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Cheverie Rock Revelry EarthCache

Hidden : 8/28/2007
Difficulty:
1.5 out of 5
Terrain:
3 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

We came to this spot in search of a physical cache (GCWZDY) and we were just amazed at this location. Unlike anywhere we have been, the geology of this location is worth the trip. As well, it is a spectacular spot for rockhounding along the beach here.

The area around Cheverie was active with mining and quarrying operations in the late 1800's. Two manganese mines and a gypsum quarry operated within this immediate area. A bit further inland several more gypsum quarries operated, all now long abandoned.

This specific location takes you to a spectacular cliff and shore of anhydrite and gypsum.

So what is anhydrite?
Anhydrite is a mineral - anhydrous calcium sulfate, CaSO4. It is in the orthorhombic crystal system, with three directions of perfect cleavage parallel to the three planes of symmetry. Distinctly developed crystals are somewhat rare, the mineral usually presenting the form of cleavage masses.The colour is white, sometimes greyish, bluish or purple. On the best developed of the three cleavages the lustre is pearly, on other surfaces it is vitreous. When exposed to water, anhydrite readily transforms to the more commonly occurring gypsum by the absorption of water.

Anhydrite is most frequently found in salt deposits with gypsum; it was, for instance, first discovered, in 1794, in a salt mine near Hall in Tirol. In this occurrence depth is critical since nearer the surface anhydrite has been altered to gypsum by absorption of circulating ground water.

From an aqueous solution calcium sulfate is deposited as crystals of gypsum, but when the solution contains an excess of sodium or potassium chloride anhydrite is deposited if temperature is above 40°C. This is one of the several methods by which the mineral has been prepared artificially, and is identical with its mode of origin in nature, the mineral is common in salt basins.

The name anhydrite was given by A. G. Werner in 1804, because of the absence of water of crystallization, as contrasted with the presence of water in gypsum. Some obsolete names for the species are muriacite and karstenite; the former, an earlier name, being given under the impression that the substance was a chloride (muriate).

In order to claim this earthcache, you MUST do the following tasks. Do NOT post a found log before receiving confirmation from the cache owner. Failure to follow what is outlined will result in deletion of the log.

1)Take a picture of yourself at the posted co-ordinates with gps in hand. The sample picture should be a good example. Post this picture once you have received comfirmation of your find from the cache owner.

2)Find a sample of anhydrite OR gypsum and take a picture of your gps with it. Post a picture and identify it with your found log.

3)E-mail the cache owner the answer to this question. What is the specific graivty of anhydrite and how does this compare to the specific gravity of gypsum?

This cache should be available to do at all but the highest tides, however it's best done during low tide. Be sure to check tide times before you go!

Additional Hints (Decrypt)

Yvfgra gb gur fanc, penpxyr cbc nf lbh jnyx ba gur ebpxf.

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)