Eventually, some of the magma pushes through vents and fissures to the Earth's surface. Since it is lighter than the solid rock around it, magma rises and collects in magma chambers. Lava Butte, however, is 4,970 feet high and has created a flow that goes five miles north and three to the west.Deep within the Earth it is so hot that some rocks slowly melt and become a thick flowing substance called magma. Normal cones in this area are generally 200 feet high while some of the larger ones reach 400 feet. Lava Butte is one of the over 400 cinder cone volcanoes that surround the Newberry volcano. Paricutin was active for nine years, during which time it destroyed the nearby town San Juan and covered a large area of around a hundred square miles with ash. It also has a crater at the top that is the result of its last explosive eruption. It was caused by gas escaping from the molten lava within, which then formed cinders which landed around the vent and eventually built the cone to an altitude of 1,200 feet. Paricutin is a cinder cone located in Mexico and first started developing on a farm in 1943. This cone is the result of Strombolian eruptions that occurred several years apart and is 500 meters high. This volcano is in a group of four cinder cone volcanoes located in the Maribios Range. It was first created in April of 1850 and since then has been one of the most active in the country. Cerro NegroĬerro Negro is located in Nicaragua and is currently the youngest volcano in Central America. In some cases when strong winds are blowing at the time of the eruption, cinder cone volcanoes may have slightly different shapes at their base, such as more of a horseshoe instead of the normal circular base. Because these fragments can seem to sparkle and glow, they can make very beautiful and dramatic displays during eruptions. Because these fragments, called scoria or cinders, are melted rock with gas-filled pieces they cool very quickly and will generally accumulate near the opening of the vent, continuing the development of the cone shape of the volcano. In their eruptions the lava will generally erupt from one of the small vents found in the crust and fragments will be sprayed into the air. When compared to the eruptions you will find with other volcanoes, cinder cone volcanoes have relatively small ones. In addition, they will generally be topped by a crater at their summit. They can range from tens of meters to hundreds and will usually be created over much shorter periods of time than other volcanoes. They are frequently near calderas, stratovolcanoes and shield volcanoes. You are most likely to find this type of volcano near other larger volcanoes and these are relatively small in comparison. The main feature of cinder cone volcanoes is their conical shape together with steeply angled sides. That is because these are the ones that have a cone-shaped peak most people have come to associate with volcanoes in general. Cinder cone volcanoes are the volcanoes that most people think of when they picture a volcano erupting. Although they can refer to a part of a volcano cinder cones, or scoria cones, are actually volcanoes themselves.
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