{"pageNumber":"1346","pageRowStart":"33625","pageSize":"25","recordCount":46734,"records":[{"id":29376,"text":"wri934181 - 1994 - Use of a precipitation-runoff model for simulating effects of forest management on streamflow in 11 small drainage basins, Oregon Coast Range","interactions":[],"lastModifiedDate":"2017-02-07T08:33:14","indexId":"wri934181","displayToPublicDate":"1995-04-01T00:00:00","publicationYear":"1994","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":"93-4181","title":"Use of a precipitation-runoff model for simulating effects of forest management on streamflow in 11 small drainage basins, Oregon Coast Range","docAbstract":"The Precipitation-Runoff Modeling System (PRMS) model of the U.S. Geological Survey was used to simulate the hydrologic effects of timber management in 11 small, upland drainage basins of the Coast Range in Oregon. The coefficients of determination for observed and simulated daily flow during the calibration periods ranged from 0.92 for the Flynn Creek Basin to 0.68 for the Priorli Creek Basin; percent error ranged from -0.25 for the Deer Creek Basin to -4.49 for the Nestucca River Basin. The coefficients of determination during the validation periods ranged from 0.90 for the Flynn Creek Basin to 0.66 for the Wind River Basin; percent error during the validation periods ranged from -0.91 for the Flynn Creek Basin to 22.3 for the Priorli Creek Basin. In addition to daily simulations, 42 storms were selected from the time-series periods in which the 11 basins were studied and used in hourly storm-mode simulations. Sources of simulation error included the quality of the input data, deficiencies in the PRMS model-algorithms, and the quality of parameter estimation. Times-series data from the Flynn Creek and Needle Branch Basins, collected during an earlier U.S. Geological Survey paired-watershed study, were used to evaluate the PRMS as a tool for predicting the hydrologic effects of timber-management practices. The Flynn Creek Basin remained forested and undisturbed during the data-collection period, while the Needle Branch Basin had been clearcut 82 percent at a midpoint during the period of data collection. Using the PRMS, streamflow at the Needle Branch Basin was simulated during the postlogging period using prelogging parameter values. Comparison of postlogging observed streamflow with the simulated data showed an increase in annual discharge volume of approximately 8 percent and a small increase in peak flows of from 1 to 2 percent. The simulated flows from the basins studied were generally insensitive to the number of hydrologic-response units used to replicate basin surface detail. The average number of hydrologic-response units used in the storm-period simulations was one-half the average number of hydrologic-response units used in the daily period simulations. With the exception of one basin, however, the coefficient of determination between observed and simulated daily flow differed by only 3 percent. Calibration and validation of the PRMS for 11 basins--that encompass a variety of forest, soil, and topographic conditions--provided regionalized parameter values. The parameter values assist the PRMS hydrologic simulations of other gaged and ungaged basins in the Coast Range with landscape conditions similar to those of the basins studied.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934181","usgsCitation":"Risley, J.C., 1994, Use of a precipitation-runoff model for simulating effects of forest management on streamflow in 11 small drainage basins, Oregon Coast Range: U.S. Geological Survey Water-Resources Investigations Report 93-4181, v, 61 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934181.","productDescription":"v, 61 p. :ill., maps ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":159844,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4181/report-thumb.jpg"},{"id":58221,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4181/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db5458fc","contributors":{"authors":[{"text":"Risley, J. C.","contributorId":88780,"corporation":false,"usgs":true,"family":"Risley","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201431,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28166,"text":"wri944054 - 1994 - Use of frequency analysis and the extended streamflow prediction procedure to estimate evacuation dates for the joint-use pool of Pueblo Reservoir, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri944054","displayToPublicDate":"1995-04-01T00:00:00","publicationYear":"1994","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":"94-4054","title":"Use of frequency analysis and the extended streamflow prediction procedure to estimate evacuation dates for the joint-use pool of Pueblo Reservoir, Colorado","docAbstract":"Part of the storage space of Pueblo Reservoir consists of a 65,950 acre-foot joint-use pool (JUP) that can be used to provide additional conservation capacity from November 1 to April 14; however, the JUP must be evacuated by April 15 and used only for flood-control capacity until November 1. A study was completed to determine if the JUP possibly could be used for conservation storage for any number of days from April 15 through May 14 under certain hydrologic conditions. The methods of the study were: (1) Frequency analysis of recorded daily mean discharge data for streamflow-gaging stations upstream and downstream from Pueblo Reservoir, and (2) Implementation of the extended streamflow prediction (ESP) procedure for the Arkansas River basin upstream from the reservoir. The frequency analyses enabled estimation of daily discharges at selected exceedance probabilities (EP's), including the 0.01 EP that was used in design of the flood- storage capacity of Pueblo Reservoir. The ESP procedure enabled probabilistic forecasts of inflow volume to the reservoir for April 15 through May 14. Daily discharges derived from the frequency analyses were routed through Pueblo Reservoir to estimate evacuation dates of the JUP for different reservoir inflow volumes; the estimates indicated a relation between the inflow volume and the JUP evacuation date. To apply the study results, only a ESP forecast of the April 15-May 14 reservoir inflow volume is needed. Study results indicate the JUP possibly could be used as late as May 5 depending on the forecast inflow volume.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944054","usgsCitation":"Kuhn, G., and Nickless, R., 1994, Use of frequency analysis and the extended streamflow prediction procedure to estimate evacuation dates for the joint-use pool of Pueblo Reservoir, Colorado: U.S. Geological Survey Water-Resources Investigations Report 94-4054, v, 46 p. :ill., map ;28 cm., https://doi.org/10.3133/wri944054.","productDescription":"v, 46 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":159359,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4054/report-thumb.jpg"},{"id":57000,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4054/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60458a","contributors":{"authors":[{"text":"Kuhn, Gerhard","contributorId":102080,"corporation":false,"usgs":true,"family":"Kuhn","given":"Gerhard","email":"","affiliations":[],"preferred":false,"id":199324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nickless, R.C.","contributorId":85229,"corporation":false,"usgs":true,"family":"Nickless","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":199323,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17514,"text":"ofr94622 - 1994 - Preliminary geologic map emphasizing bedrock formations in Contra Costa County, California: A digital database","interactions":[],"lastModifiedDate":"2022-07-18T20:33:30.885879","indexId":"ofr94622","displayToPublicDate":"1995-04-01T00:00:00","publicationYear":"1994","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":"94-622","title":"Preliminary geologic map emphasizing bedrock formations in Contra Costa County, California: A digital database","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94622","usgsCitation":"Graymer, R., Jones, D.L., and Brabb, E.E., 1994, Preliminary geologic map emphasizing bedrock formations in Contra Costa County, California: A digital database: U.S. Geological Survey Open-File Report 94-622, HTML Document, https://doi.org/10.3133/ofr94622.","productDescription":"HTML Document","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":149057,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":108694,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16666.htm","linkFileType":{"id":5,"text":"html"},"description":"16666"},{"id":1064,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1994/of94-622/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","county":"Contra Costa County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.424,\n              