Determinations of peak discharge for floods of May to June 1983 were made for 11 streams along the northern Wasatch Front from Salt Lake City to North Ogden. At nine of the streams, the floods during the spring of 1983 equaled or exceeded the 100-year flood. The peak discharge at Stone Creek was 40 times the maximum previously known flood, and the peak discharges at the other sites ranged from slightly greater to about five times that previously known. In addition to the outstanding peak discharges, streamflow at the 11 sites commonly remains high for days, weeks, or even a month.
The floods resulted from retention of an abnormally large snowpack until rain combined with above normal temperature caused rapid melting. The peak discharges and continued high flows damaged homes, highways, and drainage canals.
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L.L.","contributorId":81513,"corporation":false,"usgs":true,"family":"Hubbard","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":256579,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parks, T.D.","contributorId":17257,"corporation":false,"usgs":true,"family":"Parks","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":256577,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiss, D.L.","contributorId":68812,"corporation":false,"usgs":true,"family":"Weiss","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":256578,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hubbard, L.E.","contributorId":104945,"corporation":false,"usgs":true,"family":"Hubbard","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":256580,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":26681,"text":"wri844248 - 1984 - Geohydrology of rocks penetrated by test well UE-25p#1, Yucca Mountain area, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri844248","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4248","title":"Geohydrology of rocks penetrated by test well UE-25p#1, Yucca Mountain area, Nye County, Nevada","docAbstract":"Test well UE-25pNo1 was drilled in cooperation with the U.S. Department of Energy in the southwestern part of the Nevada Test Site, for investigations related to the isolation of high-level nuclear wastes. Rocks penetrated in the well are predominantly ash-flow tuffs of Tertiary age to a depth of 1,244 meters and dolomite of Paleozoic age to a total depth of 1,805 meters. Hydraulic head is 20 meters higher in the Paleozoic dolomite than in most of the Tertiary tuffs; this hydraulic-head difference indicates a major hydrologic barrier to the downward movement of fluid. Any vertical fluid movement from the Tertiary to the Paleozoic sections would be small, as would be movement from the Paleozoic rocks into the Tertiary rocks. In the Tertiary section, an interval of less than 30 meters in the upper Prow Pass Member of Crater Flat Tuff has an apparent transmissivity of 14 meters squared per day. In the Paleozoic section, an interval of less than 22 meters has an apparent transmissivity of 69 meters squared per day. Compositions of water from the Tertiary and Paleozoic sections are similar to regional waters from rocks of the same ages. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri844248","usgsCitation":"Craig, R.W., and Robison, J.H., 1984, Geohydrology of rocks penetrated by test well UE-25p#1, Yucca Mountain area, Nye County, Nevada: U.S. Geological Survey Water-Resources Investigations Report 84-4248, vi, 57 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844248.","productDescription":"vi, 57 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":122883,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4248/report-thumb.jpg"},{"id":55546,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4248/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a79","contributors":{"authors":[{"text":"Craig, R. W.","contributorId":40984,"corporation":false,"usgs":true,"family":"Craig","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":196820,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robison, J. 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A computer model was used to simulate the changes in streamflow and water levels from 1980 through 1999. Six pumpage options were tested using variations in pumpage rate and number of wells pumping in the model area. If the full amount appropriated by water rights were pumped rather than actual 1979 conditions of pumpage, annual pumpage would be reduced 24 percent, but net annual river loss would be reduced only 1 percent. A pumpage increase of approximately 19 percent over 1979 pumpage conditions would cause an increase of net annual river loss from 5 to 9 percent. Increased pumpage, in the form of additional wells in the model area, would cause additional ground water to be removed from storage in the aquifer and an increase in net annual river loss.