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,{"id":3079,"text":"wsp1904 - 1970 - Surface water supply of the United States, 1961-65, Part 2. South Atlantic slope and eastern Gulf of Mexico, Volume 1. Basins from James River to Savannah River","interactions":[],"lastModifiedDate":"2021-10-20T18:19:29.410377","indexId":"wsp1904","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1904","title":"Surface water supply of the United States, 1961-65, Part 2. South Atlantic slope and eastern Gulf of Mexico, Volume 1. Basins from James River to Savannah River","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1904","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Surface water supply of the United States, 1961-65, Part 2. South Atlantic slope and eastern Gulf of Mexico, Volume 1. Basins from James River to Savannah River: U.S. Geological Survey Water Supply Paper 1904, Report: x, 942 p.; 1 Plate: 27.00 × 26.50 inches, https://doi.org/10.3133/wsp1904.","productDescription":"Report: x, 942 p.; 1 Plate: 27.00 × 26.50 inches","costCenters":[],"links":[{"id":29952,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1904/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390687,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25129.htm"},{"id":29953,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1904/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139417,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1904/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.644,\n              32.05\n            ],\n            [\n              -75.517,\n              32.05\n            ],\n            [\n              -75.517,\n              38.33\n            ],\n            [\n              -83.644,\n              38.33\n            ],\n            [\n              -83.644,\n              32.05\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db69420c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528060,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2479,"text":"wsp01B - 1970 - Detergents and associated contaminants in ground water at three public-supply well fields in southwestern Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp01B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"2001","chapter":"B","title":"Detergents and associated contaminants in ground water at three public-supply well fields in southwestern Suffolk County, Long Island, New York","docAbstract":"Sampling of groups of small-diameter shallow observation wells and nearby public-supply wells screened in the upper glacial aquifer at three well fields showed that detergents (MBAS) were distributed through almost the entire saturated thickness of the aquifer. Concentrations of MBAS in water from all the wells sampled ranged from less than 0.02 to nearly 5 mg/l (milligrams per liter), whereas MBAS concentrations in water pumped from shallow public supply wells ranged from about 0.1 mg/l to about 1.3 mg/l. Upward trends in MBAS concentrations, which were observed at most of the shallow observation wells from 1961 to 1966, nearly stabilized or declined to some extent by 1968. A slight to distinct upward trend in the MBAS content of water pumped from shallow public-supply wells was observed during the same period at two of the three well fields investigated. \r\n\r\nChloride concentrations in the upper glacial aquifer, which ranged from about 5 to 80 mg/l, had a distinct upward trend at some wells apparently due to infiltration of both sewage effluent and deicing salts which were applied to roads in the winter. Nitrate concentrations also increased slightly but remained below the recommended limit for drinking water. \r\n\r\nNo MBAS was detected in water from public-supply wells tapping deeper zones in the underlying Magothy aquifer, and significant amounts of MBAS and associated contaminants are unlikely to reach those zones for many years, if present flow patterns and head relationships are not markedly changed.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp01B","usgsCitation":"Perlmutter, N., and Guerrera, A., 1970, Detergents and associated contaminants in ground water at three public-supply well fields in southwestern Suffolk County, Long Island, New York: U.S. Geological Survey Water Supply Paper 2001, iv, 22 p. :illus. (2 fold. in pocket) ;23 cm., https://doi.org/10.3133/wsp01B.","productDescription":"iv, 22 p. :illus. (2 fold. in pocket) ;23 cm.","costCenters":[],"links":[{"id":138763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2001b/report-thumb.jpg"},{"id":28562,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2001b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28563,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2001b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28564,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2001b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6679cb","contributors":{"authors":[{"text":"Perlmutter, Nathaniel M.","contributorId":32139,"corporation":false,"usgs":true,"family":"Perlmutter","given":"Nathaniel M.","affiliations":[],"preferred":false,"id":145262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guerrera, A.A.","contributorId":86751,"corporation":false,"usgs":true,"family":"Guerrera","given":"A.A.","affiliations":[],"preferred":false,"id":145263,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2477,"text":"wsp1608M - 1970 - Hydrographic and sedimentation survey of Kajakai Reservoir, Afghanistan","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1608M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1608","chapter":"M","title":"Hydrographic and sedimentation survey of Kajakai Reservoir, Afghanistan","docAbstract":"A hydrographic and sedimentation survey of Band-e Kajakai (Kajakai Reservoir) on the Darya-ye Hirmand (Helmand River) was carried out during the period September through December 1968. Underwater mapping techniques were used to determine the reservoir capacity as of 1968. Sediment range lines were established and monumented to facilitate future sedimentation surveys. Afghanistan engineers and technicians were trained to carry out future reservoir surveys. Samples were obtained of the reservoir bed and in the river upstream from the reservoir. Virtually no sediments coarser than about 0.063 millimeter were found on the reservoir bed surface. The median diameter of sands being transported into the reservoir ranged from 0.040 to 0.110 millimeter. The average annual rate of sedimentation was 7,800 acre-feet. Assuming an average density of 50 pounds per cubic foot (800 kilograms per cubic meter), the estimated average sediment inflow to the reservoir was about 8,500,000 tons (7,700,000 metric tons) per year. \r\n\r\nThe decrease in capacity at spillway elevation for the period 1953 to 1968 due to sediment deposition was 7.8 percent, or 117,700 acre-feet. Redefinition of several contours above the fill area resulted in an increase in capacity at spillway elevation of 13,600 acre-feet; thus, the net change in capacity was 7.0 percent, or 104,800 acre-feet. \r\n\r\nBased on current data and an estimated rate of compaction of deposited sediment, the assumption of no appreciable change in hydrologic conditions in the drainage area, the leading edge of the principal delta will reach the irrigation outlet in 40-45 years. \r\n\r\nIt is recommended that a resurvey of sediment range lines be made during the period 1973-75.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1608M","usgsCitation":"Perkins, D.C., and Culbertson, J.K., 1970, Hydrographic and sedimentation survey of Kajakai Reservoir, Afghanistan: U.S. Geological Survey Water Supply Paper 1608, iv, 43 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1608M.","productDescription":"iv, 43 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608m/report-thumb.jpg"},{"id":28553,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608m/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db6146cd","contributors":{"authors":[{"text":"Perkins, Don C.","contributorId":59429,"corporation":false,"usgs":true,"family":"Perkins","given":"Don","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Culbertson, James K.","contributorId":31371,"corporation":false,"usgs":true,"family":"Culbertson","given":"James","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":145258,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1912,"text":"wsp1608K - 1970 - Water resources and related geology of Dera Ismail Khan district, West Pakistan, with reference to the availability of ground water for development","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1608K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1608","chapter":"K","title":"Water resources and related geology of Dera Ismail Khan district, West Pakistan, with reference to the availability of ground water for development","docAbstract":"Dera Ismail (D.I.) Khan District contains an area of 3,450 square miles between the right bank of the Indus River and the Sulaiman Range in westcentral West Pakistan. Agriculture is the principal source of income in the District, but only a small part of the arable land is fully utilized. The region is semiarid and has an average annual rainfall of about 9 inches and a potential evapotranspirational rate of eight to nine times the annual rainfall. Thus, rainfall alone is not adequate for high-intensity cropping. \r\n\r\nIrrigation is practiced near the Indus River; the Paharpur Canal is used, as well as the traditional inundation method. Elsewhere in the District, adequate water is supplied to local areas by karezes, perennial streams from the mountains, and some recently installed tubewells (see 'Glossary'). Further development of ground-water supplies would permit a more effective utilization of most of the presently tilled land and would allow additional land to be farmed. \r\n\r\nD.I. Khan District is primarily an alluvial plain that slopes from the mountain ranges in the northern and western parts of the District toward the Indus River. Rocks in the bordering mountains are of Paleozoic to early or middle Pleistocene age. The unconsolidated rocks of the plain, of middle (?) Pleistocene to Holocene (Recent) age, consist of piedmont deposits derived from the hills to the north and west and of alluvium laid down by the Indus River. These deposits interfinger in a transitional zone about 8 to 12 miles west of the river. Lithologic and structural features indicate that the unconsolidated rocks possibly may be divided into broad units. \r\n\r\nThe investigations in D.I. Khan District have revealed two main areas of potential ground-water development based on considerations of both permeability and chemical quality of the ground water: \r\n\r\n1. A belt about 10 miles wide parallels the Indus River from the Khisor Range southward to the area immediately south of D.I. Khan town. In this belt, the material penetrated by test holes and tubewells consists predominantly of sand, which in tubewells can yield from 2 to 3 cfs (cubic feet per second) of water with only moderate drawdown. Also in this belt, ground water of good chemical quality extends to depths of 1,000 feet or more. \r\n\r\n2. The area from the mouth of the Gumal River gorge to the vicinity of Kot Azam contains sand and gravel strata that may yield from 1 to 3 cfs of water, which contains 500 to 1,500 ppm (parts per million) of total dissolved solids. \r\n\r\nOther marginal parts of the District also contain water of good chemical quality, but developmental prospects are somewhat poorer because of greater depths to water, lower permeabilities, or greater depths to aquifers, all of which would require greater costs in the tubewell installations. The stratification or zoning of water of different chemical qualities to some extent governs the local availability of useful water. Generally, the \r\nground water of poorest quality is found in the shallow zone, and quality improves with depth. The central part of the District, in a belt reaching from the vicinity of Tank southward to the Indus River near Dera Ghfizi Khan District, contains highly mineralized water and few aquifers. The mineralization of water in this belt is due primarily to large concentrations of sodium and sulfate and thus differs from the main part of the Punjab \r\nregion where highly mineralized waters are generally chloride waters. Radical changes in water quality, both horizontally and vertically, are common in the District. Changes in chemical quality of water from large-capacity wells near areas of highly mineralized water are taking place, and further changes may be expected as withdrawals continue and increase in magnitude. Under present conditions, surface-water supplies are fully utilized, and ground water is the largest supply available for development-other than \r\nthat from the Indus River.