Grain size depends upon the cooling rate as written below:
1.
longer the time it takes to cool,
larger will be the grain size
and vice versa
The cooling rate of magma primarily controls the grain size of igneous rock. Faster cooling results in smaller grains, while slower cooling leads to larger grains. Other factors that can influence grain size include the composition of the magma and the amount of gas or water present during solidification.
It depends on if it is intrusive or extrusive. If it is an intrusive rock, it is formed when magma hardens under the earth and has a larger grain size. If it is an extrusive rock, it is formed when lava hardens on the earth's surface and has a smaller grain size.
A fast cooling rate typically results in fine-grained texture in igneous rocks. This is because the minerals have less time to grow and crystallize, leading to smaller grains. Conversely, a slow cooling rate allows for more growth and results in larger grains.
that means like when somthing is in a own properties
The size of a mineral's crystals depends on factors such as the rate of cooling, the presence of impurities, and the availability of space to grow. Slower cooling rates typically result in larger crystals, while faster cooling rates produce smaller crystals. Impurities can impede crystal growth, while a lack of space can limit crystal size.
The rate of cooling of the magma primarily determines the mineral grain size in an igneous rock. Rapid cooling results in fine-grained rocks, while slow cooling allows for the formation of coarse-grained rocks. Additionally, the composition of the magma and the presence of nucleation sites can also influence the final grain size.
The cooling rate of magma primarily controls the grain size of igneous rock. Faster cooling results in smaller grains, while slower cooling leads to larger grains. Other factors that can influence grain size include the composition of the magma and the amount of gas or water present during solidification.
It depends on if it is intrusive or extrusive. If it is an intrusive rock, it is formed when magma hardens under the earth and has a larger grain size. If it is an extrusive rock, it is formed when lava hardens on the earth's surface and has a smaller grain size.
Crystal size in igneous rocks is controlled by the rate of cooling whereby the slower the rate, the larger the size of crystal.
A fast cooling rate typically results in fine-grained texture in igneous rocks. This is because the minerals have less time to grow and crystallize, leading to smaller grains. Conversely, a slow cooling rate allows for more growth and results in larger grains.
that means like when somthing is in a own properties
Porphyritic texture indicates that a magma has gone through a two stage cooling process. The magma has cooled sufficiently underground to allow some minerals to crystallize and grow in size; the magma is then expelled above ground where the remaining liquid magma solidifies quickly, allowing only small crystals to develop.
Primarily the cooling rate of the mineral compound.The faster the rate cooling smaller the crystal size of the mineral.Consequently, large crystal specimins are derived from igneous bodies with a very slow rate of cooling.
The dimensions grains in metals are modified by heating or cooling.
The size of a mineral's crystals depends on factors such as the rate of cooling, the presence of impurities, and the availability of space to grow. Slower cooling rates typically result in larger crystals, while faster cooling rates produce smaller crystals. Impurities can impede crystal growth, while a lack of space can limit crystal size.
The grain size of basalt varies depending on how quickly the lava cooled and solidified. Typically, basalt has a fine to medium grain size, with individual grains being less than 1 mm in size. Rapid cooling can result in a fine-grained basalt, while slower cooling may produce a coarser-grained texture.
It doesn't. The grain size effects the texture. If a rock has a small grain size, it will have a smooth texture. If the grain size is large, such as pebbles, the texture will be rough. For example, siltstone is one of the smoothest rocks because it contains silt particles, which are .0004cm to .006cm. Conglomerate though contains various particles including cobbles and boulders, which are from 10cm to 100cm.