considered true zooplankton organisms.<ref name=NPScrustaceans>{{NPS|url=https://web.archive.org/web/20101022/http://www.nps.gov/grca/naturescience/crustaceans.htm|work=Grand Canyon National Park|title=Crustaceans|accessdate=October 22, 2010}}</ref>

Only 48 bird species regularly nest along the river, while others use the river as a migration corridor or as an overwintering habitat. The [[Biology:Bald eagle|bald eagle]] is one species that uses the river corridor as a winter habitat.<ref name=NPSbirds>{{NPS|url=http://www.nps.gov/grca/naturescience/birds.htm|work=Grand Canyon National Park|title=Birds|accessdate=October 22, 2010}}</ref>

[[Biology:North American river otter|River otters]] may have disappeared from the park in the late 20th century, and [[Biology:Muskrat|muskrat]]s are extremely rare.<ref name=NPSmammals/> [[Biology:Beaver|Beaver]]s cut willows, cottonwoods, and shrubs for food, and can significantly affect the riparian vegetation.<ref name=NPSmammals/> Other rodents, such as [[Biology:Antelope squirrel|antelope squirrel]]s and [[Biology:Perognathinae|pocket mice]], are mostly omnivorous, using many different vegetation types.<ref name=NPSmammals/> Grand Canyon bats typically roost in desert uplands but forage on the abundance of insects along the river and its tributaries.<ref name=NPSmammals/> In addition to bats, [[Biology:Coyote|coyote]]s, [[Biology:Ringtail|ringtail]]s, and [[Biology:Spotted skunk|spotted skunk]]s are the most numerous riparian predators and prey on invertebrates, rodents, and reptiles.<ref name=NPSmammals/>

[[Biology:Raccoon|Raccoon]]s, weasels, [[Biology:Bobcat|bobcat]]s, [[Biology:Gray fox|gray fox]]es, and [[Biology:Cougar|mountain lions]] are also present but are much rarer.<ref name=NPSmammals/> Ungulate species such as mule deer and [[Biology:Desert bighorn sheep|desert bighorn sheep]] frequent the river corridor. Since the removal of 500 [[Biology:Donkey|feral burros]] in the early 1980s, bighorn sheep numbers have rebounded.<ref name=NPSmammals/> Mule deer are generally not permanent residents along the river but travel down from the rim when food and water resources there become scarce.<ref name=NPSmammals/>

The insect species commonly found in the river corridor and tributaries are [[Biology:Midge|midge]]s, [[Biology:Caddisfly|caddisflies]], [[Biology:Mayfly|mayflies]], [[Biology:Plecoptera|stoneflies]], [[Biology:Black fly|black flies]], [[Biology:Mite|mite]]s, [[Biology:Beetle|beetle]]s, [[Biology:Butterfly|butterflies]], [[Biology:Moth|moth]]s, and [[Biology:Fire ant|fire ant]]s.<ref name=NPSbugs>{{NPS|url=https://web.archive.org/web/20101022/http://www.nps.gov/grca/naturescience/insects.htm|work=Grand Canyon National Park|title=Insects, Spiders, Centipedes, Millipedes|accessdate=October 22, 2010}}</ref> Numerous species of [[Biology:Spider|spider]]s and several species of scorpions, including the [[Biology:Arizona bark scorpion|bark scorpion]] and the giant desert hairy scorpion, inhabit the riparian zone.<ref name=NPSbugs/>

Eleven aquatic and 26 terrestrial species of [[Biology:Mollusca|mollusks]] have been identified in and around Grand Canyon National Park.<ref name=NPSmollusks>{{NPS|url=https://web.archive.org/web/20101022/http://www.nps.gov/grca/naturescience/mollusks.htm|work=Grand Canyon National Park|title=Mollusks|accessdate=October 22, 2010}}</ref> Of the aquatic species, two are [[Biology:Bivalvia|bivalves]] (clams) and nine are [[Biology:Gastropoda|gastropods]] (snails).<ref name=NPSmollusks/> Twenty-six species of terrestrial gastropods have been identified, primarily [[Biology:Land snail|land snail]]s and [[Biology:Slug|slug]]s.<ref name=NPSmollusks/>

