{"pageNumber":"6813","pageRowStart":"170300","pageSize":"25","recordCount":184828,"records":[{"id":52131,"text":"ofr60123 - 1960 - Marine geology and bathymetry of nearshore shelf of Chukchi Sea, Ogotoruk Creek area, northwest Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:11:28","indexId":"ofr60123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-123","title":"Marine geology and bathymetry of nearshore shelf of Chukchi Sea, Ogotoruk Creek area, northwest Alaska","docAbstract":"During July and August 1958 the U.S. Geological Survey conducted a study in behalf of the Atomic Energy Commission of the oceanography, bathymetry, and marine geology of the nearshore shelf of the Chukchi Sea off the Ogotoruk Creek area, northwest Alaska. Ogotoruk Creek enters the Chukchi Sea about 32 miles southeast of the large cuapate spit of Point Hope at long 165 degrees 44\u001946\u001D W. and lat 68 degrees 05\u001951\u001D N. The Ogotoruk Creek area extends approximately 10 miles west and 7 miles east of the creek mouth. Knowledge of the marine geology and oceanography is confined primarily to the nearshore shelf, which includes about 70 square miles of the shelf and is defined as the sea floor lying shoreward of the 50-foot submarine contour. The 50-foot contour generally lies from 2 to 4 miles from shore. Submarine topography was studied to a distance of 15 miles from shore over an area of approximately 340 square miles.\r\n\r\nA northwest coastal current flows past the Ogotoruk Creek area and during July and August averaged 0.5 mile per hour. Persistent northerly winds cause general upwelling near shore and at times of pronounced upwelling the coastal current was reversed or appreciably reduced in speed. Longshore currents shoreward of the breaker zone averaged 0.3 mile per hour and moved to the east for the greater part of the time of the study.\r\n\r\nThe overall seaward slope of the inner 15 miles of the Chukchi shelf from a depth of 40 to 135 feet is approximately 0 degrees 04\u0019, or about 6 feet per mile. Slopes near shore to depths of 15-20 feet are steep and average 2 degrees 30\u0019. Beyond these depths they increase gradually out to a depth of 40-45 feet. Seaward of this point the shelf is flattest and slopes are as low as 0 degree 01\u0019. This terrace or flat part of the nearshore shelf is about 2 miles wide and descends to a depth of 50-55 feet beyond which the gradient increases to about 0 degree 06\u001D. At depths greater than 85 feet the submarine declivity gradually decreases to 0 degree 03\u0019 at a distance of 15 miles from shore.\r\n\r\nA flat-bottomed trough, Ogotoruk Seavalley, heads about a quarter of a mile from shore off the mouth of Ogotoruk Creek. The shallow seavalley averages only 6 feet in relief and extends 15 miles from shore to a depth of 135 feet. A number of smaller channels also indent the gentle sloping inner Chukchi shelf east of the seavalley and nearshore west of it.\r\n\r\nMany outcrops of Paleozoic and Mesozoic formations on the nearshore shelf indicate that it is a wave-planed platform. Wave planation is thought to have taken place primarily in Sangamon and rpre-Sangamon time (approximately 100,000 to 1,000,000 years ago). Ogotoruk Seavalley is believed to be a drowned subaerial valley which was excavated by Ogotoruk Creek during periods of glacially depressed sea level.\r\n\r\nUnconsolidated sediments overlying the nearshore shelf are chiefly slightly rounded residual gravel which have been derived from submerged outcrops. Detrital sand and silt, contributed from the nearby coastal area during Recent time, overlie the shelf near shore and at depth as much as 50 feet seaward of segments of the coast underlain by fine-grained clastic rocks of Mesozoic age. Owing to a small volume of detrital clasts contributed by the coastal area detrital sedimentation is not prominent over the nearshore shelf.\r\n\r\nBeaches fronting the Ogotoruk Creek area are 30-260 feet wide, range from less than 10 to about 25 feet thick, and are composed of sandy gravel having a median diameter of about 10 mm. Rounded clasts of greywacke, siltstone, limestone, and chert are the principal constituents of the gravel. Longshore currents accompanying moderate storms transport gravel and sand parallel to shore at rates of 5 cubic yards per hour. Sediment transported by longshore currents accumulates as spits at stream mouths and as areas of new beach below rocky headlands.","language":"ENGLISH","doi":"10.3133/ofr60123","usgsCitation":"Scholl, D., and Sainsbury, C., 1960, Marine geology and bathymetry of nearshore shelf of Chukchi Sea, Ogotoruk Creek area, northwest Alaska: U.S. Geological Survey Open-File Report 60-123, 58 p., https://doi.org/10.3133/ofr60123.","productDescription":"58 p.","costCenters":[],"links":[{"id":178881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1960/0123/report-thumb.jpg"},{"id":86665,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1960/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606c21","contributors":{"authors":[{"text":"Scholl, D.W.","contributorId":106461,"corporation":false,"usgs":true,"family":"Scholl","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":244851,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":244850,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":76957,"text":"tem836C - 1960 - \"Granite\" exploration hole, Area 15, Nevada Test Site, Nye County, Nevada : interim report, Part C, physical properties","interactions":[],"lastModifiedDate":"2012-02-02T00:14:09","indexId":"tem836C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"836","chapter":"C","title":"\"Granite\" exploration hole, Area 15, Nevada Test Site, Nye County, Nevada : interim report, Part C, physical properties","docAbstract":"Physical properties measurements including porosity, density, permeability, magnetic susceptibility, and thermal conductivity were made on granite samples from the U-15A 'Granite' exploration borehole, Nevada Test Site, Nye County, Nevada. Porosity values range from 0.4 to 4.8 percent, and density values range from 2.56 to 2.69 g/cc (bulk density) and from 2.66 to 2.72 g/cc (grain density). Permeability of fresh rock from the borehole is probably less than 10 -13 millidarcies. Magnetic susceptibility measurements range from 0.36 to 3.48 x 10 -3 cgs units, and thermal conductivity values range from 5.6 to 8.1 cgs units.