37.717\n            ],\n            [\n              -121.526,\n              37.717\n            ],\n            [\n              -121.526,\n              38.081\n            ],\n            [\n              -122.424,\n              38.081\n            ],\n            [\n              -122.424,\n              37.717\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c10e","contributors":{"authors":[{"text":"Graymer, R. W.","contributorId":21174,"corporation":false,"usgs":true,"family":"Graymer","given":"R. W.","affiliations":[],"preferred":false,"id":176681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, David Lawrence","contributorId":11580,"corporation":false,"usgs":true,"family":"Jones","given":"David","email":"","middleInitial":"Lawrence","affiliations":[],"preferred":false,"id":176680,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brabb, Earl E.","contributorId":48939,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":176682,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27581,"text":"wri934207 - 1994 - Hydrogeology and simulation of ground-water flow at Arnold Air Force Base, Coffee and Franklin counties, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri934207","displayToPublicDate":"1995-04-01T00:00:00","publicationYear":"1994","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":"93-4207","title":"Hydrogeology and simulation of ground-water flow at Arnold Air Force Base, Coffee and Franklin counties, Tennessee","docAbstract":"The U.S. Air Force at Arnold Air Force Base (AAFB), in Coffee and Franklin Counties, Tennessee, is investigating ground-water contamination in selected areas of the base. This report documents the results of a comprehensive investigation of the regional hydrogeology of the AAFB area. Three aquifers within the Highland Rim aquifer system, the shallow aquifer, the Manchester aquifer, and the Fort Payne aquifer, have been identified in the study area. Of these, the Manchester aquifer is the primary source of water for domestic use. Drilling and water- quality data indicate that the Chattanooga Shale is an effective confining unit, isolating the Highland Rim aquifer system from the deeper, upper Central Basin aquifer system. A regional ground-water divide, approximately coinciding with the Duck River-Elk River drainage divide, underlies AAFB and runs from southwest to northeast. The general direction of most ground-water flow is to the north- west or to the northwest or to the southeast from the divide towards tributary streams that drain the area. Recharge estimates range from 4 to 11 inches per year. Digital computer modeling was used to simulate and provide a better understanding of the ground-water flow system. The model indicates that most of the ground-water flow occurs in the shallow and Manchester aquifers. The model was most sensitive to increases in hydraulic conductivity and changes in recharge rates. Particle-tracking analysis from selected sites of ground-water contamination indicates a potential for contami- nants to be transported beyond the boundary of AAFB.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nEarth Science Information Center Open-File Reports Section [distributor],","doi":"10.3133/wri934207","usgsCitation":"Haugh, C., and Mahoney, E., 1994, Hydrogeology and simulation of ground-water flow at Arnold Air Force Base, Coffee and Franklin counties, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 93-4207, vi, 69 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934207.","productDescription":"vi, 69 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4207/report-thumb.jpg"},{"id":56437,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62531e","contributors":{"authors":[{"text":"Haugh, C.J.","contributorId":24380,"corporation":false,"usgs":true,"family":"Haugh","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":198363,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mahoney, E.N.","contributorId":75171,"corporation":false,"usgs":true,"family":"Mahoney","given":"E.N.","email":"","affiliations":[],"preferred":false,"id":198364,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2680,"text":"wsp2432 - 1994 - Estimation of peak-frequency relations, flood hydrographs, and volume-duration-frequency relations of ungaged small urban streams in Ohio","interactions":[],"lastModifiedDate":"2023-01-09T20:36:33.36204","indexId":"wsp2432","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"2432","title":"Estimation of peak-frequency relations, flood hydrographs, and volume-duration-frequency relations of ungaged small urban streams in Ohio","docAbstract":"Methods and step-by-step examples are presented to estimate (1) peak-frequency relations, (2) flood hydrographs and volumes, and (3) volume-duration frequency relations of small urban streams in Ohio. The methods were developed to assist planners in the design of hydraulic structures for which hydrograph routing is required or where the temporary storage of water is an important element of the design criteria. 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,{"id":19227,"text":"ofr94468 - 1994 - A data input program (MFI) for the U.S. Geological Survey modular finite-difference ground-water flow model","interactions":[],"lastModifiedDate":"2012-02-02T00:07:32","indexId":"ofr94468","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"94-468","title":"A data input program (MFI) for the U.S. Geological Survey modular finite-difference ground-water flow model","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS ESIC--Open-File Report Section [distributor],","doi":"10.3133/ofr94468","usgsCitation":"Harbaugh, A.W., 1994, A data input program (MFI) for the U.S. Geological Survey modular finite-difference ground-water flow model: U.S. Geological Survey Open-File Report 94-468, vi, 24 p. ;28 cm., https://doi.org/10.3133/ofr94468.","productDescription":"vi, 24 p. ;28 cm.","costCenters":[],"links":[{"id":151383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0468/report-thumb.jpg"},{"id":48687,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0468/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af5fa","contributors":{"authors":[{"text":"Harbaugh, Arlen W. harbaugh@usgs.gov","contributorId":426,"corporation":false,"usgs":true,"family":"Harbaugh","given":"Arlen","email":"harbaugh@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":180522,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18899,"text":"ofr9445 - 1994 - Calculation of a water budget and delineation of contributing sources to drainflows in the western San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2022-09-08T20:53:17.746682","indexId":"ofr9445","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"94-45","title":"Calculation of a water budget and delineation of contributing sources to drainflows in the western San Joaquin Valley, California","docAbstract":"<p>Geohydrologic data and a ground-water flow model were used to calculate a water budget and evaluate the contribution of regional groundwater flow to on-farm drainflow in a part of the western San Joaquin Valley, California. Regional ground-water flow is affected by the distribution of unconsolidated coarse- and fine-grained sediment. Predominantly coarse-grained sediment in the upslope areas results in a water table greater than 3 meters below land surface, but the low-lying areas are underlain by predominantly fine-grained sediments and have a water table within 3 meters of land surface. The vertical component of flow is downward in the upslope areas, but can be upward at some locations in the low-lying areas. </p><p>Results of model simulations indicate that about 18.5x10<sup>6</sup> cubic meters per year of drainflow originates as recharge within the fields that overlay the drainage systems (89 percent), and 2.3x10<sup>6</sup> cubic meters per year of drainflow is lateral-flowing ground water and upward-moving deep percolation originating as recharge within fields upslope of the drainage systems (11 percent). The drainage systems that intercept this upslope recharge overlay predominantly coarse-grained sediment associated with old stream channels. This ground water can move upward from depths greater than 29 meters below land surface and distances as great as 3.6 kilometers, requiring from 10 to more than 90 years to reach the drainage systems.