It depend what rock it is but extrusive rocks generally non-crystalline or have a grain size of less than 1 mm
It depends on if it is intrusive or extrusive. If it is an intrusive rock, it is formed when magma hardens under the earth and has a larger grain size. If it is an extrusive rock, it is formed when lava hardens on the earth's surface and has a smaller grain size.
Basalt and gabbro are both igneous rocks, with major differences in grain size and where they form. Basalt has fine-grained crystals and forms from lava flows on the Earth's surface, while gabbro has coarse-grained crystals and forms from magma cooling beneath the Earth's surface.
It is an example of extrusive igneous rock.
Igneous rocks formed at the Earth's surface are called extrusive igneous rocks. They form when magma cools and solidifies quickly on the Earth's surface, resulting in fine-grained or glassy textures. Examples include basalt and rhyolite.
Volcanic glass is an extrusive igneous rock. It forms when molten lava cools quickly on the Earth's surface, preventing the formation of crystals.
== Grain size. Most intrusive igneous rocks will have visible crystals. Crystals in most extrusive igneous rocks are not easily visible.
Extrusive igneous rocks are usually fine grained.
Neither. Conglomerate is a sedimentary rock. Intrusive and extrusive are descriptive terms used to classify igneous rocks.
fined grain texture
It depends on if it is intrusive or extrusive. If it is an intrusive rock, it is formed when magma hardens under the earth and has a larger grain size. If it is an extrusive rock, it is formed when lava hardens on the earth's surface and has a smaller grain size.
Extrusive igneous rocks generally have a fine grain texture. This is because they cool quickly on the Earth's surface, causing the minerals to form small crystals.
Fine grained
by the size of the crystals, big crystals intrusive, small crystals extrusive
To determine whether an igneous rock is of intrusive or extrusive origin, examine its texture and mineral grain size. Intrusive igneous rocks, formed from magma cooling slowly beneath the Earth's surface, typically display larger crystals and a coarse-grained texture. In contrast, extrusive igneous rocks, formed from lava cooling quickly on the surface, usually have a fine-grained or glassy texture with smaller crystals. Additionally, the presence of volcanic features like vesicles or a glassy surface can indicate extrusive origins.
yes, it does. when a grain size in an igneous rock is small, it means that it was probably an extrusive rock, meaning it formed on land. but if the grain size is big, it means that the rock most likely formed underground, or it was intrusive. try remembering it like this- the larger the crystals, the more time the rock had to form, and magma cools faster on land, not giving the rocks much time to form.
Petrologists use grain size as an indicator of cooling rates to differentiate between intrusive and extrusive igneous rocks. Intrusive rocks, which form from magma cooling slowly beneath the Earth's surface, typically exhibit larger, well-defined crystals due to the extended time for crystal growth. In contrast, extrusive rocks cool rapidly on the surface, resulting in smaller grains or a glassy texture. Thus, the size and texture of the mineral grains provide key insights into the rock's formation environment.
What is the effect of location on crystal size? Label the location of intrusive and extrusive igneous rocks on the diagram below. Then, illustrate the crystal size of the rock formed at that location in the appropriate callout circles.