{"pageNumber":"1713","pageRowStart":"42800","pageSize":"25","recordCount":46619,"records":[{"id":28868,"text":"wri78133 - 1978 - Sediment transport by the White River into Mud Mountain Reservoir: Washington, June 1974-June 1976","interactions":[],"lastModifiedDate":"2015-11-16T11:27:04","indexId":"wri78133","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":"78-133","title":"Sediment transport by the White River into Mud Mountain Reservoir: Washington, June 1974-June 1976","docAbstract":"<p>This reconnaissance evaluation of the sediment transport by the White River into the Mud Mountain Reservoir, in Washington, during the period June 1974-June 1976 showed that the river transported 430,000 tons of suspended sediment into the reservoir during the first year of the study and 1,400,000 tons in the second year. Daily mean suspended-sediment concentrations generally were less than 500 milligrams per liter; the highest daily mean concentration was 6,200 milligrams per liter on December 1, 1975. A good relation exists between daily suspended-sediment discharge and daily mean water discharge except during periods of runoff from glacial melt. Data from samples obtained by the use of the Helley-Smith bedload sampler indicate that the bedload measured using the sampler is about 4 percent of the suspended-sediment discharge. Potential deposition in the reservoir was estimated at 750 acre-feet during the 2 years of study. (Kosco-USGS)</p>","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Tacoma, Washington","doi":"10.3133/wri78133","collaboration":"Prepared in cooperation with U .S . Army Corps of Engineers, Seattle District","usgsCitation":"Nelson, L.M., 1978, Sediment transport by the White River into Mud Mountain Reservoir: Washington, June 1974-June 1976: U.S. Geological Survey Water-Resources Investigations Report 78-133, iv, 26 p., https://doi.org/10.3133/wri78133.","productDescription":"iv, 26 p.","numberOfPages":"32","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":159631,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri78133.PNG"},{"id":311343,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0133/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","city":"Buckley","otherGeospatial":"White River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.93553924560548,\n              47.13345427321226\n            ],\n            [\n              -121.93553924560548,\n              47.163808415712985\n            ],\n            [\n              -121.8170928955078,\n              47.163808415712985\n            ],\n            [\n              -121.8170928955078,\n              47.13345427321226\n            ],\n            [\n              -121.93553924560548,\n              47.13345427321226\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbf0b","contributors":{"authors":[{"text":"Nelson, Leonard M.","contributorId":96695,"corporation":false,"usgs":true,"family":"Nelson","given":"Leonard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":200529,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26989,"text":"wri78121 - 1978 - The biology of Salt Wells Creek and its tributaries, southwestern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:39","indexId":"wri78121","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":"78-121","title":"The biology of Salt Wells Creek and its tributaries, southwestern Wyoming","docAbstract":"A description of aquatic organisms and biological communities is presented for Salt Wells Creek, a plains stream in the Green River basin. The description includes seasonal population fluctuations of benthic organisms and algae, the food pyramid, and nutrient relations between various types of plants and animals. The algae and stream invertebrates were studied to determine baseline data and biological indicators of water quality. (Woodard-USGS).","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri78121","usgsCitation":"Engelke, M.J., 1978, The biology of Salt Wells Creek and its tributaries, southwestern Wyoming: U.S. Geological Survey Water-Resources Investigations Report 78-121, xiv, 82 p. :ill., maps ;27 cm., https://doi.org/10.3133/wri78121.","productDescription":"xiv, 82 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":158836,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0121/report-thumb.jpg"},{"id":55875,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0121/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684bdc","contributors":{"authors":[{"text":"Engelke, Morris J. Jr.","contributorId":100379,"corporation":false,"usgs":true,"family":"Engelke","given":"Morris","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197365,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48359,"text":"ofr78300G - 1978 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: July 1978","interactions":[],"lastModifiedDate":"2024-04-22T17:31:43.542505","indexId":"ofr78300G","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":"78-300","chapter":"G","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: July 1978","docAbstract":"<p><span>The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78300G","usgsCitation":"Townshend, J., Papp, J., and Tilton, S., 1978, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: July 1978: U.S. Geological Survey Open-File Report 78-300, 22 p., https://doi.org/10.3133/ofr78300G.","productDescription":"22 p.","costCenters":[],"links":[{"id":427991,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0300-g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161689,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0300-g/report-thumb.jpg"}],"country":"United States","state":"Alask","city":"Fairbanks","otherGeospatial":"College Observatory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -147.9716829972995,\n              64.92275521538983\n            ],\n            [\n              -147.9716829972995,\n              64.77266196148724\n            ],\n            [\n              -147.4142995458633,\n              64.77266196148724\n            ],\n            [\n              -147.4142995458633,\n              64.92275521538983\n            ],\n            [\n              -147.9716829972995,\n              