Chagres Formation
The Chagres Formation is a geologic formation in the Colón Province of central Panama. The sandstones and siltstones were deposited in a shallow marine environment and preserve fossils dating back to the Middle to Late Miocene period.
Description
The Chagres Formation is exposed in the northern part of the Panama Canal Zone. The formation overlies and partly overlaps the Gatún Formation. The outcrop area lies entirely west of the Panama Canal, extending from the Canal Zone southwestward along the Caribbean coast, about southwest of Colón. Calcareous strata at the base of the formation throughout most of the outcrop area in the Canal Zone constitute the Toro limestone member.The name Chagres Sandstone was proposed by MacDonald in 1919 for the sandstone forming the hills that overlook the coast from Toro Point to the mouth of the Chagres River. The sandstone is so massive that estimates of thickness are uncertain.
Fossil content
Various fossils have been found in the Chagres Formation:Fish
Alopias superciliosusBenthosema pluridensCarcharhinus brachyurusCarcharhinus cioneiCarcharhinus obscurusCarcharhinus plumbeusCarcharhinus signatusCarcharodon plicatilisCentrophorus granulosusCynoscion prolixusDalatias lichaDiaphus barrigonensis, D. rodrigueziGaleocerdo cuvierGaleorhinus galeusHemipristis serraHeptranchias perloHeterodontus sp.Isistius sp.Lampadena scaphaLepidophanes inflectus- MegalodonMustelus sp.Myctophum arcanum, M. degraciaiMyliobatis sp.Premontreia sp.Pristiophorus sp.Pseudocarcharias kamoharaiRhizoprionodon sp.Sphyrna lewiniSqualus sp.Squatina sp.
- ''Trigonognathus sp.''