Calcite (Inventory)/Spar/nailhead
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| - | + | {{Inventory image|File:Nailhead.JPG|Nailhead spar}} | |
The '''nailhead''' field should be used to list stations which exhibit nailhead [[Calcite (Inventory)/Spar|spar]]. | The '''nailhead''' field should be used to list stations which exhibit nailhead [[Calcite (Inventory)/Spar|spar]]. | ||
| - | Nailhead spar typically is "flatter" or more "cubic" than [[Calcite (Inventory)/Spar/dogtooth|dogtooth]] spar. The shape is a combination of a [[rhombohedron]] where each facet is a rhombus, and a [[ | + | Nailhead spar typically is "flatter" or more "cubic" than [[Calcite (Inventory)/Spar/dogtooth|dogtooth]] spar with blunt ends. The shape is a combination of a [[Glossary (Inventory)#Rhombohedron|rhombohedron]] where each facet is a rhombus, and a [[Glossary (Inventory)#Scalenohedral|scalenohedron]] where each facet is a triangle. This is basically a combination of the two primary crystaline shapes of calcite in a single crystal. Pure rhombohedral calcite (rhomb spar) has no specific field on the form and should be inventoried as nailhead. Except for the shape of each crystal, nailhead spar has characteristics very similar to dogtooth spar and can be found in similar locations. |
| - | Nailhead spar can occur singularly; but are usually found in clusters. They can be found lining the insides of [[vug]]s or cavities and cracks but can also occur on the ceiling or walls directly. They formed when the cave was [[phreatic]] so individual crystals can grow to be quite large; but, are usually small. They can be obscured by other formations such as [[Calcite (Inventory)/Flowstone|flowstone]], [[Calcite (Inventory)/Popcorn|popcorn]], crusts or staining. When looking for nailhead spar, take the time to look into cracks and vugs in the walls, floor and ceiling. And don't forget to examine breakdown -- it may possess a vug containing nailhead spar. | + | Nailhead spar can occur singularly; but are usually found in clusters. They can be found lining the insides of [[Glossary (Inventory)#Vug|vug]]s or cavities and cracks but can also occur on the ceiling or walls directly. They formed when the cave was [[Glossary (Inventory)#Phreatic|phreatic]] so individual crystals can grow to be quite large; but, are usually small. They can be obscured by other formations such as [[Calcite (Inventory)/Flowstone|flowstone]], [[Calcite (Inventory)/Popcorn|popcorn]], crusts or staining. When looking for nailhead spar, take the time to look into cracks and vugs in the walls, floor and ceiling. And don't forget to examine breakdown -- it may possess a vug containing nailhead spar. |
==See also== | ==See also== | ||
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==References== | ==References== | ||
*Hill, Carol; Paolo Forti (1997) ''Cave Minerals of the World (Second Edition ed.)'' National Speleological Society p 101 ISBN: [[Special:Booksources/1-879961-07-5|1-879961-07-5]] | *Hill, Carol; Paolo Forti (1997) ''Cave Minerals of the World (Second Edition ed.)'' National Speleological Society p 101 ISBN: [[Special:Booksources/1-879961-07-5|1-879961-07-5]] | ||
| + | *Palmer, Arthur N. (2007) ''Cave Geology'' CAVE BOOKS, Dayton, OH p 275 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]] | ||
| + | |||
| + | ==nailhead, Spar, Calcite== | ||
| + | <gallery perrow=1 widths=300px heights=200px> | ||
| + | File:nailheads.jpg|Nailhead spar | ||
| + | File:Nailhead spar.JPG|Nailhead spar | ||
| + | </gallery> | ||
{{Cave inventory}} | {{Cave inventory}} | ||
Current revision as of 22:16, 9 August 2013
The nailhead field should be used to list stations which exhibit nailhead spar.
Nailhead spar typically is "flatter" or more "cubic" than dogtooth spar with blunt ends. The shape is a combination of a rhombohedron where each facet is a rhombus, and a scalenohedron where each facet is a triangle. This is basically a combination of the two primary crystaline shapes of calcite in a single crystal. Pure rhombohedral calcite (rhomb spar) has no specific field on the form and should be inventoried as nailhead. Except for the shape of each crystal, nailhead spar has characteristics very similar to dogtooth spar and can be found in similar locations.
Nailhead spar can occur singularly; but are usually found in clusters. They can be found lining the insides of vugs or cavities and cracks but can also occur on the ceiling or walls directly. They formed when the cave was phreatic so individual crystals can grow to be quite large; but, are usually small. They can be obscured by other formations such as flowstone, popcorn, crusts or staining. When looking for nailhead spar, take the time to look into cracks and vugs in the walls, floor and ceiling. And don't forget to examine breakdown -- it may possess a vug containing nailhead spar.
See also
References
- Hill, Carol; Paolo Forti (1997) Cave Minerals of the World (Second Edition ed.) National Speleological Society p 101 ISBN: 1-879961-07-5
- Palmer, Arthur N. (2007) Cave Geology CAVE BOOKS, Dayton, OH p 275 ISBN-13: 978-0-939748-66-2, ISBN-10: 0-939748-66-5
nailhead, Spar, Calcite
 Nailhead spar |
 Nailhead spar |
