shield volcanoes have cinders that come out then land on it. that's what makes them bigger than cinder cone volcanoes.
shield volcanoes have cinders that come out then land on it. that's what makes them bigger than cinder cone volcanoes.
shield volcanoes have cinders that come out then land on it. that's what makes them bigger than cinder cone volcanoes.
shield volcanoes have cinders that come out then land on it. that's what makes them bigger than cinder cone volcanoes.
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
Three types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gentle slopes and are formed by low-viscosity lava, while stratovolcanoes are characterized by alternating layers of lava and ash. Cinder cone volcanoes are small, steep-sided volcanoes formed by pyroclastic material ejected during eruptions.
The three different types of volcanoes include the following; shield volcanoes, composite volcanoes, and the cinder cone volcanoes. These all have their names because of the size and shape of the out rocks of the actual volcano itself.
The Hawaiian islands are made of two types of volcanoes, shield volcanoes and cinder cone volcanoes. Shield volcanoes have broad bases with gentle slopes. Cinder cone volcanoes have steeper sides, are made from fragments of lava, and are usually located at the base of shield volcanoes.
Cinder volcanoes, composite volcanoes, frision volcanoes, and cinder cone volcanoes.
No. Shield volcanoes are quite large. Cinder cones are the smallest volcanoes.
The three types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gentle slopes and are formed by lava flows, stratovolcanoes are tall, steep-sided volcanoes built up by layers of hardened lava, rock, and ash, and cinder cone volcanoes are relatively small, steep-sided volcanoes made of pyroclastic material.
No. The Hawaiian islands are shield volcanoes.
The way a volcano is being formed, depends on the type of lava. Cinder cone volcanoes is made from andesitic lava. This type of lava is especially thick, and therefore is won't be able to ''run'' very far from the volcano. In this way, each time a cinder cone volcano erupts, it will create a new layer of lava, making the volcano higher and higher each time, but it will not increase its base area very much. It's different with shield volcanoes. They are made from another kind of lava which will advance very far from it's vent. Therefore the shield volcano won't often be very tall, but it can have a very large base area