perlite uses
Perlite is formed during volcanic occurrences being the result of the hydration
of rhyolitic obsidian, a rock resulting of a sudden chilling (cool down) of molten lava.
This expansion is due to 2 to 6% combined water in the crude Perlite rock. When quickly heated to above 1600°F (871°C), the crude rock pops in a manner similar to popcorn, as the combined water vaporizes which accounts for the amazing lightweight and other exceptional physical properties of expanded Perlite.
Perlite is a generic term for naturally occurring silicious rock, not a trade name.
The distinguishing feature that sets Perlite aside from the other volcanic glasses is that when heated to a suitable point in its softening range, it expands from 4 to 20 times its original volume.
Pennsylvania Perlite is a Perlite Institue Member as well as OMRI Certified.
Click these links for more information on Perlite
www.perlite.org | www.omri.org.