Obsidian, which is volcanic glass, is a good example.
No, extrusive rocks typically have smaller grains than intrusive rocks. Extrusive rocks form from lava that cools quickly on the Earth's surface, resulting in fine-grained or glassy textures. In contrast, intrusive rocks form from magma that cools slowly beneath the surface, allowing larger crystals to develop. Thus, intrusive rocks generally have larger grains compared to extrusive rocks.
Extrusive igneous rocks are formed when lava cools and solidifies quickly on or near the Earth's surface. Due to the rapid cooling, extrusive rocks typically have small mineral grains or a glassy texture. Common examples include basalt, andesite, and rhyolite.
Igneous rock is formed from the cooling of magma or lava.
The individual grains (crystals) in quickly cooled magma are described as aphanitic--not visible without magnification.
Extrusive igneous rocks have very small crystal grains.
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).
No, extrusive rocks typically have smaller grains than intrusive rocks. Extrusive rocks form from lava that cools quickly on the Earth's surface, resulting in fine-grained or glassy textures. In contrast, intrusive rocks form from magma that cools slowly beneath the surface, allowing larger crystals to develop. Thus, intrusive rocks generally have larger grains compared to extrusive rocks.
The intrusion is insulated by the surrounding rock, letting it cool very slowly and allowing crystals time to grow to larger sizes. In rapidly cooled rocks the grains can be so small that they are almost undetectable as no significant crystal growth happened.
You can describe the rock by the process that allowed it to cool quickly: "Extrusive" or you can describe it by its texture: "aphanitic". An extrusive rock tends to be aphanitic = Rocks formed from lava flows tend to have small crystals.
Two examples that come to my mind right away are Basalt and Obsidian. You can tell on your own if a rock has cooled quickly by whether or not you can see individual grains of minerals within the rock. So if you cant see any, then its most likely that the rock cooled quickly.
Extrusive igneous rocks are formed when lava cools and solidifies quickly on or near the Earth's surface. Due to the rapid cooling, extrusive rocks typically have small mineral grains or a glassy texture. Common examples include basalt, andesite, and rhyolite.
The major difference is their formation location: intrusive rocks are formed below the Earth's surface from the slow cooling of magma, resulting in coarse-grained textures, while extrusive rocks are formed on the Earth's surface from rapid cooling of lava, resulting in fine-grained textures. Intrusive rocks have larger mineral grains due to their slower cooling process, whereas extrusive rocks have smaller mineral grains due to their faster cooling process.
This type of igneous rock is called "extrusive igneous rock." It forms when lava cools and solidifies quickly on the Earth's surface, resulting in small mineral grains that are characteristic of rocks like basalt or rhyolite.
Small crystal grains form when molten rock cools quickly. In an extrusive igneous rock, it's referred to as aphanitic texture.
cool too quickly for mineral grains to form, resulting in a non-crystalline structure.
Coarse is intrusive: the magma cooled slowly when it was formed causing big crystals... Fine is extrusive: the magma cooled quickly when it was formed causing small crystals!! your welcome mrs. bergs class:)
Igneous rock is formed from the cooling of magma or lava.