Geodes
another name for the mineral crystals in cooling magma or lava
Yes. When magma cools and solidifies, mineral crystals are formed.
Yes. When magma cools and solidifies, mineral crystals are formed.
Yes. When magma cools and solidifies, mineral crystals are formed.
Cooling and soildification of magma.
Yes. Slow cooling magma produces larger mineral crystals.
The major factor is the amount of time the magma remains mostly liquid while cooling and solidifying. More time spent cooling produces larger crystals because of the free movement of a mineral's constituent isotopes in a somewhat liquid magma.
The rate of cooling of the magma determines the type of mineral formed by the magma or lava..
Large mineral crystals that are all about the same size are formed from magma that cooled slowly inside the earth. Small mineral crystals (not identifiable without a microscope) formed from magma that cooled rapidly, on or near the surface of the earth.
A rich assemblage of silicate-based minerals forming the igneous rocks that are solidified from magma. The faster the cooling the finer the crystals but the minerals are the same for a specific eruption or intrusion irrespective of cooling rate.
When igneous rocks cool quickly, they have small crystals and have a texture that may be described as aphanitic. When igneous rocks cool slowly, they have much larger crystals and have a texture that may be described as phaneritic or pegmatitic.
large crystals