Manganese (Inventory)
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Revision as of 12:34, 25 April 2011
Contents |
Crust
The Crust field of the Manganese section should list stations where a crust of manganese is found.
A manganese crust is a thin layer of manganese that is not firmly adhered to the substructure. It can be recognized by its dark, almost black coloring. It should not be confused with calcite that has been stained black by manganese. Moist manganese crusts often come off when touched so great care should be taken not to disturb them. They can be found on bedrock or clays.
Crust, Manganese
 Manganese crust |
Dendrite
The Dendrite field of the Manganese section should be used to record any appearance of manganese dendrites.
Manganese dendrites appear most often as tiny, scattered, black or dark purple dots on calcite or bedrock, and especially on calcite coatings over limestone bedrock. When more developed, they can appear as dark, fractal, fern-like shapes. The size can vary greatly from tiny specks to larger organized areas. Examine exposed bedrock and calcite, especially coatings on bedrock for the tell-tale dark dots which indicate manganese dendrites. A close examination is often required.
Manganese dendrites are actually a form of manganese oxide (and sometimes iron). The fractal shapes may be an indication of biological influence from iron and manganese oxidizing bacteria. Manganese dendrites could be mistaken for fossils because the branching pattern may look like leaves.
References
- Potter, Russell M. and Rossman, George R.. Mineralogy of manganese dendrites and coatings. American Mineralogist, Volume 64, pages 1219-1226, 1979: http://www.minsocam.org/ammin/AM64/AM64_1219.pdf
- Pseudofossils; Dendrites. Arkansas Geological Survey: http://www.geology.ar.gov/geology/pseudofossils.htm
Dendrite, Manganese
 Manganese dendrites |