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1608K","usgsCitation":"Hood, J.W., Khan, L.A., and Jawaid, K., 1970, Water resources and related geology of Dera Ismail Khan district, West Pakistan, with reference to the availability of ground water for development: U.S. Geological Survey Water Supply Paper 1608, viii, 74 p. :ill., maps (2 folded col.) ;24 cm., https://doi.org/10.3133/wsp1608K.","productDescription":"viii, 74 p. :ill., maps (2 folded col.) ;24 cm.","costCenters":[],"links":[{"id":138173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608k/report-thumb.jpg"},{"id":27230,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8887","contributors":{"authors":[{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144354,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Khan, Lutfe Ali","contributorId":102459,"corporation":false,"usgs":true,"family":"Khan","given":"Lutfe","email":"","middleInitial":"Ali","affiliations":[],"preferred":false,"id":144355,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jawaid, Khalid","contributorId":20309,"corporation":false,"usgs":true,"family":"Jawaid","given":"Khalid","email":"","affiliations":[],"preferred":false,"id":144353,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23594,"text":"ofr70188 - 1970 - Preliminary evaluation of availability of potable water on Elliott Key, Dade County, Florida","interactions":[],"lastModifiedDate":"2025-04-25T15:52:38.18466","indexId":"ofr70188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-188","title":"Preliminary evaluation of availability of potable water on Elliott Key, Dade County, Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70188","issn":"0094-9140","usgsCitation":"Preliminary evaluation of availability of potable water on Elliott Key, Dade County, Florida; 1970; OFR; 70-188; Klein, Howard","productDescription":"15 p.","costCenters":[],"links":[{"id":154845,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":484409,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0188/ofr-70010.pdf","text":"Report","size":"350 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"Elliott Key","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.22600826827666,\n              25.39053879054103\n            ],\n            [\n              -80.20163380819311,\n              25.41470470302494\n            ],\n            [\n              -80.20163380819311,\n              25.427591210045037\n            ],\n            [\n              -80.1871676652168,\n              25.455507247990894\n            ],\n            [\n              -80.17507951834631,\n              25.48717337503311\n            ],\n            [\n              -80.1774575144521,\n              25.494507277111623\n            ],\n            [\n              -80.1820153403211,\n              25.49236081551497\n            ],\n            [\n              -80.19529248524452,\n              25.470536279894233\n            ],\n            [\n              -80.19667964963946,\n              25.457833292368335\n            ],\n            [\n              -80.20381363795681,\n              25.442444779323594\n            ],\n            [\n              -80.21253295701119,\n              25.42794914890797\n            ],\n            [\n              -80.21094762627368,\n              25.417389505582804\n            ],\n            [\n              -80.21808161459103,\n              25.408260933001586\n            ],\n            [\n              -80.22581010193458,\n              25.4039648950601\n            ],\n            [\n              -80.23215142488318,\n              25.39573039473997\n            ],\n            [\n              -80.22561193559251,\n              25.388748530423555\n            ],\n            [\n              -80.22600826827666,\n              25.39053879054103\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"1970-10-01","noUsgsAuthors":false,"publicationDate":"1970-10-01","publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d1a","contributors":{"authors":[{"text":"Klein, Howard","contributorId":62189,"corporation":false,"usgs":true,"family":"Klein","given":"Howard","email":"","affiliations":[],"preferred":false,"id":190378,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58094,"text":"wdrWI6812 - 1970 - Water resources data for Wisconsin, 1968; Part 1. Surface water records and Part 2. Water quality records","interactions":[],"lastModifiedDate":"2012-02-02T00:12:32","indexId":"wdrWI6812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WI-68-1-2","title":"Water resources data for Wisconsin, 1968; Part 1. Surface water records and Part 2. Water quality records","language":"ENGLISH","doi":"10.3133/wdrWI6812","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Water resources data for Wisconsin, 1968; Part 1. Surface water records and Part 2. Water quality records: U.S. Geological Survey Water Data Report WI-68-1-2, 222 p., https://doi.org/10.3133/wdrWI6812.","productDescription":"222 p.","numberOfPages":"222","costCenters":[],"links":[{"id":183062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1968/wi-68-1-2/report-thumb.jpg"},{"id":88323,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1968/wi-68-1-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f16be","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533207,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13485,"text":"ofr70117 - 1970 - Schmidt hammer test method for field determination of physical properties of zeolitized tuff","interactions":[],"lastModifiedDate":"2025-12-30T18:37:47.65572","indexId":"ofr70117","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-117","title":"Schmidt hammer test method for field determination of physical properties of zeolitized tuff","docAbstract":"<p>The L-type Schmidt hammer is a hand-carried impact instrument that was originally designed and developed to test the compressive strength of concrete. When properly impacted against