Karren (Inventory)/Spitzkarren
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Spitzkarren are tower-like formations left by water dripping on dissolvable substrate like limestone, [[Gypsum (Inventory)|gypsum]], mud, guano, or even [[Corrosion residue (Inventory)|corrosion residue]] (speleosol). It could be considered the opposite of [[Karren (Inventory)/Rillenkarren|rillenkarren]] which form as rills or hollows. | Spitzkarren are tower-like formations left by water dripping on dissolvable substrate like limestone, [[Gypsum (Inventory)|gypsum]], mud, guano, or even [[Corrosion residue (Inventory)|corrosion residue]] (speleosol). It could be considered the opposite of [[Karren (Inventory)/Rillenkarren|rillenkarren]] which form as rills or hollows. | ||
| - | ==See | + | ==See== |
*[[Karren (Inventory)/Rillenkarren|Rillenkarren]] | *[[Karren (Inventory)/Rillenkarren|Rillenkarren]] | ||
{{Cave inventory}} | {{Cave inventory}} | ||
Revision as of 02:44, 29 April 2011
The spitzkarren field of the Karren section should be used to list stations which exhibit spitzkarren.
Spitzkarren are tower-like formations left by water dripping on dissolvable substrate like limestone, gypsum, mud, guano, or even corrosion residue (speleosol). It could be considered the opposite of rillenkarren which form as rills or hollows.
See
