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Bottomless Pond EarthCache

Hidden : 5/18/2010
Difficulty:
1.5 out of 5
Terrain:
1.5 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:


Not quite, but certainly deeper than might be expected. This pond, Kortright’s North Peeper Pond, is a rare example of a kettle formation.

During the last Ice Age, this area was covered in a mass of ice more than a kilometre think. When the ice finally began to melt 12,000 years ago, pieces of the glacial ice were left behind. Some of these fragments were buried underground, where they remained partially insulated from the above-ground melting. There they lay perhaps for centuries, like giant hidden ice cubes, long after the bulk of the parent glaciers had vanished. Inevitably, however, as they melted away, large depressions in the terrain were left behind. In some cases, such as here at the Peeper Pond, melt-water and perennial springs rushed in to fill the depression. A new kettle pond or lake was born.

In the thousands of years since its formation, sediments from decaying plant and animal material, pollen, soil, and air-borne dust have gradually settles to the pond’s bottom. There it has lain relatively undisturbed in seasonally-stratified layers of ooze. Due to the undisturbed quality of the pond’s bottom sediments, valuable information about the past climate, flora and faunal populations, and the presence or not of prehistoric humans in the vicinity can be determined by taking a sediment core. This involves drilling down to the bottom of the pond sediments and extracting a cylindrical cross-section of the accumulated layers. A finding of ancient corn pollen could, for instance, indicate that early humans practiced agriculture close by.

With no direct inlet or outlet for the water to flow, this pond will eventually fill in with sediments. Eventually the open water will disappear and a treed swamp will remain.

To log a find send me the length of the pond by measuring it end to end while walking along the trail along with the answers to the following questions.

1) What do many scientists think caused the ice to melt?
2) How deep is the ooze at the bottom of the pond?
3) How deep is the water on top of the sediment?

This cache was placed under direct supervision of park staff. Please use the provided trails and visit this geocache only during park hours.

Additional Hints (No hints available.)