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Plates are sliding past each other
Plates are sliding past each other
Plates are sliding past each other
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Mount St. Helens is a result of subduction as the Juan de Fuca Plate is pushed under the North American Plate.
Mount St. Helens was formed along a subduction zone, where the Juan de Fuca Plate plate dives under (subducts) the North American plate.
two examples are the Juan de fuca and the north American plate.
Juan de fuca plate are being pushed under the north american plate
two examples are the Juan de fuca and the north American plate.
Mount St. Helens was formed as a result of the Juan de Fuca plate's subduction under the North American plate.
In subduction, one tectonic plate moves under another. The most explosive volcanoes erupt in the subduction zone. This type of tectonic is happening in several places around the world, such as Chile; the Nazca plate is slipping under the South American plate. This is also happening in Washington, the Juan de Fuca plate is slipping under the Morth American plate, which is why Mount Saint Helens was formed. Subduction has also occured in Alaska, Mt. Fugi Japan, Krakatua Indonesia, and Mt. Etna Italy.
The Cascade mountains were formed by a subduction zone with the Juan De Fuca plate went under the North American plate why the Juan De Fuca went under was because its more dense than the North American plate.