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,{"id":46857,"text":"ofr6541 - 1965 - Results of stream-sediment sampling in the Iliamna quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:59","indexId":"ofr6541","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-41","title":"Results of stream-sediment sampling in the Iliamna quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/ofr6541","usgsCitation":"Detterman, R.L., and Reed, B.L., 1965, Results of stream-sediment sampling in the Iliamna quadrangle, Alaska: U.S. Geological Survey Open-File Report 65-41, 1 map., https://doi.org/10.3133/ofr6541.","productDescription":"1 map.","costCenters":[],"links":[{"id":169302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0041/report-thumb.jpg"},{"id":83743,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0041/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605620","contributors":{"authors":[{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":234207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reed, Bruce L.","contributorId":19928,"corporation":false,"usgs":true,"family":"Reed","given":"Bruce","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":234206,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40838,"text":"ofr65120 - 1965 - Preliminary geologic map and coal deposits of the northwest quarter of the Gunsight Butte quadrangle, Kane County, Utah","interactions":[{"subject":{"id":40838,"text":"ofr65120 - 1965 - Preliminary geologic map and coal deposits of the northwest quarter of the Gunsight Butte quadrangle, Kane County, Utah","indexId":"ofr65120","publicationYear":"1965","noYear":false,"title":"Preliminary geologic map and coal deposits of the northwest quarter of the Gunsight Butte quadrangle, Kane County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70046203,"text":"70046203 - 1967 - Preliminary geologic map and coal deposits of the northwest quarter of the Gunsight Butte quadrangle, Kane County, Utah","indexId":"70046203","publicationYear":"1967","noYear":false,"title":"Preliminary geologic map and coal deposits of the northwest quarter of the Gunsight Butte quadrangle, Kane County, Utah"},"id":1}],"supersededBy":{"id":70046203,"text":"70046203 - 1967 - Preliminary geologic map and coal deposits of the northwest quarter of the Gunsight Butte quadrangle, Kane County, Utah","indexId":"70046203","publicationYear":"1967","noYear":false,"title":"Preliminary geologic map and coal deposits of the northwest quarter of the Gunsight Butte quadrangle, Kane County, Utah"},"lastModifiedDate":"2013-05-30T15:13:18","indexId":"ofr65120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-120","title":"Preliminary geologic map and coal deposits of the northwest quarter of the Gunsight Butte quadrangle, Kane County, Utah","language":"ENGLISH","doi":"10.3133/ofr65120","usgsCitation":"Peterson, F., 1965, Preliminary geologic map and coal deposits of the northwest quarter of the Gunsight Butte quadrangle, Kane County, Utah: U.S. Geological Survey Open-File Report 65-120, 1 map on two sheets, https://doi.org/10.3133/ofr65120.","productDescription":"1 map on two sheets","costCenters":[],"links":[{"id":106347,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8082.htm","linkFileType":{"id":5,"text":"html"},"description":"8082"},{"id":171087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c285","contributors":{"authors":[{"text":"Peterson, Fred fpeterson@usgs.gov","contributorId":1309,"corporation":false,"usgs":true,"family":"Peterson","given":"Fred","email":"fpeterson@usgs.gov","affiliations":[],"preferred":true,"id":224024,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45735,"text":"b1199E - 1965 - Bauxite deposits of the Eufaula District, Alabama","interactions":[{"subject":{"id":55450,"text":"ofr4332 - 1943 - Bauxite deposits of Barbour and Henry Counties, Alabama","indexId":"ofr4332","publicationYear":"1943","noYear":false,"title":"Bauxite deposits of Barbour and Henry Counties, Alabama"},"predicate":"SUPERSEDED_BY","object":{"id":45735,"text":"b1199E - 1965 - Bauxite deposits of the Eufaula District, Alabama","indexId":"b1199E","publicationYear":"1965","noYear":false,"chapter":"E","title":"Bauxite deposits of the Eufaula District, Alabama"},"id":1}],"lastModifiedDate":"2012-02-02T00:10:14","indexId":"b1199E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1199","chapter":"E","title":"Bauxite deposits of the Eufaula District, Alabama","language":"ENGLISH","doi":"10.3133/b1199E","usgsCitation":"Warren, W., and Clark, L.D., 1965, Bauxite deposits of the Eufaula District, Alabama: U.S. Geological Survey Bulletin 1199, p. E1-E31, https://doi.org/10.3133/b1199E.","productDescription":"p. E1-E31","costCenters":[],"links":[{"id":109493,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20974.htm","linkFileType":{"id":5,"text":"html"},"description":"20974"},{"id":169817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1199e/report-thumb.jpg"},{"id":82355,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1199e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":82356,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1199e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e0eb","contributors":{"authors":[{"text":"Warren, W.C.","contributorId":71238,"corporation":false,"usgs":true,"family":"Warren","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":231943,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, L. D.","contributorId":11189,"corporation":false,"usgs":true,"family":"Clark","given":"L.