Earth:Caimito Formation
From HandWiki
Revision as of 13:56, 29 August 2022 by imported>Nautica (simplify)
Caimito Formation Stratigraphic range: Late Oligocene-Early Miocene | |
---|---|
Type | Formation |
Underlies | Alajuela & Gatún Formations |
Overlies | Bohío, Caraba & Gatuncillo Formations, Cretaceous basement |
Lithology | |
Primary | Marl |
Other | Siltstone, sandstone, conglomerate |
Location | |
Coordinates | [ ⚑ ] : 9°12′N 79°48′W / 9.2°N 79.8°W |
Paleocoordinates | [ ⚑ ] 7°42′N 77°30′W / 7.7°N 77.5°W |
Region | Panamá Province |
Country | ![]() |
Extent | Panama Basin |
Type section | |
Named for | Caimito Junction of Panama Railroad |
Named by | MacDonald |
Year defined | 1913 |
The Caimito Formation (Tcm)[1] is a geologic formation in Panama. The marls, sandstones and conglomerates preserve bivalve and gastropod fossils dating back to the Late Oligocene to Early Miocene period.[2] The name Caimito was proposed by MacDonald in 1913, named after the Caimito junction in the Panama Railroad during the construction of the Panama Canal.[3]
See also
- List of fossiliferous stratigraphic units in Panama
References
- ↑ Geologic Map, 1980
- ↑ Caimito Formation at Fossilworks.org
- ↑ Woodring, 1957, p.28
Bibliography
- Stewart, R.H.; J.L. Stewart, and W.P. Woodring. 1980. Geologic Map of the Panama Canal and Vicinity, 1. USGS. Accessed 2019-02-09.
- Woodring, W.P. 1957. Geology and Paleontology of Canal Zone and Adjoining Parts of Panama - 306A Geology and description of Tertiary mollusks (Gastropods: Trochidae to Turritellidae), 1–186. USGS. Accessed 2019-02-09.
![]() | Original source: https://en.wikipedia.org/wiki/Caimito Formation.
Read more |