{"pageNumber":"603","pageRowStart":"15050","pageSize":"25","recordCount":16446,"records":[{"id":38772,"text":"pp585D - 1972 - Vegetation of prairie potholes, North Dakota, in relation to quality of water and other environmental factors","interactions":[],"lastModifiedDate":"2018-03-16T14:06:00","indexId":"pp585D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"585","chapter":"D","title":"Vegetation of prairie potholes, North Dakota, in relation to quality of water and other environmental factors","docAbstract":"<p>Measurements of specific conductance provide an adequate indication of the average salinity of surface waters in natural ponds and lakes of the northern .prairie region. Yearly and seasonal variations in specific conductance were much greater in brackish and subsaline wetlands than in fresh-water areas. The principal vegetational types. Land-use practices of varying brackish to saline wetlands were sulfates and chlorides of sodium and magnesium. In less saline waters, carbonate and bicarbonate salts of calcium and potassium were of greater importance, but as salinity increased, the proportion of these compounds decreased rapidly.</p><p>A major environmental factor controlling the establishment of marsh and aquatic vegetation is the permanence of surface water. Permanence is a measure of the extent to which surface water persists at a given site. Varying degrees of water permanence during the growing season led to the establishment of distinct vegetational types, which were differentiated primarily on the 'basis of community structure or life form of the dominant vegetation.</p><p>Salinity of surface waters was closely correlated with differences in species composition of plant communities found in the principal vegetational types. Land-use practices of varying degrees of intensity also had a secondary influence on species composition. Since an unstable water chemistry is characteristic of most prairie ponds and lakes, it is more reliable to use the plant communities as indicators of average salinity than to use single measurements of specific conductance.</p><p>Characteristic species of wetland vegetational types occupied the central deeper parts of pond and lake basins or occurred as concentric peripheral bands. The wetland vegetational types are wetland low-prairie, wet-meadow, shallow-marsh emergent, deep-marsh emergent, fen emergent, submerged and floating, natural drawdown, cropland drawdown, and cropland tillage vegetation. Combinations of species (plant associations) within these vegetational types were placed in one of six salinity categories designated as fresh, slightly brackish, moderately brackish, brackish, subsaline, and saline. Salt tolerance apparently varied greatly among the various marsh and aquatic plants since the num'ber of species represented in moderately brackish&nbsp;to saline communities decreased markedly with increased salinity of the surface water environment. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of prairie potholes in North Dakota","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp585D","usgsCitation":"Stewart, R.E., and Kantrud, H., 1972, Vegetation of prairie potholes, North Dakota, in relation to quality of water and other environmental factors: U.S. Geological Survey Professional Paper 585, 35 p., https://doi.org/10.3133/pp585D.","productDescription":"35 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":22019,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0585d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0585d/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025cb","contributors":{"authors":[{"text":"Stewart, R. E.","contributorId":93426,"corporation":false,"usgs":true,"family":"Stewart","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":220427,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kantrud, H.A.","contributorId":28553,"corporation":false,"usgs":true,"family":"Kantrud","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":220426,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48070,"text":"ofr72317 - 1972 - Annual compilation and analysis of hydrologic data for urban studies in the Bryan, Texas, metropolitan area, 1969","interactions":[],"lastModifiedDate":"2017-06-14T11:09:12","indexId":"ofr72317","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-317","title":"Annual compilation and analysis of hydrologic data for urban studies in the Bryan, Texas, metropolitan area, 1969","docAbstract":"<p>Hydrologic investigations of urban areas in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin, Houston, Dallas, Dallas County, Fort Worth, San Antonio, and Bryan. Hydrologic investigations of urban areas in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin, Houston, Dallas, Dallas County, Fort Worth, San Antonio, and Bryan. 1. To determine, on the basis of historical data and hydrologic analyses, the magnitude and frequency of floods. 2. To document and define the areal extent of floods of greater than ordinary magnitude. 3. To determine the effect of urban development on flood peaks and volume. 4. To provide applied research facilities for studies at Texas A &amp; M University at College Stations. This report, the first in a series of reports to be published annually, is primarily applicable to objectives 2, 3, and 4. The report presents the basic hydrologic data collected in two study areas during the 1969 water year (October 1, 1968, to September 30, 1969) and basic hydrologic data collected during part of the 1968 water year (April 5, 1968, to September 30, 1968). The locations of the two basins within the study area, Burton Creek and Hudson Creek, are shown on figure 1.