a stiff material the device measures the amount of rebound of a spring-loaded hammer, with the rebound of the hammer being directly proportional to the strength of the material tested. Application of this instrument to rock, specifically water-saturated zeolitized tuff, is demonstrated through a set of correlation diagrams that relate Schmidt hammer rebound values, obtained from core samples and from the sites where samples were taken, to physical properties measured on rock samples in the laboratory. The properties include compressive strength, compressional and shear velocities, and dynamic and static Young's shear and bulk moduli. The correlation diagrams apply only to zeolitized tuff of the type found at the Nevada Test Site in its natural state (freshly excavated). These diagrams enable the user of the L-type Schmidt hammer to immediately obtain values of physical properties of such rocks in place, a convenience desirable where conventional sampling is not feasible or is impossible, and when results are required on short notice. The charts apply to L-type hammers that are calibrated to a nominal rebound value of 74. Calibration is made on a 35-pound-(16-kg-) test anvil with a steel-hardened test surface of Brinell hardness = 500 kg/mm<sup>2</sup><span id=\"_mce_caret\" data-mce-bogus=\"1\" data-mce-type=\"format-caret\">.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70117","usgsCitation":"Ege, J.R., Miller, D.R., and Danilchik, W., 1970, Schmidt hammer test method for field determination of physical properties of zeolitized tuff: U.S. Geological Survey Open-File Report 70-117, iv, 37 p., https://doi.org/10.3133/ofr70117.","productDescription":"iv, 37 p.","costCenters":[],"links":[{"id":498187,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0117/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147091,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0117/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd364","contributors":{"authors":[{"text":"Ege, John R.","contributorId":69534,"corporation":false,"usgs":true,"family":"Ege","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":167869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Danny R.","contributorId":75536,"corporation":false,"usgs":true,"family":"Miller","given":"Danny","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":167871,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Danilchik, Walter","contributorId":70390,"corporation":false,"usgs":true,"family":"Danilchik","given":"Walter","email":"","affiliations":[],"preferred":false,"id":167870,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":12148,"text":"ofr70348 - 1970 - Maps showing locations of holes drilled in 1948 to 1956 by U.S. Geological Survey, Slick Rock district, San Miguel County, Colorado","interactions":[],"lastModifiedDate":"2025-07-29T17:26:00.529203","indexId":"ofr70348","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-348","title":"Maps showing locations of holes drilled in 1948 to 1956 by U.S. Geological Survey, Slick Rock district, San Miguel County, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70348","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Maps showing locations of holes drilled in 1948 to 1956 by U.S. Geological Survey, Slick Rock district, San Miguel County, Colorado: U.S. Geological Survey Open-File Report 70-348, Report: 1582 p.; 18 Plates: 46.00 x 24.00 inches or smaller, https://doi.org/10.3133/ofr70348.","productDescription":"Report: 1582 p.; 18 Plates: 46.00 x 24.00 inches or smaller","costCenters":[],"links":[{"id":493120,"rank":24,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8527.htm","linkFileType":{"id":5,"text":"html"}},{"id":95086,"rank":23,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-21.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95066,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95067,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95068,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95069,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95070,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95071,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95072,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95073,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95074,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95076,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95077,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95078,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95079,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95080,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95081,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95082,"rank":19,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95083,"rank":20,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95084,"rank":21,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95085,"rank":22,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-20.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95075,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0348/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145169,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0348/report-thumb.jpg"},{"id":40182,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0348/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"San Miguel County","otherGeospatial":"Slick Rock district","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -109.017,\n              38.058\n            ],\n            [\n              -109.017,\n              37.918\n            ],\n            [\n              -108.721,\n              37.918\n            ],\n            [\n              -108.721,\n              38.058\n            ],\n            [\n              -109.017,\n              38.058\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605baf","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528915,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32671,"text":"pp529E - 1970 - Atlantic Continental Shelf and Slope of the United States - Ostracode zoogeography in the southern Nova Scotian and northern Virginian faunal provinces","interactions":[],"lastModifiedDate":"2022-05-25T11:21:44.229727","indexId":"pp529E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"529","chapter":"E","title":"Atlantic