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Crystal
Because the rapid cooling does not allow much time for crystal growth.
the cooling and solidification of molten magma or lava. This process occurs either underneath the Earth's surface, resulting in intrusive igneous rocks, or on the surface, leading to extrusive igneous rocks. The rate of cooling determines the texture and crystal size of the rock, with slower cooling allowing for larger crystals to form.
Igneous rocks are formed by cooling magma.
Magmatic (lava) cooling.
Crystal
The size of crystals decreases as the cooling increases. This is called an inverse relationship.
The size of crystals decreases as the cooling increases. This is called an inverse relationship.
The size of crystals decreases as the cooling increases. This is called an inverse relationship.
Crystal size in igneous rocks is controlled by the rate of cooling whereby the slower the rate, the larger the size of crystal.
because of quick cooling igneous rocks .
Lava flows cool rapidly compared to the cooling of rocks underground. The slower cooling time of intrusive igneous rocks allows larger crystal formation. Generally, the more cooling time, the larger the crystals.
Because the rapid cooling does not allow much time for crystal growth.
Igneous rocks are formed by cooling magma.
the cooling and solidification of molten magma or lava. This process occurs either underneath the Earth's surface, resulting in intrusive igneous rocks, or on the surface, leading to extrusive igneous rocks. The rate of cooling determines the texture and crystal size of the rock, with slower cooling allowing for larger crystals to form.
igneous rocks
Igneous rocks are formed as the result of cooling magmas.