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UP SCHIST CREEK EarthCache

Hidden : 3/3/2012
Difficulty:
2 out of 5
Terrain:
3 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:



LOOKING WEST OVER KINLOCHLEVEN


As an earthcache, there is no “box” or “container” to discover. Rather, with this cache, you discover something about the geology of the area. For more info about Earth Caches take a look at www.earthcache.org



SEAGULL ISLAND & THE PAP OF GLENCOE


This deep glen, filled by Loch Leven and with its high mountain peaks and ridges on either side, shows clear evidence of recent sculpting by glaciers. Loch Leven itself is a Fjord , a valley shaped by glaciers and flooded by the sea.



About 700 million years ago, muddy and sandy sediments settled on the bottom of an ancient ocean. They were deeply buried and then changed, metamorphosed, by great heat and pressure during the formation of a huge range of mountains, known as the Caledonian mountain chain.



SCHIST

At slightly higher temperatures and pressures, shales and muddy sediments are changed into rock called schist. This is a coarser-grained rock than slate, and develops a more wavy layering or foliation. Schists commonly contain flat, shiny flakes of a mineral known as mica. The mica crystals give the schist its distinctive slightly sparkly sheen.

An example of this can be seen by the roche moutonee layby. These Dalradian rocks are known as Binnein Shists, and in this cutting the originally horizontal layers of sediment are tilted steeply upwards as a result of ancient mountain building processes.


ROCHE MOUTONNEE
A short walk to the shore will reveal extensive areas of ice smoothed slabs displaying clear striation marks caused by the moving ice.



FOLDS

Walk a few yards westward and you will see intricate folds within the schist and also a prominent dyke formed when molten rock was injected into a fracture in the schist.



DYKE



LICHEN

As you walk this south facing shoreline you cannot help but notice the beautiful yellow/orange lichen covering patches of the rock surface.


TASKS



Your Earthcaching tasks are as follows:



1) Describe the angle to which the Schists are tilted in the rock face cutting on the opposite side of the road to the lay-by.


2) Observe the schist at this location and describe the major differences to the surrounding rock.

3) If the original clay sediments are subjected to high temperature and pressure, they successively change into rocks, the correct order of which is:

(a) Slate, Shale, Schist (b) Shale, Schist, Slate (e) Slate, Schist, Shale (d) Shale, Slate, Schist

4) Observe the Schist on either side of the dyke and describe what has happened to the rock and why.

5) At the roche mutonnee site shown in the photo above name the large peak (munro) in the distance, left of centre.


Bonus points if you can name the beautiful yellow / orange lichen.



Send the answers to 1-4 in an email to the cache owner via his profile with the heading UP SCHIST CREEK.


Do not post the answers in your log.


Optional task:

We all like to prove the integrity of our claim so a photo of you or your GPS at the Dyke would be great. Careful not to give the game away.

Cachers can log the cache before receiving my confirmation email as any logs from cachers who haven't sent the answers will be quietly deleted!

You must carry out these educational tasks as required by the Earthcaching organisation as a condition of logging the cache.

Logs that do not adhere to these guidelines will be deleted without notification.

For further info: http://www.lochabergeopark.org.uk/index.asp
See www.earthcache.org

Additional Hints (No hints available.)