Abstract
The Channeled Scabland of east-central Washington in the USA is a complex of anastomosing, rock-cut fluvial channels, rock basins, cataracts, streamlined loess hills, and immense gravel bars. It was all produced by cataclysmic erosion and deposition from Pleistocene megaflooding derived from the margins of the Cordilleran Ice Sheet that covered much of the mountainous northwestern part of North America.
Original language | English (US) |
---|---|
Title of host publication | Geomorphological Landscapes of the World |
Publisher | Springer Netherlands |
Pages | 21-28 |
Number of pages | 8 |
ISBN (Print) | 9789048130542 |
DOIs | |
State | Published - 2010 |
Keywords
- coulees
- fluvial erosion
- megaflooding
- scabland
ASJC Scopus subject areas
- Environmental Science(all)
- Earth and Planetary Sciences(all)