There are approximately 41 [[Biology:Reptile|reptile]] species in Grand Canyon National Park. Ten are considered common along the river corridor and include lizards and snakes.<ref name=NPSreptiles>{{NPS|url=http://www.nps.gov/grca/naturescience/reptiles.htm|work=Grand Canyon National Park|title=Reptiles}}</ref> [[Biology:Lizard|Lizard]] density tends to be highest along the stretch of land between the water's edge and the beginning of the upland desert community.<ref name=NPSreptiles/> The two largest lizards in the canyon are [[Biology:Gila monster|gila monster]]s and [[Biology:Chuckwalla|chuckwalla]]s.<ref name=NPSreptiles/> Many [[Biology:Snake|snake]] species, which are not directly dependent on surface water, may be found both within the inner gorge and the Colorado River corridor. Six rattlesnake species have been recorded in the park.<ref name=NPSreptiles/>

Above the river corridor a desert scrub community, composed of North American desert flora, thrives. Typical warm desert species such as [[Biology:Larrea tridentata|creosote bush]], white bursage, brittlebush, catclaw acacia, [[Biology:Fouquieria splendens|ocotillo]], mariola, western honey mesquite, [[Biology:Atriplex canescens|four-winged saltbush]], [[Biology:Artemisia tridentata|big sagebrush]], [[Biology:Coleogyne|blackbrush]], and [[Biology:Ericameria nauseosa|rubber rabbitbrush]] grow in this community.<ref name=NPSplants/> The mammalian fauna in the woodland scrub community consists of 50 species, mostly rodents and bats.<ref name=NPSmammals/> Three of the five Park [[Biology:Pack rat|woodrat]] species live in the desert scrub community.<ref name=NPSmammals/>

Except for the [[Biology:Western banded gecko|western banded gecko]], which seems to be distributed only near water along the Colorado River, all of the reptiles found near the river also appear in the uplands, but in lower densities.<ref name=NPSreptiles/> The [[Biology:Gopherus|desert gopher tortoise]], a threatened species, inhabits the desert scrublands in the western end of the park.<ref name=NPSreptiles/>

Some of the common insects and animals found at elevations above {{convert|2,000|ft}} are [[Biology:Vespidae|orange paper wasps]], [[Biology:Honey bee|honey bee]]s, black flies, [[Biology:Tarantula hawk|tarantula hawk]]s, [[Biology:Pentatomidae|stink bugs]], beetles, [[Biology:Black garden ant|black ants]], and [[Biology:Monarch butterfly|monarch]] and [[Biology:Swallowtail butterfly|swallowtail butterflies]].<ref name=NPSbugs/> [[Biology:Solifugae|Solifugids]], [[Biology:Huntsman spider|wood spiders]], garden spiders, [[Biology:Latrodectus|black widow spiders]], and [[Biology:Tarantula|tarantula]]s can be found in the desert scrub and higher elevations.<ref name=NPSbugs/>

====Upper Sonoran and Transition====
[[File:Californian Condor 50 MC.jpg|thumb|A California condor in flight, photographed from Navajo Bridge at Marble Canyon, 2008. Wild condors are numbered to aid wildlife researchers. As of April 2009, there were 172 wild California condors known.]]
The Upper Sonoran Life Zone includes most of the inner canyon and South Rim at elevations from {{convert|3500|to|7000|ft}}.<ref name=NPSanimals/> This zone is generally dominated by blackbrush, [[Biology:Sagebrush|sagebrush]], and pinyon-juniper woodlands. Elevations of {{convert|3500|to|4000|ft}} are in the Mojave Desert Scrub community of the Upper Sonoran. This community is dominated by the four-winged saltbush and creosote bush; other important plants include [[Biology:Agave utahensis|Utah agave]], [[Biology:Salix exigua|narrowleaf mesquite]], [[Biology:Krameria|ratany]], catclaw acacia, and various [[Biology:Cactus|cacti]] species.<ref name=NPSanimals/>

