{"pageNumber":"6504","pageRowStart":"162575","pageSize":"25","recordCount":184904,"records":[{"id":3981,"text":"cir558 - 1968 - Generalized hydrology of prairie potholes on the Coteau du Missouri, North Dakota","interactions":[],"lastModifiedDate":"2018-02-16T16:18:03","indexId":"cir558","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"558","title":"Generalized hydrology of prairie potholes on the Coteau du Missouri, North Dakota","docAbstract":"This report presents all the information, obtained during the investigation, that lends itself to generalization. It describes conditions on that part of the Coteau du Missouri where there is little integration of drainage systems. The surface of the glacial drift in this region is dotted with shallow depressions known as prairie potholes that hold water for varying lengths of time. Precipitation directly on a pothole is the basic source of its water supply, but it is only about half the potential evaporation; therefore, potholes tend to go dry. Basin inflow from melting snow or rain occurs only when the soil is frozen or saturated, a condition so erratic in occurrence that seasonal or annual precipitation is of little value as an indication of basin inflow. Net seepage outflow occurs from potholes on the higher parts of the Coteau at very low rates, but it can amount to 20 to 30 percent of the total water loss from a pothole. Net seepage inflow occurs at the potholes on the lower parts of the Coteau. \r\n\r\nThe phreatic surface (water table) tends to be a subdued image of the topography and is generally very near the land surface. The water surfaces of the potholes are part of the phreatic surface, and therefore they can be used to prepare a contour map of the phreatic surface; wells usually act as piezometers and thus are useless for such a purpose. \r\n\r\nGenerally, potholes with water relatively low in dissolved solids have net seepage outflow, and those with water containing high concentration of dissolved solids have net seepage inflow. The direction of ground-water movement can therefore be inferred from the quality of water in potholes. The total salinity of water in a pothole is largely a function of the rate of ground-water flow and the relationship of seepage inflow to outflow. \r\n\r\nThe species of emergent aquatic vegetation that grow in a pothole are directly related to the permanence and salinity of the water at the particular site of each species. The report contains a table of the common species that can be used as indicators of these conditions.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir558","usgsCitation":"Eisenlohr, W.S., and Sloan, C.E., 1968, Generalized hydrology of prairie potholes on the Coteau du Missouri, North Dakota: U.S. Geological Survey Circular 558, v, 12 p., https://doi.org/10.3133/cir558.","productDescription":"v, 12 p.","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":31066,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0558/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124470,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0558/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aed63","contributors":{"authors":[{"text":"Eisenlohr, William Stewart","contributorId":36533,"corporation":false,"usgs":true,"family":"Eisenlohr","given":"William","email":"","middleInitial":"Stewart","affiliations":[],"preferred":false,"id":147945,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sloan, Charles E.","contributorId":74364,"corporation":false,"usgs":true,"family":"Sloan","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":147946,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38758,"text":"pp613A - 1968 - An early Reticuloceras Zone fauna from the Hale Formation in northwestern Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:09:54","indexId":"pp613A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"613","chapter":"A","title":"An early Reticuloceras Zone fauna from the Hale Formation in northwestern Arkansas","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to paleontology, 1968","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp613A","usgsCitation":"Gordon, M., 1968, An early Reticuloceras Zone fauna from the Hale Formation in northwestern Arkansas: U.S. Geological Survey Professional Paper 613, p. A1-A21, https://doi.org/10.3133/pp613A.","productDescription":"p. A1-A21","costCenters":[],"links":[{"id":119649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0613a/report-thumb.jpg"},{"id":65622,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0613a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684c51","contributors":{"authors":[{"text":"Gordon, Mackenzie Jr.","contributorId":13225,"corporation":false,"usgs":true,"family":"Gordon","given":"Mackenzie","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":220401,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3973,"text":"cir460C - 1968 - The Vigil Network: Preservation and access of data","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir460C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"460","chapter":"C","title":"The Vigil Network: Preservation and access of data","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir460C","usgsCitation":"Emmett, W.W., and Hadley, R.F., 1968, The Vigil Network: Preservation and access of data: U.S. Geological Survey Circular 460, iii, 21 p. :maps ;26 cm., https://doi.org/10.3133/cir460C.","productDescription":"iii, 