Cinder cones are the mountainous structure built up by some volcanoes. Most of the material that makes up the cone is ash and cinders expelled from the top of the cone.
There are three kinds of cone volcanoes shield cones, composite cones, and cinder cones. Shield cones have very fluid lava. They erupt with a quiet lava flow. An example of a shield cone volcano is Mauna Loa. A shield cone is pretty much a little dome that has been flattened. Composite cones have sticky lava and rock bits. They have the most explosive eruptions An example of a composite cone volcano is Vesuvius. Composite cones are steep at the top but gentle at the bottom. Cinder cones have cinders. They have explosive eruptions An example is Paricutin. A cinder cone is very steep.
No. The most explosive variety of volcanic activity would be the caldera-forming eruptions of stratovolcanoes. Cinder cone eruptions are only mildly explosive.
Cinder cones are usually found on the sides of shield volcanoes, calderas, and stratovolcanoes. Many cinder cones can be found in Hawaii on the volcano of Mauna Kea. The most active cinder cone is found in Nicaragua. It is named Cerro Negro, and according to geologists and scientist has erupted around 20 times since 1850.
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
Cinder cones are the mountainous structure built up by some volcanoes. Most of the material that makes up the cone is ash and cinders expelled from the top of the cone.
No. Cinder cones are the most common variety.
There are three kinds of cone volcanoes shield cones, composite cones, and cinder cones. Shield cones have very fluid lava. They erupt with a quiet lava flow. An example of a shield cone volcano is Mauna Loa. A shield cone is pretty much a little dome that has been flattened. Composite cones have sticky lava and rock bits. They have the most explosive eruptions An example of a composite cone volcano is Vesuvius. Composite cones are steep at the top but gentle at the bottom. Cinder cones have cinders. They have explosive eruptions An example is Paricutin. A cinder cone is very steep.
No. The most explosive variety of volcanic activity would be the caldera-forming eruptions of stratovolcanoes. Cinder cone eruptions are only mildly explosive.
Cinder cones are usually found on the sides of shield volcanoes, calderas, and stratovolcanoes. Many cinder cones can be found in Hawaii on the volcano of Mauna Kea. The most active cinder cone is found in Nicaragua. It is named Cerro Negro, and according to geologists and scientist has erupted around 20 times since 1850.
Most volcanoes of any type, including cinder cones, are found at plate boundaries, but some are associated with hot spots.
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
Like most cinder cones Paricutin was fed by mafic magma.
The most common volcano is the cinder cone volcano. Unlike shield volcanoes and stratovolcanoes, many cinder cones are monogenetic, meaning they form from a single, relatively short period of activity and then never erupt again.
Most Cinder Volacnoes are found in North America.
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In general, composite volcanoes are the most dangerous volcanoes because they are more explosive than the other types.