\r\n\r\n\r\n","language":"ENGLISH","doi":"10.3133/tem836C","usgsCitation":"Izett, G.A., 1960, \"Granite\" exploration hole, Area 15, Nevada Test Site, Nye County, Nevada : interim report, Part C, physical properties: U.S. Geological Survey Trace Elements Memorandum 836, 37 p.; 3 figs.; 10 tables, https://doi.org/10.3133/tem836C.","productDescription":"37 p.; 3 figs.; 10 tables","numberOfPages":"37","costCenters":[],"links":[{"id":192008,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0836c/report-thumb.jpg"},{"id":91204,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0836c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4900e4b0b290850eecba","contributors":{"authors":[{"text":"Izett, Glen Arthur","contributorId":90303,"corporation":false,"usgs":true,"family":"Izett","given":"Glen","email":"","middleInitial":"Arthur","affiliations":[],"preferred":false,"id":288214,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4504,"text":"cir414D - 1960 - Ecological systems and the water resources","interactions":[],"lastModifiedDate":"2017-03-22T16:43:18","indexId":"cir414D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"414","chapter":"D","title":"Ecological systems and the water resources","docAbstract":"<p>In ancient Sparta there were two principal classes of society, the citizen and the helot. The citizen was trained principally to be a warrior. The helot, a serf, was the tiller of the land but could be called to military duty. The history of Herodotus makes it amply clear that making war was the biggest business of the times. Because the Spartans were always marching off to war with someone, they found the landbound position of their city, located as its is in a small central basin nearly surrounded by mountains, somewhat of a disadvantage. When they were under attack, of course, this situation was a favorable one inasmuch as a seaborne enemy had to march inland to come to grips with the Lacedaemonians. The relatively small size of the independent states meant that the Spartans had no direct access through their own lands to the sea.</p><p>There is evidence that the Spartans reached an agreement with surrounding states concerning a free corridor. There would be maintained by all the Grecian states of the Peloponnesus an access route stretching essentially from Sparta to Corinth, through which a marching army could have access to a seaport. As a secondary benefit, this no man's land, which in our western lingo might be called a stock driveway, allowed merchants and their caravans to move freely between the flourishing trading port of Corinth and the inland cities to the south and west.</p><p>Apparently one portion of the agreement between the states with regard to the use of this access zone was that there should be no permanent agricultural or grazing in the driveway. As a result, through several centuries B.C. during which there was high population density in the Aegean area, one strip of land was exempted from the pressures of grazing, lumbering, and agriculture which characterized most of the rest of the landscape. Today this driveway maintains a forest cover. In contrast, mountainsides nearby with an even larger annual rainfall support hardly a tree.</p><p>It is not entirely apparent why subsequent centuries did not see this area denuded. Even with the scanty details known to me it seems clear that the peculiar history of this one area potentially offers us a greater insight into some aspects of forest and land conditions of classical times than extant written records. The several references to sources of timber and cutting of forests contained in the vivid chronicle of Herodotus are valuable, but they lack species identification for the most part. Though rich in human understanding and psychological insight, his history strongly resembles the travel sagas of the Spanish Conquistadors of our Southwest, who had no real eye for \"country.\" Even a careful reading of the works of early travelers such as Coronado, Garces, and Espejo, gives no picture of the nature of the country, its vegetation, or its rivers.</p><p>To describe a biota there is no substitute for a sample. It is logical to ask what one might want to know which would require the preservation of a sample. Whether such a question is asked at all is a reflection on the stage of intellectual maturity of a civilization. We take for granted that there is social gain in the erection and maintenance of a museum of fine arts, a museum of natural history, or a historical museum. Sooner or later we should be mature enough to extend this concept to include a \"museum\" consisting of samples of land types as nearly as possible unaffected by man.</p>","conferenceTitle":"Sixth Biennial Wilderness Conference","conferenceDate":"March 20-21, 1959","conferenceLocation":"San Francisco, CA","language":"English","publisher":"U.s. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir414D","usgsCitation":"Leopold, L.B., 1960, Ecological systems and the water resources: U.S. Geological Survey Circular 414, 6 p., https://doi.org/10.3133/cir414D.","productDescription":"6 p.","startPage":"21","endPage":"26","costCenters":[],"links":[{"id":338128,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir414C","text":"Circular 414-C: The conservation attitude"},{"id":338127,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir414B","text":"Circular 414-B: The challenge of water management"},{"id":338126,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir414A","text":"Circular 414-A: Conservation and protection"},{"id":117278,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0414d/report-thumb.jpg"},{"id":31564,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0414d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"publicComments":"Presented before the Sixth Biennial Wilderness Conference, sponsored by California Academy of Science, San Francisco, Calif, March 20-21, 1959","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627b9c","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":149348,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4532,"text":"cir414C - 1960 - The conservation attitude","interactions":[],"lastModifiedDate":"2017-03-22T16:50:51","indexId":"cir414C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"414","chapter":"C","title":"The conservation attitude","docAbstract":"<p>Forsaking his inheritance and its assurance of a comfortable existence, Guatama Buddha adopted the life of a pauper to seek the intellectual joys of pure contemplation. Under a mulberry tree, it is said, he propounded a 12-point program of ethical conduct stressing the development of a disinterested outlook in each individual. Temples, ritual, and idols he considered distractions from the basic need. He felt that there was a basic need for the development of an attitude.