Granular texture.
That it cooled very slowly.
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.
An igneous rock's crystal size is dependent on how long it takes to cool from magma into a solid. Intrusive igneous rocks, the ones that solidify from magma underground, are slow to harden, giving crystals plenty of time to grow larger. Extrusive igneous rocks, formed from lava above ground, cool fairly rapidly, not allowing the crystals much time to grow in size.
Igneous rock forms when magma cools and hardens. This type of rock can be classified as intrusive (plutonic) if it cools below the Earth's surface (slow cooling) or extrusive (volcanic) if it cools quickly on the Earth's surface. Examples of igneous rocks include granite, basalt, and obsidian.
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.
The size of the mineral crystals in an igneous rock determines the rock's texture.
The size of the crystals in an igneous rock tells us how fast the magma cooled.
Small
mineral crystals
by the size of the crystals, big crystals intrusive, small crystals extrusive
When magma cools down it forms a type of rock called igneous rock. Igneous rock can cool inside the earth or it can cool after it has come out on the earth's surface. When it is formed inside it is called intrusive but when it is on the earth's surface it is called extrusive.
== Grain size. Most intrusive igneous rocks will have visible crystals. Crystals in most extrusive igneous rocks are not easily visible.
please anyone else can answer this question I'm in hurry pls.
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.
The texture depends on the size and shape of the crystals you see in it. The larger the crystals, the slower the rate of cooling. This suggests that it is an intrusive rock. Smaller crystals suggest more rapid cooling indicating that it is an extrusive rock. INTRUSIVE- cooled inside the earth and had more time to create crystals EXTRUSIVE- cooled on the surface of the earth and created small crystals
Pegmatite texture is a coarse-grained igneous rock texture characterized by exceptionally large crystals. These crystals can be several centimeters to several meters in size. The slow cooling of molten rock in pegmatite formations allows for the growth of such large crystals.
Texture