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,{"id":33923,"text":"b1317B - 1970 - Peat deposits of southeastern New York","interactions":[],"lastModifiedDate":"2012-02-02T00:09:28","indexId":"b1317B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1317","chapter":"B","title":"Peat deposits of southeastern New York","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1317B","usgsCitation":"Cameron, C.C., 1970, Peat deposits of southeastern New York: U.S. Geological Survey Bulletin 1317, 32 p, https://doi.org/10.3133/b1317B.","productDescription":"32 p","costCenters":[],"links":[{"id":163440,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1317b/report-thumb.jpg"},{"id":61809,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1317b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4412","contributors":{"authors":[{"text":"Cameron, Cornelia Clermont","contributorId":20737,"corporation":false,"usgs":true,"family":"Cameron","given":"Cornelia","email":"","middleInitial":"Clermont","affiliations":[],"preferred":false,"id":212178,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1670,"text":"wsp1984 - 1970 - Hydrologic effects of floodwater-retarding structures on Garza-Little Elm Reservoir, Texas","interactions":[],"lastModifiedDate":"2023-03-14T20:01:38.704886","indexId":"wsp1984","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":"1984","title":"Hydrologic effects of floodwater-retarding structures on Garza-Little Elm Reservoir, Texas","docAbstract":"<p>The Texas District of the Water Resources Division of the U.S. Geological Survey has collected and analyzed hydrologic data since 1953 to define the effects of systems of floodwater-retarding structures on downstream water and sediment yield. The district project includes 11 study areas ranging from 18 to 80 square miles in size and from 0 to 67 in percent of study area controlled by floodwaterretarding structures. The 11 study areas are within that part of Texas where the west-to-east average annual runoff ranges from about 2 to 7 inches. This report presents results of analyses, development of methodolgy, and results of application of methods for defining the downstream effects of systems of floodwaterretarding structures.</p>\n<p>Annual inflow to and outflow from the system of floodwater-retarding reservoirs in seven of the 11 study areas were found to be related by the equation: O=0.98/ 0.68, where O is annual outflow, in inches, and / is annual net inflow, in inches. Transmission loss of structure outflow to the downstream study-area stream-gaging station was determined and compared with the transmission loss of natural flood flow between tandem stream-gaging stations on Denton Creek, a tributary to Elm Fork Trinity River above Dallas.</p>\n<p>Trap efficiency of most floodwater-retarding structures was found by the U.S. Soil Conservation Service to be about 97 percent. Downstream increases in suspended-sediment concentration in the outflow were found to be large in a study area with mostly silt and clay sediments, but even a large increase in suspendedsediment concentration did not represent a significant quantitative pickup of sediment by the outflow water.</p>\n<p>Water consumption in floodwater-retarding reservoirs from the combined actions of evaporation, evapotranspiration, and seepage was found to be as much as twice the average annual consumption attributable to evaporation alone. Average annual consumption in reservoirs in the seven study areas analyzed ranged from 1.57 inches of equivalent runoff in the easternmost study area, where annual runoff averaged 6.96 inches, to 0.77 inch of equivalent runoff in the westernmost study area, where the average annual runoff was 2.35 inches. The effect of consumption on downstream flow is partially offset by rainfall on pool surface. Studies covering as much as 15 years of streamflow record at the stream-gaging&nbsp;stations that gage outflow from the Deep and Honey Creek study areas indicated no increase in base flow.</p>\n<p>Multiple-linear-regression techniques were used in developing methodology to determine reservoir consumption in seven study areas. The physical and climatic fnctors influencing consumption were grouped as variables in regard to their relative effect on the actions of evaporation, evapotranspiration, and seepage. The resulting generalized equation was then used in synthesizing the consumptive effects of a planned system of 162 floodwater-retarding reservoirs controlling 26 percent of a 1,660-square-mile drainage basin upstream from a major water-supply reservoir. The analyses were based on the assumption that all water consumed at the floodwater-retarding reservoirs would have reached the downstream watersupply reservoir. Water-sediment discharge relationships were derived for the runoff into the structures as well as for the runoff through and below the structures. A mathematical response model of the floodwater-retarding reservoir systems and the entire drainage basin was computer programed to yield monthly water and sediment inflow to the water-supply reservoir.