BETA TEST - Fossil data and pages are very much experimental and under development. Please report any problems
T-1: T, Salt Lake County, Utah, USA
| Lat/Long (Decimal) | 40.77,-111.825 |
|---|---|
| Co-ordinates Derivation | based on nearby landmark |
| Given Location | Utah, United States |
| Mindat.org Region (for given coordinates) | Salt Lake County, Utah, USA |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| T-1: T(B) Ft. Douglas | Schubert J K, Bottjer D J (1995) | Thaynes | Most recently, the Thaynes formation has been separated into four facies belts, which include a basinal facies, an outer shelf facies, an inner shelf facies, and a red bed facies. the basinal facies consists of dark grey to black very siltly lime mudstones and gray to loive drab siltstones and shales. The outer shelf facies belt is characterized by dark grayish brown whole fossil wackestone, ranging to light gray bioclastic grainstone, with minor interbedded sanstone, siltstone, and mudstone. Th | packstone | 251.3 - 247.2 Ma Early/Lower Triassic |
| T-3: T(B) Ft. Douglas | Schubert J K, Bottjer D J (1995) | Thaynes | Most recently, the Thaynes formation has been separated into four facies belts, which include a basinal facies, an outer shelf facies, an inner shelf facies, and a red bed facies. the basinal facies consists of dark grey to black very siltly lime mudstones and gray to loive drab siltstones and shales. The outer shelf facies belt is characterized by dark grayish brown whole fossil wackestone, ranging to light gray bioclastic grainstone, with minor interbedded sanstone, siltstone, and mudstone. Th | packstone | 251.3 - 247.2 Ma Early/Lower Triassic |
Recorded Fossils
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