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844082","usgsCitation":"Dunlap, L.E., Lindgren, R.J., and Carr, J.E., 1984, Projected effects of ground-water withdrawals in the Arkansas River Valley, 1980-99, Hamilton and Kearny Counties, southwestern Kansas: U.S. Geological Survey Water-Resources Investigations Report 84-4082, vi, 168 p., https://doi.org/10.3133/wri844082.","productDescription":"vi, 168 p.","costCenters":[],"links":[{"id":408273,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35975.htm","linkFileType":{"id":5,"text":"html"}},{"id":55778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4082/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157450,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4082/report-thumb.jpg"}],"country":"United States","state":"Kansas","county":"Hamilton County, Kearny County","otherGeospatial":"Arkansas River Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102.079,\n 37.8030\n ],\n [\n -101.373,\n 37.8030\n ],\n [\n -101.373,\n 38.056\n ],\n [\n -102.079,\n 38.056\n ],\n [\n -102.079,\n 37.8030\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d9c1","contributors":{"authors":[{"text":"Dunlap, L. 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The maps are based on analyses by the South Carolina Department of Health and Environmental Control of water samples taken during the period 1972 to 1982 from 442 public and private wells developed in the Piedmont. In general, alkalinity, hardness, and concentrations of sodium, magnesium, and chloride were higher in the Carolina Slate Belt than they were in the other geologic belts of the Piedmont. 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1984 - Controlled photomosaic of the Phaethontis Southeast Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:10","indexId":"i1603","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1603","subseriesTitle":"NONE","title":"Controlled photomosaic of the Phaethontis Southeast Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1603","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Controlled photomosaic of the Phaethontis Southeast Quadrangle of Mars: U.S. Geological Survey IMAP 1603, 1 photomosaic ;53 x 59 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1603.","productDescription":"1 photomosaic ;53 x 59 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":251379,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1603/report.pdf","size":"28","linkFileType":{"id":1,"text":"pdf"}},{"id":251380,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1603/plate-1.pdf","size":"9178","linkFileType":{"id":1,"text":"pdf"}},{"id":252244,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1603/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68685f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534021,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12110,"text":"ofr83851 - 1984 - Hydrology of area 39, Western region, Interior Coal Province, Kansas and Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr83851","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-851","title":"Hydrology of area 39, Western region, Interior Coal Province, Kansas and Missouri","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83851","usgsCitation":"Bevans, H., Skelton, J., Kenny, J.F., and Davis, J.V., 1984, Hydrology of area 39, Western region, Interior Coal Province, Kansas and Missouri: U.S. Geological Survey Open-File Report 83-851, v, 176p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr83851.","productDescription":"v, 176p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":95057,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0851/report.pdf","size":"22990","linkFileType":{"id":1,"text":"pdf"}},{"id":144778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0851/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604442","contributors":{"authors":[{"text":"Bevans, H.E.","contributorId":102892,"corporation":false,"usgs":true,"family":"Bevans","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":165113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skelton, John","contributorId":70392,"corporation":false,"usgs":true,"family":"Skelton","given":"John","email":"","affiliations":[],"preferred":false,"id":165110,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kenny, J. F.","contributorId":100378,"corporation":false,"usgs":true,"family":"Kenny","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":165112,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Davis, Jerri V. jdavis@usgs.gov","contributorId":99149,"corporation":false,"usgs":true,"family":"Davis","given":"Jerri","email":"jdavis@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":false,"id":165111,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":60011,"text":"mf1510B - 1984 - Geochemical maps of the Cornplanter Roadless Area, Warren