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,{"id":9413,"text":"ofr77690 - 1977 - Exploration for ground water to develop energy resources in the semi-arid West","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr77690","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-690","title":"Exploration for ground water to develop energy resources in the semi-arid West","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77690","usgsCitation":"Head, W.J., 1977, Exploration for ground water to develop energy resources in the semi-arid West: U.S. Geological Survey Open-File Report 77-690, 4 leaves :ill. ;27 cm.; (5 p. - PGS), https://doi.org/10.3133/ofr77690.","productDescription":"4 leaves :ill. ;27 cm.; (5 p. - PGS)","costCenters":[],"links":[{"id":141782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8cdc","contributors":{"authors":[{"text":"Head, William J.","contributorId":96686,"corporation":false,"usgs":true,"family":"Head","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":159643,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9594,"text":"ofr77676 - 1977 - Digital model of the Arikaree Aquifer near Wheatland, southeastern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr77676","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-676","title":"Digital model of the Arikaree Aquifer near Wheatland, southeastern Wyoming","docAbstract":"A digital model that mathematically simulates the flow of ground water, approximating the flow system as two-dimensional, has been applied to predict the long-term effects of irrigation and proposed industrial pumping from the unconfined Arikaree aquifer in a 400 square-mile area in southeastern Wyoming. Three cases that represent projected maximum, mean, and minimum combined irrigation and industrial ground-water withdrawals at annual rates of 16,176, 11,168, and 6,749 acre-feet, respectively, were considered. Water-level declines of more than 5 feet over areas of 124, 120, and 98 square miles and depletions in streamflow of 14.4, 8.9, and 7.2 cfs from the Laramie and North Laramie Rivers were predicted to occur at the end of a 40-year simulation period for these maximum, mean, and minimum withdrawal rates, respectively. A tenfold incrase in the vertical hydraulic conductivity that was assumed for the streambeds results in smaller predicted drawdowns near the Laramie and North Laramie Rivers and a 36 percent increase in the predicted depletion in streamflow for the North Laramie River. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77676","usgsCitation":"Hoxie, D.T., 1977, Digital model of the Arikaree Aquifer near Wheatland, southeastern Wyoming: U.S. Geological Survey Open-File Report 77-676, vi, 54 p. :ill., maps ;28 cm.; (88 p. - PGS), https://doi.org/10.3133/ofr77676.","productDescription":"vi, 54 p. :ill., maps ;28 cm.; (88 p. - PGS)","costCenters":[],"links":[{"id":142137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0676/report-thumb.jpg"},{"id":37323,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0676/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db6594f5","contributors":{"authors":[{"text":"Hoxie, Dwight T.","contributorId":77531,"corporation":false,"usgs":true,"family":"Hoxie","given":"Dwight","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":159970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9360,"text":"ofr77221 - 1977 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1975","interactions":[],"lastModifiedDate":"2017-06-14T11:02:47","indexId":"ofr77221","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-221","title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1975","docAbstract":"<p>No abstract available.<br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr77221","usgsCitation":"Harmsen, L., 1977, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1975: U.S. Geological Survey Open-File Report 77-221, 91 p., https://doi.org/10.3133/ofr77221.","productDescription":"91 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":140857,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db607b5c","contributors":{"authors":[{"text":"Harmsen, Lynn","contributorId":19941,"corporation":false,"usgs":true,"family":"Harmsen","given":"Lynn","email":"","affiliations":[],"preferred":false,"id":159542,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43977,"text":"ofr7762 - 1977 - Land use and land cover and associated maps for Eastville, Maryland, Virginia, and North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:10:29","indexId":"ofr7762","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-62","title":"Land use and land cover and associated maps for Eastville, Maryland, Virginia, and North Carolina","language":"ENGLISH","doi":"10.3133/ofr7762","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Land use and land cover and associated maps for Eastville, Maryland, Virginia, and North Carolina: U.S. Geological Survey Open-File Report 77-62, 4 maps., https://doi.org/10.3133/ofr7762.","productDescription":"4 maps.","costCenters":[],"links":[{"id":173755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1432","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":531512,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55109,"text":"wdrWY761 - 1977 - Water resources data, Wyoming, water year 1976; volume 1. Missouri River basin","interactions":[],"lastModifiedDate":"2025-02-21T14:58:51.456678","indexId":"wdrWY761","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WY-76-1","title":"Water resources data, Wyoming, water year 1976; volume 1. Missouri River basin","docAbstract":"<p>Water resources data for the 1976 water year for Wyoming consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of wells. This report, in two volumes, contains discharge records for 226 gaging stations; stage only records for 1 lake; stage and contents for 16 lakes and reservoirs; water quality for 116 gaging stations, 68 ungaged stations, 4 lakes and reservoirs, and 253 wells and springs; and water levels for 48 observation wells. Also included are 111 crest-stage partial-record stations. Additional water data were collected at: various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Wyoming.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWY761","collaboration":"Prepared in cooperation with the State of Wyoming and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Water resources data, Wyoming, water year 1976; volume 1. Missouri River basin: U.S. Geological Survey Water Data Report WY-76-1, ix, 631 p., https://doi.org/10.3133/wdrWY761.","productDescription":"ix, 631 p.","costCenters":[],"links":[{"id":482265,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1976/wy-76-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181830,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1976/wy-76-1/report-thumb.jpg"}],"country":"United