As magma cools slowly, large coarse crystals form. This is described as a phaneritic texture.
Coarse crystal grain.
pegmatitic
Coarse
Large mineral crystals can form when magma is able to cool slowly underground, creating intrusive igneous rock.
The size of the crystal relates to how long the crystals were forming. For example crystals that cooled slowly are larger than those cooling faster.
I think like granite, amethysts are formed from magma deep underground. This helps them to cool slowly forming the large crystals they have.
pegmatitic
Large crystals with a coarse crystal grain texture.
Coarse
The texture of the rock product of slow cooling magma is referred to as coarse grained.
crystal
Large mineral crystals can form when magma is able to cool slowly underground, creating intrusive igneous rock.
It is mineral
If the crystal grows quickly then it is going to be the quicker one to grow, and thus larger, though not always the most valuable since underground crystals can take millions of years to come to be.
rock because when the lava or magma cools slowly it starts to harden.
If the grains of the rock are larger, then it either is an intrusive igneous rock,( a rock formed from molten rock that cooled slowly over long periods of time underground) or a sedimentary rock that was formed from large sediments.
Cooled slowly underground the pseudo crystals of columnar basalt, such as the Giants Causeway in Ireland may be in a metre size range.
The three main categories of igneous rock texture are aphanitic, phaneritic, and porphyritic. Aphanitic texture is described as a crystalline igneous structure that is too small to be seen with the naked eye. This texture indicates that the rock was cooled at or near the surface, quickly, with little time for crystal growth. Phaneritic texture is described as a rock with a visible crystalline structure, indicating that the rock was cooled slowly from magma underground, allowing ample time for crystal growth. Porphyritic texture is the presence of larger, visible phenocrysts suspended in a larger aphanitic matrix. This indicates a two-stage cooling process, where some minerals developed slowly underground in magma which was then erupted on the surface, causing the remaining minerals to form quickly.