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Perched in Mount Uniacke EarthCache

This cache has been archived.

Geocaching HQ Admin: It has now been over 30 days since Geocaching HQ submitted the disabled log below and, unfortunately, the cache owner has not posted an Owner maintenance log and re-enabled this geocache. As a result, we are now archiving this cache page.

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Hidden : 1/18/2008
Difficulty:
1.5 out of 5
Terrain:
1.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

This will be a great but significant hike along a great trail system. The trails are well marked with maps and trail markers. No bushwacking is needed so please stay on the trails at all times.

Wetlands Trail

This loop can be accessed along the Barrens Trail, or by the Post Road Trail. Anticipate a 3-hour round trip from the Trailhead(7km). Follow the Post Road Trail to Black Brook(1.5km). Leave the Post Road through a small ravine into a grassy marshland.

This nature-lovers hike features a brook,two lakes (Thompson Lake & Clark Lake), a beaver dam,Pitcher plants and the objective of this EarthCache a Perched Boulder.

Glaciers Sculpted the Landforms A huge ice sheet, several kilometers thick, covered much of Nova Scotia between 10,000 and 70,000 years ago. Glacial action yielded distinctive erosional and depositional features.

Erosion of the landscape included the gouging and plucking out of boulders and rocks, so that depressions were carved. Rocks at the base of moving glaciers left scratches called glacial striations on the bedrock surface. Bogs and small marshy lakes are also features of glaciations; they formed because of poor drainage of the hollows that were eroded by glacial action.

As they moved, the glaciers also deposited a mixture of unsorted rocks, gravel, sand and clay known as glacial till. This till formed hill-like drumlins such as Citadel Hill, McNabs Island, Georges Island and other hills in the Halifax area. There is also a series of drumlins along the east coast of St. Margaret’s Bay. As the glaciers retreated, boulders or erratics were deposited. Today, numerous erratics can be seen on the landscape of Peggys Cove.

A Perched boulder is a glacial erratic that has been transported by a glacier and rests precariously at a different location then its source.

A large, angular boulder of granite perched on a ridge of granite was left here by a glacier when it melted.

In order to claim this Earthcache please post a picture of you and/or your GPS with the Perched blouder in the background. Also, e-mail me the answers to the following three questions:

1. What is the approximate height of the two boulders?

2. Estimate the weight of the Perched boulder. You will need to estimate the volume of he boulder and multiply that by the "weight density" for typical granite (use 168 pounds/cubic foot).

You do not need to wait for confirmiation from me before posting online. However, any logs that do not fulfill ALL requirements will be deleted.

Additional Hints (Decrypt)

oevat n pnzren

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)