States","state":"Wyoming","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-110.048476,40.997555],[-110.121639,40.997101],[-110.125709,40.99655],[-110.237848,40.995427],[-110.250709,40.996089],[-110.375714,40.994947],[-110.500718,40.994746],[-110.539819,40.996346],[-110.715026,40.996347],[-110.750727,40.996847],[-111.046723,40.997959],[-111.046551,41.251716],[-111.0466,41.360692],[-111.046264,41.377731],[-111.045789,41.565571],[-111.045818,41.579845],[-111.046689,42.001567],[-111.047109,42.142497],[-111.047107,42.148971],[-111.047058,42.182672],[-111.047097,42.194773],[-111.047074,42.280787],[-111.04708,42.34942],[-111.046801,42.504946],[-111.046719,42.513118],[-111.046017,42.582723],[-111.043564,42.722624],[-111.044135,42.874924],[-111.043959,42.96445],[-111.043957,42.969482],[-111.043924,42.975063],[-111.044129,43.018702],[-111.044156,43.020052],[-111.044206,43.022614],[-111.044034,43.024581],[-111.044034,43.024844],[-111.044033,43.026411],[-111.044094,43.02927],[-111.043997,43.041415],[-111.044058,43.04464],[-111.044063,43.046302],[-111.044086,43.054819],[-111.044117,43.060309],[-111.04415,43.066172],[-111.044162,43.068222],[-111.044143,43.072364],[-111.044235,43.177121],[-111.044266,43.177236],[-111.044232,43.18444],[-111.044168,43.189244],[-111.044229,43.195579],[-111.044617,43.31572],[-111.045205,43.501136],[-111.045706,43.659112],[-111.04588,43.681033],[-111.046118,43.684902],[-111.046051,43.685812],[-111.04611,43.687848],[-111.046421,43.722059],[-111.046435,43.726545],[-111.04634,43.726957],[-111.046715,43.815832],[-111.046515,43.908376],[-111.046917,43.974978],[-111.047064,43.983467],[-111.047349,43.999921],[-111.049077,44.020072],[-111.048751,44.060403],[-111.048751,44.060838],[-111.048633,44.062903],[-111.048452,44.114831],[-111.049119,44.124923],[-111.049695,44.353626],[-111.049148,44.374925],[-111.049216,44.435811],[-111.049194,44.438058],[-111.048974,44.474072],[-111.055208,44.624927],[-111.055333,44.666263],[-111.055511,44.725343],[-111.056416,44.749928],[-111.056888,44.866658],[-111.055629,44.933578],[-111.056207,44.935901],[-111.055199,45.001321],[-111.044275,45.001345],[-110.785008,45.002952],[-110.761554,44.999934],[-110.750767,44.997948],[-110.705272,44.992324],[-110.552433,44.992237],[-110.547165,44.992459],[-110.48807,44.992361],[-110.402927,44.99381],[-110.362698,45.000593],[-110.342131,44.999053],[-110.324441,44.999156],[-110.28677,44.99685],[-110.199503,44.996188],[-110.110103,45.003905],[-110.026347,45.003665],[-110.025544,45.003602],[-109.99505,45.003174],[-109.875735,45.003275],[-109.798687,45.002188],[-109.75073,45.001605],[-109.663673,45.002536],[-109.574321,45.002631],[-109.386432,45.004887],[-109.375713,45.00461],[-109.269294,45.005283],[-109.263431,45.005345],[-109.103445,45.005904],[-109.08301,44.99961],[-109.062262,44.999623],[-108.621313,45.000408],[-108.578484,45.000484],[-108.565921,45.000578],[-108.500679,44.999691],[-108.271201,45.000251],[-108.249345,44.999458],[-108.238139,45.000206],[-108.218479,45.000541],[-108.14939,45.001062],[-108.000663,45.001223],[-107.997353,45.001565],[-107.911743,45.001292],[-107.750654,45.000778],[-107.608854,45.00086],[-107.607824,45.000929],[-107.49205,45.00148],[-107.351441,45.001407],[-107.13418,45.000109],[-107.125633,44.999388],[-107.105685,44.998734],[-107.084939,44.996599],[-107.074996,44.997004],[-107.050801,44.996424],[-106.892875,44.995947],[-106.888773,44.995885],[-106.263586,44.993788],[-106.024814,44.993688],[-105.928184,44.993647],[-105.914258,44.999986],[-105.913382,45.000941],[-105.848065,45.000396],[-105.076607,45.000347],[-105.038405,45.000345],[-105.025266,45.00029],[-105.019284,45.000329],[-105.01824,45.000437],[-104.765063,44.999183],[-104.759855,44.999066],[-104.72637,44.999518],[-104.665171,44.998618],[-104.663882,44.998869],[-104.470422,44.998453],[-104.470117,44.998453],[-104.250145,44.99822],[-104.057698,44.997431],[-104.055914,44.874986],[-104.056496,44.867034],[-104.055963,44.768236],[-104.055963,44.767962],[-104.055934,44.72372],[-104.05587,44.723422],[-104.055777,44.700466],[-104.055938,44.693881],[-104.05581,44.691343],[-104.055877,44.571016],[-104.055892,44.543341],[-104.055927,44.51773],[-104.055389,44.249983],[-104.054487,44.180381],[-104.054562,44.141081],[-104.05495,43.93809],[-104.055077,43.936535],[-104.055488,43.853477],[-104.055488,43.853476],[-104.055138,43.750421],[-104.055133,43.747105],[-104.054902,43.583852],[-104.054885,43.583512],[-104.05484,43.579368],[-104.055032,43.558603],[-104.054787,43.503328],[-104.054786,43.503072],[-104.054779,43.477815],[-104.054766,43.428914],[-104.054614,43.390949],[-104.054403,43.325914],[-104.054218,43.30437],[-104.053884,43.297047],[-104.053876,43.289801],[-104.053127,43.000585],[-104.052863,42.754569],[-104.052809,42.749966],[-104.052583,42.650062],[-104.052741,42.633982],[-104.052586,42.630917],[-104.052773,42.611766],[-104.052775,42.61159],[-104.052775,42.610813],[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,{"id":26656,"text":"wri7720 - 1977 - Water quality in Rhode River at Smithsonian Institution Pier near Annapolis, Maryland, January 1974 through December 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri7720","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-20","title":"Water quality in Rhode River at Smithsonian Institution Pier near Annapolis, Maryland, January 1974 through December 1975","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri7720","usgsCitation":"Cory, R.L., 1977, Water quality in Rhode River at Smithsonian Institution Pier near Annapolis, Maryland, January 1974 through December 1975: U.S. Geological Survey Water-Resources Investigations Report 77-20, iii, 48 p. :ill., map ;26 cm., https://doi.org/10.3133/wri7720.","productDescription":"iii, 48 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":158208,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9afe","contributors":{"authors":[{"text":"Cory, Robert L.","contributorId":77967,"corporation":false,"usgs":true,"family":"Cory","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196786,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23857,"text":"ofr77740 - 1977 - Analysis of bottom material from the Willamette River, Portland Harbor, Oregon","interactions":[],"lastModifiedDate":"2016-06-21T13:41:24","indexId":"ofr77740","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-740","title":"Analysis of bottom material from the Willamette River, Portland Harbor, Oregon","docAbstract":"<p>The bottom material of the Willamette River, Portland Harbor, was sampled in duplicate on February 1, 1977. Results are reported on the following analyses of the material: immediate and long-term oxygen demand; particle size; percent moisture; residue, loss on ignition; and chemical.