The Flaxville gravel and its relation to other terrace gravels of the northern Great Plains
Links
- Document: Report (pdf)
- Larger Work: This publication is Chapter J of Shorter contributions to general geology, 1917
- NGMDB Index Page: National Geologic Map Database Index Page (html)
- Download citation as: RIS | Dublin Core
Abstract
In Nebraska and South Dakota there are widespread deposits of gravel and other material, largely superficial and generally uninitiated, known as the White River, Arikaree, Ogalalla, and other formations, which range in age from Oligocene to Pleistocene. West of these deposits, on the flanks of the Rocky Mountains, are several high plateaus covered with gravel, whose age, though not know, is generally regarded as Pleistocene.
Study Area
Publication type | Report |
---|---|
Publication Subtype | USGS Numbered Series |
Title | The Flaxville gravel and its relation to other terrace gravels of the northern Great Plains |
Series title | Professional Paper |
Series number | 108 |
Chapter | J |
DOI | 10.3133/pp108J |
Year Published | 1918 |
Language | English |
Publisher | U.S. Geological Survey |
Description | ii, 10 p. |
Larger Work Type | Report |
Larger Work Subtype | USGS Numbered Series |
Larger Work Title | Shorter contributions to general geology, 1917 (Professional Paper 108) |
First page | 179 |
Last page | 184 |
Country | Canada, United States |
State | Alberta, Montana, Saskatchewan |
Online Only (Y/N) | N |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |