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The rate at which the rock cool from the liquid magma determines their texture
A vesicular igneous texture generally indicates rapid cooling.
It is likely to have a coarse-grained texture.
The texture would be glass-like.
The Igneous rock formed when magma cools are; 1. Extrusive (Volcanic) Igneous Rock; which are igneous rocks formed when magma cools outside the earths crust. The texture of of extrusive igneous rock is fine grained. 2. Intrusive (Plutonic) Igneous Rock; these are igneous rocks formed by gradual cooling of magma within the earths crust. The texture is coarse grained.
Intrusive igneous rock has a coarse, visible crystalline texture. Intrusive igneous rocks are formed from slow cooling of magma. The additional time spent in a liquid state allows for the creation of larger mineral crystals. An igneous rock with a coarse texture is said to be phaneritic.
Igneous rock is formed through the cooling and solidification of magma or lava.
Igneous rocks are formed by cooling magma.
Its a igneous rock whenit is made formed by magma.
igneous rock is formed by heating and cooling.
Rock and igneous plants
Igneous rocks are formed as the result of cooling magmas.