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72317","collaboration":"Prepared in cooperation with Texas Agricultural and Mechanical University","usgsCitation":"Robbins, W., 1972, Annual compilation and analysis of hydrologic data for urban studies in the Bryan, Texas, metropolitan area, 1969: U.S. Geological Survey Open-File Report 72-317, iv, 49 p., https://doi.org/10.3133/ofr72317.","productDescription":"iv, 49 p.","numberOfPages":"53","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1969-01-01","temporalEnd":"1969-12-31","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":162388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0317/report-thumb.jpg"},{"id":285951,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0317/report.pdf","text":"Report","size":"15.45 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Bryan","otherGeospatial":"Burton Creek, Hudson Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96.5,30.5 ], [ -96.5,30.75 ], [ -95.25,30.75 ], [ -95.25,30.5 ], [ -96.5,30.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bb6c","contributors":{"authors":[{"text":"Robbins, W.D.","contributorId":72852,"corporation":false,"usgs":true,"family":"Robbins","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":236769,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38805,"text":"pp569C - 1972 - Hydrologic significance of lithofacies of the Cane River Formation or equivalents of Arkansas, Louisiana, Mississippi, and Texas","interactions":[],"lastModifiedDate":"2025-04-15T19:06:17.1923","indexId":"pp569C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"569","chapter":"C","title":"Hydrologic significance of lithofacies of the Cane River Formation or equivalents of Arkansas, Louisiana, Mississippi, and Texas","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geohydrology of the Claiborne Group (Professional Paper 569)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp569C","usgsCitation":"Payne, J., 1972, Hydrologic significance of lithofacies of the Cane River Formation or equivalents of Arkansas, Louisiana, Mississippi, and Texas: U.S. Geological Survey Professional Paper 569, Report: 16 p.; 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,{"id":68527,"text":"ha449 - 1972 - Floods on Loop Creek and Richland Creek near Belleville, Illinois","interactions":[],"lastModifiedDate":"2022-12-12T20:05:04.998728","indexId":"ha449","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"449","title":"Floods on Loop Creek and Richland Creek near Belleville, Illinois","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha449","usgsCitation":"Camp, J.D., 1972, Floods on Loop Creek and Richland Creek near Belleville, Illinois: U.S. Geological Survey Hydrologic Atlas 449, 1 Plate: 45.00 × 30.50 inches, https://doi.org/10.3133/ha449.","productDescription":"1 Plate: 45.00 × 30.50 inches","costCenters":[],"links":[{"id":185709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410302,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15835.htm","linkFileType":{"id":5,"text":"html"}},{"id":90128,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/449/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Illinois","city":"Belleville","otherGeospatial":"Loop Creek, Richland Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90,\n              38.492\n            ],\n            [\n              -90,\n              38.625\n            ],\n            [\n              -89.875,\n              38.625\n            ],\n            [\n              -89.875,\n              38.492\n            ],\n            [\n              -90,\n              38.492\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df83e","contributors":{"authors":[{"text":"Camp, Joseph D.","contributorId":47869,"corporation":false,"usgs":true,"family":"Camp","given":"Joseph","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":278401,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68374,"text":"ha416 - 1972 - Ground water in Kearny County, southwestern Kansas","interactions":[],"lastModifiedDate":"2012-02-10T00:11:29","indexId":"ha416","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"416","title":"Ground water in Kearny County, southwestern Kansas","language":"ENGLISH","doi":"10.3133/ha416","usgsCitation":"Gutentag, E.D., 1972, Ground water in Kearny County, southwestern Kansas: U.S. Geological Survey Hydrologic Atlas 416, 10 col. maps on two sheets ;80 x 91 cm., https://doi.org/10.3133/ha416.","productDescription":"10 col. maps on two sheets ;80 x 91 cm.","costCenters":[],"links":[{"id":185801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89866,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/416/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89867,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/416/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -101.5,37.75 ], [ -101.5,38.25 ], [ -101.25,38.25 ], [ -101.25,37.75 ], [ -101.5,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db78","contributors":{"authors":[{"text":"Gutentag, Edwin D.","contributorId":76287,"corporation":false,"usgs":true,"family":"Gutentag","given":"Edwin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":278110,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68335,"text":"ha452 - 1972 - Average water content of snowpack in Maine","interactions":[],"lastModifiedDate":"2022-09-28T19:28:58.094676","indexId":"ha452","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"452","title":"Average water content