A cinder cone volcano is constructed from pyroclastic materials ejected from a central vent. These pyroclastic materials which include lava, lahars, tuffs & welded tuffs accumulate to form the cone shape we observe in these tyoes of volcanoes. They generally have slopes ranging between 30 to 40 degrees. Cinder cones are generally small volcanoes and do not exceed 500m in height. Cinder cones erupt Andesitic lava which has a relativley high viscosity meaning it is thick and flows slowly. Because of the viscosity of the lava they erupt fairly explosivley.Cinder cones are very small and has lava that is very active and are very explosive
A cinder cone is a volcano that occurs near a volcanic vent. It is from "small" to "medium" height compared to other types of volcano, and it has steep sides built up of volcanic (clastic) rock. The sides are not "strong" as such, and if it erupts and expells lava, the lava will push out the weakest side (unless it actually "fountains" straight up) and flow out and down from there. The result will be a horseshoe shaped "partial cone" with the missing side being the way the lava will exit. There are a couple of examples in Paricutin in Mexico and Cerro Negro in Nicaragua. Links are provided to related Wikipedia articles. Knowledge is free there. Why not surf on over and help yourself?
its big
Ghicci Volcano, Alasad Volcano, Sheperd Volcano, Roach Volcano, Soap Volcano, and Price Volcano
Cinder cones are the mountainous structure built up by some volcanoes. Most of the material that makes up the cone is ash and cinders expelled from the top of the cone.
cinder cone volcanoes: consist of primarily erupted volcanic ash and rock fragments, or cinders. When the volcano erupts the ash and rock are ejected onto the mountain. As this process continues the volcano "grows" higher because of the debris build up.
Shield Volcanoes:Large base areaGentle slopeContains basic lavaFrequent eruptionsQuiet and gentle eruptionsVery tall in height due to large base areaComposite Volcanoes:Relatively small base areaConcave slopeContains acidic lavaViolent eruptionsRepeated eruptionsErupts from the side conesUsually not very tall in height due to gentle slopesAcid-lava VolcanoesSmall base areaSteep slopeContains acidic lavaViolent eruptionsCreates crater lakes (caldera) after eruptionsTall in height due to steep slopesCinder ConesSmall base areaSteep slopesSymmetrical slopesModerate eruptionsNot tall in height as slopes are easily eroded
shield volcanoes have cinders that come out then land on it. that's what makes them bigger than cinder cone volcanoes.
volcanoes in guatemala
Some cinder cone volcanoes in the Philippines are Musuan, or Calayao Volcano, and Mayon Volcano.
Some famous cinder cone volcanoes include Parícutin in Mexico, Sunset Crater in Arizona, and Cerro Negro in Nicaragua.
sunset crater
There are many hundreds of cinder cone volcanoes in the world. Some are in Hawaii but most are not. The Hawaiian islands themselves are shield volcanoes.
Some cinder cone volcanoes in the Philippines are Musuan, or Calayao Volcano, and Mayon Volcano.
Some famous cinder cone volcanoes include Parícutin in Mexico, Sunset Crater in Arizona, and Cerro Negro in Nicaragua.
Ghicci Volcano, Alasad Volcano, Sheperd Volcano, Roach Volcano, Soap Volcano, and Price Volcano
Cinder cones are the mountainous structure built up by some volcanoes. Most of the material that makes up the cone is ash and cinders expelled from the top of the cone.
There are four basic types of volcanos. They are cinder cones, shield volcanoes, composite volcanoes, and lava domes. Composite volcanoes share some characteristics of all the others.
Cerro Negro, Mount Shasta, Lava Butte
Most volcanoes of any type, including cinder cones, are found at plate boundaries, but some are associated with hot spots.