• Mission
• Staff
• Offices
• Announcements
• Site Overview

The distance from the fault to a steady-state no-flow boundary depends on the head, evapotranspiration rate (assumed to be 101.6 cm/yr [40 in/yr]), and the thickness of the fault gouge (KGouge = 3.2x10 ^-7 cm/s)

(Click image to return to the Geologic Odyssey)

Terms of Use | Accessibility

Revised: 27 June, 2012

© 2007 - 2008 NMBGMR
or as specified

Copyright © 2007 - 2008 New Mexico Bureau of Geology & Mineral Resources unless otherwise specified.