</p>\n<p>Results of the response model showed that with full development, depletion of annual yield to the large reservoir would be as much as 10 percent in the early years; but after the permanent pools of the floodwater-retarding structures had mostly filled with sediment, depletion of annual yield would be generally less than 1 percent. The depletion of yield to Garza-Little Elm Reservoir during the 39-year synthesized period of study was estimated as 296,800 acre-feet out of 18,256,000 acre-feet total yield. During the same period, the floodwater-retarding structures were estimated to have kept 19,700 acre-feet of sediment from being deposited in the reservoir.</p>\n<p>\"Firm\"- or \"critical\"-yield studies were made of the large reservoir on the basis of two sets of conditions : with floodwater-retarding structures in the drainage basin, and without such structures. Results of the firm-yield studies indicated that with full development, annual firm yield would be initially reduced by 10 percent. After 30 or more years, when the permanent pools of the floodwaterretarding reservoirs would be mostly filled with sediment, the firm yield would be almost the same with or without the upstream development.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1984","usgsCitation":"Gilbert, C.R., and Sauer, S.P., 1970, Hydrologic effects of floodwater-retarding structures on Garza-Little Elm Reservoir, Texas: U.S. Geological Survey Water Supply Paper 1984, Report: vii, 95 p.; 3 Plates: 39.48 x 33.34 inches or smaller, https://doi.org/10.3133/wsp1984.","productDescription":"Report: vii, 95 p.; 3 Plates: 39.48 x 33.34 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":414124,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25366.htm","linkFileType":{"id":5,"text":"html"}},{"id":94719,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1984/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":94718,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1984/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138233,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1984/report-thumb.jpg"},{"id":26745,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1984/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":94717,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1984/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Garza-Little Elm Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -96.775,\n              33.083\n            ],\n            [\n              -96.775,\n              33.625\n            ],\n            [\n              -97.617,\n              33.625\n            ],\n            [\n              -97.617,\n              33.083\n            ],\n            [\n              -96.775,\n              33.083\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db60703b","contributors":{"authors":[{"text":"Gilbert, Clarence R.","contributorId":30965,"corporation":false,"usgs":true,"family":"Gilbert","given":"Clarence","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sauer, Stanley P.","contributorId":38966,"corporation":false,"usgs":true,"family":"Sauer","given":"Stanley","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":143951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3030,"text":"wsp1899G - 1970 - Measurement of mixing characteristics of the Missouri River between Sioux City, Iowa, and Plattsmouth, Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:46","indexId":"wsp1899G","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":"1899","chapter":"G","title":"Measurement of mixing characteristics of the Missouri River between Sioux City, Iowa, and Plattsmouth, Nebraska","docAbstract":"Measurements of longitudinal dispersion, transverse mixing, channel geometry, and transverse velocity distribution were made in the Missouri River at a flow of about 33,000 cubic feet per second. The results show that the longitudinal dispersion coefficient for the 141-mile reach from Sioux City, Iowa, to Plattsmouth, Nebr., is about 16,000 square feet per second (approximately 5,600 U*d, where U* is the shear velocity and d is mean depth). The transverse mixing coefficient, Ez, for a 6-mile reach immediately downstream from Blair, Nebr., is about 1.3 square feet per second (approximately 0.6 U*d). The value of the longitudinal dispersion coefficient is one of the largest ever measured, and the value of the ratio Ez/U*d is approximately three times as large as that frequently reported for small straight channels.