Shallow ground water may limit the location of construction and excavation projects in parts of the Front Range Urban Corridor. A shallow water table occurs from 0 to 50 feet below the land surface principally in the alluvial deposits along the streams and rivers in the Boulder-Fort Collins-Greeley area. This shallow water table underlies approximately 400 square miles and is maintained by natural recharge within the South Platte River basin and by the infiltration of irrigation water that is diverted into the basin from streams and reservoirs in the Colorado and the Laramie River basins. Return flow from irrigation, which is mostly ground water, helps maintain the flow of the South Platte River and its tributaries. The report includes a map from which depth to water table and the direction of ground-water movement can be determined. The map, compiled on a topographic base, shows the areal extent of the saturated materials and the altitude and configuration of the ground-water surface. The water-table contour map was prepared using data from approximately 400 wells. Monitoring of shallow ground-water within the study area shows depths to water have changed only slightly over the last 20 years, except for some seasonal and drought-related fluctuations. Gradients, computed from ground-water measurements, range from 27.7 feet per mile in Lone Tree-Spring Creek valley to 10.3 feet per mile in the South Platte River valley. The shallow ground-water underflow from the major tributaries in the basin is about 29,000 acre-feet per year, and underflow calculated at a cross section near Kersey is about 12,000 acre-feet per year.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834058","usgsCitation":"Schneider, P.A., 1983, Shallow ground water in the Boulder-Fort Collins-Greeley area, Front Range urban corridor, Colorado, 1975-77: U.S. Geological Survey Water-Resources Investigations Report 83-4058, 1 Plate: 41.96 × 31.86 inches, https://doi.org/10.3133/wri834058.","productDescription":"1 Plate: 41.96 × 31.86 inches","costCenters":[],"links":[{"id":161788,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410064,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35694.htm","linkFileType":{"id":5,"text":"html"}},{"id":84582,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4058/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","city":"Boulder, Fort Collins, Greeley","otherGeospatial":"Front Range urban corridor","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.46470339334677,\n 40.68848809489273\n ],\n [\n -105.46470339334677,\n 39.92665986663209\n ],\n [\n -104.58735150676397,\n 39.92665986663209\n ],\n [\n -104.58735150676397,\n 40.68848809489273\n ],\n [\n -105.46470339334677,\n 40.68848809489273\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f420a","contributors":{"authors":[{"text":"Schneider, Paul A. Jr.","contributorId":50183,"corporation":false,"usgs":true,"family":"Schneider","given":"Paul","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":235982,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28953,"text":"wri824092 - 1983 - Mean annual runoff and peak flow estimates based on channel geometry of streams in southeastern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri824092","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4092","title":"Mean annual runoff and peak flow estimates based on channel geometry of streams in southeastern Montana","docAbstract":"Equations using channel-geometry measurements were developed for estimating mean runoff and peak flows of ungaged streams in southeastern Montana. Two separate sets of esitmating equations were developed for determining mean annual runoff: one for perennial streams and one for ephemeral and intermittent streams. Data from 29 gaged sites on perennial streams and 21 gaged sites on ephemeral and intermittent streams were used in these analyses. Data from 78 gaged sites were used in the peak-flow analyses. Southeastern Montana was divided into three regions and separate multiple-regression equations for each region were developed that relate channel dimensions to peak discharge having recurrence intervals of 2, 5, 10, 25, 50, and 100 years. Channel-geometery relations were developed using measurements of the active-channel width and bankfull width. Active-channel width and bankfull width were the most significant channel features for estimating mean annual runoff for al types of streams. Use of this method requires that onsite measurements be made of channel width. The standard error of estimate for predicting mean annual runoff ranged from about 38 to 79 percent. The standard error of estimate relating active-channel width or bankfull width to peak flow ranged from about 37 to 115 percent. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824092","usgsCitation":"Omang, R.J., Parrett, C., and Hull, J.A., 1983, Mean annual runoff and peak flow estimates based on channel geometry of streams in southeastern Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4092, v, 38 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824092.","productDescription":"v, 38 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":120150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4092/report-thumb.jpg"},{"id":57829,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db61047f","contributors":{"authors":[{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":200675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parrett, Charles","contributorId":9635,"corporation":false,"usgs":true,"family":"Parrett","given":"Charles","email":"","affiliations":[],"preferred":false,"id":200674,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hull, J. A.","contributorId":39345,"corporation":false,"usgs":true,"family":"Hull","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200676,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10759,"text":"ofr83331 - 1983 - Reconnaissance geology of the Ghazzalah Quadrangle, sheet 26/41 A, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr83331","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-331","title":"Reconnaissance geology of the Ghazzalah Quadrangle, sheet 26/41 A, Kingdom of Saudi Arabia","docAbstract":"The Ghazzalah quadrangle is located in the northern Precambrian shield of Saudi Arabia between lat 26?30' and 27?00' N. and long 41?00' and 41?30' E. The area is underlain by two lithologically distinct, Precambrian volcanosedimentary units and a wide range of dioritoid and granitoid plutonic intrusive rocks. The only Phanerozoic rocks consist of one outcrop of Tertiary(?) basalt and widespread but thin deposits of Quaternary detritus. \r\n\r\nThe Banana greenstone, the oldest rock in the quadrangle, consists of intermediate volcanic and subvolcanic rocks and minor interbedded marble, which have been metamorphosed to greenschist-facies assemblages. Volcanic rocks mainly range in composition from basalt to andesite, and subvolcanic rocks consist of diorite and diabase. \r\n\r\nThe Banana greenstone is unconformably overlain by silicic volcanic rocks and minor arkosic sandstone and breccia of the Hadn formation. Preservation of delicate volcanic textures suggests that the rocks have been only incipiently metamorphosed. Unpublished rubidium/strontium isotopic data for the Hadn formation suggest an age of 620 to 610 Ma. \r\n\r\nIntrusive rocks are separable according to their ages relative to the Hadn formation. Those that are unconformably overlain by the Hadn formation consist of hornblende quartz diorite and gabbro, which may be consanguineous with the Banana greenstone, and younger tonalite, biotite-hornblende granodiorite, syenogranite, and monzogranite. Plutons of monzogranite, alkali-feldspar g,ranite, syenbgranite, peralkaline granite, and hypabyssal intrusions of granophyre were probably emplaced during a period coincident with and (or) following Hadn volcanism. Uranium-lead and rubidium/strontium isotopic data for two plutons in the adjacent Al Qasr quadrangle suggest that plutonic activity persisted in the region until about 580 to 570 Ma. \r\n\r\nFaulting appears to postdate all of the plutonic rocks. The dominant faults belong to a northeast-trending system of right-lateral shears; a subordinant system consists of mainly north- to northwest-trending faults.