| Revision as of 13:29, 19 January 2005 editMellum (talk | contribs)Extended confirmed users819 editsm add wikilink← Previous edit | Revision as of 04:30, 21 January 2005 edit undoVsmith (talk | contribs)Administrators271,499 editsm shift 2nd image down a bitNext edit → | ||
| Line 1: | Line 1: | ||
| ], below that is pumice and in lower right hand color is ] (light color).]] | ], below that is pumice and in lower right hand color is ] (light color).]] | ||
| '''Pumice''' is a light, porous type of ] ]. It is formed during explosive ] eruptions when liquid ] is ejected into the air as a froth containing masses of gas bubbles. As the lava solidifies, the bubbles are frozen into the rock. Any type of igneous rock — ], ], ] or ] — can form pumice given suitable eruptive conditions. When larger amounts of gas are present, the result is a finer-grained variety of pumice known as '''pumicite'''. | '''Pumice''' is a light, porous type of ] ]. It is formed during explosive ] eruptions when liquid ] is ejected into the air as a froth containing masses of gas bubbles. As the lava solidifies, the bubbles are frozen into the rock. Any type of igneous rock — ], ], ] or ] — can form pumice given suitable eruptive conditions. When larger amounts of gas are present, the result is a finer-grained variety of pumice known as '''pumicite'''. | ||
| ⚫ | It is considered a ] because it has no crystal structure. Pumice varies in density according to the thickness of the solid material between the bubbles; many samples float in ]. It is widely used to make lightweight ] and as an ], especially in polishes and ] exfoliants. | ||
| <div style="float:left;margin-right:0.5em;text-align:center"> | <div style="float:left;margin-right:0.5em;text-align:center"> | ||
| ]<br> | ]<br> | ||
| <small>''Specimen of highly porous pumice from ] volcano <br>on ], ]. Density of specimen <br>approx 0.25 ]/]. Scale in ]s.''</small></div> | <small>''Specimen of highly porous pumice from ] volcano <br>on ], ]. Density of specimen <br>approx 0.25 ]/]. Scale in ]s.''</small></div> | ||
| ⚫ | It is considered a ] because it has no crystal structure. Pumice varies in density according to the thickness of the solid material between the bubbles; many samples float in ]. It is widely used to make lightweight ] and as an ], especially in polishes and ] exfoliants. | ||
| When used as an additive for ], fine-grained version of pumice called ] is mixed with ] to form a light-weight, smooth, plaster-like ]. This form of concrete was used as far back as ] times. | When used as an additive for ], fine-grained version of pumice called ] is mixed with ] to form a light-weight, smooth, plaster-like ]. This form of concrete was used as far back as ] times. | ||
Revision as of 04:30, 21 January 2005
Pumice is a light, porous type of pyroclastic igneous rock. It is formed during explosive volcanic eruptions when liquid lava is ejected into the air as a froth containing masses of gas bubbles. As the lava solidifies, the bubbles are frozen into the rock. Any type of igneous rock — andesite, basalt, dacite or rhyolite — can form pumice given suitable eruptive conditions. When larger amounts of gas are present, the result is a finer-grained variety of pumice known as pumicite.
It is considered a glass because it has no crystal structure. Pumice varies in density according to the thickness of the solid material between the bubbles; many samples float in water. It is widely used to make lightweight concrete and as an abrasive, especially in polishes and cosmetic exfoliants.
on Tenerife, Canary Islands. Density of specimen
approx 0.25 g/cm³. Scale in centimetres.
When used as an additive for cement, fine-grained version of pumice called pozzolan is mixed with lime to form a light-weight, smooth, plaster-like concrete. This form of concrete was used as far back as Roman times.
Categories: