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A Few Observations on Ground Water
in Devils Postpile National Monument
Chris Farrar
U.S. Geological Survey
y Ca
Long Valle
Dry Creek
ldera
Mammoth
Mtn
MCWD
San Joaquin Ridge
Wells
Devils
Postpile
Dry Creek
Geology from
Snow Making Wells
Bailey 1989
Devils
Postpile
Volcanic
Rocks are
the
principal
groundwater
reservoir
Mammoth Mtn
MCWD
Qal & pumice
Glacial
Basalt,
Andesite, &
Dacite
Bishop Tuff
Granitic
Basement
Not to Scale
Thin, Discontinuous, Unconsolidated, Porous
GW
SW
Extensive, Laterally Continuous,
Consolidated with Fracture
Permeability. Principal Aquifers.
GW
Mostly
SW
Two Distinct Members, Welded &
Unwelded Zones. Thermal Water.
Minor Aquifer Potential
Fracture Permeability, Limited
GW Storage and Flow
Ground-Water Conditions and Connections
• Qal, Qp, & Qg:
Support Meadows, Wetlands, and Fens
Vulnerable to Climate Change and Local Pumping
• Volcanic Rocks:
Main Source of Water to Wells and Springs
Connections to External GW Basins
Water Quality Issues – As, Fe, Mn, Thermal-water
Ground-Water Vulnerabilities
• Unconsolidated Aquifers:
Climate Change – Change seasonal hydrograph
Change in recharge & ET
Local Water-Use: Probably minor & manageable
Changes in GW—SW relations
• Volcanic Rock Aquifers:
Climate Change – Probably less significant to R & ET
External Basin Water-Use – effects unlikely but possible
Springs have greatest vulnerability
Changes in GW—SW possible but localized
• Water Quality:
Mixing thermal and non-thermal, Ski-area pollutants
Hydrologic Assessment
Monitor
Inventory
Hydrogeology
Develop Hydrologic Budget
and
Monitor for Changes and Trends
Preserve, Protect, and Wise Frugal Use
Inventory
• Existing Data
• Springs – Flow,
temperature, chemistry
• Tributary Streams – flow
durations, sources
• Wells – GWLs,
temperature logs, litho.
data
Monitoring Needs
• Piezometers:
near streams, meadows,
and fens
• Springs:
Flow, temperature, and
chemistry
• San Joaquin River:
Establish Stage-discharge
• Water-use: accounting
and Ground-Water levels
• Micromet being done now
Questions ?
Comments?