Lava cools to become a crust of stone with many small air bubbles, often called lavarock
Rocks And Magma .
These are called lava domes.
volcano
A lava dome
Aa lava is the type of lava that forms a thick, brittle crust.
Silica will determine if the lava is hot and runny or thick and slow!
Aa is lava that forms a thick ,brittle crust . Pahoehoe is a lava that forms a thin crust. Pillow lava forms when lava erupts underwater. Blocky lava is kool, stiff lava that does not travel far from thr eruption site.
Lava tubs form as a result of pahoehoe lava flows. As one of these flows progresses, it builds of a layer of rock on top of it. eventually, thus becomes thick enough to support is own weight, and forms an insulating tube through which lava can flow.
Lava tubes formed from mafic lava form when the lava forms a crust over itself, creating a tube through which it can flow and later leave empty. Felsic lava forms a crust, but is too viscous to entirely flow out of it.
Aa lava is the type of lava that forms a thick, brittle crust.
2. Thick or runny lava. Thick flows slowly, runny flows faster.
Aa
Silica will determine if the lava is hot and runny or thick and slow!
Aa is lava that forms a thick ,brittle crust . Pahoehoe is a lava that forms a thin crust. Pillow lava forms when lava erupts underwater. Blocky lava is kool, stiff lava that does not travel far from thr eruption site.
This is called a lava dome.
Lava tubs form as a result of pahoehoe lava flows. As one of these flows progresses, it builds of a layer of rock on top of it. eventually, thus becomes thick enough to support is own weight, and forms an insulating tube through which lava can flow.
Lava tubes formed from mafic lava form when the lava forms a crust over itself, creating a tube through which it can flow and later leave empty. Felsic lava forms a crust, but is too viscous to entirely flow out of it.
A shield volcano. Generally they have runny lava that forms lots of thick layers. The Hawaiian island volcanos are good examples.
Pahoehoe
No. Pumice forms from gas-rich lava that is ejected into the air.
You would find the largest crystals in a lava flow in the center of the flow. The largest forms of igneous intrusions are called batholiths.