what happens is that it forms a caldera
A form of volcano that collapses in on itself is called a caldera. This occurs when a volcano erupts and empties its magma chamber, leading to a significant loss of structural support. As a result, the ground above the emptied chamber collapses, creating a large depression. Calderas can be quite vast and may eventually fill with water, forming lakes.
A caldera is a large bowl-shaped formation that occurs when the top of a volcano collapses into the emptied magma chamber beneath it. This can happen during a volcanic eruption when the magma chamber is emptied, causing the structure above it to collapse inward.
Deception Island is a caldera volcano, which is formed when the top of a volcano collapses into the emptied magma chamber below. It is a type of stratovolcano located in the South Shetland Islands of Antarctica.
A Volcano that spawns a new cone, partially filling its caldera, is called, a somma volcano. When the new cone outgrows the original caldera, it is given a name of its own. It is the original volcano, the underlying structure, that is known as the somma volcano. These can be, and often are, stratovolcanoes themselves.
Sometimes after an eruption , the top of a volcano may collapse down into the partially emptied magma chamber. Which creates a very large opening called a caldera.
A form of volcano that collapses in on itself is called a caldera. This occurs when a volcano erupts and empties its magma chamber, leading to a significant loss of structural support. As a result, the ground above the emptied chamber collapses, creating a large depression. Calderas can be quite vast and may eventually fill with water, forming lakes.
A caldera is a large bowl-shaped formation that occurs when the top of a volcano collapses into the emptied magma chamber beneath it. This can happen during a volcanic eruption when the magma chamber is emptied, causing the structure above it to collapse inward.
Deception Island is a caldera volcano, which is formed when the top of a volcano collapses into the emptied magma chamber below. It is a type of stratovolcano located in the South Shetland Islands of Antarctica.
calderacalderaIt forms a caldera.
A Volcano that spawns a new cone, partially filling its caldera, is called, a somma volcano. When the new cone outgrows the original caldera, it is given a name of its own. It is the original volcano, the underlying structure, that is known as the somma volcano. These can be, and often are, stratovolcanoes themselves.
Sometimes after an eruption , the top of a volcano may collapse down into the partially emptied magma chamber. Which creates a very large opening called a caldera.
Caldera
Caldera
A saucer-shaped depression at the mouth of a volcano is called a volcanic caldera. Calderas are formed when a volcano collapses into the emptied magma chamber below, creating a large, basin-like crater.
A caldera is formed when a volcano collapses into the emptied magma chamber below after a major eruption, leaving a large, basin-shaped depression. This collapse can be triggered by the withdrawal of magma during an eruption or by the weight of material above the magma chamber becoming unstable.
A mass rock is formed when a volcano's magma chamber empties and the overlying rock collapses into the empty chamber. This creates a steep-walled depression or caldera at the volcano's summit. It is a common feature of collapsed volcanoes.
The large circular depression at the top of a volcano that forms when the roof of the magma chamber collapses is called a caldera. Calderas can be huge in size and are formed during explosive volcanic eruptions or when the magma chamber empties and the summit collapses into the void left behind.