Continental Shelf and Slope of the United States - Ostracode zoogeography in the southern Nova Scotian and northern Virginian faunal provinces","docAbstract":"<p>Ostracodes were identified from 236 bottom samples taken in the region from Nova Scotia to Long Island. There is a distinctive difference between the assemblages in the northern and southern parts of this region. Many sublittoral cryophilic species are not present south of Cape Cod or the Northeast Channel, and several thermophilic species a.re not .found north of Cape Cod or Georges Bank. The ostracode assemblages in the southern part of the cold-temperate Nova Scotian province are a mixture of amphiatlantic cryophilic species and endemic, mainly thermophilic species; European forms make up approximately 50 percent of the species. Less than 25 percent of the species known from the mild-temperate Virginian province have been reported from European waters. More endemic species pass Cape Cod from the south than amphiatlantic cryophilic species do from the north. This is consistent with the fact that summer isotherms are more compressed than winter isotherms in the Cape Cod region, and the southern limit of distribution of most amphiatlantic species is regulated by summer high temperatures. The distribution data on which these interpretations are based are presented in a series of .figures and over 60 species distribution maps. </p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp529E","usgsCitation":"Hazel, J.E., 1970, Atlantic Continental Shelf and Slope of the United States - Ostracode zoogeography in the southern Nova Scotian and northern Virginian faunal provinces: U.S. Geological Survey Professional Paper 529, Report: v,  21 p.; 69 Plates, https://doi.org/10.3133/pp529E.","productDescription":"Report: v,  21 p.; 69 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,{"id":5693,"text":"ofr7025 - 1970 - A proposed streamflow data program for Michigan","interactions":[],"lastModifiedDate":"2016-10-13T15:49:29","indexId":"ofr7025","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-25","title":"A proposed streamflow data program for Michigan","docAbstract":"<p>An evaluation of the streamflow data available in Michigan was made to provide guidelines for planning future water resource programs. 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A streamflow data program based on the guidelines developed in this rstudy is proposed for the future. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr7025","usgsCitation":"Bent, P., 1970, A proposed streamflow data program for Michigan: U.S. Geological Survey Open-File Report 70-25, Document: v, 69 p.; 2 Plates: 20.04 x 23.00 inches and 19.94 x 23.77 inches, https://doi.org/10.3133/ofr7025.","productDescription":"Document: v, 69 p.; 2 Plates: 20.04 x 23.00 inches and 19.94 x 23.77 inches","costCenters":[{"id":382,"text":"Michigan Water Science 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,{"id":1843,"text":"wsp1473 - 1970 - Study and interpretation of the chemical characteristics of natural water","interactions":[],"lastModifiedDate":"2018-03-08T12:58:39","indexId":"wsp1473","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1473","title":"Study and interpretation of the chemical characteristics of natural water","docAbstract":"<p>The chemical composition of natural water is derived from many different sources of solutes, including gases and aerosols from the atmosphere, weathering and erosion of rocks and soil, solution or precipitation reactions occurring below the land surface, and cultural effects resulting from activities of man. Some of the processes of solution or precipitation of minerals can be closely evaluated by means of principles of chemical equilibrium including the law of mass action and the Nernst equation. Other processes are irreversible and require consideration of reaction mechanisms and rates. The chemical composition of the crustal rocks of the earth and the composition of the ocean and the atmosphere are significant in evaluating sources of solutes in natural fresh water.</p>\n<p>The ways in which solutes are taken up or precipitated and the amounts present in solution are influenced by many environmental factors, especially climate, structure and position: of rock strata, and biochemical effects associated with life cycles of plants and animals, both microscopic and macroscopic. Taken all together and in application with the further influence of the general circulation of all water in the hydrologic cycle, the chemical principles and environmental factors form a basis for the developing science of natural-water chemistry.</p>\n<p>Fundamental data used in the determination of water quality are obtained by the chemical analysis of water samples in the laboratory or onsite sensing of chemical properties in the field. Sampling is complicated by changes in composition of moving water and the effects of particulate suspended material. Most of the constituents determined are reported in gravimetric units, usually milligrams per liter or milliequivalents per liter.</p>\n<p>More than 60 constituents and properties are included in water analyses frequently enough to provide a basis for consideration of the sources from which each is generally derived, most probable forms of elements and ions in solution, solubility controls, expected concentration ranges and other chemical factors. Concentrations of elements that are commonly present in amounts less than a few tens of micrograms per liter cannot always be easily explained, but present information suggests many are controlled by solubility of hydroxide or carbonate or by sorption on solid particles.</p>\n<p>Chemical analyses may be grouped and statistically evaluated by averages, frequency distributions, or ion correlations to summarize large volumes of data. Graphing of analyses or of groups of analyses aids in showing chemical relationships among waters, probable sources of solutes, areal water-quality regimen, and water-resources evaluation. Graphs may show water type based on chemical composition, relationships among ions, or groups of ions in individual waters or&nbsp;many waters considered simultaneously. The relationships of water quality to hydrologic parameters, such as stream discharge rate or ground-water flow patterns, can be shown by mathematical equations, graphs, and maps.