Bering Glacier is a glacier in the U.S. state of Alaska. It currently terminates in Vitus Lake south of Alaska's Wrangell-St. Elias National Park, about from the Gulf of Alaska. Combined with the Bagley Icefield, where the snow that feeds the glacier accumulates, the Bering is the largest glacier in North America. The glacier is named after Vitus Bering.
The glacial retreat has an interesting side effect, an increase in the frequency of earthquakes in the region. The Wrangell and Saint Elias mountain ranges that spawn the Bering Glacier were created by the collision of the Pacific Plate and North American tectonic plates (the Pacific Plate is being subducted underneath the North American Plate). The weight of the vast amount of ice in the Bering Glacier is enough to depress the Earth's crust, stabilizing the boundary between the two plates. As the glaciers lose mass, the pressure of the ice is diminished. This reduced compression allows the rocks along faults to move more freely, resulting in more earthquakes.
Scientists from the Michigan Tech Research Institute, working with U.S. Geological Survey and U.S. Bureau of Land Management, have recently discovered that the glacier is releasing approximately of water a year, more than twice the amount of water in the entire Colorado River. Bering Glacier Melting Faster Than Scientists Thought Newswise, Retrieved on August 24, 2008.
Meltwater at the terminus collects in Vitus Lake, which flows via the Seal River to the Gulf of Alaska.
target="_blank" rel="nofollow"> Bering Glacier National Forest Service, USDA
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