</p><p>The Brahmins as well as the lower castes recognized the merits of the system suggested by Buddha, but they molded his teachings into an accessory to existing rituals and dogma. They soon forgot that Guatama wanted no idols and no temples. They forgot his admonition that an attitude was the thing that really counted. Despite his expressed wish, today Buddha in stone, in bronze, and in gold ponders these things in thousands of temples and hears the prayers of millions who still seek the truths of an ethical life.</p><p>Today, conservation has its temples. The temples of conservation include hundreds of irrigation reservoirs; it has prayer-sticks in miles of contour plow furrows, and the Buddha of a drop-inlet structure looks down on a conservation pool in myriad detention dams.</p><p>Conservation is well established today in the minds of the American public. It seems appropriate to analyze at this time just what it is that is established in the public mind. In what ways have we, too, substituted the temples, the ritual, and the idols for an attitude? </p>","conferenceTitle":"Annual meeting of the Milwaukee County Conservation Alliance","conferenceDate":"December 5, 1958","conferenceLocation":"Milwaukee, WI","language":"English","publisher":"U.s. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir414C","usgsCitation":"Leopold, L.B., 1960, The conservation attitude: U.S. Geological Survey Circular 414, 5 p., https://doi.org/10.3133/cir414C.","productDescription":"5 p.","startPage":"15","endPage":"19","costCenters":[],"links":[{"id":338125,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir414D","text":"Circular 414-D: Ecological systems and the water resources"},{"id":338124,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir414B","text":"Circular 414-B: The challenge of water management"},{"id":338123,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/cir414A","text":"Circular 414-A: Conservation and protection"},{"id":126276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0414c/report-thumb.jpg"},{"id":31589,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0414c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"publicComments":"Presented before the annual meeting of the Milwaukee County Conservation Alliance, Milwaukee, Wis., December 5, 1958","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668a1e","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":149416,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42345,"text":"ofr6035 - 1960 - Aeromagnetic map of the Antler Peak area, Humboldt and Lander Counties, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:02","indexId":"ofr6035","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-35","title":"Aeromagnetic map of the Antler Peak area, Humboldt and Lander Counties, Nevada","language":"ENGLISH","doi":"10.3133/ofr6035","usgsCitation":"Dempsey, W.J., 1960, Aeromagnetic map of the Antler Peak area, Humboldt and Lander Counties, Nevada: U.S. Geological Survey Open-File Report 60-35, 1 map, https://doi.org/10.3133/ofr6035.","productDescription":"1 map","costCenters":[],"links":[{"id":135656,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80111,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1960/0035/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697286","contributors":{"authors":[{"text":"Dempsey, William J.","contributorId":21517,"corporation":false,"usgs":true,"family":"Dempsey","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":226326,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52099,"text":"ofr6067 - 1960 - Ground-water resources of the Headquarters (Cantonment) area, White Sands Proving Ground, Dona Ana County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:11:35","indexId":"ofr6067","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-67","title":"Ground-water resources of the Headquarters (Cantonment) area, White Sands Proving Ground, Dona Ana County, New Mexico","language":"ENGLISH","doi":"10.3133/ofr6067","usgsCitation":"Herrick, E.H., 1960, Ground-water resources of the Headquarters (Cantonment) area, White Sands Proving Ground, Dona Ana County, New Mexico: U.S. Geological Survey Open-File Report 60-67, 203 p., 1 plate, https://doi.org/10.3133/ofr6067.","productDescription":"203 p., 1 plate","costCenters":[],"links":[{"id":100137,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1960/0067/report.pdf","size":"74291","linkFileType":{"id":1,"text":"pdf"}},{"id":178256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1960/0067/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d4e9","contributors":{"authors":[{"text":"Herrick, E. H.","contributorId":87199,"corporation":false,"usgs":true,"family":"Herrick","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":244802,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62366,"text":"gq131 - 1960 - Geology of the Blockhouse quadrangle, Tennessee","interactions":[],"lastModifiedDate":"2021-11-10T20:58:51.148149","indexId":"gq131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"131","title":"Geology of the Blockhouse quadrangle, Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq131","usgsCitation":"Neuman, R.B., and Wilson, R.L., 1960, Geology of the Blockhouse quadrangle, Tennessee: U.S. Geological Survey Geologic Quadrangle 131, Report: 1 p.; Plate, https://doi.org/10.3133/gq131.","productDescription":"Report: 1 p.; Plate","costCenters":[],"links":[{"id":102129,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_578.htm","linkFileType":{"id":5,"text":"html"},"description":"578"},{"id":248542,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0131/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0131/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Tennessee","otherGeospatial":"Blockhouse quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84,35.625 ], [ -84,35.75 ], [ -83.875,35.75 ], [ -83.875,35.625 ], [ -84,35.625 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6077af","contributors":{"authors":[{"text":"Neuman, Robert B.","contributorId":104046,"corporation":false,"usgs":true,"family":"Neuman","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":267289,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, Robert Lake","contributorId":84008,"corporation":false,"usgs":true,"family":"Wilson","given":"Robert","email":"","middleInitial":"Lake","affiliations":[],"preferred":false,"id":267288,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47276,"text":"ofr6073 - 1960 - Generalized geologic map of a part of the Confusion Range, Utah","interactions":[],"lastModifiedDate":"2022-09-13T18:15:37.644529","indexId":"ofr6073","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-73","title":"Generalized geologic map of a part of