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.
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
Both shield volcanoes and cinder cones primarily erupt basaltic lava.
They do not produce lava flows.
A cinder cone volcano typically has basaltic lava, which is low in silica content and flows easily. This results in the formation of steep-sided cones made of mostly cinders and volcanic ash.
Cinder cones typically have Strombolian eruptions, which are characterized by small to moderate explosions of lava and gas. These eruptions are named after the Stromboli volcano in Italy, which exhibits similar explosive activity.
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
Both shield volcanoes and cinder cones primarily erupt basaltic lava.
Yes, cinder cones can produce lava flows. Typically, these flows are relatively short and are composed of basaltic lava. Cinder cones are formed from the accumulation of volcanic cinders and ash around a central vent.
They do not produce lava flows.
A cinder cone volcano typically has basaltic lava, which is low in silica content and flows easily. This results in the formation of steep-sided cones made of mostly cinders and volcanic ash.
Cinder cones typically have Strombolian eruptions, which are characterized by small to moderate explosions of lava and gas. These eruptions are named after the Stromboli volcano in Italy, which exhibits similar explosive activity.
Cinder cones produce ash and chunks of lava rock called scoria.
No. Cinder cones are the most common variety.
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.
explosive
Acid lava cones are smaller and much steeper than ash/cinder cones. Acid lava cones are almost convex in shape and are formed due to thick lava that does not flow freely and cools before reaching very far. This gives in the conical 'dumpy' shape. While ash and cinder cones are more symmetrical and concave in shape. They are formed due to volcanic lava or volcanic bombs (of solidified lava) that was shot up in the air, cool and hardened and broke up into tiny pieces (of ash or cinders) before coming back down to the earth's surface.
Cinder cones are not made from lava flows. They are made of fragments of righ that have piled up and rest at their angle of repose.