The Missouri Basin Region lies in the north-central part of the United States and southern Canada. It includes parts of Alberta and Saskatchewan in Canada; parts of Montana, Wyoming, North Dakota, South Dakota, Minnesota, Iowa, Colorado, Kansas, and Missouri, and all of Nebraska in the United States. The region includes about one-sixth of the contiguous United States and requires large water supplies for irrigation, industrial, public, and rural uses. Climate ranges from semiarid to subhumid. Normal annual precipitation increases generally eastward in the downstream direction, but precipitation is not a dependable source of supply. The Missouri River and its tributaries furnish water to many users, but surface water is often inadequate to meet large demands. Numerous surface reservoirs help to regulate streamflow and provide storage, but they also allow an increase in evapotranspiration, which in some areas exceeds normal precipitation. Ground water occurs in aquifers classified as alluvial deposits of sand and gravel, glacial deposits, dune-sand deposits, basin-fill deposits of sand and gravel, sandstone, siltstone, fractured sandy clay, limestone, and dolomite. Ground water can be developed and managed in an orderly manner provided adequate geologic and hydrologic data are available to determine aquifer characteristics and response to pumping and other hydraulic stresses. These data and determinations are essential to design, testing, and implementation of water management plans.
\nUnconsolidated and semiconsolidated aquifers include valley-fill alluvium, areally extensive alluvium, glacial deposits, and basin-fill deposits. The aquifers normally consist of alluvial sand and gravel that contain unconfined ground water that lies near the land surface. Many wells completed in the alluvial aquifers have high yields of good-quality water because most alluvial aquifers are highly transmissive and hydraulically connected to streams. Aquifers in glacial deposits may be difficult to locate and in some areas contain saline water; nevertheless, these aquifers are sources of water supply for many users. Basin-fill aquifers are as much as several thousand feet thick, and many contain large ground-water supplies. Ground-water mining has occurred in semiconsolidated aquifers because of withdrawals from wells. Unconsolidated and semiconsolidated aquifers have potential for conjunctive use with surface water, recycling to reuse available supplies, artificial recharge, and salvage of evapotranspired water.
\nSandstone aquifers lie near the land surface and in structural basins. Interbasin movement of ground water occurs in the Virgelle (Milk River aquifer), Fox Hills-basal Hell Creek, and Dakota aquifers. Sandstone aquifers are less transmissive than unconsolidated and semiconsolidated aquifers in general. Confined sandstone aquifers are common, and flowing wells are obtained in many areas. However, flowing wells may cause large declines in water levels if uncontrolled. Water quality is variable in sandstone aquifers but is adequate for most needs. Sandstone aquifers have potential for artificial recharge, induced interaquifer leakage, conjunctive use with surface water, and mining of ground water.
\nLimestone and dolomite aquifers are extensive in the region, but in some areas they lie deep below the land surface. The occurrence of ground water in small pores, fractures, or large caverns causes yields from wells to range widely. Large flows through cavern systems in the aquifers are indicated by large springs in some areas. Water quality is extremely variable and must be considered in any water-development plan. Limestone and dolomite aquifers have potential for development of large water supplies in some areas. The development may be aided by induced recharge and interaquifer leakage.
\nSaline ground water occurs throughout the Missouri Basin Region. Dissolved-solids concentration as much as 30,000 milligrams per liter has been measured in aquifers in glacial deposits in Montana. Saline water is common in sandstone aquifers in Wyoming, North Dakota, and South Dakota; maximum reported concentration is 280,000 milligrams per liter in water from the Tensleep Sandstone in Wyoming. Limestone contains saline water in many areas; maximum dissolved-solids concentration is about 350,000 milligrams per liter for the Madison Group in the Williston Basin in North Dakota.
\nComprehensive water-management planning in the Missouri Basin Region will require periodic or continuing inventory of precipitation, streamflow, surface-water storage, and ground water. Water demands for irrigation, industrial, public supply, and rural use are increasing rapidly. Reliance on ground-water supplies is increasing even though in many areas the ground water is still mostly undeveloped. Optimal use of water supplies will require the establishment of realistic goals and carefully conceived water-management plans, each of which will necessarily be based on an adequate baseline of hydrologic data and knowledge of the highly variable hydrologic systems in the region.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813Q","usgsCitation":"Taylor, O., 1978, Summary appraisals of the nation's ground-water resources – Missouri basin region: U.S. Geological Survey Professional Paper 813, Report: v., 41 p.; 3 Plates: 25.50 x 20.32 inches or smaller, https://doi.org/10.3133/pp813Q.","productDescription":"Report: v., 41 p.; 3 Plates: 25.50 x 20.32 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","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":392897,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5071.htm"},{"id":123063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813q/report-thumb.jpg"},{"id":65559,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813q/report.pdf","text":"Report","size":"15.58 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":65558,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813q/plate-3.pdf","text":"Plate 3","size":"7.46 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":65557,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813q/plate-2.pdf","text":"Plate 2","size":"7.25 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":65556,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813q/plate-1.pdf","text":"Plate 1","size":"7.64 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"}],"country":"United States","state":"Colorado, Iowa, Kansas, Minnesota, Missouri, Montana, Nebraska, North Dakota, South Dakota, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.99414062499999,\n 49.49667452747045\n ],\n [\n -111.4453125,\n 50.45750402042058\n ],\n [\n -108.896484375,\n 50.3454604086048\n ],\n [\n -104.853515625,\n 50.12057809796008\n ],\n [\n -102.041015625,\n 49.15296965617042\n ],\n [\n -98.96484375,\n 47.635783590864854\n ],\n [\n -97.822265625,\n 46.92025531537451\n ],\n [\n -97.55859375,\n 46.31658418182218\n ],\n [\n -97.3828125,\n 45.583289756006316\n ],\n [\n -96.328125,\n 44.77793589631623\n ],\n [\n -95.537109375,\n 44.02442151965934\n ],\n [\n -94.921875,\n 43.51668853502909\n ],\n [\n -93.603515625,\n 42.42345651793833\n ],\n [\n -92.021484375,\n 40.91351257612758\n ],\n [\n -91.49414062499999,\n 39.027718840211605\n ],\n [\n -91.40625,\n 37.50972584293751\n ],\n [\n -92.63671875,\n 36.87962060502676\n ],\n [\n -94.5703125,\n 37.43997405227057\n ],\n [\n -96.85546875,\n 37.92686760148135\n ],\n [\n -98.7890625,\n 37.92686760148135\n ],\n [\n -103.88671875,\n 38.20365531807149\n ],\n [\n -105.46875,\n 38.134556577054134\n ],\n [\n -107.05078125,\n 39.16414104768742\n ],\n [\n -108.45703125,\n 41.31082388091818\n ],\n [\n -110.21484375,\n 42.87596410238254\n ],\n [\n -111.09374999999999,\n 44.213709909702054\n ],\n [\n -111.4453125,\n 44.653024159812\n ],\n [\n -112.939453125,\n 44.96479793033104\n ],\n [\n -112.939453125,\n 45.460130637921004\n ],\n [\n -113.90625,\n 46.37725420510028\n ],\n [\n -114.169921875,\n 47.69497434186282\n ],\n [\n -113.99414062499999,\n 49.49667452747045\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69969c","contributors":{"authors":[{"text":"Taylor, O. James","contributorId":23958,"corporation":false,"usgs":true,"family":"Taylor","given":"O. James","affiliations":[],"preferred":false,"id":220313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10364,"text":"ofr78448 - 1978 - Spectral reflectance measurements of plants in the East Tintic