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Fifes Peaks are located east of the Cascade crest. Most weather fronts originating in the Pacific Ocean travel northeast toward the Cascade Mountains.As fronts approach, they are forced upward by the peaks of the Cascade Range (orographic lift), causing them to drop their moisture in the form of rain or snow onto the Cascades.
Cascade Volcanic Arc Pemberton Volcanic Belt Mount Overill is a volcanic peak in southwestern British Columbia , Canada , located 81 km (50 mi) east of Rivers Inlet and 2 km (1 mi) northwest of Mount Somolenko .
The active stratovolcano of Mount St. Helens is located only 19 miles (31 km) to the north-northeast, easily visible from the summit of Tumtum Mountain on clear days. The historic Yale Bridge , a one-lane metal suspension bridge built in 1932 over the steep canyon of the Lewis River at the eastern end of Lake Merwin , is located about 2.5 miles ...
It is the second youngest of four overlapping volcanic cones which together form the most voluminous stratovolcano in the Cascade Range. At 12,335 feet (3,760 m), Shastina is taller than Mount Adams and would rank as the third highest volcano in the Cascades behind Mount Rainier and Shasta were it not nestled on the western flank of its higher ...
Cinnamon Butte; Highest point; Elevation: 6,427 ft (1,959 m) NAVD 88 [1] Coordinates: 1]: Geography; Location: Douglas County, Oregon, U.S.: Parent range: Cascades: Topo map: USGS Mount Thielsen: Geology; Rock age: Holocene? [2]: Mountain type(s): Cinder cone, lava dome, volcanic field: Volcanic arc: Cascade Volcanic Arc: Last eruption: More than 6845 years ago [2]: Cinnamon Butte is a group ...
The Juan de Fuca tectonic plate is being subducted under the North American Plate, leading to volcanic activity in the Cascades like at West Crater. In southern Washington state, the Cascade Range, which sits south of the dacitic Garibaldi Volcanic Belt, spans 600 miles (970 km) from British Columbia in Canada to Lassen Peak in northern California in the United States.
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The Cascade volcanoes have had more than 100 eruptions over the past few thousand years, many of them explosive eruptions. [21] However, certain Cascade volcanoes can be dormant for hundreds or thousands of years between eruptions, and therefore the great risk caused by volcanic activity in the regions is not always readily apparent.