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Geology of Mount Shasta - Google 検索
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Mount Shasta was primarily constructed during four major cone-building episodes that were centered on separate vents. Each of the cone-building periods produced andesite lava flows, block-and-ash flows, and mudflows originating mainly at the central vents.
2023ねん11月6にち
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Shasta and several lesser peaks of the Cascade range that have been built by flows of lava and ash. As different as these two ranges are, both are the results ...
2023/11/06 · Mount Shasta is located in the Cascade Range in northern California about 65 km (40 mi) south of the Oregon-California border.
The origin of the name "Shasta · The mountain consists of four overlapping dormant volcanic cones that have built a complex shape, including the main summit and ...
ERUPTIONS When Did Mt. Shasta Last Erupt? A U.S. Geological Survey report in 1980 states that a pyroclastic flow and hot mudflow traveled down Ash Creek and ...
2020/08/10 · Mount Shasta, a 400 km3 volcano in northern California (United States), is the most voluminous stratocone of the Cascade arc.
Mount Shasta is a typical strato-volcano, principally composed of andesitic and basaltic lavas with only minor flows of dacite. It had almost attained its ...
Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sergeants Ridge runs parallel to the U-shaped ...
Mount Shasta dominates the landscape almost everywhere in the Shasta River watershed. At 14,162 feet high, the mountain looms far above everything else.