Sequiota Park

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The entirity of Galloway Creek is repleat with karst features, but some of the more interesting ones are found north of Covington Street.

25 total photos
Last updated on 10-02-2007

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Sequiota Park » 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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