Topografische kaart Kenai Fjords National Park
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Naam: Topografische kaart Kenai Fjords National Park, hoogte, reliëf.
Gemiddelde hoogte: 518 m
Minimale hoogte: -2 m
Maximale hoogte: 1.972 m
The park's landscape has been shaped by plate tectonics, with the Pacific Plate subducting beneath the North American Plate. The process has lowered the elevation of the Kenai Mountains, gradually pulling glacial features down into the sea, which is at the same time rising. The floors of the fjords can be from 600 to 1,000 feet (180 to 300 m) below the present sea level. The motion of the North Pacific Plate has accreted a variety of terranes against the shoreline, so that the coastal region is a mixture of rocks that originated elsewhere, together with local igneous rock. Predominant rock types include shale and graywacke, with greenstone, tuff and chert.
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