Search results
Results from the WOW.Com Content Network
The climate of Western Alaska is determined largely by the Bering Sea and the Gulf of Alaska. It is a subarctic oceanic climate in the southwest and a continental subarctic climate farther north. The temperature is somewhat moderate considering how far north the area is.
The climate of western Alaska is determined in large part by the Bering Sea and the Gulf of Alaska. It is a subarctic oceanic climate in the southwest and a continental subarctic climate farther north. The temperature is somewhat moderate considering how far north the area is. This region has a tremendous amount of variety in precipitation.
The topographic elevation of a summit measures the height of the summit above a geodetic sea level. [b] The first table below ranks the 100 highest major summits of Alaska by elevation. The topographic prominence of a summit is a measure of how high the summit rises above its surroundings.
The climate of western Alaska is determined in large part by the Bering Sea and the Gulf of Alaska. It is a subarctic oceanic climate in the southwest and a continental subarctic climate farther north. The temperature is somewhat moderate considering how far north the area is. This region has a tremendous amount of variety in precipitation.
Malibu Canyon, Santa Monica Mountains. The Pacific Coast Ranges (officially gazetted as the Pacific Mountain System [1] in the United States; French: chaînes côtières du Pacifique; Spanish: cadena costera del Pacífico) [2] are the series of mountain ranges that stretch along the West Coast of North America from Alaska south to Northern and Central Mexico.
The Seward Peninsula is a large peninsula on the western coast of the U.S. state of Alaska whose westernmost point is Cape Prince of Wales. The peninsula projects about 200 mi (320 km) into the Bering Sea between Norton Sound, the Bering Strait, the Chukchi Sea, and Kotzebue Sound, just below the Arctic Circle. The entire peninsula is about 210 ...
Southwest Alaska includes a huge swath of terrain 500 miles (800 km) from the western Bering Sea coast to Cook Inlet.Although much of the region is coastal, it also includes tens of thousands of square miles of interior boreal forests, swamps, and highlands, and the immense mountain barrier of the southern Alaska/Aleutian Range.
The Brooks Range (Gwich'in: Gwazhał [1]) is a mountain range in far northern North America stretching some 700 miles (1,100 km) from west to east across northern Alaska into Canada's Yukon Territory. Reaching a peak elevation of 8,976 feet (2,736 m) on Mount Isto, the range is believed to be approximately 126 million years old.