100 degrees Celsius over the next billion years is what I read when searching the same question.
Earthquake waves travel fastest in the interior of the Earth, as speed of waves increases as we go inside the Earth. The speed of a wave depends on the properties of the medium it travels in. The wave propagates faster in the denser and heavier core.
In reference to the cooling of magma into rock, basalt is formed from rapid cooling.
You would examine a fracture surface of the rock. Intrusive igneous rocks that have cooled very slowly underground have visible crystals and are said to have a phaneritic texture. Granite is an example of this type of rock. Extrusive igneous rocks that have cooled quickly from lava above or on the surface generally will have crystals too small to be visible with the naked eye, in a texture that is referred to as aphanitic. Obsidian is an example of this type of rock.
Obsidian is formed from very rapidly cooling lava.
it depends on if it is intrusive or extrusive (intrusive is below the earth and extrusive is at or above the earth) intrusive has a bigger crystal because it takes time to cool down.
They are either made through the fast cooling of lava, or the slow cooling if magma in the Earth.
Pumice is the result of extremely fast cooling lava.
Earthquake waves travel fastest in the interior of the Earth, as speed of waves increases as we go inside the Earth. The speed of a wave depends on the properties of the medium it travels in. The wave propagates faster in the denser and heavier core.
when something is heated the particles are moving very fast and then has it cools down (and heat releases into the air) particles begin to slow down, which means theyre cooling down.
the sun does not go downvthe earth rotates.
Yes. Fast cooling of magma causes small crystal size or no crystal at all.
Fast cooling=small crystals Slow cooling=big crystals
Craters and fast cooling
In reference to the cooling of magma into rock, basalt is formed from rapid cooling.
Fast cooling lava or magma creates an aphanitic or small crystal (grain) textured igneous rock.
You would examine a fracture surface of the rock. Intrusive igneous rocks that have cooled very slowly underground have visible crystals and are said to have a phaneritic texture. Granite is an example of this type of rock. Extrusive igneous rocks that have cooled quickly from lava above or on the surface generally will have crystals too small to be visible with the naked eye, in a texture that is referred to as aphanitic. Obsidian is an example of this type of rock.
Because gravity holds us down!