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Relative Flow of Groundwater Through Various Layers

Relative Flow of Groundwater Through Various Layers

Blue dye was simultaneously introduced into the bottom of wells number one, two, and three on the right side of the model. The dye shows that groundwater is flowing fastest through the fractured bedrock aquifer and slowest through the unconfined aquifer.
Galleries: Geologic Strata, Groundwater Model, Water Cycle
Keywords: fractured bedrock, aquiclude, aquifer, aquitard, water flow
Photo Location: FCIT Photo Studio, Tampa, FL
Photographer: Dr. Roy Winkelman
Date of Photo: 08/08/2013
Device Make: Canon
Device Model: Canon EOS 5D Mark II
Exposure Time: 0.1
F Number: 13
Original Dimensions: 5616×3744
Picture Orientation: Landscape
GPS Coordinates: 28°3'40.85"N 82°24'36.26"W
Picture Number: 23200