Emigrant Springs Formation
Geology
The Emigrant Springs Formation is predominately composed of various carbonate rocks, and is overlain by the Dunderberg Formation, whilst it is underlain by the Patterson Pass Shale. It also contains three members, which are as follows, in ascending stratigraphic order (lowest to highest):
Members
- Member A: This member is the thinnest, only getting up to 256 ft (78 m) thick, and is composed of medium-gray, thin to medium-bedded calcisiltite and calcilutite, with breccia's in the upper beds of the member.
- Member B: This member is the thickest, getting up to 1,509 ft (460 m) thick, and is dominated by light-olive-gray, yellowish or pink calcisiltite, which contains silt-sized quartz grains. At the base of this member, there are also mudstones present, transitioning to medium-light-gray, thin to thick-bedded calcisiltite and calcilutite above.
- Member C: This member can get up to 495 ft (151 m) thick, and is primarily composed of medium-gray oolitic calcarenite, calcilutite and calcisiltite.
Paleobiota
The Emigrant Springs Formation contains a small number of trilobites, and a collection of conodonts, and various molluscs.
Notes
Uncertain or tentative taxa are in small text
crossed out taxa are discredited.