64.92275521538983\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673754","contributors":{"authors":[{"text":"Townshend, J.B.","contributorId":30623,"corporation":false,"usgs":true,"family":"Townshend","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":237300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Papp, J.E.","contributorId":95057,"corporation":false,"usgs":true,"family":"Papp","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":237301,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tilton, S.P.","contributorId":15670,"corporation":false,"usgs":true,"family":"Tilton","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":237299,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38628,"text":"pp1017 - 1978 - Ore deposits of the Gilman District, Eagle County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:10:36","indexId":"pp1017","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"1017","title":"Ore deposits of the Gilman District, Eagle County, Colorado","docAbstract":"The Gilman mining district, known also in the past as the Red Cliff district, is in the mountains of southeastern Eagle County, west-central Colorado. The district is the leading source of zinc in Colorado and one of the major base-metal mining districts in the State. As valued at the time of production, total output of zinc, silver, copper, lead, and gold through 1972 was about $328 million. About 90 percent of this total was produced after 1930. \r\n\r\nThe productive part of the district is an area of about 3 square miles (7.8 square kilometers) on the northeast side of the deep canyon of the Eagle River between the small towns of Gilman and Red Cliff. The ore deposits are principally replacement deposits in dolomites of Mississippian and Devonian age and in quartzite of Cambrian age. A few productive veins occur in Precambrian rocks. The replacement deposits crop out in the cliffs of the canyon wall and extend northeastward downdip beneath Battle Mountain, which is composed of a thick sequence of Pennsylvanian clastic rocks. The deposits were originally worked through several separate mines along the canyon wall, but since 1918, all deposits in dolomite rocks, except some small ones near Red Cliff, have been worked through the Eagle mine of the New Jersey Zinc Company at Gilman. \r\n\r\nThe Gilman district lies on the eastern flank of the huge anticline of the Sawatch Range, near the steeply plunging north end of the anticline. Sedimentary rocks on the flank of this part of the anticline dip homoclinally northeastward to a synclinal axis about 8 mi (miles) (13 km (kilometers> northeast of Gilman and then rise more steeply to the Gore fault at the edge of the Gore Range. The homocline is broken by only a few faults most of which have displacements of less than 100 ft (feet) (30 m (meters>. In contrast, the underlying Precambrian rocks are broken by numerous faults and shear zones related to the Homestake shear zone, a northeast-trending master shear zone several miles wide. Fractures and shear zones along the northwest side of the master zone extend beneath the Gilman district. \r\n\r\nThe Gilman district is at the northwestern edge of the northeast-trending Colorado mineral belt as defined by mineralized areas and bodies of intrusive porphyries. Neighboring mining districts in the mineral belt to the southeast of Gilman are the Kokomo lead-zinc district, 13 mi (21 km) distant; the Climax molybdenum district, 16 mi (26 km) distant; and the Leadville district, 20 mi (32 km) distant. These districts, as well as others farther away, are characterized by abundant intrusive rocks of Laramide and middle Tertiary ages and by complex faults systems. The Gilman district, in contrast, contains only a single sill of porphyry and has very simple geologic structure. This probably reflects a position either at the side of or high above a batholith that is inferred from geologic and geophysical data to underlie the mineral belt at shallow depth. \r\n\r\nThe rock column preserved in the district consists, in succession downward, of (1) grit, conglomerate, sandstone, and shale of the Pennsylvanian Minturn Formation, as much as 6,300 ft (1,920 m) thick; (2) shale, limestone, and. sandstone of the Pennsylvanian Belden Formation, 200 ft (61 m) thick; (3) a sill of quartz latite porphyry of the Cretaceous Pando Porphyry about 80 ft (24 m) thick intruded in the basal shale of the Belden Formation; (4) dolomitized limestone of the Mississippian Leadville Dolomite, 110-140 ft (34-43 m) thick; (5) sandstone and sandy and cherty dolomite of the Mississippian or Devonian Gilman Sandstone, 15-50 ft (4.5-15 m) thick; (6) thin-bedded primary or diagenetic dolomite of the Mississippian(?) and Devonian Dyer Dolomite, 50-80 ft (15-24 m) thick; (7) quartzite, conglomerate, and green shale of the Devonian Parting Formation, 35-50 ft (11-15 m) thick; (8) sandstone and shale of the Ordovician Harding Sandstone, 14-80 ft (4.2-24 m) thick; (9) shaly and sandy dolomite and dolom","language":"ENGLISH","doi":"10.3133/pp1017","usgsCitation":"Lovering, T.S., Tweto, O., and Lovering, T., 1978, Ore deposits of the Gilman District, Eagle County, Colorado: U.S. Geological Survey Professional Paper 1017, 90 p., https://doi.org/10.3133/pp1017.","productDescription":"90 p.","costCenters":[],"links":[{"id":120496,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1017/report-thumb.jpg"},{"id":65451,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1017/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1017/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdec4","contributors":{"authors":[{"text":"Lovering, T. S.","contributorId":108085,"corporation":false,"usgs":true,"family":"Lovering","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":220188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tweto, Ogden","contributorId":52939,"corporation":false,"usgs":true,"family":"Tweto","given":"Ogden","affiliations":[],"preferred":false,"id":220186,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lovering, T.G.","contributorId":55014,"corporation":false,"usgs":true,"family":"Lovering","given":"T.G.","affiliations":[],"preferred":false,"id":220187,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38699,"text":"pp813L - 1978 - Summary appraisals of the nation's ground-water resources – Tennessee region","interactions":[{"subject":{"id":49320,"text":"ofr77609 - 1977 - Summary