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":231942,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42646,"text":"ofr6580 - 1965 - Preliminary geologic map of the Palisades Peak quadrangle, Bonneville County, Idaho, and Teton County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:11:04","indexId":"ofr6580","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-80","title":"Preliminary geologic map of the Palisades Peak quadrangle, Bonneville County, Idaho, and Teton County, Wyoming","language":"ENGLISH","doi":"10.3133/ofr6580","usgsCitation":"Jobin, D., 1965, Preliminary geologic map of the Palisades Peak quadrangle, Bonneville County, Idaho, and Teton County, Wyoming: U.S. Geological Survey Open-File Report 65-80, 1 map, https://doi.org/10.3133/ofr6580.","productDescription":"1 map","costCenters":[],"links":[{"id":106362,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8113.htm","linkFileType":{"id":5,"text":"html"},"description":"8113"},{"id":168257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80416,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0080/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae84","contributors":{"authors":[{"text":"Jobin, D. A.","contributorId":41062,"corporation":false,"usgs":true,"family":"Jobin","given":"D. A.","affiliations":[],"preferred":false,"id":226876,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2875,"text":"wsp1809C - 1965 - Ground-water in the upper Star Valley, Wyoming","interactions":[{"subject":{"id":52369,"text":"ofr63129 - 1963 - Ground water in the upper Star Valley, Wyoming","indexId":"ofr63129","publicationYear":"1963","noYear":false,"title":"Ground water in the upper Star Valley, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":2875,"text":"wsp1809C - 1965 - Ground-water in the upper Star Valley, Wyoming","indexId":"wsp1809C","publicationYear":"1965","noYear":false,"chapter":"C","title":"Ground-water in the upper Star Valley, Wyoming"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1809C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"C","title":"Ground-water in the upper Star Valley, Wyoming","docAbstract":"The upper Star Valley covers about 55 square miles of lowland in the westernmost part of Wyoming. The altitude of the floor of the valley is 6,000-6,700 feet. The climate is cool; the growing season, short. Annual precipitation averages about 18 inches, and total precipitation in July and August averages 2.2 inches. Additional supplies of water are needed for irrigation of pasture and hay. The principal water-bearing formation is a thick body of gravel of Pleistocene age. Consolidated to semiconsolidated sedimentary formations of Paleozoic to Tertiary age form the surrounding mountains and underlie the gravel. These bedrock formations yield small amounts of water to wells on the margins of the valley. \r\n\r\nMost of the recharge to the gravel aquifer is received at the heads of alluvial fans by infiltration from tributaries that drain the surrounding mountains. Snow upon the valley floor provides a significant amount of recharge. Water moves toward the Salt River, which flows northward through the valley and which has large gains due to ground-water inflow. \r\n\r\nOn the east side of the valley, the water table is 100-200 feet below land surface at a distance of half a mile from the mountain front. On the west side of the valley, the depth to water is rarely more than 30 feet. Depth to water decreases toward the center of the valley. \r\n\r\nThe gravel aquifer can provide sufficient water for supplemental irrigation. Irrigation supplies of several hundreds of gallons per minute have been developed at two localities on the west side of the valley. Two pumping tests showed values for transmissibility of 82,500 and 370,000 gallons per day per foot in the vicinity of a well on the east side of the valley and a well on the west side, respectively. \r\n\r\nThe ground water is of good quality for irrigation usage through most of the valley. Hardness of the water exceeds 200 parts per million, however, and this characteristic makes the water somewhat undesirable for domestic and industrial use. Water beneath the northwestern part of the valley has relatively high content of sodium and chloride.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1809C","usgsCitation":"Walker, E.H., 1965, Ground-water in the upper Star Valley, Wyoming: U.S. Geological Survey Water Supply Paper 1809, iv, 27 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1809C.","productDescription":"iv, 27 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138978,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809c/report-thumb.jpg"},{"id":29503,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29504,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db66826e","contributors":{"authors":[{"text":"Walker, Eugene H.","contributorId":24761,"corporation":false,"usgs":true,"family":"Walker","given":"Eugene","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2026,"text":"wsp1789 - 1965 - Ground water in the upper part of the Teton Valley, Teton Counties, Idaho and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1789","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1789","title":"Ground water in the upper part of the Teton Valley, Teton Counties, Idaho and Wyoming","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1789","usgsCitation":"Kilburn, C., 1965, Ground water in the upper part of the Teton Valley, Teton Counties, Idaho and Wyoming: U.S. Geological Survey Water Supply