Obsidian - volcanic glass - is one type of rock that would fit that description. It is glassy (grainless) and frequently has pockets of trapped air bubbles in it.
A rock with little to no grain development and a vesicular texture is typically called a vesicular rock. It is formed from a volcanic eruption, where gases trapped in the lava create bubbles or vesicles. The most common example is vesicular basalt.
Pumice is so fine grained, it actually doesn't have a grain--because it is a natural volcanic glass. The rough texture is caused by the vesicular nature of the rock--trapped pockets of gas bubbles with sharp glassy edges.
Grain shape.
Pure obsidian actually has a glassy texture (grain), with no discernible crystalline structure.
texture
texture
fined grain texture
Granite has a heterogeneous grain pattern or texture.
Fine grain, rough and soft
Grain
Grain
Grain
Pumice is so fine grained, it actually doesn't have a grain--because it is a natural volcanic glass. The rough texture is caused by the vesicular nature of the rock--trapped pockets of gas bubbles with sharp glassy edges.
It doesn't. The grain size effects the texture. If a rock has a small grain size, it will have a smooth texture. If the grain size is large, such as pebbles, the texture will be rough. For example, siltstone is one of the smoothest rocks because it contains silt particles, which are .0004cm to .006cm. Conglomerate though contains various particles including cobbles and boulders, which are from 10cm to 100cm.
Grain shape.
Pure obsidian actually has a glassy texture (grain), with no discernible crystalline structure.
Grain size and arrangement.
no