the Confusion Range, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6073","usgsCitation":"Hose, R.K., Repenning, C.A., and Ziony, J., 1960, Generalized geologic map of a part of the Confusion Range, Utah: U.S. Geological Survey Open-File Report 60-73, 1 Plate: 48.97 × 26.74 inches, https://doi.org/10.3133/ofr6073.","productDescription":"1 Plate: 48.97 × 26.74 inches","costCenters":[],"links":[{"id":171171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":406611,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7981.htm","linkFileType":{"id":5,"text":"html"}},{"id":84233,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1960/0073/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Confusion Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.5,\n              39.25\n            ],\n            [\n              -113.883,\n              39.25\n            ],\n            [\n              -113.883,\n              39.5\n            ],\n            [\n              -113.5,\n              39.5\n            ],\n            [\n              -113.5,\n              39.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af2f4","contributors":{"authors":[{"text":"Hose, Richard Kenneth","contributorId":23915,"corporation":false,"usgs":true,"family":"Hose","given":"Richard","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":234961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Repenning, Charles Albert","contributorId":106883,"corporation":false,"usgs":true,"family":"Repenning","given":"Charles","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":234962,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ziony, Joseph I.","contributorId":16829,"corporation":false,"usgs":true,"family":"Ziony","given":"Joseph I.","affiliations":[],"preferred":false,"id":234960,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":71772,"text":"tei819 - 1960 - Strontium sorption studies on crandallite","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"tei819","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"819","title":"Strontium sorption studies on crandallite","language":"ENGLISH","doi":"10.3133/tei819","usgsCitation":"May, I., Schnepfe, M.M., and Naeser, C.R., 1960, Strontium sorption studies on crandallite: U.S. Geological Survey Trace Elements Investigations 819, 27 p., 9 fig., https://doi.org/10.3133/tei819.","productDescription":"27 p., 9 fig.","costCenters":[],"links":[{"id":186398,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/819/report-thumb.jpg"},{"id":91012,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/819/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4b0d","contributors":{"authors":[{"text":"May, Irving","contributorId":39771,"corporation":false,"usgs":true,"family":"May","given":"Irving","email":"","affiliations":[],"preferred":false,"id":284735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schnepfe, Marian M.","contributorId":98782,"corporation":false,"usgs":true,"family":"Schnepfe","given":"Marian","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":284736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Naeser, Charles R.","contributorId":12093,"corporation":false,"usgs":true,"family":"Naeser","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":284734,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57720,"text":"ofr60166 - 1960 - Ground water in Oklahoma","interactions":[],"lastModifiedDate":"2018-11-05T10:34:32","indexId":"ofr60166","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-166","title":"Ground water in Oklahoma","docAbstract":"<p>One of the first requisites for the intelligent planning of utilization and control of water and for the administration of laws relating to its use is data on the quantity, quality, and mode of occurrence of the available supplies. The collection, evaluation and interpretation, and publication of such data are among the primary functions of the U. S. Geological Survey, Since 1895 the Congress has made appropriations to the Survey for investigation of the water resources of the Nation. In 1929 the Congress adopted the policy of dollar-for-dollar cooperation with the States and local governmental agencies in water resources investigations of the U. S. Geological Survey, In 1937 a program of ground-water investigations was started in cooperation with the Oklahoma Geological Survey, and in 1949 this program was expanded to include cooperation with the Oklahoma Planning and Resources Board, In 1957 the State Legislature created the Oklahoma Water Resources Board as the principal State water agency and it became the principal local cooperator.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr60166","usgsCitation":"Leonard, A., 1960, Ground water in Oklahoma: U.S. Geological Survey Open-File Report 60-166, 12 p., https://doi.org/10.3133/ofr60166.","productDescription":"12 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,{"id":2057,"text":"wsp1495 - 1960 - Geology and ground water in Napa and Sonoma Valleys, Napa and Sonoma Counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1495","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1495","title":"Geology and ground water in Napa and Sonoma Valleys, Napa and Sonoma Counties, California","docAbstract":"Napa and Sonoma Valleys are adjacent alluvium-filled valleys about 40 miles northeast of San Francisco. They occupy alined and structurally controlled depressions in the northern Coast Ranges physiographic province and drain south into San Pablo Bay. The valleys are surrounded and underlain by unconsolidated marine and continental sediments and volcanic rocks of Pliocene and Pleistocene age, which are water bearing in large part and together make up relatively extensive ground-water basins. Napa Valley, the eastern valley, is the larger and has a valley-floor area of about 85 square miles. Sonoma Valley has a valley-floor area of about 35 square miles; in addition, about 10 square miles is unreclaimed tidal marsh. \r\n\r\nThe rock units of Napa and Sonoma Valleys are divided into four classes on the basis of their distribution and relative capacity to yield water: (a) Consolidated virtually non-water-bearing chiefly sedimentary (some metamorphic) rocks that range in age from Jurassic ( ?) to Pliocene; (b) marine shale and sand of the Petaluma formation (Pliocene) and the Merced formation (Pliocene and Pleistocene) that do not crop out within Napa or Sonoma Valleys but perhaps are penetrated by some deep wells drilled in Sonoma Valley; (c) Sonoma volcanics of Pliocene age, parts of which are non-water-bearing and parts of which locally yield large quantities of water; and (d) unconsolidated