It is a valcano the is the cilinder
Cinder volcanoes, composite volcanoes, frision volcanoes, and cinder cone volcanoes.
Cinder cone volcanoes erupt explosively, but not as violently as composite volcanoes.
cinder cone volcanoes usually form around lithospheric plate boundaries.
Cinder cone, shield, and composite
Cinder cone, shield, and composite
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 main types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gently sloping sides and are formed by layers of lava flows. Stratovolcanoes are characterized by steep sides and explosive eruptions. Cinder cone volcanoes are small, steep-sided volcanoes built from explosive eruptions that eject fragmented rock.
A cinder cone has basaltic lava, which has a fairly low viscosity.
Cinder cone volcanoes are much shorter and a little bit wider.
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.
volcanoes in guatemala
Some famous cinder cone volcanoes include Parícutin in Mexico, Sunset Crater in Arizona, and Cerro Negro in Nicaragua.