Corrosion residue (Inventory)
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| - | '''Corrosion residues''' are relatively insoluable minerals which were once part of the bedrock. They were left behind and concentrated when the bedrock was dissolved. On the ''CCNP Cave Inventory Form'', the [[Recorder (Inventory)|recorder]] is asked only to distinguish them by color. There are three color categories on the form: red, brown and yellow. They can usually be found on the floor as fluffy, colored soils (speleosols) but could appear in cracks or [[Glossary (Inventory)#Vug|vug]]s or on shelves and ledges. They could even appear as a type of crust or coating. Several colors could be present at a single location. Many caves in the Guadalupes have exceptional examples of corrosion residue. | + | '''Corrosion residues''' are relatively insoluable minerals which were once part of the bedrock. They were left behind and concentrated when the bedrock was dissolved. They are the waste products form bacterial processes which utilize manganese and iron in the rock for energy. |
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| + | On the ''CCNP Cave Inventory Form'', the [[Recorder (Inventory)|recorder]] is asked only to distinguish them by color. There are three color categories on the form: red, brown and yellow. They can usually be found on the floor as fluffy, colored soils (speleosols) but could appear in cracks or [[Glossary (Inventory)#Vug|vug]]s or on shelves and ledges. They could even appear as a type of crust or coating. Several colors could be present at a single location. Many caves in the Guadalupes have exceptional examples of corrosion residue. | ||
The ''CCNP Cave Inventory Form'' asks the recorder to include the thickness if possible. An estimate of how thick the accumulation is should be included next to the station. | The ''CCNP Cave Inventory Form'' asks the recorder to include the thickness if possible. An estimate of how thick the accumulation is should be included next to the station. | ||
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==References== | ==References== | ||
*Palmer, Arthur N. (2007) ''Cave Geology'' CAVE BOOKS, Dayton, OH pp 337-338 ISBN-13: [[Special:Booksources/978-0-939748-66-2|978-0-939748-66-2]], ISBN-10: [[Special:Booksources/0-939748-66-5|0-939748-66-5]] | *Palmer, Arthur N. (2007) ''Cave Geology'' CAVE BOOKS, Dayton, OH pp 337-338 ISBN-13: [[Special:Booksources/978-0-939748-66-2|978-0-939748-66-2]], ISBN-10: [[Special:Booksources/0-939748-66-5|0-939748-66-5]] | ||
| + | *Various (June 2004) ''Core Values'' Carlsbad Caverns National Park; as published by Bob Hoff: [http://carlsbadcavernshistory.blogspot.com/2011/05/carlsbad-caverns-national-park-core.html] | ||
{{Cave inventory}} | {{Cave inventory}} | ||
Revision as of 00:24, 26 May 2011
Corrosion residues are relatively insoluable minerals which were once part of the bedrock. They were left behind and concentrated when the bedrock was dissolved. They are the waste products form bacterial processes which utilize manganese and iron in the rock for energy.
On the CCNP Cave Inventory Form, the recorder is asked only to distinguish them by color. There are three color categories on the form: red, brown and yellow. They can usually be found on the floor as fluffy, colored soils (speleosols) but could appear in cracks or vugs or on shelves and ledges. They could even appear as a type of crust or coating. Several colors could be present at a single location. Many caves in the Guadalupes have exceptional examples of corrosion residue.
The CCNP Cave Inventory Form asks the recorder to include the thickness if possible. An estimate of how thick the accumulation is should be included next to the station.
Contents |
Fields
Example
Corrosion Residue
- Red CR: GG39 (thin film)
- Brown CR: GG40 (4 inches)
- Yellow CR: GG37 (3 cm), 38 (2.5 cm)
See also
References
- Palmer, Arthur N. (2007) Cave Geology CAVE BOOKS, Dayton, OH pp 337-338 ISBN-13: 978-0-939748-66-2, ISBN-10: 0-939748-66-5
- Various (June 2004) Core Values Carlsbad Caverns National Park; as published by Bob Hoff: [1]
