Ash, cinder and bombs erupt explosively to form a cone shaped hill
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Cinder cone volcanoes can be found in a number of areas with different climates. Climate does not affect the formation of volcanoes.
Parasitic cone volcanos and cinder cone volcanos are not the same when classifying. Cinder cone volcanos are the most popular type of volcano, named for its cone shaped formation. Cinder cone volcano are also considered the smallest type of volcanos and can stand alone or grow on the flanks of other volcanos. The parasitic cone volcanos are similar to the cinder cones, however, the volcano is found on the flanks of other volcanos, hence, the name. It is created by flank eruptions of larger volcanos.
A cinder cone volcano typically has basaltic lava, which is low in silica content and flows easily. This results in the formation of steep-sided cones made of mostly cinders and volcanic ash.
Cinder Cone
it is a volcano in hawwaii that is a cinder cone
Paricutin is a cinder cone volcano.
i believe one cinder cone volcano is in Hawaii
The magma in a cinder cone is typically thick, meaning it has high viscosity. This is because cinder cone volcanoes are formed from highly viscous and gas-rich magma which tends to solidify quickly, leading to the formation of cinders and ash during eruptions.
Mount Paricutin in Mexico is a cinder cone volcano. It erupted in 1943 and is known for its relatively steep slopes and cone-shaped profile, characteristics typical of cinder cone volcanoes. Unlike composite volcanoes, which are built up by multiple layers of lava flows, ash, and other volcanic debris, cinder cones primarily consist of small fragments of volcanic rock called cinders. Paricutin's formation and eruption provide a classic example of cinder cone volcanism.
A cinder cone has basaltic lava, which has a fairly low viscosity.
yes cinder cone volcano are made from magma