\r\n\r\nThe peralkaline-granite plutons underlying Jibal Ba'gham and Jibal ar Rumman have the most economic potential. Wadi samples from these areas show an anomalous concentrations of tin, lead, niobium, and yttrium. Localized, intense radiometric anomalies in the Ba'gham intrusive complex are associated with high concentrations )f thorium, uranium, andrare-earth elements.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83331","usgsCitation":"Quick, J.E., 1983, Reconnaissance geology of the Ghazzalah Quadrangle, sheet 26/41 A, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-331, 48 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83331.","productDescription":"48 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":143383,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0331/report-thumb.jpg"},{"id":38563,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0331/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38564,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0331/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38565,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0331/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38566,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0331/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60422c","contributors":{"authors":[{"text":"Quick, James E.","contributorId":21552,"corporation":false,"usgs":true,"family":"Quick","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161913,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18437,"text":"ofr83696 - 1983 - Long-range plans for hydrologic investigations in New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr83696","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-696","title":"Long-range plans for hydrologic investigations in New Mexico","docAbstract":"Objectives of the hydrologic-data-collection projects presented in this report include continuing to identify future data needs; conducting an analysis of the water-quality, ground-water, and surface-water observation networks; and entering all available current and historical hydrologic data into the U.S. Geological Survey Water Data Storage and Retrieval System (WATSTORE). Objectives of areal-appraisal studies include evaluating the water resources in the Gallup-Grants-Zuni-Acoma Sag area and on the eastern flank of the Sandi and Manzano Mountains in Bernalillo County. Potential projects for basin assessments include quantifying the ground-water/surface-water relationships on rivers with flows governed by compacts and an investigation of the water resources of the Estancia Basin. Projects that will assist in the evaluation of energy-related activities include describing the effects of resaturation of coal mines and of milling operations on the quality and quantity of ground and surface water. Activities that need to be undertaken to assist in addressing waste-disposal problems include the evaluation of the hydrologic factors influencing the feasibility of cleanup at the Albuquerque South Valley ' superfund ' site and the establishment of a monitoring network at the Waste Isolation Pilot Plant project near Carlsbad. Scientific methods that need to be developed include (1) the testing of analytical techniques for estimating site-specific conditions with the results of digital hydrologic models, and (2) the determination of the influence of recharge from ephemeral streams on alluvial aquifers. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83696","usgsCitation":"Case, H.L., and Welder, G.E., 1983, Long-range plans for hydrologic investigations in New Mexico: U.S. Geological Survey Open-File Report 83-696, iv, 29 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr83696.","productDescription":"iv, 29 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0696/report-thumb.jpg"},{"id":47788,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0696/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6352fb","contributors":{"authors":[{"text":"Case, H. L. III","contributorId":70435,"corporation":false,"usgs":true,"family":"Case","given":"H.","suffix":"III","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":179117,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welder, G. E.","contributorId":100814,"corporation":false,"usgs":true,"family":"Welder","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":179118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10768,"text":"ofr83240 - 1983 - Desktop computer processing of coincident and central loop time domain electromagnetic data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:24","indexId":"ofr83240","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-240","title":"Desktop computer processing of coincident and central loop time domain electromagnetic data","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83240","usgsCitation":"Raab, P., and Frischknecht, F.C., 1983, Desktop computer processing of coincident and central loop time domain electromagnetic data: U.S. Geological Survey Open-File Report 83-240, 43 p. ill. ;28 cm., https://doi.org/10.3133/ofr83240.","productDescription":"43 p. ill. ;28 cm.","costCenters":[],"links":[{"id":143513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0240/report-thumb.jpg"},{"id":38574,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0240/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667d01","contributors":{"authors":[{"text":"Raab, Paul","contributorId":73201,"corporation":false,"usgs":true,"family":"Raab","given":"Paul","email":"","affiliations":[],"preferred":false,"id":161931,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frischknecht, Frank C.","contributorId":57838,"corporation":false,"usgs":true,"family":"Frischknecht","given":"Frank","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":161930,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10776,"text":"ofr83421 - 1983 - Preliminary map of limonitic hydrothermal alteration for portions of the Needles 1° x 2° quadrangle, Arizona and California","interactions":[],"lastModifiedDate":"2022-11-02T18:42:12.871146","indexId":"ofr83421","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-421","title":"Preliminary map of limonitic hydrothermal alteration for portions of the Needles 1° x 2° quadrangle, Arizona and California","docAbstract":"Portions of the Needles quadrangle have been designated by the Bureau of Land Management as potential wilderness areas and are being evaluated by a multidisciplinary team to determine the mineral-resource potential. As a part of this study Landsat images are being used to map the generalized distribution of limonitic materials as a guide to hydrothermal alteration which, in turn, acts as a guide to mineralized systems. The term limonite, defined by Blanchard (1968) as a general term for hydrous iron oxides, is here modified to include any material with the unique spectral reflectance properties of the ferric oxide minerals such as hematite and goethite, as defined by Hunt (1980).
