When lava cools very suddenly (a process known as quenching), it creates a glassy, or hyaline, texture. This sudden cooling also creates very small, often microscopic, crystals in the rock. The most well-known example of a glassy textured igneous rock is obsidian.
It is likely to have a coarse-grained texture.
The texture would be glass-like.
A vesicular igneous texture generally indicates rapid cooling.
The rate at which the rock cool from the liquid magma determines their texture
Rock and igneous plants
It is likely to have a coarse-grained texture.
The texture would be glass-like.
A vesicular igneous texture generally indicates rapid cooling.
The rate at which the rock cool from the liquid magma determines their texture
yes because of the fast cooling rate
Rock and igneous plants
The texture of the rock product of slow cooling magma is referred to as coarse grained.
The rock formed by cooling a liquid rock after processing is called a crystal.
Its a igneous rock whenit is made formed by magma.
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.
The resultant rock would have a porphyritic texture; large crystals (usually feldspars) scattered among small crystal grains.
The texture is mostly determined by the time spent in cooling from magma or lava. The quicker the transition from molten to solid, the finer the texture.