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Paricutin is an example of a cinder cone volcano. It formed in 1943 in Mexico from a series of eruptions that built up a cone-shaped mountain.
by an undersea volcano that erupted from the ocean's floor. Spewing its lava (molten rock), the volcano built an undersea mountain that grew higher and higher, eventually growing above the surface of the sea.
Edinburgh castle is built on the site of an extinct volcano.
A scoria cone volcano, also known as a cinder cone volcano, is the type of volcano that has small basaltic cones built during one short eruptive episode. These volcanoes are characterized by their steep sides and formed by the accumulation of volcanic debris, such as scoria and ash, ejected during explosive eruptions.
A strato-volcano, also known as a composite volcano, is made from alternating layers of solidified lava flows, volcanic ash, and other volcanic debris. These layers are built up over time as the volcano continues to erupt, creating the classic cone shape associated with strato-volcanoes.
Paricutin is an example of a cinder cone volcano. It formed in 1943 in Mexico from a series of eruptions that built up a cone-shaped mountain.
A volcano is formed when magma from beneath the Earth's crust reaches the surface through a vent or opening. While a mountain can be a volcano if it has been built up by volcanic activity, not all mountains are volcanoes.
Arenal Volcano in Costa Rica was formed through a series of eruptions that began around 7,000 years ago. The volcano is part of the Pacific Ring of Fire and its cone shape was created over time as layers of ash and lava built up from repeated eruptions. The most recent major eruption occurred in 1968.
A shield volcano.
Edinburgh castle is built on the site of an extinct volcano.
by an undersea volcano that erupted from the ocean's floor. Spewing its lava (molten rock), the volcano built an undersea mountain that grew higher and higher, eventually growing above the surface of the sea.
the two of earths plat collided and formed upwards and made a volcano!
A scoria cone volcano, also known as a cinder cone volcano, is the type of volcano that has small basaltic cones built during one short eruptive episode. These volcanoes are characterized by their steep sides and formed by the accumulation of volcanic debris, such as scoria and ash, ejected during explosive eruptions.
Edinburgh Castle is built high upon the basalt remains of a long extinct volcano.
A stratiform volcano is a type of volcano that is characterized by layers of lava flow that have gradually built up over time. These volcanoes tend to have broad, flat shapes with gentle slopes. They are typically associated with non-explosive eruptions that result in the slow extrusion of lava.
A strato-volcano, also known as a composite volcano, is made from alternating layers of solidified lava flows, volcanic ash, and other volcanic debris. These layers are built up over time as the volcano continues to erupt, creating the classic cone shape associated with strato-volcanoes.
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