That there are hot spots concisting of gas under the earths surface.
A hot spot is not associated with a plate boundary.
Villarrica is a hot spot
All of the Hawaiian islands are volcanic in origin. The volcanoes are fed by a hot spot, where extra hot material wells up in the mantle, generating magma. This hot spot generally stays in one place while the Pacific Plate above it moves. As this happens, older volcanoes are carried away from the hot spot and lose their source of magma.
When a volcano moves away from a hot spot, it typically becomes inactive as the magma supply from the hot spot diminishes. Over time, the volcano may erode and eventually subside, leading to the formation of a seamount if it is underwater. Meanwhile, a new volcano may form over the hot spot as the tectonic plate continues to move, creating a chain of volcanic islands or seamounts. This process is evident in locations like the Hawaiian Islands.
what is a hot spot on a volcanoe
Villarrica is a hot spot
Villarrica is a hot spot
A hot spot is not associated with a plate boundary.
Villarrica is a hot spot
There are more than just five hot spots throughout the whole Earth. There is the Tasman hot spot, the Hawaii hot spot, the Galapagos hot spot, the Yellowstone hot spot, Easter Island hot spot, Bouvet hot spot, St. Helena hot spot, the Canary Islands hot spot, and then Iceland hot spot.
it is not a hot spot they can afford a police system
Hot spot volcanoes are not associated with plate boundaries except where the hot spot is coincidentally near one.
A hot spot. An example of a hot spot are the islands in Hawaii which were made from hot spots.
Hot Spot - musical - was created in 1963.
a dislexics hot spot
make your own hot spot
All of the Hawaiian islands are volcanic in origin. The volcanoes are fed by a hot spot, where extra hot material wells up in the mantle, generating magma. This hot spot generally stays in one place while the Pacific Plate above it moves. As this happens, older volcanoes are carried away from the hot spot and lose their source of magma.