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dc.contributor.authorMontgomery, E. L.
dc.contributor.authorDeWitt, R. H.
dc.date.accessioned2013-08-29T22:48:47Z
dc.date.available2013-08-29T22:48:47Z
dc.date.issued1974-04-20
dc.identifier.issn0272-6106
dc.identifier.urihttp://hdl.handle.net/10150/300367
dc.descriptionFrom the Proceedings of the 1974 Meetings of the Arizona Section - American Water Resources Assn. and the Hydrology Section - Arizona Academy of Science - April 19-20, 1974, Flagstaff, Arizonaen_US
dc.description.abstractThe inner basin is a collapse and erosional feature in San Francisco Mountain, an extinct volcano of late Cenozoic age, which lies approximately eight miles north of flagstaff, Arizona. The main aquifer's coefficient of transmissibility is approximately 14,000 gallons per day per foot and the storage coefficient was 0.08. Aquifer boundaries increased rates of drawdown of water levels in the inner basin well field. Inner basin springs which issue from perched reservoirs are not affected by pumpage of inner basin wells. Recharge is greater than the average yield from springs and wells in the basin which has an average of 8,000 acre-feet of water in storage in the principal aquifer. A large amount of water is lost from the inner basin aquifer system via leakage into underlying fractured volcanic rocks. It is believed that a part of this water could be intercepted by pumpage from a well constructed in the interior valley.
dc.language.isoen_USen_US
dc.publisherArizona-Nevada Academy of Scienceen_US
dc.rightsCopyright ©, where appropriate, is held by the author.en_US
dc.subjectHydrology -- Arizona.en_US
dc.subjectWater resources development -- Arizona.en_US
dc.subjectHydrology -- Southwestern states.en_US
dc.subjectWater resources development -- Southwestern states.en_US
dc.subjectWater resourcesen_US
dc.subjectWater supplyen_US
dc.subjectGroundwater basinsen_US
dc.subjectPumpingen_US
dc.subjectAquifer characteristicsen_US
dc.subjectArizonaen_US
dc.subjectGroundwater miningen_US
dc.subjectGroundwateren_US
dc.subjectGroundwater rechargeen_US
dc.subjectAquifersen_US
dc.subjectWater wellsen_US
dc.subjectWater sourcesen_US
dc.subjectWater yielden_US
dc.subjectHydrogeologyen_US
dc.subjectWater storageen_US
dc.subjectTransmissivityen_US
dc.subjectStorage coefficienten_US
dc.subjectBoundaries (surfaces)en_US
dc.subjectSpringsen_US
dc.subjectPerched wateren_US
dc.subjectLeakageen_US
dc.subjectSan Francisco volcano (Ariz)en_US
dc.subjectFlagstaff (Ariz)en_US
dc.titleWater Resources of the Inner Basin of San Francisco Volcano, Coconino County, Arizonaen_US
dc.typetexten_US
dc.typeProceedingsen_US
dc.contributor.departmentNorthern Arizona Universityen_US
dc.contributor.departmentCity of Flagstaff Water Departmenten_US
dc.identifier.journalHydrology and Water Resources in Arizona and the Southwesten_US
dc.description.collectioninformationThis article is part of the Hydrology and Water Resources in Arizona and the Southwest collections. Digital access to this material is made possible by the Arizona-Nevada Academy of Science and the University of Arizona Libraries. For more information about items in this collection, contact anashydrology@gmail.com.en_US
refterms.dateFOA2018-06-17T18:43:00Z
html.description.abstractThe inner basin is a collapse and erosional feature in San Francisco Mountain, an extinct volcano of late Cenozoic age, which lies approximately eight miles north of flagstaff, Arizona. The main aquifer's coefficient of transmissibility is approximately 14,000 gallons per day per foot and the storage coefficient was 0.08. Aquifer boundaries increased rates of drawdown of water levels in the inner basin well field. Inner basin springs which issue from perched reservoirs are not affected by pumpage of inner basin wells. Recharge is greater than the average yield from springs and wells in the basin which has an average of 8,000 acre-feet of water in storage in the principal aquifer. A large amount of water is lost from the inner basin aquifer system via leakage into underlying fractured volcanic rocks. It is believed that a part of this water could be intercepted by pumpage from a well constructed in the interior valley.


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