\nThe map shows areas of limonitic hydrothermal alteration but does not show hydrothermally altered areas lacking limonitic materials. Table 1 lists, for each hydrothermally altered area detected, the type of alteration and the anomalous trace-element geochemical suite found in that area.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83421","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Raines, G.L., 1983, Preliminary map of limonitic hydrothermal alteration for portions of the Needles 1° x 2° quadrangle, Arizona and California: U.S. Geological Survey Open-File Report 83-421, Report: 7 p.; 1 Plate: 32.47 × 26.82 inches, https://doi.org/10.3133/ofr83421.","productDescription":"Report: 7 p.; 1 Plate: 32.47 × 26.82 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":409069,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14042.htm","linkFileType":{"id":5,"text":"html"}},{"id":38580,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0421/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":38579,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0421/plate-1.pdf","text":"Map","linkFileType":{"id":1,"text":"pdf"},"description":"Map"},{"id":145071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0421/report-thumb.jpg"}],"scale":"250000","projection":"Transverse Mercator Projection","country":"United States","state":"Arizona, California","otherGeospatial":"Needles quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116,\n 35\n ],\n [\n -116,\n 34\n ],\n [\n -114,\n 34\n ],\n [\n -114,\n 35\n ],\n [\n -116,\n 35\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d825","contributors":{"authors":[{"text":"Raines, Gary L.","contributorId":48162,"corporation":false,"usgs":true,"family":"Raines","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161946,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10272,"text":"ofr83286 - 1983 - A hydrogeochemical survey in east-central Nevada","interactions":[],"lastModifiedDate":"2022-07-22T21:20:44.950179","indexId":"ofr83286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-286","title":"A hydrogeochemical survey in east-central Nevada","docAbstract":"A hydrogeochemical survey utilizing waters from springs and wells was conducted in east-central Nevada. None of the trace elements commonly associated with mineralization were found to be highly anomalous in the study area. Slightly anomalous values for some elements were found in the southern valleys of the study area and in a few scattered areas that contained old mines. Data from this study revealed no new areas of significant mineralization.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83286","usgsCitation":"McHugh, J., Miller, W.R., and Ficklin, W.H., 1983, A hydrogeochemical survey in east-central Nevada: U.S. Geological Survey Open-File Report 83-286, i, 28 p., https://doi.org/10.3133/ofr83286.","productDescription":"i, 28 p.","costCenters":[],"links":[{"id":404396,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13966.htm","linkFileType":{"id":5,"text":"html"}},{"id":38129,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0286/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0286/report-thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.49,\n 37.874\n ],\n [\n -114,\n 37.874\n ],\n [\n -114,\n 38.5\n ],\n [\n -114.49,\n 38.5\n ],\n [\n -114.49,\n 37.874\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae468","contributors":{"authors":[{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":161115,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. Roger","contributorId":60191,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"Roger","affiliations":[],"preferred":false,"id":161114,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ficklin, Walter H.","contributorId":52565,"corporation":false,"usgs":true,"family":"Ficklin","given":"Walter","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161113,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":21097,"text":"ofr83662 - 1983 - Geology and mineral resource potential map of the Mount Washington Wilderness, Deschutes, Lane, and Linn Counties, Oregon","interactions":[],"lastModifiedDate":"2022-02-02T19:46:35.207096","indexId":"ofr83662","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-662","title":"Geology and mineral resource potential map of the Mount Washington Wilderness, Deschutes, Lane, and Linn Counties, Oregon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83662","usgsCitation":"Taylor, E.M., Causey, J., and MacLeod, N.S., 1983, Geology and mineral resource potential map of the Mount Washington Wilderness, Deschutes, Lane, and Linn Counties, Oregon: U.S. Geological Survey Open-File Report 83-662, 20 p., https://doi.org/10.3133/ofr83662.","productDescription":"20 p.","costCenters":[],"links":[{"id":50686,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0662/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154550,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0662/report-thumb.jpg"},{"id":395297,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14162.htm"}],"country":"United States","state":"Oregon","county":"Deschutes County, Lane County, Linn County","otherGeospatial":"Mount Washington Wilderness","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.00592041015626,\n 44.213709909702054\n ],\n [\n -121.75323486328124,\n 44.213709909702054\n ],\n [\n -121.75323486328124,\n 44.38669150215206\n ],\n [\n -122.00592041015626,\n 44.38669150215206\n ],\n [\n -122.00592041015626,\n 44.213709909702054\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46ec","contributors":{"authors":[{"text":"Taylor, E. M.","contributorId":55842,"corporation":false,"usgs":true,"family":"Taylor","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":183834,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Causey, J. D.","contributorId":64652,"corporation":false,"usgs":true,"family":"Causey","given":"J. D.","affiliations":[],"preferred":false,"id":183835,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"MacLeod, N. S.","contributorId":55816,"corporation":false,"usgs":true,"family":"MacLeod","given":"N.