alluvial deposits mainly of Quaternary age. The deposits of classes (c) and (d) contain the most important aquifers in the area. \r\n\r\nMost of the water used in these valleys is pumped from wells in the younger and older alluvium in the Huichica and Glen Ellen formations. and in the Sonoma volcanics. The principal aquifers are the younger and older alluvium. but appreciable quantities of water are pumped locally from the Sonoma volcanics. The Huichica and Glen Ellen formations yield water in small quantities and at most places supply water only for limited domestic uses. \r\n\r\nThe younger alluvium COIM3ists of interbedded deposits of unconsolidated gravel. sand, silt. and. locally, peat. These deposits underlie the flood plains and channels of the Napa River. Sonoma Creek, and their tributaries, low alluvial fans or plains graded to these streams. and the tidal marshlands. The older alluvium of Napa and Sonoma Valleys is composed of lenticular deposits of unconsolidated and poorly sorted clay, silt. sand. and gravel. Where exposed, claypan or hardpan soil is characteristically developed at the surface. \r\n\r\nThe Huichica formation is composed of deformed continental beds consisting mostly of yellow silt with some interbedded lenses of silt and gravel, and silt and boulders. At the base are beds of redeposited volcanic material, silt, clay, and lenses of coarse gravel and boulders. The Glen Ellen fcrmation consists of alluvial clay, silt, sand, and gravel in clearly stratified but generally lenticular beds. The Sonoma volcanics constitute a thick and highly variate series of continental volcanic rocks, including andesite, basalt, and minor rhyolite flows and interbedded coarse- to fine-grained pyroclastic tuff and breccia, redeposited tuff and pumice, and diatomaceous mud, silt, and sand. A prominent body of rhyolite flows and tuff with some obsidian and perlitic glass, called the St. Helena rhyolite member, occurs in the upper part. \r\n\r\nEstimated ground-water pumpage for all uses in the year 1949-50 was about 5,600 acre-feet in Napa Valley and about 2,400 acre-feet in Sonoma Valley. Of this quantity the amounts pumped for irrigation were about 2,900 and 1,900 acre-feet, respectively. \r\n\r\nWater levels in wells in the central parts of the valleys range from a few feet above the land surface to about 50 feet below, with an average of about 25 feet. The quality of the water in most wells is satisfactory for domestic use and irrigation. Locally at the southern end of the valley some contamination of the native waters is caused by the movement of salty wate","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1495","usgsCitation":"Kunkel, F., and Upson, J.E., 1960, Geology and ground water in Napa and Sonoma Valleys, Napa and Sonoma Counties, California: U.S. Geological Survey Water Supply Paper 1495, v, 252 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1495.","productDescription":"v, 252 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138463,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1495/report-thumb.jpg"},{"id":27593,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1495/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27594,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1495/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27595,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1495/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27596,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1495/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27597,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1495/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27598,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1495/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db68604a","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":144610,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Upson, Joseph Edwin","contributorId":21528,"corporation":false,"usgs":true,"family":"Upson","given":"Joseph","email":"","middleInitial":"Edwin","affiliations":[],"preferred":false,"id":144609,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2840,"text":"wsp1481 - 1960 - Geology and ground-water resources of the Winter Garden district, Texas, 1948","interactions":[],"lastModifiedDate":"2016-08-22T10:51:28","indexId":"wsp1481","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1481","title":"Geology and ground-water resources of the Winter Garden district, Texas, 1948","docAbstract":"<p>The Winter Garden district, as described in this report, includes all of Dimmit and Zavala Counties and the eastern part of Maverick County a total of about 3,200 square miles. The fleldwork for the investigation was completed in 1948.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1481","usgsCitation":"Turner, S.F., Robinson, T.W., and White, W.N., 1960, Geology and ground-water resources of the Winter Garden district, Texas, 1948: U.S. Geological Survey Water Supply Paper 1481, Report: v, 247 p.; 4 Plates: 24.50 x 31.13 inches or smaller, https://doi.org/10.3133/wsp1481.","productDescription":"Report: v, 247 p.; 4 Plates: 24.50 x 31.13 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":138685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1481/report-thumb.jpg"},{"id":29406,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1481/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29407,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1481/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29408,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1481/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29409,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1481/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29410,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1481/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685323","contributors":{"authors":[{"text":"Turner, Samuel Foster","contributorId":26287,"corporation":false,"usgs":true,"family":"Turner","given":"Samuel","email":"","middleInitial":"Foster","affiliations":[],"preferred":false,"id":145884,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, T. W.","contributorId":82285,"corporation":false,"usgs":true,"family":"Robinson","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145885,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, Walter N.","contributorId":99124,"corporation":false,"usgs":true,"family":"White","given":"Walter","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":145886,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3324,"text":"cir427 - 1960 - A field instrument for quantitative determination of beryllium by activation analysis","interactions":[],"lastModifiedDate":"2018-01-02T20:38:35","indexId":"cir427","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"427","title":"A field instrument for quantitative determination of beryllium by activation analysis","docAbstract":"A low-cost instrument has been developed for quantitative determinations of beryllium in the field by activation analysis. The instrument makes use of the gamma-neutron reaction between gammas emitted by an artificially radioactive source (Sb124) and beryllium as it occurs in nature. The instrument and power source are mounted in a panel-type vehicle. Samples are prepared by hand-crushing the rock to approximately ?