Mountains, Utah","interactions":[],"lastModifiedDate":"2026-02-04T17:43:23.773158","indexId":"ofr78448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-448","title":"Spectral reflectance measurements of plants in the East Tintic Mountains, Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78448","usgsCitation":"Milton, N., 1978, Spectral reflectance measurements of plants in the East Tintic Mountains, Utah: U.S. Geological Survey Open-File Report 78-448, 126 p., https://doi.org/10.3133/ofr78448.","productDescription":"126 p.","costCenters":[],"links":[{"id":143400,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0448/report-thumb.jpg"},{"id":499527,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0448/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"East Tintic Mountains","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"47\",\"properties\":{\"name\":\"Utah\",\"nation\":\"USA 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Nancy","contributorId":85188,"corporation":false,"usgs":true,"family":"Milton","given":"Nancy","affiliations":[],"preferred":false,"id":161260,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26721,"text":"wri77123 - 1978 - Fluvial sediment study of Fishtrap and Dewey Lakes drainage basins, Kentucky-Virginia","interactions":[],"lastModifiedDate":"2025-01-08T22:40:11.942634","indexId":"wri77123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-123","title":"Fluvial sediment study of Fishtrap and Dewey Lakes drainage basins, Kentucky-Virginia","docAbstract":"Fourteen drainage basins above Fishtrap and Dewey Lakes in the Levisa Fork and Johns Creek drainage basins of eastern Kentucky and southwestern Virginia were studied to determine sedimentation rates and origin of sediment entering the two lakes. The basins ranged in size from 1.68 to 297 square miles. Sediment yields ranged from 2,890 to 21,000 tons per square mile where surface-mining techniques predominated, and from 732 to 3 ,470 tons per square mile where underground mining methods predominated. Yields, in terms of tons per acre-foot of runoff, ranged from 2.2 to 15 for surface-mined areas, and from 0.5 to 2.7 for underground-mined areas. Water and sediment discharges from direct runoff during storms were compared for selected surface-mined and underground-mined areas. Data points of two extensively surface-mined areas, one from the current project and one from a previous project in Beaver Creek basin, McCreary County, Kentucky, grouped similarly in magnitude and by season. Disturbed areas from mining activities determined from aerial photographs reached 17 percent in one study area where extensive surface mining was being practiced. For most areas where underground mining was practiced, percentage disturbed area was almost negligible. Trap efficiency of Fishtrap Lake was 89 percent, and was 62 percent for Dewey Lake. Average annual deposition rates were 464 and 146 acre-feet for Fishtrap and Dewey Lakes, respectively. The chemical quality of water in the Levisa Fork basin has been altered by man 's activities.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri77123","usgsCitation":"Curtis, W.F., Flint, R.F., George, F.H., and Santos, J.F., 1978, Fluvial sediment study of Fishtrap and Dewey Lakes drainage basins, Kentucky-Virginia: U.S. Geological Survey Water-Resources Investigations Report 77-123, xi, 92 p., https://doi.org/10.3133/wri77123.","productDescription":"xi, 92 p.","costCenters":[],"links":[{"id":366194,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158260,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0123/report-thumb.jpg"},{"id":465926,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35124.htm","text":"Dewey Lake","linkFileType":{"id":5,"text":"html"}},{"id":465927,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35125.htm","text":"Fishtrap Lake","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Kentucky, Virginia","otherGeospatial":"Dewey Lake, Fishtrap Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.7764892578125,\n 37.38979975341983\n ],\n [\n -82.29583740234375,\n 37.38979975341983\n ],\n [\n -82.29583740234375,\n 37.75334401310656\n ],\n [\n -82.7764892578125,\n 37.75334401310656\n ],\n [\n -82.7764892578125,\n 37.38979975341983\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47c3e4b07f02db4a7e1d","contributors":{"authors":[{"text":"Curtis, William F.","contributorId":70433,"corporation":false,"usgs":true,"family":"Curtis","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flint, Russell F.","contributorId":91144,"corporation":false,"usgs":true,"family":"Flint","given":"Russell","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196889,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"George, Frederick H.","contributorId":16462,"corporation":false,"usgs":true,"family":"George","given":"Frederick","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":196886,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Santos, John F.","contributorId":21530,"corporation":false,"usgs":true,"family":"Santos","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196887,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":61080,"text":"mf880F - 1978 - Geochemical maps showing the distribution and abundance of gold in stream sediments and of gold and silver in heavy-mineral concentrates in the Seward and Blying Sound quadrangles, Alaska","interactions":[],"lastModifiedDate":"2025-04-23T13:28:42.448896","indexId":"mf880F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"880","chapter":"F","title":"Geochemical maps showing the distribution and abundance of gold in stream sediments and of gold and silver in heavy-mineral concentrates in the Seward and Blying Sound quadrangles, Alaska","docAbstract":"Reconnaissance geochemical and mineralogical sampling was done in the Seward and Blying Sound quadrangles during 1975 and 1976 as part of the Alaska Mineral Resources Assessment Program (AMRAP). These maps show the distribution and abundance of gold and silver in heavy-mineral concentrates.
Stream-sediment and heavy-mineral concentrate samples were collected from active stream channels and locally, from the interface of streambeds with intermediate- to low-tide beaches. Most of the stream sediment is fine- to coarse-grained sand, with a clay-silt fraction in streams discharging from glaciers. Stream sediment samples were air dried and sieved through a 80-mesh (0.2 mm) sieve, and the minus-80 mesh fraction was saved for analysis. A split of each sample was analyzed for gold by a 10 gram atomic-absorption method (Ward and others, 1969). Another split was analyzed for 16 elements by a semiquantitative spectrographic method (Grimes and Marranzino, 1968).
The heavy-mineral concentrates were obtained by panning stream sediments in the field to remove most of the light minerals. The panned samples were sieved though a 20-mesh (0.8 mm) screen in the laboratory, and the minus-20 mesh fraction was further separated with bromoform (specific gravity: 2.86) to remove any remaining light-mineral grains. Magnetite and other strongly magnetic heavy minerals were removed from the heavy-mineral fraction by use of a hand magnet. The remaining sample was passed through a Frantz Isodynamic Separator1 and a nonmagnetic fraction was obtained at a setting of 0.6 amperes. A split of this fraction was pulverized and analyzed for 16 elements including gold and silver by semiquantitative spectrographic method used for analyzing the stream sediment. The remaining split of the nonmagnetic fraction was examined for its mineralogic composition using a binocular microscope and X-ray diffraction. The nonmagnetic concentrates primarily contain muscovite, sphene, zircon, apatite, rutile, and anatase. Ore minerals such as gold, scheelite, minium, and most sulfides are also found in this fraction.
Sample sites and gold and silver values (in parts per million) are indicated by symbols as defined in the histograms. The maps show two populations for gold in stream sediments and for gold and silver heavy mineral concentrates. One population consists of generally higher gold and silver values found in samples collected in the sedimentary terrane in the western half of the area. The other population consists of generally lower gold and silver values found in samples collected in areas of sheeted basalt dikes, pillow basalts, and sedimentary terrane in the eastern half of the area. The anomalous silver values found on Knight Island and Latouche Island are associated with chalcopyright- and pyrite-bearing rocks.
