Sequiota Park

This Gallery

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 10-01-2007

Statistics

Posted By: admin
Viewed: 207
Comments: 0

This Gallery

Popular Tags

No tags have been created or used yet.

Browse All Tags

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

Page 11 of 25 (25 items) « First ... < Previous 9 10 11 12 13 Next > ... Last »

View Sizes View Details

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)

Thumbnail (100x75)
Small (160x120)
Medium (500x374)
Large (640x478)
Original (855x639)

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.

Comments

No Comments