Vesicles.
Obsidian rocks are cooled very fast, and you cannot see the crystals in them.
Rapid cooling of lava in which tiny crystals form results in a glassy texture.
extrusive rocks cools faster because it is in open air or under the sea
A vesicular igneous texture generally indicates rapid cooling.
Glassy igneous rocks cool the fastest. The most likely had more nucleation. Pegmatic cooled the slowest, which is why its crystals are larger than 1 cm. Phaneritic is the next slowest in cooling. Porphyritic has slow then rapid cooling, while aphanitic igneous rocks also have rapid cooling.
Vesicles.
The rock is said to be extrusive or possess an aphanitic texture, as a result of relatively rapid cooling.
Fine-grained
Yes. In that basalt is formed from rapid cooling of lava at or near the surface.
Obsidian is an example of a rapidly cooled rock, also known as volcanic glass.
rapid cooling
no . they come from rapid cooling lava
A phenomenon of supercooling is possible.
Pumice is simply a frothy, gas entrained volcanic glass, a result of the extremely rapid cooling of felsic lava after eruption.
Obsidian rocks are cooled very fast, and you cannot see the crystals in them.
Basalt is formed from relatively rapid cooling magma.
Overheating, and rapid cooling.