Granite
how the grains interlock and the pressure it formed under
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.
No. Obsidian is formed by the very rapid cooling of lava which means that crystals do not have time to form.
in a delta from sand grains deposited, buried, and cemented together by minerals.
rocks are formed from grains and grains are small and the rocks are big. Sedimentary rocks are formed when grains or sediments are compacted together.
how the grains interlock and the pressure it formed under
The slower a mineral cools, the larger the crystals it forms. Rapid cooling produces fine grained rocks / minerals, while slow cooling produces large grained rocks / minerals. In the case of igneous rocks, for example, you can tell whether it was formed inside the earth and underwent slow cooling (like granite) or was formed during extrusion from the earth, (such as during a volcanic eruption), which would expose it to water or air, cooling it rapidly. If it has large, chunky crystals, in is an intrusive rock, formed inside the earth, and cooled very slowly. If it is very fine grained or has no grains, (such as obsidian), it is an extrusive rock.
Their texture could be formed from slow-cooling magma, from mineral precipitation and crystallization in pockets or fractures, or from recrystallization during metamorphism.
Quartz and mica. Clay minerals come from decomposing feldspars.
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.
No. Obsidian is formed by the very rapid cooling of lava which means that crystals do not have time to form.
in a delta from sand grains deposited, buried, and cemented together by minerals.
A vesicular igneous texture generally indicates rapid cooling.
rocks are formed from grains and grains are small and the rocks are big. Sedimentary rocks are formed when grains or sediments are compacted together.
yes it does
A rock formed from grains stuck together would be Porous
No. It is vesicular glass, like pumice.