21 p. :maps ;26 cm.","costCenters":[],"links":[{"id":120761,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0460c/report-thumb.jpg"},{"id":31058,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0460c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d5c6","contributors":{"authors":[{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":147932,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":147931,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61780,"text":"gq730 - 1968 - Geologic map of the Mount Callaghan quadrangle, Lander County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:10:29","indexId":"gq730","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"730","title":"Geologic map of the Mount Callaghan quadrangle, Lander County, Nevada","language":"ENGLISH","doi":"10.3133/gq730","usgsCitation":"Stewart, J.H., and McKee, E.H., 1968, Geologic map of the Mount Callaghan quadrangle, Lander County, Nevada: U.S. Geological Survey Geologic Quadrangle 730, 1 map., https://doi.org/10.3133/gq730.","productDescription":"1 map.","costCenters":[],"links":[{"id":108213,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12285.htm","linkFileType":{"id":5,"text":"html"},"description":"12285"},{"id":103451,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2037.htm","linkFileType":{"id":5,"text":"html"},"description":"2037"},{"id":248072,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0730/report.pdf","size":"29","linkFileType":{"id":1,"text":"pdf"}},{"id":252732,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0730/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117,39.5 ], [ -117,39.75 ], [ -116.75,39.75 ], [ -116.75,39.5 ], [ -117,39.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a5d5","contributors":{"authors":[{"text":"Stewart, John Harris","contributorId":63790,"corporation":false,"usgs":true,"family":"Stewart","given":"John","email":"","middleInitial":"Harris","affiliations":[],"preferred":false,"id":266357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":266356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35332,"text":"b1254H - 1968 - Wapiti formation and Trout Peak Trachyandesite, northwestern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:09:35","indexId":"b1254H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1254","chapter":"H","title":"Wapiti formation and Trout Peak Trachyandesite, northwestern Wyoming","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1254H","usgsCitation":"Nelson, W.H., and Pierce, W.G., 1968, Wapiti formation and Trout Peak Trachyandesite, northwestern Wyoming: U.S. Geological Survey Bulletin 1254, p. H1-H11, illus., map. ;24 cm., https://doi.org/10.3133/b1254H.","productDescription":"p. H1-H11, illus., map. ;24 cm.","costCenters":[],"links":[{"id":166069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1254h/report-thumb.jpg"},{"id":63191,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1254h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd4c9","contributors":{"authors":[{"text":"Nelson, Willis H.","contributorId":84777,"corporation":false,"usgs":true,"family":"Nelson","given":"Willis","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":214465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, William Gamewell","contributorId":105361,"corporation":false,"usgs":true,"family":"Pierce","given":"William","email":"","middleInitial":"Gamewell","affiliations":[],"preferred":false,"id":214466,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68473,"text":"ha284 - 1968 - Ground-water resources of the eastern shore of Virginia and the James, York, and Rappahannock river basins of Virginia east of the fall line","interactions":[],"lastModifiedDate":"2012-02-02T00:13:37","indexId":"ha284","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"284","title":"Ground-water resources of the eastern shore of Virginia and the James, York, and Rappahannock river basins of Virginia east of the fall line","language":"ENGLISH","doi":"10.3133/ha284","usgsCitation":"DeBuchananne, G.D., 1968, Ground-water resources of the eastern shore of Virginia and the James, York, and Rappahannock river basins of Virginia east of the fall line: U.S. Geological Survey Hydrologic Atlas 284, 2 maps on sheet 112 x 61 cm. fold. in envelope 30 cm., https://doi.org/10.3133/ha284.","productDescription":"2 maps on sheet 112 x 61 cm. fold. in envelope 30 cm.","costCenters":[],"links":[{"id":187934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90018,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/284/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90019,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/284/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a661","contributors":{"authors":[{"text":"DeBuchananne, George D.","contributorId":10040,"corporation":false,"usgs":true,"family":"DeBuchananne","given":"George","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":278293,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41965,"text":"ofr68294 - 1968 - Aeromagnetic map of the Wilson Reservoir, Bull Run, and Owyhee quadrangles and part of the Hat Peak quadrangle, Elko County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr68294","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-294","title":"Aeromagnetic map of the Wilson Reservoir, Bull Run, and Owyhee quadrangles and part of the Hat Peak quadrangle, Elko