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr77740","issn":"0094-9140","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"McKenzie, S.W., 1977, Analysis of bottom material from the Willamette River, Portland Harbor, Oregon: U.S. Geological Survey Open-File Report 77-740, iv, 8 p., https://doi.org/10.3133/ofr77740.","productDescription":"iv, 8 p.","numberOfPages":"15","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":155686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr77740.PNG"},{"id":324119,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0740/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680a80","contributors":{"authors":[{"text":"McKenzie, Stuart W.","contributorId":27841,"corporation":false,"usgs":true,"family":"McKenzie","given":"Stuart","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":190868,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11813,"text":"ofr7756 - 1977 - Ground-water resources and geology of Colquitt County, Georgia","interactions":[],"lastModifiedDate":"2016-12-14T10:12:07","indexId":"ofr7756","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-56","title":"Ground-water resources and geology of Colquitt County, Georgia","docAbstract":"<p>Limestone beds of Eocene, Oligocene, and lower Miocene age, called the principal artesian aquifer, are the chief source of ground water for Colquitt County. Because streams are small, undependable and relatively inaccessible to most users, ground water is the most important source for increased industrial and agricultural water use. Southeast of Moultrie the principal artesian aquifer is very productive, and has transmissivity in excess of 145,000 feet squared per day (13,500 meters squared per day). A structural or paleogeographic feature called the Suwannee strait traverses the county from near the southwest corner to the northeast corner. In this strait, limestone in the principal artesian aquifer is partly replaced by fine-grained clastic sediment, impairing transmissivity and making wells hard to construct. Transmissivity is much lower northwest of the strait than it is southeast, probably because of facies changes in the aquifer.</p>\n<p>In the belt of the hypothesized Ochlockonee fault, water containing greater-than-usual concentrations of dissolved solids is produced. This anomaly could be the result of the fault having acted as a conduit when the vertical hydraulic gradient was upward from a deeper aquifer, or be the result of the movement of ground water from a sulfate-rich source in the sediments of the Suwannee strait. In south-central Colquitt County, clay-capped permeable beds extending above potentiometric surfaces create conditions favorable for breathing wells.</p>\n<p>Predominantly clastic beds of Miocene age overlie the Suwannee Limestone. These beds have a transmissivity of about 2,280 feet squared per day (215 meters squared per day), but they are of comparatively little importance because larger yields can be obtained from the underlying principal artesian aquifer. Moreover, wells are difficult to construct in the poorly consolidated clastic sediments, and water from these shallow beds is likely to be depleted during droughts.</p>\n<p>The ground water is generally hard, but is otherwise of good quality. One exception is near the hypothesized Ochlockonee fault where water contains higher-than-usual concentrations of various ions, especially sulfate. Another exception occurs along the axis of the Suwannee strait where clay minerals in the channel facies may soften the water by ion exchange.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Doraville, Georgia","doi":"10.3133/ofr7756","collaboration":"Prepared in cooperation with Georgia Department of Natural Resources, Geologic and Water Resources Division","usgsCitation":"Zimmerman, E.A., 1977, Ground-water resources and geology of Colquitt County, Georgia: U.S. Geological Survey Open-File Report 77-56, vi, 41 p., https://doi.org/10.3133/ofr7756.","productDescription":"vi, 41 p.","numberOfPages":"52","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":144821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr7756.jpg"},{"id":325511,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","county":"Colquitt 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E. A.","contributorId":75533,"corporation":false,"usgs":true,"family":"Zimmerman","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":163774,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43574,"text":"ofr7713 - 1977 - Land use and land cover and associated maps for Seattle, Washington (covers western 50% of the Seattle map sheet only; east 50% will be covered by 1:100,000-scale map sheet)","interactions":[],"lastModifiedDate":"2012-02-02T00:11:05","indexId":"ofr7713","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-13","title":"Land use and land cover and associated maps for Seattle, Washington (covers western 50% of the Seattle map sheet only; east 50% will be covered by 1:100,000-scale map sheet)","language":"ENGLISH","doi":"10.3133/ofr7713","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Land use and land cover and associated maps for Seattle, Washington (covers western 50% of the Seattle map sheet only; east 50% will be covered by 1:100,000-scale map sheet): U.S. Geological Survey Open-File Report 77-13, 4 maps., https://doi.org/10.3133/ofr7713.","productDescription":"4 maps.","costCenters":[],"links":[{"id":168580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af332","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":531249,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27572,"text":"wri7716 - 1977 - Application of thermal imagery and aerial photography to hydrologic studies of karst terrane in Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:08:43","indexId":"wri7716","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-16","title":"Application of thermal imagery and aerial photography to hydrologic studies of karst terrane in Missouri","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri7716","usgsCitation":"Harvey, E., Williams, J., and Dinkel, T., 1977, Application of thermal imagery and aerial photography to hydrologic studies of karst terrane in Missouri: U.S. Geological Survey Water-Resources Investigations Report 77-16, vi, 58 p. :ill., maps ;26 cm., https://doi.org/10.3133/wri7716.","productDescription":"vi, 58 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":95644,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0016/report.pdf","size":"7607","linkFileType":{"id":1,"text":"pdf"}},{"id":158910,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0016/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a5be","contributors":{"authors":[{"text":"Harvey, E.J.","contributorId":47416,"corporation":false,"usgs":true,"family":"Harvey","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":198352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, J.H.","contributorId":29482,"corporation":false,"usgs":true,"family":"Williams","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":198350,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dinkel, T.R.","contributorId":34555,"corporation":false,"usgs":true,"family":"Dinkel","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":198351,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26982,"text":"wri7711 - 1977 - Artificial-recharge tests in Upper Black Squirrel Creek basin, Jimmy Camp Valley, and Fountain Valley, El Paso County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri7711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-11","title":"Artificial-recharge tests in Upper Black Squirrel Creek basin, Jimmy Camp Valley, and Fountain Valley, El Paso County, Colorado","docAbstract":"Artificial-recharge tests were conducted in the alluvium in upper Black Squirrel Creek basin, the alluvium in Jimmy Camp Valley, and in the alluvium overlying the Widefield aquifer which is located in an ancestral channel in Fountain Valley, Colo. Nine artificial-recharge pits with areas of approximately 9,200 square feet each were excavated in the unsaturated zones above the three aquifers. Each artificial-recharge site was instrumented to measure inflow, stage fluctuations, and water-table fluctuations. Artificial-recharge tests of approximately 10 days ' duration were conducted at each of the nine artificial-recharge sites and one extended test of approximately 30 days ' duration was conducted in each of the three study areas. Periphyton growth, present in most of the artificial-recharge ponds, was insufficient to cause noticeable decline in the rate of infiltration. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri7711","usgsCitation":"Emmons, P., 1977, Artificial-recharge tests in Upper Black Squirrel Creek basin, Jimmy Camp Valley, and Fountain Valley, El Paso County, Colorado: U.S. Geological Survey Water-Resources Investigations Report 77-11, iv, 49 p. :ill., maps ;26 cm., https://doi.org/10.3133/wri7711.","productDescription":"iv, 49 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":123461,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0011/report-thumb.jpg"},{"id":55869,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0011/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c6b","contributors":{"authors":[{"text":"Emmons, P.J.","contributorId":60630,"corporation":false,"usgs":true,"family":"Emmons","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":197358,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9748,"text":"ofr77433 - 1977 - Nitrogen in water in Nassau and Suffolk counties, Long Island, New York, in 1971","interactions":[],"lastModifiedDate":"2012-02-02T00:06:06","indexId":"ofr77433","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-433","title":"Nitrogen in water in Nassau and Suffolk counties, Long Island, New York, in 1971","docAbstract":"The concentration of inorganic nitrogen was measured in samples from 521 wells in the upper glacial and Magothy aquifers and from 46 streams in Nassau and Suffolk Counties during May 1971. The predominant form of dissolved nitrogen was nitrate. Nitrate concentrations (as N) in the upper glacial aquifer in both counties ranged from 0 to 20 milligrams per liter (mg/L) ; those in the Magothy aquifer ranged from 0 to 20 mg/L but were generally much lower in Suffolk County than in Nassau County. Nitrate concentrations (as N) decreased with depth in both counties; below 400 feet, concentrations ranged from 0 to 0.2 mg/L. \r\n\r\nNitrate concentrations (as N) of streams ranged from 0 to ii mg/L, which is an indication of the general quality of water in much of the upper glacial aquifer, the source of most of the streamflow. Generally, concentrations of total nitrogen in streams draining the sewered area of Nassau County were lower than those in streams draining the unsewered area. Median concentrations of total inorganic nitrogen (as N) were 1.3 mg/L for the sewered area and 7.5 mg/L for the unsewered area. About 5,500 pounds of nitrate (as N) was estimated to be discharged daily in surface flow to tidewater from Nassau and Suffolk Counties.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77433","usgsCitation":"Katz, B.G., Ragone, S.E., and Harr, C.A., 1977, Nitrogen in water in Nassau and Suffolk counties, Long Island, New York, in 1971: U.S. Geological Survey Open-File Report 77-433, 46 leaves :maps (some fold. in envelope) ;29 cm., https://doi.org/10.3133/ofr77433.","productDescription":"46 leaves :maps (some fold. in envelope) ;29 cm.","costCenters":[],"links":[{"id":141242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0433/report-thumb.jpg"},{"id":37493,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0433/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37494,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0433/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37495,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0433/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37496,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0433/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37497,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0433/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697288","contributors":{"authors":[{"text":"Katz, Brian G. bkatz@usgs.gov","contributorId":1093,"corporation":false,"usgs":true,"family":"Katz","given":"Brian","email":"bkatz@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":160227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ragone, Stephen E.","contributorId":74374,"corporation":false,"usgs":true,"family":"Ragone","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160229,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harr, C. Albert","contributorId":28978,"corporation":false,"usgs":true,"family":"Harr","given":"C.","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":160228,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9415,"text":"ofr77706 - 1977 - Geochemistry and mineralogy of the carbonates of the Creede mining district, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr77706","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-706","title":"Geochemistry and mineralogy of the carbonates of the Creede mining district, Colorado","docAbstract":"This paper describes the results of a study of the carbonate gangue in the silver-base metal ore deposit of the Creede mining district, located in Tertiary volcanic rocks of the central San Juan Mountains, southwestern Colorado. Two carbonate stages can be distinguished and defined on the basis of mineral association, compositional range and position in the sequence of ore deposition. Electron microprobe analyses show that the early pre-ore carbonate stage is comprised of rhodochrosite with a compositional range of 68 to 93 mole percent MnCO3, 7 to 32 mole percent FeCO3, 2 to 15 mole percent CaCO3, and 0.5 to 4 mole percent MgCO3. The later intra-ore carbonate stage is made up of siderite-manganosiderite with a broad range of iron content (33 to 94 mole percent FeCO3; 6 to 67 mole percent MnCO3; 1 to 13 mole percent CaCO3; and 1 to 10 mole percent MgCO3). Both carbonate stages are spatially restricted within the vein system, the rhodochrosite limited to the southern third and the siderite limited to the northern two-thirds. The two stages have not been found at the same sample locality. \r\n\r\nThe two stages of carbonate define two of the five main depositional stages in the history of the Creede hydrothermal system and thereby document broad scale variations within the depositing, and continually evolving fluids. However, the complexity of the textural and mineralogical variations within each carbonate stage limits their usefulness in unraveling the finer details of the character of the ore fluids. The frequently massive rhodochroslte has undergone several periods of leaching and regrowth which, except at one locality, cannot be resolved by compositional, textural or color variations. Although some compositionally zoned siderite rhombs have been documented, the siderite, too, has had a complicated history of leaching and regrowth. The zoning indicates (i) an early low-calcium siderite + hematite growth followed by (2) relatively high-calcium siderite depositlon (without hematite) followed by (3) low-calcium siderite deposition without hematite. The composition of the high-calcium siderite lies well outside of the recognized stability field for siderite at 250?C and, therefore, is considered either a metastable phase or possibly a new mineral. \r\n\r\nCarbon and oxygen