Approximately 30 bird species breed primarily in the desert uplands and cliffs of the inner canyon.<ref name=NPSbirds/> Virtually all bird species present breed in other suitable habitats throughout the Sonoran and Mohave deserts.<ref name=NPSbirds/> The abundance of bats, swifts, and riparian birds provides ample food for peregrines, and suitable eyrie sites are plentiful along the steep canyon walls. Also, several critically endangered [[Biology:California condor|California condor]]s have made the eastern part of the Park their home, having been re-introduced to the Colorado Plateau on the Arizona Strip earlier.<ref name=NPSbirds/>
[[File:Buteo jamaicensis in flight, Grand Canyon NP, Arizona, USA.png|thumb|Red-tailed Hawk flying at the south rim of Grand Canyon]]
[[File:Elk at Grand Canyon.png|thumb|An elk searching for water at Grand Canyon National Park in 2018.]]
The conifer forests provide habitat for 52 animal species.<ref name=NPSanimals/> [[Biology:Porcupine|Porcupine]]s, shrews, [[Biology:Red squirrel|red squirrel]]s, [[Biology:Kaibab squirrel|tassel-eared Kaibab]] and [[Biology:Abert's squirrel|Abert's squirrel]]s, Indian peacocks, [[Biology:American black bear|black bear]], mule deer, and [[Biology:Elk|elk]] are found at the park's higher elevations on the Kaibab Plateau.<ref name=NPSmammals/>

Above the desert scrub and up to {{convert|6200|ft}} is a pinyon pine forest and one seed juniper woodland.<ref name=NPSplants/> Within this woodland one can find big sagebrush, [[Biology:Gutierrezia|snakeweed]], [[Biology:Ephedra (plant)|Mormon tea]], Utah agave, banana and narrowleaf [[Biology:Yucca|Yucca]], winterfat, Indian ricegrass, dropseed, and needlegrass.<ref name=NPSplants/> There are a variety of snakes and lizards here, but one species of reptile, the [[Biology:Greater short-horned lizard|mountain short-horned lizard]], is a particularly abundant inhabitant of the piñon-juniper and ponderosa pine forests.<ref name=NPSreptiles/>

Ponderosa pine forests grow at elevations between {{convert|6500|and|8200|ft}}, on both North and South rims in the Transition life zone.<ref name=NPSplants/> The South Rim includes species such as gray fox, mule deer, bighorn sheep, [[Biology:Rock squirrel|rock squirrel]]s, pinyon pine, and Utah juniper.<ref name=NPSanimals/> Additional species such as [[Biology:Gambel oak|Gambel oak]], New Mexico locust, mountain mahogany, elderberry, creeping mahonia, and fescue have been identified in these forests.<ref name=NPSplants/> The [[Biology:Tiger salamander|Utah tiger salamander]] and the [[Biology:Great Basin spadefoot|Great Basin spadefoot toad]] are two amphibians that are common in the rim forests.<ref name=NPSamphib/> Of the approximately 90 bird species that breed in the coniferous forests, 51 are summer residents and at least 15 of these are known to be neotropical migrants.<ref name=NPSbirds/>

====Canadian and Hudsonian====
Elevations of {{convert|8,200|to|9,000|ft}} are in the Canadian Life Zone, which includes the North Rim and the [[Earth:Kaibab Plateau|Kaibab Plateau]].<ref name=NPSanimals/> Spruce-fir forests characterized by [[Biology:Picea engelmannii|Engelmann spruce]], [[Biology:Blue spruce|blue spruce]], [[Biology:Douglas fir|Douglas fir]], [[Biology:Abies concolor|white fir]], [[Biology:Aspen|aspen]], and [[Biology:Rowan|mountain ash]], along with several species of perennial grasses, groundsels, [[Biology:Achillea millefolium|yarrow]], [[Biology:Potentilla|cinquefoil]], [[Biology:Lupinus|lupines]], [[Biology:Cyperaceae|sedges]], and [[Biology:Aster (genus)|asters]], grow in this sub-alpine climate.<ref name=NPSplants/> Mountain lions, Kaibab squirrels, and [[Biology:American goshawk|American goshawk]]s are found here.<ref name=NPSanimals/>