appraisals of the Nation's ground-water resources; Tennessee region, including part of Tennessee and adjacent areas","indexId":"ofr77609","publicationYear":"1977","noYear":false,"title":"Summary appraisals of the Nation's ground-water resources; Tennessee region, including part of Tennessee and adjacent areas"},"predicate":"SUPERSEDED_BY","object":{"id":38699,"text":"pp813L - 1978 - Summary appraisals of the nation's ground-water resources – Tennessee region","indexId":"pp813L","publicationYear":"1978","noYear":false,"chapter":"L","title":"Summary appraisals of the nation's ground-water resources – Tennessee region"},"id":1}],"lastModifiedDate":"2021-12-14T22:10:25.510843","indexId":"pp813L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"813","chapter":"L","title":"Summary appraisals of the nation's ground-water resources – Tennessee region","docAbstract":"<p>Ground water is an abundant and little-used resource in the Tennessee Region, a 41,000 square mile area dominated by the Tennessee River system and including parts of Alabama, Georgia, Kentucky, Mississippi, North Carolina, Tennessee, and Virginia. One-fifth to one-fourth of the precipitation that falls on the region enters the ground-water reservoirs. During the year approximately the same amount of water leaves the ground-water system, sustaining the dry-weather flow of streams. Recharge for the region is about 22,000 million gallons per day or 0.5 million gallons per day per square mile. The major types of aquifers in the region are unconsolidated material (including sand and regolith), carbonate rocks, and fractured noncarbonate rocks. One or more of these aquifer types occurs in each of the six physiographic subdivisions of the region. The productivity of these aquifers depends on their hydraulic properties and on the distribution of these properties. The unconsolidated sand aquifers are the most homogeneous in composition and most predictable in occurrence. These aquifers commonly yield 200 to 600 gallons per minute per well depending on the thickness of sand penetrated.</p>\n<p>The most difficult aquifers to predict in regard to depth and yield are the carbonate rocks. In these aquifers it is possible to drill dry holes within a few hundred feet of wells capable of producing several thousand gallons per minute. However, with an adequate reconnaissance study to determine the occurrence of ground water and a planned test drilling program, yields of up to 300 gallons per minute per well can be expected in the carbonate aquifers. Potential yields from the fractured noncarbonate aquifers are lower than in the carbonate rocks.</p>\n<p>The chemical and physical properties of ground water in the Tennessee Region are usually within the limits recommended by the Environmental Protection Agency for drinking water, and the ground water in all but some very shallow aquifers tends to be free of pathogenic microorganisms. Saline water is not known to occur in significant quantities in the region.</p>\n<p>In 1970, 173 million gallons per day of ground water were used in the Tennessee Region. This was less than 8 percent of the total quantity of water used in the region and only 0.8 percent of the estimated ground-water recharge. Ground water is used chiefly as a source of water supply for rural areas and small towns. A lesser amount is used by industries and commercial establishments located beyond the limits of municipal water-supply systems. However, there is potential for significantly increased use in order to augment surface-water supplies and to utilize the total water resource more efficiently.</p>\n<p>Hydrologic studies and adequate test drilling would greatly increase the chances of locating large amounts of ground water, especially in the nine-tenths of the Tennessee Region that is underlain by either carbonate rocks or fractured noncarbonate rocks which have highly variable water-bearing properties. Collectively, such studies are useful in developing a concept of the hydrologic system which would permit the development of criteria for selecting well sites in other areas with a similar geological and hydrological setting. Hydrologic studies that include test drilling have been conducted in all parts of the region except the Cumberland Plateau.</p>\n<p>Some of the basic data necessary for hydrologic studies, such as geologic maps, well records, and streamflow records are available throughout the region. However, detailed information on groundwater levels, ground-water quality, and aquifer characteristics are not equally available throughout the region. This type of information cannot be obtained quickly when it is needed; it must be the product of a continuing program of studies designed to evaluate the Tennessee Region's ground-water resource.</p>\n<p>Because of the interdependence of ground water and surface water, water management efforts can be fully effective only if they involve the whole water resource. In the Tennessee Region, surface water is highly controlled, but there is at present no regionwide water-resources management plan that includes ground water.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813L","usgsCitation":"Zurawski, A., 1978, Summary appraisals of the nation's ground-water resources – Tennessee region: U.S. Geological Survey Professional Paper 813, iv., 35 p., https://doi.org/10.3133/pp813L.","productDescription":"iv., 35 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":392908,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5067.htm"},{"id":65553,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813l/report.pdf","text":"Report","size":"5.82 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,{"id":38701,"text":"pp813P - 1978 - Summary appraisals of the Nation's ground-water resources; Alaska","interactions":[],"lastModifiedDate":"2016-01-11T18:44:45","indexId":"pp813P","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"813","chapter":"P","title":"Summary appraisals of the Nation's ground-water resources; Alaska","docAbstract":"<p>Alaska has enormous surface-water resources, but many of the streams are frozen for most of the year and most contain glacial silt that makes them unacceptable for human use. These factors lend special significance to ground water as a water-supply source, even though perennially frozen ground (permafrost) profoundly modifies ground-water flow systems in much of Alaska north of the maritime southern coast and southeastern panhandle areas. Frozen ground is a virtually impermeable layer that restricts recharge, discharge, and movement of ground water, acts as a confining layer and limits the volume of unconsolidated deposits and bedrock in which water may be stored.