isotopic compositions of the carbonates together with the hydrogen isotopic composition of inclusion fluids suggest that the fluids depositing the carbonates either were deep-seated in origin, or, less likely, were meteoric waters which came in contact with a large volume of magmatic rock with which it exchanged isotopes. The oxygen and hydrogen isotopic compositions of the fluids that deposited the carbonates are significantly different from those that yielded the other vein minerals (sphalerite, chlorite, sericite, quartz, adularla). The latter minerals appear to-have been deposited from two distinctive fluids of meteoric origin. The stability fields of minerals present during the carbonate stages have been calculated for 250?Co The results indicate that conditions during carbonate deposition were not drastically different from those suggested by Barton and others (1977) for main-stage ore deposition, although little ore, if any, was deposited during the carbonate stages. A new value for the free energy of formation of siderite was calculated since all of the most recently published values predict too small a stability field for the siderite based on the occurrence of siderite at Creede, The change to the more iron-rich composition of the later stage carbonate was probably controlled by the pyrite-chlorite buffer which was not present during early-stage carbonate deposition.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr77706","usgsCitation":"Wetlaufer, P.H., 1977, Geochemistry and mineralogy of the carbonates of the Creede mining district, Colorado: U.S. Geological Survey Open-File Report 77-706, x, 134 leaves :ill. (1 fold. in pocket) maps ;28 cm., https://doi.org/10.3133/ofr77706.","productDescription":"x, 134 leaves :ill. (1 fold. in pocket) maps ;28 cm.","costCenters":[],"links":[{"id":141799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0706/report-thumb.jpg"},{"id":37124,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1977/0706/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37125,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0706/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab712","contributors":{"authors":[{"text":"Wetlaufer, Pamela Heald","contributorId":35317,"corporation":false,"usgs":true,"family":"Wetlaufer","given":"Pamela","email":"","middleInitial":"Heald","affiliations":[],"preferred":false,"id":159647,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9067,"text":"ofr77758 - 1977 - A proposal for studies of the water resources of the Mescalero Apache Indian Reservation, Otero County, Mew Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr77758","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-758","title":"A proposal for studies of the water resources of the Mescalero Apache Indian Reservation, Otero County, Mew Mexico","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr77758","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, A proposal for studies of the water resources of the Mescalero Apache Indian Reservation, Otero County, Mew Mexico: U.S. Geological Survey Open-File Report 77-758, 20 leaves :maps (1 fold.) ;27 cm.; (17 p., 3 sheets - PGS), https://doi.org/10.3133/ofr77758.","productDescription":"20 leaves :maps (1 fold.) ;27 cm.; (17 p., 3 sheets - PGS)","costCenters":[],"links":[{"id":94907,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1977/0758/report.pdf","size":"7433","linkFileType":{"id":1,"text":"pdf"}},{"id":143572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1977/0758/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d57","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":528895,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25858,"text":"wri7784 - 1977 - Water resources inventory of northwest Florida","interactions":[],"lastModifiedDate":"2019-07-22T10:44:04","indexId":"wri7784","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-84","title":"Water resources inventory of northwest Florida","docAbstract":"Water resources of the 16 counties of the northwest Florida appear adequate unitl at least 2020. In the 4 westernmost counties, the sand-and-gravel aquifer and streams combined could provide 2,200 to 3,600 million gallons per day of water. Streams outside these counties could provide 5,600 million gallons per day. The Floridan aquifer could provide 220 million gallons per day. Generally, water of quality suitable for most purposes is available throughout the area, although water in smaller streams and in the sand-and-gravel aquifer is acidic and locally contains excessive iron. Water in the upper part of the Floridan aquifer is generally fresh, but saline at depth and in some coastal areas. The quantity of water available in the study area is about 8,020 to 9,420 million gallons per day and projected needs for the year 2020 range from 2,520 to 4,130 million gallons per day. ' Approximate method ' flood-prone area maps cover most of the area. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7784","usgsCitation":"Dysart, J., Pascale, C., and Trapp, H., 1977, Water resources inventory of northwest Florida: U.S. Geological Survey Water-Resources Investigations Report 77-84, v, 114 p. , https://doi.org/10.3133/wri7784.","productDescription":"v, 114 p. ","costCenters":[],"links":[{"id":365763,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0084/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158288,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0084/report-thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.659912109375,\n              29.554345125748267\n            ],\n            [\n              -83.880615234375,\n              29.554345125748267\n            ],\n            [\n              -83.880615234375,\n              31.043521630684204\n            ],\n            [\n              -87.659912109375,\n              31.043521630684204\n            ],\n            [\n              -87.659912109375,\n              29.554345125748267\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f09ff","contributors":{"authors":[{"text":"Dysart, J.E.","contributorId":23939,"corporation":false,"usgs":true,"family":"Dysart","given":"J.E.","affiliations":[],"preferred":false,"id":195370,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pascale, C.A.","contributorId":68724,"corporation":false,"usgs":true,"family":"Pascale","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":195371,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trapp, Henry","contributorId":107693,"corporation":false,"usgs":true,"family":"Trapp","given":"Henry","affiliations":[],"preferred":false,"id":195372,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27262,"text":"wri7727 - 1977 - Low-flow characteristics at gaging stations on the Wisconsin, Fox, and Wolf rivers, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-21T10:32:44","indexId":"wri7727","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-27","title":"Low-flow characteristics at gaging stations on the Wisconsin, Fox, and Wolf rivers, Wisconsin","docAbstract":"<p>Low-flow characteristics are presented at eleven gaging stations on the main stem of the Wisconsin, Fox, and Wolf Rivers in this report. The low-flow characteristics presented are the annual minimum 7-day mean flow below which the flow will fall on the average of once in 2 years (Q7, 2) and the annual minimum 7-day mean flow below which the flow will fall on the average of once in 10 years (Q7, I0).