About the Cover
Cover: In “Fault Zone Deformation Overprints Permeability of Nonwelded Ignimbrite: Chalk Cove Fault, Bishop Tuff, Bishop, California,” p. 610–627, Cynthia L. Dinwiddie, Kelly Keighley Bradbury, Ronald N. McGinnis, Randall W. Fedors, and David A. Ferrill explore the role of secondary heterogeneity in our ability to understand and predict lateral flow. Field staff are shown working at Transect CCHW1, with the photographer standing near Transect CC2/CC3, at Chalk Cove Fault, a natural analog site for the the Paintbrush nonwelded hydrogeologic unit at Yucca Mountain. In the mid-ground is the Owens River Valley, and the mountains in the background are the Sierra Nevada.
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Copyright © 2008 by the Soil Science Society of America.