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1899G","usgsCitation":"Yotsukura, N., Fischer, H.B., and Sayre, W., 1970, Measurement of mixing characteristics of the Missouri River between Sioux City, Iowa, and Plattsmouth, Nebraska: U.S. Geological Survey Water Supply Paper 1899, iv, 29 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1899G.","productDescription":"iv, 29 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":139524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1899g/report-thumb.jpg"},{"id":29861,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1899g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db6110ff","contributors":{"authors":[{"text":"Yotsukura, Nobuhiro","contributorId":81884,"corporation":false,"usgs":true,"family":"Yotsukura","given":"Nobuhiro","email":"","affiliations":[],"preferred":false,"id":146174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fischer, Hugo B.","contributorId":36542,"corporation":false,"usgs":true,"family":"Fischer","given":"Hugo","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146173,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sayre, William W.","contributorId":93894,"corporation":false,"usgs":true,"family":"Sayre","given":"William W.","affiliations":[],"preferred":false,"id":146175,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2124,"text":"wsp1983 - 1970 - An appraisal of ground water for irrigation in the Wadena area, central Minnesota","interactions":[{"subject":{"id":55910,"text":"ofr69150 - 1969 - An appraisal of ground water for irrigation in the Wadena area, central Minnesota","indexId":"ofr69150","publicationYear":"1969","noYear":false,"title":"An appraisal of ground water for irrigation in the Wadena area, central Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":2124,"text":"wsp1983 - 1970 - An appraisal of ground water for irrigation in the Wadena area, central Minnesota","indexId":"wsp1983","publicationYear":"1970","noYear":false,"title":"An appraisal of ground water for irrigation in the Wadena area, central Minnesota"},"id":1}],"lastModifiedDate":"2018-03-12T13:14:40","indexId":"wsp1983","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":"1983","title":"An appraisal of ground water for irrigation in the Wadena area, central Minnesota","docAbstract":"<p>The Wadena area is part of a large sandy plain in central Minnesota whose soils have low water-holding capacity. Drought conditions which adversely affect plant growth frequently occur in the summer when moisture is most needed. To reduce the risk of crop failure in the area supplemental irrigation is on the increase.</p>\n<p>This study was made to evaluate the ground-water resources of the area and to determine possible effects of development on them. About half the area's approximately 102,000 acres is considered irrigable at the present time. In 1967, about 1,100 acres were under irrigation.</p>\n<p>Outwash sand and gravel, which forms the water-table aquifer, is the main source of water presently known. Saturated thickness ranges from 0 to 70 feet and averages about 36 feet. Sandy till underlies the outwash. Within the till are sand and gravel lenses whose distribution and water-yielding characteristics were not determined.</p>\n<p>Average annual precipitation at the U.S. Weather Bureau station in Wadena from 1934 to 1967 was 26.4 inches, of which about 22.5 inches was lost by evapotranspiration, and the balance of 3.9 inches was surface runoff. Even in wet years, evapotranspiration during the .summer months exceeds precipitation, and a moisture deficiency for optimum plant growth occurs.</p>\n<p>In 1967, about 8 inches of the total precipitation of 19.3 inches reached the water table. Recharge to the water table in 1967 was about 70,000 acre-feet.</p>\n<p>Result of field aquifer (pumping) tests were used to estimate transmissivity values at test-hole sites. Information gained by auger test drilling was the basis for estimating transmissivity values elsewhere. Transmissivity of the watertable aquifer in most of the Wadena area ranges from 15,000 to 120,000 gallons per day per foot. A map was prepared to show the maximum yield, in gallons per minute, which might be obtained from individual wells completed in the water-table aquifer. The map indicates that in about 60 percent of the area, individual wells can be pumped at rates greater than 300 gallons per minute for a 30-day period if drawdown in the pumped well is two-thirds the saturated thickness after correction for dewatering.</p>\n<p>Quality of both ground and surface waters is such that they are well suited for irrigation. Locally, nitrate concentrations in ground water, in excess of the U.S. Public Health Service's drinking water standards, might be related to a local source of organic pollution or to the increased use of fertilizers which accompanies irrigation.</p>\n<p>An electric analog model of the water-table aquifer in the Wadena area was built and used to analyze possible effects of ground-water development of the hydrologic system. The model was designed to .simulate existing hydrologic conditions and used to predict changes in the system which might result from development. The withdrawal of large quantities of ground water would lower the water table, thereby reducing evapotranspiration losses and making more water available for beneficial use. Additional water would be salvaged when normal ground-water discharge to streams is intercepted by pumping from wells.</p>\n<p>Analyses were made to determine effects of development on ground-water levels under different development schemes both after a single irrigation season and after 5 and 20 successive years of irrigation. Where development is concentrated, some interference between wells can be expected. Although water levels recover rapidly when pumps are shut off, recovery will not be complete prior to the next irrigation season in heavily developed areas. After several years of watertable lowering, yields from wells will decrease because of deceased saturated thickness, unless climatic changes result in abnormally high amounts of recharge.