County, Pennsylvania","interactions":[],"lastModifiedDate":"2016-08-22T15:24:51","indexId":"mf1510B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1510","chapter":"B","title":"Geochemical maps of the Cornplanter Roadless Area, Warren County, Pennsylvania","docAbstract":"The U.S. Geological Survey (USGS) made a reconnaissance geochemical survey of the Cornplanter Roadless Area (fig. 1) to test for indistinct or unexposed mineral deposits that might be recognized by their geochemical halos or patterns formed by the distribution of trace elements. Lesure, assisted by Andrew E. Grosz, collected 22 stream-sediment, 63 soil, and 23 rock samples from within and dear the study area during October 1980. All samples were analyzed for 31 elements using semi-quantitative spectrographic methods by Day in USGS laboratories, Denver, Colo. (table 1). In addition, the samples were also analyzed for zinc by means of an atomic absorption method by B.F. Arbogast and W.C. Martin, USGS laboratories, Denver Colo. J.T. Hanley and P.G. Schruben formatted the analytical data by computer methods for table 1.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1510B","usgsCitation":"Lesure, F.G., and Day, G.W., 1984, Geochemical maps of the Cornplanter Roadless Area, Warren County, Pennsylvania: U.S. Geological Survey Miscellaneous Field Studies Map 1510, 49.59 x 36.73 inches, https://doi.org/10.3133/mf1510B.","productDescription":"49.59 x 36.73 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1510B.PNG"},{"id":327323,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1510-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Pennsylvania","county":"Warren","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.9795970916748,\n 41.98667384282501\n ],\n [\n -78.97187232971191,\n 41.991586098378676\n ],\n [\n -78.97024154663086,\n 41.992798155077665\n ],\n [\n -78.96672248840332,\n 41.995158409781546\n ],\n [\n -78.96294593811034,\n 41.99662555102285\n ],\n [\n -78.96002769470215,\n 41.993499861564736\n ],\n [\n -78.95779609680176,\n 41.99113954535575\n ],\n [\n -78.9535903930664,\n 41.98833256890643\n ],\n [\n -78.95221710205078,\n 41.986163456874266\n ],\n [\n -78.95050048828125,\n 41.98539787027622\n ],\n [\n -78.94775390625,\n 41.98016611546063\n ],\n [\n -78.94723892211914,\n 41.97748626968658\n ],\n [\n -78.9462947845459,\n 41.97525297872791\n ],\n [\n -78.94148826599121,\n 41.968425003549285\n ],\n [\n -78.94097328186035,\n 41.96612757631881\n ],\n [\n -78.94062995910645,\n 41.964085349226664\n ],\n [\n -78.93985748291016,\n 41.96210687930571\n ],\n [\n -78.93857002258301,\n 41.95891566933552\n ],\n [\n -78.9382266998291,\n 41.95687321108292\n ],\n [\n -78.93771171569824,\n 41.953426414345635\n ],\n [\n -78.93745422363281,\n 41.9510007789743\n ],\n [\n -78.9371109008789,\n 41.948192033224366\n ],\n [\n -78.93685340881348,\n 41.94685145185191\n ],\n [\n -78.93728256225586,\n 41.94468092700416\n ],\n [\n -78.93839836120605,\n 41.94219111633131\n ],\n [\n -78.94037246704102,\n 41.93989274326094\n ],\n [\n -78.95805358886719,\n 41.94085040877467\n ],\n [\n -78.95788192749023,\n 41.9613410034882\n ],\n [\n -78.95659446716309,\n 41.96127718008789\n ],\n [\n -78.95676612854004,\n 41.96721248283543\n ],\n [\n -78.958740234375,\n 41.96702103008676\n ],\n [\n -78.96406173706055,\n 41.9829734519797\n ],\n [\n -78.97212982177734,\n 41.980931764968034\n ],\n [\n -78.9747905731201,\n 41.980229919937884\n ],\n [\n -78.97805213928223,\n 41.981250782878995\n ],\n [\n -78.97976875305176,\n 41.98316485678062\n ],\n [\n -78.98054122924805,\n 41.985142672697684\n ],\n [\n -78.9795970916748,\n 41.98667384282501\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae072","contributors":{"authors":[{"text":"Lesure, Frank G.","contributorId":20068,"corporation":false,"usgs":true,"family":"Lesure","given":"Frank","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":262986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Day, Gordon W.","contributorId":21520,"corporation":false,"usgs":true,"family":"Day","given":"Gordon","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":262987,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27160,"text":"wri844004 - 1984 - Magnitude and frequency of floods from urban streams in Leon County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri844004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4004","title":"Magnitude and frequency of floods from urban streams in Leon County, Florida","docAbstract":"Techniques are provided for estimating flood magnitudes for urban-flow streams in Leon County, Florida, for recurrence intervals of 2, 5, 10, 25, 50, 100, and 500 years. Synthetic flood peaks were generated by using a calibrated lumped-parameter rainfall-runoff model, pan evaporation data from Milton, Florida, and long-term unit rainfall records from Thomasville-Collidge, Georgia, and Pensacola, Florida. The flood peaks were used in multiple linear regression analyses to derive regional equations relating flood magnitude to basin characteristics. Significant basin characteristics were drainage area and impervious area. The average standard error of prediction ranged from + or - 32 percent for the 5-year recurrence interval to + or - 47 percent for the 500-year recurrence interval flood. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844004","usgsCitation":"Franklin, M., and Losey, G., 1984, Magnitude and frequency of floods from urban streams in Leon County, Florida: U.S. Geological Survey Water-Resources Investigations Report 84-4004, iv, 37 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844004.","productDescription":"iv, 37 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":124176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4004/report-thumb.jpg"},{"id":56037,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4004/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64952f","contributors":{"authors":[{"text":"Franklin, M.A.","contributorId":13631,"corporation":false,"usgs":true,"family":"Franklin","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":197664,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Losey, G.T.","contributorId":12522,"corporation":false,"usgs":true,"family":"Losey","given":"G.T.","email":"","affiliations":[],"preferred":false,"id":197663,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10543,"text":"ofr84619 - 1984 - Literature review and need for additional study of surface-water quality in the Cuyahoga Valley National Recreation Area, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr84619","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-619","title":"Literature review and need for additional study of surface-water quality in the Cuyahoga Valley National Recreation Area, Ohio","docAbstract":"The Cuyahoga Valley National Recreation Area encompasses about 24 miles of the middle reach of the Cuyahoga River and parts of four major tributaries -- Furnace Run, Brandywine Creek, Chippewa Creek, and TInkers Creek. Water quality in this reach does not meet Ohio water-quality standards for dissolved oxygen, fecal bacteria, ammonia, and lead. Point sources of effluent contribute contaminants. \r\n\r\nOn the basis of a review of scientific and technical literature, National Park Service management goals, and water-quality data collected by the U.S. Geological Survey, three subject areas for future study are suggested: (1) The dissolved oxygen regime, (2) chemical quality of base flow, and (3) quality of storm-water runoff.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84619","usgsCitation":"Childress, C., 1984, Literature review and need for additional study of surface-water quality in the Cuyahoga Valley National Recreation Area, Ohio: U.S. Geological Survey Open-File Report 84-619, iv, 58 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84619.","productDescription":"iv, 58 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0619/report-thumb.jpg"},{"id":38386,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0619/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4eb9","contributors":{"authors":[{"text":"Childress, C.J.","contributorId":88734,"corporation":false,"usgs":true,"family":"Childress","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":161570,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":59341,"text":"mf1568B - 1984 - Aeromagnetic map of the Fossil Springs Roadless Area, Yavapai, Gila, and Coconino counties, Arizona","interactions":[],"lastModifiedDate":"2016-08-22T10:25:00","indexId":"mf1568B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1568","chapter":"B","title":"Aeromagnetic map of the Fossil Springs Roadless Area, Yavapai, Gila, and Coconino counties, Arizona","docAbstract":"The aeromagnetic map of the Fossil Springs Roadless Area was compiled from data collected in 1980 by Airmag Surveys, Inc., for the U.S. Geological Survey. Total magnetic intensity measurements were made along east-west flight lines about 0.5 mi apart and flown at an average altitude of 1,000 ft above the ground surface. A regional magnetic field (the International Geomagnetic Reference Field, 1975, updated to months flown) was removed from the data and a constant of 50,800 gammas was added to the adjusted total field intensity values.
\nThe roadless area includes the upper part of Fossil Creek and its northeastern tributaries in Sandrock Canyon and Calf Pen Canyon. The extremely rugged canyon of Fossil Creek is in several places more than 1,500 ft deep. Elevation of the canyon floor ranges from 4,600 ft near the mouth of Calf Pen Canyon to 3,500 ft at the southwest end of the area. Peaks and ridges on the uplands bordering the canyons range in elevation from 5,300 ft west of Fossil Springs to 6,900 ft in the northeastern part of the area. Maximum topographic relief along these uplands is less than 200 ft.
