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Department of Geography, Geology and Planning

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25 total photos
Last updated on 10-02-2007

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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.
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  • Aperture Value: F6.6
  • Date/Time Original: 10/24/2004 11:57:44 AM
  • Exposure Time: 180/50000 sec
  • Flash: Flash did not fire, auto
  • Focal Length: 7.6 mm
  • Model: HP PhotoSmart C945 (V01.46)
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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.

Comments

Anonymous said:

What I love about this park is that it looks like it is constantly being taken care of but in a non-invasive way - no signs of human presence. This is what I would call art.

9:02 PM on April 26, 2011

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