TITLE:
Food Security: Impact of European Settlement and Infrastructure on Columbia River Salmon Migration
AUTHORS:
Kenneth R. Olson, Cory D. Suski
KEYWORDS:
Bonneville Slide, Land of Flowing Milk and Honey, Lewis and Clark Expedition, Missoula Flood, Mount St. Helens, Oregon Trail, Willamette Valley
JOURNAL NAME:
Open Journal of Soil Science,
Vol.11 No.7,
July
1,
2021
ABSTRACT: The 2000 km Columbia River is the longest river in the Pacific Northwest region of North America. It starts in British Columbia, Canada and flows through the states of Oregon and Washington before discharging into Pacific Ocean near Cape Disappointment. The mouth of the Columbia River is a deep water harbor and 180 km of the river can be accessed by navigation. Based on flow volume, the river is the 4th largest river in the United States. The headwaters and approximately 800 km of the Columbia River lie in Canada. Columbia Lake and the Columbia Wetlands are located in British Columbia and are the headwaters of the Columbia River. The lake has an elevation of 820 m above sea level and drains to the Pacific Ocean near Astoria, Oregon. The Ocean tides flow up river to Portland, Oregon. This paper highlights how the geological and landscape resources of the Columbia River and tributaries watershed contributed to the economic development of this historically rich region of North America. The Columbia River is one of the most biologically diverse freshwater systems in the United States. The Columbia River system with trails and cruise ships was designed to increase use of the Columbia River, to promote recreational tourism, and to create a generation of people who are willing to protect and provide environmental stewardship of the river basin resources.