Paper 1789, iv, 60 p. :illus., maps (4 fold. in pocket) ;24 cm., https://doi.org/10.3133/wsp1789.","productDescription":"iv, 60 p. :illus., maps (4 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":137628,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1789/report-thumb.jpg"},{"id":27495,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1789/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27496,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1789/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27497,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1789/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27498,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1789/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27499,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1789/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d6f2","contributors":{"authors":[{"text":"Kilburn, Chabot","contributorId":83499,"corporation":false,"usgs":true,"family":"Kilburn","given":"Chabot","email":"","affiliations":[],"preferred":false,"id":144548,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2000,"text":"wsp1802 - 1965 - Fluvial sediment of the Mississippi River at St. Louis, Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1802","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1802","title":"Fluvial sediment of the Mississippi River at St. Louis, Missouri","docAbstract":"An investigation of the fluvial sediment of the Mississippi River at St. Louis, Mo., was begun in 1948. Most data have been obtained only to determine the daily suspended-sediment discharge and the particle-size distribution of suspended sediment and bed material, but a few data have been obtained to study the flow resistance, the vertical distribution of sediment and velocity, and the bed-material discharge. \r\n\r\nThe flow of the Mississippi River at St. Louis is made up of the flows from the Missouri River, which had an average flow of 79,860 cubic feet per second for 1897-1958 at Hermann, Mo., and from the upper Mississippi River, which had an average flow of 91,890 cubic feet per second for 1928-58 at Alton, Il. The Missouri River is partly controlled by reservoirs that had a total capacity of 90,300,000 acre-feet in 1956, and the upper Mississippi River is partly controlled by lakes and reservoirs that had a total capacity of 4,890,000 acre-feet in 1956. The flows of the Missouri and upper Mississippi Rivers have not become mixed at St. Louis; so the river has a lateral gradient of suspended-sediment concentration. The concentration near the west bank has been as much as 2,400 parts per million greater than the concentration near the east bank. \r\n\r\nSuspended-sediment discharges from April 1948 to September 1958 ranged from 4,250 to 7,010,000 tons per day and averaged 496,000 tons per day. Mean concentrations for water years decreased steadily from 1,690 parts per million in 1949 to 403 parts per million in 1956, but they increased to 756 parts per million in 1958. Effects of new reservoirs in the Missouri River basin on the concentration have been obscured by the close relation of concentration to streamflow. Measured suspended-sediment discharge through September 1958 averaged 47 percent clay, 38 percent silt, and 15 percent sand. Variations of particle size were due mainly to differences in the source areas of the sediment. Most of the bed material in the main flow was between 0.125 and 1.000 millimeter in diameter. The average of median diameters was related to the discharge for periods of 1 year and longer. Geometric quartile deviations of the bed material ranged from 1.1 to 2.5 and averaged 1.5. \r\n\r\nThe mean elevation of the bed had a range of almost 10 feet and was related to the median diameter of bed material by the regression equation hb=363.0 - 7.8 d50 for which the standard error of estimate was 0.91 foot. \r\n\r\nThe resistance to flow as measured by Manning's n ranged from 0.024 to 0.041 and was related to the discharge and mean velocity but not to the shear velocity. Normal dune height is 2-8 feet, and average dune length is about 250 feet. When the resistance to flow was low, much of the bed was fairly fiat; a few dunes were present, but they were much longer than the average. For a given discharge during individual rises in stage, the gage height was lower for increasing discharge than for decreasing discharge even though the bed elevation was higher. The changes in gage height were not caused by changes in energy gradient due to changing discharge, by channel storage between the gage and the measuring section, nor by return of overbank flow; but they were probably caused by a combination of changes in roughness due to changing bed configuration and of changes in turbulence constant due to changing sediment concentration. Turbulence constants (Von Karman's k) computed from velocity measurements at 5-10 points in the vertical and from routine velocity measurements at 2 points in the vertical averaged 0.35 and 0.33, respectively. \r\n\r\nThe exponent z1 of the vertical distribution of concentration for different size ranges varied with about the 0.77 power of the fall velocity. Except for the difference between the theoretical variation and the actual variation of z1 with changing fall velocity, the theoretical equation for the vertical distribution of sediment concentration seems to apply reasonably well for the Miss","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1802","usgsCitation":"Jordan, P.R., 1965, Fluvial sediment