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If the rocks are igneous then in general:- Coarse = slowly. Fine = fast. However if the rocks are metamorphic or sedimentary then grain size has nothing to do with cooling and indicates other things.
Not as heavy as metamorphic but it really depends on the type of igneous rock and the size
1.Grain Size 2.Grain Shape 3.Grain Pattern
The cooling rate of the rock.
Geologists classify rocks by where they are formed; above ground or under ground
== Grain size. Most intrusive igneous rocks will have visible crystals. Crystals in most extrusive igneous rocks are not easily visible.
It depend what rock it is but extrusive rocks generally non-crystalline or have a grain size of less than 1 mm
Crystal size in igneous rocks is controlled by the rate of cooling whereby the slower the rate, the larger the size of crystal.
yes, it does. when a grain size in an igneous rock is small, it means that it was probably an extrusive rock, meaning it formed on land. but if the grain size is big, it means that the rock most likely formed underground, or it was intrusive. try remembering it like this- the larger the crystals, the more time the rock had to form, and magma cools faster on land, not giving the rocks much time to form.
If the rocks are igneous then in general:- Coarse = slowly. Fine = fast. However if the rocks are metamorphic or sedimentary then grain size has nothing to do with cooling and indicates other things.
Fast cooling lava or magma creates an aphanitic or small crystal (grain) textured igneous rock.
Rocks with a large grain size perhaps with angular grain shapes.
They are rocks with a small grain size.
The rate at which the igneous rock cools controls grain size. Slower cooling results in larger crystals while faster cooling results in smaller crystals.
Not as heavy as metamorphic but it really depends on the type of igneous rock and the size
crystal size
1.Grain Size 2.Grain Shape 3.Grain Pattern