County, Nevada","language":"ENGLISH","doi":"10.3133/ofr68294","usgsCitation":"Petrafeso, F.A., and Long, C.L., 1968, Aeromagnetic map of the Wilson Reservoir, Bull Run, and Owyhee quadrangles and part of the Hat Peak quadrangle, Elko County, Nevada: U.S. Geological Survey Open-File Report 68-294, 1 map, https://doi.org/10.3133/ofr68294.","productDescription":"1 map","costCenters":[],"links":[{"id":136666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79725,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0294/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68bdbb","contributors":{"authors":[{"text":"Petrafeso, F. A.","contributorId":50874,"corporation":false,"usgs":true,"family":"Petrafeso","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":225780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, C. L.","contributorId":98699,"corporation":false,"usgs":true,"family":"Long","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":225781,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4005,"text":"cir586 - 1968 - Index of surface-water records to September 30, 1967 - Hawaii and other Pacific areas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir586","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"586","title":"Index of surface-water records to September 30, 1967 - Hawaii and other Pacific areas","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir586","usgsCitation":"Eisenhuth, H., 1968, Index of surface-water records to September 30, 1967 - Hawaii and other Pacific areas: U.S. Geological Survey Circular 586, 25 p. ;26 cm., https://doi.org/10.3133/cir586.","productDescription":"25 p. ;26 cm.","costCenters":[],"links":[{"id":120822,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0586/report-thumb.jpg"},{"id":31090,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0586/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2f63","contributors":{"authors":[{"text":"Eisenhuth, H.P.","contributorId":38140,"corporation":false,"usgs":true,"family":"Eisenhuth","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":147970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68342,"text":"ha186 - 1968 - Availability of ground water in parts of the Cairo and Barlow quadrangles in the Jackson Purchase region, Kentucky","interactions":[],"lastModifiedDate":"2022-11-28T20:00:07.737023","indexId":"ha186","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"186","title":"Availability of ground water in parts of the Cairo and Barlow quadrangles in the Jackson Purchase region, Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha186","usgsCitation":"Hansen, A., 1968, Availability of ground water in parts of the Cairo and Barlow quadrangles in the Jackson Purchase region, Kentucky: U.S. Geological Survey Hydrologic Atlas 186, 1 Plate: 51.50 × 40.00 inches, https://doi.org/10.3133/ha186.","productDescription":"1 Plate: 51.50 × 40.00 inches","costCenters":[],"links":[{"id":409746,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15549.htm","linkFileType":{"id":5,"text":"html"}},{"id":89818,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/186/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":190416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"Kentucky","otherGeospatial":"Barlow quadrangle, Cairo quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.175,\n              37\n            ],\n            [\n              -89.175,\n              37.125\n            ],\n            [\n              -89,\n              37.125\n            ],\n            [\n              -89,\n              37\n            ],\n            [\n              -89.175,\n              37\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660589","contributors":{"authors":[{"text":"Hansen, Arnold J.","contributorId":33316,"corporation":false,"usgs":true,"family":"Hansen","given":"Arnold J.","affiliations":[],"preferred":false,"id":278065,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2381,"text":"wsp1856 - 1968 - Water for the growing needs of Harrison County, Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1856","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1856","title":"Water for the growing needs of Harrison County, Mississippi","docAbstract":"The potential for water-supply development in Harrison County is almost unlimited. During an average year, more than 350 billion gallons of water flow into the Gulf of Mexico from the streams of the county. With storage reservoirs these streams have a potential sustained supply of hundreds of millions of. gallons per day. Recreation uses and flood-control benefits could also be considered in reservoir design. \r\n\r\nUpstream from the zones of salt-water penetration, mineral content is low and fairly constant. Water in the streams generally has high color and low pH ; treatment would be required for most municipal and industrial uses. Impoundment in reservoirs normally would have little effect on the quality of the surface water. However, impoundment would trap most of the suspended-sediment load of the streams. \r\n\r\nFlooding along the major streams of Harrison County is a minor hazard at present (1966), but with further industrial development and urbanization, flooding in these now rural areas could become serious. Intense rainfall from thunderstorms and hurricanes causes serious local flooding in the populous areas near the coast. Tidal flooding, a result of tropical storms, is an ever-present hazard in areas near the coast. \r\n\r\nThe ground-water reservoir, which at present provides all fresh-water supplies, is capable of supporting many times the 25 million gallons per day withdrawal through existing wells. Fresh water occurs to depths as great as 2,500 feet in sand aquifers of Pliocene and Miocene age. Many of the aquifers have high transmissibility; most of those tested have transmissibility in the range, of 50,000-100,000 gallons per day per foot. Although few wells produce more than 1,000 gallons per minute, several of the aquifers can yield two to three times that amount to wells designed for the higher production. \r\n\r\nArtesian water levels along the coast are declining at a rate of 1 foot per year on the average; however, water levels are still above or only slightly below the land surface in most places, and considerable additional drawdown is economically available. Newly discovered deep aquifers (1,700-2,500 ft) have water levels 100 feet above the surface and probably will provide flow yields of 2,000 gallons per minute or more. The temperature of this deep water is nearly 100?F. \r\n\r\nNearly all the ground water is of good quality and requires little or no treatment for most uses. It is soft, and total mineral content is usually less than 250 parts per million. Color is seldom a problem, although it may have to be considered in the undeveloped deep aquifers. The pH ordinarily is greater than 7.0, but it is slightly less than 7.0 in most places in the shallow aquifers.","language":"ENGLISH","publisher":"Geological Survey; for sale by the Supt. of Docs.] U.S. Govt. Print. 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,{"id":3952,"text":"cir592 - 1968 - Interpreting pan-concentrate analysis of stream sediments in geochemical exploration for gold","interactions":[],"lastModifiedDate":"2017-06-25T13:10:19","indexId":"cir592","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"592","title":"Interpreting pan-concentrate analysis of stream sediments in geochemical exploration for gold","docAbstract":"A study of methods of collecting and processing samples to determine whether or not gold is present in areas of moderate size was undertaken in the northwestern part of the San Juan Mountains, Colo. As part of this study, 57 samples of pan concentrates were taken from streams draining three types of areas: (1)'barren' areas, where gold mineralization might be geologically possible but no deposits are known, (2) slightly mineralized areas that contain only a few known veins and prospects and small mines, and (3) well-mineralized areas that contain numerous veins and some very productive mines. The concentrate samples were analyzed by the fire-assay-atomic-absorption method. Replicate analyses of large samples gave results consistent enough to permit placing considerable confidence in the results obtained for smaller samples on which only one analysis was made. For general field practice, it is necessary to pan only enough sand and gravel to yield about 15 grams of concentrate. The analytical r6sults are also quantitatively compatible with known geologic relations and indicate that a few samples from a stream are adequate to distinguish between 'barren' and mineralized areas and to determine the relative amount of gold in mineralized areas. In other areas of similar gold deposits, data of this type should help decide whether more intensive search for gold deposits is justified.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir592","usgsCitation":"Fischer, R.P., and Fisher, F.S., 1968, Interpreting pan-concentrate analysis of stream sediments in geochemical exploration for gold: U.S. Geological Survey Circular 592, iii, 9 p. :illus., map. ;26 cm., https://doi.org/10.3133/cir592.","productDescription":"iii, 9 p. :illus., map. ;26 cm.","costCenters":[],"links":[{"id":31039,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0592/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0592/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfc29","contributors":{"authors":[{"text":"Fischer, Richard Philip","contributorId":94283,"corporation":false,"usgs":true,"family":"Fischer","given":"Richard","email":"","middleInitial":"Philip","affiliations":[],"preferred":false,"id":147887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, Frederick S.","contributorId":17979,"corporation":false,"usgs":true,"family":"Fisher","given":"Frederick","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":147886,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4003,"text":"cir579 - 1968 - Index of surface-water records to September 30, 1967: Part 9. - Colorado River basin","interactions":[{"subject":{"id":3992,"text":"cir509 - 1965 - Index of surface-water records to December 31, 1963: Part 9. - Colorado River basin","indexId":"cir509","publicationYear":"1965","noYear":false,"title":"Index of surface-water records to December 31, 1963: Part 9. - Colorado River basin"},"predicate":"SUPERSEDED_BY","object":{"id":4003,"text":"cir579 - 1968 - Index of surface-water records to September 30, 1967: Part 9. - Colorado River basin","indexId":"cir579","publicationYear":"1968","noYear":false,"title":"Index of surface-water records to September 30, 1967: Part 9. - Colorado River basin"},"id":1},{"subject":{"id":4003,"text":"cir579 - 1968 - Index of surface-water records to September 30, 1967: Part 9. - Colorado River basin","indexId":"cir579","publicationYear":"1968","noYear":false,"title":"Index of surface-water records to September 30, 1967: Part 9. - Colorado River basin"},"predicate":"SUPERSEDED_BY","object":{"id":25119,"text":"cir659 - 1971 - Index of surface-water records to September 30, 1970: Part 9. - Colorado River basin","indexId":"cir659","publicationYear":"1971","noYear":false,"title":"Index of surface-water records to September 30, 1970: Part 9. - Colorado River basin"},"id":2}],"supersededBy":{"id":25119,"text":"cir659 - 1971 - Index of surface-water records to September 30, 1970: Part 9. - Colorado River basin","indexId":"cir659","publicationYear":"1971","noYear":false,"title":"Index of surface-water records to September 30, 1970: Part 9. - Colorado River basin"},"lastModifiedDate":"2017-02-21T17:02:29","indexId":"cir579","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"579","title":"Index of surface-water records to September 30, 1967: Part 9. - Colorado River basin","docAbstract":"<p>This report lists the streamflow and reservoir stations in the Colorado River basin for which records have been or are to be published in reports of the Geological Survey for periods through September 30, 1967. 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,{"id":4211,"text":"cir574 - 1968 - Index of surface-water records to September 30, 1967 - Part 4, St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:47","indexId":"cir574","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"574","title":"Index of surface-water records to September 30, 1967 - Part 4, St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir574","usgsCitation":"Anderson, B., and Ham, C., 1968, Index of surface-water records to September 30, 1967 - Part 4, St. Lawrence River basin: U.S. Geological Survey Circular 574, 39 p. :ill., map ;26 cm., https://doi.org/10.3133/cir574.","productDescription":"39 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":118230,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0574/report-thumb.jpg"},{"id":31325,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0574/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2eaf","contributors":{"authors":[{"text":"Anderson, B.A.","contributorId":73581,"corporation":false,"usgs":true,"family":"Anderson","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":148415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ham, C.B.","contributorId":73582,"corporation":false,"usgs":true,"family":"Ham","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":148416,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62415,"text":"gq711 - 1968 - Bedrock geologic map of the Castle Reef quadrangle, Teton and Lewis and Clark Counties, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:10:42","indexId":"gq711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"711","title":"Bedrock geologic map of the Castle Reef quadrangle, Teton and Lewis and Clark Counties, Montana","language":"ENGLISH","doi":"10.3133/gq711","usgsCitation":"Mudge, M.R., 1968, Bedrock geologic map of the Castle Reef quadrangle, Teton and Lewis and Clark Counties, Montana: U.S. Geological Survey Geologic Quadrangle 711, 1 map., https://doi.org/10.3133/gq711.","productDescription":"1 map.","costCenters":[],"links":[{"id":103433,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2019.htm","linkFileType":{"id":5,"text":"html"},"description":"2019"},{"id":180152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.75,47.6175 ], [ -112.75,47.75 ], [ -112.61749999999999,47.75 ], [ -112.61749999999999,47.6175 ], [ -112.75,47.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db6363b2","contributors":{"authors":[{"text":"Mudge, Melville Rhodes","contributorId":77119,"corporation":false,"usgs":true,"family":"Mudge","given":"Melville","email":"","middleInitial":"Rhodes","affiliations":[],"preferred":false,"id":267352,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62837,"text":"gq726 - 1968 - Geologic map of the Camp Desert Rock quadrangle, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:10:41","indexId":"gq726","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"726","title":"Geologic map of the Camp Desert Rock quadrangle, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/gq726","usgsCitation":"Hinrichs, E.N., 1968, Geologic map of the Camp Desert Rock quadrangle, Nye County, Nevada: U.S. Geological Survey Geologic Quadrangle 726, 1 map., https://doi.org/10.3133/gq726.","productDescription":"1 map.","costCenters":[],"links":[{"id":103448,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2034.htm","linkFileType":{"id":5,"text":"html"},"description":"2034"},{"id":248985,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0726/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":251658,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0726/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.11749999999999,36.6175 ], [ -116.11749999999999,36.75 ], [ -116,36.75 ], [ -116,36.6175 ], [ -116.11749999999999,36.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d493","contributors":{"authors":[{"text":"Hinrichs, E. Neal","contributorId":46488,"corporation":false,"usgs":true,"family":"Hinrichs","given":"E.","email":"","middleInitial":"Neal","affiliations":[],"preferred":false,"id":267938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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