1 The use of trade names is for descriptive purposes only and does not constitute endorsement of those products by the U.S. Geological Survey.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78279","collaboration":"Prepared in cooperation with the New York State Museum and Science Service Geological Survey","usgsCitation":"U.S. Geological Survey, 1978, Aeromagnetic map of the eastern part of the Adirondacks Mountains, New York: U.S. Geological Survey Open-File Report 78-279, 1 Plate: 24.55 x 33.66 inches, https://doi.org/10.3133/ofr78279.","productDescription":"1 Plate: 24.55 x 33.66 inches","costCenters":[],"links":[{"id":136548,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0279/report-thumb.jpg"},{"id":277901,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0279/plate-1.pdf"},{"id":463509,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14665.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"New York","otherGeospatial":"Adirondack Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.4976,42.9966 ], [ -74.4976,44.7497 ], [ -73.2493,44.7497 ], [ -73.2493,42.9966 ], [ -74.4976,42.9966 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b8ef","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":147999,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":530732,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28940,"text":"wri7851 - 1978 - Physiography and surficial geology of the copper-nickel study region, northeastern Minnesota","interactions":[],"lastModifiedDate":"2024-01-08T22:28:23.652704","indexId":"wri7851","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"78-51","title":"Physiography and surficial geology of the copper-nickel study region, northeastern Minnesota","docAbstract":"The Copper-Nickel study region lies in the Superior Upland physiographic province and is located approximately 60 miles north of Duluth and 100 miles southeast of International Falls, Minnesota. It straddles the Laurentian Divide, which separates Hudson Bay and Lake Superior drainage. The topography exhibits a southwesterly trending lineation that parallels the strike of southeastward-dipping bedrock units and the southwestward direction of ice movement during Pleistocene glaciation. For this study, the region has been divided into seven physiographic areas based on geomorphic features related to the bedrock surface, glacial deposits, and hydrogeologic significance.
\nThe surficial geology is largely a result of two southwestward advances of the Rainy Lobe of the Laurentian ice sheet. The Toimi Drumlin Field, the oldest glacial deposit, covers much of the southern part of the region. It is bounded on the north by the Vermilion Moraine Complex, an east-west trending series of terminal and recessional moraines that mark the southerly extent of the second advance of the Rainy Lobe. Thin ground moraine and small outwash deposits occur both within and north of the Vermilion Moraine Complex except in the Embarrass and Dunka River basins where outwash deposits up to 200 feet in thickness fill a deep bedrock valley.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri7851","collaboration":"Prepared in cooperation with Minnesota Environmental Quality Board Copper-Nickel Study Staff","usgsCitation":"Olcott, P.G., and Siegel, D.I., 1978, Physiography and surficial geology of the copper-nickel study region, northeastern Minnesota: U.S. Geological Survey Water-Resources Investigations Report 78-51, Document: iv, 22 p.; 3 Plates: 20.99 x 25.11 inches or smaller, https://doi.org/10.3133/wri7851.","productDescription":"Document: iv, 22 p.; 3 Plates: 20.99 x 25.11 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":424201,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35256.htm","linkFileType":{"id":5,"text":"html"}},{"id":95737,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0051/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95735,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0051/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95734,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0051/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158311,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0051/report-thumb.jpg"},{"id":95736,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0051/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.25,\n 47.75\n ],\n [\n -91.916667,\n 47.75\n ],\n [\n -91.75,\n 47.916667\n ],\n [\n -91.5,\n 47.77\n ],\n [\n -91.5,\n 47.5\n ],\n [\n -91.75,\n 47.5\n ],\n [\n -91.75,\n 47.25\n ],\n [\n -92.25,\n 47.25\n ],\n [\n -92.25,\n 47.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685996","contributors":{"authors":[{"text":"Olcott, P. G.","contributorId":79903,"corporation":false,"usgs":true,"family":"Olcott","given":"P.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":200651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siegel, D. I.","contributorId":77562,"corporation":false,"usgs":true,"family":"Siegel","given":"D.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":200650,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":26740,"text":"wri78134 - 1978 - Land use, land cover, and drainage on the Albemarle-Pamlico Peninsula, Eastern North Carolina, 1974","interactions":[],"lastModifiedDate":"2025-07-21T17:19:29.617438","indexId":"wri78134","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"78-134","title":"Land use, land cover, and drainage on the Albemarle-Pamlico Peninsula, Eastern North Carolina, 1974","docAbstract":"A land use, land cover, and drainage map of the 2,000-square-mile Albermarle-Pamlico peninsula of eastern North Carolina has been prepared, at a scale of 1:125,000, as part of a larger study of the effects of large-scale land clearing on regional hydrology. The peninsula includes the most extensive area of wetland in North Carolina and one of the largest in the country. In recent years the pace of land clearing on the peninsula has accelerated as land is being converted from forest, swamp, and brushland to agricultural use. Conversion of swamps to intensive farming operations requires profound changes in the landscape. Vegetation is uprooted and burned and ditches and canals are dug to remove excess water. What is the impact of these changes on ground-water supplies and on the streams and surrounding coastal waters which receive the runoff This map will aid in answering these and similar questions that have arisen about the patterns of land use and the artificial drainage system that removes excess water from the land. By showing both land use and drainage, this map can be used to identify those areas where water-related problems may occur and help assess the nature and causes of these problems. The map covers the entire area east of the Suffolk Scarp, an area of about 2,000 square miles, for the year 1974 using data from 1974-76. Land use and land cover were compiled and modified from the U.S. Geological Survey 's Rocky Mount and Manteo LUDA maps. Additional information came from U.S. Geological Survey orthophotoquads, Landsat imagery, and field checking. Drainage was mapped from orthophotoquads, some field inspection, and 7-1/2 minute topographic quadrangle maps.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri78134","collaboration":"Prepared in cooperation with the North Carolina Department of Natural Resources and Community Development","usgsCitation":"Daniel, C., 1978, Land use, land cover, and drainage on the Albemarle-Pamlico Peninsula, Eastern North Carolina, 1974: U.S. Geological Survey Water-Resources Investigations Report 78-134, 2 Plates: 47.94 x 30.89 inches and 47.90 x 31.02 inches, https://doi.org/10.3133/wri78134.","productDescription":"2 Plates: 47.94 x 30.89 inches and 47.90 x 31.02 inches","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":158490,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0134/report-thumb.jpg"},{"id":492647,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0134/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":492646,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0134/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":492648,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0134/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Albemarle-Pamplico Peninsula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.046875,\n 34.44315867450577\n ],\n [\n -78.046875,\n 36.57142382346277\n ],\n [\n -74.99267578125,\n 36.57142382346277\n ],\n [\n -74.99267578125,\n 34.44315867450577\n ],\n [\n -78.046875,\n 34.44315867450577\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf98","contributors":{"authors":[{"text":"Daniel, C.C.","contributorId":53427,"corporation":false,"usgs":true,"family":"Daniel","given":"C.C.","email":"","affiliations":[],"preferred":false,"id":196918,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7355,"text":"ofr78706 - 1978 - Multichannel seismic reflection and sonobuoy refraction data in the outer southern California Borderland","interactions":[],"lastModifiedDate":"2026-02-19T18:42:07.880284","indexId":"ofr78706","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-706","title":"Multichannel seismic reflection and sonobuoy refraction data in the outer southern California Borderland","docAbstract":"During the L1-78-SC cruise of the USGS research vessel S. P. Lee (April 25 - May 11, 1978) seven sonobuoy profiles and 200 km of 24-channel seismic reflection data were recorded in the outer southern California Continental Borderland. These data were obtained, at the request of the Deep Sea Drilling Project (DSDP), to evaluate possible drill sites along the southern California continental margin.
The drill sites shown in Figure 1 were proposed by the Ocean Paleo-environmental Panel for DSDP Leg 63--secheduled for Sept. - Nov. 1978. These sites were selected in order to provide an expanded Neogene record of paleoceanographic-paleoclimatic events and associated evolutionary development of planktic communities along the eastern side of the north Pacific Ocean. Site selection was made prior to this survey on the basis of available single-channel seismic reflection profiles. Thus, the proposed sites shown on Fig. 1 may be relocated or eliminated when the data presented in this report are incorporated with earlier data. The combined data will be evaluated for safety and pollution hazards by Leg 63 site proponents and the DSDP safety panels.
