in

GeoSciences

Department of Geography, Geology and Planning

This Gallery

29 total photos
Last updated on 10-02-2007

Statistics

  • Posted By: admin
  • Viewed: 963
  • Comments: 0
  • Ratings: 0
  • Rating

Popular Tags

No tags have been created or used yet.

Page 7 of 29 (29 items) « First ... < Previous 5 6 7 8 9 Next > ... Last »
 
It all begins at Fulbright Spring (behind the fence at the bottom of the limestone outcrop). The spring used to operatea grist mill on this site. Today, it is captured for city water use. Dye traces indicate a subterranean connection with Valley Water Mill
View Sizes View Details
  • Aperture Value: F4.6
  • Date/Time Original: 10/13/2004 2:58:20 PM
  • Exposure Time: 45/50000 sec
  • Flash: Flash did not fire, auto
  • Focal Length: 7.6 mm
  • Model: HP PhotoSmart C945 (V01.46)
More
It all begins at Fulbright Spring (behind the fence at the bottom of the limestone outcrop). The spring used to operatea grist mill on this site. Today, it is captured for city water use. Dye traces indicate a subterranean connection with Valley Water Mill on the northeastern edge of Springfield, but given the karst topography of the Springfield Plateau, it would not be astonishing if it drained a much larger area. Other water sources used at this facility include the deep well shown on the middle right, as well as incoming pipelines from McDaniel Reservoir. Additional water can be pumped from Stockton Reservoir, via Fellows Lake and McDaniel Lake.

Comments

No Comments

Add Comment

(required)  
(optional)
(required)  
Add
Powered by Community Server (Non-Commercial Edition), by Telligent Systems
  • Maintained by: Geosciences
  • • Last Modified:
  • • URL: