Techniques are developed for estimating 100-year flood depths in natural channels of unregulated Pennsylvania streams that drain less than 2,200 square miles. Equations and graphs are presented relating the depth of the 100-year flood above median stage and drainage area in five defined hydrologic areas in the State. Another graph defines the relation between drainage area and median depth of flow over the low point of riffles. Thus 100-year depths on riffles can be estimated by summing depth values derived from two simple relations.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864195","usgsCitation":"Flippo, H.N., 1990, Technique for estimating depths of 100-year floods in Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 86-4195, Report: iv, 16 p.; 1 Plate: 21.38 x 16.49 inches, https://doi.org/10.3133/wri864195.","productDescription":"Report: iv, 16 p.; 1 Plate: 21.38 x 16.49 inches","numberOfPages":"21","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":310317,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4195/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":158728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri864195.jpg"},{"id":310318,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4195/plate-1.pdf","text":"Plate 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Jr.","contributorId":36597,"corporation":false,"usgs":true,"family":"Flippo","given":"Herbert","suffix":"Jr.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":197600,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":39656,"text":"pp1370G - 1990 - Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste - Characterization of the Bonneville region, Utah and Nevada","interactions":[{"subject":{"id":12311,"text":"ofr84744 - 1984 - Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste; characterization of the Bonneville region, Utah and Nevada","indexId":"ofr84744","publicationYear":"1984","noYear":false,"title":"Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste; characterization of the Bonneville region, Utah and Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":39656,"text":"pp1370G - 1990 - Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste - Characterization of the Bonneville region, Utah and Nevada","indexId":"pp1370G","publicationYear":"1990","noYear":false,"chapter":"G","title":"Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste - Characterization of the Bonneville region, Utah and Nevada"},"id":1}],"lastModifiedDate":"2017-08-31T15:40:00","indexId":"pp1370G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"1370","chapter":"G","title":"Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste - Characterization of the Bonneville region, Utah and Nevada","docAbstract":"The Bonneville region of the Basin and Range province in westcentral Utah and adjacent Nevada includes several basins lying south of the Great Salt Lake Desert. Physiographically, the region consists of linear, north-trending mountain ranges separated by valleys, many of which are closed basins underlain by thick sequences of fill. Surface drainage of open basins and ground-water flow is to the Great Salt Lake Desert. In structure and composition the ranges are faulted Paleozoic rocks, locally intruded by Mesozoic and Tertiary plugs and stocks. In the southern and northeastern parts of the region, volcanic rocks are widespread and form large parts of some mountain ranges. The Paleozoic sedimentary rocks include great thicknesses of carbonate rocks which compose a significant aquifer in the region
Media considered to have potential for isolation of high-level radioactive waste in the region include intrusive rocks, such as granite; ash-flow tuff; and basalt and basaltic andesite lava flows. These rock types, basin fill, and possibly other rock types, may have potential as host media in the unsaturated zone. Quaternary tectonism in the region is evidenced by seismic activity, local areas of above-normal geothermal heat flow, Quaternary faulting, late Cenozoic volcanic activity, and active vertical crustal movement.
The Bonneville region is part of a large ground-water flow system that is integrated partly through basin-fill deposits, but largely through an underlying carbonate-rock sequence. The region includes: (1) several topographically closed basins with virtually no local surface discharge that are drained by the underlying carbonate-rock aquifer; (2) closed basins with local surface discharge by evapotranspiration; and (3) basins open to the Great Salt Lake Desert that discharge by groundwater underflow and evapotranspiration. The carbonate-rock aquifer discharges to large springs in the Desert and in basins tributary to the Desert. The climate is arid to semiarid with the greatest precipitation in the mountain ranges. Most recharge probably occurs by infiltration of runoff as it leaves the mountains, although some recharge probably occurs directly to the carbonate rocks in the mountain areas. The concentration of dissolved solids in ground water is generally less than 500 milligrams per liter. Dissolved-solids concentrations increase in the Great Salt Lake Desert and in major valleys adjoining the Desert. The predominant chemical constituents in ground water are calcium, magnesium, and sodium bicarbonate. Chloride-type water is associated with the higher dissolved-solids content of water in and near the Great Salt Lake Desert.
The majority of the mineral occurrences containing base- and precious-metal deposits in the Bonneville region are of Tertiary age. Fluorspar is the primary industrial mineral. Coal, oil, and gas have not been produced in significant amounts.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr90188","usgsCitation":"Burtell, R.T., 1990, Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, September 1989: U.S. Geological Survey Open-File Report 90-188, 1 Plate: 26.36 × 45.44 inches, https://doi.org/10.3133/ofr90188.","productDescription":"1 Plate: 26.36 × 45.44 inches","costCenters":[],"links":[{"id":170798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":408761,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17875.htm","linkFileType":{"id":5,"text":"html"}},{"id":78937,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0188/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -83,\n 31\n ],\n [\n -83,\n 26.5\n ],\n [\n -80,\n 26.5\n ],\n [\n -80,\n 31\n ],\n [\n -83,\n 31\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682aaf","contributors":{"authors":[{"text":"Burtell, R. 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United States concise 1990: U.S. Geological Survey Professional Paper 1200, 526 p., https://doi.org/10.3133/pp1200US.","productDescription":"526 p.","costCenters":[],"links":[{"id":119150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1200us/report-thumb.jpg"},{"id":65408,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1200us/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b19d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529868,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27216,"text":"wri894210 - 1990 - Application of a distributed-routing rainfall-runoff model to flood-frequency estimation in Somerset County, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:43","indexId":"wri894210","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-4210","title":"Application of a distributed-routing rainfall-runoff model to flood-frequency estimation in Somerset County, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri894210","usgsCitation":"Fulton, J., 1990, Application of a distributed-routing rainfall-runoff model to flood-frequency estimation in Somerset County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 89-4210, vii, 78 p. :ill. ;28 cm., https://doi.org/10.3133/wri894210.","productDescription":"vii, 78 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4210/report-thumb.jpg"},{"id":56088,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4210/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67ab5e","contributors":{"authors":[{"text":"Fulton, J.L.","contributorId":49407,"corporation":false,"usgs":true,"family":"Fulton","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":197748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17829,"text":"ofr89391 - 1990 - Water-quality data-collection activities in Colorado and Ohio; Phase III, evaluation of existing data for use in assessing regional water-quality conditions and trends","interactions":[{"subject":{"id":17829,"text":"ofr89391 - 1990 - Water-quality data-collection activities in Colorado and Ohio; Phase III, evaluation of existing data for use in assessing regional water-quality conditions and trends","indexId":"ofr89391","publicationYear":"1990","noYear":false,"title":"Water-quality data-collection activities in Colorado and Ohio; Phase III, evaluation of existing data for use in assessing regional water-quality conditions and trends"},"predicate":"SUPERSEDED_BY","object":{"id":31064,"text":"wsp2295C - 1992 - Water-quality data-collection activities in Colorado and Ohio: Phase III-evaluation of existing data for use in assessing regional water-quality conditions and trends","indexId":"wsp2295C","publicationYear":"1992","noYear":false,"chapter":"C","title":"Water-quality data-collection activities in Colorado and Ohio: Phase III-evaluation of existing data for use in assessing regional water-quality conditions and trends"},"id":1}],"supersededBy":{"id":31064,"text":"wsp2295C - 1992 - Water-quality data-collection activities in Colorado and Ohio: Phase III-evaluation of existing data for use in assessing regional water-quality conditions and trends","indexId":"wsp2295C","publicationYear":"1992","noYear":false,"title":"Water-quality data-collection activities in Colorado and Ohio: Phase III-evaluation of existing data for use in assessing regional water-quality conditions and trends"},"lastModifiedDate":"2016-11-30T15:28:33","indexId":"ofr89391","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-391","title":"Water-quality data-collection activities in Colorado and Ohio; Phase III, evaluation of existing data for use in assessing regional water-quality conditions and trends","docAbstract":"During the past several years, a growing number of questions have been raised by members of Congress and others about the status of current waterquality conditions in the Nation, trends in water quality, and the major factors that affect water-quality conditions and trends. One area of particular interest and concern has been the suitability of existing water-quality data for addressing these types of questions at regional and national scales. In response to these questions and concerns, the U.S. Geological Survey began a pilot study in Colorado and Ohio to (1) determine the characteristics of current water-quality data-collection activities of Federal, State, regional, and local agencies and universities; and (2) determine how well the data from these activities, collected for various purposes and using different procedures, can be used to improve our ability to address the aforementioned questions.
Colorado and Ohio were chosen for the pilot study because they represent regions with different types of water-quality issues and programs. The results of the study are specific to the two States and are not intended to be extrapolated to other States.
The study was divided into three phases whose objectives were:
Phase I Identify and inventory 1984 water-quality data-collection programs, including costs, in Colorado and Ohio, and identify those programs that meet a set of broad criteria for producing data that potentially are appropriate for water-quality assessments of regional and national scope.
Phase II Evaluate the quality assurance of field and laboratory procedures used to produce the data from programs that met the broad criteria of Phase I.
Phase III Compile the qualifying data from Phase II and evaluate the extent to which the resulting data base can be used to address selected water-quality questions for the two States.
This report presents the results of Phase III, focusing on (1) the number of measurements made at each data-collection site for selected constituents, (2) the areal distribution of those sites that have sufficient data for selected types of analyses, and (3) the availability of key ancillary information such as streamflow to address broad-scope questions such as:
The purpose of this map is to aid in the mineral-resource assessment and exploration of covered host rocks by displaying and interpreting data that can be used to estimate the depth of basin fill in the Winnemucca 1° by 2° quadrangle, Nevada. Publicly available information used in making this map includes water, petroleum, and geothermal well data, gravity data and models, seismic profiles, and geologic and geomorphic reports.
\nWells logs used for this map of the Winnemucca quadrangle are from the following sources: (1) logs of more than 1,000 water wells reported to the State of Nevada Division of Water Resources, which are on file with them in Reno and at the with U.S. Geological Survey in Carson City, (2) 44 petroleum wells collected by the Nevada Bureau of Mines (Lintz, 1957; Schilling and Garside, 1968; Garside and Schilling, 1977, Garside and others, 1977; 1988), and (3) Two geothermal wells reported in Zoback (1979) and Flynn and others (1982). Data from isostatic residual and Bouguer gravity maps by Wagini (1985) contributed to the interpretation of basin configuration. Gravity models of Dixie Valley (Schaefer, 1982, and Speed, 1976) and Grass Valley (Grannell and Noble, 1977) and seismic profiles of Grass and Pine Valleys (Potter and others, 1987) helped refine basis interpretations in those areas. The geologic base map of Paleozoic and Mesozoic igneous and sedimentary rocks, Tertiary volcanic and sedimentary rocks, and Cenozoic structures was simplified from Stewart and Carlson (1976b).
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1955","usgsCitation":"Moring, B.C., 1990, Map showing drill-hole depths, lithologic intercepts, and partial isopachs of basin fill in the Winnemucca 1 degree by 2 degrees quadrangle, Nevada: U.S. Geological Survey Miscellaneous Field Studies Map 1955, 1 Plate: 30.15 x 31.48 inches, https://doi.org/10.3133/mf1955.","productDescription":"1 Plate: 30.15 x 31.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":486593,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5525.htm","linkFileType":{"id":5,"text":"html"}},{"id":327361,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1955/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180602,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1955.PNG"}],"scale":"250000","country":"United States","state":"Nevada","otherGeospatial":"Winnemucca 1 degree by 2 degrees quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -118,\n 41\n ],\n [\n -118,\n 40\n ],\n [\n -116,\n 40\n ],\n [\n -116,\n 41\n ],\n [\n -118,\n 41\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67cac2","contributors":{"authors":[{"text":"Moring, B. C.","contributorId":91462,"corporation":false,"usgs":true,"family":"Moring","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":263653,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17103,"text":"ofr89576 - 1990 - Evaluation of three electronic report processing systems for preparing hydrologic reports of the U.S Geological Survey, Water Resources Division","interactions":[],"lastModifiedDate":"2012-02-02T00:07:18","indexId":"ofr89576","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-576","title":"Evaluation of three electronic report processing systems for preparing hydrologic reports of the U.S Geological Survey, Water Resources Division","docAbstract":"In 1987, the Water Resources Division of the U.S. Geological Survey undertook three pilot projects to evaluate electronic report processing systems as a means to improve the quality and timeliness of reports pertaining to water resources investigations. The three projects selected for study included the use of the following configuration of software and hardware: Ventura Publisher software on an IBM model AT personal computer, PageMaker software on a Macintosh computer, and FrameMaker software on a Sun Microsystems workstation. The following assessment criteria were to be addressed in the pilot studies: The combined use of text, tables, and graphics; analysis of time; ease of learning; compatibility with the existing minicomputer system; and technical limitations. It was considered essential that the camera-ready copy produced be in a format suitable for publication. Visual improvement alone was not a consideration. This report consolidates and summarizes the findings of the electronic report processing pilot projects. Text and table files originating on the existing minicomputer system were successfully transformed to the electronic report processing systems in American Standard Code for Information Interchange (ASCII) format. Graphics prepared using a proprietary graphics software package were transferred to all the electronic report processing software through the use of Computer Graphic Metafiles. Graphics from other sources were entered into the systems by scanning paper images. Comparative analysis of time needed to process text and tables by the electronic report processing systems and by conventional methods indicated that, although more time is invested in creating the original page composition for an electronically processed report , substantial time is saved in producing subsequent reports because the format can be stored and re-used by electronic means as a template. Because of the more compact page layouts, costs of printing the reports were 15% to 25% less than costs of printing the reports prepared by conventional methods. Because the largest report workload in the offices conducting water resources investigations is preparation of Water-Resources Investigations Reports, Open-File Reports, and annual State Data Reports, the pilot studies only involved these projects. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr89576","usgsCitation":"Stiltner, G., 1990, Evaluation of three electronic report processing systems for preparing hydrologic reports of the U.S Geological Survey, Water Resources Division: U.S. Geological Survey Open-File Report 89-576, 66 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89576.","productDescription":"66 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":150457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0576/report-thumb.jpg"},{"id":46232,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0576/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa051","contributors":{"authors":[{"text":"Stiltner, G.J.","contributorId":56668,"corporation":false,"usgs":true,"family":"Stiltner","given":"G.J.","affiliations":[],"preferred":false,"id":174940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36158,"text":"b1673 - 1990 - Selected caves and lava-tube systems in and near Lava Beds National Monument, California","interactions":[],"lastModifiedDate":"2015-11-23T11:34:45","indexId":"b1673","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"1673","title":"Selected caves and lava-tube systems in and near Lava Beds National Monument, California","docAbstract":"Lava Beds National Monument (fig. 1) lies on the north slope of the huge Medicine Lake shield (fig. 2), a complex volcanic edifice of greater volume than the steep-sided Mount Shasta volcanic cone, which towers as a snowclad land mark 40 mi southwest of the monument (fig. 3).
