Weches Formation Explained

Weches Formation
Type:Formation
Age:Paleogene
Period:Paleogene
Prilithology:sandstone, shale, clay
Otherlithology:marl, limestone
Region:,

The Weches Formation is a greensand, slay, and shale geologic formation in Louisiana and Eastern Texas.[1] [2] It preserves fossils dating back to the Paleogene period, specifically the Eocene.

Description

The Weches Formation is a fossiliferous glauconite rich sand that graduates into a clay. It is considered one of the principal iron bearing beds in Eastern Texas, and is mined for sand in gravel in parts of Texas where exposed.[3] The Weches Formation was originally called the Weches Greensand, and was considered a member of the Mount Selman Formation before being raised to formation status.[4]

See also

References

Notes and References

  1. Web site: Weches Formation . Mineral Resources Online Spatial Data Geology by state Texas . USGS . 30 June 2018.
  2. Eargle . D. Hoye . Nomenclature of formations of Claiborne Group, middle Eocene, Coastal Plain of Texas . United States Geological Survey Bulletin . 1968 . 1251-D . 10–11 . 30 June 2018.
  3. United States Department of Agriculture . Soil Survey of Marion and Cass Counties, Texas . USDA Soil Survey . 2009 . 2 . 30 June 2018.
  4. White . Walter A. . Sayre . A. N. . Heuser . J. F. . Geology and ground-water resources of the Lufkin area, Texas . United States Geological Survey Water Supply Paper . 1941 . 849-A . 26–27 . 30 June 2018 .