Taxus Baccata

by | Mar 15, 2018 | Taxus Baccata

How Can We Help?
You are here:
< Back

The Big Snowy Group is a stratigraphical unit of Chesterian age in the Williston Basin.

It takes the name from Big Snowy Mountains in Montana, and was first described on the north slopes of the mountain by H.W. Smith in 1935.

Lithology

Subdivisions

The Big Snowy Group is composed of three subdivisions, from top to base: [1]

  • Heath Formation: black shale with sandstone lenses.
  • Otter Formation: limestone and grey to green shale
  • Kibbey Formation: shaly sandstone

Distribution

The Big Snowy Group reaches a maximum thickness of 135 metres (440 ft) in the Williston Basin.[1] It is exposed in outcrop in the Big Snowy Mountains, Little Belt Mountains, Castle Mountains and Lombard Hills of central Montana. It occurs in the sub-surface throughout the central part of the Williston Basin and into a limited area of south-central Saskatchewan.

Relationship to other units

The Big Snowy Group is unconformably overlain by the Tyler Formation in Montana, and by the Watrous Formation in Saskatchewan; It disconformably overlays the Madison Group.[1]

References

  1. ^ a b c d Lexicon of Canadian Geologic Units. "Big Snowy Group". Archived from the original on 2013-02-21. Retrieved 2010-02-03.
Categories
Table of Contents