Montane meadows and subalpine grassland communities of the Hudsonian life zone are rare and located only on the North Rim.<ref name=NPSplants/> Both are typified by many grass species. Some of these grasses include [[Biology:Bouteloua gracilis|blue]] and [[Biology:Bouteloua eriopoda|black grama]], [[Biology:Hilaria rigida|big galleta]], [[Biology:Oryzopsis hymenoides|Indian ricegrass]], and [[Biology:Aristida|three-awns]].<ref name=NPSplants/> The wettest areas support sedges and [[Earth:Forb|forb]]s.<ref name=NPSplants/>
{{wide image|Grand Canyon Panorama 2013.jpg|800px|View from the South Rim|center}}

==Grand Canyon tourism==
Grand Canyon National Park is one of the world's premier natural attractions, attracting about five million visitors per year. Overall, 83% were from the United States: California (12%), Arizona (9%), Texas (5%), Florida (3%) and New York (4%) represented the top domestic visitors. Seventeen percent of visitors were from outside the United States; the most prominently represented nations were the United Kingdom (3%), Canada (4%), Japan (2%), Germany (2%) and the Netherlands (1%).<ref>
{{cite web | title = Executive Summary of Grand Canyon Tourism | publisher = Northern Arizona University | url = http://www.nau.edu/hrm/ahrrc/reports/G_C_EXEC_SUMMARY.pdf#search=grandcanyon | archive-url = https://web.archive.org/web/20100928184338/http://www.nau.edu/hrm/ahrrc/reports/G_C_EXEC_SUMMARY.pdf#search=grandcanyon | archive-date = September 28, 2010 | format = PDF | access-date = January 4, 2007}}</ref>
The South Rim is open all year, weather permitting.  The North Rim is generally open mid-May to mid-October.<ref>
{{cite web|url=http://www.nps.gov/grca/planyourvisit/hours.htm|title=Operating Hours & Seasons – Grand Canyon National Park|url-status=live|archive-url=https://web.archive.org/web/20110303012942/http://www.nps.gov/grca/planyourvisit/hours.htm|archive-date=March 3, 2011|df=mdy-all}}</ref>

===Activities===
[[File:NPS grand-canyon-regional-map.jpg|thumb|upright=1.75|Grand Canyon regional map]]
[[Image:Grand Canyon rafting 2006.jpg|thumb|Rafters in the Grand Canyon pass one of the rapids of the (mud-)"colored" Colorado River]]

There are many viewing points on all sides of the canyon, with the most accessible locations inside Grand Canyon National Park and the Hualapai Indian Reservation. About 90% of tourists visit the South Rim from Arizona State Route 64, which averages {{Convert|7,000|feet|m}} above sea level. The South Rim houses two visitor centers, a geological museum, art gallery/bookstore, and other attractions near Grand Canyon Village. Further east along the South Rim is the Desert View Watchtower. Grand Canyon National Park also has a visitor center in an easterly area known as the North Rim, via Arizona State Route 67; the center and the road are closed in winter months.<ref>[https://www.nps.gov/grca/planyourvisit/upload/GRCAmap2.pdf Grand Canyon Area Map]</ref> On the Hualapai reservation, Grand Canyon West is the third major area with tourist services, about {{cvt|125|mi}} driving from Las Vegas and about {{convert|250|mi|km}} by road from Grand Canyon Village at the South Rim.<ref name=Skywalk>{{cite web|url=http://www.nps.gov/grca/planyourvisit/skywalk.htm|title=Skywalk|work=Grand Canyon National Park|access-date=March 19, 2013|url-status=live|archive-url=https://web.archive.org/web/20130308141115/http://www.nps.gov/grca/planyourvisit/skywalk.htm|archive-date=March 8, 2013|df=mdy-all}}</ref> The tribe opened the glass-bottomed Grand Canyon Skywalk in 2007, which has since attracted "thousands of visitors a year, most from Las Vegas".<ref name=nyt14>{{cite news|author1=Adam Nagourney|title=Where 2 Rivers Meet, Visions for Grand Canyon Clash|url=https://www.nytimes.com/2014/12/04/us/where-2-rivers-meet-visions-for-grand-canyon-clash.html?_r=1|access-date=March 5, 2015|work={{wipe|The New York Times}}|date=December 3, 2014|url-status=live|archive-url=https://web.archive.org/web/20150403071156/http://www.nytimes.com/2014/12/04/us/where-2-rivers-meet-visions-for-grand-canyon-clash.html?_r=1|archive-date=April 3, 2015|df=mdy-all}}</ref> Also at Grand Canyon West is Guano Point, which features a narrow peninsula surrounded on all sides by steep dropoffs. On the north side of the canyon to the west, the Grand Canyon–Parashant National Monument has no paved roads and no visitor services.

