Yes. Fast cooling of magma causes small crystal size or no crystal at all.
Fast cooling lava or magma creates an aphanitic or small crystal (grain) textured igneous rock.
The resultant rock would have a porphyritic texture; large crystals (usually feldspars) scattered among small crystal grains.
The speed at which the magma/lava cools ie. fast cooling = not much time for crystals to form = little or no small crystals slow cooling = much time for crystals to form = big crystals
Generally, large crystals represent slow cooling rates and small crystals represent fast cooling rates. Crystals need time to form and since extrusive rocks cool very quickly, they have very tiny crystals and some don't even have crystals because the rate of cooling was so fast that crystals didn't have time to nucleate. On the other hand, intrusive rocks cool rather slowly allowing crystals to grow.
small,light grains of rock larger rocks slow movig large,heavy pieces of rock fast moving smaller rocks
yes it does
Fast cooling lava or magma creates an aphanitic or small crystal (grain) textured igneous rock.
The resultant rock would have a porphyritic texture; large crystals (usually feldspars) scattered among small crystal grains.
Slow cooling of igneous rocks typically forms large crystal grains. This is because slow cooling allows more time for mineral grains to grow, resulting in larger crystals. Examples of rocks formed through slow cooling and having large crystal grains include granite and gabbro.
Fast cooling=small crystals Slow cooling=big crystals
The speed at which the magma/lava cools ie. fast cooling = not much time for crystals to form = little or no small crystals slow cooling = much time for crystals to form = big crystals
fast cooling lava -small crystals or no crystals
fast cooling lava -small crystals or no crystals
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.
no
Pumice is the result of extremely fast cooling lava.
Generally, large crystals represent slow cooling rates and small crystals represent fast cooling rates. Crystals need time to form and since extrusive rocks cool very quickly, they have very tiny crystals and some don't even have crystals because the rate of cooling was so fast that crystals didn't have time to nucleate. On the other hand, intrusive rocks cool rather slowly allowing crystals to grow.