No. Pumice cools very rapidly above the surface. It is a glassy rock. Glass forms when lava cools too quickly for crystals to form.
i thing becaUSE THEY ARE COOLED
Because they freeze really fast. When the strawberry is slowly frozen the inside of the strawberry will not freeze as quickly and could still rot in the proces of freezing.
Though pumice and granite are both igneous rocks, they are very different. Pumice is of extrusive origin (which means it formed when magma reached Earth's surface) and granite is of intrusive origin (which means it formed below Earth's surface). Pumice has a vesicular texture and granite is phaneritic (or coarse grained).
Porphyritic
Both move very slowly.
the particle will vibrate more slowly around its position.
yes, to a certain extend. The rock is cooled by the thermal extraction. It will slowly warm up again from radioactive decay (fission) in the earths core and crust.
i thing becaUSE THEY ARE COOLED
A crystal is a homogeneous solid substance that has a natural geometrically regular form. The crystals that form in slowly cooled magma produce large grains.
Because they freeze really fast. When the strawberry is slowly frozen the inside of the strawberry will not freeze as quickly and could still rot in the proces of freezing.
Crystallisation
Though pumice and granite are both igneous rocks, they are very different. Pumice is of extrusive origin (which means it formed when magma reached Earth's surface) and granite is of intrusive origin (which means it formed below Earth's surface). Pumice has a vesicular texture and granite is phaneritic (or coarse grained).
That it cooled very slowly.
That it cooled very slowly.
Igneous rocks that cooled slowly are intrusive. Igneous rocks that cooled quickly are extrusive. Intrusive rocks form larger crystals, because the crystals have a longer time to grow. Extrusive rocks have small to no crystals, because they had little or no time to grow/form.
Large mineral crystals that are all about the same size are formed from magma that cooled slowly inside the earth. Small mineral crystals (not identifiable without a microscope) formed from magma that cooled rapidly, on or near the surface of the earth.
Porphyritic