Cooling rate of molten rock
The bigger it is, the slower it cools and vise versa. -Life Science last year; Lots o' geology.
Not as heavy as metamorphic but it really depends on the type of igneous rock and the size
The size of the mineral crystals which comprise the rock.
The small bits that rocks are made from are called grains. These grains can vary in size and shape, and are typically composed of minerals or other solid materials.
Grains found in igneous rock are minerals that solidified from a molten state. They can be coarse or fine, depending on the cooling rate of the magma. Common minerals found as grains in igneous rock include quartz, feldspar, mica, and olivine. The size, shape, and arrangement of these grains can provide clues about the cooling history and composition of the rock.
The cooling rate of molten rock
== Grain size. Most intrusive igneous rocks will have visible crystals. Crystals in most extrusive igneous rocks are not easily visible.
The size shape and pattern of the rocks grains
They have mineral grains of nearly equal size, and have large crystals because they were cooled slowly.
igneous is the texture of igneous rocks. The texture of igneous rocks is defined by 3 ways: a) Crystallinity- it expresses the degree of formation of crystals in an igneous rock. the texture of an igneous rock may be Holocyrstalline (Completely characterised by crystals, Hemicrystalline (partially having crystals) and holocrystalline (no crystals). b) Granularity- it is the size of the grains. it may be equigranular (when mineral grains are equal in size) or inequigranular (when mineral grains are not equal in size). c) shape of crystals- The shape of crystals may be Euhedral (When all crystals are of same shape), Subhedral (when they are partially similar in shape), Anhedral (when they are completely different in shape).
The bigger it is, the slower it cools and vise versa. -Life Science last year; Lots o' geology.
The longer that magma is able to cool, the larger the crystals will be. Intrusive rocks will have larger crystals than extrusive rocks. For example granite (intrusive) has larger grains than rhyolite (extrusive).
The rock is conglomerate. The other rock would be Breccia if its grains were not rounded.
Not as heavy as metamorphic but it really depends on the type of igneous rock and the size
Difference in temperature of the varying layers of the Earth's surface where either of the rocks solidify,causes difference in size of grains of rocks.When solidified below the Earth's surface,the grains are comparatively larger crystals than extrusive igneous ones.Intrusive rocks form underneath the Earth's surface(eg.,granite). Magma cools slowly so it has time to form large crystals.Extrusive rocks are ones that form from lava (blasted out of a volcano) so they cool very quickly, not allowing large crystals to form(eg.,obsidian).
Tiny rocks the size of salt grains are generally called, "Sand".
crystal size