-inch mesh size and smaller. Sample volumes are kept constant by means of a standard measuring cup. Instrument calibration, made by using standards of known BeO content, indicates the analyses are reproducible and accurate to within ? 0.25 percent BeO in the range from 1 to 20 percent BeO with a sample counting time of 5 minutes. Sensitivity of the instrument maybe increased somewhat by increasing the source size, the sample size, or by enlarging the cross-sectional area of the neutron-sensitive phosphor normal to the neutron flux.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir427","usgsCitation":"Vaughn, W., Wilson, E., and Ohm, J., 1960, A field instrument for quantitative determination of beryllium by activation analysis: U.S. Geological Survey Circular 427, 9 p. :illus. ;27cm., https://doi.org/10.3133/cir427.","productDescription":"9 p. :illus. ;27cm.","costCenters":[],"links":[{"id":30333,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0427/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0427/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec8d","contributors":{"authors":[{"text":"Vaughn, William W.","contributorId":107267,"corporation":false,"usgs":true,"family":"Vaughn","given":"William W.","affiliations":[],"preferred":false,"id":146669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, E.E.","contributorId":68299,"corporation":false,"usgs":true,"family":"Wilson","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":146667,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ohm, J.M.","contributorId":83508,"corporation":false,"usgs":true,"family":"Ohm","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":146668,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2959,"text":"wsp1629 - 1960 - Surface water supply of the United States, 1959, Part 6-A, Missouri River Basin above Sioux City, Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"wsp1629","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1629","title":"Surface water supply of the United States, 1959, Part 6-A, Missouri River Basin above Sioux City, Iowa","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1629","usgsCitation":"Wells, J.V., 1960, Surface water supply of the United States, 1959, Part 6-A, Missouri River Basin above Sioux City, Iowa: U.S. Geological Survey Water Supply Paper 1629, x, 415 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1629.","productDescription":"x, 415 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":139282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1629/report-thumb.jpg"},{"id":29668,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1629/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db69437f","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2338,"text":"wsp1487 - 1960 - Geology and ground-water resources of the lower Little Bighorn River Valley, Big Horn County, Montana, with special reference to the drainage of waterlogged lands","interactions":[],"lastModifiedDate":"2023-07-18T10:57:54.875188","indexId":"wsp1487","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1487","title":"Geology and ground-water resources of the lower Little Bighorn River Valley, Big Horn County, Montana, with special reference to the drainage of waterlogged lands","docAbstract":"<p>The lower Little Bighorn River valley, Montana, is in the unglaciated part of the Missouri Plateau section of the Great Plains physiographic province. The river and its principal tributaries rise in the Bighorn Mountains, and the confluence of this northward-flowing stream with the Bighorn River is near the east edge of Hardin, Mont. The normal annual precipitation ranges from about 12 inches in the northern part of the area to 15 inches in the southern part. The economy of the area is founded principally on farming, much of the low-lying land adjacent to the river being irrigated. The irrigated land is within the Crow Indian Reservation, although a part is privately owned. The bedrock formations exposed in the area are of Cretaceous age and include the Parkman sandstone, Claggett shale, Eagle sandstone, Telegraph Creek shale, and Cody shale. The Cloverly formation, Tensleep sandstone, and Madison limestone, which underlie but are not exposed in the area, and the Parkman sandstone in the southern half of the area appear to be the principal bedrock aquifers. All except the Parkman lie at depths ranging from a few feet to several thousand feet, and all appear to be capable of yielding water in commercial quantities. Some of the other formations arc capable of yielding enough water for domestic and stock needs. The river alluvium of Recent age and the Pleistocene terrace deposits are the principal unconsolidated formations in the area with respect to water supply and drainage. Wells yielding as much as 100 gallons per minute may be developed in favorable areas. Pumping tests reveal that the transmissibility of the coarser unconsolidated materials probably ranges from about 15,000 to 30,000 gallons per day per foot. Two tests of the Parkman sandstone showed transmissibilities of 6,000 and 20,000 gallons per day per foot. Although a test of the Cloverly formation showed a transmissibility of only 3,000 gallons per day per foot, the high artesian pressure--80 pounds per square inch at the land surface--in the Cloverly caused the tested well to yield about 200 gallons per minute by natural flow; this is greater than the yield of any other single well in the area. Textural properties were compared with the hydraulic properties determined by laboratory tests to show the relation between different types of waterbearing materials. Materials classified as heavy soils-normally somewhat dense and impervious-had an average permeability of 7.2 gallons per day per square foot, which was more than expected. One sample of very coarse alluvial material had a permeability of 6,000 gallons per day per square foot. The depth to water beneath irrigation