Rafting, hiking, running, and helicopter tours are also popular in the canyon area. The Grand Canyon Ultra Marathon is a {{convert|78|mi|km|adj=on}} race over 24 hours. The floor of the valley is accessible by foot, muleback, or by boat or raft from upriver. Hiking down to the river and back up to the rim in one day is discouraged by park officials because of the distance, steep and rocky trails, change in elevation, and danger of [[Medicine:Heat exhaustion|heat exhaustion]] from the much higher temperatures at the bottom. Rescues are required annually of unsuccessful rim-to-river-to-rim travelers. Nevertheless, hundreds of fit and experienced hikers complete the trip every year.{{Citation needed|date=November 2018}}

Camping on the North and South rims is generally restricted to established campgrounds and reservations are highly recommended, especially at the busier South Rim. There is at large camping available along many parts of the North Rim managed by Kaibab National Forest. North Rim campsites are only open seasonally due to road closures from weather and winter snowpack. All overnight camping below the rim requires a backcountry permit from the Backcountry Office (BCO).<ref name=backcountry>{{cite web|url=http://www.nps.gov/grca/planyourvisit/backcountry-permit.htm|title=Backcountry Permit|work=Grand Canyon National Park|access-date=October 22, 2010|url-status=live|archive-url=https://web.archive.org/web/20101218060402/http://www.nps.gov/grca/planyourvisit/backcountry-permit.htm|archive-date=December 18, 2010|df=mdy-all}}</ref> Each year Grand Canyon National Park receives approximately 30,000 requests for backcountry permits. The park issues 13,000 permits, and close to 40,000 people camp overnight.<ref name=backcountry/> The earliest a permit application is accepted is the first of the month, four months before the proposed start month.
[[File:Grand canyon.ogg|thumb|left|A 6-minute video of a flight over the Grand Canyon (view in high quality)]]
Tourists wishing for a more vertical perspective can go skydiving, board helicopters and small airplanes in Boulder, Las Vegas, Phoenix and Grand Canyon National Park Airport (seven miles from the South Rim) for canyon flyovers. Scenic flights are no longer allowed to fly within {{convert|1500|feet}} of the rim within the national park because of a late 1990s crash.<ref>Moorman, Robert W. "[http://vtol.org/E3EF4A00-B7F8-11E4-A5170050568D0042 Noise in the Parks]" ''AHS International'', 2015. [http://vtol.org/news/ahs-updates-helicopter-noise-library Source] {{webarchive|url=https://web.archive.org/web/20150220023533/http://vtol.org/news/ahs-updates-helicopter-noise-library |date=February 20, 2015 }}</ref> The last aerial video footage from below the rim was filmed in 1984. However, some helicopter flights land on the Havasupai and Hualapai Indian Reservations within Grand Canyon (outside of the park boundaries).

In 2016, skydiving at the Grand Canyon become possible with the first Grand Canyon Skydiving operation opening up at the Grand Canyon National Park Airport, on the South Rim.

