Kachemak Bay, Alaska: An Exploration of People and Place

Where are We?
Who are We?
What are the Dynamic Forces that Shape Our Place?
Volcanoes
Tides, Winds, Weather
Earthquakes
Geology
Glaciers
How Have We Survived?
What are the Challenges of Living Here?
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Volcanic Viewpoints Photo Gallery

Cutaway of earth's crust, showing overlapping tectonic plates and Cook Inlet volcanoes
Geologic Cutaway
U.S. Geological Survey

Geologic Cutaway of Tectonic Plates

The earth's surface is a network of large interlocking plates, like the pieces of a puzzle. The plates move in relationship to one another. We live at the edge, where the Pacific Plate slides under the North American Plate, about 2½ to 3 inches a year. As it curves beneath the Kenai Peninsula, the Pacific Plate descends to a depth of 30 miles. When it reaches the west side of Cook Inlet, it is 60 miles below the surface. Subduction, the process whereby one plate dives under another, produces the volcanoes west of Kachemak Bay. Eight percent of all active volcanoes on earth are found in Alaska.

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