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Can active volcanoes become in active?

Updated: 8/20/2019
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11y ago

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Some types of volcanoes are known as "monogenetic" meaning they are formed in and limited to, one single eruption, commonly forming cinder cones. One example is Paricutin in the Trans-Mexican Volcanic Belt.

Some volcanoes become dormant, meaning they haven't erupted in several hundred thousand years, but are thought to still contain eruptible magma somewhere beneath them. An example would be Mt Ranier in the Cascades Arc.

Some volcanoes become inactive or "extinct" because the magmatic system feeding them becomes shut off, migrates to another volcano, or simply stops supplying them (this is poorly understood as the timescales over which this occurs are so huge). An example of this would be the Hawaii-Emperor Seamount Chain - the islands are all volcanoes that become progressively older the further North you go. This is because the magma source feeding the volcanoes came from a "hot-spot" or "mantle-plume" located in a fixed position underneath the Pacific tectonic plate. As the plate moved over the top, the magma source become cut off, rendering one volcano extinct, while building another one slightly further South.

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