Effects of Hurricane Fault Architecture on Groundwater Flow in the Timpoweap Canyon of Southwestern, Utah
Hydrogeologically important features of fault zones include undamaged country rock, the damage zone, and the core zone. Fault cores generally have low porosity and permeability, and often act as a barrier to groundwater flow. The damage zone, by contrast, consists of small faults and fracture networ...
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Format: | Others |
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BYU ScholarsArchive
2005
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Online Access: | https://scholarsarchive.byu.edu/etd/583 https://scholarsarchive.byu.edu/cgi/viewcontent.cgi?article=1582&context=etd |