of the Mississippi River at St. Louis, Missouri: U.S. Geological Survey Water Supply Paper 1802, viii, 89 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1802.","productDescription":"viii, 89 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":138367,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1802/report-thumb.jpg"},{"id":27444,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1802/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aea9e","contributors":{"authors":[{"text":"Jordan, Paul Robert","contributorId":57819,"corporation":false,"usgs":true,"family":"Jordan","given":"Paul","email":"","middleInitial":"Robert","affiliations":[],"preferred":false,"id":144507,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2169,"text":"wsp1644 - 1965 - Quality of surface waters of the United States, 1959, Parts 7 & 8, lower Mississippi River Basin and western Gulf of Mexico Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1644","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1644","title":"Quality of surface waters of the United States, 1959, Parts 7 & 8, lower Mississippi River Basin and western Gulf of Mexico Basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1644","usgsCitation":"Love, S.K., 1965, Quality of surface waters of the United States, 1959, Parts 7 & 8, lower Mississippi River Basin and western Gulf of Mexico Basins: U.S. Geological Survey Water Supply Paper 1644, xi, 508 p. :ill. ;25 cm., https://doi.org/10.3133/wsp1644.","productDescription":"xi, 508 p. :ill. ;25 cm.","costCenters":[],"links":[{"id":138307,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1644/report-thumb.jpg"},{"id":27780,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1644/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651c04","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144764,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2369,"text":"wsp1804 - 1965 - Drought of the 1950's with special reference to the Mid-continent","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1804","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1804","title":"Drought of the 1950's with special reference to the Mid-continent","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1804","usgsCitation":"Nace, R.L., and Pluhowski, E.J., 1965, Drought of the 1950's with special reference to the Mid-continent: U.S. Geological Survey Water Supply Paper 1804, v, 88 p. :illus. (2 fold. in pocket) maps. ;24 cm., https://doi.org/10.3133/wsp1804.","productDescription":"v, 88 p. :illus. (2 fold. in pocket) maps. ;24 cm.","costCenters":[],"links":[{"id":137743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1804/report-thumb.jpg"},{"id":28308,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1804/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28309,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1804/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28310,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1804/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633d37","contributors":{"authors":[{"text":"Nace, Raymond L.","contributorId":93460,"corporation":false,"usgs":true,"family":"Nace","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145090,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pluhowski, Edward J.","contributorId":87911,"corporation":false,"usgs":true,"family":"Pluhowski","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145089,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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,{"id":2537,"text":"wsp1662B - 1965 - Specific yield - laboratory experiments showing the effect of time on column drainage","interactions":[],"lastModifiedDate":"2018-06-13T11:36:21","indexId":"wsp1662B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1662","chapter":"B","title":"Specific yield - laboratory experiments showing the effect of time on column drainage","docAbstract":"<p>The increasing use of ground water from many major aquifers in the United States has required a more thorough understanding of gravity drainage, or specific yield. This report describes one phase of specific yield research by the U.S. Geological Survey's Hydrologic Laboratory in cooperation with the California Department of Water Resources. </p><p>An earlier phase of the research concentrated on the final distribution of moisture retained after drainage of saturated columns of porous media. This report presents the phase that concentrated on the distribution of moisture retained in similar columns after drainage for various periods of time. </p><p>Five columns, about 4 cm in diameter by 170 cm long, were packed with homogenous sand of very fine, medium, and coarse sizes, and one column was packed with alternating layers of coarse and medium sand. The very fine materials were more uniform in size range than were the medium materials. As the saturated columns drained, tensiometers installed throughout the length recorded changes in moisture tension. The relation of tension to moisture content, determined for each of the materials, was then used to convert the tension readings to moisture content. Data were then available on the distribution of retained moisture for different periods of drainage from 1 to 148 hours. Data also are presented on the final distribution of moisture content by weight and volume and on the degree of saturation. </p><p>The final zone of capillary saturation was approximately 12 cm for coarse sand, 13 cm for medium sand, and 52 cm for very fine sand. The data showed these zones were 92 to 100 percent saturated. </p><p>Most of the outflow from the columns occurred in the earlier hours of drainage--90 percent in 1 hour for the coarse materials, 50 percent for the medium, and 60 percent for the very fine. Although the largest percentage of the specific yield was reached during the early hours of drainage, this study amply demonstrates that a very long time would be required to reach drainage equilibrium. </p><p>In the layered columns the middle (medium sand) layer functioned as a hanging water column accelerating the drainage of the overlying coarse-sand layer. After the middle layer started to drain, the moisture distribution as retained in all three layers showed trends similar to that obtained when the same materials were tested in homogenous columns.