</p>\n<p>About 75 water analyses selected from the literature are tabulated to illustrate the relationships described, and some of these, along with many others that are not tabulated, are also utilized in demonstrating graphing and mapping techniques.</p>\n<p>Relationships of water composition to source rock type are illustrated by graphs of some of the tabulated analyses. Activities of man may modify water composition extensively through direct effects of pollution and indirect results of water development, such as intrusion of sea water in ground-water aquifiers.</p>\n<p>Water-quality standards for domestic, agricultural, and industrial use have been published by various agencies. Irrigation project requirements for water quality are particularly intricate.</p>\n<p>Fundamental knowledge of processes that control natural water composition is required for rational management of water quality.&nbsp;</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1473","usgsCitation":"Hem, J.D., 1970, Study and interpretation of the chemical characteristics of natural water (2nd edition): U.S. Geological Survey Water Supply Paper 1473, xiv, 363 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1473.","productDescription":"xiv, 363 p. :ill., maps ;24 cm.","startPage":"1","endPage":"363","numberOfPages":"380","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":532,"text":"Pennsylvania Water Science 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,{"id":47919,"text":"ofr7146 - 1970 - Water temperatures of California streams, north coastal subregion","interactions":[],"lastModifiedDate":"2012-02-02T00:10:03","indexId":"ofr7146","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"71-46","title":"Water temperatures of California streams, north coastal subregion","language":"ENGLISH","doi":"10.3133/ofr7146","usgsCitation":"Blodgett, J.C., 1970, Water temperatures of California streams, north coastal subregion: U.S. Geological Survey Open-File Report 71-46, 92 p. : tables ; 27 cm., https://doi.org/10.3133/ofr7146.","productDescription":"92 p. : tables ; 27 cm.","costCenters":[],"links":[{"id":162916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd20c","contributors":{"authors":[{"text":"Blodgett, J. C.","contributorId":32154,"corporation":false,"usgs":true,"family":"Blodgett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":236528,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56016,"text":"ofr70193 - 1970 - Summary of ground-water occurrence in California","interactions":[],"lastModifiedDate":"2012-02-02T00:12:07","indexId":"ofr70193","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-193","title":"Summary of ground-water occurrence in California","language":"ENGLISH","doi":"10.3133/ofr70193","usgsCitation":"Kunkel, F., 1970, Summary of ground-water occurrence in California: U.S. Geological Survey Open-File Report 70-193, 10 p., 1 fig., https://doi.org/10.3133/ofr70193.","productDescription":"10 p., 1 fig.","costCenters":[],"links":[{"id":181787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6991d1","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":254645,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63894,"text":"gp705 - 1970 - Aeromagnetic map of the Maynard quadrangle, Middlesex County, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-10T00:10:56","indexId":"gp705","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"705","title":"Aeromagnetic map of the Maynard quadrangle, Middlesex County, Massachusetts","language":"ENGLISH","doi":"10.3133/gp705","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Aeromagnetic map of the Maynard quadrangle, Middlesex County, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 705, 1 map., https://doi.org/10.3133/gp705.","productDescription":"1 map.","costCenters":[],"links":[{"id":250194,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0705/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":250195,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0705/plate-1.pdf","size":"4022","linkFileType":{"id":1,"text":"pdf"}},{"id":253663,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0705/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.5,42.3675 ], [ -71.5,42.5 ], [ -71.36749999999999,42.5 ], [ -71.36749999999999,42.3675 ], [ -71.5,42.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691e28","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3138,"text":"wsp1961 - 1970 - Quality of surface waters of the United States, 1965. Parts 1 and 2. north Atlantic Slope Basins and South Atlantic Slope and Eastern Gulf of Mexico Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"wsp1961","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1961","title":"Quality of surface waters of the United States, 1965. Parts 1 and 2. north Atlantic Slope Basins and South Atlantic Slope and Eastern Gulf of Mexico Basins","language":"ENGLISH","publisher":"United States Govt. Print. Off.,","doi":"10.3133/wsp1961","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Quality of surface waters of the United States, 1965. Parts 1 and 2. north Atlantic Slope Basins and South Atlantic Slope and Eastern Gulf of Mexico Basins: U.S. Geological Survey Water Supply Paper 1961, xiii, 779p ;23 cm., https://doi.org/10.3133/wsp1961.","productDescription":"xiii, 779p ;23 cm.","costCenters":[],"links":[{"id":139428,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1961/report-thumb.jpg"},{"id":30049,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1961/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651a00","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528103,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":954,"text":"wsp1798G - 1970 - Sedimentation in Plum Creek subwatershed no. 4, Shelby County, north-central Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1798G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1798","chapter":"G","title":"Sedimentation in Plum Creek subwatershed no. 4, Shelby County, north-central Kentucky","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1798G","usgsCitation":"Anttila, P.W., 