In the United States, where do volcanoes like the one shown in diagram C occur?
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The answer is the fissure vent of Hawaii.
A crevice vent, otherwise called a volcanic gap or emission gap, is a straight volcanic vent through which magma emits, more often than not with no hazardous movement. The vent is regularly a couple meters wide and might be numerous kilometers long. Crevice vents can bring about substantial surge basalts which run first in magma directs and later in magma tubes. After some time the ejection develops splash resp. fiery debris cones and may focus on one or some of them. Little crevice vents may not be effectively detectable from the air, but rather the pit columns or the ravines developed by some of them are.
The barriers that nourish gaps achieve the surface from profundities of a couple of kilometers and associate them to further magma supplies, regularly under volcanic focuses. Crevices are generally found in or along breaks and crack zones, for example, Iceland and the East African Rift. Crevice vents are regularly some portion of the structure of shield volcanoes.
A crevice vent, otherwise called a volcanic gap or emission gap, is a straight volcanic vent through which magma emits, more often than not with no hazardous movement. The vent is regularly a couple meters wide and might be numerous kilometers long. Crevice vents can bring about substantial surge basalts which run first in magma directs and later in magma tubes. After some time the ejection develops splash resp. fiery debris cones and may focus on one or some of them. Little crevice vents may not be effectively detectable from the air, but rather the pit columns or the ravines developed by some of them are.
The barriers that nourish gaps achieve the surface from profundities of a couple of kilometers and associate them to further magma supplies, regularly under volcanic focuses. Crevices are generally found in or along breaks and crack zones, for example, Iceland and the East African Rift. Crevice vents are regularly some portion of the structure of shield volcanoes.
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The answer is the fissure vent of Hawaii.
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