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1662B","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Prill, R.C., Johnson, A., and Morris, D.A., 1965, Specific yield - laboratory experiments showing the effect of time on column drainage: U.S. Geological Survey Water Supply Paper 1662, iv, 55 p., https://doi.org/10.3133/wsp1662B.","productDescription":"iv, 55 p.","costCenters":[],"links":[{"id":138581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1662b/report-thumb.jpg"},{"id":28778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1662b/report.pdf","text":"Report","size":"1.51 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db64853b","contributors":{"authors":[{"text":"Prill, Robert C.","contributorId":86317,"corporation":false,"usgs":true,"family":"Prill","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":145365,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morris, Donald Arthur","contributorId":13960,"corporation":false,"usgs":true,"family":"Morris","given":"Donald","email":"","middleInitial":"Arthur","affiliations":[],"preferred":false,"id":145364,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2626,"text":"wsp1810 - 1965 - Summary of floods in the United States during 1961","interactions":[],"lastModifiedDate":"2017-09-06T16:28:04","indexId":"wsp1810","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1810","title":"Summary of floods in the United States during 1961","docAbstract":"<p>This report describes the most outstanding floods in the United States during 1961. The most damaging floods during the year were those caused by snowmelt in March and April in the upper Mississippi River basin and those accompanying Hurricane Carla in September.</p><p>Hurricane Carla traveled northward along the east edge of Texas and then northeastward through southeastern Oklahoma, northwestern Arkansas, southeastern Missouri, and central Illinois. Heavy rains and floods occurred east of the hurricane's path in Texas and west of its path for the remainder of its journey.</p><p>Mississippi, Alabama, and Georgia had moderate to severe floods in February and March from a series of large-area rainstorms. Many maximum peak discharges occurred, and streams remained at high stages for periods longer than any known before. Property damage was high and four lives were lost.</p><p>Extensive flooding took place in May from southeastern Kansas and northeastern Oklahoma through northern Arkansas, southern Missouri, northern Kentucky, and the southern parts of Illinois, Indiana, and Ohio. Maximum discharges occurred at many sites throughout the area.</p><p>Heavy flooding was experienced on Kootenai River at Bonners Ferry, Idaho, in May and June. These floods were noteworthy for their duration.</p><p>The most tragic flood of the year was in July in Charleston, W. Va. A small area cloudburst flood caused 22 deaths and damage of more than \\$1 million.</p><p>Severe flooding occurred in December in the Tombigbee River, Pearl River, and Pascagoula River basins in Mississippi, Louisiana, and Alabama. Much damage resulted, and from two to three thousand persons were evacuated from large flooded areas.</p><p>In addition to the floods mentioned above, 19 others of lesser magnitude are considered important enough to be included in this annual summary.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1810","collaboration":"Prepared in cooperation with Federal, State, and local agencies","usgsCitation":"Rostvedt, J., 1965, Summary of floods in the United States during 1961: U.S. Geological Survey Water Supply Paper 1810, vi, 123 p., https://doi.org/10.3133/wsp1810.","productDescription":"vi, 123 p.","numberOfPages":"128","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":28943,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1810/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1810/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699281","contributors":{"authors":[{"text":"Rostvedt, J.O.","contributorId":24757,"corporation":false,"usgs":true,"family":"Rostvedt","given":"J.O.","email":"","affiliations":[],"preferred":false,"id":145524,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2676,"text":"wsp1809Q - 1965 - Ground-water resources and geology of Seminole, Decatur, and Grady Counties, Georgia","interactions":[],"lastModifiedDate":"2022-02-02T22:03:54.948109","indexId":"wsp1809Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"Q","title":"Ground-water resources and geology of Seminole, Decatur, and Grady Counties, Georgia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1809Q","usgsCitation":"Sever, C.W., 1965, Ground-water resources and geology of Seminole, Decatur, and Grady Counties, Georgia: U.S. Geological Survey Water Supply Paper 