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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.
because of quick cooling igneous rocks .
A vesicular igneous texture generally indicates rapid cooling.
the crystal size of its minerals
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
Primarily the cooling rate of the mineral compound.The faster the rate cooling smaller the crystal size of the mineral.Consequently, large crystal specimins are derived from igneous bodies with a very slow rate of cooling.
because of quick cooling igneous rocks .
A vesicular igneous texture generally indicates rapid cooling.
Because the rapid cooling does not allow much time for crystal growth.
the crystal size of its minerals
the crystal size of its minerals
Crystal size in igneous rocks is generally a marker for how long magma or lava took to cool and solidify. Larger crystal size is indicative of slow cooling.
Quick cooling of magma results in small crystal formation. Slow cooling magma results in larger crystals.