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Lava.
The study of Earth's surface landforms is known as geomorphology.
Magma or lavaLava is molten rock. Magma is a mixture of molten rock and solids.
Intrusive igneous rocks are made from magma. Magma that is extruded onto the Earth's surface is known as lava and forms extrusive igneous rocks.
This is known as igneous petrogenesis.The liquification process is known as melting (or partial melting as commonly not all mantle material melts at the same temperature). This material is then normally either erupted onto the Earth's surface forming extrusive igneous rocks or intruded into the earth's crust froming intrusive igneous rocks when it cools. Together they can be thought of as the formational process that igenous rocks undergo which is known as igneous petrogenesis.
Lava.
The "crust" or biosphere
Metamorphic and igneous rocks are the two most common under the surface of earth.
This is known as the epicentre.
The study of Earth's surface landforms is known as geomorphology.
Magma that reaches the Earth's surface is known as lava.
The study of Earth's surface landforms is known as geomorphology.
toponym.
Igneous rock formed in the earths crust is known as intrusive rock. The magma that forms it cools slowly and therefore, creates rock with large crystals. An example of an intrusive igneous rock is granite.
Magma that reaches the surface is referred to as lava.magma that has reached the earth's surface tends to cool faster, that is why the rock will have more holes in it than a rock that has not reached the earth's surface. magma that has cooled enough to become a rock is known as a igneous rock. but there are two types of igneous rock. ther is intrusive igneous and extrusive igneous. intrusive is when the magma has cooled on the inside. this rock will have large crystals because it has cooled slower and most likely it will have a fine grained texture. extrusive igneous is when magma has reached earths surface (thats when it becomes lava) and has cooled. these rock with either have very small microscopic crystals or no crystals at all because the lava cools so quickly that they do not have enough time to really form.
This is known as the epicentre.
They are called Plutons, or plutonic igneous rocks, and are known as intrusive igneous rocks also.