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Kettletown Geology Earthcache EarthCache

Hidden : 6/5/2005
Difficulty:
1 out of 5
Terrain:
3 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:

We'll start at 41 25.600 / 73 12.544 on the Miller Trail exploring interesting geological features (passing many geocaches on the way) and finish on the southern trails finding the answers to this multistage earthcache.

At those coords on the trail you see a brown basalt boulder. Where did it come? How did it get here among all these grey rocks? After all, the nearest basalt bedrock is three miles away (to the northwest).

During the last ice age, daily melting would refreeze at night, grabbing rock fragments which would then be carried along with the glacier. Ultimately, they were left here, worn round from their long journey. They are called erratics.

Continue to 41 25.696 / 73 12.413, you'll see more basalt erratics on your way. Once there notice the lighter colored pegmatite erratic on the left (northwest) with it's crystals. Pegmatite forms from molten rock far below the surface and cools more slowly, resulting in large white or pink crystal intrusions.

You will be near a small stream when you arrive at 41 25.980 / 73 12.700 where you'll see gneiss (pronounced "nice") boulders. They appear black with white banding. Originally basalt when this area was covered by ocean ages ago, heat and pressure changed them to what you see now--a type of metamorphic rock.

Now head to one of the overlook trails and find what looks like a "stone step" by 41 25.675 / 73 12.730. What are those hard dark reddish lumps sticking up from it? Garnets. Harder than the stone they are embedded in, they survive rain, wind, ice and your shoes as the surrounding rock gets eroded away.

So ends the first part of our adventure... Now to claim your find, head over to the trailhead of Pomperaug: 41 25.714 / 73 12.232 (hike or drive to pull-off parking) or the upper camping area trailhead 41 25.356 / 73 12.200 (park at the station and walk up the road unless camping or invited guest) and hunt for the answers!

IMPORTANT: Click here to email the answers to the following questions when you submit your log (do NOT put in your log even encrypted):

  1. What could, 41 25.075 / 73 12.000 this area be called?
  2. Along the trail at: 41 25.118 / 73 12.009, do you find basalt, garnets, gneiss or pegmatite?
  3. At this location: 41 25.455 / 73 12.100, which rocks are these?
In your online log feel free to answer the following:
What is the most interesting thing you learned from this cache?
How many people were in your group? Ages?

Glossary:
basalt; the dark, dense, igneous rock of a lava flow
bedrock; unbroken solid rock below soil
erratic; wandering, not fixed
erode; eat away, disintegrate
garnet; hard pink, red, brown or green gems
gneiss; metamorphic rock with bands of different color (pronounced "nice")
igneous; rock that was molten
intrusion; injection of molten rock
metamorphic; exhibiting profound change
pegmatite; coarse crystalline igneous rock

For more details: CT DEP Kettletown Geology

Additional Hints (No hints available.)