of snowpack in Maine","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha452","usgsCitation":"Hayes, G.S., 1972, Average water content of snowpack in Maine: U.S. Geological Survey Hydrologic Atlas 452, 1 Plate: 31.00 × 35.00 inches, https://doi.org/10.3133/ha452.","productDescription":"1 Plate: 31.00 × 35.00 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,{"id":68042,"text":"ha421 - 1972 - Availability and quality of ground water in the Ashland quadrangle, Jackson County, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:27:05","indexId":"ha421","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"421","title":"Availability and quality of ground water in the Ashland quadrangle, Jackson County, Oregon","language":"ENGLISH","doi":"10.3133/ha421","usgsCitation":"Robison, J.H., 1972, Availability and quality of ground water in the Ashland quadrangle, Jackson County, Oregon: U.S. Geological Survey Hydrologic Atlas 421, 1 map., https://doi.org/10.3133/ha421.","productDescription":"1 map.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":187737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89295,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/421/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.75,42 ], [ -122.75,42.25 ], [ -122.5,42.25 ], [ -122.5,42 ], [ -122.75,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f40","contributors":{"authors":[{"text":"Robison, J. H.","contributorId":60183,"corporation":false,"usgs":true,"family":"Robison","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277554,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68371,"text":"ha456 - 1972 - Floods in the Río Guanajibo Valley, southwestern Puerto Rico","interactions":[],"lastModifiedDate":"2022-11-23T21:15:09.693047","indexId":"ha456","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"456","title":"Floods in the Río Guanajibo Valley, southwestern Puerto Rico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha456","usgsCitation":"Haire, W.J., 1972, Floods in the Río Guanajibo Valley, southwestern Puerto Rico: U.S. Geological Survey Hydrologic Atlas 456, 1 Plate: 55.53 × 34.00 inches, https://doi.org/10.3133/ha456.","productDescription":"1 Plate: 55.53 × 34.00 inches","costCenters":[],"links":[{"id":185798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":409612,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15842.htm","linkFileType":{"id":5,"text":"html"}},{"id":89856,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/456/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","country":"United States","state":"Puerto Rico","otherGeospatial":"Río Guanajibo Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -67.192,\n              18.056\n            ],\n            [\n              -67.192,\n              18.194\n            ],\n            [\n              -66.94,\n              18.194\n            ],\n            [\n              -66.94,\n              18.056\n            ],\n            [\n              -67.192,\n              18.056\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0a4e","contributors":{"authors":[{"text":"Haire, William J.","contributorId":70482,"corporation":false,"usgs":true,"family":"Haire","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278106,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68232,"text":"ha383 - 1972 - Water-resources reconnaissance of the Ozark plateaus province, northern Arkansas","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"ha383","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"383","title":"Water-resources reconnaissance of the Ozark plateaus province, northern Arkansas","language":"ENGLISH","doi":"10.3133/ha383","usgsCitation":"Lamonds, A.G., 1972, Water-resources reconnaissance of the Ozark plateaus province, northern Arkansas: U.S. Geological Survey Hydrologic Atlas 383, 2 maps. ;99 x 112 cm. fold. to 30 x 20 cm., https://doi.org/10.3133/ha383.","productDescription":"2 maps. ;99 x 112 cm. fold. to 30 x 20 cm.","costCenters":[],"links":[{"id":188039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89602,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89603,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89604,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89605,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89606,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89607,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89608,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89609,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94,35.5 ], [ -94,36.5 ], [ -91,36.5 ], [ -91,35.5 ], [ -94,35.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9b55","contributors":{"authors":[{"text":"Lamonds, A. G.","contributorId":8450,"corporation":false,"usgs":true,"family":"Lamonds","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277884,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68300,"text":"ha461 - 1972 - Hydrogeologic characteristics of the valley-fill aquifer in the Arkansas River Valley, Bent County, Colorado","interactions":[],"lastModifiedDate":"2018-09-25T10:22:27","indexId":"ha461","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"461","title":"Hydrogeologic characteristics of the valley-fill aquifer in the Arkansas River Valley, Bent County, Colorado","docAbstract":"<p>The investigation on which this report is based is a part of a comprehensive evaluation of the water resources of the Arkansas River valley undertaken by the U.S. Geological Survey in cooperation with the Colorado Water Conservation Board and the Southeastern Colorado Water