units was mapped, thus showing the waterlogged areas. Waterlogging is not a serious problem where the water table is more than 6 feet below the land surface. For the drainage studies the unconsolidated deposits are classified in two zones-coarse-grained sediments resting on the relatively impermeable bedrock floor and overlying fine-grained sediments which extend to the land surface. The transmissibility of the coarse-sediment zone generally is many times greater than that of the fine-sediment zone. Because in many places drains could not be economically dug deep enough to enter the coarse zone, the study of the effectiveness of drainage completed in the fine zone received much attention. The studies showed that, despite a considerable thickness of fine-grained sediments between the bottom of the drain and the top of the coarse zone, drainage ditches frequently were effective in relieving waterlogging of fields nearby. Pilot relief wells installed in existing drains showed that the effectiveness of some drains could be increased appreciably by installing a series of relief wells. Records of fluctuations of water levels in 196 observation wells and water-level contour maps were studied to show the principal areas of recharge and discharge in the irrigable areas.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1487","usgsCitation":"Moulder, E.A., Klug, M.F., Morris, D.A., Swenson, F.A., and Krieger, R.A., 1960, Geology and ground-water resources of the lower Little Bighorn River Valley, Big Horn County, Montana, with special reference to the drainage of waterlogged lands: U.S. Geological Survey Water Supply Paper 1487, Report: viii, 223 p.; 13 Plates: 17.00 × 42.65 inches or smaller, https://doi.org/10.3133/wsp1487.","productDescription":"Report: viii, 223 p.; 13 Plates: 17.00 × 42.65 inches or smaller","costCenters":[],"links":[{"id":28222,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28221,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28217,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28216,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28215,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28214,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28213,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396137,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24428.htm"},{"id":28223,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1487/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138575,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1487/report-thumb.jpg"},{"id":28210,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28211,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28212,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28218,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28219,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28220,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1487/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","county":"Big Horn County","otherGeospatial":"lower Little Bighorn River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.529,\n              45.266\n            ],\n            [\n              -107.338,\n              45.266\n            ],\n            [\n              -107.338,\n              45.72\n            ],\n            [\n              -107.529,\n              45.72\n            ],\n            [\n              -107.529,\n              45.266\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68530a","contributors":{"authors":[{"text":"Moulder, E. A.","contributorId":78719,"corporation":false,"usgs":true,"family":"Moulder","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145043,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klug, M. F.","contributorId":97372,"corporation":false,"usgs":true,"family":"Klug","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145044,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morris, D. A.","contributorId":56204,"corporation":false,"usgs":true,"family":"Morris","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145041,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swenson, F. 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,{"id":2022,"text":"wsp1475B - 1960 - Hydrology of Cornfield Wash, Sandoval County, New Mexico, 1951-55","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1475B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1475","chapter":"B","title":"Hydrology of Cornfield Wash, Sandoval County, New Mexico, 1951-55","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"United States Government Printing Office,","doi":"10.3133/wsp1475B","usgsCitation":"Kennon, F., and Peterson, H.V., 1960, Hydrology of Cornfield Wash, Sandoval County, New Mexico, 1951-55: U.S. Geological Survey Water Supply Paper 1475, iv, 45-102, [1] p. :ill., maps ;24 cm. & 1 map in pocket., https://doi.org/10.3133/wsp1475B.","productDescription":"iv, 45-102, [1] p. :ill., maps ;24 cm. & 1 map in pocket.","costCenters":[],"links":[{"id":137614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475b/report-thumb.jpg"},{"id":27489,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27490,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604a0a","contributors":{"authors":[{"text":"Kennon, F.W.","contributorId":88332,"corporation":false,"usgs":true,"family":"Kennon","given":"F.W.","affiliations":[],"preferred":false,"id":144543,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, Harold V.","contributorId":9630,"corporation":false,"usgs":true,"family":"Peterson","given":"Harold","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":144542,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":2584,"text":"wsp1536B - 1960 - Water levels near a well discharging from an unconfined aquifer","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1536B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1536","chapter":"B","title":"Water levels near a well discharging from an unconfined aquifer","language":"ENGLISH","publisher":"U.S. Department of the Interior, Geological Survey ;","doi":"10.3133/wsp1536B","isbn":"pbk","usgsCitation":"Remson, I., McNeary, S., and Randolph, J., 1960, Water levels near a well discharging from an unconfined aquifer: U.S. Geological Survey Water Supply Paper 1536, iii, [13] p. ;23 cm., https://doi.org/10.3133/wsp1536B.","productDescription":"iii, [13] p. ;23 