\nMuch of the north and south flanks of the Medicine Lake shield were built from molten lava transmitted through lava tubes. These tubes formed beneath the congealing surface of basalt flows in somewhat the same way that a brook may continue to flow beneath a cover of its own winter ice. As molten lava emerges from a vent and flows downslope, congealing lava from the top and sides of the central channel often forms a bridge over the lava stream. The sticking together of bits of lava spatter and fragile lava crusts strengthens the bridge in the manner that thin crusts of floating ice raft together to cover a brook during early stages of a winter freeze. Eruption of basalt lava, however, is a much more violent and spasmodic process than the steady gathering of water that feeds a brook. If liquid lava stops rising from its source deep within the earth, the still-molten lava moving beneath the crusted-over top of a lava flow will continue to drain downhill and may ultimately leave an open lavatube cave-often large enough for people to walk through. It is rare, however, to find such a simple scenario recorded intact among the hundreds of lava-tube caves in the monument. Even before the top and walls of a lava flow have time to cool during a pause in lava supply, a new and violent eruption of lava may refill the open tube, overflow its upper end, and spread a new lava flow beside or on top of the first flow. Even if the original tube is large enough to contain the renewed supply of lava, this tube must deliver the new lava beyond the end of its original flow and thus the lava field extends farther and farther downslope. If the gradient of flow flattens, the tube may subdivide into a number of smaller distributaries, which spread laterally over the more gently sloping ground.
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1673","usgsCitation":"Waters, A.C., Donnelly-Nolan, J.M., and Rogers, B.W., 1990, Selected caves and lava-tube systems in and near Lava Beds National Monument, California: U.S. Geological Survey Bulletin 1673, ix, 102 p.; 6 Plates: 41.40 x 49.12 inches or smaller, https://doi.org/10.3133/b1673.","productDescription":"ix, 102 p.; 6 Plates: 41.40 x 49.12 inches or smaller","numberOfPages":"116","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":97246,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1673/plate-3.pdf","size":"712","linkFileType":{"id":1,"text":"pdf"}},{"id":97247,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1673/plate-4.pdf","size":"873","linkFileType":{"id":1,"text":"pdf"}},{"id":97245,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1673/plate-2.pdf","size":"1105","linkFileType":{"id":1,"text":"pdf"}},{"id":97248,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1673/plate-5.pdf","size":"1076","linkFileType":{"id":1,"text":"pdf"}},{"id":97249,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1673/plate-6.pdf","size":"1192","linkFileType":{"id":1,"text":"pdf"}},{"id":165346,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1673/report-thumb.jpg"},{"id":311550,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1673/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":97244,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1673/plate-1.pdf","size":"2006","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Lava Beds National Monument","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.6845703125,\n 41.65239288426814\n ],\n [\n -121.6845703125,\n 41.84808170729207\n ],\n [\n -121.43463134765625,\n 41.84808170729207\n ],\n [\n -121.43463134765625,\n 41.65239288426814\n ],\n [\n -121.6845703125,\n 41.65239288426814\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa66d","contributors":{"authors":[{"text":"Waters, Aaron Clement","contributorId":8081,"corporation":false,"usgs":true,"family":"Waters","given":"Aaron","email":"","middleInitial":"Clement","affiliations":[],"preferred":false,"id":215864,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Donnelly-Nolan, Julie M. 0000-0001-8714-9606 jdnolan@usgs.gov","orcid":"https://orcid.org/0000-0001-8714-9606","contributorId":3271,"corporation":false,"usgs":true,"family":"Donnelly-Nolan","given":"Julie","email":"jdnolan@usgs.gov","middleInitial":"M.