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":183833,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":28866,"text":"wri834083 - 1983 - Flood elevations for the Soleduck River at Sol Duc Hot Springs, Clallam County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri834083","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4083","title":"Flood elevations for the Soleduck River at Sol Duc Hot Springs, Clallam County, Washington","docAbstract":"Elevations and inundation areas of a 100-year flood of the Soleduck River, Washington, were determined by the U.S. Geological Survey for the area in the vicinity of the Sol Duc Hot Springs resort, a public facility in the Olympic National Park that under Federal law must be located beyond or protected from damage by a 100-year flood. Results show that most flooding could be eliminated by raising parts of an existing dike. In general, little flood damage is expected, except at the southern end of an undeveloped airstrip that could become inundated and hazardous due to flow from a tributary. The airstrip is above the 100-year flood of the Soleduck River.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834083","usgsCitation":"Nelson, L.M., 1983, Flood elevations for the Soleduck River at Sol Duc Hot Springs, Clallam County, Washington: U.S. Geological Survey Water-Resources Investigations Report 83-4083, iii, 20 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834083.","productDescription":"iii, 20 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118932,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4083/report-thumb.jpg"},{"id":57746,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4083/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef25f","contributors":{"authors":[{"text":"Nelson, L. M.","contributorId":39773,"corporation":false,"usgs":true,"family":"Nelson","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":200527,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26478,"text":"wri824051 - 1983 - Potential effects of surface coal mining on the hydrology of the Snider Creek area, Rosebud and Ashland coal fields, southeastern Montana","interactions":[],"lastModifiedDate":"2024-01-11T17:50:15.788671","indexId":"wri824051","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4051","title":"Potential effects of surface coal mining on the hydrology of the Snider Creek area, Rosebud and Ashland coal fields, southeastern Montana","docAbstract":"The Snider Creek area of the Rosebud and Ashland coal fields contains strippable reserves of Federal coal that have been identified for potential lease sale. A hydrologic study has been conducted in the potential lease area to describe the existing hydrologic systems and to assess potential impacts of surface coal mining on local water resources. Hydrogeologic data collected from stock wells, observation wells, and drill holes indicate that shallow aquifers exist within the Tullock, Lebo Shale, and tongue River Members of the Fort Union Formation (Paleocene age) and within valley alluvium (Pleistocene and Holocene age). Most of the wells in the area are completed in the basal part of the Tongue River Member or in the upper part of the Lebo Shale Member and are used for watering of livestock. Small stock reservoirs are the primary source of surface water; Snider Creek and all other streams that originate in the area are ephemeral. The Terrett coal bed, the primary coal bed of the area, is located above the water table. Mining of the Terrett coal bed would destroy one stock well and several small reservoirs. Four other wells near the coal outcrop might be destroyed by mining. Alternative ground-water supplies are available to replace those lost by mining. Degradation of the quality of ground water, caused by the leaching of soluble salts from mine spoils, is not anticipated. (USGS)","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824051","usgsCitation":"Cannon, M.R., 1983, Potential effects of surface coal mining on the hydrology of the Snider Creek area, Rosebud and Ashland coal fields, southeastern Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4051, iv, 32 p., https://doi.org/10.3133/wri824051.","productDescription":"iv, 32 p.","costCenters":[],"links":[{"id":424339,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49152.htm","linkFileType":{"id":5,"text":"html"}},{"id":55300,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4051/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123644,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4051/report-thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Rosebud and Ashland coal fields, Snider Creek area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -106.25,\n 45.9333\n ],\n [\n -106.4,\n 45.9333\n ],\n [\n -106.4,\n 45.8611\n ],\n [\n -106.25,\n 45.8611\n ],\n [\n -106.25,\n 45.9333\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4ff","contributors":{"authors":[{"text":"Cannon, M. R.","contributorId":99140,"corporation":false,"usgs":true,"family":"Cannon","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":196460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10321,"text":"ofr82771 - 1983 - Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr82771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-771","title":"Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982","docAbstract":"The rockslide/debris avalanche from the north face of Mount St. Helens that precipitated the volcano 's eruption on May 18, 1980 , blocked outflow from Spirit Lake, Washington. There has been no surface outflow since that time. From May 21, 