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr9445","usgsCitation":"Fio, J.L., 1994, Calculation of a water budget and delineation of contributing sources to drainflows in the western San Joaquin Valley, California: U.S. Geological Survey Open-File Report 94-45, v, 39 p., https://doi.org/10.3133/ofr9445.","productDescription":"v, 39 p.","costCenters":[],"links":[{"id":406406,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12447.htm","linkFileType":{"id":5,"text":"html"}},{"id":48300,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0045/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"western San Joaquin Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.821,\n              36.713\n            ],\n            [\n              -120.5,\n              36.713\n            ],\n            [\n              -120.5,\n              36.949\n            ],\n            [\n              -120.821,\n              36.949\n            ],\n            [\n              -120.821,\n              36.713\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e74b2","contributors":{"authors":[{"text":"Fio, John L.","contributorId":77543,"corporation":false,"usgs":true,"family":"Fio","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":179944,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19064,"text":"ofr94626 - 1994 - Topographic data requirements for EOS global change research","interactions":[],"lastModifiedDate":"2017-03-28T11:50:59","indexId":"ofr94626","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"94-626","title":"Topographic data requirements for EOS global change research","docAbstract":"<p>This document is a result of Earth Observing System Data and Information System (EOSDIS) Version 0 activities of the Land Processes Distributed Active Archive Center at the U.S. Geological Survey's EROS Data Center. A relatively small part of the Version 0 funding provided by NASA is used to address topographic data issues related to EOS. These issues include identifying and improving access to existing sources of topographic data, data generation, facilitating the use of topographic data in global change research by demonstrating derivative products, and inventorying the specific topographic data requirements of EOS investigators. </p><p>There is a clear need for global topographic data in EOSDIS. Only 10 percent of the global land surface is covered by high-resolution data that are available to the global change science community. Alternative sources for new data exist or have been proposed; however, none of them alone can fulfill the data requirements by the launch of the first EOS platform in 4 years. There is no operational provider of all the source data that are required. Even if appropriate global source data existed, a concerted production effort would be necessary to ensure the existence of the requisite topographic data before EOS launch. Additionally, no funding from NASA or any other agency has been appropriated for a new mapping mission or for other means of data acquisition. </p><p>This effort to document requirements is an initial step toward understanding the severity of the data shortage. It is well beyond the scope of Version 0 funding and capabilities to provide the required data in the proper timeframe. The shortage of data and the lack of a plan for providing the necessary topographic data through EOSDIS in time for launch are issues that must be addressed by the EOS program. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94626","usgsCitation":"Gesch, D.B., 1994, Topographic data requirements for EOS global change research: U.S. Geological Survey Open-File Report 94-626, vi, 60 p., https://doi.org/10.3133/ofr94626.","productDescription":"vi, 60 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":48505,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0626/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151066,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0626/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62aa9e","contributors":{"authors":[{"text":"Gesch, Dean B. 0000-0002-8992-4933 gesch@usgs.gov","orcid":"https://orcid.org/0000-0002-8992-4933","contributorId":2956,"corporation":false,"usgs":true,"family":"Gesch","given":"Dean","email":"gesch@usgs.gov","middleInitial":"B.","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":180243,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44732,"text":"wri944126 - 1994 - Potential for, and possible effects of, artificial recharge in Carson Valley, Douglas County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:59","indexId":"wri944126","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"94-4126","title":"Potential for, and possible effects of, artificial recharge in Carson Valley, Douglas County, Nevada","docAbstract":"Rapid population growth in Carson Valley, west- central Nevada, requires a dependable municipal water source. Artificial recharge of aquifers using available flow of the Carson River is one way to increase the amount of water in underground storage and maintain a dependable ground-water supply. Ground water can be artificially recharged by routing excess surface water or, after proper treatment, routing wastewater to infiltration basins or injection wells. Withdrawal wells would remove stored water when needed. As a first step, maps showing areas in Carson Valley with high, low, moderate and unknown potential for artificial recharge were developed on the basis of the distribution of geologic units, depth to water, specific yield, infiltration rate, and location of natural recharge and discharge. For recharge by means of infiltration, areas totaling 5,700 acres have high potential, 23,900 acres have moderate potential, and 6,200 acres have low potential. For recharge through injection, areas totaling 7,800 acres have high potential and 43,500 acres have moderate potential; 23,000 acres have unknown potential because data are lacking on subsurface conditions. A ground-water-flow model was used to assess the possible results of artificial recharge. Simulations with no accompanying ground-water withdrawal show that, when recharge by injection is simulated near the valley floor, heads in the semiconfined aquifer increase over much of the valley, floor; only about 20 percent of the recharged water is stored in the aquifer after 5 years and as much as 80 percent is lost to streamflow and evapotranspiration. When recharge is simulated on the eastern side of the valley, 80 percent of the recharged water remains in storage after 5 years. When recharge is simulated near the valley floor, more water is lost to discharge than when recharge is on the eastern side of the valley. When recharge is applied for long periods without accompanying withdrawal, recharged water moves downgradient to discharge areas. The recharge water that discharges to the surface-water system could in turn replenish base flow of the Carson River and benefit downstream users.","language":"ENGLISH","doi":"10.3133/wri944126","usgsCitation":"Maurer, D.K., and Peltz, L.A., 1994, Potential for, and possible effects of, artificial recharge in Carson Valley, Douglas County, Nevada: U.S. Geological Survey Water-Resources Investigations Report 94-4126, 87 p.; 7 maps on 4 sheets : col. ; 37 x 27 cm., sheets 61 x 102 cm., folded in envelope 30 x 24 cm. , https://doi.org/10.3133/wri944126.","productDescription":"87 p.; 7 maps on 4 sheets : col. ; 37 x 27 cm., sheets 61 x 102 cm., folded in envelope 30 x 24 cm. ","costCenters":[],"links":[{"id":99323,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4126/report.pdf","size":"108","linkFileType":{"id":1,"text":"pdf"}},{"id":99324,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4126/plate-1.pdf","size":"5233","linkFileType":{"id":1,"text":"pdf"}},{"id":99325,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4126/plate-2.pdf","size":"5671","linkFileType":{"id":1,"text":"pdf"}},{"id":99326,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4126/plate-3.pdf","size":"6154","linkFileType":{"id":1,"text":"pdf"}},{"id":99327,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1994/4126/plate-4.pdf","size":"5942","linkFileType":{"id":1,"text":"pdf"}},{"id":167921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4126/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683327","contributors":{"authors":[{"text":"Maurer, Douglas K. dkmaurer@usgs.gov","contributorId":2308,"corporation":false,"usgs":true,"family":"Maurer","given":"Douglas","email":"dkmaurer@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":230334,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peltz, Lorri A.","contributorId":29401,"corporation":false,"usgs":true,"family":"Peltz","given":"Lorri","email":"","middleInitial":"A.","affiliations":[{"id":12701,"text":"US Geological Survey","active":true,"usgs":false}],"preferred":false,"id":230335,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26038,"text":"wri944067 - 1994 - Flow and salinity in West Neck Creek, Virginia, 1989-92, and salinity in North Landing River, North Carolina, 1991-92","interactions":[],"lastModifiedDate":"2023-04-10T19:17:52.874938","indexId":"wri944067","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"94-4067","title":"Flow and salinity in West Neck Creek, Virginia, 1989-92, and salinity in North Landing River, North Carolina, 1991-92","docAbstract":"<p>Flow and salinity were monitored during 1989-92 in West Neck Creek, Virginia, which provides a direct hydraulic connection between the brackish waters of Chesapeake Bay and the relatively fresh waters of Currituck Sound. During the 308 days for which data were available, flow was to the south 64 percent of the time, but 80 percent of the southward flows were less than 40 cubic feet per second. Flows ranged from 356 cubic feet per second to the south to 50 cubic feet per second to the north, and the highest flows were associated with precipitation events. Salinity ranged from less than 0.1 to 24.5 parts per thousand, and the highest salinities were observed during periods of sustained, high northerly winds. Salt transport ranged from 34,510 tons per day to the south to 302 tons per day to the north.