Conservancy District. The study reach extends 150 miles from Pueblo to the Kansas State line. The water-resources investigation of the stream aquifer system in the Arkansas River valley, which began in 1963, is being made to provide information about the water resources for planning, management, and administration of the supply. </p><p>The objectives of the investigation are to define the effects of present water use, to determine the relation between ground and surface water, and to evaluate the effects of proposed changes in water law and management. The major steps in the study are: (1) Inventory the water resources, (2) describe the hydrogeologic character of the aquifer, (3) document and evaluate the effects of development, (4) construct and verify models to aid in the evaluation of the hydrology, and (5) develop models to test water-management plans and to optimize water use. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha461","collaboration":"Prepared in cooperation with the Colorado Water Conservation Board and the Southeastern Colorado Water Conservancy District","usgsCitation":"Hurr, R.T., and Moore, J.E., 1972, Hydrogeologic characteristics of the valley-fill aquifer in the Arkansas River Valley, Bent County, Colorado: U.S. Geological Survey Hydrologic Atlas 461, 4 Plates: 40 x 33 inches or smaller, https://doi.org/10.3133/ha461.","productDescription":"4 Plates: 40 x 33 inches or smaller","costCenters":[],"links":[{"id":186622,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89735,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/461/plate-3.pdf","text":"Plate 3","size":"315 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":89736,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/461/plate-4.pdf","text":"Plate 4","size":"266 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 4"},{"id":89733,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/461/plate-1.pdf","text":"Plate 1","size":"4.85 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":89734,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/461/plate-2.pdf","text":"Plate 2","size":"4.71 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"}],"scale":"62500","country":"United States","state":"Colorado","county":"Bent County","otherGeospatial":"Arkansas River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.38333333333334,38 ], [ -103.38333333333334,38.166666666666664 ], [ -102.75,38.166666666666664 ], [ -102.75,38 ], [ -103.38333333333334,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628c24","contributors":{"authors":[{"text":"Hurr, R. Theodore","contributorId":27023,"corporation":false,"usgs":true,"family":"Hurr","given":"R.","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":277989,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, John E.","contributorId":33688,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":277990,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68383,"text":"ha380 - 1972 - Water resources of the Crow Wing River watershed, central Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T13:23:16","indexId":"ha380","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"380","title":"Water resources of the Crow Wing River watershed, central Minnesota","docAbstract":"<p>The Crow Wing River, a tributary of the Mississippi River, drains an area of about 3,760 square miles, essentially all of which is covered by glacial deposits.</p>\n<p>Topography of most of the watershed is slightly- to moderately-undulating and has local relief of up to about 50 feet. 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,{"id":68320,"text":"ha426 - 1972 - Reconnaissance of the Rifle River, a cold-water river in the northeastern part of Michigan's Southern Peninsula","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha426","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"426","title":"Reconnaissance of the Rifle River, a cold-water river in the northeastern part of Michigan's Southern Peninsula","language":"ENGLISH","doi":"10.3133/ha426","usgsCitation":"Hendrickson, G.E., and Doonan, C.J., 1972, Reconnaissance of the Rifle River, a cold-water river in the northeastern part of Michigan's Southern Peninsula: U.S. Geological Survey Hydrologic Atlas 426, 1 map on two sheets., https://doi.org/10.3133/ha426.","productDescription":"1 map on two sheets.","costCenters":[],"links":[{"id":185890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89777,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/426/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89778,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/426/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89779,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/426/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89780,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/426/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89781,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/426/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.25,44.25 ], [ -84.25,44.5 ], [ -84,44.5 ], [ -84,44.25 ], [ -84.25,44.