1980, when the first measurement of lake level was made, to August 1, 1982, Spirit Lake has increased its volume from 122,800 acre-ft to 264 ,000 acre-ft, an increase of 115%. Lake level has risen approximately 54 ft during this period. Hydrologic and geologic properties of the debris dam are unknown, but the materials obviously are easily erodible. Steep walled channels up to 60 ft deep have been eroded into the dam and are extending headward toward the lowest points on the crest. In addition, it appears that the lower areas on the crest of the dam are underlain by ash cloud deposits of low density. Indications are that the debris dam could fail by headward erosion, by overtopping with rapid downcutting, or by ' piping ' and rapid erosion. Each type of failure can produce rapid release of stored lake water with very high discharge rates. On the basis of observed filling rates of the lake over the last two yr and precipitation records at four long-term, low altitude National Weather Service stations, it is expected that normal precipitation will fill the lake to the dam crest in December 1985. This estimate is also based on the assumption that loss of water from the lake by seepage continues at the present rate until December 1985. With normal precipitation during the coming yr (August 1982 through July 1983 the lake will fill to a level 50 ft below the lowest existing point on the crest of the debris dam, which is at 3,532 ft altitude. If precipitation exceeds normal by 1.5 times during this coming year, the lake level will be 40 ft below the 3 ,532-ft crest of the debris dam by the end of July 1983. This same lake level can be reached by the end of March 1983 if precipitation from October through March is twice the winter mean. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82771","usgsCitation":"Meyer, W., and Carpenter, P.J., 1983, Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982: U.S. Geological Survey Open-File Report 82-771, iv, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82771.","productDescription":"iv, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0771/report-thumb.jpg"},{"id":38172,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0771/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f481e","contributors":{"authors":[{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":161195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carpenter, Philip J.","contributorId":85034,"corporation":false,"usgs":true,"family":"Carpenter","given":"Philip","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161194,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10564,"text":"ofr821013 - 1983 - Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","interactions":[{"subject":{"id":10564,"text":"ofr821013 - 1983 - Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","indexId":"ofr821013","publicationYear":"1983","noYear":false,"title":"Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":2420,"text":"wsp2227 - 1987 - Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico","indexId":"wsp2227","publicationYear":"1987","noYear":false,"title":"Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico"},"id":1}],"supersededBy":{"id":2420,"text":"wsp2227 - 1987 - Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico","indexId":"wsp2227","publicationYear":"1987","noYear":false,"title":"Water resources of the Zuni tribal lands, McKinley and Cibola Counties, New Mexico"},"lastModifiedDate":"2022-09-07T15:44:24.905824","indexId":"ofr821013","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-1013","title":"Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico","docAbstract":"An evaluation of the water resources of the Zuni Tribal lands in west-central New Mexico was made to determine the yield, variability, and quality of water available to the Pueblo of Zuni. This study is needed to aid in orderly development of these resources.
Rocks of Permian to Quaternary age supply stock, irrigation, and domestic water to the Zuni Indians. The Glorieta Sandstone and San Andres Limestone (Glorieta-San Andres aquifer) of Permian age and sandstones in the Chinle Formation of Triassic age provide most of this water supply.
Water in the Glorieta-San Andres aquifer is confined by minimal-permeability shales and is transmitted through the aquifer along interconnected solution channels and fractures. Water-level and water-quality information indicate greater hydraulic conductivities along the southern boundaries of Zuni Tribal lands.
Well yields from the Glorieta-San Andres aquifer are as much as 150 gallons per minute and aquifer transmissivity ranges from 30 to 1,400 feet squared per day. Long-term, water-level declines of as much as 29 feet have been measured near pumping centers at Black Rock. Multiple-well aquifer tests are needed to further define aquifer properties (storage, transmissivity, and leakage from confining units) and the effects of well design on well yields. Dissolved-solids concentrations in water from the aquifer ranged from 331 to 1,068 milligrams per liter. Calcium and sulfate are the predominant ions.
Water in sandstones of the Chinle Formation is confined by adjacent shales and is transmitted along interconnected fractures. Well yields range from 5 to 125 gallons per minute and aquifer transmissivity ranges from 40 to 1,400 feet squared per day. Water-level declines of as much as 27 feet have been measured near Zuni Village. Dissolved-solids concentrations in water from the aquifer ranged from 215 to 1,980 milligrams per liter. Sodium and bicarbonate are the predominant ions.
Other sources of ground water are used primarily for livestock watering by means of windmills, with the exception of buried alluvial channel deposits along the Rio Pescado. These deposits provide domestic and irrigation water through springs and wells to Pescado and Black Rock.