</p>\n<p>Ground water is an untested resource in most of Alaska, but in many areas potential development of ground water far exceeds current use. Alluvium of major river valleys, such as the Yukon, Tanana, Kuskokwim and Susitna Rivers, probably contains the most extensive aquifers in the State. Large amounts of ground water are also stored in glacial outwash aquifers that underlie coastal basins and valleys, such as those at Kenai and Anchorage in the Cook Inlet lowland. Individual wells yielding more than 1,000 gallons per minute have been developed in the Tanana River valley, Cook Inlet lowland, and the coastal valleys at Seward and Juneau. Comparable yields should be possible in other areas that have similar geohydrologic environments. No major aquifers have been identified in glacial and glaciolacustrine deposits of interior valleys or in deltaic deposits. Major bedrock aquifers have been identified only in carbonate rocks of the Brooks Range and on the north side of the Alaska Range. Springs issuing from the carbonate rocks of the Brooks Range have discharges as great as 16,000 gallons per minute.</p>\n<p>Most ground-water recharge occurs beneath reaches of stream channels that are losing flow to the ground-water system. Most ground-water discharge also takes place along reaches of stream channels. This discharge augments streamflows during summer and maintains low flows during winter when there is no surface-water runoff. On the basis of a streamflow hydrograph separation technique and using the 60 percent flow-duration value as an indicator of ground-water discharge, it is estimated that 25 percent of the total volume of streamflow in Alaska (exclusive of coastal, maritime environments) is contributed by ground-water discharge.</p>\n<p>The thawing of frozen ground in the permafrost regions of Alaska causes construction and engineering problems. Disturbance of the ground surface disrupts the natural thermal equilibrium and tends to thaw part of the permafrost. Thawing can cause loss of strength, a decrease in volume, and an increase in erosion potential, particularly if the frozen ground is fine grained and poorly drained.</p>\n<p>Present deficiencies in the ground-water information base are obvious limiting factors to ground-water development in Alaska. There is a need to extend the ground-water data-collection network and to pursue special research into the quantitative aspects of ground-water hydrology in cold regions, particularly the continuous permafrost zone.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813P","usgsCitation":"Zenone, C., and Anderson, G.S., 1978, Summary appraisals of the Nation's ground-water resources; Alaska: U.S. Geological Survey Professional Paper 813, vi., 28 p., https://doi.org/10.3133/pp813P.","productDescription":"vi., 28 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":119943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813p/report-thumb.jpg"},{"id":65555,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813p/report.pdf","text":"Report","size":"8.84 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,{"id":38702,"text":"pp813Q - 1978 - Summary appraisals of the nation's ground-water resources – Missouri basin region","interactions":[],"lastModifiedDate":"2021-12-14T21:56:38.395429","indexId":"pp813Q","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"813","chapter":"Q","title":"Summary appraisals of the nation's ground-water resources – Missouri basin region","docAbstract":"<p>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.</p>\n<p>Unconsolidated 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.&nbsp;Unconsolidated and semiconsolidated aquifers have potential for conjunctive use with surface water, recycling to reuse available supplies, artificial recharge, and salvage of evapotranspired water.</p>\n<p>Sandstone 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.&nbsp;Sandstone aquifers have potential for artificial recharge, induced interaquifer leakage, conjunctive use with surface water, and mining of ground water.</p>\n<p>Limestone 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.&nbsp;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.</p>\n<p>Saline 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.</p>\n<p>Comprehensive 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.</p>","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 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,{"id":32604,"text":"pp1099B - 1978 - Land use and land cover information and air-quality planning","interactions":[],"lastModifiedDate":"2012-02-02T00:09:19","indexId":"pp1099B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"1099","chapter":"B","title":"Land use and land cover information and air-quality planning","docAbstract":"The land use and land cover information developed by the U.S. Geological Survey in the Central Atlantic Regional Ecological Test Site project has been proven useful when used in an improved technique for estimating emissions, diffusion, and impact patterns of sulfur dioxide (S02) and particulate matter. \r\n\r\nImplementation of plans to control air quality requires land use and land cover information, which, until this time, has been inadequate. The land use and land cover data were used in updating information on the sources of point and area emissions of S02 and particulate matter affecting the Norfolk-Portsmouth area of Virginia for the 1971-72 winter (Dec.-Jan.