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.
Stratovolcanoes, also known as composite volcanoes, are formed from both flowing lava and falling cinders and tephra. These types of volcanoes have steep slopes and are characterized by alternating explosive eruptions and effusive lava flows. Mount St. Helens in the USA and Mount Fuji in Japan are examples of stratovolcanoes.
Stratovolcanoes, also known as composite volcanoes, are formed from both flowing lava and falling cinders and tephra. These volcanoes are characterized by their steep-sided cones and explosive eruptions, which result in a combination of lava flows and ash deposits. Some well-known stratovolcanoes include Mount St. Helens in the United States and Mount Fuji in Japan.
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 steep-sided volcano of lava and tephra is called a stratovolcano. Stratovolcanoes are characterized by their tall, conical shape and explosive eruptions caused by the buildup of pressure from gases and molten rock beneath the surface.
Communists make them
Cinder cone volcano
No. Cinder cones are formed by basaltic magma.
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.
Stratovolcanoes, also known as composite volcanoes, are formed from both flowing lava and falling cinders and tephra. These types of volcanoes have steep slopes and are characterized by alternating explosive eruptions and effusive lava flows. Mount St. Helens in the USA and Mount Fuji in Japan are examples of stratovolcanoes.
some times in Hawaii or in an ocean
Cinder cone volcanoes are formed by basaltic magma.
Three landforms that can be created from ash are cinder cone volcanoes, composite volcanoes, and shield volcanoes. Lava plateaus can also be formed.
Stratovolcanoes, also known as composite volcanoes, are formed from both flowing lava and falling cinders and tephra. These volcanoes are characterized by their steep-sided cones and explosive eruptions, which result in a combination of lava flows and ash deposits. Some well-known stratovolcanoes include Mount St. Helens in the United States and Mount Fuji in Japan.
Cinder Cone, Shield, and Strato.
They're all volcanoes..., they are both formed by plates overlapping or clashing together
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.