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Plutonic rocks are intrusive (they solidify before they reach the surface) and have larger crystals because the crystals have had a longer time to accumulate in the heat under the surface.

Volcanic rocks are extrusive (they solidify on or near the surface) and have smaller crystals because the element has less time to accumulate when they cool quickly.

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Related Questions

As the rate of cooling of igneous rocks increases the size of the crystals that form .?

The size of crystals decreases as the cooling increases. This is called an inverse relationship.


As the rate of cooling of igneous rocks increases the size of the crystals that form?

The size of crystals decreases as the cooling increases. This is called an inverse relationship.


How is the size of crystals in an igneous rock related to the formation of a rock?

If an igneous rock is formed from slowly cooling magma under the ground, it has more time to form crystals and so the crystals it forms are much larger than igneous rock formed from more quickly cooling magma or lava.


. As the rate of cooling of igneous rocks increases the size of the crystals that form?

The size of crystals decreases as the cooling increases. This is called an inverse relationship.


How is the size of mineral crystals in igneous rock related to the rate at which they cool?

When igneous rocks cool quickly, they have small crystals and have a texture that may be described as aphanitic. When igneous rocks cool slowly, they have much larger crystals and have a texture that may be described as phaneritic or pegmatitic.


What are Igneous rocks that have large crystals and small crystals?

Igneous rocks with large crystals are called intrusive rocks, formed from magma cooling slowly beneath the Earth's surface, allowing for large crystals to form. Igneous rocks with small crystals are called extrusive rocks, formed from lava cooling quickly on the Earth's surface, resulting in small crystals due to rapid cooling.


What is the best clue to tell in extrusive igneous rocks from in instrusive igneous rock?

Extrusive igneous rocks have smaller crystals due to rapid cooling on the Earth's surface, while intrusive igneous rocks have larger crystals due to slower cooling beneath the Earth's surface. This difference in crystal size can help distinguish between the two types of rocks.


How does the rate of cooling influence crystal size of igneous rocks and how does that help you to distinguish between intrusive and extrusive igneous rocks?

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).


What rate of cooling produces the largest crystals in igneous rocks?

A slow rate of cooling will typically produce the largest crystals in igneous rocks. This allows more time for crystals to grow and develop before the magma solidifies completely. Rapid cooling results in smaller crystals or no crystals at all (forming volcanic glass).


Do igneous rocks have small crystals large crystals or no 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.


What is the difference in appearance between igneous rocks that have cooled slowly and igneous rocks that have cooled quickly?

Igneous rocks that cooled slowly are intrusive. Igneous rocks that cooled quickly are extrusive. Intrusive rocks form larger crystals, because the crystals have a longer time to grow. Extrusive rocks have small to no crystals, because they had little or no time to grow/form.


Why do some igneous rocks have big crystals or grains and some igneous rocks have small crystals or grains?

Igneous rocks with big crystals or grains form from slow cooling beneath the Earth's surface, allowing time for larger crystals to grow. In contrast, igneous rocks with small crystals or grains form from fast cooling at or near the Earth's surface, limiting the time available for crystal growth.