In 2014, a developer announced plans to build a multimedia complex on the canyon's rim called the Grand Canyon Escalade. On {{convert|420|acre}} there would be shops, an IMAX theater, hotels and an RV park. A gondola would enable easy visits to the canyon floor where a "riverwalk" of "connected walkways, an eatery, a tramway station, a seating area and a wastewater package plant" would be situated. On October 31, 2017, the Navajo Nation Council voted against the project.<ref name="escaladecancelled">{{Cite web |date=2017-11-01 |title=Navajo Nation Votes Down Controversial Hotel and Tram Project at Grand Canyon |url=https://www.nbcnews.com/news/us-news/navajo-nation-votes-down-controversial-hotel-tram-project-grand-canyon-n816666 |access-date=2021-04-24 |website=NBC News}}</ref>

==Grand Canyon fatalities==
=== Mid-1800s to 2015 ===
[[Image:GrandCanyonRescueHelicopter1978.jpg|thumb|Grand Canyon rescue helicopter, 1978]]

About 770 deaths have occurred between the mid-1800s and 2015.<ref name="Deathsactivetimes">{{Cite web |url=https://www.theactivetimes.com/travel/national-parks/how-many-people-die-grand-canyon-and-it-becoming-too-dangerous |title=How Many People Die in the Grand Canyon and is it Becoming Too Dangerous? |last=The Active Times |date=August 9, 2016 |url-status=live |archive-url=https://web.archive.org/web/20170219044507/http://www.theactivetimes.com/travel/national-parks/how-many-people-die-grand-canyon-and-it-becoming-too-dangerous |archive-date=February 19, 2017 |df=mdy-all }}</ref><ref name="Deathscitylab">{{Cite news |url=https://www.citylab.com/environment/2015/05/mapping-the-grand-canyons-gruesome-legacy-of-death/394040/ |title=This Grim Map Shows How People Have Died at the Grand Canyon |last=Citylab |newspaper=Bloomberg.com |date=May 26, 2015 |url-status=live |archive-url=https://web.archive.org/web/20170820010819/https://www.citylab.com/environment/2015/05/mapping-the-grand-canyons-gruesome-legacy-of-death/394040/ |archive-date=August 20, 2017 |df=mdy-all }}</ref> Of the fatalities that occurred from 1869 to 2001, some were as follows: 53 resulted from falls; 65 were attributable to environmental causes, including heat stroke, cardiac arrest, dehydration, and hypothermia; 7 were caught in flash floods; 79 were drowned in the Colorado River; 242 perished in airplane and helicopter crashes (128 of them in the 1956 disaster mentioned below); 25 died in freak errors and accidents, including lightning strikes and rock falls; and 23 were the victims of homicides.<ref>{{Cite book | first1 = Michael P. | last1 = Ghiglieri | first2 = Thomas M. | last2 = Myers | title = Over the Edge: Death in Grand Canyon | publisher = Puma Press | year = 2001 | isbn = 978-0970097316}}</ref>

====1956 air disaster====

In 1956, the Grand Canyon was the site of the deadliest commercial aviation disaster in history at the time.

On the morning of June 30, 1956, a TWA Lockheed Super Constellation and a United Airlines [[Engineering:Douglas DC-7|Douglas DC-7]] departed Los Angeles International Airport within three minutes of one another on eastbound transcontinental flights. Approximately 90 minutes later, the two propeller-driven airliners collided above the canyon while both were flying in unmonitored airspace.

The wreckage of both planes fell into the eastern portion of the canyon, on Temple and [[Earth:Chuar Butte|Chuar Butte]]s, near the confluence of the Colorado and Little Colorado rivers. The disaster killed all 128 passengers and crew members aboard both planes.

This accident led to the institution of high-altitude airways and direct radar observation of aircraft (known as [[Engineering:Air traffic control|positive control]]) by en route ground controllers.