The ship's tracks (Fig. 1) were located by an integrated Satellite-Loran C-Doppler Sonar navigation system. Average survey speed was about 5 kts. A 1326 cu in (21,723 CC) tuned air gun array provided the sound source for both reflection and refraction profiles. The air gun array was fired at 50 m (about 18 sec.) intervals by the integrated navigation system.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78706","usgsCitation":"Crouch, J.K., Holmes, M., McCulloh, T.H., Long, A.T., and Brune, R., 1978, Multichannel seismic reflection and sonobuoy refraction data in the outer southern California Borderland: U.S. Geological Survey Open-File Report 78-706, 3 p., 10 sheets :ill., map ;29 cm., https://doi.org/10.3133/ofr78706.","productDescription":"25 p.","costCenters":[],"links":[{"id":500217,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0706/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141393,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0706/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"California 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H.","contributorId":106494,"corporation":false,"usgs":true,"family":"McCulloh","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":155384,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Long, A. T. along@usgs.gov","contributorId":20744,"corporation":false,"usgs":true,"family":"Long","given":"A.","email":"along@usgs.gov","middleInitial":"T.","affiliations":[],"preferred":false,"id":155380,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Brune, R.H.","contributorId":91491,"corporation":false,"usgs":true,"family":"Brune","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":155383,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":29699,"text":"wri7942 - 1978 - Water-table map of Walworth County, Wisconsin","interactions":[],"lastModifiedDate":"2019-07-26T10:11:49","indexId":"wri7942","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-42","title":"Water-table map of Walworth County, Wisconsin","docAbstract":"A map of the water table in Walworth County in southeastern Wisconsin was prepared using water levels from nearly 600 wells. The work was done as a cooperative project between the U.S. Geological Survey, the University of Wisconsin-Extension, Geological and Natural History Survey, and the Southeastern Wisconsin Regional Planning Commission. The map (scale 1:100 ,000) shows the altitude of the water table in increments of 20 feet, with supplemental 10-foot contours. The altitude ranges from less than 780 feet along parts of the eastern border of the county to more than 1,000 feet in a small area near the central part of the county. (Woodard-USGS)
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7942","usgsCitation":"Sherrill, M.G., and Erickson, J.R., 1978, Water-table map of Walworth County, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 79-42, 1 Plate: 25.07 x 20.53 inches, https://doi.org/10.3133/wri7942.","productDescription":"1 Plate: 25.07 x 20.53 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":159506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0042/report-thumb.jpg"},{"id":365974,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0042/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Walworth County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.5413,42.8445],[-88.3044,42.8444],[-88.3027,42.6134],[-88.3016,42.4979],[-88.4099,42.4977],[-88.5047,42.4981],[-88.6288,42.4985],[-88.6737,42.4977],[-88.7059,42.4972],[-88.7719,42.4957],[-88.7737,42.4958],[-88.774,42.5855],[-88.7744,42.6728],[-88.7753,42.7587],[-88.7757,42.8455],[-88.66,42.8453],[-88.5413,42.8445]]]},\"properties\":{\"name\":\"Walworth\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ccd","contributors":{"authors":[{"text":"Sherrill, Marvin G.","contributorId":91469,"corporation":false,"usgs":true,"family":"Sherrill","given":"Marvin","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":201973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, John R.","contributorId":76365,"corporation":false,"usgs":true,"family":"Erickson","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":201972,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66275,"text":"i1087 - 1978 - Channel migration of the White River in the eastern Uinta Basin, Utah and Colorado","interactions":[],"lastModifiedDate":"2017-02-16T11:09:56","indexId":"i1087","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1087","title":"Channel migration of the White River in the eastern Uinta Basin, Utah and Colorado","docAbstract":"The White River is the largest stream in the southeastern part of the Uinta Basin in Utah and Colorado. This map shows the changes that have occurred in the location of the main channel of the river from 1936 to 1974. The map indicated that certain reaches of the river are subject to different rates of channel migration. Also shown is the boundary of the flood plain, which is mapped at the point of abrupt break in slope. This map documents the position of the river channel prior to any withdrawals of water or alteration of the flow characteristics of the white river that may occur in order to meet water requirements principally associated with the proposed oil-shale industry or other development in the area.
The channel locations were determined from aerial photographs taken at four different time periods for the following Federal agencies: In 1936, U.S. Soil Conservation Services; 1953, U.S. Corps of Engineers; 1965, U.S. Geological Survey; and in 1974, U.S. Bureau of Land Management. The 1936 delineation, which is actually based upon photographs that were taken in 1936 and 1937, was made by projection of the original photographs on a base map that was prepared from 1:24,000 scale topographic maps. The 1953, 1965, and 1974 delineations were produced from stereographic models. The 1965 delineation was compiled from photographs that were taken during 1962-65. The delineation is labeled as 1965 for simplicity, however, because the photographs for 1965 cover about 60 percent of the study read of the river, and because no changed were discernable in those areas of repetitive photographic coverage.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i1087","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Jurado, A., and Fields, F.K., 1978, Channel migration of the White River in the eastern Uinta Basin, Utah and Colorado: U.S. Geological Survey IMAP 1087, 1 Map: 33.95 x 39.64 Inches; Cover: 9.20 x 11.87 inches, https://doi.org/10.3133/i1087.","productDescription":"1 Map: 33.95 x 39.64 Inches; Cover: 9.20 x 11.87 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":255735,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1087/plate-1.pdf","text":"Map I-1087","size":"8.57 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":255736,"rank":300,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/1087/report.pdf","text":"Folio Cover","size":"29.2 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":255737,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1087/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"Colorado, Utah","otherGeospatial":"Uinta Basin, White River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.70083333333334,39.916666666666664 ], [ -109.70083333333334,40.1175 ], [ -109,40.1175 ], [ -109,39.916666666666664 ], [ -109.70083333333334,39.916666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e6296","contributors":{"authors":[{"text":"Jurado, Antonio","contributorId":73264,"corporation":false,"usgs":true,"family":"Jurado","given":"Antonio","email":"","affiliations":[],"preferred":false,"id":274283,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fields, Fred K.","contributorId":69981,"corporation":false,"usgs":true,"family":"Fields","given":"Fred","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":274284,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24071,"text":"ofr78684 - 1978 - Hydrologic environment of the Silurian salt deposits in parts of Michigan, Ohio, and New York","interactions":[],"lastModifiedDate":"2016-11-07T10:05:18","indexId":"ofr78684","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-684","title":"Hydrologic environment of the Silurian salt deposits in parts of Michigan, Ohio, and New York","docAbstract":"The aggregate thickness of evaporites (salt, gypsum, and anhydrite) in the Silurian Salina sequence in Michigan exceeds 1200 feet in areas near the periphery of the Michigan basin, where the salt beds are less than 3000 feet below land surface. In northeast Ohio the aggregate thickness of salt beds is as much as 200 feet in places, and in western New York it is more than 500 feet, where th beds are less than 3000 feet deep.
The salt-bearing rocks dip regionally on the order of 50 feet per mile; those in Michigan dip toward the center of the Michigan basin, and those in Ohio and New York, in the Appalachian basin, dip generally southward. The rocks in both basins thicken downdip. Minor folds and faults occur in the salt-bearing rocks in all three states. Some of this defrmation has been attenuated or absorbed bo the salt beds.
