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Pumice
is a type of lava rock that's full of bubble holes. The
bubbles formed as the lava was blasted out of a volcano, and were trapped
as the lava cooled and hardened.
To learn more about pumice, scroll farther down this page. |
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| How to recognize pumice | |
| Other rocks that look like pumice | |
| Special things to look for | |
| Where pimice came from | |
| How pumice formed | |
| Other names for pumice | |
| Links to Websites about pumice |
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Scoria:
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Some
pumice floats!
Actually, almost all fresh, gray pumice floats. But our reddish brown pumice has been exposed to the weather for so long that it has started to turn into clay. Because clay plugs many of the bubble holes, some of our pumice doesn't float anymore. |
There are no volcanoes in Chicago, so the pumice
we find in our area had to come from somewhere else.
Somebody must have shipped it here by truck or train.
However, so far we haven't found out where it came from.
Pumice was a bubble-filled lava that exploded out
of a volcano. It then cooled and hardened quickly
that the bubbles could not escape.
In fact, pumice cooled so quickly that crystals
couldn't form -- the most of the rock between the
bubble-holes is volcanic glass. Volcanic glass
without bubble holes is called obsidian.
We use the scientific name "pumice" for this
rock,
but it is also known by other names:
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Here are some ways to classify pumice (by
grouping it with similar types of rocks):
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At the
Children's Museum of Indianapolis Web site, you can help
solve the "Mystery of the Floating Rock." Go to:
< http://www.childrensmuseum.org/geomysteries/floatingrock/a1.html
>
Here's a Franklin Institute Web page about pumice:
< http://www.fi.edu/fellows/payton/rocks/expert/pumice.htm
>
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Copyright 2001-2002 Eric D. Gyllenhaal
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This page was created on May 2, 2001, and it was last updated on July 27, 2002.