The Bidahochi Formation of Miocene and Pliocene age could potentially provide an additional supply of water chemically suitable for most uses. Seismic-reflection techniques are being used to locate buried channels eroded in the rocks underlying the Bidahochi Formation. These buried channels may contain thicker sections of saturated sands and gravels that could be developed for stock and domestic use.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821013","collaboration":"Prepared in cooperation with the Pueblo of Zuni","usgsCitation":"Orr, B.R., 1983, Water resources of the Zuni Tribal Lands, McKinley and Cibola counties, New Mexico: U.S. Geological Survey Open-File Report 82-1013, Report: 179 p.; 2 Plates: 23.21 x 19.52 inches and 20.83 x 30.61 inches, https://doi.org/10.3133/ofr821013.","productDescription":"Report: 179 p.; 2 Plates: 23.21 x 19.52 inches and 20.83 x 30.61 inches","costCenters":[],"links":[{"id":406315,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1013/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406314,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1013/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406313,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1013/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1013/report-thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Cibola County, McKinley County","otherGeospatial":"Zuni Tribal Lands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.061279296875,\n 34.134541681937364\n ],\n [\n -107.0068359375,\n 34.134541681937364\n ],\n [\n -107.0068359375,\n 35.96022296929667\n ],\n [\n -109.061279296875,\n 35.96022296929667\n ],\n [\n -109.061279296875,\n 34.134541681937364\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f03be","contributors":{"authors":[{"text":"Orr, Brennon R.","contributorId":18747,"corporation":false,"usgs":true,"family":"Orr","given":"Brennon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10565,"text":"ofr831 - 1983 - Chemical analyses of selected Tertiary and Quaternary volcanic rocks, Cascade Range, Washington","interactions":[{"subject":{"id":10565,"text":"ofr831 - 1983 - Chemical analyses of selected Tertiary and Quaternary volcanic rocks, Cascade Range, Washington","indexId":"ofr831","publicationYear":"1983","noYear":false,"title":"Chemical analyses of selected Tertiary and Quaternary volcanic rocks, Cascade Range, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":38465,"text":"pp1434 - 1988 - Landslides, Floods, and Marine Effects of the Storm of January 3-5, 1982, in the San Francisco Bay Region, California","indexId":"pp1434","publicationYear":"1988","noYear":false,"title":"Landslides, Floods, and Marine Effects of the Storm of January 3-5, 1982, in the San Francisco Bay Region, California"},"id":1}],"supersededBy":{"id":38465,"text":"pp1434 - 1988 - Landslides, Floods, and Marine Effects of the Storm of January 3-5, 1982, in the San Francisco Bay Region, California","indexId":"pp1434","publicationYear":"1988","noYear":false,"title":"Landslides, Floods, and Marine Effects of the Storm of January 3-5, 1982, in the San Francisco Bay Region, California"},"lastModifiedDate":"2012-02-02T00:06:28","indexId":"ofr831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-1","title":"Chemical analyses of selected Tertiary and Quaternary volcanic rocks, Cascade Range, Washington","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr831","usgsCitation":"Ort, K., Tabor, R.W., and Frizzell, V.A., 1983, Chemical analyses of selected Tertiary and Quaternary volcanic rocks, Cascade Range, Washington: U.S. Geological Survey Open-File Report 83-1, 15 p. ;28 cm., https://doi.org/10.3133/ofr831.","productDescription":"15 p. ;28 cm.","costCenters":[],"links":[{"id":144135,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0001/report-thumb.jpg"},{"id":38399,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0001/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4a1c","contributors":{"authors":[{"text":"Ort, K.M.","contributorId":17236,"corporation":false,"usgs":true,"family":"Ort","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":161601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tabor, R. W.","contributorId":16002,"corporation":false,"usgs":true,"family":"Tabor","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":161600,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frizzell, Virgil A.","contributorId":87934,"corporation":false,"usgs":true,"family":"Frizzell","given":"Virgil","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161602,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10260,"text":"ofr83396 - 1983 - Seismic-reflection data collected in the Baltimore Canyon and Cape Hatteras areas during 1982, Gyre cruise 82-G-10B","interactions":[],"lastModifiedDate":"2024-11-25T22:57:27.956903","indexId":"ofr83396","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-396","title":"Seismic-reflection data collected in the Baltimore Canyon and Cape Hatteras areas during 1982, Gyre cruise 82-G-10B","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83396","usgsCitation":"McGregor, B.A., 1983, Seismic-reflection data collected in the Baltimore Canyon and Cape Hatteras areas during 1982, Gyre cruise 82-G-10B: U.S. Geological Survey Open-File Report 83-396, 5 p., https://doi.org/10.3133/ofr83396.","productDescription":"5 p.","costCenters":[],"links":[{"id":143135,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0396/report-thumb.jpg"},{"id":368900,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0396/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":464510,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14008.htm","text":"Baltimore Canyon","linkFileType":{"id":5,"text":"html"}},{"id":464511,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14009.htm","text":"Cape Hatteras","linkFileType":{"id":5,"text":"html"}}],"country":"United States","otherGeospatial":"Baltimore Canyon, Cape Hatteras","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.514543627322,\n 38.37922375578077\n ],\n [\n -75.60111811259628,\n 38.37922375578077\n ],\n [\n -75.60111811259628,\n 35.36603278137427\n ],\n [\n -74.514543627322,\n 35.36603278137427\n ],\n [\n -74.514543627322,\n 38.37922375578077\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb627","contributors":{"authors":[{"text":"McGregor, Bonnie A.","contributorId":61022,"corporation":false,"usgs":true,"family":"McGregor","given":"Bonnie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161091,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10461,"text":"ofr8336 - 1983 - Gain-loss study along two streams in the upper Sabine River basin, Texas; August-September 1981","interactions":[],"lastModifiedDate":"2016-08-11T15:30:58","indexId":"ofr8336","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-36","title":"Gain-loss study along two streams in the upper Sabine River basin, Texas; August-September 1981","docAbstract":"A gain-loss study was made August-September 1981 along the upper Sabine River from Lake Tawakoni to Farm Road 2517 near Carthage and along Lake Fork Creek from Lake Fork Reservoir to its junction (mouth) with the Sabine River. The hydrologic data collected during the gain-loss study indicated that during periods of low flow on the Sabine River, at least as much water as is released from Lake Tawakoni and from Lake Fork Reservoir will be available downstream at Farm Road 14 near Big Sandy and at Farm Road 2517 near Carthage. Gains from bank seepage and small tributary inflows compensate for losses due to evaporation, evapotranspiration, and loss of water into the alluvial aquifer.