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri944067","usgsCitation":"Bales, J., and Skrobialowski, S., 1994, Flow and salinity in West Neck Creek, Virginia, 1989-92, and salinity in North Landing River, North Carolina, 1991-92: U.S. Geological Survey Water-Resources Investigations Report 94-4067, iv, 36 p., https://doi.org/10.3133/wri944067.","productDescription":"iv, 36 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":54819,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4067/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":415525,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47966.htm","linkFileType":{"id":5,"text":"html"}},{"id":122771,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4067/report-thumb.jpg"}],"country":"United States","state":"North Carolina, Virginia","otherGeospatial":"North Landing River, West Neck Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.1,\n              36.5\n            ],\n            [\n              -76.1,\n              36.8333\n            ],\n            [\n              -76,\n              36.8333\n            ],\n            [\n              -76,\n              36.5\n            ],\n            [\n              -76.1,\n              36.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df4c2","contributors":{"authors":[{"text":"Bales, Jerad","contributorId":47390,"corporation":false,"usgs":true,"family":"Bales","given":"Jerad","affiliations":[],"preferred":false,"id":195687,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skrobialowski, S. C.","contributorId":99585,"corporation":false,"usgs":true,"family":"Skrobialowski","given":"S. C.","affiliations":[],"preferred":false,"id":195688,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17218,"text":"ofr94662 - 1994 - Hazard of earthquake-induced lateral-spread ground failure on the Central California Coast modeled from earth-science map data in a geographic information system","interactions":[],"lastModifiedDate":"2012-02-02T00:07:15","indexId":"ofr94662","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"94-662","title":"Hazard of earthquake-induced lateral-spread ground failure on the Central California Coast modeled from earth-science map data in a geographic information system","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94662","usgsCitation":"Pike, R.J., Bernknopf, R., Tinsley, J.C., and Mark, R.K., 1994, Hazard of earthquake-induced lateral-spread ground failure on the Central California Coast modeled from earth-science map data in a geographic information system: U.S. Geological Survey Open-File Report 94-662, 46 p. :ill., maps (1 col.) ;28 cm., https://doi.org/10.3133/ofr94662.","productDescription":"46 p. :ill., maps (1 col.) ;28 cm.","costCenters":[],"links":[{"id":149379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0662/report-thumb.jpg"},{"id":21652,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0662/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46365,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0662/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63f0c0","contributors":{"authors":[{"text":"Pike, Richard J. rpike@usgs.gov","contributorId":5753,"corporation":false,"usgs":true,"family":"Pike","given":"Richard","email":"rpike@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":175452,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bernknopf, R. L.","contributorId":46082,"corporation":false,"usgs":true,"family":"Bernknopf","given":"R. L.","affiliations":[],"preferred":false,"id":175454,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tinsley, J. C.","contributorId":65827,"corporation":false,"usgs":true,"family":"Tinsley","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":175455,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mark, R. K.","contributorId":32159,"corporation":false,"usgs":true,"family":"Mark","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":175453,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":66626,"text":"i2387 - 1994 - Geologic maps of the southwestern Puerto Rico Parguera to Guanica insular shelf","interactions":[],"lastModifiedDate":"2018-03-14T14:17:48","indexId":"i2387","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2387","title":"Geologic maps of the southwestern Puerto Rico Parguera to Guanica insular shelf","docAbstract":"<p>These maps describe the sediments and sedimentary environment of the southwestern Puerto Rico shelf (index). In addition to presenting new data, the maps summarize earlier geological investigations. </p><p>There are two morphological zones separated along a line extending southward from Punta Jorobaflo. The Parguera shelf extends from this line to the western boundary of the study area, and the Guanica shelf extends from Punta Jorobado to the eastern study limit (fig. 1). The age and character of the underlying limestone bedrock, the depositional environment, the history of subaerial erosion, and the intensity of modem physical processes differ in each of these shelf areas. However, the bedrock surface of both the Parquera and Guanica shelves is primarily karst; the limestone surface was modified by reef growth and sediment deposition after the last glacial lowstand. Although several anticlines and faults that trend parallel to the shoreline have been mapped on the adjacent land areas (Volckmann, 1984), no evidence was found to suggest major structural features on the shelf.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2387","usgsCitation":"Morelock, J., Winget, E.A., and Goenaga, C., 1994, Geologic maps of the southwestern Puerto Rico Parguera to Guanica insular shelf: U.S. Geological Survey IMAP 2387, 4 maps :col. ;35 x 66 cm. and smaller on sheet 147 x 102 cm., folded in envelope 30 x 24 cm. +1 pamphlet (6 p. ; 28 cm.), https://doi.org/10.3133/i2387.","productDescription":"4 maps :col. ;35 x 66 cm. and smaller on sheet 147 x 102 cm., folded in envelope 30 x 24 cm. +1 pamphlet (6 p. ; 28 cm.)","costCenters":[],"links":[{"id":91583,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/2387/report.pdf","text":"Report","size":"710 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":107407,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10263.htm","linkFileType":{"id":5,"text":"html"},"description":"10263"},{"id":189615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2387/report-thumb.jpg"}],"scale":"40000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -67.11749999999999,17.850833333333334 ], [ -67.11749999999999,17.984166666666667 ], [ -66.86749999999999,17.984166666666667 ], [ -66.86749999999999,17.850833333333334 ], [ -67.11749999999999,17.850833333333334 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c527","contributors":{"authors":[{"text":"Morelock, Jack","contributorId":27145,"corporation":false,"usgs":true,"family":"Morelock","given":"Jack","email":"","affiliations":[],"preferred":false,"id":274816,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winget, Elizabeth A.","contributorId":38165,"corporation":false,"usgs":true,"family":"Winget","given":"Elizabeth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":274818,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goenaga, Carlos","contributorId":32569,"corporation":false,"usgs":true,"family":"Goenaga","given":"Carlos","email":"","affiliations":[],"preferred":false,"id":274817,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30174,"text":"wri934231 - 1994 - Nutrients, suspended sediment, and pesticides in waters of the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-90","interactions":[],"lastModifiedDate":"2023-03-31T18:31:40.4718","indexId":"wri934231","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"93-4231","title":"Nutrients, suspended sediment, and pesticides in waters of the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-90","docAbstract":"<p>Available data on nutrients (phosphorus and nitrogen), suspended sediment, and pesticides in the Red River of the North Basin, a study unit under the U.S. Geological Survey National