Occuring near the middle of thick sedimentary sequences, the salt beds are bounded aboe and below by beds containing water having dissolved-solids concentrations several times that seawter. The brines occur commonly in discrete zones of high permeability at specific places in the stratigraphic sequence.
In northeast Ohio two prominent brine zones are recognized by the driller, the Devonian Oriskany Sandstone, or 'first water' zone, above the Salina Formation, and the Newburg or 'second water' zone below the Salina. In each aquifer there is a vertical component of hydraulic head, but little brine probably moves through the salt beds because their permeability is extremely low. Also, ther is little evidence of dissolution of the salt in areas distant from the outcrop, suggesting that if brine does move through the salt, movement is at a slow enough rate so that, in combination with the saturated or near-saturated condition of the water, it precludes significant dissolution. Principal brine movement is probably in the permeable zones in the direction of the hydraulic gradient.
Two areas in Michigan and one area each in Ohio and New York appear suitable for additional investigation of salt beds for purposes radioactive waste disposal. One of the Michigan areas is in the northern part of the southern peninsula, in Presque Isle and Alpena Counties; the other is in the southern part of the southern peninsula, in Oakland, Macomb, and St. Clair Counties (fig. 3). In northeast Ohio the area that appears to be suitable for investigation includes most of the eastern half of Lake County and extends eastward into Ashtabula County and southward into Geauga County. In western New York conditions may warrant additional investigation in Schuyler, Tompkins, and western Cortland Counties.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Columbus, OH","doi":"10.3133/ofr78684","issn":"0094-9140","usgsCitation":"Norris, S., 1978, Hydrologic environment of the Silurian salt deposits in parts of Michigan, Ohio, and New York: U.S. Geological Survey Open-File Report 78-684, iii, 31 p., https://doi.org/10.3133/ofr78684.","productDescription":"iii, 31 p.","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":157248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":330791,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0684/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606df8","contributors":{"authors":[{"text":"Norris, Stanley E.","contributorId":63844,"corporation":false,"usgs":true,"family":"Norris","given":"Stanley E.","affiliations":[],"preferred":false,"id":191271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27090,"text":"wri7849 - 1978 - Ten-year low mean monthly discharge determinations for ungaged streams near waste-stabilization ponds in Wisconsin","interactions":[],"lastModifiedDate":"2015-10-21T09:47:13","indexId":"wri7849","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"78-49","title":"Ten-year low mean monthly discharge determinations for ungaged streams near waste-stabilization ponds in Wisconsin","docAbstract":"Communities that use fill-and-draw waste-water treatment lagoons or waste-stabilization ponds are required to discharge during the spring and fall of the year at a rate that does not exceed the assimilative capacity of the receiving stream. The 10-year low mean monthly discharge (MMQ10) for October, November, April, and May for the receiving stream has been used to establish the discharge rate for the treatment systems at the appropriate time of the year. To determine the MMQ10 for the receiving stream the monthly mean discharge first was estimated by using a technique developed by Riggs (1969). Once the monthly mean discharge was determined the MMQ10 of the ungaged stream was estimated by using a graphical correlation between the monthly mean discharge and the MMQ10 of at least three gaging stations near the waste-stabilization pond.The MMQ10 for these gaging stations were determined by a log-Pearson Type III frequency analysis.
\nThe MMQ10 was determined for Maple Creek at Valmy, Aliens Creek near Oakdale, North Branch Manitowoc River at Sherwood, East Fork Poplar River near Curtiss, and Yellow River at Barronette.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7849","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Field, S.J., 1978, Ten-year low mean monthly discharge determinations for ungaged streams near waste-stabilization ponds in Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 78-49, iii, 16 p., https://doi.org/10.3133/wri7849.","productDescription":"iii, 16 p.","numberOfPages":"20","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":158651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0049/report-thumb.jpg"},{"id":55956,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68535b","contributors":{"authors":[{"text":"Field, Stephen J.","contributorId":53800,"corporation":false,"usgs":true,"family":"Field","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197536,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18369,"text":"ofr781019 - 1978 - An instrument system for long-term sediment transport studies on the continental shelf","interactions":[],"lastModifiedDate":"2024-02-09T20:05:45.390348","indexId":"ofr781019","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-1019","title":"An instrument system for long-term sediment transport studies on the continental shelf","docAbstract":"A bottom-mounted instrument system has been designed and built to monitor processes of bottom-sediment movement on the Continental Shelf. The system measures bottom current speed and direction, pressure, temperature, and light transmission, and photographs the bottom. The instrument operates in a burst sample mode. The system can be deployed for periods of 2-6 months to monitor intermittent processes of sediment movement such as storms, and to assess seasonal variability. Deployments of the system on the U.S. East Coast Continental Shelf show sediment resuspension and changes in bottom microtopography due to surface waves, tidal currents, and storms.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr781019","usgsCitation":"Butman, B., and Folger, D.W., 1978, An instrument system for long-term sediment transport studies on the continental shelf: U.S. Geological Survey Open-File Report 78-1019, 24 p., https://doi.org/10.3133/ofr781019.","productDescription":"24 p.","costCenters":[],"links":[{"id":425549,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1019/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151765,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1019/report-thumb.jpg"}],"country":"United States","otherGeospatial":"East Coast Continental Shelf","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68456c","contributors":{"authors":[{"text":"Butman, Bradford 0000-0002-4174-2073 bbutman@usgs.gov","orcid":"https://orcid.org/0000-0002-4174-2073","contributorId":943,"corporation":false,"usgs":true,"family":"Butman","given":"Bradford","email":"bbutman@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":178994,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Folger, David W.","contributorId":96663,"corporation":false,"usgs":true,"family":"Folger","given":"David","email":"","middleInitial":"W.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":178995,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":33288,"text":"b1440 - 1978 - A gravity study of the northern part of the Arctic National Wildlife Range, Alaska","interactions":[],"lastModifiedDate":"2016-12-20T14:25:32","indexId":"b1440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"1440","title":"A gravity study of the northern part of the Arctic National Wildlife Range, Alaska","docAbstract":"Interpretation of all publicly available onshore gravity data provides a basis for outlining regional elements of the basement and overlying structure in the northern part of the Arctic National Wildlife Range. Major post-Carboniferous sedimentary basins whose centers lie offshore on the Beaufort Shelf extend onshore in the northern part of the study area. There is strong evidence that dense basement rocks beneath these onshore extensions rise to relatively shallow depths along the northeast Alaskan coast. Geologic studies and interpretation of the gravity data indicate that the gross structural and stratigraphic framework of this area is similar to that of the Prudhoe Bay region to the west.
A high potential for petroleum accumulation in the Wildlife Range is indicated by the surface presence of oil seeps, oil sands, and outcrops of reservoir and source rocks along the southern margins of the onshore basinal areas. Present data suggest that the greatest potential for onshore accumulations of hydrocarbons lies in the area south and east of Barter Island and that possibilities exist there for commercially substantial reserves. The potential of this area cannot be fully assessed, however, until the subsurface extent of several major unconformities is known. Unfortunately, gravity data alone are of little use in such determinations.
