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San Felasco Hammock Sink EarthCache

Hidden : 8/16/2015
Difficulty:
1.5 out of 5
Terrain:
3 out of 5

Size: Size:   other (other)

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Geocache Description:

This earthcache is located along the trails of San Felasco Hammock Preserve.  There is a $4 parking fee for the park and the trails are open from 8:00 AM to sunset, 365 days a year. Depending on the trails you choose to reach this area, it may be as much as 3.5 miles one way. Please plan accordingly and be sure to take plenty of water. You will also likely want to have bug spray and as always, be aware of your surroundings in nature areas in Florida.


Sinkholes can form in several different ways and can either be gradual or catestropic collapses. This earthcache is designed to teach you about the basics of sinkhole formation and to look at and think about the sinkhole at this location.

SOLUTION SINKHOLES

Solution sinkholes form where soluble bedrock (i.e., limestone, dolomite, marble, and rock salt) is exposed at the land surface and thus subjected to weathering by dissolution. Surface water collects in natural depressions and slowly dissolves a sinkhole.




SUBSIDENCE SINKHOLES

Subsidence sinkholes are similar to solution sinkholes, except that the soluble bedrock is covered by a thin layer of soil and/or sediment. Surface water infiltration dissolves cavities where the bedrock is most significantly fractured, and the sediment fills in the void left by the disolved limestone. The sediment often will restrict the flow of water through the bedrock in these and it allows the sinkhole to become water filled.




COLLAPSE SINKHOLES

Collapse sinkholes form when surface materials suddenly sink into a subsurface cavity or cave. These tend to be the most catestrophic types of sinkholes. The cavities form slowly over time, as groundwater moves along fractures in soluble bedrock and enlarges them through dissolution, and the actual collapse can occur either when the weight of the overlying ground becomes more than the "roof" can support or if an underground cave is normally water filled and groundwater levels drop, the resulting air pocket may allow for collapse.




To claim credit for this earthcache, send the answers to the following questions to the cache owner through their profile above. Please do not post answers in your log, even if encrypted. If answers are posted in your log or you do not send answers, your log will be deleted.

1) Looking the long way across the sinkhole from the posted coordinates, how far across the the sinkhole?

2) Describe the slopes leading down into the sink hole.

3) Based on the types of sinkholes listed in the description and from looking at the sinkhole, how do you think this sinkhole formed?

4) If there is water in the sink, how far is it from the rim of the sinkhole to the water level? If there is no water, how deep do you estimate the sink to be?

5) If there is water in the sink, do you think that it is a holding pond from rainwater or connected to the aquifer? Why?

6) Optional: Please feel free to post pictures in the area.

References:

http://water.usgs.gov/edu/sinkholes.html

http://www4.uwsp.edu/geo/faculty/ozsvath/lectures/Sinkholes.htm

Additional Hints (No hints available.)