pumice
Pumice meets those requirements.
Fast cooling lava can trap air bubbles, creating a bubbly or vesicular texture.
Vesicular rocks contain lots of small cavities, usually filled with air. Non- vesicular ones don't have these holes. Vesicles are formed when magma suddenly rushes out on to the surface and its dissolved gases come out of solution, blowing bubbles in the liquid rock which are preserved as it cools quickly and sets. An example of a vesicular rock is pumice.
The bubbles and pores are from trapped gasses which expanded in the molten material as it neared the surface. They're usually found in extrusive igneous rocks, those that have solidified in the air or on the surface.
Scoria and pumice are vesicular igneous rocks.
Pumice meets those requirements.
The common usage of "lava rock" in the USA refers to a black rock with a number of visible bubbles or air pockets that is formed from cooled lava on the surface. Although lava rock is an igneous rock, it is not the same as the definition for the word igneous, which can also include igneous rocks which have solidified from magma below the surface.
Pumice has tiny air pockets to help it float in water.
pumiceThe type of igneous rock that floats is called Pumice. It isn't lighter than other rocks, just less dense because it has lots of very small air bubbles trapped in it. You can see these if you look at the exterior of the rock.
Fast cooling lava can trap air bubbles, creating a bubbly or vesicular texture.
it is an extrusive rock
Any type of Igneous rock.
That is a type of rock called pumice.
extrusive igneous rock
Pumice is similar to scoria in appearance and formed from very rapidly cooled lava, entrapping expanding gas in the form of air pockets and ruptured bubbles, giving it a vesicular texture.
Vesicular pumice is an extrusive igneous rock that consists of a foam of mineral matter (usually silica-rich and glassy) enclosing bubbles of gas (usually carbon dioxide). The mineral material itself is denser that water, but the bubbles make the rock overall less dense than water, and it will float. Pieces of pumice may often be found washed up on beaches. Pumice is formed when magma of intermediate or felsic composition having a large proportion of dissolved gasses is simultaneously rapidly de-pressurised and rapidly cooled. The gasses exsolve like bubbles in warm and shaken soda-pop, and the mineral matter solidifies before the foam can collapse.
One of the most common events that causes the rapid cooling of an igneous rock is its collision with a water-based object. This is included but not limited to bodies of water, icebergs, and snow. The rapid cooling causes air bubbles to be trapped within the rapidly hardening rock, thus resulting in a far less dense geological structure. Certain types of igneous rock, such as pumice, have so much air trapped it that it is less dense than water, enabling it to float.