</p>\n<p>To provide accurate and consistent low-flow characteristics for uniform evaluation of waste effluent, a long-term period of streamflow record was used for the analyses. The record selected for the study was 1915-75. This was found to be the most representative that included longterm streamflow conditions and various degrees of regulation by storage reservoirs.</p>\n<p>The Q7, 10 discharge on the Wisconsin River ranged from lUO cubic feet per second at the Wisconsin River at Rainbow Lake near Lake Tomahawk gaging station to 2,790 cubic feet per second at the Wisconsin River at Muscoda gaging station. On the Fox-Wolf Rivers, the Q7, 10 ranged from 360 cubic feet per second at Fox River at Berlin to 950 cubic feet per second at Fox River at Rapide Croche dam near Wrightstown.</p>\n<p>Low-flow characteristics that reflect unregulated and regulated conditions on the upper Wisconsin River were compared. This analysis showed no apparent difference in Q7, 10 discharge values due to regulation at the Wisconsin River at Merrill gaging station, although a more detailed study is warranted to fully evaluate the effect of storage.</p>\n<p>The magnitude of the low-flow characteristics are in some instances affected by the period of record. These characteristics can vary as much as &plusmn;30 percent at some gaging stations depending on whether or not the severe drought of the 1930's was included in the analysis.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7727","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Gebert, W., and Holmstrom, B.K., 1977, Low-flow characteristics at gaging stations on the Wisconsin, Fox, and Wolf rivers, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 77-27, iii, 20 p., https://doi.org/10.3133/wri7727.","productDescription":"iii, 20 p.","numberOfPages":"26","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":119849,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0027/report-thumb.jpg"},{"id":56137,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0027/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","otherGeospatial":"Fox River, Wisconsin River, Wolf 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,{"id":27035,"text":"wri76113 - 1977 - Ground-water resources of the Lexington, Kentucky, area","interactions":[],"lastModifiedDate":"2019-08-05T11:08:25","indexId":"wri76113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"76-113","title":"Ground-water resources of the Lexington, Kentucky, area","docAbstract":"Ground water in the Lexington, Kentucky, area occurs in Ordovician Limestones in which cavity development is generally limited to about 100 feet below land surface. Some wells produce about 300 gallons per minute in some of the large stream valleys , about 50 gallons per minute in the rolling upland and small stream valleys, and about 5 gallons per minute on hilltops and steep slopes. Many wells throughout the area do not furnish adequate water for domestic supplies because no significant water-bearing openings are penetrated during drilling. Ground-water use is limited mostly to domestic and stock supplies and a few small public supplies. Ground water is generally a calcium bicarbonate type and in places contains sodium chloride and (or) hydrogen sulfide. Bacterial pollution of ground water is widespread because of direct recharge of polluted runoff and streamflow to cavernous limestones. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri76113","usgsCitation":"Faust, R., 1977, Ground-water resources of the Lexington, Kentucky, area: U.S. Geological Survey Water-Resources Investigations Report 76-113, Report: v, 24 p.; 4 Plates: 13.94 x 16.79 inches or smaller , https://doi.org/10.3133/wri76113.","productDescription":"Report: v, 24 p.; 4 Plates: 13.94 x 16.79 inches or smaller ","costCenters":[],"links":[{"id":366227,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0113/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366228,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0113/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366229,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0113/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366230,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0113/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366231,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0113/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158624,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0113/report-thumb.jpg"}],"country":"United States","state":"Kentucky","city":"Lexington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.605712890625,\n              37.965854128749434\n            ],\n            [\n              -84.3804931640625,\n              37.965854128749434\n            ],\n            [\n              -84.3804931640625,\n              38.09998264736481\n            ],\n            [\n              -84.605712890625,\n              38.09998264736481\n            ],\n            [\n              -84.605712890625,\n              37.965854128749434\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a92e4b07f02db657904","contributors":{"authors":[{"text":"Faust, R.J.","contributorId":80700,"corporation":false,"usgs":true,"family":"Faust","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":197446,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64713,"text":"i1012 - 1977 - Leasable mineral and waterpower land classification map of the Choteau 1° x 2° quadrangle, Montana","interactions":[{"subject":{"id":46366,"text":"ofr74169 - 1974 - Leasable mineral and waterpower land classification map, Choteau Quadrangle, Montana, showing lands withdrawn, classified, and valuable prospectively for leasable minerals and occurrences of other selected minerals, lands withdrawn or classified for waterpower and reservoir sites","indexId":"ofr74169","publicationYear":"1974","noYear":false,"title":"Leasable mineral and waterpower land classification map, Choteau Quadrangle, Montana, showing lands withdrawn, classified, and valuable prospectively for leasable minerals and occurrences of other selected minerals, lands withdrawn or classified for waterpower and reservoir sites"},"predicate":"SUPERSEDED_BY","object":{"id":64713,"text":"i1012 - 1977 - Leasable mineral and waterpower land classification map of the Choteau 1° x 2° quadrangle, Montana","indexId":"i1012","publicationYear":"1977","noYear":false,"title":"Leasable mineral and waterpower land classification map of the Choteau 1° x 2° quadrangle, Montana"},"id":1}],"lastModifiedDate":"2021-11-01T21:14:21.530942","indexId":"i1012","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"1012","title":"Leasable mineral and waterpower land classification map of the Choteau 1° x 2° quadrangle, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1012","usgsCitation":"Bateman, A., and Lutz, G.A., 1977, Leasable mineral and waterpower land classification map of the Choteau 1° x 2° quadrangle, Montana: U.S. Geological Survey IMAP 1012, 1 Plate: 32.78 × 23.32 inches, https://doi.org/10.3133/i1012.","productDescription":"1 Plate: 32.78 × 23.32 