cm.","costCenters":[],"links":[{"id":137841,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1536b/report-thumb.jpg"},{"id":28858,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1536b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9cec","contributors":{"authors":[{"text":"Remson, Irwin","contributorId":89115,"corporation":false,"usgs":true,"family":"Remson","given":"Irwin","email":"","affiliations":[],"preferred":false,"id":145442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McNeary, S.S.","contributorId":14797,"corporation":false,"usgs":true,"family":"McNeary","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":145440,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Randolph, J.R.","contributorId":19532,"corporation":false,"usgs":true,"family":"Randolph","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":145441,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2930,"text":"wsp1569 - 1960 - Surface water supply of Hawaii, 1956-58","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp1569","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1569","title":"Surface water supply of Hawaii, 1956-58","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1569","usgsCitation":"Wells, J.V., 1960, Surface water supply of Hawaii, 1956-58: U.S. Geological Survey Water Supply Paper 1569, vii, 295 p. ;24 cm., https://doi.org/10.3133/wsp1569.","productDescription":"vii, 295 p. ;24 cm.","costCenters":[],"links":[{"id":139017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1569/report-thumb.jpg"},{"id":29639,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1569/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69769a","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146016,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2334,"text":"wsp1490 - 1960 - Geology and ground-water resources of Platte County, Wyoming, with a section on Chemical quality of the water","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1490","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1490","title":"Geology and ground-water resources of Platte County, Wyoming, with a section on Chemical quality of the water","docAbstract":"Platte County, Wyo., has an area of 2,114 square miles and, in 1950, had a population of 7,925; it lies within parts of two major physiographic provinces, the northern extension of the Southern Rocky Mountains and the northwestern part of the Great Plains. The Laramie Range and related structures lie along the western margin of the county and constitute the eastern limit of the Rocky Mountain Front Range. The High Plains section of the Great Plains province extends eastward from the Laramie Range over the remainder of the county. The original surface of the High Plains has been deeply eroded, and in the northeastern part of the county it is broken by the broad uplifted structural platform of the Hartville Hills. The North Platte River and its tributaries have entrenched their channels as much as 1,000 feet into the plains, leaving wide, very flat intervalley areas that are interrupted by a few isolated buttes and outlying ridges. Well-defined terraces, locally called the Wheatland Flats, have been formed in central Platte County. The climate is semiarid, the average annual precipitation being about 15 inches. Farming and stockraising are the principal occupations in the county. \r\n\r\nMost of the rocks exposed in the county are of Tertiary and Quaternary age, although rocks as old as Precambrian crop out locally. The Arikaree and Brule formations and younger deposits, including Tertiary ( ?) deposits (undifferentiated) and terrace, flood-plain, and other alluvial deposits, underlie more than two-thirds of the county. Mesozoic, Paleozoic, and Precambrian rocks crop out in the other third and underlie the younger rocks at great depths elsewhere. Small supplies of ground water adequate for domestic and stock use can be obtained from shallow wells in the Casper, Hartville, Cloverly, Brule, and Arikaree formations and in the terrace and flood-plain deposits. Small to moderate amounts of ground water can be obtained from the 'Converse sand' of the Hartville formation. Several flowing wells obtain water from this sand near Glendo. Moderate to large supplies of ground water adequate for small-scale irrigation or industrial uses or for public supply can be obtained from properly constructed wells penetrating thick saturated sections of the Arikaree formation and from the terrace and flood-plain deposits. Large supplies of ground water can be obtained from the flood-plain deposits of the North Platte River near Guernsey, where wells commonly yield more than 1,000 gpm (gallons per minute). The aquifers with greatest potential for additional groundwater development in Platte County, in decreasing order of importance, are the flood-plain deposits along the North Platte River and its tributaries, the Arikaree formation and terrace deposits in parts of the Wheatland Flats, and the 'Converse sand' in the general vicinity of Glendo.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1490","usgsCitation":"Morris, D.A., Babcock, H.M., and Langford, R., 1960, Geology and ground-water resources of Platte County, Wyoming, with a section on Chemical quality of the water: U.S. Geological Survey Water Supply Paper 1490, vi, 195 p. :ill., maps, charts ;24 cm., https://doi.org/10.3133/wsp1490.","productDescription":"vi, 195 p. :ill., maps, charts ;24 cm.","costCenters":[],"links":[{"id":109950,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24431.htm","linkFileType":{"id":5,"text":"html"},"description":"24431"},{"id":138465,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1490/report-thumb.jpg"},{"id":28195,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1490/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28196,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1490/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28197,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1490/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28198,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1490/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28199,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1490/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6859f9","contributors":{"authors":[{"text":"Morris, D. A.","contributorId":56204,"corporation":false,"usgs":true,"family":"Morris","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Babcock, H. M.","contributorId":90698,"corporation":false,"usgs":true,"family":"Babcock","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":145030,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langford, R.H.","contributorId":59426,"corporation":false,"usgs":true,"family":"Langford","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":145029,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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