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1983","collaboration":"Prepared in cooperation with the West Central Minnesota Resource Conservation and Development Project and the Minnesota Department of Conservation, Division of Waters, Soils and Minerals","usgsCitation":"Lindholm, F., 1970, An appraisal of ground water for irrigation in the Wadena area, central Minnesota: U.S. Geological Survey Water Supply Paper 1983, Document: v, 56 p.; 12 Plates: 24 x 19 inches or smaller, https://doi.org/10.3133/wsp1983.","productDescription":"Document: v, 56 p.; 12 Plates: 24 x 19 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":27719,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27720,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27723,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27722,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27724,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1983/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27712,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27713,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138257,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1983/report-thumb.jpg"},{"id":27721,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27714,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27715,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27716,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27717,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27718,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1983/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Wadena area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.25,\n              46.541667\n            ],\n            [\n              -95.25,\n              46.316667\n            ],\n            [\n              -94.75,\n              46.316667\n            ],\n            [\n              -94.75,\n              46.541667\n            ],\n            [\n              -95.25,\n              46.541667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685a66","contributors":{"authors":[{"text":"Lindholm, F.G.","contributorId":41807,"corporation":false,"usgs":true,"family":"Lindholm","given":"F.G.","email":"","affiliations":[],"preferred":false,"id":144705,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3369,"text":"cir629 - 1970 - Water laws and concepts","interactions":[],"lastModifiedDate":"2017-06-25T12:59:32","indexId":"cir629","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":"629","title":"Water laws and concepts","docAbstract":"Throughout human history various laws and customs have developed concerning the individual rights and rights in common to the waters of the earth. Many existing laws and concepts are clearly influenced by the environment in which they originated and reflect the relative abundance or scarcity of water. Many concepts reflect the people's original interests in the water and once established have been passed from generation to generation with little modification. Some laws and concepts have been carried by people in their migrations and colonial expansions to vastly different environments, with rather curious consequences. In many places water laws that had been well adapted to the natural environment have become less tenable because of man's activities in modifying that environment, or because of increasing use of water: Increasing consumptive use shifts the water economy toward lesser abundance or increasing deficiency; increasing nonconsumptive use results in pollution of the water resources, so that they become less suitable for other users. The water-rights systems in the United States vary from State to State: some are reasonably fitted to their environment, some have outlived their place in history, some are wasteful of water, some show favoritism to certain special interests or segments of the population. Water-use rights are universally recognized as real property, with constitutional protection against deprivation without due process of law.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir629","usgsCitation":"Thomas, H.E., 1970, Water laws and concepts: U.S. Geological Survey Circular 629, iii, 18 p. ;26 cm., https://doi.org/10.3133/cir629.","productDescription":"iii, 18 p. ;26 cm.","costCenters":[],"links":[{"id":30379,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1970/0629/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124564,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1970/0629/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a081","contributors":{"authors":[{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146733,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6261,"text":"pp635 - 1970 - Uppermost Cretaceous and Tertiary stratigraphy of Fossil