Sequiota Park

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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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Last updated on 10-01-2007

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Sequiota Park » After leaving the reservoir, water flows into the main, generally dry, streambed of Galloway Creek. Minor downcutting is evident locally. This location is just south of Covington Street.

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Aperture Value: F2.9
Date/Time Original: 10/24/2004 12:34:26 PM
Exposure Time: 265/50000 sec
Flash: Flash did not fire, auto
Focal Length: 7.6 mm
Model: HP PhotoSmart C945 (V01.46)

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After leaving the reservoir, water flows into the main, generally dry, streambed of Galloway Creek. Minor downcutting is evident locally. This location is just south of Covington Street.

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