Cinder cones form around a volcanic vent. Lava explodes into the air and cools very quickly forming accumulating a ring of volcanic fragments (like scoria or tuff) around the vent. They are not very tall or strong because there is nothing cementing the fragments together. Their slope never exceeds the angle of repose (approximately 45 degrees). They are not associated with any specific type of lava. Any flavour is possible.
Both shield volcanoes and cinder cones erupt low-viscosity basaltic lava and have eruptions that are only mildly explosive if at all.Cinder cones are small, steep-sloped volcanoes composed primarily of a chunky variety of basalt called scoria.Shield volcanoes are large, gently sloping volcanoes composed primarily of layers of lava flows.
No one know if there are active volcanoes on Venus. There are old ones. There is no evidence of plate motion on Venus.
mostly earthquakes or plate tectonic movement.
Strato and Cinder-cone volcanos but cinder cones can have non explosive too but not strato
Earthquakes can cause a volcano to erupt.
Cinder cone volcanoes erupt explosively, but not as violently as composite volcanoes.
Cinder cone volcanoes erupt explosivly.
Shield volcanoes erupt least violently cinder cone most violently and compost can erupt either way.
they are made out of rock
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Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
I don't know I'm asking you
Both erupt basaltic lava, which has a low silica content and a high temperature.
Ash, cinder and bombs erupt explosively to form a cone shaped hill
When a Cinder Cone volcano erupts it shoots out ash, and that's how they form also, ash builds up on there sides and grow taller and taller every time a cinder cone erupts. Hope this helps!
No. Cinder cone volcanoes erupt fountains of lava, which is how the cinder cone is built up. Cinder cones that are nearing the end of activity may also produce lava flows.
The three major types of volcanoes are shield volcanoes, cinder cone volcanoes, and stratovolcanoes. Shield volcanoes have broad, gently sloping sides and are primarily composed of basaltic lava. Cinder cone volcanoes are small, steep-sided volcanoes that erupt primarily cinder-sized fragments. Stratovolcanoes are tall, conical volcanoes composed of alternating layers of lava flows, volcanic ash, and other materials.