Water-Quality Assessment (NAWQA) Program, are reviewed. These data were collected by several agencies during 1970-90. Nutrient concentrations in surface water are higher downgradient from agricultural and urban areas than in other areas, but generally do not exceed U.S. Environmental Protection Agency (USEPA) Maximum Contaminant Levels (MCLs). The 10 milligram per liter (mg/L) drinking water MCL for nitrate (as nitrogen) was rarely exceeded. Some of the largest nutrient inputs to the surface-water system appear to come from the Fargo-Moorhead area. The highest nitrogen concentrations usually were found in the Red River of the North. Nitrogen composition was mostly organic nitrogen with some nitrate. Ammonia nitrogen was negligible except during mid-winter, when concentrations could exceed 1.0 mg/L. Streams draining the corn-dominated cropland in the southern part of the basin had relatively high nitrogen concentrations compared to parts of the basin where small-grain crops, forests, and wetlands predominate. The Pembina River in the northern part of the basin had a large range in nitrogen concentrations that often exceeded those in the Red River of the North. The highest phosphorus concentrations generally were found in of the Red River of the North, although tributary streams occasionally had peak concentrations that exceeded those in the Red River of the North. Median nitrate concentrations in ground water were less than 1.0 mg/L as nitrogen in all counties in the basin except in Otter Tail and Decker Counties in Minnesota. Half of the wells in Otter Tail County had nitrate-nitrogen concentrations exceeding 2.8 mg/L. Shallow, surficial aquifers tended to have the highest nitrate concentrations.</p>\n<p>Median suspended-sediment concentrations were less than 100 mg/L except in the Red River of the North near the Canadian border at Emerson, Manitoba and the Pembina River. The Pembina River occasionally had high suspended sediment concentrations; about 10 percent of the samples exceeded 2,000 mg/L.</p>\n<p>For both surface and ground water, available pesticide data were limited in spatial and temporal coverage. The majority of pesticide analyses for the Red River of the North Basin show no concentrations above laboratory reporting limits. Reported concentrations usually were below USEPA MCLs. Only a few analyses of pesticides in ground water had concentrations above laboratory reporting limits. Wells that had reportable levels are mainly in the southern and southeastern part of the basin, where atrazine was the most commonly detected pesticide.</p>\n<p>A relatively large fraction of stream samples had detectable quantities of 2,4-D, a- and y-HCH, and atrazine. These samples covered time spans of as much as 15 years and were from sites downstream from large drainage basins; however, concentrations were well below US EPA MCLs. One county-level study showed higher 2,4-D concentrations at upstream sites than at the outlet from a small basin. This indicates that downstream sites may fail to show impaired water-quality and the fate of pesticides used in the basin. Following the 1972 ban on DDT, concentrations of DDT in fish samples from the Red River of the North quickly decreased. Fish concentrations of DDE and DDD decreased more slowly. Low levels of DDE and DDD were detected in fish 14 years after the DDT ban.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/wri934231","usgsCitation":"Tornes, L., and Brigham, M.E., 1994, Nutrients, suspended sediment, and pesticides in waters of the Red River of the North Basin, Minnesota, North Dakota, and South Dakota, 1970-90: U.S. Geological Survey Water-Resources Investigations Report 93-4231, viii, 62 p., https://doi.org/10.3133/wri934231.","productDescription":"viii, 62 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"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":415017,"rank":3,"type":{"id":36,"text":"NGMDB Index 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,{"id":44746,"text":"wri934190 - 1994 - Estimated freshwater withdrawals in Texas, 1990","interactions":[],"lastModifiedDate":"2016-08-16T13:33:21","indexId":"wri934190","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"93-4190","title":"Estimated freshwater withdrawals in Texas, 1990","docAbstract":"<p>This report presents 1990 freshwater withdrawal estimates for Texas by source and category. Withdrawal source is either ground water or surface water. Withdrawal categories include: self-supplied irrigation, thermoelectric-power generation, water supply, industrial and mining, and other (domestic, commercial, livestock). Withdrawal data are aggregated by county, major aquifer, and principal river basin. Only the four major categories of irrigation, thermoelectric-power generation, water supply, and industrial and mining are illustrated in this report, although all data are tabulated.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri934190","collaboration":"Prepared in cooperation with the Texas Water Development Board","usgsCitation":"Lurry, D.L., 1994, Estimated freshwater withdrawals in Texas, 1990: U.S. Geological Survey Water-Resources Investigations Report 93-4190, 2 Plates: 35.00 x 24.70 inches and 35.00 x 24.63 inches, https://doi.org/10.3133/wri934190.","productDescription":"2 Plates: 35.00 x 24.70 inches and 35.00 x 24.63 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":18580,"text":"ofr94580 - 1994 - Listing of geochemical data and assessment of variability for soils and alfalfa of the Uncompahgre Project Area, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:29","indexId":"ofr94580","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"94-580","title":"Listing of geochemical data and assessment of variability for soils and alfalfa of the Uncompahgre Project Area, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94580","usgsCitation":"Crock, J., Stewart, K.C., and Severson, R.C., 1994, Listing of geochemical data and assessment of variability for soils and alfalfa of the Uncompahgre Project Area, Colorado: U.S. Geological Survey Open-File Report 94-580, 83 leaves :ill., maps ;28 cm., https://doi.org/10.3133/ofr94580.","productDescription":"83 leaves :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151868,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0580/report-thumb.jpg"},{"id":47929,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0580/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4eed","contributors":{"authors":[{"text":"Crock, J.G.","contributorId":58236,"corporation":false,"usgs":true,"family":"Crock","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":179379,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, K. C.","contributorId":46519,"corporation":false,"usgs":true,"family":"Stewart","given":"K.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":179378,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Severson, R. C.","contributorId":46498,"corporation":false,"usgs":true,"family":"Severson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":179377,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26589,"text":"wri934229 - 1994 - Assessment of selected constituents in surface water of the upper Snake River basin, Idaho and western Wyoming, water years 1975-89","interactions":[],"lastModifiedDate":"2013-11-22T14:24:17","indexId":"wri934229","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"93-4229","title":"Assessment of selected constituents in surface water of the upper Snake River basin, Idaho and western Wyoming, water years 1975-89","docAbstract":"In 1991, a water-quality investigation of \nthe upper Snake River Basin was initiated as part \nof the U.S. Geological Survey's National Water-Quality Assessment Program. The initial task of \nthe assessment was to compile and analyze available nutrient, suspended sediment, and pesticide \ndata collected in the basin. For analysis of nutrients \nand suspended sediment, data collected during \nwater years 1980-89 were used. For pesticides, an \nadditional 5 years of data were included for a total \nassessment period encompassing water years \n1975-89.\nNearly 9,000 analyses of nutrients and suspended sediment from more than 450 stations were \nretrieved from the U.S. Environmental Protection \nAgency STORET and U.S. Geological Survey \nWATSTORE data bases. Nineteen stations had \nsufficient analyses for quantitative assessment. Of \nthe 19 stations analyzed, 4 are located on relatively \nunaffected stream reaches, 8 are at or near mouths \nof tributary basins affected by agricultural activities, and 7 are on the main stem of the Snake River.