Pumice is a disordered material, a result of quick freezing of a boiling glass, and is irregular in all directions. It has no preferred cleavage direction, and indeed is not classed as a mineral, for it lacks both a single chemical form, and a defined crystal arrangement.
The pumice with which I'm most familiar is white to light yellow, but depending on the source material, it will be darker as the magma component is increased. Scoria is a more magma-rich form, and is denser than the white variety.
cleavage....
In general, pumice will float. There is enough trapped air in pumice that it is buoyant.
Dolomite typically exhibits three cleavage planes that intersect at approximately 90 degrees, resulting in rhombohedral cleavage.
Floating rocks: pumice. Non-floating rocks: all but pumice. Pumice can float on water because its density is so low, due to trapped bubbles of air which formed during its solidification from lava.
It has both. It's cleavage is perfect, and it's fracture is sub-conchoidal.
The fracture type of the Pumice rock is either jagged or splintery. The Pumice has both fracture and cleavage type.
Pumice can be white, gray, or even pink.
how did pumice get here
No. Pumice is inorganic.
Sulfur's cleavage is imperfect.
No. Pumice does not have grains.
Pumice.
Yes. Pumice is defined as being highly vesicular.
Pumice is found after volcanic eruptions producing lava.
yes pumice is an igneous rock.
No, pumice has nothing to do with drywall.
cleavage....