1809, Report: iv, 30 p.; 2 Plates: 35.50 × 22.50 inches and 18.00 × 25.00 inches, https://doi.org/10.3133/wsp1809Q.","productDescription":"Report: iv, 30 p.; 2 Plates: 35.50 × 22.50 inches and 18.00 × 25.00 inches","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":29027,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809q/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29026,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809q/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29028,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809q/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138271,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809q/report-thumb.jpg"},{"id":395318,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25012.htm"}],"country":"United States","state":"Georgia","county":"Decatur 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,{"id":2771,"text":"wsp1809B - 1965 - Geology and ground-water resources of Waushara County, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-02T13:14:56","indexId":"wsp1809B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"B","title":"Geology and ground-water resources of Waushara County, Wisconsin","docAbstract":"<p>Abundant ground water for irrigation is available in the outwash deposits in western Waushara County, and many more large-capacity wells can be developed in these deposits without seriously lowering the water level. Pumping for irrigation temporarily lowers water levels in the vicinity of the wells but has not lowered regional water levels. Pumpage has probably intercepted and utilized some of the recharge that would have been rapidly discharged from the aquifer. Ground water is continuously being discharged to streams and to the atmosphere by evapotranspiration, but intermittent recharge from precipitation replaces the discharged water. Recharge and discharge are in approximate balance, maintaining about the same amount of ground water in storage. Further recharge to the aquifer is rapidly discharged to streams. The sandstones, till, and glaciolacustrine deposits in Waushara County generally yield small to moderate amounts of water to wells but do not produce enough water for irrigation ; recent alluvium may yield large quantities of water to wells. In general, the ground water is of good quality, except for hardness and local high-iron concentrations.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1809B","collaboration":"Prepared in cooperation with the University of Wisconsin Geological and Natural History Survey","usgsCitation":"Summers, W.K., 1965, Geology and ground-water resources of Waushara County, Wisconsin: U.S. Geological Survey Water Supply Paper 1809, Report: iv, 32 p.; 3 Plates: 41.96 x 22.00 inches and 39.5 x 22.5 inches, https://doi.org/10.3133/wsp1809B.","productDescription":"Report: iv, 32 p.; 3 Plates: 41.96 x 22.00 inches and 39.5 x 22.5 inches","numberOfPages":"40","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":29216,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29217,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29218,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29219,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809b/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Waushara County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.5977,44.2458],[-89.488,44.244],[-89.4835,44.244],[-89.3649,44.2439],[-89.3464,44.2439],[-89.2469,44.2438],[-89.2245,44.2433],[-89.1288,44.243],[-89.104,44.243],[-89.007,44.2426],[-88.9821,44.243],[-88.8871,44.2426],[-88.8859,44.1587],[-88.8882,44.1136],[-88.8861,44.0713],[-88.8862,43.9833],[-88.944,43.9836],[-89.0063,43.9834],[-89.1283,43.9833],[-89.1658,43.983],[-89.2472,43.9827],[-89.3654,43.9824],[-89.4823,43.982],[-89.598,43.9824],[-89.5981,44.0685],[-89.5976,44.156],[-89.5977,44.2458]]]},\"properties\":{\"name\":\"Waushara\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685374","contributors":{"authors":[{"text":"Summers, William Kelly","contributorId":69532,"corporation":false,"usgs":true,"family":"Summers","given":"William","email":"","middleInitial":"Kelly","affiliations":[],"preferred":false,"id":145756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2818,"text":"wsp1809K - 1965 - Hydrology of melt-water channels in southwestern Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T11:37:22","indexId":"wsp1809K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"K","title":"Hydrology of melt-water channels in southwestern Minnesota","docAbstract":"<p>Melt-water channel deposits are among the most important aquifers in southwestern Minnesota, but permeable zones within the deposits are difficult to locate. Interpretation of the depositional history of proglacial channel deposits from aerial photographs and test-hole samples indicates the position of the permeable zones. Generally, the coarse-grained deposits are in headwater areas, near the confluence of two channels, in bends, or at the junction of sluiceways. Locally, these deposits yield as much as 1,000 gallons per minute to wells.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1809K","collaboration":"Prepared in cooperation with the Division of Waters, Minnesota Department of Conservation, and the Marshall Municipal Utilities","usgsCitation":"Thompson, G.L., 1965, Hydrology of melt-water channels in southwestern Minnesota: U.S. Geological Survey Water Supply Paper 1809, Document: iii, 11 p.; 3 Plates: 22.5 x 24.0 inches or smaller, https://doi.org/10.3133/wsp1809K.","productDescription":"Document: iii, 11 p.; 3 Plates: 22.5 x 24.0 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":138826,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809k/report-thumb.jpg"},{"id":29372,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809k/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29373,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809k/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29374,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809k/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29375,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.83974838256835,\n              44.41207977247278\n            ],\n            [\n              -95.83974838256835,\n              44.4853617812836\n            ],\n            [\n              -95.73469161987305,\n              44.4853617812836\n            ],\n            [\n              -95.73469161987305,\n              44.41207977247278\n            ],\n            [\n              -95.83974838256835,\n              44.41207977247278\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602031","contributors":{"authors":[{"text":"Thompson, Gerald L.","contributorId":61402,"corporation":false,"usgs":true,"family":"Thompson","given":"Gerald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145847,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2870,"text":"wsp1613E - 1965 - Geology and occurrence of fresh and brackish ground water in Glynn County, Georgia","interactions":[],"lastModifiedDate":"2019-12-30T10:05:52","indexId":"wsp1613E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1613","chapter":"E","title":"Geology and occurrence of fresh and brackish ground water in Glynn County, Georgia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1613E","usgsCitation":"Wait, R.L., 1965, Geology and occurrence of fresh and brackish ground water in Glynn County, Georgia: U.S. Geological Survey Water Supply Paper 1613, Report: vi, 94 p.; 4 Plates: 12.00 x 21.50 inches or smaller, https://doi.org/10.3133/wsp1613E.","productDescription":"Report: vi, 94 p.; 4 Plates: 12.00 x 21.50 inches or smaller","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":138966,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1613e/report-thumb.jpg"},{"id":29483,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29484,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29485,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29486,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1613e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29487,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1613e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","county":"Glynn County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.0404052734375,\n              30.949346915468563\n            ],\n            [\n              -81.1505126953125,\n              30.949346915468563\n            ],\n            [\n              -81.1505126953125,\n              31.5504526754715\n            ],\n            [\n              -82.0404052734375,\n              31.5504526754715\n            ],\n            [\n              -82.0404052734375,\n              30.949346915468563\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6848a0","contributors":{"authors":[{"text":"Wait, Robert L.","contributorId":12839,"corporation":false,"usgs":true,"family":"Wait","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145937,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2899,"text":"wsp1801 - 1965 - Geology and availability of ground water in the northern part of the White Sands Missile Range and vicinity, New Mexico","interactions":[],"lastModifiedDate":"2022-01-11T22:38:15.201218","indexId":"wsp1801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1801","title":"Geology and availability of ground water in the northern part of the White Sands Missile Range and vicinity, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1801","usgsCitation":"Weir, J., 1965, Geology and availability of ground water in the northern part of the White Sands Missile Range and vicinity, New Mexico: U.S. Geological Survey Water Supply Paper 1801, Report: v, 78 p.; 1 Plate: 37.00 × 28.00 inches, https://doi.org/10.3133/wsp1801.","productDescription":"Report: v, 78 p.; 1 Plate: 37.00 × 28.00 inches","costCenters":[],"links":[{"id":394227,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24996.htm"},{"id":29565,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1801/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29566,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1801/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138380,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1801/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"White Sands Missile Range and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.872,\n              33.233\n            ],\n            [\n              -106.013,\n              33.233\n            ],\n            [\n              -106.013,\n              33.953\n            ],\n            [\n              -106.872,\n              33.953\n            ],\n            [\n              -106.872,\n              33.233\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686459","contributors":{"authors":[{"text":"Weir, J. E.","contributorId":88715,"corporation":false,"usgs":true,"family":"Weir","given":"J. E.","affiliations":[],"preferred":false,"id":145978,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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