\nData indicate that nitrite plus nitrate and total \nphosphorus concentrations generally increased in a \ndownstream direction along the Snake River; concentrations were largest at the mouths of drainage \nbasins tributary to the Snake River. Water-quality \nstations were categorized as unaffected or minimally affected, agriculturally affected, or main \nstem to compare nutrient concentrations between \ndrainage basins of differing land use/land cover. \nConcentrations of nitrite plus nitrate, total nitrogen, \ndissolved orthophosphate, and total phosphorus \nwere significantly (p<0.05) larger at agriculturally\naffected and main-stem stations than at unaffected \nstations; and concentrations of nitrite plus nitrate, \ntotal nitrogen, and total phosphorus at agriculturally affected stations were significantly larger than \nat main-stem stations. Significant differences in \nseasonal concentrations of some nutrient species \nalso were noted.\nFew suspended sediment and pesticide data \nwere available for the study basin. Only six stations \nhad sufficient data for quantitative assessment of \nsuspended sediment. A direct positive relation \nexists between suspended sediment concentration \nand streamflow; concentrations are largest in April, \nMay, and June at high streamflow. Most of the \npesticide data compiled from STORET and \nWATSTORE were collected during water years \n1975-79. Only 33 pesticide samples, excluding \nsamples collected for a Rural Clean Water \nProgram, were collected from surface water and \nbottom sediment during water years 1980-89. \nBottom sediment collected near the mouth of the \nHenrys Fork during the late 1970's had the largest \nconcentrations of pesticides in the basin; DOT, \nODD, and DDE concentrations exceeded 10 micrograms per kilogram.\nMass movement of nutrients and suspended \nsediment in the upper Snake River Basin is \ncontrolled primarily by changes in streamflow. \nBetween two and three times as much total nitrogen, total phosphorus, and suspended sediment \nwere transported out of the basin in water year \n1984 (high-flow year) compared with 1989 (low-flow year). Reservoirs on the main stem of the \nSnake River probably trap much of the nutrient and \nmost of the suspended sediment load generated \nfrom upper parts of the basin.\nA more extensive data-collection program in \nthe upper Snake River Basin is needed to address a \nnumber of water-quality issues. These include \nan analysis of effects of land use on the quality of \nsurface water; quantification of mass movement of \nnutrients and suspended sediment at key locations \nin the basin; distribution of aquatic organisms; and \ntemporal and spatial distribution of pesticides in \nsurface water, bottom sediment, and biota.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri934229","usgsCitation":"Clark, G.M., 1994, Assessment of selected constituents in surface water of the upper Snake River basin, Idaho and western Wyoming, water years 1975-89: U.S. Geological Survey Water-Resources Investigations Report 93-4229, v, 49 p., https://doi.org/10.3133/wri934229.","productDescription":"v, 49 p.","numberOfPages":"54","temporalStart":"1975-01-01","temporalEnd":"1989-12-31","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":123540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4229/report-thumb.jpg"},{"id":55458,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4229/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","projection":"Albers Equal-Area projection","country":"United States","state":"Idaho;Montana;Nevada;Utah;Wyoming","otherGeospatial":"Snake River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.0,41.5 ], [ -115.0,45.0 ], [ -110.0,45.0 ], [ -110.0,41.5 ], [ -115.0,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6697d7","contributors":{"authors":[{"text":"Clark, Gregory M. gmclark@usgs.gov","contributorId":1377,"corporation":false,"usgs":true,"family":"Clark","given":"Gregory","email":"gmclark@usgs.gov","middleInitial":"M.","affiliations":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"preferred":true,"id":196666,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26147,"text":"wri944042 - 1994 - Relation of stream quality to streamflow, and estimated loads of selected water-quality constituents in the James and Rappahannock rivers near the fall line of Virginia, July 1988 through June 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:08:34","indexId":"wri944042","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"94-4042","title":"Relation of stream quality to streamflow, and estimated loads of selected water-quality constituents in the James and Rappahannock rivers near the fall line of Virginia, July 1988 through June 1990","docAbstract":"This report presents the results of a study by the U.S. Geological Survey, in cooperation with the Virginia Department of Environmental Quality-- Division of Intergovernmental Coordination to monitor and estimate loads of selected nutrients and suspended solids discharged to Chesapeake Bay from two major tributaries in Virginia. From July 1988 through June 1990, monitoring consisted of collecting depth-integrated, cross-sectional samples from the James and Rappahannock Rivers during storm- flow conditions and at scheduled intervals. Water- quality constituents that were monitored included total suspended solids (residue, total at 105 degrees Celsius), dissolved nitrite plus nitrate, dissolved ammonia, total Kjeldahl nitrogen (ammonia plus organic), total nitrogen, total phosphorus, dissolved orthopohosphorus, total organic carbon, and dissolved silica. Daily mean load estimates of each constituent were computed by month, using a seven-parameter log-linear-regression model that uses variables of time, discharge, and seasonality. Water-quality data and constituent- load estimates are included in the report in tabular and graphic form. The data and load estimates provided in this report will be used to calibrate the computer modeling efforts of the Chesapeake Bay region, evaluate the water quality of the Bay and the major effects on the water quality, and assess the results of best-management practices in Virginia.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944042","usgsCitation":"Belval, D., Campbell, J., and Woodside, M.D., 1994, Relation of stream quality to streamflow, and estimated loads of selected water-quality constituents in the James and Rappahannock rivers near the fall line of Virginia, July 1988 through June 1990: U.S. Geological Survey Water-Resources Investigations Report 94-4042, vi, 85 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944042.","productDescription":"vi, 85 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158325,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4042/report-thumb.jpg"},{"id":54941,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4042/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686512","contributors":{"authors":[{"text":"Belval, D.L.","contributorId":52186,"corporation":false,"usgs":true,"family":"Belval","given":"D.L.","affiliations":[],"preferred":false,"id":195899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, J.P.","contributorId":80310,"corporation":false,"usgs":true,"family":"Campbell","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":195900,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Woodside, M. D.","contributorId":98722,"corporation":false,"usgs":true,"family":"Woodside","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":195901,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25796,"text":"wri944138 - 1994 - A technique for estimating ground-water levels at sites in Rhode Island from observation-well data","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"wri944138","displayToPublicDate":"1995-03-01T00:00:00","publicationYear":"1994","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":"94-4138","title":"A technique for estimating ground-water levels at sites in Rhode Island from observation-well data","docAbstract":"Estimates of future high, median, and low ground- water levels are needed for engineering and architectural design decisions and for appropriate selection of land uses. For example, the failure of individual underground sewage-disposal systems due to high ground-water levels can be prevented if accurate water-level estimates are available. Estimates of extreme or average conditions are needed because short duration preconstruction obser- vations are unlikely to be adequately represen- tative. Water-level records for 40 U.S. Geological Survey observation wells in Rhode Island were used to describe and interpret water-level fluctuations. The maximum annual range of water levels average about 6 feet in sand and gravel and 11 feet in till. These data were used to develop equations for estimating future high, median, and low water levels on the basis of any one measurement at a site and records of water levels at observation wells used as indexes. The estimating technique relies on several assumptions about temporal and spatial variations: (1) Water levels will vary in the future as they have in the past, (2) Water levels fluctuate seasonally (3) Ground-water fluctuations are dependent on site geology, and (4) Water levels throughout Rhode Island are subject to similar precipitation and climate. Comparison of 6,697 estimates of high, median, and low water levels (depth to water level exceeded 95, 50, and 5 percent of the time, respectively) with the actual measured levels exceeded 95, 50, and 5 percent of the time at 14 sites unaffected by pumping and unknown reasons, yielded mean squared errors ranging from 0.34 to 1.53 square feet, 0.30 to 1.22 square feet, and 0.32 to 2.55 square feet, respectively. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri944138","usgsCitation":"Socolow, R.S., Frimpter, M.H., Turtora, M., and Bell, R.W., 1994, A technique for estimating ground-water levels at sites in Rhode Island from observation-well data: U.S. Geological Survey Water-Resources Investigations Report 94-4138, iv, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944138.","productDescription":"iv, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118721,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_94_4138.jpg"},{"id":2047,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri944138/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5cc5","contributors":{"authors":[{"text":"Socolow, Roy S.","contributorId":65070,"corporation":false,"usgs":true,"family":"Socolow","given":"Roy","email":"","middleInitial":"S.","affiliations":[{"id":376,"text":"Massachusetts Water Science Center","active":true,"usgs":true}],"preferred":false,"id":195113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frimpter, Michael H.","contributorId":8074,"corporation":false,"usgs":true,"family":"Frimpter","given":"Michael","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":195111,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turtora, Michael mturtora@usgs.gov","contributorId":4260,"corporation":false,"usgs":true,"family":"Turtora","given":"Michael","email":"mturtora@usgs.gov","affiliations":[{"id":270,"text":"FLWSC-Tampa","active":true,"usgs":true}],"preferred":true,"id":195110,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bell, Richard W.","contributorId":44141,"corporation":false,"usgs":true,"family":"Bell","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":195112,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":18549,"text":"ofr94668 - 1994 - Digital data for quantitative geochemistry of rocks from the Adelaide Mining District, Humboldt County, Nevada","interactions":[],"lastModifiedDate":"2013-09-18T07:34:13","indexId":"ofr94668","displayToPublicDate":"1995-02-01T00:00:00","publicationYear":"1994","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":"94-668","title":"Digital data for quantitative geochemistry of rocks from the Adelaide Mining District, Humboldt County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94668","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Cookro, T.M., 1994, Digital data for quantitative geochemistry of rocks from the Adelaide Mining District, Humboldt County, Nevada: U.S. Geological Survey Open-File Report 94-668, 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr94668.","productDescription":"1 computer disk ;3 1/2 in.","costCenters":[],"links":[{"id":151457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":277759,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1994/0668/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d525","contributors":{"authors":[{"text":"Cookro, Theresa M.","contributorId":47808,"corporation":false,"usgs":true,"family":"Cookro","given":"Theresa","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":179323,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20361,"text":"ofr94405 - 1994 - Analytical data-management systems; 1, Data management strategy for geological databases","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr94405","displayToPublicDate":"1995-02-01T00:00:00","publicationYear":"1994","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":"94-405","title":"Analytical data-management systems; 1, Data management strategy for geological databases","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94405","usgsCitation":"O’Connor, J.T., 1994, Analytical data-management systems; 1, Data management strategy for geological databases: U.S. Geological Survey Open-File Report 94-405, 33 leaves ;28 cm., https://doi.org/10.3133/ofr94405.","productDescription":"33 leaves ;28 cm.","costCenters":[],"links":[{"id":153120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0405/report-thumb.jpg"},{"id":49893,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0405/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f92b","contributors":{"authors":[{"text":"O’Connor, J. T.","contributorId":92266,"corporation":false,"usgs":true,"family":"O’Connor","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":182517,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20362,"text":"ofr94406 - 1994 - Analytical data-management systems; 2, Normalization, atomicity, and structure of geosciences data","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr94406","displayToPublicDate":"1995-02-01T00:00:00","publicationYear":"1994","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":"94-406","title":"Analytical data-management systems; 2, Normalization, atomicity, and structure of geosciences data","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94406","usgsCitation":"O’Connor, J.T., 1994, Analytical data-management systems; 2, Normalization, atomicity, and structure of geosciences data: U.S. Geological Survey Open-File Report 94-406, 19 leaves ;28 cm., https://doi.org/10.3133/ofr94406.","productDescription":"19 leaves ;28 cm.","costCenters":[],"links":[{"id":153138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0406/report-thumb.jpg"},{"id":49894,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0406/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f932","contributors":{"authors":[{"text":"O’Connor, J. T.","contributorId":92266,"corporation":false,"usgs":true,"family":"O’Connor","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":182518,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19108,"text":"ofr94377 - 1994 - Hydrologic data for the Puerco River basin, western New Mexico, October 1, 1991, through September 30, 1992","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr94377","displayToPublicDate":"1995-02-01T00:00:00","publicationYear":"1994","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":"94-377","title":"Hydrologic data for the Puerco River basin, western New Mexico, October 1, 1991, through September 30, 1992","docAbstract":"Hydrologic data collected during October 1, 1991, through September 30, 1992, in the Puerco River Basin, Western New Mexico, are summarized. The effects of uranium mining and a 1979 tailings pond spill, in combination with naturally occurring and potentially hazardous trace elements, have created a concern that surface water and ground water in the Puerco River Basin may be unsafe for irrigation, livestock watering, and domestic use; therefore, a data collection network was established to monitor the suitability of the water resources in the Puerco River Basin. The data collection network consisted of one streamflow-gaging station, three water-well dusters, and nine streambed sites. The network is located along a reach of the Puerco River beginning near the confluence of the Puerco River and Pipeline Arroyo and ending approximately 9 miles upstream from the New Mexico-Arizona State line. Data tabulated and presented include mean daily discharge, ground-water hydrographs, water quality, and sediment chemistry and particle-size distribution.","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division, [New Mexico District] ;\r\nCan be purchased from U.S. Geological Survey, Earth Science Information Center, Open-File Reports Section,","doi":"10.3133/ofr94377","usgsCitation":"Gold, R.L., and Rankin, D.R., 1994, Hydrologic data for the Puerco River basin, western New Mexico, October 1, 1991, through September 30, 1992: U.S. Geological Survey Open-File Report 94-377, iv, 33 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr94377.","productDescription":"iv, 33 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":150654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0377/report-thumb.jpg"},{"id":48544,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0377/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db6083cc","contributors":{"authors":[{"text":"Gold, Robert Louis","contributorId":13256,"corporation":false,"usgs":true,"family":"Gold","given":"Robert","email":"","middleInitial":"Louis","affiliations":[],"preferred":false,"id":180317,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rankin, Dale