Earth:Eltanin Fault System

Short description: Series of faults that offset the Pacific-Antarctic Ridge

<mapframe zoom="2" text="Approximate surface projection on Southern Ocean of Eltanin Fault System components (violet). Other nearby fracture zones (orange) and associated features such as probable extension of fracture zones are also shown (lighter orange). Click to expand map to obtain interactive fracture zone details." align="right" height="240" latitude="-66" longitude="-105" width="275">{{Wikipedia:Map data/Fracture zone}}</mapframe>

Pacific Ocean depth map showing the Heezen Fault and the Tharp Fault as #17.

The Eltanin Fault System (Eltanin Fracture Zone) is a series of six or seven dextral transform faults that offset the Pacific-Antarctic Ridge, a spreading zone between the Pacific Plate and the Antarctic Plate. This is extending by up to 7.93 cm/year (3.12 in/year). It was named after USNS Eltanin. The affected zone of the Pacific-Antarctic Ridge is about 800 km (500 mi) long, between 56° S, 145° W and 54.5° S, 118.5° W, southwest of Easter Island, and about as far as one can get from land on planet Earth (48°52.6′S 123°23.6′W). However, the total offset is about 1600 km. The two major faults in the Eltanin Fracture Zone are the Heezen transform fault and the Tharp transform fault, usually known as fracture zones as they extend inactively from the Pacific-Antarctic Ridge. A third named after Hollister, which is the shortest to the south, also exists and its active transform region has been linked to the other transform regions of the Eltanin Fault System. They are about 1,000 km (620 mi) long and have been in the last 50 years the location of many earthquakes of up to title|Moment mag. scale|M_w|dotted=no}}  6.4. One segment of the Heezen transform has ruptured with an average repeat interval of 4 years. Others related faults include the Vacquier Transform Fault, the Menard Transform Fault, and the Udintsev Fault.

To the northwest, in an almost linear fashion as seafloor features, are the Hollister Ridge and the Louisville Seamount Chain.

See also

• Hollister Ridge

Sources

• Sykes, Lynn R.; Ekstörm, Göran (2011). "Earthquakes along Eltanin transform system, SE Pacific Ocean: fault segments characterized by strong and poor seismic coupling and implications for long-term earthquake prediction". Geophysical Journal International 188 (2): 421–434. doi:10.1111/j.1365-246X.2011.05284.x. Bibcode: 2012GeoJI.188..421S. 

Further reading

• Beutel, Erin K.; Okal, Emile A. (2003). "Strength asperities along oceanic transform faults: a model for the origin of extensional earthquakes on the Eltanin transform system". Earth and Planetary Science Letters 216 (1/2): 27–41. doi:10.1016/S0012-821X(03)00484-9. Bibcode: 2003E&PSL.216...27B. 
• Kashintsev, G.L.; Frikh-khar, D. (1978). "Structure of the oceanic crust in the Eltanin Fault Zone (Pacific Ocean) based on petrographic data". Oceanology 18: 39–42. 
• Lonsdale, Peter (1986). "Tectonic and magmatic ridges in the eltanin fault system, South Pacific". Marine Geophysical Researches 8 (3): 203–242. doi:10.1007/BF00305484. Bibcode: 1986MarGR...8..203L. 
• Lonsdale, Peter (1994). "Structural geomorphology of the Eltanin fault system and adjacent transform faults of the Pacific-Antarctic plate boundary". Marine Geophysical Researches 16 (2): 105–143. doi:10.1007/BF01224756. Bibcode: 1994MarGR..16..105L. 
• Okal, Emile A.; Langenhorst, Amy R. (2000). "Seismic properties of the Eltanin Transform System, South Pacific". Physics of the Earth and Planetary Interiors 119 ((3/4): 185–208. doi:10.1016/S0031-9201(99)00169-7. Bibcode: 2000PEPI..119..185O. 
• Stewart, Lisa M.; Okal, Emile A. (1983). "Seismicity and Aseismic Slip Along the Eltanin Fracture Zone". Journal of Geophysical Research 88 (B12): 10,495–10,507. doi:10.1029/jb088ib12p10495. Bibcode: 1983JGR....8810495S. http://www.earth.northwestern.edu/people/emile/PDF/EAO040.pdf.