Pumice is a low density rock formed during volcanic eruptions when expanding gas within the magma becomes trapped as the rock solidifies. This forms the honeycomb/ aerated texture. Pumis is know to float on the surface around volcanic erruptions close to water.
gas
gases
Fast cooling lava can trap air bubbles, creating a bubbly or vesicular texture.
Pumice
Pumice is full of holes called vesicles formed from gasses escaping the molten rock. The holes greatly reduce its density.
Pumice and scoria are volcanic rock. They form form the lava the erupts from the volcano and contains bubbles from gasses. These bubbles cause the cavities you're calling air holes.
Pumice is a volcanic rock that forms when a volcano ejects "foamy" lava. The gas bubbles remain in place after the rock solidifies. One of Pumice's most notable characteristics is that it will float in water.
pumice
It is a glassy igneous rock, so there are holes in it. The holes make the rock less dense than other igneous rocks that are Not glassy.
I'd say pumice is the closest to your description.
* Vesicular rock texture is generally displayed in extrusive igneous rocks which contain many vesicles of trapped air, such as pumice or scoria. * Igneous rocks containing holes which were produced as gases escaped from the upper part of lava flow.
* Vesicular rock texture is generally displayed in extrusive igneous rocks which contain many vesicles of trapped air, such as pumice or scoria. * Igneous rocks containing holes which were produced as gases escaped from the upper part of lava flow.
Pumice is such a rock.
The rock comes from a volcano and is known as pumice.
Igneous rocks form when lava or magma cools.But when cooling there are air bubbles that are trapped in the lava.Prime examples of this event are found in pumice and scoria
The air and gases escape from the lava as it cools. This makes the little holes that you see. The rock is called pumice.
Vesicular solidified lava, an extrusive igneous rock.
That is a type of rock called pumice.
Pumice is a form of volcanic glass that is rich in silica. There are also fairly high amounts of aluminum oxide, sodium oxide, and potassium oxide. The holes or vesicles are the remnants of gas bubbles that formed when the pumice was still molten.