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Red Granite EarthCache

Hidden : 1/27/2009
Difficulty:
1.5 out of 5
Terrain:
2 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

I am a proud

As this is an EarthCache, there is no container and there are special logging requirements which must be met in order to log the find. Logs not meeting the requirements may be deleted.

- The listed coordinates are near the quarry. -

- Nearby parking is available. -


Local information:
In the late 1800s red granite was discovered here in what was at the time known as Sand Prairie. Mining soon followed this discovery and attracted skilled stonecutters from as far away as Europe. Granite blocks were cut for use in street building and routinely shipped as far as Chicago. In the early to mid 1920s the introduction of Portland cement greatly decreased the demand for granite as a paver.

Visitors to the park may swim, fish or scuba dive at their own risk as there are no life-guards. Redgranite Quarry Park is located on the north side of Hwy. 21 behind the post office in downtown Redgranite. Park hours which are from 7am to 7pm are strictly enforced. Please abide by the posted hours and rules while visiting.


- Red Granite -

Wisconsin's State Rock:
On March 9, 1971 Wisconsin designated red granite as its state rock in part due to its abundance, uniqueness, economic value, and historical significance. The word granite comes from the Latin granum, a grain, in reference to the grained structure of such a crystalline rock. In our area, we often find granite along railroad tracks, in parking lots, in river gravels -- and in graveyards (many headstones are made of red granite).

Granite formation:
Granite being an igneous rock, was formed under great pressure deep beneath the Earth's surface. Igneous rocks are one of the three main rock types (the others being sedimentary and metamorphic rock). Igneous rocks are formed by slow solidification of cooled magma (molten rock). Larger crystals are generally indicative of longer cooling times.

Widely distributed around the world, mountain ranges are often made up of large amounts of granite. Much of the granite seen today was intruded onto the Earths crust during the Precambrian period (from 4,567.17 to 542 million years ago) however granite has intruded onto the Earths crust during most geologic periods.

Red granite appearance:
From a distance, red granite looks reddish or pink. Here the granite is made mostly of the minerals feldspar and quartz. The feldspar gives this granite its red hue and the quartz crystals appear as a semi-clear gray or purple color. There are also small crystals of mica and other darker minerals which appear as specks in the rock. Many broken surfaces are flat and shine in the sunlight.

Uses of granite:
Because of its hardness and comparative cheapness in relation to marble, granite has been used for thousands of years for both internal and external features. It is commonly used outdoors in construction of buildings, bridges, paving, for monuments (like Mount Rushmore) and indoors for items such as tile, countertops, stair treads and much more. It can be cut into virtually any shape, and is practically unscratchable.

- Logging Requirements: -

1. Take a photo of yourself with your GPS (or your GPS alone) at a recognizable part of the site. I may allow exceptions to this requirement if you contact me PRIOR TO LOGGING your find on a case by case basis.

2. There is a post near the edge of the quarry with three 3 signs attached to it. What does the middle sign warn of at this location?

3. Perform a scratch test on the rock and email me through my profile the results of your test. Did you scratch the rock with the nail OR did the nail scratch off on the rock surface?

To carry out the scratch test all you need is a shiny new nail. Using the sharp point of the nail on a flat section of rock, try to scratch a small line (less than an inch in length is fine) on the surface of your rock. If the nail digs in and scratches off a line of powdered rock, then the nail is harder than the rock.

In the example pictured above (left) the nail scratched off a line of powdered white limestone. In the example on the right the nail rubbed off on the rock thus the rock was harder than the nail.


Sources:
http://saltthesandbox.org/rocks/scratchtest.htm
http://www.cloburn.co.uk/thequarryprocess.htm
http://www.redgranitewisconsin.com/
http://www.shgresources.com/wi/symbols/rock/
http://en.wikipedia.org/wiki/Igneous_rock

This listing approved on 12/16/2008 by the Redgranite village board at its scheduled meeting.
*Extra special thanks to Geocacher team
"JimandLinda" without whom this cache would not have been possible.

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