basin, southwestern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:44","indexId":"pp635","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":"635","title":"Uppermost Cretaceous and Tertiary stratigraphy of Fossil basin, southwestern Wyoming","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp635","usgsCitation":"Oriel, S.S., and Tracey, J.I., 1970, Uppermost Cretaceous and Tertiary stratigraphy of Fossil basin, southwestern Wyoming: U.S. Geological Survey Professional Paper 635, 53 p., https://doi.org/10.3133/pp635.","productDescription":"53 p.","costCenters":[],"links":[{"id":139596,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0635/report-thumb.jpg"},{"id":112784,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0635/report.pdf","size":"12940","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db60644d","contributors":{"authors":[{"text":"Oriel, Steven S.","contributorId":108079,"corporation":false,"usgs":true,"family":"Oriel","given":"Steven","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":152398,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracey, Joshua I. Jr.","contributorId":55420,"corporation":false,"usgs":true,"family":"Tracey","given":"Joshua","suffix":"Jr.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":152397,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56037,"text":"ofr70232 - 1970 - Artificial recharge, Yucaipa, California","interactions":[],"lastModifiedDate":"2020-02-07T08:24:16","indexId":"ofr70232","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":"70-232","title":"Artificial recharge, Yucaipa, California","docAbstract":"<p>The Yucaipa area is a small alluvial-filled basin bordered on three sides by crystalline bedrock. Several faults that transect the alluvial deposits retard the flow of ground water and divide the area into seven separate ground-water subbasins. Each of the subbasins was evaluated as a potential recharge site, and Wilson Creek subbasin was selected as the most favorable. The study indicates that artificial recharge of 6,000 acre-feet per year should be possible through surface spreading in Wilson Creek subbasin.</p><p>The test drilling and infiltration test conducted at the Yucaipa damsite indicate that material underlying the site is highly permeable and readily transmits water. An unlined reservoir at this site would initially lose a considerable quantity of water through infiltration and would be difficult, if not impossible, to fill. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70232","collaboration":"Prepared in cooperation with the San Bernardino Valley Municipal Water District","usgsCitation":"Moreland, J.A., 1970, Artificial recharge, Yucaipa, California: U.S. Geological Survey Open-File Report 70-232, iv, 44 p., https://doi.org/10.3133/ofr70232.","productDescription":"iv, 44 p.","costCenters":[],"links":[{"id":372133,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0232/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0232/report-thumb.jpg"}],"country":"United States","state":"California","city":"Yucaipa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.14344024658202,\n              33.993188345311886\n            ],\n            [\n              -116.96044921875,\n              33.993188345311886\n            ],\n            [\n              -116.96044921875,\n              34.091904555072404\n            ],\n            [\n              -117.14344024658202,\n              34.091904555072404\n            ],\n            [\n              -117.14344024658202,\n              33.993188345311886\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c22","contributors":{"authors":[{"text":"Moreland, Joe A.","contributorId":48171,"corporation":false,"usgs":true,"family":"Moreland","given":"Joe","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":254677,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19159,"text":"ofr70145 - 1970 - Preliminary geologic map of the Geminus quadrangle of the Moon","interactions":[{"subject":{"id":19159,"text":"ofr70145 - 1970 - Preliminary geologic map of the Geminus quadrangle of the Moon","indexId":"ofr70145","publicationYear":"1970","noYear":false,"title":"Preliminary geologic map of the Geminus quadrangle of the Moon"},"predicate":"SUPERSEDED_BY","object":{"id":66016,"text":"i841 - 1974 - Geologic map of the Geminus Quadrangle of the Moon","indexId":"i841","publicationYear":"1974","noYear":false,"title":"Geologic map of the Geminus Quadrangle of the Moon"},"id":1}],"supersededBy":{"id":66016,"text":"i841 - 1974 - Geologic map of the Geminus Quadrangle of the Moon","indexId":"i841","publicationYear":"1974","noYear":false,"title":"Geologic map of the Geminus Quadrangle of the Moon"},"lastModifiedDate":"2026-01-07T15:20:53.124625","indexId":"ofr70145","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":"70-145","title":"Preliminary geologic map of the Geminus quadrangle of the Moon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70145","usgsCitation":"Grolier, M.J., 1970, Preliminary geologic map of the Geminus quadrangle of the Moon: U.S. Geological Survey Open-File Report 70-145, Report: 7 p.; 1 Plate: 42.51 x 30.07 