answersLogoWhite

0


Best Answer

Slowing cooling produces large crystals eg granite. Fast cooling makes much smaller crystals eg basalt

User Avatar

Wiki User

15y ago
This answer is:
User Avatar
More answers
User Avatar

AnswerBot

2mo ago

Slow cooling of igneous rocks typically forms large crystal grains. This is because slow cooling allows more time for mineral grains to grow, resulting in larger crystals. Examples of rocks formed through slow cooling and having large crystal grains include granite and gabbro.

This answer is:
User Avatar

User Avatar

Wiki User

15y ago

Yes, all rocks are made of crystals, and the slower a volcanic rock (magma) cools the larger the crystals grow (because there is more time for them to get bigger).

This answer is:
User Avatar

Add your answer:

Earn +20 pts
Q: Does slow cooling of igneous rocks form large or small crystal grains?
Write your answer...
Submit
Still have questions?
magnify glass
imp
Related questions

What do large crystal grains in an igneous rock indicate?

Large crystal grains in an igneous rock indicate that the rock cooled slowly at depth beneath the Earth's surface, allowing sufficient time for the crystals to grow. This slow cooling process typically occurs in intrusive or plutonic igneous rocks.


What is the textural difference between coarse-grained phaneritic and fine-grained aphanitic rocks?

Coarse-grained phaneritic rocks have large, visible crystals that formed slowly beneath the Earth's surface, giving them a rough texture. In contrast, fine-grained aphanitic rocks have tiny crystals that formed quickly at or near the Earth's surface, resulting in a smooth texture without visible crystals.


Large crystal grains in an igneous rock are an indication that crystals formed?

slowly from a magma with abundant time to grow. This can suggest an intrusive or plutonic igneous rock type, such as granite. Rapid cooling leads to small crystal grains, characteristic of extrusive or volcanic igneous rocks like basalt.


Lin found an igneous rock with large grains of mineral crystal where did this rock most likely form?

d. on the surface of the Earth


Is the crystal in the igneous rock large if it cools slowly from magma?

Yes. Slow cooling magma produces larger mineral crystals.


What the grains found in igneous rock?

Grains found in igneous rock are minerals that solidified from a molten state. They can be coarse or fine, depending on the cooling rate of the magma. Common minerals found as grains in igneous rock include quartz, feldspar, mica, and olivine. The size, shape, and arrangement of these grains can provide clues about the cooling history and composition of the rock.


What type of crystals is formed from slow cooling?

Crystals formed from slow cooling typically have larger crystal sizes due to more time for the atoms to arrange in an ordered structure. This results in minerals with well-defined crystal faces and clearer textures, as seen in intrusive igneous rocks like granite and gabbro.


Formed from slow cooling magma speckled with large minerals grains?

This describes an igneous rock with a coarse-grained texture, likely formed deep within the Earth's crust where cooling is slower, allowing time for large mineral grains to form. This type of rock is typically intrusive, such as granite or diorite, and is characterized by its visibly distinct mineral grains.


What are three things crystal size dependent on?

Crystal size is dependent on factors such as temperature, rate of cooling, and concentration of solute in the solution. These factors can influence the rate of crystal growth and therefore affect the final size of the crystals formed.


Size of sedimentary mineral crystal grain?

that means like when somthing is in a own properties


What type of rock that forms from magma or lava is rock?

Igneous rock is formed from the cooling of magma or lava.


What does an igneous rock's crystal grain size indicate to the observer?

The size of the mineral crystals in an igneous rock is related to the rate of time spent in cooling from magma. Longer exposure to the crystallization temperature means larger crystals. Less time means smaller crystals, or in the case of obsidian, which cools extremely quickly, no crystallization.