A caldera.
I actually had problems with this question on my crossword puzzle. The answer is actually a caldera. ---------------------------------- A volcanic crater would also be a correct answer.
The basin-shaped crater at the top of a volcano is called a caldera. It is typically formed after a volcanic eruption causes the volcano to collapse inward, creating a large depression. Calderas can range in size from a few kilometers to tens of kilometers in diameter.
No. A caldera is a volcanic structure. It is formed by the collapse of a volcao rather than a magma body.
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 volcanic crater is a large, basin-like depression at the summit of a volcano. It forms when the magma chamber beneath a volcano is emptied during an eruption, causing the overlying rock to collapse into the chamber. Craters can also be formed by explosive eruptions that blow out the summit of a volcano.
I actually had problems with this question on my crossword puzzle. The answer is actually a caldera. ---------------------------------- A volcanic crater would also be a correct answer.
The basin-shaped crater at the top of a volcano is called a caldera. It is typically formed after a volcanic eruption causes the volcano to collapse inward, creating a large depression. Calderas can range in size from a few kilometers to tens of kilometers in diameter.
No. A caldera is a volcanic structure. It is formed by the collapse of a volcao rather than a magma body.
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.
The basin shaped crater at the top of a mountain is called a caldera. It forms when a volcano collapses into itself after an eruption, creating a large, circular depression.
A volcanic crater is a large, basin-like depression at the summit of a volcano. It forms when the magma chamber beneath a volcano is emptied during an eruption, causing the overlying rock to collapse into the chamber. Craters can also be formed by explosive eruptions that blow out the summit of a volcano.
When the top of a volcanic mountain collapses, it forms a volcanic crater or caldera. This creates a bowl-shaped depression at the summit of the volcano.
A bowl-shaped depression that forms around the vent of a volcano is a crater. These craters can be formed by the explosion of volcanic material or the collapse of the volcanic cone following an eruption.
A hollow or depression in the Earth's surface is known as a cavity or crater. These formations can occur naturally due to erosion, volcanic activity, or impacts, or they can be human-made through activities like mining or excavation. Cavities and craters can vary in size and shape depending on the geologic processes that formed them.
A large depression in the land or ocean floor is typically known as a basin or a trough. These depressions can form through various geological processes such as tectonic activity, erosion, or volcanic activity. Basins and troughs can vary in size and shape, and are often associated with the accumulation of sediments.
A mountain basin is a bowl-shaped depression or hollow surrounded by higher ground such as mountains or hills. They are typically formed through geological processes like erosion or volcanic activity, and can sometimes contain bodies of water like lakes. Mountain basins can have unique ecosystems and provide important habitats for various plant and animal species.
A basin is a large, bowl-shaped container typically used for holding water or other liquids. It can also refer to a geological formation, such as a depression in the earth's surface that collects water.