inches, https://doi.org/10.3133/ofr70145.","productDescription":"Report: 7 p.; 1 Plate: 42.51 x 30.07 inches","costCenters":[],"links":[{"id":151558,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0145/report-thumb.jpg"},{"id":498380,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0145/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":498379,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","otherGeospatial":"Geminus quadrangle, Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b387","contributors":{"authors":[{"text":"Grolier, Maurice J.","contributorId":98292,"corporation":false,"usgs":true,"family":"Grolier","given":"Maurice","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":180416,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66244,"text":"i659 - 1970 - Map showing landforms and sedimentary deposits of the Padre Island portion of the South Bird Island 7.5-minute quadrangle, Texas","interactions":[],"lastModifiedDate":"2025-08-05T16:37:42.536423","indexId":"i659","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"659","title":"Map showing landforms and sedimentary deposits of the Padre Island portion of the South Bird Island 7.5-minute quadrangle, Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i659","usgsCitation":"Hunter, R.E., and Dickinson, K.A., 1970, Map showing landforms and sedimentary deposits of the Padre Island portion of the South Bird Island 7.5-minute quadrangle, Texas: U.S. Geological Survey IMAP 659, 1 Plate: 30.42 × 36.78 inches, https://doi.org/10.3133/i659.","productDescription":"1 Plate: 30.42 × 36.78 inches","costCenters":[],"links":[{"id":255721,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0659/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255722,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0659/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":255723,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0659/report-thumb.jpg"},{"id":395485,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9437.htm"}],"scale":"24000","country":"United States","state":"Texas","otherGeospatial":"Padre Island portion of the South Bird Island 7.5-minute quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.356,\n              27.375\n            ],\n            [\n              -97.25,\n              27.375\n            ],\n            [\n              -97.25,\n              27.5\n            ],\n            [\n              -97.356,\n              27.5\n            ],\n            [\n              -97.356,\n              27.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a495a","contributors":{"authors":[{"text":"Hunter, R. E.","contributorId":48148,"corporation":false,"usgs":true,"family":"Hunter","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":274231,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickinson, K. A.","contributorId":77528,"corporation":false,"usgs":true,"family":"Dickinson","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":274232,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67316,"text":"i574 - 1970 - Map showing recently active breaks along the San Andreas and related faults between Cholame Valley and Tejon Pass, California","interactions":[{"subject":{"id":46487,"text":"ofr68311 - 1968 - Map showing recently active breaks along the San Andreas and related faults between Cholame Valley and Tejon Pass, California","indexId":"ofr68311","publicationYear":"1968","noYear":false,"title":"Map showing recently active breaks along the San Andreas and related faults between Cholame Valley and Tejon Pass, California"},"predicate":"SUPERSEDED_BY","object":{"id":67316,"text":"i574 - 1970 - Map showing recently active breaks along the San Andreas and related faults between Cholame Valley and Tejon Pass, California","indexId":"i574","publicationYear":"1970","noYear":false,"title":"Map showing recently active breaks along the San Andreas and related faults between Cholame Valley and Tejon Pass, California"},"id":1}],"lastModifiedDate":"2022-10-27T20:44:23.804421","indexId":"i574","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"574","title":"Map showing recently active breaks along the San Andreas and related faults between Cholame Valley and Tejon Pass, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i574","usgsCitation":"Vedder, J.G., and Wallace, R.E., 1970, Map showing recently active breaks along the San Andreas and related faults between Cholame Valley and Tejon Pass, California: U.S. Geological Survey IMAP 574, Report: 1 p.; 2 Plates: 52.65 × 29.79 inches and 52.43 × 34.62 inches, https://doi.org/10.3133/i574.","productDescription":"Report: 1 p.; 2 Plates: 52.65 × 29.79 inches and 52.43 × 34.62 inches","costCenters":[],"links":[{"id":408831,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9360.htm","linkFileType":{"id":5,"text":"html"}},{"id":256357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0574/report-thumb.jpg"},{"id":256356,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0574/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256355,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0574/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256354,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0574/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"California","otherGeospatial":"Cholame