R.","contributorId":50924,"corporation":false,"usgs":true,"family":"Rankin","given":"Dale","email":"","middleInitial":"R.","affiliations":[{"id":472,"text":"New Mexico Water Science Center","active":true,"usgs":true}],"preferred":false,"id":180318,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31797,"text":"ofr94467 - 1994 - State water-data reports; hydrologic records of the United States water years 1990, 1991, 1992, and 1993","interactions":[{"subject":{"id":49683,"text":"ofr93626 - 1993 - State water-data reports; hydrologic records of the United States water years 1990, 1991, and 1992","indexId":"ofr93626","publicationYear":"1993","noYear":false,"title":"State water-data reports; hydrologic records of the United States water years 1990, 1991, and 1992"},"predicate":"SUPERSEDED_BY","object":{"id":31797,"text":"ofr94467 - 1994 - State water-data reports; hydrologic records of the United States water years 1990, 1991, 1992, and 1993","indexId":"ofr94467","publicationYear":"1994","noYear":false,"title":"State water-data reports; hydrologic records of the United States water years 1990, 1991, 1992, and 1993"},"id":1}],"lastModifiedDate":"2012-02-02T00:08:59","indexId":"ofr94467","displayToPublicDate":"1995-02-01T00:00:00","publicationYear":"1994","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":"94-467","title":"State water-data reports; hydrologic records of the United States water years 1990, 1991, 1992, and 1993","language":"ENGLISH","doi":"10.3133/ofr94467","usgsCitation":"Alt, D., 1994, State water-data reports; hydrologic records of the United States water years 1990, 1991, 1992, and 1993: U.S. Geological Survey Open-File Report 94-467, One CD-ROM. , https://doi.org/10.3133/ofr94467.","productDescription":"One CD-ROM. ","costCenters":[],"links":[{"id":160037,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e4490","contributors":{"authors":[{"text":"Alt, D.F.","contributorId":17653,"corporation":false,"usgs":true,"family":"Alt","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":206972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":31795,"text":"ofr94410 - 1994 - Preliminary bedrock geologic map of parts of the Lower Waterford, Concord, Littleton, and Miles Pond 7 1/2-minute quadrangles, Vermont and New Hampshire","interactions":[],"lastModifiedDate":"2022-03-28T21:52:31.230577","indexId":"ofr94410","displayToPublicDate":"1995-02-01T00:00:00","publicationYear":"1994","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":"94-410","title":"Preliminary bedrock geologic map of parts of the Lower Waterford, Concord, Littleton, and Miles Pond 7 1/2-minute quadrangles, Vermont and New Hampshire","docAbstract":"<p>The map area, in east-central Vermont and adjacent New Hampshire, consists of parts of the Lower Waterford, Concord, Littleton and Miles Pond 7 1/2-minute quadrangles (Fig. 1) that together constitute the Littleton 15-minute quadrangle. The mapping is part of the effort to produce a new bedrock geologic map of Vermont through the collection of field data at a scale of 1:24,000. The focus of my part of the project is to map and interpret the \"New Hampshire sequence\" rocks (White and Jahns, 1950) that crop out in Vermont and their relationship to those of the \"Vermont sequence\", or the Connecticut Valley trough, west of the Monroe line, here a fault (Hatch, 1988a). The work is a continuation of mapping just initiated by N.L. Hatch, Jr., prior to his death in 1991. This particular map area was chosen as the place to initiate this study because it includes one of the largest areas of the New Hampshire sequence in Vermont, because it is adjacent to and on strike with the Littleton-Moosilauke area in New Hampshire that includes the type area of most of the units of the New Hampshire sequence (Billings, 1935, 1937), and because the Connecticut River here runs roughly east to west across the regional strike and might provide a good stratigraphic section across the rocks under study. The mapping showed that no bedrock is exposed along either bank of the Connecticut River across most of the area, but there are excellent exposures in the spillways of two large dams, Moore Dam on the east and Comerford Dam on the west (about 100 m west of the Lower Waterford quadrangle), along Interstate Highway 93 (1-93), and adequate exposures in the hills above the river. My mapping was mostly in the Vermont parts of the Littleton 15-minute quadrangle but included some work in the Barnett 7 1/2 x 15-minute quadrangle to the west and a zone along the New Hampshire side of the Connecticut River that included Albee Hill, Partridge Lake, Highland Croft farm, the former Fitch farm, and the outskirts of Littleton. The Vermont mapping is thus tied to the classic Littleton-Moosilauke area of Billings (1937) and the fossiliferous Fitch and Littleton Formations in their type areas.</p>","conferenceTitle":"U.S. Geological Survey","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr94410","collaboration":"Prepared in cooperation with the State of Vermont","usgsCitation":"Rankin, D., 1994, Preliminary bedrock geologic map of parts of the Lower Waterford, Concord, Littleton, and Miles Pond 7 1/2-minute quadrangles, Vermont and New Hampshire: U.S. Geological Survey Open-File Report 94-410, Report: 28 p.; 3 Plates: 31.29 x 33.48 inches or smaller, https://doi.org/10.3133/ofr94410.","productDescription":"Report: 28 p.; 3 Plates: 31.29 x 33.48 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":310022,"rank":303,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0410/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":310021,"rank":302,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0410/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":310020,"rank":301,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1994/0410/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":60004,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0410/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0410/report-thumb.jpg"},{"id":397760,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19306.htm"}],"scale":"24000","country":"United States","state":"New Hampshire, Vermont","otherGeospatial":"Lower Waterford, Concord, Littleton, and Miles Pond 7 1/2-minute quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72,\n              44.31\n            ],\n            [\n              -71.792,\n              44.31\n            ],\n            [\n              -71.792,\n              44.455\n            ],\n            [\n              -72,\n              44.455\n            ],\n            [\n              -72,\n              44.31\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c99b","contributors":{"authors":[{"text":"Rankin, Douglas W. dwrankin@usgs.gov","contributorId":1770,"corporation":false,"usgs":true,"family":"Rankin","given":"Douglas W.","email":"dwrankin@usgs.gov","affiliations":[],"preferred":true,"id":206970,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17291,"text":"ofr94263 - 1994 - Lake Baikal, 1992; processing of multichannel seismic reflection data","interactions":[],"lastModifiedDate":"2012-02-02T00:07:20","indexId":"ofr94263","displayToPublicDate":"1995-02-01T00:00:00","publicationYear":"1994","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":"94-263","title":"Lake Baikal, 1992; processing of multichannel seismic reflection data","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr94263","usgsCitation":"Agena, W., Lee, M.W., Miller, J.J., and Hutchinson, D.R., 1994, Lake Baikal, 1992; processing of multichannel seismic reflection data: U.S. Geological Survey Open-File Report 94-263, 37 p. :chiefly ill., map ;28 cm., https://doi.org/10.3133/ofr94263.","productDescription":"37 p. :chiefly ill., map ;28 cm.","costCenters":[],"links":[{"id":150100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1994/0263/report-thumb.jpg"},{"id":46429,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1994/0263/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b441b","contributors":{"authors":[{"text":"Agena, Warren F.","contributorId":67079,"corporation":false,"usgs":true,"family":"Agena","given":"Warren F.","affiliations":[],"preferred":false,"id":175769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Myung W.","contributorId":84358,"corporation":false,"usgs":true,"family":"Lee","given":"Myung","middleInitial":"W.","affiliations":[],"preferred":false,"id":175770,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, J. J.","contributorId":54588,"corporation":false,"usgs":true,"family":"Miller","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":175768,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hutchinson, D. R.","contributorId":31770,"corporation":false,"usgs":true,"family":"Hutchinson","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":175767,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
]}