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Limestone Paving (Clints and Grykes) EarthCache

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coman123: Area temporary closed. sorry

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Hidden : 12/1/2011
Difficulty:
1.5 out of 5
Terrain:
2.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:



Limestone Paving
(Clints and Grykes)

No I'm not talking about paving  downtown Kingston
This is more of Mother Nature showing off her construction skills

Allow me to explain.

As you leave the trail heading to GZ, you will notice a lot of exposed Limestone.

You should also notice a good example of Limestone Paving
or in Geological Terms

Clints and Grykes

No I have not lost my mind creating this Earth Cache

So Just what are Clints and Grykes (Grikes as some spell it)?

Well.............



 


 Limestone pavement is made up of two separate but integral parts known as clints and grykes.

Clints are the blocks of limestone that constitute the paving, their area and shape is directly dependent
upon the frequency and pattern of grykes. Grykes are the fissures or spaces  that isolate the individual clints.

 A limestone pavement is a natural Karst
landform consisting of a flat, incised surface of
exposed
limestone that resembles an artificial pavement.
(Karst:  a geologic formation shaped by the
dissolution of a layer or layers
of soluble bedrock, usually carbonate rock
such as limestone or dolomite)


 

Conditions for
limestone pavements are created when the advancing glacier scrapes away
  and exposes horizontally-bedded limestone, the glacial
retreat leaves behind a flat and bare surface.

Limestone is slightly soluble in water and especially in acid rain, so
corrosive drainage along joints and cracks in the limestone can produce slabs
called "clints" isolated by deep fissures called "grikes" or "grykes".

If the grikes are fairly straight and the clints are uniform in size, the
resemblance to man-made paving stones is striking, but often they are less
regular. Limestone pavements that develop beneath a mantle of topsoil
usually exhibit more rounded forms.

At Ground Zero is a great example of Clints and Grykes forming a field of Limestone Pavement

To log this Earth Cache you must send me the answers to the following questions
Via my Geocaching Profile

++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++

1) What is the Average depth of the Grykes at GZ?

++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++

2) Is the area of Limestone Paving at GZ bigger or smaller then
100 meters square?
For those of you not great with math, From GZ can you walk 50 meters
in every direction and still be on the Limestone Pavement?

++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++

Are most of the Clints near GZ, Uniform in shape or Irregular?
Please explain.

++++++++++++++++++++++++++++++++++++++++++++++++++++++++++++

Which direction was the Glacier traveling in this area
More North and South
or
More East and West

+++++++++++++++++++++++++++++++++++++++++++++++++++++++++++

Although Pictures are not mandatory for logging this Earth Cache
they are always welcomed

And finally, my Earth Caches are meant to be fun and educational, and are not
meant to stress you out trying to get perfect answers on the questions.

Once the answers are sent, please log the Earth Cache, if
there is concern with your answers, I'll contact you.

Happy (Earth) Caching everyone

Coman123





Additional Hints (No hints available.)