Their texture could be formed from slow-cooling magma, from mineral precipitation and crystallization in pockets or fractures, or from recrystallization during metamorphism.
They have mineral grains of nearly equal size, and have large crystals because they were cooled slowly.
No. They are usually fine grained.No, lava rocks do not have large grains they have very small grains.
Fine grains of rocks are referred to as "clasts." The word "clast" comes from the Greek word "klastos," meaning "broken."
according to composition i.e. mineral grains, fossils, animal/plant matter, chemical composition etc. and grain size (gravel, sand, silt, clay) for example sandstone is made up of mainly rock fragments or mineral grains (quartz, feldspar, clay) weathered form other rocks and has grains that are 1/16-2mm large.
granite
Metamorphic rocks that consist of only one mineral and have large interlocking crystals often have a coarse-grained texture. This means that the individual mineral grains are easily visible to the naked eye. Examples of such rocks include quartzite (formed from quartz) and marble (formed from calcite).
They have mineral grains of nearly equal size, and have large crystals because they were cooled slowly.
No. They are usually fine grained.No, lava rocks do not have large grains they have very small grains.
Fine grains of rocks are referred to as "clasts." The word "clast" comes from the Greek word "klastos," meaning "broken."
No. Obsidian is formed by the very rapid cooling of lava which means that crystals do not have time to form.
large grains
Intrusive
They are rocks formed from lava at or near the surface. Basalt is a typical fine-grained extrusive igneous rock, composed of mineral crystals that require magnification to see. The fine-grained texture is due to rapid solidification of the lava which leaves little time for large mineral crystal formation.
according to composition i.e. mineral grains, fossils, animal/plant matter, chemical composition etc. and grain size (gravel, sand, silt, clay) for example sandstone is made up of mainly rock fragments or mineral grains (quartz, feldspar, clay) weathered form other rocks and has grains that are 1/16-2mm large.
according to composition i.e. mineral grains, fossils, animal/plant matter, chemical composition etc. and grain size (gravel, sand, silt, clay) for example sandstone is made up of mainly rock fragments or mineral grains (quartz, feldspar, clay) weathered form other rocks and has grains that are 1/16-2mm large.
There are three types of rocks--igneous, metamorphic, and sedimentary.Igneous rocks form from cooled magma(melted rock underneath Earth's surface). An igneous rock is intrusive if it formed underneath Earth's surface; they usually have large mineral grains, or crystals. An igneous rock is extrusive if it formed near Earth's surface; the lava(what magma's called when it's reached the surface) cooled so quickly that there was no time for mineral grains to grow. They have fine grained texture.Metamorphic rocks are formed underground by heat and pressure. A metamorphic rock is foliated if it has bands(layers). It is nonfoliated if it has no bands. Metamorphic rocks can be formed from any other type of rock.Sedimentary rocks are formed from sediments, which is why they're called sedimentary rocks. Sediments are loose materials like pieces of rock, mineral grains, and dead plants and animals. These sediments have been compressed and cemented to form a rock. Sedimentary rocks can also form when minerals are dissolved in liquid and when the liquid evaporates, rocks are left behind.Rock Cycle: Igneous, metamorphic, and sedimentary rocks can be changed from one type of rock to another through a process called the rock cycle. The sediments in sedimentary rocks can actually be broken parts of other rocks, like igneous and metamorphic. All the rocks are connected.
granite