-Feb.) and the annual 1972 period, and for a future annual period-1985. This emission information is used as input to the Air Quality Display Model of the Environmental Protection Agency to obtain diffusion and impact patterns for the three periods previously mentioned. The results are: (1) During the 1971-72 winter, estimated S02 amounts over an area with southwest-northeast axis in the central section of Norfolk exceeded both primary and secondary levels, (2) future annual levels of S02, estimated by anticipated residential development and point-source changes, are not expected to cause serious deterioration of the region's present air quality, and (3) for the 1971-72 winter, and annual 1972, period the diffusion results showed that both primary and secondary standards for particulate matter are regularly exceeded in central Norfolk and Portsmouth. In addition, on the basis of current control programs, the 1985 levels of particulate matter are expected to exceed the presently established secondary air-quality standards through central Norfolk and Portsmouth and in certain areas of Virginia Beach. \r\n\r\nLand use and land cover information can be used to estimate emissions for inputs to diffusion models and to interpret the implications of diffusion patterns for: (1) Implementing various control strategies, (2) selecting sites of air sampling stations, and (3) predicting the effects that proposed changes in land use and land cover might have on emission patterns and air quality.","language":"ENGLISH","doi":"10.3133/pp1099B","usgsCitation":"Reed, W., and Lewis, J., 1978, Land use and land cover information and air-quality planning: U.S. Geological Survey Professional Paper 1099, p. B1-B43, https://doi.org/10.3133/pp1099B.","productDescription":"p. B1-B43","costCenters":[],"links":[{"id":125035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1099b/report-thumb.jpg"},{"id":60461,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1099b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae055","contributors":{"authors":[{"text":"Reed, W.E.","contributorId":79935,"corporation":false,"usgs":true,"family":"Reed","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":208770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, J.E.","contributorId":37388,"corporation":false,"usgs":true,"family":"Lewis","given":"J.E.","affiliations":[],"preferred":false,"id":208769,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40762,"text":"ofr78361 - 1978 - Deep drilling data, Raft River Geothermal Area, Idaho; Standard American Oil Co., Malta, Naf, and Strevell Petroleum test boreholes","interactions":[],"lastModifiedDate":"2012-02-02T00:10:54","indexId":"ofr78361","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":"78-361","title":"Deep drilling data, Raft River Geothermal Area, Idaho; Standard American Oil Co., Malta, Naf, and Strevell Petroleum test boreholes","language":"ENGLISH","doi":"10.3133/ofr78361","usgsCitation":"Oriel, S.S., Williams, P.L., Covington, H., Keys, H., Scott, W., and Shaver, K., 1978, Deep drilling data, Raft River Geothermal Area, Idaho; Standard American Oil Co., Malta, Naf, and Strevell Petroleum test boreholes: U.S. Geological Survey Open-File Report 78-361, 2 maps., https://doi.org/10.3133/ofr78361.","productDescription":"2 maps.","costCenters":[],"links":[{"id":170821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98251,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0361/plate-1_a.pdf","size":"4208","linkFileType":{"id":1,"text":"pdf"}},{"id":98252,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0361/plate-1_b.pdf","size":"4084","linkFileType":{"id":1,"text":"pdf"}},{"id":98253,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0361/plate-2.pdf","size":"3674","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db6725b6","contributors":{"authors":[{"text":"Oriel, Steven S.","contributorId":108079,"corporation":false,"usgs":true,"family":"Oriel","given":"Steven","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":223903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, P. L.","contributorId":79109,"corporation":false,"usgs":true,"family":"Williams","given":"P.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":223900,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Covington, H. R.","contributorId":92671,"corporation":false,"usgs":true,"family":"Covington","given":"H. R.","affiliations":[],"preferred":false,"id":223902,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Keys, H.R.","contributorId":36615,"corporation":false,"usgs":true,"family":"Keys","given":"H.R.","email":"","affiliations":[],"preferred":false,"id":223899,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Scott, W.","contributorId":29498,"corporation":false,"usgs":true,"family":"Scott","given":"W.","affiliations":[],"preferred":false,"id":223898,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Shaver, K.C.","contributorId":90370,"corporation":false,"usgs":true,"family":"Shaver","given":"K.C.","email":"","affiliations":[],"preferred":false,"id":223901,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":41082,"text":"ofr78220 - 1978 - Preliminary bedrock, surficial, and structural data maps of the Southbridge Quadrangle, Massachusetts and Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:10:51","indexId":"ofr78220","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":"78-220","title":"Preliminary bedrock, surficial, and structural data maps of the Southbridge Quadrangle, Massachusetts and Connecticut","language":"ENGLISH","doi":"10.3133/ofr78220","usgsCitation":"Moore, G.E., 1978, Preliminary bedrock, surficial, and structural data maps of the Southbridge Quadrangle, Massachusetts and Connecticut: U.S. Geological Survey Open-File Report 78-220, 4 maps. +1 text (16 p., mounted on 1 sheet), https://doi.org/10.3133/ofr78220.","productDescription":"4 maps. +1 text (16 p., mounted on 1 sheet)","costCenters":[],"links":[{"id":170803,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0220/report-thumb.jpg"},{"id":78940,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0220/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78941,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0220/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78942,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0220/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78943,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0220/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":78944,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0220/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c8cd","contributors":{"authors":[{"text":"Moore, George E. Jr.","contributorId":104114,"corporation":false,"usgs":true,"family":"Moore","given":"George","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":224455,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48356,"text":"ofr78300D - 1978 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 1978","interactions":[],"lastModifiedDate":"2024-04-22T17:55:56.843282","indexId":"ofr78300D","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":"78-300","chapter":"D","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 1978","docAbstract":"<p><span>The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78300D","usgsCitation":"Townshend, J., Papp, J., Moorman, M., and Tilton, S., 1978, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: April 1978: U.S. Geological Survey Open-File Report 78-300, 23 p., https://doi.org/10.3133/ofr78300D.","productDescription":"23 p.","costCenters":[],"links":[{"id":427999,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0300-d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161686,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0300-d/report-thumb.jpg"}],"country":"United States","state":"Alaska","city":"Fairbanks","otherGeospatial":"College Observatory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -147.9716829972995,\n              64.92275521538983\n            ],\n            [\n              -147.9716829972995,\n              64.77266196148724\n            ],\n            [\n              -147.4142995458633,\n              64.77266196148724\n            ],\n            [\n              -147.4142995458633,\n              64.92275521538983\n            ],\n            [\n              -147.9716829972995,\n              64.92275521538983\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673893","contributors":{"authors":[{"text":"Townshend, J.B.","contributorId":30623,"corporation":false,"usgs":true,"family":"Townshend","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":237288,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Papp, J.E.","contributorId":95057,"corporation":false,"usgs":true,"family":"Papp","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":237289,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moorman, M.J.","contributorId":12084,"corporation":false,"usgs":true,"family":"Moorman","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":237286,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tilton, S.P.","contributorId":15670,"corporation":false,"usgs":true,"family":"Tilton","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":237287,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":17432,"text":"ofr78823 - 1978 - Nebraska water data programs for 1978","interactions":[],"lastModifiedDate":"2026-02-17T19:32:17.836472","indexId":"ofr78823","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":"78-823","title":"Nebraska water data programs for 1978","docAbstract":"<p>Projects of the Water Resources Division, U.S. Geological Survey, and of State agencies represented by members of the Nebraska Water Data Coordinating Committee are described. The committee members represent the Nebraska Department of Water Resources, Nebraska Department of Environmental Control, Nebraska Department of Health, Conservation and Survey Division of the University of Nebraska-Lincoln, Nebraska Water Resources Center of the University of Nebraska, Nebraska Natural Resources Commission, and Nebraska Game and Parks Commission.&nbsp;</p><p>Current measuring sites are listed. Indexes to streamflow records and flood-prone area maps and a list of recently published reports also are included. 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,{"id":42568,"text":"ofr78557 - 1978 - Sample location map, analytical data, and statistical summary of analyses of rock samples, Chignik and Sutwik Island quadrangles, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:11:04","indexId":"ofr78557","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":"78-557","title":"Sample location map, analytical data, and statistical summary of analyses of rock samples, Chignik and Sutwik Island quadrangles, Alaska","language":"ENGLISH","doi":"10.3133/ofr78557","usgsCitation":"Yount, M.E., Cooley, E., and O’Leary, R.M., 1978, Sample location map, analytical data, and statistical summary of analyses of rock samples, Chignik and Sutwik Island quadrangles, Alaska: U.S. Geological Survey Open-File Report 78-557, 1 map., https://doi.org/10.3133/ofr78557.","productDescription":"1 map.","costCenters":[],"links":[{"id":168757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98901,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0557/plate-1.pdf","size":"10992","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fde8e","contributors":{"authors":[{"text":"Yount, M. E.","contributorId":76748,"corporation":false,"usgs":true,"family":"Yount","given":"M.","middleInitial":"E.","affiliations":[],"preferred":false,"id":226727,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cooley, E.F.","contributorId":83072,"corporation":false,"usgs":true,"family":"Cooley","given":"E.F.","email":"","affiliations":[],"preferred":false,"id":226728,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Leary, Richard M.","contributorId":19936,"corporation":false,"usgs":true,"family":"O’Leary","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":226726,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":43002,"text":"ofr78495 - 1978 - Statistical analysis of geochemical data from Glacier Bay National Monument, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:27","indexId":"ofr78495","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":"78-495","title":"Statistical analysis of geochemical data from Glacier Bay National Monument, Alaska","language":"ENGLISH","doi":"10.3133/ofr78495","usgsCitation":"Johnson, B.R., 1978, Statistical analysis of geochemical data from Glacier Bay National Monument, Alaska: U.S. Geological Survey Open-File Report 78-495, 26 maps ;50 x 68 cm., 16 p., https://doi.org/10.3133/ofr78495.","productDescription":"26 maps ;50 x 68 cm., 16 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,{"id":44183,"text":"ofr78783 - 1978 - Subsurface geology and porosity distribution, Madison Limestone and underlying formations, Powder River basin, northeastern Wyoming and southeastern Montana and adjacent areas","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"ofr78783","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":"78-783","title":"Subsurface