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":215863,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rogers, Bruce W.","contributorId":91549,"corporation":false,"usgs":true,"family":"Rogers","given":"Bruce","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":215865,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27955,"text":"wri904021 - 1990 - Methods for selection and hydrologic description of potential landfill sites in southeastern San Diego County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri904021","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4021","title":"Methods for selection and hydrologic description of potential landfill sites in southeastern San Diego County, California","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904021","usgsCitation":"Kaehler, C., 1990, Methods for selection and hydrologic description of potential landfill sites in southeastern San Diego County, California: U.S. Geological Survey Water-Resources Investigations Report 90-4021, v, 73 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904021.","productDescription":"v, 73 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":126461,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4021/report-thumb.jpg"},{"id":56763,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8e0c","contributors":{"authors":[{"text":"Kaehler, C. A.","contributorId":59469,"corporation":false,"usgs":true,"family":"Kaehler","given":"C. A.","affiliations":[],"preferred":false,"id":198963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26370,"text":"wri904062 - 1990 - Results of test drilling in Howell Township, Monmouth County, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:32","indexId":"wri904062","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4062","title":"Results of test drilling in Howell Township, Monmouth County, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri904062","usgsCitation":"Brown, G.A., and Zapecza, O., 1990, Results of test drilling in Howell Township, Monmouth County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 90-4062, v, 42 p. :ill. ;28 cm., https://doi.org/10.3133/wri904062.","productDescription":"v, 42 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":158084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4062/report-thumb.jpg"},{"id":55162,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4062/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6055f8","contributors":{"authors":[{"text":"Brown, G. A.","contributorId":23582,"corporation":false,"usgs":true,"family":"Brown","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zapecza, O. S.","contributorId":22787,"corporation":false,"usgs":true,"family":"Zapecza","given":"O. 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Volume 1. Southern Great Basin from Mexican Border to Mono Lake Basin; and Pacific Slope Basins from Tijuana River to Santa Maria River","interactions":[],"lastModifiedDate":"2012-09-01T01:01:51","indexId":"wdrCA891","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-89-1","title":"Water Resources Data, California, Water Year 1989. Volume 1. Southern Great Basin from Mexican Border to Mono Lake Basin; and Pacific Slope Basins from Tijuana River to Santa Maria River","docAbstract":"Water resources data for the 1989 water year for California consist of records of stage, discharge, and water quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in wells. Volume 1 contains discharge records for 137 gaging stations; stage and contents for 15 lakes and reservoirs; water quality for 25 streams; and precipitation for 8 gaging stations. Also included are 15 crest-stage partial-record stations, 7 miscellaneous measurement sites, and 5 water-quality partial record stations. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Sacramento, CA","doi":"10.3133/wdrCA891","collaboration":"Prepared in cooperation with the California Department of Water Resources and with other agencies","usgsCitation":"Hoffman, E., Bowers, J.C., and Jensen, R., 1990, Water Resources Data, California, Water Year 1989. Volume 1. 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This report contains discharge records for 178 gaging stations and stage and contents for 26 lakes and reservoirs; water quality for 26 gaging stations and 10 miscellaneous sites; continuous daily tide stage for 12 sites; and water levels for 43 observation wells. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements in this report. The collection of water-resources data in North Carolina is a part of the National Water-Data System operated by the U.S. Geological Survey in cooperation with State, municipal, and Federal agencies.