\nDissolved solids concentrations in the Sabine River, estimated from specific conductance, increased from about 120 milligrams per liter near the upstream end of the reach to about 400 milligrams per liter near the downstream end of the reach. Water with these concentrations of dissolved solids generally is suitable for most uses.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8336","usgsCitation":"Myers, D.R., 1983, Gain-loss study along two streams in the upper Sabine River basin, Texas; August-September 1981: U.S. Geological Survey Open-File Report 83-36, iv, 11 p., https://doi.org/10.3133/ofr8336.","productDescription":"iv, 11 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":38331,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145033,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0036/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1451","contributors":{"authors":[{"text":"Myers, Dennis R.","contributorId":57860,"corporation":false,"usgs":true,"family":"Myers","given":"Dennis","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":161443,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18409,"text":"ofr8324 - 1983 - Two newly discovered submarine canyons on Alaskan continental margin of Bering Sea","interactions":[],"lastModifiedDate":"2021-11-19T21:16:27.102062","indexId":"ofr8324","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-24","title":"Two newly discovered submarine canyons on Alaskan continental margin of Bering Sea","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8324","usgsCitation":"Carlson, P.R., Fischer, J., and Karl, H., 1983, Two newly discovered submarine canyons on Alaskan continental margin of Bering Sea: U.S. Geological Survey Open-File Report 83-24, Report: 37 p.; 1 Plate: 28.97 × 42.01 inches, https://doi.org/10.3133/ofr8324.","productDescription":"Report: 37 p.; 1 Plate: 28.97 × 42.01 inches","costCenters":[],"links":[{"id":47747,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0024/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47746,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0024/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151217,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0024/report-thumb.jpg"},{"id":391951,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13950.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -178,\n 59.25\n ],\n [\n -175.25,\n 59.25\n ],\n [\n -175.25,\n 57.10\n ],\n [\n -178,\n 57.10\n ],\n [\n -178,\n 59.25\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623aba","contributors":{"authors":[{"text":"Carlson, Paul R.","contributorId":81469,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":179071,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fischer, Jeffrey M. 0000-0003-2996-9272 fischer@usgs.gov","orcid":"https://orcid.org/0000-0003-2996-9272","contributorId":573,"corporation":false,"usgs":true,"family":"Fischer","given":"Jeffrey M.","email":"fischer@usgs.gov","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":false,"id":179069,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Karl, Herman A.","contributorId":55796,"corporation":false,"usgs":true,"family":"Karl","given":"Herman A.","affiliations":[],"preferred":false,"id":179070,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10323,"text":"ofr83116 - 1983 - Specifications for updating USGS land use and land cover maps","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr83116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-116","title":"Specifications for updating USGS land use and land cover maps","docAbstract":"To meet the increasing demands for up-to-date land use and land cover information, a primary goal of the U.S. Geological Survey's (USGS) national land use and land cover mapping program is to provide for periodic updating of maps and data in a timely and uniform manner. The technical specifications for updating existing USGS land use and land cover maps that are presented here cover both the interpretive aspects of detecting and identifying land use and land cover changes and the cartographic aspects of mapping and presenting the change data in conventional map format. They provide the map compiler with the procedures and techniques necessary to then use these change data to update existing land use and land cover maps in a manner that is both standardized and repeatable. Included are specifications for the acquisition of remotely sensed source materials, selection of compilation map bases, handling of data base corrections, editing and quality control operations, generation of map update products for USGS open file, and the reproduction and distribution of open file materials. These specifications are planned to become part of the National Mapping Division's Technical Instructions.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83116","usgsCitation":"Milazzo, V.A., 1983, Specifications for updating USGS land use and land cover maps: U.S. Geological Survey Open-File Report 83-116, iii, 65 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83116.","productDescription":"iii, 65 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":143654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0116/report-thumb.jpg"},{"id":38174,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0116/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e5e03","contributors":{"authors":[{"text":"Milazzo, Valerie A.","contributorId":88717,"corporation":false,"usgs":true,"family":"Milazzo","given":"Valerie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161197,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9157,"text":"ofr83346 - 1983 - GRAVPOLY; a modification of a three-dimensional gravity modeling program","interactions":[],"lastModifiedDate":"2012-02-02T00:06:18","indexId":"ofr83346","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-346","title":"GRAVPOLY; a modification of a three-dimensional gravity modeling program","docAbstract":"The three-dimensional magnetic modelling program of Donald Plouff (Plouff, 1975) has been made operational on a Honeywell Multics 68/80 computer. Modifications were made to input and output procedures to make the program compatible with U.S. Geological Survey (USGS) standard geophysical input and output formats.