When a magma cools/solidifies, crystals are formed. The quicker the magma cools, the tinier the crystals. A granite for example, which is formed through slow cooling in the Earth's crust, consists out of big crystals. Contrary, magma erupting at the surface (which is then called lava) cools rapidly and consists out of tiny crystals. In extreme cases, the lava cools so rapidly that the resulting rock appears glassy. Hope this helps!
yes
No. Small crystals form.
Yes, obsidian rock cools quickly. It is formed from lava that cools rapidly upon exposure to air or water, preventing the formation of crystal structures. This rapid cooling results in its glassy texture and characteristic smooth surface. As a result, obsidian is considered an extrusive igneous rock.
Obsidian is formed from volcanic lava that cools quickly with minimal crystal growth. It is primarily derived from rhyolitic magma that cools rapidly on the Earth's surface, leading to the formation of a glassy rock without distinct mineral crystals.
When a volcano erupts the molten cools quickly it is also known as volcano glass
crystal
Fine crystal grain.
Fine
fine
yes
Small crystal grains form when molten rock cools quickly. In an extrusive igneous rock, it's referred to as aphanitic texture.
"Larger than if it cools quickly" is about all that's definitively possible to say.
No. Small crystals form.
It is mineral
When molten rock cools quickly, fine-grained crystals form. This happens because there is not enough time for larger crystals to grow before the rock solidifies, resulting in smaller crystals being formed.
Large crystals with a coarse crystal grain texture.
Pumice.