geology and porosity distribution, Madison Limestone and underlying formations, Powder River basin, northeastern Wyoming and southeastern Montana and adjacent areas","docAbstract":"To evaluate the Madison Limestone and associated rocks as potential sources for water supplies in the Powder River Basin and adjacent areas, an understanding of the geologic framework of these units, their lithologic facies patterns, the distribution of porosity zones, and the relation between porosity development and stratigraphic facies is necessary. \r\n\r\nRegionally the Madison is mainly a fossiliferous limestone. However, in broad areas of the eastern Rocky Mountains and western Great Plains, dolomite is a dominant constituent and in places the Madison is almost entirely dolomite. Within these areas maximum porosity development is found and it seems to be related to the coarser crystalline dolomite facies. The porosity development is associated with tabular and fairly continuous crystalline dolomite beds separated by non-porous limestones. \r\n\r\nThe maximum porosity development in the Bighorn Dolomite, as in the Madison, is directly associated with the occurrence of a more coarsely crystalline sucrosic dolomite facies. Well data indicate, however, that where the Bighorn is present in the deeper parts of the Powder River Basin, it may be dominated by a finer crystalline dolomite facies of low porosity. \r\n\r\nThe 'Winnipeg Sandstone' is a clean, generally well-sorted, medium-grained sandstone. It shows good porosity development in parts of the northern Powder River Basin and northwestern South Dakota. Because the sandstone is silica-cemented and quartzitic in areas of deep burial, good porosity is expected only where it is no deeper than a few thousand feet. \r\n\r\nThe Flathead Sandstone is a predominantly quartzose, slightly feldspathic sandstone, commonly cemented with iron oxide. Like the 'Winnipeg Sandstone,' it too is silica-cemented and quartzitic in many places so that its porosity is poor in areas of deep burial. \r\n\r\nIllustrations in this report show the thickness, percent dolomite, and porosity-feet for the Bighorn Dolomite and the Madison Limestone and its subdivisions. The porosity-feet for the 'Winnipeg' and Flathead Sandstones and four regional geologic sections are also shown.","language":"ENGLISH","doi":"10.3133/ofr78783","usgsCitation":"Peterson, J.A., 1978, Subsurface geology and porosity distribution, Madison Limestone and underlying formations, Powder River basin, northeastern Wyoming and southeastern Montana and adjacent areas: U.S. Geological Survey Open-File Report 78-783, 16 maps and 5 cross sections ;on 21 sheets 92 x 121 cm.; 32 p., https://doi.org/10.3133/ofr78783.","productDescription":"16 maps and 5 cross sections ;on 21 sheets 92 x 121 cm.; 32 p.","costCenters":[],"links":[{"id":161513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0783/report-thumb.jpg"},{"id":81578,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81579,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81580,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81581,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81582,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81583,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81584,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81585,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81586,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81587,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81588,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81589,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81590,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81591,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81592,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81593,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81594,"rank":416,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81595,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81596,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81597,"rank":419,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-20.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81598,"rank":420,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1978/0783/plate-21.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81599,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0783/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6997bc","contributors":{"authors":[{"text":"Peterson, James A.","contributorId":106872,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":229298,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":48365,"text":"ofr78327 - 1978 - Mineral resources of the Cabinet Mountains Wilderness, Lincoln and Sanders Counties, Montana","interactions":[{"subject":{"id":48365,"text":"ofr78327 - 1978 - Mineral resources of the Cabinet Mountains Wilderness, Lincoln and Sanders Counties, Montana","indexId":"ofr78327","publicationYear":"1978","noYear":false,"title":"Mineral resources of the Cabinet Mountains Wilderness, Lincoln and Sanders Counties, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":33353,"text":"b1501 - 1981 - Mineral resources of the Cabinet Mountains Wilderness, Lincoln and Sanders counties, Montana","indexId":"b1501","publicationYear":"1981","noYear":false,"title":"Mineral resources of the Cabinet Mountains Wilderness, Lincoln and Sanders counties, Montana"},"id":1}],"supersededBy":{"id":33353,"text":"b1501 - 1981 - Mineral resources of the Cabinet Mountains Wilderness, Lincoln and Sanders counties, Montana","indexId":"b1501","publicationYear":"1981","noYear":false,"title":"Mineral resources of the Cabinet Mountains Wilderness, Lincoln and Sanders counties, Montana"},"lastModifiedDate":"2012-08-11T01:01:51","indexId":"ofr78327","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":"78-327","title":"Mineral resources of the Cabinet Mountains Wilderness, Lincoln and Sanders Counties, Montana","docAbstract":"This report describes the differential array, of seismometers recently installed at the Hollister, California, Municipal Airport. Such an array of relatively closely spaced seismometers has already been installed in El Centro and provided useful information for both engineering and seismological applications from the 1979 Imperial