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63afa5","contributors":{"authors":[{"text":"Hendrickson, G. E.","contributorId":99958,"corporation":false,"usgs":true,"family":"Hendrickson","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":278023,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doonan, C. J.","contributorId":62592,"corporation":false,"usgs":true,"family":"Doonan","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278022,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68312,"text":"ha377 - 1972 - Water resources of Clay, Greene, Craighead, and Poinsett Counties, Arkansas","interactions":[{"subject":{"id":55906,"text":"ofr69127 - 1969 - Water resources of Clay, Greene, Craighead and Poinsett Counties, Arkansas","indexId":"ofr69127","publicationYear":"1969","noYear":false,"title":"Water resources of Clay, Greene, Craighead and Poinsett Counties, Arkansas"},"predicate":"SUPERSEDED_BY","object":{"id":68312,"text":"ha377 - 1972 - Water resources of Clay, Greene, Craighead, and Poinsett Counties, Arkansas","indexId":"ha377","publicationYear":"1972","noYear":false,"title":"Water resources of Clay, Greene, Craighead, and Poinsett Counties, Arkansas"},"id":1}],"lastModifiedDate":"2019-08-23T12:57:37","indexId":"ha377","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"377","title":"Water resources of Clay, Greene, Craighead, and Poinsett Counties, Arkansas","docAbstract":"<p>Water is available in Clay, Greene, Craighead, and Poinsett Counties from ground-water and surface-water sources. However, ground water is more accessible in many places than surface water. Ground water is available from the alluvium, which covers all the area except Crowleys Ridge, and is also available from other formations below the alluvium.</p><p>Surface water is available from the Black and Cache Rivers west of Crowleys Ridge, and from the St/ Francis and Little Rivers, and from many ditches and laterals east of the ridge. Continuous water supplies are not available from streams on Crowleys Ridge, but additional surface-water supplies could be made available from reservoirs storage on the ridge. Average annual streamflow ranges from 1.2 cfs per sq mi (Cubic feet per second per square mile) in the western part of the four counties to 1.4 cfs per sq mi in the eastern part. Average annual precipitation is about 48 inches.</p><p>Use of water in the area for agriculture greatly exceeds all other used combined, and progressively greater amounts of water are being used for irrigation. In 1965, 111.4 mgd (million gallons per day) was used for irrigation of other crops. An additional 16.9 mgd was used by industry, municipalities, and others. Of these amounts, 180.1 mgd was ground water and 19.7 mgd was surface water, or a total of 199.8 mgd. More than 80 manufacturing firms, many of which are closely allied to agriculture, use moderate amounts of water, mostly from municipal supplies.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha377","collaboration":"Prepared in cooperation with the Arkansas Geological Commission","usgsCitation":"Hines, M.S., Plebuch, R.O., and Lamonds, A.G., 1972, Water resources of Clay, Greene, Craighead, and Poinsett Counties, Arkansas: U.S. Geological Survey Hydrologic Atlas 377, 2 Plates: 44.00 x 38.50 inches and 45.00 x 38.00 inches, https://doi.org/10.3133/ha377.","productDescription":"2 Plates: 44.00 x 38.50 inches and 45.00 x 38.00 inches","costCenters":[],"links":[{"id":366867,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/377/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185693,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/377/plate-1-thumb.jpg"},{"id":89760,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/377/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas","county":"Clay County, Craighead County, Greene County, Poinsett County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91,35.5 ], [ -91,36.5 ], [ -90.5,36.5 ], [ -90.5,35.5 ], [ -91,35.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f08aa","contributors":{"authors":[{"text":"Hines, Marion S.","contributorId":29388,"corporation":false,"usgs":true,"family":"Hines","given":"Marion","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":278012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plebuch, Raymond O.","contributorId":15177,"corporation":false,"usgs":true,"family":"Plebuch","given":"Raymond","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":278011,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lamonds, A. G.","contributorId":8450,"corporation":false,"usgs":true,"family":"Lamonds","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":278010,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61403,"text":"mf339 - 1972 - Preliminary photointerpretation map of landslide and other surficial deposits of the Mount Hamilton quadrangle and parts of the Mount Boardman and San Jose quadrangles, Alameda and Santa Clara Counties, California","interactions":[],"lastModifiedDate":"2016-08-23T10:30:43","indexId":"mf339","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"339","title":"Preliminary photointerpretation map of landslide and other surficial deposits of the Mount Hamilton quadrangle and parts of the Mount Boardman and San Jose quadrangles, Alameda and Santa Clara Counties, California","docAbstract":"<p>The nine San Francisco Bay region counties lie within a geologically active, young, and dynamic part of the central and northern Coast Ranges of California. Significant movements of the earth's crust are occurring here at the present time, posing numerous problems to urbanization, including some of special concern. Geological processes such as fault movements, earthquakes, land subsidence, landsliding, slow downslope movement of bedrock and surficial materials, coastal and stream erosion, flooding, and sedimentation are all potentially hazardous. Because of these factors, an understanding of the operation of physical processes in the bay region is desirable for harmonious, efficient, and safe land-use planning, particularly now, with greatly expanded pressures for urban growth.