South of the mountain front, large granitic intrusions are marked by a sharply defined gravity minimum. The subsurface distribution of these bodies could probably be mapped by detailed gravity surveys. Detailed aeromagnetic surveys should serve equally well for such a purpose.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b1440","usgsCitation":"Kososki, B.A., Reiser, H.N., Cavit, C.D., and Detterman, R.L., 1978, A gravity study of the northern part of the Arctic National Wildlife Range, Alaska: U.S. Geological Survey Bulletin 1440, Report: iii, 21 p.; 3 Plates: 46.50 x 22.00 inches or smaller, https://doi.org/10.3133/b1440.","productDescription":"Report: iii, 21 p.; 3 Plates: 46.50 x 22.00 inches or smaller","costCenters":[],"links":[{"id":331286,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":61070,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1440/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61071,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1440/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61072,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1440/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61073,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1440/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Arctic National Wildlife Range","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -147,\n 69\n ],\n [\n -147,\n 70.5\n ],\n [\n -141,\n 70.5\n ],\n [\n -141,\n 69\n ],\n [\n -147,\n 69\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae587","contributors":{"authors":[{"text":"Kososki, B. A.","contributorId":85182,"corporation":false,"usgs":true,"family":"Kososki","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":210362,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reiser, H. N.","contributorId":13199,"corporation":false,"usgs":true,"family":"Reiser","given":"H.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":210359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cavit, C. D.","contributorId":20370,"corporation":false,"usgs":true,"family":"Cavit","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":210360,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Detterman, R. L.","contributorId":71525,"corporation":false,"usgs":true,"family":"Detterman","given":"R.","middleInitial":"L.","affiliations":[],"preferred":false,"id":210361,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":28325,"text":"wri77114 - 1978 - Altitude and configuration of the top of the Floridan Aquifer, Duval County, Florida","interactions":[],"lastModifiedDate":"2019-08-05T11:01:40","indexId":"wri77114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-114","title":"Altitude and configuration of the top of the Floridan Aquifer, Duval County, Florida","docAbstract":"Structural contours on the top of the Floridan aquifer in Duval County, Florida, show that the top of the aquifer ranges from less than 300 feet below sea level to more than 600 feet below sea level. Two inferred concealed faults occur in the aquifer; one trending northeast-southwest in the eastern part of the county. The maximum vertical displacement of the top of the aquifer of both faults is about 150 feet. A geologic section included on the map shows the geologic formations of Eocene age that comprise the Floridan aquifer. These are, in ascending order: the Lake City Limestone, the Avon Park Limestone, and the Ocala Limestone. 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G.W.","contributorId":64294,"corporation":false,"usgs":true,"family":"Leve","given":"G.W.","affiliations":[],"preferred":false,"id":199596,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29698,"text":"wri7941 - 1978 - Water-table map of Racine County, Wisconsin","interactions":[],"lastModifiedDate":"2019-07-26T10:13:38","indexId":"wri7941","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-41","title":"Water-table map of Racine County, Wisconsin","docAbstract":"A map (scale 1:100,000) of the water table in Racine County in southeastern Wisconsin was prepared using water levels from more than 250 wells. The work was done as a cooperative project between the U.S. Geological Survey and the Southeastern Wisconsin Regional Planning Commission. The map shows the altitude of the water table in increments of 20 feet, with supplemental 10-foot contours. The altitude ranges from less than 520 feet at a point in a cone of depression in the eastern part of the county to more than 820 feet at two points, one along the border in the southwestern corner of the county and another in the northwestern corner. (Woodard-USGS)
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7941","usgsCitation":"Sherrill, M., and Schiller, J., 1978, Water-table map of Racine County, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 79-41, 1 Plate: 20.62 x 15.09 inches, https://doi.org/10.3133/wri7941.","productDescription":"1 Plate: 20.62 x 15.09 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":365975,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1979/0041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0041/report-thumb.jpgpg"}],"country":"United States","state":"Wisconsin","county":"Racine County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-87.8268,42.8446],[-87.8262,42.8423],[-87.822,42.8336],[-87.8135,42.8244],[-87.8043,42.8156],[-87.7946,42.8064],[-87.7884,42.8018],[-87.7798,42.7967],[-87.7687,42.792],[-87.762,42.7864],[-87.7589,42.7823],[-87.759,42.78],[-87.7647,42.7769],[-87.7737,42.768],[-87.7795,42.758],[-87.7797,42.7517],[-87.7817,42.7471],[-87.7789,42.7321],[-87.779,42.7285],[-87.7773,42.7239],[-87.7773,42.7212],[-87.7825,42.7126],[-87.7845,42.7072],[-87.7853,42.7017],[-87.7911,42.6941],[-87.7925,42.6895],[-87.7951,42.6828],[-87.8003,42.6728],[-87.801,42.671],[-87.8347,42.6715],[-87.9532,42.6711],[-88.0692,42.6715],[-88.187,42.6718],[-88.1862,42.6137],[-88.3027,42.6134],[-88.3044,42.8444],[-88.1868,42.8451],[-88.0699,42.8447],[-87.9524,42.8448],[-87.8355,42.8447],[-87.8268,42.8446]]]},\"properties\":{\"name\":\"Racine\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99f5","contributors":{"authors":[{"text":"Sherrill, M.G.","contributorId":19945,"corporation":false,"usgs":true,"family":"Sherrill","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":201970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schiller, J.J.","contributorId":46135,"corporation":false,"usgs":true,"family":"Schiller","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":201971,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36800,"text":"fwsobs78_81 - 1978 - Surface mining and fish/wildlife needs in the eastern United States: proceedings of a symposium","interactions":[],"lastModifiedDate":"2012-02-02T00:09:56","indexId":"fwsobs78_81","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"78/81","title":"Surface mining and fish/wildlife needs in the eastern United States: proceedings of a symposium","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Samuel, D.E., Stauffer, J.R., Hocutt, C.H., and Mason, W., 1978, Surface mining and fish/wildlife needs in the eastern United States: proceedings of a symposium: FWS/OBS 78/81, 386 p. : ill., maps; 27 cm. + addendum.","productDescription":"386 p. : ill., maps; 27 cm. + addendum","costCenters":[],"links":[{"id":165632,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698252","contributors":{"authors":[{"text":"Samuel, David E.","contributorId":100916,"corporation":false,"usgs":true,"family":"Samuel","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":216970,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stauffer, Jay R.","contributorId":51816,"corporation":false,"usgs":true,"family":"Stauffer","given":"Jay","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":216969,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hocutt, Charles H.","contributorId":41493,"corporation":false,"usgs":true,"family":"Hocutt","given":"Charles","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":216968,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mason, William T.","contributorId":27516,"corporation":false,"usgs":true,"family":"Mason","given":"William T.","affiliations":[],"preferred":false,"id":216967,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":36793,"text":"fwsobs78_95 - 1978 - Mined land reclamation for fish and wildlife in the eastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:09:56","indexId":"fwsobs78_95","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"78/95","title":"Mined land reclamation for fish and wildlife in the eastern United States","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"U.S. Fish and Wildlife Service, 1978, Mined land reclamation for fish and wildlife in the eastern United States: FWS/OBS 78/95, 12 p. : col. ill.; 27 cm.","productDescription":"12 p. : col. ill.; 27 cm.","costCenters":[],"links":[{"id":165626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6356cc","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529593,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3805,"text":"cir786 - 1978 - General geology, petroleum appraisal, and nature of environmental hazards, eastern Pacific shelf latitude 28° to 38° north","interactions":[],"lastModifiedDate":"2022-01-05T22:06:07.063122","indexId":"cir786","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"786","title":"General geology, petroleum appraisal, and nature of environmental hazards, eastern Pacific shelf latitude 28° to 38° north","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir786","usgsCitation":"Howell, D.G., McCulloch, D.S., and Vedder, J.G., 1978, General geology, petroleum appraisal, and nature of environmental hazards, eastern Pacific shelf latitude 28° to 38° north: U.S. Geological Survey Circular 786, iii, 29 p., https://doi.org/10.3133/cir786.","productDescription":"iii, 29 p.","costCenters":[],"links":[{"id":393941,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23576.htm"},{"id":30875,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0786/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1978/0786/report-thumb.jpg"}],"country":"Mexico, United States","otherGeospatial":"eastern Pacific shelf","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.617,\n 28\n ],\n [\n -120.15,\n 28\n ],\n [\n -120.15,\n 38\n ],\n [\n -123.617,\n 38\n ],\n [\n -123.617,\n 28\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b08e5","contributors":{"authors":[{"text":"Howell, D. G.","contributorId":52546,"corporation":false,"usgs":true,"family":"Howell","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":147636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCulloch, David S. dmccullo@usgs.gov","contributorId":3100,"corporation":false,"usgs":true,"family":"McCulloch","given":"David","email":"dmccullo@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":147635,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vedder, J. G.","contributorId":97873,"corporation":false,"usgs":true,"family":"Vedder","given":"J.","middleInitial":"G.","affiliations":[],"preferred":false,"id":147637,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8490,"text":"ofr781093 - 1978 - Postulated model of uranium occurrence in the central mining area, Marysvale District, west-central Utah","interactions":[{"subject":{"id":8490,"text":"ofr781093 - 1978 - Postulated model of uranium occurrence in the central mining area, Marysvale District, west-central Utah","indexId":"ofr781093","publicationYear":"1978","noYear":false,"title":"Postulated model of uranium occurrence in the central mining area, Marysvale District, west-central Utah"},"predicate":"SUPERSEDED_BY","object":{"id":64982,"text":"i1177 - 1979 - Uranium in the central mining area, Marysvale district, west central Utah","indexId":"i1177","publicationYear":"1979","noYear":false,"title":"Uranium in the central mining area, Marysvale district, west central Utah"},"id":1}],"supersededBy":{"id":64982,"text":"i1177 - 1979 - Uranium in the central mining area, Marysvale district, west central Utah","indexId":"i1177","publicationYear":"1979","noYear":false,"title":"Uranium in the central mining area, Marysvale district, west central Utah"},"lastModifiedDate":"2022-09-26T20:59:27.512346","indexId":"ofr781093","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-1093","title":"Postulated model of uranium occurrence in the central mining area, Marysvale District, west-central Utah","docAbstract":"Uranium in the central mining area of Marysvale, Utah occurs in hydrothermal veins cutting granitic and volcanic rocks in the eastern source area of the Mount Belknap Volcanics. A preliminary model for the origin of the veins envisages deposition in near-surface fractures above an unexposed pluton that may host a porphyry-type ore deposit. This model is based on the work in progress by the U.S. Geological Survey, and embodies all presently available data from field mapping, literature study, fluid inclusion studies, and diverse geochemical and isotopic studies. Recent advances in uranium geochemistry have been particularly helpful. The work is not yet complete so this model should be considered as a progress report suggesting possible targets for exploration and testing; such testing would in turn lead to refinements in the model and to a clearer understanding of vein-type uranium deposits in general.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr781093","usgsCitation":"Cunningham, C.G., and Steven, T.A., 1978, Postulated model of uranium occurrence in the central mining area, Marysvale District, west-central Utah: U.S. Geological Survey Open-File Report 78-1093, Report: i, 19 p.; 1 Plate: 15.17 x 19.18 inches, https://doi.org/10.3133/ofr781093.","productDescription":"Report: i, 19 p.; 1 Plate: 15.17 x 19.18 inches","costCenters":[],"links":[{"id":143642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1093/report-thumb.jpg"},{"id":407368,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/1093/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":407367,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1093/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Marysvale District","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,38.446 ], [ -112.25,38.522 ], [ -112.167,38.522 ], [ -112.167,38.446], [ -112.25,38.446 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6839e9","contributors":{"authors":[{"text":"Cunningham, Charles G.","contributorId":85940,"corporation":false,"usgs":true,"family":"Cunningham","given":"Charles","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":157808,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steven, Thomas August","contributorId":73174,"corporation":false,"usgs":true,"family":"Steven","given":"Thomas","email":"","middleInitial":"August","affiliations":[],"preferred":false,"id":157807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7734,"text":"ofr78928 - 1978 - Scour and fill in a stream channel, East Fork River, western Wyoming","interactions":[{"subject":{"id":7734,"text":"ofr78928 - 1978 - Scour and fill in a stream channel, East Fork River, western Wyoming","indexId":"ofr78928","publicationYear":"1978","noYear":false,"title":"Scour and fill in a stream channel, East Fork River, western Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":5674,"text":"pp1117 - 1979 - Scour and fill in a stream channel, East Fork River, western Wyoming","indexId":"pp1117","publicationYear":"1979","noYear":false,"title":"Scour and fill in a stream channel, East Fork River, western Wyoming"},"id":1}],"supersededBy":{"id":5674,"text":"pp1117 - 1979 - Scour and fill in a stream channel, East Fork River, western Wyoming","indexId":"pp1117","publicationYear":"1979","noYear":false,"title":"Scour and fill in a stream channel, East Fork River, western Wyoming"},"lastModifiedDate":"2019-08-29T13:03:08","indexId":"ofr78928","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-928","title":"Scour and fill in a stream channel, East Fork River, western Wyoming","docAbstract":"Frequent soundings of 11 cross sections located on the East Fork River, western Wyoming, during a spring flood revealed two sequences of channel scour and fill. All sections either scoured or filled at the flood crests relative to their low-flow condition. The sections which scoured at high flow (called scouring sections) generally tended to fill at low flow. Conversely, the sections which filled at high flow (called filling sections) generally tended to scour at low flow. The critical discharge at which the character of a section changed from scouring to filling or vice versa was approximately the bankfull discharge. Therefore, at any discharge except bankfull, some sections were accumulating bed material (fill), while others were being depleted of bed material (scour). (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr78928","usgsCitation":"Andrews, E.D., 1978, Scour and fill in a stream channel, East Fork River, western Wyoming: U.S. Geological Survey Open-File Report 78-928, iv, 73 p. , https://doi.org/10.3133/ofr78928.","productDescription":"iv, 73 p. ","costCenters":[],"links":[{"id":367100,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0928/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0928/report-thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"East Fork River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.49335098266602,\n 42.66640693046163\n ],\n [\n -109.3860626220703,\n 42.66640693046163\n ],\n [\n -109.3860626220703,\n 42.679785307071114\n ],\n [\n -109.49335098266602,\n 42.679785307071114\n ],\n [\n -109.49335098266602,\n 42.66640693046163\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6976c2","contributors":{"authors":[{"text":"Andrews, Edmund D. eandrews@usgs.gov","contributorId":3828,"corporation":false,"usgs":true,"family":"Andrews","given":"Edmund","email":"eandrews@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":156510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10814,"text":"ofr78272 - 1978 - Drilling during 1977 in the Danforth Hills coal field, Easton Gulch and Devils Hole Gulch quadrangles, Moffat County, Colorado","interactions":[],"lastModifiedDate":"2022-02-23T23:01:12.95253","indexId":"ofr78272","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-272","title":"Drilling during 1977 in the Danforth Hills coal field, Easton Gulch and Devils Hole Gulch quadrangles, Moffat County, Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78272","usgsCitation":"Reheis, M.J., 1978, Drilling during 1977 in the Danforth Hills coal field, Easton Gulch and Devils Hole Gulch quadrangles, Moffat County, Colorado: U.S. Geological Survey Open-File Report 78-272, Report: i, 29 p.; 1 Plate: 28.00 × 50.00 inches, https://doi.org/10.3133/ofr78272.","productDescription":"Report: i, 29 p.; 1 Plate: 28.00 × 50.00 inches","costCenters":[],"links":[{"id":396412,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14663.htm"},{"id":38611,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0272/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0272/report-thumb.jpg"},{"id":94994,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0272/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Moffat County","otherGeospatial":"Easton Gulch and Devils Hole Gulch quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.883,\n 40.227\n ],\n [\n -108,\n 40.227\n ],\n [\n -108,\n 40.325\n ],\n [\n -107.883,\n 40.325\n ],\n [\n -107.883,\n 40.227\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633d98","contributors":{"authors":[{"text":"Reheis, Marith J. 0000-0002-8359-323X","orcid":"https://orcid.org/0000-0002-8359-323X","contributorId":9657,"corporation":false,"usgs":true,"family":"Reheis","given":"Marith","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":162014,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":58370,"text":"mf880E - 1978 - Geochemical map showing the distribution and abundance of copper in stream sediments in the Seward and Blying Sound quadrangles, Alaska","interactions":[],"lastModifiedDate":"2023-05-23T20:58:22.987417","indexId":"mf880E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"880","chapter":"E","title":"Geochemical map showing the distribution and abundance of copper in stream sediments in the Seward and Blying Sound quadrangles, Alaska","docAbstract":"Reconnaissance geochemical and mineralogical sampling was done in the Seward and Blying Sound quadrangles during 1975 and 1976 as part of the Alaska Mineral Resources Assessment Program (AMRAP). This map shows the distribution and abundance of copper in stream-sediment samples.
