bruh
Materials formed from molten rock include igneous rocks like granite and basalt, as well as volcanic glass like obsidian. When molten rock cools and solidifies, it forms these materials through processes like crystallization.
Granite is an igneous rock that forms on top of the Earth's crust. It is composed mainly of quartz and feldspar minerals and is commonly found in continental crust.
When hot molten material is thrown out of the earth's crust, it forms volcanic rocks such as basalt, andesite, or rhyolite. These rocks cool and solidify to create landforms like volcanic cones, lava flows, or volcanic domes.
The molten material moving upward within the Earth's crust is called magma. Magma is formed from the melting of rocks in the Earth's mantle and can rise to the surface through volcanic activity. As magma cools and solidifies, it forms igneous rocks.
bruh
because the molten rock cools in the water and forms a oceanic crust
metamorphic rock
Materials formed from molten rock include igneous rocks like granite and basalt, as well as volcanic glass like obsidian. When molten rock cools and solidifies, it forms these materials through processes like crystallization.
New land
A volcanic fissure or fissure vent forms when a central crack develops in the Earth's crust and allows molten rock to seep out onto the surface. This can result in the eruption of lava and the formation of new volcanic landforms.
Granite is an igneous rock that forms on top of the Earth's crust. It is composed mainly of quartz and feldspar minerals and is commonly found in continental crust.
Magma is newly formed hot molten rock that is forced upward from Earth's mantle through a vent or fissure in the crust. When this molten material reaches the surface, it solidifies and accumulates over time to form volcanic mountains.
When hot molten material is thrown out of the earth's crust, it forms volcanic rocks such as basalt, andesite, or rhyolite. These rocks cool and solidify to create landforms like volcanic cones, lava flows, or volcanic domes.
The continental crust is the layer of Earth that forms the continents. It is thicker and less dense than the oceanic crust, which is why it floats higher on the denser mantle beneath.
When molten material reaches the surface of the Earth, it can solidify into different forms depending on the speed of cooling. If it cools quickly, it forms extrusive igneous rocks like basalt. If it cools slowly underground, it forms intrusive igneous rocks like granite.
The molten material moving upward within the Earth's crust is called magma. Magma is formed from the melting of rocks in the Earth's mantle and can rise to the surface through volcanic activity. As magma cools and solidifies, it forms igneous rocks.