&nbsp;</p>\n<p>This map presents preliminary information about one aspect of the physical environment necessary to sound land-use planning--the nature and distribution of surficial deposits. Because surficial deposits are common and well developed in much of the bay region, it is useful to know how and why they have formed, as well as what properties they possess. When maps like this are used in combination with other types of environmental information, such as data on soils, bedrock geology, slopes, vegetation, climatic variation, seismic response, and hydrology, it should be easier to arrive at sound decisions regarding the physical aspects of land use. The U.S. Geological Survey is studying many of these factors in the bay region and hopes to provide the community with much of the required information as part of its San Francisco Bay Region Study in cooperation with the&nbsp;Department of Housing and Urban Development.</p>\n<p>The representation of surficial deposits on this map reflects the way in which a geologist, working exclusively with aerial photographs, interpreted the origin of various elements of the present landscape. The deposits shown here have not been examined in the field. However, by viewing overlapping vertical aerial photographs through a stereoscope, the geologist sees a three-dimensional relief model of the ground surface and can study and interpret the origins of landforms with considerable ease. In fact, for mapping surficial deposits, particularly in reconnaissance-type studies, photointerpretation has advantages over both ground observations and laboratory studies of surficial materials. Of course, better information can be provided when all aspects of the study are integrated. These preliminary photointerpretation maps are only the first stage in a detailed study of surficial deposits in the bay region, but they should provide land-use planners with immediately useful information about the regional distribution of landslide and other surficial deposits.</p>\n<p>This map indicates the dominant surficial processes that have probably been operative by showing the distribution of different types of surficial deposits. Processes such as weathering, erosion, sedimentation, and the slow as well as rapid downslope movement of earth materials have constantly reshaped the land surface in the past and will continue to in the future, although at varying rates. The processes are interrelated to varying degrees. For example, crustal uplift of the Coast Ranges will lead to increased erosion and downcutting by streams that in turn generally results in increased deposition of sediments in river valleys, lakes, and shoreline areas. Older flood planes and river deposits may be eroded, leaving elevated terrace deposits. In addition, downcutting by streams may cause adjacent slopes to become unstable, thereby increasing the possibility of slope failures.</p>\n<p>Man's activities can alter natural physical processes in many ways. Simple acts such as overwatering a lawn or placing a septic tank drainfield in ground that is marginally stable may weaken the bedrock and surficial materials enough to induce landsliding. Relatively stable areas may be made unstable as a result of construction activities that involve cutting or oversteepening of natural slopes. Engineers, builders, conservationists, and others concerned with land use must evaluate the potential effects of all types of development, and maps that show the nature and distribution of surficial deposits should provide much of the basic information they need.</p>\n<p>This map, then, shows the cumulative effects of various processes that have yielded surficial deposits up to the time the photographs used for photointerpretation were taken. It does not indicate directly areas where processes will be most active, nor does it show the rate at which they will operate. However, knowledge of the history of geologic events is a key to understanding and predicting the evolution of an area, even where man's activities significantly change the character of the land. Almost all new landslides, for example, occur in areas with a history of landslide activity.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf339","collaboration":"Prepared in Cooperation with the Department of Housing and Urban Development","usgsCitation":"Nilsen, T., 1972, Preliminary photointerpretation map of landslide and other surficial deposits of the Mount Hamilton quadrangle and parts of the Mount Boardman and San Jose quadrangles, Alameda and Santa Clara Counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 339, 2 Plates: 34.72 x 21.90 inches and 32.46 x 21.57 inches, https://doi.org/10.3133/mf339.","productDescription":"2 Plates: 34.72 x 21.90 inches and 32.46 x 21.57 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf339.JPG"},{"id":327592,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0339/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":327593,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0339/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"California","county":"Alameda County, Santa Clara County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122,37.75 ], [ -122,38 ], [ -121.41666666666667,38 ], [ -121.41666666666667,37.75 ], [ -122,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696599","contributors":{"authors":[{"text":"Nilsen, Tor H.","contributorId":100016,"corporation":false,"usgs":true,"family":"Nilsen","given":"Tor H.","affiliations":[],"preferred":false,"id":265587,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68424,"text":"ha438 - 1972 - Floods at Caguas, Gurabo, Juncos, and San Lorenzo, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha438","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"438","title":"Floods at Caguas, Gurabo, Juncos, and San Lorenzo, Puerto Rico","language":"ENGLISH","doi":"10.3133/ha438","usgsCitation":"Fields, F.K., 1972, Floods at Caguas, Gurabo, Juncos, and San Lorenzo, Puerto Rico: U.S. Geological Survey Hydrologic Atlas 438, 1 map., https://doi.org/10.3133/ha438.","productDescription":"1 map.","costCenters":[],"links":[{"id":186611,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89950,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/438/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -66.08333333333333,18.166666666666668 ], [ -66.08333333333333,18.333333333333332 ], [ -65.86749999999999,18.333333333333332 ], [ -65.86749999999999,18.166666666666668 ], [ -66.08333333333333,18.166666666666668 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e72f4","contributors":{"authors":[{"text":"Fields, Fred K.","contributorId":69981,"corporation":false,"usgs":true,"family":"Fields","given":"Fred","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68144,"text":"ha215 - 1972 - Analysis of the ground-water system by electrical-analog model, Avra Valley, Pima and Pinal Counties, Arizona","interactions":[],"lastModifiedDate":"2021-12-29T20:12:01.575883","indexId":"ha215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"215","title":"Analysis of the ground-water system by electrical-analog model, Avra Valley, Pima and Pinal Counties, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha215","usgsCitation":"Moosburner, O., 1972, Analysis of the ground-water system by electrical-analog model, Avra Valley, Pima and Pinal Counties, Arizona: U.S. Geological Survey Hydrologic Atlas 215, 2 Plates: 42.60 × 33.00 inches and 38.50 × 32.79 inches, https://doi.org/10.3133/ha215.","productDescription":"2 Plates: 42.60 × 33.00 inches and 38.50 × 32.79 inches","costCenters":[],"links":[{"id":186375,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393619,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15581.htm"},{"id":89448,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/215/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89447,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/215/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"Arizona","county":"Pima County, Pinal County","otherGeospatial":"Avra Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.45,\n              32\n            ],\n            [\n              -111.083,\n              32\n            ],\n            [\n              -111.083,\n              32.633\n            ],\n            [\n              -111.45,\n              32.633\n            ],\n            [\n              -111.45,\n              32\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680031","contributors":{"authors":[{"text":"Moosburner, Otto","contributorId":41822,"corporation":false,"usgs":true,"family":"Moosburner","given":"Otto","email":"","affiliations":[],"preferred":false,"id":277726,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68264,"text":"ha475 - 1972 - Ground-water resources of McLean County, west-central North Dakota","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"ha475","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"475","title":"Ground-water resources of McLean County, west-central North Dakota","language":"ENGLISH","doi":"10.3133/ha475","usgsCitation":"Klausing, R.L., 1972, Ground-water resources of McLean County, west-central North Dakota: U.S. Geological Survey Hydrologic Atlas 475, 1 col. map ;76 cm. x 116 cm. in folder 30 cm. x 24 cm., https://doi.org/10.3133/ha475.","productDescription":"1 col. map ;76 cm. x 116 cm. in folder 30 cm. x 24 cm.","costCenters":[],"links":[{"id":188470,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89663,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/475/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"26720","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -10.366666666666667,47.166666666666664 ], [ -10.366666666666667,47.833333333333336 ], [ -10.066666666666666,47.833333333333336 ], [ -10.066666666666666,47.166666666666664 ], [ -10.366666666666667,47.166666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696da7","contributors":{"authors":[{"text":"Klausing, Robert L.","contributorId":55797,"corporation":false,"usgs":true,"family":"Klausing","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277930,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68142,"text":"ha459 - 1972 - Floods in Hampshire Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha459","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"459","title":"Floods in Hampshire Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha459","usgsCitation":"Mycyk, R.T., and Duerk, M.D., 1972, Floods in Hampshire Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 459, 1 col. map ;58 x 43 cm., on sheet 76 x 112 cm., https://doi.org/10.3133/ha459.","productDescription":"1 col. map ;58 x 43 cm., on sheet 76 x 112 cm.","costCenters":[],"links":[{"id":186373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89443,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/459/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.61749999999999,42 ], [ -88.61749999999999,42.1175 ], [ -88.5,42.1175 ], [ -88.5,42 ], [ -88.61749999999999,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e713c","contributors":{"authors":[{"text":"Mycyk, Roman