Valley and Tehon Pass","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.436,\n              34.683\n            ],\n            [\n              -120.436,\n              35.857\n            ],\n            [\n              -118.744,\n              35.857\n            ],\n            [\n              -118.744,\n              34.683\n            ],\n            [\n              -120.436,\n              34.683\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a32d2","contributors":{"authors":[{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":275973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wallace, R. E.","contributorId":6823,"corporation":false,"usgs":true,"family":"Wallace","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":275972,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56038,"text":"ofr70237 - 1970 - Floods in Riley quadrangle, northeastern Illinois","interactions":[{"subject":{"id":56038,"text":"ofr70237 - 1970 - Floods in Riley quadrangle, northeastern Illinois","indexId":"ofr70237","publicationYear":"1970","noYear":false,"title":"Floods in Riley quadrangle, northeastern Illinois"},"predicate":"SUPERSEDED_BY","object":{"id":68137,"text":"ha464 - 1972 - Floods in Riley Quadrangle, Northeastern Illinois","indexId":"ha464","publicationYear":"1972","noYear":false,"title":"Floods in Riley Quadrangle, Northeastern Illinois"},"id":1}],"supersededBy":{"id":68137,"text":"ha464 - 1972 - Floods in Riley Quadrangle, Northeastern Illinois","indexId":"ha464","publicationYear":"1972","noYear":false,"title":"Floods in Riley Quadrangle, Northeastern Illinois"},"lastModifiedDate":"2012-02-02T00:11:48","indexId":"ofr70237","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":"70-237","title":"Floods in Riley quadrangle, northeastern Illinois","language":"ENGLISH","doi":"10.3133/ofr70237","usgsCitation":"Mycyk, R., and Grant, R., 1970, Floods in Riley quadrangle, northeastern Illinois: U.S. Geological Survey Open-File Report 70-237, 9 p., 11 figs., https://doi.org/10.3133/ofr70237.","productDescription":"9 p., 11 figs.","costCenters":[],"links":[{"id":174828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6256fd","contributors":{"authors":[{"text":"Mycyk, R.T.","contributorId":32566,"corporation":false,"usgs":true,"family":"Mycyk","given":"R.T.","affiliations":[],"preferred":false,"id":254678,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grant, R.S.","contributorId":103726,"corporation":false,"usgs":true,"family":"Grant","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":254679,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67368,"text":"i590 - 1970 - Surficial and engineering geology of the central part of the Yukon-Koyukuk lowland, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:17","indexId":"i590","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"590","subseriesTitle":"NONE","title":"Surficial and engineering geology of the central part of the Yukon-Koyukuk lowland, Alaska","language":"ENGLISH","doi":"10.3133/i590","usgsCitation":"Weber, F.R., and Pewe, T.L., 1970, Surficial and engineering geology of the central part of the Yukon-Koyukuk lowland, Alaska: U.S. Geological Survey IMAP 590, 1 map on two sheets :col. ;92 x 82 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i590.","productDescription":"1 map on two sheets :col. ;92 x 82 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106856,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9373.htm","linkFileType":{"id":5,"text":"html"},"description":"9373"},{"id":187665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -158,64.75 ], [ -158,65.5 ], [ -156,65.5 ], [ -156,64.75 ], [ -158,64.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db68929b","contributors":{"authors":[{"text":"Weber, F. R.","contributorId":105303,"corporation":false,"usgs":true,"family":"Weber","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":276067,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pewe, T. L.","contributorId":35786,"corporation":false,"usgs":true,"family":"Pewe","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":276066,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39689,"text":"pp683A - 1970 - Late Miocene nonmarine diatoms from the Kilgore area, Cherry County, Nebraska","interactions":[],"lastModifiedDate":"2020-02-28T09:38:49","indexId":"pp683A","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":"683","chapter":"A","title":"Late Miocene nonmarine diatoms from the Kilgore area, Cherry County, Nebraska","docAbstract":"<p>The Valentine Formation of A. L. Lugn, which is of late Miocene and early Pliocene age, contains diatomaceous and plant-bearing sediments at a locality on the north bluff of the Niobrara River, about 10 miles south of Kilgore, Cherry County, Nebr. The fossil flora has been studied by H. D. MacGinitie, who concluded that the deposit is of late Miocene age. Correlative strata near Valentine, Nebr., several miles east of this