Stream-sediment samples were collected at 569 sites from active stream channels and locally, from the interface of streambeds with intermediate- to low-tide beaches. Most of the stream sediment is fine- to coarse-grained sand, with a clay-silt fraction in streams discharging from glaciers.
The stream sediment samples were air dried and sieved through a 80-mesh (0.2 mm) sieve, and the minus-80 mesh fraction was saved for analysis. A split of each sample was analyzed for copper and 15 other elements by a semiquantitative spectrographic method (Grimes and Marranzino, 1968). Other splits were analyzed for gold and zinc by atomic absorption methods (Warren and others, 1969).
Sample sites and copper values (in parts per million) are indicated on the map by symbols identified in the histogram. The weakly anomalous values are considered to be significant only where they were detected in stream-sediment or heavy-mineral concentrate samples that also contained strongly anomalous values of other metals such as arsenic, gold, lead or tungsten.
The map shows two populations for copper in stream sediments. One population consisting of generally lower copper values represents the samples collected from the sedimentary terrane in the central and western parts of the quadrangles. The other population consisting of generally higher copper values includes samples collected in areas of sheeted basalt dikes and pillow basalts in the eastern part of the quadrangles and from the sedimentary terrane of Latouche Island; in these areas chalcopyrite and pyrite were observed as fine-grained disseminations in the rocks and as mineral particles in the heavy-mineral concentrates.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf880E","isbn":"0607803495","usgsCitation":"Tripp, R.B., Crim, W., Cooley, E., and Day, G., 1978, Geochemical map showing the distribution and abundance of copper in stream sediments in the Seward and Blying Sound quadrangles, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 880, 1 Plate: 40.54 x 34.52 inches, https://doi.org/10.3133/mf880E.","productDescription":"1 Plate: 40.54 x 34.52 inches","costCenters":[],"links":[{"id":417367,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0880-E/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182959,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0880-E/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Blying Sound Quadrangle, Seward Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150,59.5 ], [ -150,61 ], [ -147,61 ], [ -147,59.5 ], [ -150,59.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae0d8","contributors":{"authors":[{"text":"Tripp, R. B.","contributorId":88707,"corporation":false,"usgs":true,"family":"Tripp","given":"R.","middleInitial":"B.","affiliations":[],"preferred":false,"id":258919,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crim, W.D.","contributorId":8820,"corporation":false,"usgs":true,"family":"Crim","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":258916,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cooley, E.F.","contributorId":83072,"corporation":false,"usgs":true,"family":"Cooley","given":"E.F.","email":"","affiliations":[],"preferred":false,"id":258918,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":258917,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":11763,"text":"ofr78132 - 1978 - An oilspill risk analysis for the eastern Gulf of Mexico (proposed sale 65) Outer Continental Shelf lease area","interactions":[],"lastModifiedDate":"2014-03-25T08:18:35","indexId":"ofr78132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-132","title":"An oilspill risk analysis for the eastern Gulf of Mexico (proposed sale 65) Outer Continental Shelf lease area","docAbstract":"An oilspill risk analysis was conducted to determine the relative environmental hazards of developing oil in different regions of the Eastern Gulf of Mexico Outer Continental Shelf lease area. The study analyzed the probability of spill occurrence, likely paths of the spills, and locations in space and time of such objects as recreational and biological resources likely to be vulnerable. These results combined to yield estimates of the overall oilspill risk associated with development of the proposed lease area. This risk is compared to the existing oilspill risk from existing leases in the area. The analysis implicitly includes estimates of weathering rates and slick dispersion and an indication of the possible mitigating effects of cleanups.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78132","usgsCitation":"Wyant, T., and Slack, J.R., 1978, An oilspill risk analysis for the eastern Gulf of Mexico (proposed sale 65) Outer Continental Shelf lease area: U.S. Geological Survey Open-File Report 78-132, ix, 72 p., https://doi.org/10.3133/ofr78132.","productDescription":"ix, 72 p.","numberOfPages":"83","costCenters":[],"links":[{"id":144454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr78132.jpg"},{"id":284487,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0132/report.pdf"}],"country":"United States","otherGeospatial":"Gulf Of Mexcio","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89.93,22.82 ], [ -89.93,30.73 ], [ -77.65,30.73 ], [ -77.65,22.82 ], [ -89.93,22.82 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4ca5e4b0b290850f11b8","contributors":{"authors":[{"text":"Wyant, Timothy","contributorId":26672,"corporation":false,"usgs":true,"family":"Wyant","given":"Timothy","email":"","affiliations":[],"preferred":false,"id":163693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slack, James R.","contributorId":43778,"corporation":false,"usgs":true,"family":"Slack","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":163694,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27813,"text":"wri77124 - 1978 - Appraisal of shallow ground-water resources and management alternatives in the Upper Peace and Eastern Alafia River Basins, Florida","interactions":[],"lastModifiedDate":"2019-08-05T10:02:38","indexId":"wri77124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"77-124","title":"Appraisal of shallow ground-water resources and management alternatives in the Upper Peace and Eastern Alafia River Basins, Florida","docAbstract":"In southwest Florida, the shallow aquifer system underlying the 1,250-square-mile upper Peace and eastern Alafia River basins is a relatively untapped source of supply. The aquifer system ranges between 50 and 300 feet thick and is composed of a surficial sand unit underlain by a limestone unit. Sand and clay confining beds separate the shallow aquifer system from the highly productive, extensively developed deep aquifer system. The hydrologic budget of the area indicates that annual leakage of water from the shallow to the deep aquifer system is 2.6 inches while annual pumpage from the deep aquifer system averages 5.5 inches. Management alternatives to be considered for efficient use of the shallow ground-water resources include development by withdrawal wells or connector wells for recharge. One solution for a gridded network of wells consists of 540 wells spaced 7,000 feet apart, each producing 453 gallons per minute. The network would derive water to meet demand by capturing water that would normally have run off evapotranspired. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri77124","usgsCitation":"Hutchinson, C.B., 1978, Appraisal of shallow ground-water resources and management alternatives in the Upper Peace and Eastern Alafia River Basins, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-124, v, 57 p., https://doi.org/10.3133/wri77124.","productDescription":"v, 57 p.","costCenters":[],"links":[{"id":366187,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0124/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0124/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Alafia River, Peace 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