T.","contributorId":58331,"corporation":false,"usgs":true,"family":"Mycyk","given":"Roman","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":277722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duerk, Marvin D.","contributorId":96768,"corporation":false,"usgs":true,"family":"Duerk","given":"Marvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":277723,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68059,"text":"ha476 - 1972 - Ground-water resources of Benson and Pierce Counties, north-central North Dakota","interactions":[],"lastModifiedDate":"2018-06-04T10:38:20","indexId":"ha476","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"476","title":"Ground-water resources of Benson and Pierce Counties, north-central North Dakota","docAbstract":"<p>The purpose of this investigation is to provide information about the ground-water resources in Benson and Pierce Counties that is sufficient for planning the safe and intelligent development of water supplies for irrigation, domestic, stock, industrial, and municipal purposes.&nbsp; The investigation is part of a statewide program to determine the location and extent of ground-water aquifers; to evaluate the occurrence and movement of ground water within the aquifers, including sources of recharge and discharge; to determine potential yields to wells developed in the aquifers; and to determine the chemical quality of ground water.</p><p>Benson and Pierce Counties cover an area of 2,512 square miles in north-central North Dakota.&nbsp; This study, which began in July 1967 and was completed in June 1971, was made cooperatively by the U.S. Geological Survey, the North Dakota State Water Commission, the North Dakota Geological Survey, and the Benson and Pierce Counties Water Management Districts.&nbsp; This interim report presents only the major conclusions of the study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha476","usgsCitation":"Randich, P., 1972, Ground-water resources of Benson and Pierce Counties, north-central North Dakota: U.S. Geological Survey Hydrologic Atlas 476, 43.0 x 34.5 inches, https://doi.org/10.3133/ha476.","productDescription":"43.0 x 34.5 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":186110,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89322,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/476/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"26720","country":"United States","state":"North Dakota","county":"Benson County, Pierce 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,{"id":68327,"text":"ha436 - 1972 - Reconnaissance of the Manistee River, a cold-water river in the northwestern part of Michigan's Southern Peninsula","interactions":[],"lastModifiedDate":"2016-10-06T13:24:47","indexId":"ha436","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"436","title":"Reconnaissance of the Manistee River, a cold-water river in the northwestern part of Michigan's Southern Peninsula","docAbstract":"<p>The cold-water streams of the northern states provide unique recreational values to the American people (wilderness or semi-wilderness atmosphere, fast-water canoeing, trout fishing), but expanding recreational needs must be balanced against the growing demand of water for public and industrial supplies, irrigation, and dilution of sewage and other wastes. In order to make intelligent decisions regarding use and management of water resources for recreation and other demands, an analysis of hydrologic factors related to recreation is essential.</p><p>The Manistee River is one of Michigan's well-known trout streams-a stream having numerous public access sites and campgrounds. Upstream from Cameron Bridge (see location map) the Manistee is rated as a first-class trout stream but below Cameron Bridge the river is rated only as a fair trout stream by the Michigan Department of Natural Resources. As a Michigan canoe trail it is second only to the Au Sable River in popularity. Esthetically, the Manistee is one of Michigan's most attractive rivers, its waters flowing cool and clean, and around each bend a pleasant wilderness scene. This report deals with that part of the river upstream from State Highway M-66 at Smithville. Several hard-surface roads give access to the upper river as shown on the location map. Numerous dirt roads and trails give access to the river at intermediate points. The recreational values of the Manistee depend on its characteristics of streamflow, water quality, and bed and banks. This atlas describes these characteristics and shows how they relate to recreational use.</p><p>Much of the information presented here was obtained from basic records of the U.S. Geological Survey's Water Resources Division. Additional information was obtained from field reconnaissance surveys in 1968 and 1969. The study was made in cooperation with the Michigan Geological Survey, Gerald E. Eddy, Chief. Assistance was also obtained from other sections of the Michigan Department of Natural Resources.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha436","collaboration":"Prepared in cooperation with the Michigan Geological Survey","usgsCitation":"Hendrickson, G.E., and Doonan, C.J., 1972, Reconnaissance of the Manistee River, a cold-water river in the northwestern part of Michigan's Southern Peninsula: U.S. Geological Survey Hydrologic Atlas 436, 2 Plates: 30 x 31 inches and 44 x 41 inches, https://doi.org/10.3133/ha436.","productDescription":"2 Plates: 30 x 31 inches and 44 x 41 inches","costCenters":[{"id":382,"text":"Michigan Water Science 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