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The limestone exposed in Sequiota Park is Mississippian in age. It is referred to as the Burlington-Keokuk formations (undivided). It is rich with crinoid and brachipod fossils.

25 total photos
 Last updated on 10-02-2007

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Sequiota Park

 

Sequiota Park » After caves form, they tend to slowly be occluded by calcite or aragonite (CaCO3) precipitates such as the the features shown here; these are referred to as speleothems (not formations). Flowstone and microgours (tiny rimstone dams) are common along this p
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After caves form, they tend to slowly be occluded by calcite or aragonite (CaCO3) precipitates such as the the features shown here; these are referred to as speleothems (not formations). Flowstone and microgours (tiny rimstone dams) are common along this p
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  • Aperture Value: F2.9
  • Date/Time Original: 10/24/2004 12:06:47 PM
  • Exposure Time: 270869/100000 sec
  • Flash: Flash did not fire, auto
  • Focal Length: 7.6 mm
  • Model: HP PhotoSmart C945 (V01.46)
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After caves form, they tend to slowly be occluded by calcite or aragonite (CaCO3) precipitates such as the the features shown here; these are referred to as speleothems (not formations). Flowstone and microgours (tiny rimstone dams) are common along this passageway.

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