inches","costCenters":[],"links":[{"id":391238,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8884.htm"},{"id":255148,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1012/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1012/report-thumb.jpg"},{"id":255147,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1012/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Montana","otherGeospatial":"Choteau 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,47 ], [ -114,48 ], [ -112,48 ], [ -112,47 ], [ -114,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a87d3","contributors":{"authors":[{"text":"Bateman, A. F. Jr.","contributorId":24411,"corporation":false,"usgs":true,"family":"Bateman","given":"A. F.","suffix":"Jr.","affiliations":[],"preferred":false,"id":272027,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lutz, G. A.","contributorId":71604,"corporation":false,"usgs":true,"family":"Lutz","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":272028,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3474,"text":"cir767 - 1977 - Current oil and gas production from North American Upper Cretaceous chalks","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"cir767","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"767","title":"Current oil and gas production from North American Upper Cretaceous chalks","docAbstract":"Production of oil and natural gas from North American chalks has increased significantly during the past five years, spurred by the prolific production from North Sea chalks, as well as by higher prices and improved production technology. Chalk reservoirs have been discovered in the Gulf Coast in the Austin Group, Saratoga and Annona Chalks, Ozan Formation, Selma Group, Monroe gas rock (an informal unit of Navarro age), and other Upper Cretaceous units. In the Western Interior, production has been obtained from the Cretaceous Niobrara and Greenhorn Formations. Significant, though subcommercial, discoveries of natural gas and gas condensate also have been made in the Upper Cretaceous Wyandot Formation on the Scotian Shelf of eastern Canada. \r\n\r\nAll North American chalk units share a similar depositional and diagenetic history. The chalks consist primarily of whole and fragmented coccoliths with subordinate planktonic and benthonic Foraminifera, inoceramid prisms, oysters, and other skeletal grains. Most have between 10 and 35 percent HCl-insoluble residue, predominantly clay. Deposition was principally below wave base in tens to hundreds of meters of water. \r\n\r\nThe diagenetic history of a chalk is critical in determining its reservoir potential. All chalk has a stable composition (low-Mg calcite) and very high primary porosity. With subsequent burial, mechanical and chemical (solution-transfer) compaction can reduce or completely eliminate pore space. The degree of loss of primary porosity in chalk sections is normally a direct function of the maximum depth to which it has been buried. Pore-water chemistry, pore-fluid pressures, and tectonic stresses also influence rates of cementation. Oil or gas reservoirs of North American chalk fall into three main groups: \r\n\r\n1. Areas with thin overburden and significant primary porosity retention (for example, Niobrara Formation of Kansas and eastern Colorado). \r\n\r\n2. Areas with thicker overburden but considerable fracturing. Here primary porosity has been largely lost but secondary (fracture) porosity provides some storage capacity and greatly improves permeability (for example, Austin Group of the Pearsall field, Texas). \r\n\r\n3. Areas with thick overburden in which marine pore fluids have been retained, or where hydrocarbons (including biogenically generated methane) were introduced early in the diagenetic history. \r\n\r\nIn these settings, primary porosity is reduced to a lesser degree than in group two, and adequate reservoir properties can be maintained to depths approaching 2,000 m (6,600 ft) (for example, Scotian Shelf of Canada). \r\n\r\nContinued small-scale oil and gas discoveries can be expected from these types of reservoirs in North America. The prolific production of oil and gas from North Sea chalk reservoirs will not be matched in North America unless deeply buried, overpressured chalks can be located. It is the early formation of overpressures and (or) early oil input into North Sea chalks that have preserved porosities as high as 40 percent at 3,000- to 3,500-m (9,800- to 11,500-ft) depths and provided the outstanding reservoir capacity of those chalks.","language":"ENGLISH","publisher":"Dept. of the Interior, Geological Survey,","doi":"10.3133/cir767","usgsCitation":"Scholle, P.A., 1977, Current oil and gas production from North American Upper Cretaceous chalks: U.S. Geological Survey Circular 767, iv, 51 p. :ill., maps ;26 cm. , https://doi.org/10.3133/cir767.","productDescription":"iv, 51 p. :ill., maps ;26 cm. ","costCenters":[],"links":[{"id":126710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1977/0767/report-thumb.jpg"},{"id":30485,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1977/0767/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ec52","contributors":{"authors":[{"text":"Scholle, Peter A.","contributorId":48954,"corporation":false,"usgs":true,"family":"Scholle","given":"Peter","email":"","middleInitial":"A.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":146992,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25891,"text":"wri7751 - 1977 - Sources of emergency water supplies in Santa Clara County, California","interactions":[],"lastModifiedDate":"2019-07-22T12:11:56","indexId":"wri7751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-51","title":"Sources of emergency water supplies in Santa Clara County, California","docAbstract":"Water distribution systems in Santa Clara County, Calif., may be damaged and rendered inoperable by a large earthquake or other disaster. In such an event, individual agencies may have to implement emergency measures to supply water for drinking, firefighting, decontamination, or other purposes. In Santa Clara County, 128 wells have been identified as potential water-supply sources in emergencies. The criteria used to select the wells are: yield of at least 3 liters per second (50 gallons per minute), good water quality, ready accessibility, and available emergency power. Purification methods of small water supplies are described. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7751","usgsCitation":"Akers, J.P., 1977, Sources of emergency water supplies in Santa Clara County, California: U.S. Geological Survey Water-Resources Investigations Report 77-51, Report: iv, 21 p.; 1 Plate: 32.13 x 27.16 inches, https://doi.org/10.3133/wri7751.","productDescription":"Report: iv, 21 p.; 1 Plate: 32.13 x 27.16 inches","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":365787,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0051/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365788,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0051/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158545,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0051/report-thumb.jpg"}],"country":"United 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P.","contributorId":82678,"corporation":false,"usgs":true,"family":"Akers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":195430,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43127,"text":"ofr7717 - 1977 - Land use and land cover and associated maps for Port Townsend, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:01","indexId":"ofr7717","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-17","title":"Land use and land cover and associated maps for Port Townsend, Washington","language":"ENGLISH","doi":"10.3133/ofr7717","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1977, Land use and land cover and associated maps for Port Townsend, Washington: U.S. Geological Survey Open-File Report 77-17, 5 maps ;56 x 75 cm., https://doi.org/10.3133/ofr7717.","productDescription":"5 maps ;56 x 75 cm.","costCenters":[],"links":[{"id":135568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6afc02","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":530977,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25561,"text":"wri77120 - 1977 - Ground-water resources of the Upper Winooski River basin, Vermont","interactions":[],"lastModifiedDate":"2015-10-21T11:21:49","indexId":"wri77120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-120","title":"Ground-water resources of the Upper Winooski River basin, Vermont","docAbstract":"<p>Ground water in the upper Winooski River basin, Vermont, occurs in bedrock and in overlying unconsolidated deposits of glacial origin. Bedrock in the area is composed of a series of metamorphic and igneous rocks. Median yield for 126 wells in four different bedrock formations ranges from 5 to 6 gallons per minute, and median depth ranges from 130 to 200 feet. Lineaments, interpreted as fracture of breakage zones in bedrock, were mapped to identify zones where well yields are expected to be higher than average.</p>\n<p>Unconsolidated deposits in the upper Winooski River basin include unsorted till, water-sorted clay, silt, sand, and gravel. Properly constructed wells in saturated deposits of sand or gravel having high permeability can yield large quantities of water. Twenty-six domestic wells in these unconsolidated deposits have a median yield of 18 gallons per minute and a median depth of 58 feet.</p>\n<p>Chemical analysis of water from six wells indicate a median hardness of 120 milligrams per liter, (as CaCO<sub>3</sub>), which is moderately hard. Iron and manganese are common constituents of ground water in the area, and several analyses show concentrations of these elements which exceed recommended National Academy of Sciences and National Academy of Engineering (1973) limits for public drinking water supplies.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri77120","collaboration":"Prepared in cooperation with the State of Vermont, Agency of Environmental Conservation, Department of Water Resources","usgsCitation":"Hodges, A.L., Willey, R.E., Ashley, J.W., and Butterfield, D., 1977, Ground-water resources of the Upper Winooski River basin, Vermont: U.S. Geological Survey Water-Resources Investigations Report 77-120, Report: iv, 27 p.; 4 Plates: 33.88 x 42.89 inches or smaller, https://doi.org/10.3133/wri77120.","productDescription":"Report: iv, 27 p.; 4 Plates: 33.88 x 42.89 inches or smaller","numberOfPages":"34","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":310270,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0120/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310271,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0120/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":310272,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0120/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":310273,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0120/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":310274,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1977/0120/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":157665,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri77120.PNG"}],"country":"United States","state":"Vermont","otherGeospatial":"Upper Winooski River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.92724609375,\n              44.15856343854312\n            ],\n            [\n              -72.92724609375,\n              44.49650533109348\n            ],\n            [\n              -72.11975097656249,\n              44.49650533109348\n            ],\n            [\n              -72.11975097656249,\n              44.15856343854312\n            ],\n            [\n              -72.92724609375,\n              44.15856343854312\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db649202","contributors":{"authors":[{"text":"Hodges, Arthur L. 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,{"id":26262,"text":"wri77107 - 1977 - Preliminary digital model of the Arikaree aquifer in the Sweetwater River basin, central Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:02:05","indexId":"wri77107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1977","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":"77-107","title":"Preliminary digital model of the Arikaree aquifer in the Sweetwater River basin, central Wyoming","docAbstract":"In central Wyoming, Potentially large supplies of ground water are available in the Sweetwater River basin from the Arikaree aquifer, which consists of the upper part of the White River, the Arikaree, and the Ogallala Formations. A preliminary digital model was developed for the Arikaree aquifer using a small amount of poorly distributed data, an estimated distribution of recharge, and a conceptual model of the Arikaree aquifer flow system. Calibration of the model was based on reproduction of the potentiometric surface and the base flow of the Sweetwater River in November 1975. Calculated steady-state hydraulic heads were within 50 feet of the observed heads in about 98 percent of the nodes. The calculated leakage from the Arikaree aquifer to he Sweetwater River in the western area was within about 12 percent of the leadage determined by gain and loss studies. In order to develop a comprehensive digital model that would respond to hydraulic stress in nearly the same manner as the actual aquifer flow system, measured responses of the aquifer to stress are needed. Also needed are additional data on aquifer characteristics, recharge to the aquifer, and stream-aquifer relationships. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri77107","usgsCitation":"Borchert, W.B., 1977, Preliminary digital model of the Arikaree aquifer in the Sweetwater River basin, central Wyoming (WRI/OFR): U.S. Geological Survey Water-Resources Investigations Report 77-107, iii, 19 p. :maps (some fold. in pocket) ;27 cm. --, https://doi.org/10.3133/wri77107.","productDescription":"iii, 19 p. :maps (some fold. in pocket) ;27 cm. --","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":157796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0107/report-thumb.jpg"},{"id":55073,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6692c9","contributors":{"authors":[{"text":"Borchert, W. B.","contributorId":34965,"corporation":false,"usgs":true,"family":"Borchert","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":196078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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