Gneiss, pronounced 'nice', is a coarse grained banded metamorphic rock.
Limestone can be both coarse-grained and fine-grained, depending on its composition and how it formed. Coarse-grained limestone typically contains larger mineral grains visible to the naked eye, while fine-grained limestone has smaller mineral grains that are not easily seen without magnification.
Metamorphic rock can vary in texture, with some being rough due to the presence of mineral grains and others being smooth due to recrystallization of minerals during the metamorphic process. The texture of metamorphic rock depends on factors such as the original rock type and the intensity of heat and pressure.
Granite is a coarse-grained igneous rock, meaning it is made up of large interlocking crystals. These crystals form as the magma cools slowly beneath the Earth's surface, allowing for the growth of larger grains rather than small ones.
Methods of formation. If crystalline (igneous or metamorphic) they would most likely have had differing rates of cooling. If sedimentary, they would most likely have had differing depositional environments (higher energy for larger grain sizes).
Breccia is a coarse-grained sedimentary rock that is composed of large, angular fragments.
Please.
Yes. Exactly, they do have both, fine grained and coarse grained rocks.
Metamorphic rock can be coarse grained or fine grained.
coarse grained
Slate typically does not have abundant coarse-grained mica in it. Mica is more commonly found in other metamorphic rocks such as schist and gneiss. Slate is formed from the low-grade metamorphism of shale or mudstone, resulting in a fine-grained, foliated rock without abundant coarse-grained minerals like mica.
If the rocks are igneous then in general:- Coarse = slowly. Fine = fast. However if the rocks are metamorphic or sedimentary then grain size has nothing to do with cooling and indicates other things.
Limestone can be both coarse-grained and fine-grained, depending on its composition and how it formed. Coarse-grained limestone typically contains larger mineral grains visible to the naked eye, while fine-grained limestone has smaller mineral grains that are not easily seen without magnification.
Fine grained has larger crystals and coarse grained has smaller crystals
Fine grained has larger crystals and coarse grained has smaller crystals
It is coarse-grained.
Metamorphic rock can vary in texture, with some being rough due to the presence of mineral grains and others being smooth due to recrystallization of minerals during the metamorphic process. The texture of metamorphic rock depends on factors such as the original rock type and the intensity of heat and pressure.
A peridotite is a dense, coarse-grained igneous rock