{{wide image|Cedar Ridge, Grand Canyon.jpg|1000px|South Kaibab Trail at Cedar Ridge. [[Earth:O'Neill Butte|O'Neill Butte]] on the left.}}

=== ''Over the Edge'' ===
In ''Over the Edge: Death in Grand Canyon'', Thomas M. Myers, a journalist and author, documents every death in the Grand Canyon.<ref>{{cite book |last1=Ghiglieri |first1=Michael Patrick |title=Over the edge : death in Grand Canyon : gripping accounts of all known fatal mishaps in the most famous of the world's seven natural wonders |date=2001 |publisher=Puma Press |location=Flagstaff, AZ |isbn=978-0970097316 |edition=}}</ref>

===Charlie Haeger===
On October 3, 2020, former Major League Baseball player Charlie Haeger was found dead from a self-inflicted gunshot wound on a canyon trail. He was under investigation for the murder of his ex-girlfriend which had taken place the day before in Scottsdale.<ref>{{cite web |url=https://www.azcentral.com/story/news/local/scottsdale/2020/10/03/scottsdale-man-suspected-killing-ex-girlfriends-escaped-police/3608639001/ |title=Former MLB player suspected of killing ex-girlfriend found dead of self-inflicted gunshot wound |last=Ackley |first=Madeline |work=Arizona Republic |date=October 3, 2020 |access-date=July 7, 2021 |via=azcentral.com }}</ref>

==See also==
{{div col|colwidth=30em}}
* Copper Canyon, Mexico
* Verdon Gorge, {{wipe|France}}
* Grand Canyon National Park
* ''Grand Canyon Suite''
* Grand Canyon Ultra Marathon
* Jacob Lake, Arizona
* List of Colorado River rapids and features
* List of trails in Grand Canyon National Park
* ''Making North America'' (2015 PBS film)
* ''A Bigger Grand Canyon'', 1998 painting
* Pine Creek Gorge – gorge in northeastern Pennsylvania also known as the "Pennsylvania Grand Canyon"
* [[Astronomy:Valles Marineris|Valles Marineris]] – A gigantic canyon on [[Astronomy:Mars|Mars]], one of the largest in the Solar System
{{div col end}}
{{clear}}

==References==
{{reflist}}

==External links==
{{external media
| image1 = [[Social:Public domain|Public domain]] {{webarchive |url=https://web.archive.org/web/20100830173528/http://www.nps.gov/grca/learn/photosmultimedia/photogallery.htm |date=August 30, 2010 |title=images }} from the National Park Service.
}}
* [http://www.nps.gov/grca/ Grand Canyon National Park Service]
* [http://hikearizona.com/map.php?QX=4101 Grand Canyon Backcountry Use Areas – Map]
* {{osmrelation|183377}}

'''History'''
* [http://www.grandcanyonbiblio.org/ Grand Canyon Bibliography] {{Webarchive|url=https://web.archive.org/web/20160117082424/http://www.grandcanyonbiblio.org/ |date=January 17, 2016 }}&nbsp;– bibliography of the Grand Canyon. 37,462 items produced between 1540 and the present.
* [http://www.bobspixels.com/kaibab.org/misc/gc_hist.htm Grand Canyon Explorer: History timeline] from 10,000 years ago to 1994.

'''Travel and sites'''
* [http://grandcanyoncvb.org/ Grand Canyon Chamber & Visitor's Bureau]
* [http://travel.nytimes.com/2009/05/31/travel/31hours.html?em 36 Hours at the Grand Canyon] by ''The New York Times'', May 31, 2009

'''Multimedia'''
* [http://www.nps.gov/grca/learn/photosmultimedia/photogallery.htm NPS Photographs]
* [https://web.archive.org/web/20090825014319/http://landsat.usgs.gov/images/gallery/56_M.jpg Grand Canyon 3-D perspective] &nbsp;– view looking southwesterly, showing North Rim and Canyon.
* [https://www.google.com/intl/sg/maps/streetview/#grand-canyon Grand Canyon – Street View – Google Maps]


[[Category:Colorado Plateau]]

{{Sourceattribution|Grand Canyon}}