1970, Sedimentation in Plum Creek subwatershed no. 4, Shelby County, north-central Kentucky: U.S. Geological Survey Water Supply Paper 1798, iv, 54 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1798G.","productDescription":"iv, 54 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":110023,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24990.htm","linkFileType":{"id":5,"text":"html"},"description":"24990"},{"id":138074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1798g/report-thumb.jpg"},{"id":25475,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1798g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1798g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbc7a","contributors":{"authors":[{"text":"Anttila, Peter W.","contributorId":27423,"corporation":false,"usgs":true,"family":"Anttila","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":142911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23351,"text":"ofr70162 - 1970 - Sources of pesticides in Florida waters","interactions":[],"lastModifiedDate":"2012-02-02T00:08:18","indexId":"ofr70162","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-162","title":"Sources of pesticides in Florida waters","language":"ENGLISH","publisher":"United States Department of the Interior, Geological Survey, Water Resources Division,","doi":"10.3133/ofr70162","issn":"0094-9140","usgsCitation":"Higer, A., and Kolipinski, M., 1970, Sources of pesticides in Florida waters: U.S. Geological Survey Open-File Report 70-162, 20 p. :map ;27 cm., https://doi.org/10.3133/ofr70162.","productDescription":"20 p. :map ;27 cm.","costCenters":[],"links":[{"id":157361,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e75d7","contributors":{"authors":[{"text":"Higer, A.L.","contributorId":8501,"corporation":false,"usgs":true,"family":"Higer","given":"A.L.","affiliations":[],"preferred":false,"id":189950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kolipinski, M.C.","contributorId":68769,"corporation":false,"usgs":true,"family":"Kolipinski","given":"M.C.","affiliations":[],"preferred":false,"id":189951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67910,"text":"ha339 - 1970 - Water resources of the Wild Rice River watershed, northwestern Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T12:07:55","indexId":"ha339","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"339","title":"Water resources of the Wild Rice River watershed, northwestern Minnesota","docAbstract":"<p>The Wild Rice watershed includes two general physiographic areas- the glacial Lake Agassiz Plain and a glacial moraine.</p>\n<p>The lake plain is extremely flat in the western part, sloping only a few feet per mile, but in the eastern part the plain is traversed in a north-south direction by long, narrow beach ridges up to 20 feet high. The moraine is an area of hills and depressions. The local relief is low in the western part of the moraine but increases to more than 200 feet in the east. Altitude of the land surface ranges from 800 feet above mean sea level where the Red River flows north out of the area to 2,040 feet near the southeastern edge of the watershed (one of the highest points in Minnesota).</p>\n<p>The area of the watershed is about 2,600 square miles and includes most of Mahnomen and Norman Counties and parts of Becker, Clay, Clearwater, and Polk Counties. The population of the area is about 37,000 people of which about 70 percent live on farms. The economy is based principally on farming. The area of lake clay and silt is used mostly for raising sugar beets and wheat; and potatoes are grown largely on the sandy soils. In the western part of the morainal area small grain, dairy, and cattle farming is the most common. The eastern part of the morainal area is important for forest products and recreation. Industries in the area are small and are based on agricultural processing and service.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha339","collaboration":"Prepared in cooperation with the Minnesota Department of Conservation, Division of Waters, Soils, and Minerals","usgsCitation":"Winter, T.C., Bidwell, L.E., and Maclay, R.W., 1970, Water resources of the Wild Rice River watershed, northwestern Minnesota: U.S. Geological Survey Hydrologic Atlas 339, Document: 1 p. 4 Plates: 41.66 x 40.27 inches or smaller, https://doi.org/10.3133/ha339.","productDescription":"Document: 1 p. 4 Plates: 41.66 x 40.27 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":101437,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/339/plate-1.pdf","size":"8948","linkFileType":{"id":1,"text":"pdf"}},{"id":101436,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/339/report.pdf","size":"42","linkFileType":{"id":1,"text":"pdf"}},{"id":101438,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/339/plate-2.pdf","size":"7443","linkFileType":{"id":1,"text":"pdf"}},{"id":101439,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/339/plate-3.pdf","size":"7660","linkFileType":{"id":1,"text":"pdf"}},{"id":101440,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/339/plate-4.pdf","size":"6766","linkFileType":{"id":1,"text":"pdf"}},{"id":189361,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/339/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Minnesota","otherGeospatial":"Wild Rice River watershed","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97,47 ], [ -97,47.5 ], [ -95.5,47.5 ], [ -95.5,47 ], [ -97,47 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f02df","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277303,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bidwell, L. E.","contributorId":100029,"corporation":false,"usgs":true,"family":"Bidwell","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":277304,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maclay, Robert W.","contributorId":13210,"corporation":false,"usgs":true,"family":"Maclay","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277302,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3777,"text":"cir625 - 1970 - Gold content of water, plants, and animals","interactions":[],"lastModifiedDate":"2017-06-25T12:55:06","indexId":"cir625","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"625","title":"Gold