Tiny crystals in the igneous rock tells you it cooled quickley.
The presence of large crystals in an igneous rock indicates that the rock cooled slowly beneath the Earth's surface, allowing sufficient time for the crystals to grow to a larger size. This type of slow cooling typically occurs in intrusive igneous rocks, such as granite.
The size of crystals in an igneous rock is called texture. Texture can range from fine-grained (small crystals) to coarse-grained (large crystals).
Igneous rocks can have both small and large crystals, depending on how quickly they cool. If an igneous rock cools slowly beneath the Earth's surface, it can form large crystals, while rapid cooling at the Earth's surface or in an eruption can result in small or no visible crystals.
Phenocrysts are the larger mineral grains in a porphyritic igneous rock. These crystals are surrounded by a finer-grained matrix known as the groundmass. The presence of phenocrysts helps in understanding the cooling history of the rock.
You would expect to find an igneous rock with small crystals near the Earth's surface where the rock cools relatively quickly, such as in volcanic eruptions or magma intrusions that do not have much time to grow large crystals. These rocks are known as volcanic or extrusive igneous rocks.
The presence of large crystals in an igneous rock indicates that the rock cooled slowly beneath the Earth's surface, allowing sufficient time for the crystals to grow to a larger size. This type of slow cooling typically occurs in intrusive igneous rocks, such as granite.
Intrusive rock normally has visible crystals. Extrusive igneous rock has small crystals. A black extrusive igneous rock with small crystals could be basalt.
The size of the crystals in an igneous rock tells us how fast the magma cooled.
Granite with larger crystals, basalt with smaller crystals.
The rock with crystals inside in can be igneous rock, but no, idk about the minerals.
sedimantry
yes
The size of the mineral crystals in an igneous rock determines the rock's texture.
The size of crystals in an igneous rock is called texture. Texture can range from fine-grained (small crystals) to coarse-grained (large crystals).
Well The Igneous Rock: When it Forms Underground the Pressure combines with Large crystals :)
Igneous rocks can have both small and large crystals, depending on how quickly they cool. If an igneous rock cools slowly beneath the Earth's surface, it can form large crystals, while rapid cooling at the Earth's surface or in an eruption can result in small or no visible crystals.
The presence of large and small crystals in igneous rock indicates a varied cooling history of the magma from which the rock formed. Large crystals suggest that the magma cooled slowly, allowing time for the crystals to grow, typically occurring in intrusive (plutonic) environments. In contrast, small crystals indicate rapid cooling, which is characteristic of extrusive (volcanic) environments. This mixed texture may point to a complex cooling process, such as the mingling of different magma types or changes in cooling rates during the rock's formation.