Deformation of the Sea Floor off the North-west Coast of the United States

1971 ◽  
Vol 232 (31) ◽  
pp. 97-98 ◽  
Author(s):  
GEORGE PETER ◽  
OMAR E. DeWALD
Keyword(s):  
United States ◽  
West Coast ◽  
The United States ◽  
Sea Floor ◽  
North West ◽  
The North

Blood and Bones

2021 ◽  
pp. 142-165
Author(s):  
Benjamin Hoy
Keyword(s):  
United States ◽  
Great Lakes ◽  
West Coast ◽  
The United States ◽  
Annual Reports ◽  
The Arctic ◽  
North West ◽  
The North ◽  
The Us ◽  
Major Region

By 1874, Canada and the United States had surveyed land and placed boundary stones over 6,000 kilometers of territory. They had established a cohesive skeleton for the border in every major region except the Arctic. Drawing on government correspondence, annual reports, and paylists, chapter 7 rebuilds the bureaucratic footprint of the Canada–US border at the end of the nineteenth century. It maps the positions and operations of the North-West Mounted Police and American soldiers as well as customs, immigration, and Indian Affairs personnel. In doing so, it shows how the border diverged across the East Coast, Great Lakes, Prairies, West Coast, and Artic, as well as differentiating the US approach to its border with Canada and Mexico.

Entanglements of marine mammals and seabirds in central California and the north-west coast of the United States 2001–2005

2009 ◽  
Vol 58 (7) ◽  
pp. 1045-1051 ◽  
Author(s):  
Emma Moore ◽  
Shannon Lyday ◽  
Jan Roletto ◽  
Kate Litle ◽  
Julia K. Parrish ◽  
...  
Keyword(s):  
United States ◽  
West Coast ◽  
Marine Mammals ◽  
The United States ◽  
Central California ◽  
North West ◽  
The North

scholarly journals Activity of the Coleman Glacier, Mt. Baker, Washington, U.S.A., 1949–1955

1956 ◽  
Vol 2 (20) ◽  
pp. 708-713
Author(s):  
Kermit B. Bengtson
Keyword(s):  
United States ◽  
The United States ◽  
The State ◽  
North West ◽  
Long Period ◽  
The North

AbstractThe Coleman Glacier on Mt. Baker in the State of Washington began to advance about 1949 after a long period of rapid retreat. Since that year the terminus has advanced continuously a total of about 300 m. and considerable thickening of the entire glacier has occurred. The continued advance of the Coleman Glacier and other evidence are interpreted as manifestations of a trend during the last decade towards a slightly cooler and moist climate in the north-west of the United States.

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