Virgin Formation
Geologic formation in Utah, United States
From Wikipedia, the free encyclopedia
The Virgin Formation is a geologic formation in Utah. It preserves fossils dating back to the Triassic period (Spathian substage).[1]
| Virgin Formation | |
|---|---|
| Stratigraphic range: Spathian | |
| Type | Formation |
| Unit of | Thaynes Group |
| Thickness | 150 m (490 ft) |
| Lithology | |
| Primary | Limestone |
| Other | Siltstone, shale |
| Location | |
| Coordinates | 37°12′6″N 113°11′23″W |
| Region | Utah |
| Country |  United States |
| Type section | |
| Named for | Virgin, Utah |
| Named by | Bassler and Reeside |
| Year defined | 1921 |
  Virgin Formation (the United States)  Virgin Formation (Utah) | |
Description
The Virgin Formation consists of gray to yellowish gray to greenish gray limestone, occasionally fossiliferous, alternating with greenish yellow to reddish brown to gray shale or siltstone. The limestone beds are up to 20 feet (6.1 m) thick.[2][3] Total thickness of the formation is up to 150 meters (490 ft).[4] About 30% of the total section of the formation is limestone.[5]
The formation rests on the "lower red member" of the Moenkopi Group and underlies the Shnabkaib Member of the Moenkopi Group.[4] More recently, the Virgin Formation is interpreted as a formation of the Thaynes Group.[6]
The formation is interpreted as having been deposited in a near-shore shallow marine environment. The lower part shows cyclic sedimentation, while the upper part of the formation to the southeast was deposited in lagoons in an arid climate while marine deposition continued to the north.[5]
Fossils
The formation contains marine fossils, including crinoids, pelecypods, gastropods, worms, crustaceans, and the ammonoid Tirolites. The latter is characteristic of the early Spathian stage of the Early Triassic.[3][1]
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