content of water, plants, and animals","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir625","usgsCitation":"Jones, R.S., 1970, Gold content of water, plants, and animals: U.S. Geological Survey Circular 625, iii, 15 p. ;26 cm., https://doi.org/10.3133/cir625.","productDescription":"iii, 15 p. ;26 cm.","costCenters":[],"links":[{"id":116996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1970/0625/report-thumb.jpg"},{"id":30848,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1970/0625/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4cd4","contributors":{"authors":[{"text":"Jones, Robert Sprague","contributorId":41814,"corporation":false,"usgs":true,"family":"Jones","given":"Robert","email":"","middleInitial":"Sprague","affiliations":[],"preferred":false,"id":147583,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4805,"text":"pp713 - 1970 - Mercury in the environment","interactions":[],"lastModifiedDate":"2012-02-02T00:05:44","indexId":"pp713","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"713","title":"Mercury in the environment","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/pp713","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Mercury in the environment: U.S. Geological Survey Professional Paper 713, 67 p., https://doi.org/10.3133/pp713.","productDescription":"67 p.","costCenters":[],"links":[{"id":117055,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0713/report-thumb.jpg"},{"id":31766,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0713/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624cf4","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528382,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":941,"text":"wsp1850A - 1970 - Floods of March-May 1965 in the upper Mississippi River basin","interactions":[{"subject":{"id":52498,"text":"ofr65145 - 1965 - The 1965 Mississippi River flood in Iowa","indexId":"ofr65145","publicationYear":"1965","noYear":false,"title":"The 1965 Mississippi River flood in Iowa"},"predicate":"SUPERSEDED_BY","object":{"id":941,"text":"wsp1850A - 1970 - Floods of March-May 1965 in the upper Mississippi River basin","indexId":"wsp1850A","publicationYear":"1970","noYear":false,"chapter":"A","title":"Floods of March-May 1965 in the upper Mississippi River basin"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1850A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1850","chapter":"A","title":"Floods of March-May 1965 in the upper Mississippi River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1850A","usgsCitation":"Anderson, D., and Burmeister, I., 1970, Floods of March-May 1965 in the upper Mississippi River basin: U.S. Geological Survey Water Supply Paper 1850, v, 448 p., https://doi.org/10.3133/wsp1850A.","productDescription":"v, 448 p.","costCenters":[],"links":[{"id":137218,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1850a/report-thumb.jpg"},{"id":25427,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1850a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfb54","contributors":{"authors":[{"text":"Anderson, D.B.","contributorId":47762,"corporation":false,"usgs":true,"family":"Anderson","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":142893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burmeister, I.L.","contributorId":85944,"corporation":false,"usgs":true,"family":"Burmeister","given":"I.L.","email":"","affiliations":[],"preferred":false,"id":142894,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3842,"text":"cir601E - 1970 - Sediment problems in urban areas","interactions":[],"lastModifiedDate":"2018-03-12T11:43:54","indexId":"cir601E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"601","chapter":"E","title":"Sediment problems in urban areas","docAbstract":"<p>A recognition of and solution to sediment problems in urban areas is necessary if society is to have an acceptable living environment. Soil erosion and sediment deposition in urban areas are as much an environmental blight as badly paved and littered streets, dilapidated buildings, billboard clutter, inept land use, and air, water, and noise pollution. In addition, sediment has many direct and indirect effects on streams that may be either part of or very remote from the urban environment. Sediment, for example, is widely recognized as a pollutant of streams and other water bodies.</p>\n<p>One obstacle to a scientific recognition and an engineering solution to sediment-related environmental problems is that such problems are bound in conflicting and generally undefinable political and institutional restraints. Also, some of the difficulty may involve the fact that the scientist or engineer, because of his relatively narrow field of investigation, cannot always completely envision the less desirable effects of his work and communicate alternative solutions to the public. For example, the highway and motor-vehicle engineers have learned how to provide the means by which one can transport himself from one point to another with such great efficiency that a person's employment in this country is now commonly more than 5 miles from his residence. However, providing such efficient personal transport has created numerous serious environmental problems. Obstacles to recognition of and action to control sediment problems in and around urban areas are akin to other environmental problems with respect to the many scientific, engineering, economic, and social aspects.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir601E","usgsCitation":"Guy, H., 1970, Sediment problems in urban areas: U.S. Geological Survey Circular 601, v, 8 p., https://doi.org/10.3133/cir601E.","productDescription":"v, 8 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":30915,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1970/0601e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118396,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1970/0601e/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbfca","contributors":{"authors":[{"text":"Guy, Harold P.","contributorId":6434,"corporation":false,"usgs":true,"family":"Guy","given":"Harold P.","affiliations":[],"preferred":false,"id":147707,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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