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Igneous rock is formed from the cooling of magma or lava.
When igneous rocks from a volcanic eruption cool, they can form either intrusive or extrusive rocks. Intrusive igneous rocks form when magma cools slowly beneath the Earth's surface, resulting in larger mineral grains. Examples include granite and diorite. Extrusive igneous rocks form when lava cools quickly on the Earth's surface, resulting in smaller mineral grains. Examples include basalt and pumice.
The description oof it is big grains and there are visual and you can touch them always remember that it is intrusive igneous rock not extrusive rock igneous rock. and the color of it is GRAY!!!! Thankz for asking the questions ask more
Intrusive igneous rocks are created when magma pushes up into the Earth's crust and cools there. Although the decrease in pressure the magma experiences as it rises in the crust allows it to solidify, this is still a fairly slow process, so intrusive igneous rocks tend to have larger grains than extrusive igneous rocks. Granite and Gabbro are both intrusive igneous rocks.
Extrusive igneous rocks have very small crystal grains.
intrusive
That is correct.
All molten rock is capable of cooling quickly into fine-grained rocks, but here are some common fine-grained igneous rocks: Basalt Obsidian Andesite Rhyolite Tuff (a rock made from volcanic ash)
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).
Igneous rock is formed from the cooling of magma or lava.
The difference is the size of grains. Rhyolite is the felsic igneous rock with fine-grained size. Whereas, granite is the equivalent in composition but with coarse-grained size.
Cooling rate usually determines this the faster a mineral cools the finer the grains and the longer a mineral has to cool the larger the grain sizes. This relates to the rock being either being an intrusive or extrusive igenous rock, generally intrusive ones generally have longer to cool and thus have larger grains while extrusive ones have less time to cool and have finer grains. other factors can come into play as well especially in intrusive igneous rock, things like solid state diffusion and intrusions causing chill margins or pegmitites can change grain size as well. A more detailed description of the factors causing grains size would include factors such as nucleation, growth rate, crystal growth, undercooling and other factors
When igneous rocks from a volcanic eruption cool, they can form either intrusive or extrusive rocks. Intrusive igneous rocks form when magma cools slowly beneath the Earth's surface, resulting in larger mineral grains. Examples include granite and diorite. Extrusive igneous rocks form when lava cools quickly on the Earth's surface, resulting in smaller mineral grains. Examples include basalt and pumice.
The description oof it is big grains and there are visual and you can touch them always remember that it is intrusive igneous rock not extrusive rock igneous rock. and the color of it is GRAY!!!! Thankz for asking the questions ask more
No pumice is not a porphyritic igneous rock, a porphyritic rock is characterized by the presence of phenocrysts (large mineral grains) and very small mineral grains with none in between. This implies that there was two different stages of cooling. Pumice is an extrusive igneous rock that cooled very quickly.
Intrusive or extrusive describe properties of an igneous rock. An intrusive rock is formed within the crust and it insulated and cooled slowly. Some examples of an intrusive rock include diorite, granite, gabbro, and periodite. They have large grains because they have more time for growth. On the other hand, extrusive rocks cool at the surface rapidly. They are comprised of tiny crystals and/or glass. Some examples include rhyolite, andesite, and basalt.
Intrusive igneous rocks are created when magma pushes up into the Earth's crust and cools there. Although the decrease in pressure the magma experiences as it rises in the crust allows it to solidify, this is still a fairly slow process, so intrusive igneous rocks tend to have larger grains than extrusive igneous rocks. Granite and Gabbro are both intrusive igneous rocks.