Tephra, or dried lava.
Basaltic. There is more gas content than in most basaltic magma so that when a cinder cone erupts, The pressure builds up and makes the eruption somewhat explosive. Tephra, or dried lava/magma, is shot up, and joined to the volcano making it larger. In Science. Cinder cone volcanoes are the most common type of volcanoes. They are characterized by steeply angled sides and a conical shape. They are relatively small in size and can rang … e from tens to hundreds of meters in height. They are often found along the flanks of larger, more mountain sized volcanoes A cinder cone or scoria cone is a steep conical hill of loose pyroclastic fragments, such as either volcanic clinkers, cinders, volcanic ash, or scoria that has been built around a volcanic vent. The most famous cinder cone, Paricutin, grew out of a corn field in Mexico in 1943 from a new vent. Eruptions continued for 9 years, built the cone to a height of 424 meters, and produced lava flows that covered 25 km². The Earth's most historically active cinder cone is Cerro Negro in Nicaragua. C inder cones are the simplest type of volcano. They are built from particles and blobs of congealed lava ejected from a single vent. As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as cinders around the vent to form a circular or oval cone.  The Cinder-cone Volcano. Cinder cone volcanoes are the most common kind of volcanoes.They are steep sided cones of basaltic fragments and are smaller and simpler than composite volcanoes. Streaming gases carry liquid lava blobs into the atmosphere that fall back to earth around a single vent to form the cone.  Scoria cones, also known as cinder cones, are the most common type of volcano. They are also the smallest type, with heights generally less than 300 meters. They can occur as discrete volcanoes on basaltic lava fields, or as parasitic cones generated by flank eruptions on shield volcanoes and stratovolcanoes.  Cinder cone volcanoes are steep, cone-shaped volcanoes built from lava fragments called 'cinders.' These volcanic cinders, also known as ' scoria ,' are glassy volcanic fragments that explode from the volcano and cool quickly, building up the sides of the cinder cone volcano fairly quickly. Cinder Cone Volcanoes. Cinder cone volcanoes are steep, cone-shaped volcanoes built from lava fragments called 'cinders.' These volcanic cinders, also known as ' scoria ,' are glassy volcanic fragments that explode from the volcano and cool quickly. Cinder cones. Cinder cones are the simplest type of volcano. They are built from particles and blobs of congealed lava ejected from a single vent. As the gas-charged lava is blown violently into the air, it breaks into small fragments that solidify and fall as cinders around the vent to form a circular or oval cone. Shield volcanoes. Shield volcanoes, the third type of volcano, are built almost entirely of fluid lava flows. Flow after flow pours out in all directions from a central summit vent, or group of vents, building a broad, gently sloping cone of flat, domical shape, with a profile much like that of a warrior's shield. Cinder Cone Volcano. Although they can refer to a part of a volcano cinder cones, or scoria cones, are actually volcanoes themselves. Cinder cone volcanoes are the volcanoes that most people think of when they picture a volcano erupting. That is because these are the ones that have a cone-shaped peak most people have come to associate with volcanoes in general. Lava Butte. Lava Butte is one of the over 400 cinder cone volcanoes that surround the Newberry volcano. Normal cones in this area are generally 200 feet high while some of the larger ones reach 400 feet. Lava Butte, however, is 4,970 feet high and has created a flow that goes five miles north and three to the west. Cinder cone volcanoes (also called scoria cones) are the most common type of volcano and are the symmetrical cone shaped volcanoes we typically think of. They may occur as single volcanoes or as secondary volcanoes on the sides of stratovolcanoes or shield volcanoes. A volcano is a vent or fissure in Earth's crust through which lava, ash, rock and gases erupt. A volcano is also a mountain formed by the accumulation of these eruptive products. Let's take a look at how volcanoes form: Earth's crust is 40 to 250 miles (64 to 402 kilometers) thick.
http://www.answers.com/Q/Type_of_lava_in_a_cinder_cone_volcano https://en.wikipedia.org/wiki/Cinder_cone http://pubs.usgs.gov/gip/volc/types.html http://kilmer.wikispaces.com/Volcano+Types http://www.geology.sdsu.edu/how_volcanoes_work/scoriacone_page.html http://study.com/academy/lesson/types-of-volcanoes-shield-cinder-cones-composite-cones.html http://www.factmonster.com/ipka/A0862596.html http://www.basicplanet.com/cinder-cone-volcano/ http://www.livescience.com/27295-volcanoes.html
what type of lava comes out of a cinder cone volcano