Valley earthquake. Differential ground motions, principally due to horizontally propagating surface waves, are important in determining the stresses in such extended structures as large mat foundations for nuclear power stations, dams, bridges and pipelines. Further, analyses of the records of the 1979 Imperial Valley earthquake from the differential array have demonstrated the utility of short-baseline array data in tracking the progress of the rupture wave front of an earthquake.","language":"ENGLISH","doi":"10.3133/ofr78327","usgsCitation":"Lindsey, D.A., Wells, J.D., Van Loenen, R.E., Banister, D.P., Welded, R., Zilka, N.T., and Schmauch, S., 1978, Mineral resources of the Cabinet Mountains Wilderness, Lincoln and Sanders Counties, Montana: U.S. Geological Survey Open-File Report 78-327, vi, 99 p. : maps (14 fold. in envelope) ; 27 cm., https://doi.org/10.3133/ofr78327.","productDescription":"vi, 99 p. : maps (14 fold. in envelope) ; 27 cm.","costCenters":[],"links":[{"id":262843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2d2","contributors":{"authors":[{"text":"Lindsey, David A. 0000-0002-9466-0899 dlindsey@usgs.gov","orcid":"https://orcid.org/0000-0002-9466-0899","contributorId":773,"corporation":false,"usgs":true,"family":"Lindsey","given":"David","email":"dlindsey@usgs.gov","middleInitial":"A.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":237322,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, J. D.","contributorId":58647,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":237326,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Loenen, R. E.","contributorId":99130,"corporation":false,"usgs":true,"family":"Van Loenen","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":237328,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Banister, D. P.","contributorId":25212,"corporation":false,"usgs":true,"family":"Banister","given":"D.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":237324,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Welded, R.D.","contributorId":9311,"corporation":false,"usgs":true,"family":"Welded","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":237323,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Zilka, N. T.","contributorId":97490,"corporation":false,"usgs":true,"family":"Zilka","given":"N.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":237327,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schmauch, S. W.","contributorId":53790,"corporation":false,"usgs":true,"family":"Schmauch","given":"S. W.","affiliations":[],"preferred":false,"id":237325,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":48369,"text":"ofr78984 - 1978 - Field data from an observation well in Hillsborough Bay near Tampa, Florida, drilled March 14 to April 5, 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:10:04","indexId":"ofr78984","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":"78-984","title":"Field data from an observation well in Hillsborough Bay near Tampa, Florida, drilled March 14 to April 5, 1978","language":"ENGLISH","doi":"10.3133/ofr78984","usgsCitation":"Sinclair, W.C., 1978, Field data from an observation well in Hillsborough Bay near Tampa, Florida, drilled March 14 to April 5, 1978: U.S. Geological Survey Open-File Report 78-984, 25 p., illus. incl. tables, https://doi.org/10.3133/ofr78984.","productDescription":"25 p., illus. incl. tables","costCenters":[],"links":[{"id":162736,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5a06","contributors":{"authors":[{"text":"Sinclair, William C.","contributorId":14798,"corporation":false,"usgs":true,"family":"Sinclair","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":237337,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48390,"text":"ofr78819 - 1978 - Water quality investigation of Francis Slocum Lake, Luzerne County, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-12T11:07:55","indexId":"ofr78819","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":"78-819","title":"Water quality investigation of Francis Slocum Lake, Luzerne County, Pennsylvania","docAbstract":"<p>This report summarizes water-quality data collected in the Francis Slocum Lake drainage basin, Pennsylvania, during an assessment from October 1976 to September 1977. Data were collected for nitrogen, phosphorus, carbon, and fecal coliform and fecal streptococcal bacteria.<br></p><p>Results of the restricted sampling indicate that nutrient recycling within the lake is sufficient to support the periodic luxurient growth of algae and aquatic weeds. Inflows are not contributing high concentrations of nutrients to the ecosystem. Sampling for enteric bacteria indicate the sanitary quality is sufficiently high for water-contact recreation.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78819","collaboration":"Prepared in cooperation with the Pennsylvania Department of Environmental Resources, Bureau of State Parks","usgsCitation":"Barker, J.L., 1978, Water quality investigation of Francis Slocum Lake, Luzerne County, Pennsylvania: U.S. Geological Survey Open-File Report 78-819, iv, 11 p., https://doi.org/10.3133/ofr78819.","productDescription":"iv, 11 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":169775,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0819/report-thumb.jpg"},{"id":343693,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0819/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","county":"Luzerne County","otherGeospatial":"Francis Slocum Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.9016227722168,\n              41.329002115630715\n            ],\n            [\n              -75.87982177734375,\n              41.32919547384916\n            ],\n            [\n              -75.8799934387207,\n              41.34827066308899\n            ],\n            [\n              -75.9016227722168,\n              41.34827066308899\n            ],\n            [\n              -75.9016227722168,\n              41.329002115630715\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99fa","contributors":{"authors":[{"text":"Barker, James L.","contributorId":53000,"corporation":false,"usgs":true,"family":"Barker","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":237404,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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