Grand Coulee
The Grand Coulee used to be a river in the U.S. state of Washington. This dry river stretches for sixty miles from the Grand Coulee Dam to Soap Lake. A feature known as Dry Falls divides the Coulee into two parts. Dry Falls is thought to be the remains of the largest waterfall ever, two or three times higher than Niagara Falls.[1]
Geological history
The Grand Coulee is granite bedrock which is 40 to 60 million years old. The volcanic basalt is 2,000 metres (6,600 ft) thick. The coulee is said to have been made when the Columbia River was blocked by a large glacier. At the end of the last ice age the Columbia River went back to its old route and left the coulee. The coulee is a mile wide and was formed by a river that now flows a different way.[2]
Modern Uses
The area surrounding the Grand Coulee is shrub land. It has a rainfall of twelve inches per year. The Lower Grand Coulee contains the Park, Blue, Alkali, Lenore, and Soap lakes. Until recently, the Upper Coulee was dry.
The Columbia Basin Project dammed the river in 1952. It used the Grand Coulee as an irrigation network. The Upper Grand Coulee was dammed and made Banks Lake. The lake is filled by pumps from the Grand Coulee Dam. Banks Lake feeds a hundred-mile (160 km) irrigation system.
Grand Coulee Media
Looking northward in Grand Coulee.
Part of the Grand Coulee has been dammed and filled with water as part of the Columbia Basin Project.
Formation of Grand Coulee
References
- ↑ Dry Falls, GoNorthWest.com, accessed November 2009
- ↑ The Geologic Story of the Columbia Basin Archived 2009-11-05 at the Wayback Machine, bpa.gov, November 2009