\nThe Fossil Springs Roadless Area is underlain by more than 3,000 ft of Paleozoic rocks consisting mostly of sandstone, shale, dolomite, and limestone. West of Fossil Springs and along most of the border of the area, these rocks are generally overlain by late Tertiary volcanic rocks, mainly basaltic lavas and pyroclastic deposits. Quaternary alluvial, colluvial, landslide, and travertine deposits overlie large parts of the country rock in the canyons. In the southwestern part of the area, the volcanic rocks are more than 2,000 ft thick. Along the northwest and northeast margins, these rocks are 300-400 ft thick.
\nThe prevailing dip of the Paleozoic strata is low to the north or northeast. The dominant homoclinal structure is interrupted by several fault blocks, in which the strata dip westward or southward. All the faults are high-angle normal faults and have displacements commonly ranging from about 50 to 400 ft. Although fault relations are obscure within the volcanic sequence, many faults seem to displace the volcanic rocks less than the underlying Paleozoic rocks. The volcanic rocks, which rest unconformably on the Paleozoic strata, are flat lying in the northern part of the map area, but west of Fossil Springs they dip gently southwestward. The ancestral Mogollon Rim, a north-northwest-trending escarpment of Paleozoic rocks now concealed by Tertiary volcanic rocks lies near Fossil Springs (Twenter, 1962).
\nThe magnetic anomalies and patterns on the aeromagnetic map reflect variations of magnetization in the underlying rocks. Basaltic rocks contain moderate amounts of magnetic minerals, mainly magnetite, and possess strong intensities of magnetization. The more silicic volcanic rocks have much lower magnetization intensities. Sedimentary rocks contain little or no magnetite and are virtually nonmagnetic.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1568B","usgsCitation":"Davis, W.E., and Weir, G.W., 1984, Aeromagnetic map of the Fossil Springs Roadless Area, Yavapai, Gila, and Coconino counties, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1568, Plate: 43.52 x 29.85 inches, https://doi.org/10.3133/mf1568B.","productDescription":"Plate: 43.52 x 29.85 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326367,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1568B.JPG"},{"id":327211,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1568-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Arizona","county":"Coconino County, Gila County, Yavapai County","otherGeospatial":"Fossil Springs Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.66666666666667,34.3675 ], [ -111.66666666666667,34.5 ], [ -111.45083333333334,34.5 ], [ -111.45083333333334,34.3675 ], [ -111.66666666666667,34.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6966c3","contributors":{"authors":[{"text":"Davis, W. E.","contributorId":100844,"corporation":false,"usgs":true,"family":"Davis","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":261819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weir, G. W.","contributorId":107290,"corporation":false,"usgs":true,"family":"Weir","given":"G.","middleInitial":"W.","affiliations":[],"preferred":false,"id":261820,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26950,"text":"wri834081 - 1984 - Ground-water conditions and shallow test-well information in the eastern half of Merced County, California, 1977-82","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri834081","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4081","title":"Ground-water conditions and shallow test-well information in the eastern half of Merced County, California, 1977-82","docAbstract":"The city of Merced, other municipalities, and irrigation in the vicinity of Merced in the San Joaquin Valley of California depend on ground water for water supply. Water-level data for 1977-81 show that there has been no significant change in water levels, indicating that during this period, recharge in the Merced area balance natural discharge and withdrawals by pumping. Lithologic logs of shallow test wells drilled around Merced indicate shallow fine-grained material in the aquifer that could interfere with surface artificial recharge to the aquifer system. Short-term and seasonal fluctuations of water levels in wells perforated at different depths and in different aquifers show dissimilar patterns in some areas. The expansion and refinement of the observation-well network will provide a data base for water-management decisions and for assessments of ground-water conditions in the future. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834081","usgsCitation":"Elliott, A.L., 1984, Ground-water conditions and shallow test-well information in the eastern half of Merced County, California, 1977-82: U.S. Geological Survey Water-Resources Investigations Report 83-4081, iv, 56 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834081.","productDescription":"iv, 56 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122975,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4081/report-thumb.jpg"},{"id":55838,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4081/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69c0b3","contributors":{"authors":[{"text":"Elliott, A. 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