they form from both...ithink
Igneous rocks with a large grain size, such as granite, form from the slow cooling of magma beneath the Earth's surface. As the molten rock cools over extended periods, crystals have the time to grow larger, resulting in the coarser texture characteristic of these rocks. This process often occurs in intrusive igneous formations, where the surrounding rock insulates the magma, allowing for gradual solidification. In contrast, rapid cooling of magma at the surface leads to finer-grained volcanic rocks.
Igneous rocks with large crystals are known as intrusive or plutonic rocks. These rocks form underground as magma cools slowly, allowing large crystals to grow. Common examples include granite and diorite.
Igneous rocks, such as granite or diorite, are formed when large masses of magma solidify far below Earth's surface. These rocks have a coarse texture due to the slow cooling process, allowing large mineral crystals to form.
Coalesced magma bodies are referred to as plutonic rocks, they have a porphyritic texture or larger crystals since elements are allotted more time to segregate to their desired energy environments and precipitate minerals.
No, while all rocks on Earth were molten at one point, most rock types do not form from magma. Rocks that form from magma or lava are igneous rocks. Most of the rocks at Earth's surface are sedimentary. These rocks form from the remains of rock that have been broken own into tiny pieces or dissolved in water. These components eventually settle, usually in a body of water, and are buried and turned to stone. Metamorphic rocks make up a third category. These form from rocks that have been altered under enormous heat and pressure while remaining solid.
Igneous rocks.
Intrusive rocks are igneous rocks that form when magma solidifies below the Earth's surface. They usually form by rather slow cooling, which allows time for large crystals to grow, and these large crystals tend to give them a coarse grain. Extrusive rocks are igneous rocks that form when magma solidifies above the Earth's surface. They usually form by comparatively rapid cooling, which does not allow time for large crystals to form, so they are often fine-grained or amorphous.
Igneous rocks with a large grain size, such as granite, form from the slow cooling of magma beneath the Earth's surface. As the molten rock cools over extended periods, crystals have the time to grow larger, resulting in the coarser texture characteristic of these rocks. This process often occurs in intrusive igneous formations, where the surrounding rock insulates the magma, allowing for gradual solidification. In contrast, rapid cooling of magma at the surface leads to finer-grained volcanic rocks.
another name for the mineral crystals in cooling magma or lava
igneous rocks
Igneous rocks form as a result of cooling magma. As the magma cools and solidifies, it forms rocks such as granite, basalt, and obsidian. The size of the mineral crystals in the rock is determined by the rate of cooling.
They form underground from the cooling and solidification of magma.
Igneous rocks form because, magma cools under the ground, or magma erupts, then cools on the ground forming these rocks.
igneous rocks are formed through the cooling and solidification of magma.
Igneous
Igneous rocks with large crystals are known as intrusive or plutonic rocks. These rocks form underground as magma cools slowly, allowing large crystals to grow. Common examples include granite and diorite.
Rocks that form when hot magma solidifies are igneous rocks.