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Sandstone Traditional Cache

This cache has been archived.

Knagur Green: Due to no response from the CO after the request to maintain or replace the cache, I am archiving it to, stop it showing on the listings and/or to create place for the geocaching community.

The Geocache Maintenance guideline explains a CO's responsibility towards checking and maintaining the cache when problems are reported.

Please note that if geocaches are archived by a reviewer or Geocaching HQ for lack of maintenance, they are not eligible for unarchival. This is explained in the Help Center

If the CO feels that this cache has been archived in error please feel free to contact me within 30 days, via email or message via my profile ,quoting the GC number concerned

Thank you for understanding

Knagur Green
Groundspeak Volunteer Reviewer

More
Difficulty:
2 out of 5
Terrain:
2 out of 5

Size: Size:   micro (micro)

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Geocache Description:

A Traditional Cache as part of a Mini-Series.

Materials that were once part of older rocks, materials, animals or plants are called sedimentary rocks. They are deposited by water, wind or ice and accumulate in layers (strata). The majority of deposits occur on the ocean floors although some form in fresh water and on the land. In time, the loose materials harden into solid rocks. Sedimentary rocks fall into 2 categories; clastic or non-clastic. Clastic sedimentary rocks are are formed through a number of weathering and movement processes and are classified according to the size of the mineral grains making up that particular rock. The finest clastic particles are clay, followed by silt and sand. Gravel (conglomerate) is also a type of sedimentary rock. Non-clastic sedimentary rocks are formed by chemical or organic processes.
Source: http://www.namibian.org/travel/namibia/rocks_minerals.html

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