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Carolina\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697b9a","contributors":{"authors":[{"text":"Ragland, B.C.","contributorId":27127,"corporation":false,"usgs":true,"family":"Ragland","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":251409,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barker, R.G.","contributorId":93121,"corporation":false,"usgs":true,"family":"Barker","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":251412,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eddins, W.H.","contributorId":47796,"corporation":false,"usgs":true,"family":"Eddins","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":251410,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Padyk, 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Volume 2. Pacific Slope Basins from Arroyo Grande to Oregon State Line except Central Valley","interactions":[],"lastModifiedDate":"2012-09-04T17:16:10","indexId":"wdrCA892","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-89-2","title":"Water Resources Data, California, Water Year 1989. Volume 2. Pacific Slope Basins from Arroyo Grande to Oregon State Line except Central Valley","docAbstract":"Water resources data for the 1989 water year for California consist of records of stage, discharge, and water. quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in wells. Volume 2 contains discharge records for 127 gaging stations, stage and contents for 7 lakes and reservoir and water quality for 32 stations. Also included is 1 low-flow partial-record station and 22 waterquality partial-record stations. These data represent that part of the National Water Data System operated by the u.s. Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Sacramento, CA","doi":"10.3133/wdrCA892","collaboration":"Prepared in cooperation with the California Department of Water Resources and with other agencies","usgsCitation":"Palmer, J.R., Shelton, W., Trujillo, L., and Markham, K., 1990, Water Resources Data, California, Water Year 1989. Volume 2. Pacific Slope Basins from Arroyo Grande to Oregon State Line except Central Valley (Legacy Report): U.S. Geological Survey Water Data Report CA-89-2, x, 320 p., https://doi.org/10.3133/wdrCA892.","productDescription":"x, 320 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":174137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_ca_89_2.jpg"},{"id":260161,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1989/ca-89/WDR-1989-vol2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.83333333333333,35 ], [ -119.83333333333333,42 ], [ -124.4,42 ], [ -124.4,35 ], [ -119.83333333333333,35 ] ] ] } } ] }","edition":"Legacy Report","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc3a9","contributors":{"authors":[{"text":"Palmer, J. R.","contributorId":83559,"corporation":false,"usgs":true,"family":"Palmer","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":250264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shelton, W.F.","contributorId":48241,"corporation":false,"usgs":true,"family":"Shelton","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":250262,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trujillo, L.F.","contributorId":71959,"corporation":false,"usgs":true,"family":"Trujillo","given":"L.F.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":250263,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Markham, K.L.","contributorId":14041,"corporation":false,"usgs":true,"family":"Markham","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":250261,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":54411,"text":"wdrCA895 - 1990 - Water Resources Data, California, Water Year 1989. Volume 5. Ground-Water Data","interactions":[],"lastModifiedDate":"2012-09-01T01:01:51","indexId":"wdrCA895","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-89-5","title":"Water Resources Data, California, Water Year 1989. Volume 5. Ground-Water Data","docAbstract":"Water resources data for the 1989 water year for California consist of records of stage, discharge, and water quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in weils. Volume 5 contains water levels for 1,037 observation wells and water-quality data for 254 monitoring wells. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperatine State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey, Water Resources Division","publisherLocation":"Sacramento, CA","doi":"10.3133/wdrCA895","collaboration":"Prepared in cooperation with other Federal, State, and local agencies","usgsCitation":"Lamb, C.E., Johnson, J.A., Fogelman, R.P., and Grillo, D., 1990, Water Resources Data, California, Water Year 1989. Volume 5. Ground-Water Data (Legacy Report): U.S. Geological Survey Water Data Report CA-89-5, vii, 398 p., https://doi.org/10.3133/wdrCA895.","productDescription":"vii, 398 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":181923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_ca_89_5.jpg"},{"id":260074,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1989/ca-89/WDR-1989-vol5.