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83346","usgsCitation":"Godson, R.H., 1983, GRAVPOLY; a modification of a three-dimensional gravity modeling program: U.S. Geological Survey Open-File Report 83-346, 55 p. ill. ;28 cm., https://doi.org/10.3133/ofr83346.","productDescription":"55 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0346/report-thumb.jpg"},{"id":36784,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0346/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4889e4b07f02db51b822","contributors":{"authors":[{"text":"Godson, Richard H.","contributorId":11190,"corporation":false,"usgs":true,"family":"Godson","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":159197,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47071,"text":"ofr83523 - 1983 - Geologic map of the Challis 1 degree x 2 degree Quadrangle, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:10:40","indexId":"ofr83523","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-523","title":"Geologic map of the Challis 1 degree x 2 degree Quadrangle, Idaho","language":"ENGLISH","doi":"10.3133/ofr83523","usgsCitation":"Fisher, F.S., McIntyre, D.H., and Johnson, K.M., 1983, Geologic map of the Challis 1 degree x 2 degree Quadrangle, Idaho: U.S. Geological Survey Open-File Report 83-523, 1 map and 1 data sheet :col. ;45 x 64 cm., on sheet 64 x 97 cm. and sheet 84 x 73 cm. +28 cm.)1 pamphlet (i, 39 leaves ;, https://doi.org/10.3133/ofr83523.","productDescription":"1 map and 1 data sheet :col. ;45 x 64 cm., on sheet 64 x 97 cm. and sheet 84 x 73 cm. +28 cm.)1 pamphlet (i, 39 leaves ;","costCenters":[],"links":[{"id":108460,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14088.htm","linkFileType":{"id":5,"text":"html"},"description":"14088"},{"id":170730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0523/report-thumb.jpg"},{"id":84045,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0523/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84046,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0523/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d23d","contributors":{"authors":[{"text":"Fisher, Frederick S.","contributorId":17979,"corporation":false,"usgs":true,"family":"Fisher","given":"Frederick","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":234589,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McIntyre, D. H.","contributorId":45726,"corporation":false,"usgs":true,"family":"McIntyre","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":234590,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Kathleen M. kjohnson@usgs.gov","contributorId":2110,"corporation":false,"usgs":true,"family":"Johnson","given":"Kathleen","email":"kjohnson@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":234588,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":41236,"text":"ofr83395 - 1983 - Preliminary geologic map of Furnas Volcano, San Miguel, Azores","interactions":[],"lastModifiedDate":"2012-02-02T00:10:52","indexId":"ofr83395","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-395","title":"Preliminary geologic map of Furnas Volcano, San Miguel, Azores","language":"ENGLISH","doi":"10.3133/ofr83395","usgsCitation":"Moore, R.B., 1983, Preliminary geologic map of Furnas Volcano, San Miguel, Azores: U.S. Geological Survey Open-File Report 83-395, 1 map :photocopy ;on sheet 91 x 21 cm., https://doi.org/10.3133/ofr83395.","productDescription":"1 map :photocopy ;on sheet 91 x 21 cm.","costCenters":[],"links":[{"id":171224,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79045,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0395/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c04d","contributors":{"authors":[{"text":"Moore, Richard B. rmoore@usgs.gov","contributorId":1464,"corporation":false,"usgs":true,"family":"Moore","given":"Richard","email":"rmoore@usgs.gov","middleInitial":"B.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":224697,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25782,"text":"wri834168 - 1983 - Streamflow losses along the Balcones Fault Zone, Nueces River basin, Texas","interactions":[],"lastModifiedDate":"2016-08-09T13:52:13","indexId":"wri834168","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4168","title":"Streamflow losses along the Balcones Fault Zone, Nueces River basin, Texas","docAbstract":"An investigation was conducted to quantify and to determine distribution of streamflow losses and gains that occur during sustained flow conditions in the Balcones Fault Zone of the Nueces River basin. The streams studied include the West Nueces, Nueces, Dry Frio, Frio, and Sabinal Rivers, and Seco, Hondo, and Verde Creeks. Streamflow measurements made during the recession of storm flows identified direct recharge to outcrops of the Edwards aquifer and related limestones that ranged from as high as 393 cubic feet per second for the Dry Frio River to as low as 42 cubic feet per second for the Sabinal River. Recharge to outcrops of the Buda Limestone, Eagle Ford Shale, and Austin Group also eventually reaches the Edwards aquifer, and measurements identified losses to these formations ranging from as high as 174 cubic feet per second for the Frio River to near zero for Verde Creek.
\nStatistical evaluations of historical daily flow records for the streams that have gaging stations upstream and downstream from the recharge zone provided mathematical relationships that expressed downstream flow in terms of other significant parameters. For each stream, flow entering the recharge zone is most significant in defining downstream flow; for some streams, antecedent flows at the upstream site and ground-water levels are also significantly related to downstream flow. The analyses also determined the discharges required upstream from the recharge zone to sustain flow downstream from that zone. These discharges ranged from 355 cubic feet per second for the combined Frio and Dry Frio Rivers to 33 cubic feet per second for the Nueces River. The entire flows of lesser magnitude are generally lost to recharge to the aquifer.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri834168","usgsCitation":"Land, L.F., Boning, C., Harmsen, L., and Reeves, R., 1983, Streamflow losses along the Balcones Fault Zone, Nueces River basin, Texas: U.S. Geological Survey Water-Resources Investigations Report 83-4168, Report: vi, 72 p.; Plate: 19.69 x 11.68 inches, https://doi.org/10.3133/wri834168.","productDescription":"Report: vi, 72 p.; Plate: 19.69 x 11.68 inches","numberOfPages":"77","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":157279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4168/report-thumb.jpg"},{"id":54532,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4168/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54533,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4168/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Nueces River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4da6","contributors":{"authors":[{"text":"Land, L. F.","contributorId":17253,"corporation":false,"usgs":true,"family":"Land","given":"L.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":195051,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boning, C.W.","contributorId":31021,"corporation":false,"usgs":true,"family":"Boning","given":"C.W.","affiliations":[],"preferred":false,"id":195053,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harmsen, Lynn","contributorId":19941,"corporation":false,"usgs":true,"family":"Harmsen","given":"Lynn","email":"","affiliations":[],"preferred":false,"id":195052,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Reeves, R.D.","contributorId":95043,"corporation":false,"usgs":true,"family":"Reeves","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":195054,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}