locality, are reported to contain a vertebrate fauna of late Miocene age. The Kilgore diatom assemblage consists of 45 taxa of nonmarine diatoms. Of these, four species are herein recorded as new, one species has been previously reported from the middle Pliocene of France, and the remaining 40 taxa are identified as still living in modern nonmarine environments. The diatom assemblage suggests deposition in a relatively shallow, small lake. The waters of this lake were probably hard, and perhaps at times somewhat alkaline or saline. It is difficult to separate the influences of ecology and geologic age on the composition of the diatom assemblage, but this problem should be resolved as other Tertiary assemblages are studied. The five presumably extinct species may prove to be useful for stratigraphic correlation when their geologic ranges are better known. The composition of the assemblage, the relative number of taxa, and the absence of several widespread modern genera and species of nonmarine diatoms should be of value in identifying other late Miocene assemblages and in distinguishing them from assemblages of different age.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to paleontology, 1970","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp683A","usgsCitation":"Andrews, G., 1970, Late Miocene nonmarine diatoms from the Kilgore area, Cherry County, Nebraska: U.S. Geological Survey Professional Paper 683, 40 p., https://doi.org/10.3133/pp683A.","productDescription":"40 p.","costCenters":[],"links":[{"id":119895,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0683a/report-thumb.jpg"},{"id":67417,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0683a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nebraska","county":"Cherry County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-102.0829,42.9979],[-102.0007,42.9973],[-101.9652,42.9971],[-101.7528,42.9958],[-101.6775,42.9953],[-101.2277,42.9953],[-100.7509,42.9947],[-100.6721,42.9949],[-100.3938,42.996],[-100.1984,42.997],[-100.1985,42.8461],[-100.1984,42.782],[-100.184,42.7829],[-100.1837,42.4338],[-100.1675,42.4348],[-100.1667,42.0881],[-100.2675,42.0871],[-100.6156,42.0872],[-100.73,42.0885],[-100.8444,42.0896],[-100.9582,42.0897],[-100.9841,42.09],[-101.1016,42.0913],[-101.1926,42.0914],[-101.3094,42.0925],[-101.3323,42.0927],[-101.4097,42.0942],[-101.4251,42.0936],[-101.4492,42.0933],[-101.6861,42.0945],[-101.7733,42.0938],[-101.803,42.0934],[-101.8902,42.0962],[-101.9199,42.0958],[-102.0065,42.0958],[-102.0393,42.0962],[-102.0387,42.1826],[-102.0402,42.4448],[-102.0669,42.4448],[-102.0664,42.5302],[-102.0665,42.7867],[-102.0846,42.7864],[-102.0836,42.9606],[-102.0829,42.9979]]]},\"properties\":{\"name\":\"Cherry\",\"state\":\"NE\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8bca","contributors":{"authors":[{"text":"Andrews, G.W.","contributorId":106549,"corporation":false,"usgs":true,"family":"Andrews","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":221989,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56036,"text":"ofr70227 - 1970 - Compilation of data for Michigan lakes","interactions":[],"lastModifiedDate":"2017-01-20T10:52:26","indexId":"ofr70227","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":"70-227","title":"Compilation of data for Michigan lakes","docAbstract":"<p>Michigan's more than 11,000 lakes are a valuable resource. Primarily, they are used for recreation but many have potential for industrial use and for water supply. </p><p>Lakes have water surfaces ·that expand and decrease in area, and levels that rise and fall. Records of lakes levels show that lake stages change, have seasonal trends, and may fluctuate several feet each year. Often; these changes affect the use of lakes and cause erosion of their shorelines. It is important, therefore, to monitor lake levels in order to add to their understanding and to provide a basis for increasing their usefulness. </p><p>In the early 1940's, and in cooperation with the Michigan Department of Natural Resources, a network of lake gages was established in Michigan to observe lake levels. In subsequent years, this network of lake gages was changed to provide a broad areal coverage of lakes in the State, to answer specific requests for data, and to obtain information on a large portion of Michigan's many lakes. These data have been applied primarily in studies involving the design of lake-level control facilities and establishing legal levels for lakes. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr70227","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources Geological Survey Division","usgsCitation":"Miller, J.B., and Thompson, T., 1970, Compilation of data for Michigan lakes: U.S. Geological Survey Open-File Report 70-227, ix, 368 p., https://doi.org/10.3133/ofr70227.","productDescription":"ix, 368 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":174727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0227/report-thumb.jpg"},{"id":272565,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0227/report.pdf"}],"country":"United 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