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.13333333333334,32.5 ], [ -114.13333333333334,42 ], [ -124.4,42 ], [ -124.4,32.5 ], [ -114.13333333333334,32.5 ] ] ] } } ] }","edition":"Legacy Report","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc1ab","contributors":{"authors":[{"text":"Lamb, C. E.","contributorId":59793,"corporation":false,"usgs":true,"family":"Lamb","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":250272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, J. A.","contributorId":88375,"corporation":false,"usgs":true,"family":"Johnson","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":250273,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fogelman, R. P.","contributorId":96688,"corporation":false,"usgs":true,"family":"Fogelman","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":250274,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grillo, D.A.","contributorId":45727,"corporation":false,"usgs":true,"family":"Grillo","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":250271,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":55098,"text":"wdrWV881 - 1990 - Water resources data, West Virginia, water year 1988","interactions":[],"lastModifiedDate":"2025-02-19T14:35:03.029177","indexId":"wdrWV881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WV-88-1","title":"Water resources data, West Virginia, water year 1988","docAbstract":"Water-resources data for the 1988 water year for West Virginia consist of records of stage, discharge, and water quality of streams; contents of reservoirs; and water levels of observation wells. This report contains discharge records for 79 streamflow-gaging stations; stage only records for 7 gaging stations, and 2 crest-stage partial-record stations; (2) change in contents for 1 reservoir; (3) water-quality records for 15 streamflow-gaging stations; and (4) water-level records for 30 observation wells. Locations of these sites are shown on figures 4 and 5. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in West Virginia.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWV881","collaboration":"Prepared in cooperation with the State of West Virginia and with other agencies","usgsCitation":"Ward, S., Macy, J.A., Taylor, F., and Ferrell, G., 1990, Water resources data, West Virginia, water year 1988: U.S. Geological Survey Water Data Report WV-88-1, viii, 185 p., https://doi.org/10.3133/wdrWV881.","productDescription":"viii, 185 p.","costCenters":[],"links":[{"id":482188,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1988/wv-88-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181091,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1988/wv-88-1/report-thumb.jpg"}],"country":"United States","state":"West 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A.","contributorId":10047,"corporation":false,"usgs":true,"family":"Macy","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":252655,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, F.M.","contributorId":31465,"corporation":false,"usgs":true,"family":"Taylor","given":"F.M.","email":"","affiliations":[],"preferred":false,"id":252656,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ferrell, G.M.","contributorId":92681,"corporation":false,"usgs":true,"family":"Ferrell","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":252657,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1242,"text":"wsp2341B - 1990 - Evaluation of site-selection criteria, well design, monitoring techniques, and cost analysis for a ground-water supply in Piedmont crystalline rocks, North Carolina","interactions":[],"lastModifiedDate":"2017-02-01T10:30:37","indexId":"wsp2341B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2341","chapter":"B","title":"Evaluation of site-selection criteria, well design, monitoring techniques, and cost analysis for a ground-water supply in Piedmont crystalline rocks, North Carolina","docAbstract":"A statistical analysis of data from wells drilled into the crystalline rocks of the Piedmont and Blue Ridge provinces of North Carolina verified and refined previously proposed criteria for the siting of wells to obtain greater than average yields. An opportunity to test the criteria was provided by the expansion of the town of Cary's municipal ground-water system. Three criteria were used: type of rock, thickness of saturated regolith based upon topography, and presence of fractures and joints based upon drainage lineations. A conceptual model of the local hydrogeologic system was developed to guide the selection of the most favorable well sites, and on the basis of the model, six type sites were determined. Eleven of 12 test wells that were located on the basis of type sites yielded from slightly above average to as much as six times the average yield to be expected from particular rock types as reported in the literature. Only one well drilled at a type site had a less than average yield. One well not located at any of the type sites produced little water.\r\n\r\nLong-term testing and monitoring after the wells were put into production showed that an 18-hour-on, 6-hour-off pumping cycle was much more effective in terms of total production, reduced head loss, and less drawdown than a 5-day-on and 2-day-off cycle. It was also observed that long-term yields by the production wells were about 75 percent of those predicted on the basis of 24-hour pumping tests and only about 60 percent of the driller's reported yields.\r\n\r\nCost analysis showed that, by using criteria-selected well sites, a cost-effective well system can be developed that will provide water at an equivalent or lower cost than a surface-water supply. The analysis showed that the system would be cost effective if only one high-yield well were obtained out of every four drilled.","language":"ENGLISH","publisher":"U.S. G.P.O. ;\r\nFor sale by the Books and Open-File Reports Section, U.S. Geological Survey,","doi":"10.3133/wsp2341B","usgsCitation":"Daniel, C., 1990, Evaluation of site-selection criteria, well design, monitoring techniques, and cost analysis for a ground-water supply in Piedmont crystalline rocks, North Carolina: U.S. Geological Survey Water Supply Paper 2341, 1 v. (various pagings) :ill., maps ;28 cm., https://doi.org/10.3133/wsp2341B.","productDescription":"1 v. 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