{"pageNumber":"4843","pageRowStart":"121050","pageSize":"25","recordCount":184582,"records":[{"id":29000,"text":"wri864052 - 1986 - Geophysical well-log analysis of fractured crystalline rocks at East Bull Lake, Ontario, Canada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri864052","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4052","title":"Geophysical well-log analysis of fractured crystalline rocks at East Bull Lake, Ontario, Canada","docAbstract":"Various conventional geophysical borehole measurements were made in conjunction with measurements using a recently designed, low-frequency, acoustic-waveform probe and slow velocity flowmeter for characterization of a fractured mafic intrusion in southern Ontario, Canada. Conventional geophysical measurements included temperature, caliper, gamma, acoustic, single-point resistance, and acoustic televiewer logs. Hole stability problems prevented the use of neutron and gamma-gamma logs, because these logs require that a radioactive source be lowered into the borehole. Measurements were made in three boreholes as much as 850 m deep and penetrating a few tens of meters into granitic basement. All rocks within the mafic intrusion were characterized by minimal gamma radiation and acoustic velocities of about 6.9 km/sec. The uniformity of the acoustic velocities and the character of acoustic-waveform logs made with a conventional high-frequency logging source correlated with the density of fractures evident on televiewer logs. Sample intervals of high-frequency waveform logs were transformed into interpretations of effective fracture opening using a recent model for acoustic attenuation in fractured rocks. The new low-frequency sparker source did not perform as expected at depths below 250 m because of previously unsuspected problems with source firing under large hydrostatic heads. A new heat-pulse, slow velocity flowmeter was used to delineate in detail the flow regime indicated in a general way by temperature logs. The flowmeter measurements indicated that water was entering 2 of the boreholes at numerous fractures above a depth of 200 m, with flow in at least 2 of the boreholes exiting through large isolated fractures below a depth of 400 m. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864052","usgsCitation":"Paillet, F.L., and Hess, A., 1986, Geophysical well-log analysis of fractured crystalline rocks at East Bull Lake, Ontario, Canada: U.S. Geological Survey Water-Resources Investigations Report 86-4052, vi, 37 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864052.","productDescription":"vi, 37 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4052/report-thumb.jpg"},{"id":57867,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4052/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b368","contributors":{"authors":[{"text":"Paillet, Frederick L.","contributorId":63820,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, A.E.","contributorId":71979,"corporation":false,"usgs":true,"family":"Hess","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":200764,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61520,"text":"mf1581B - 1986 - Geochemical map of the North Fork John Day River Roadless Area, Grant County, Oregon","interactions":[],"lastModifiedDate":"2016-08-23T10:39:47","indexId":"mf1581B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1581","chapter":"B","title":"Geochemical map of the North Fork John Day River Roadless Area, Grant County, Oregon","docAbstract":"<p><span>The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine their mineral resource potential. Results must be made available to the public and submitted to the President&nbsp;and the Congress. This report presents the analytical results of a geochemical survey of the North Fork John Day River Roadless Area&nbsp;(B6253) in the Umatilla and Wallowa-Whitman&nbsp;National Forests, Grant County, Oregon. The North Fork John Day River Roadless Area was classified&nbsp;as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.</span></p>\n<p><span>The North Fork John Day River Roadless Area comprised 21,210 acres in the&nbsp;Umatilla and Wallowa-Whitman&nbsp;National Forests, Grant County, Oregon, about 30 miles northwest of Baker, Oregon. The irregularly shaped area extends for about 1 mile on both sides of a 25-mile segment of the North Fork John Day River from Big Creek on the west to North Fork John Day Campground on the east. Most of the roadless area is in the northern half of the Desolation Butte 15-minute quadrangle. The eastern end of the area is in parts of the Granite and Trout Meadows 7&frac12;-minute quadrangles.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1581B","usgsCitation":"Evans, J.G., 1986, Geochemical map of the North Fork John Day River Roadless Area, Grant County, Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1581, 36.58 x 25.48 inches, https://doi.org/10.3133/mf1581B.","productDescription":"36.58 x 25.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":182476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1581b.PNG"},{"id":327606,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1581-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Grant County","otherGeospatial":"North Fork John Day River Roadless Area, Umatilla National Forest, Wallowa-Whitman National Forest","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.66666666666667,44.833333333333336 ], [ -118.66666666666667,45 ], [ -118.41666666666667,45 ], [ -118.41666666666667,44.833333333333336 ], [ -118.66666666666667,44.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae1f7","contributors":{"authors":[{"text":"Evans, James G. jevans@usgs.gov","contributorId":2396,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"jevans@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":265863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28945,"text":"wri854296 - 1986 - Flood-depth frequency relations for streams in Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:08:37","indexId":"wri854296","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4296","title":"Flood-depth frequency relations for streams in Alabama","docAbstract":"Equations were defined for estimating the depth of water for floods having recurrence intervals of 2, 5, 10, 25, 50, 100, and 200 years on rural and urban streams in Alabama. Multiple regression analyses were made using the ' maximum RSQUARE improvement ' procedures. The dependent variable was the flood depth and the independent variables were 10 basin and climatic characteristics. For rural streams, drainage area size (0.44 to 1,344 sq mi) was the only statistically significant independent variable tested to estimate flood depths in six different hydrologic areas. Other variables affecting flood depth relations are reflected in the equation constant and coefficient for each hydrologic area. These account for differences in geologic and topographic characteristics. For urban streams, drainage area size (0.16 to 83.5 sq mi) and percent impervious area (8.3% to 42.9%) of the basin were the most significant independent variables tested to estimate flood depths. For most streams where the drainage area is &gt; 1,344 sq mi, the drainage basin extends into more than one hydrologic area and the equations presented would not apply. Flood profile data and gaging station records are available from the U.S. Geological Survey for use in estimating flood depths for these large streams. Flood routing and historic flood profiles are also available for many of the large streams which have flood regulation. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854296","usgsCitation":"Olin, D., 1986, Flood-depth frequency relations for streams in Alabama: U.S. Geological Survey Water-Resources Investigations Report 85-4296, iv, 46 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854296.","productDescription":"iv, 46 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121566,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4296/report-thumb.jpg"},{"id":57821,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4296/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a0e4b07f02db494602","contributors":{"authors":[{"text":"Olin, D.A.","contributorId":106905,"corporation":false,"usgs":true,"family":"Olin","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":200659,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28864,"text":"wri854316 - 1986 - Effect of bank protection measures, Stehekin River, Chelan County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri854316","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4316","title":"Effect of bank protection measures, Stehekin River, Chelan County, Washington","docAbstract":"An investigation of the lower Stehekin River was conducted to study the effects on flood elevations and velocities from four bank protection and flood prevention measures that are being contemplated as a means of reducing erosional losses of river bank property. These measures are: bank armoring, armored revetment levees, spur dikes, and redevelopment of old cutoff channels. The banks at seven study sites could be armored without adverse effect on the flood velocities and elevations. The largest increases due to armoring--up to 1.6 ft/sec in velocity and 1 ft in elevation--occurred in the vicinity of sites 5, 6, and 7 where the gradient of the river channel is about 50 ft/mi and the velocities are high to begin with (about 6 to 13 ft/sec). The use of a levee in conjunction with armoring on the northeast bank from sites 5 to 7 would increase the velocities as much as 2.8 ft/sec and increase the elevation as much as 1 ft, but it would also provide some flood protection to the east bank, which is frequently inundated. Spur dikes were considered a practical alternative only at site 3, where reduced bank erosion may occur without aggravating flood inundation or erosion elsewhere. The rerouting of flood flow through an old cutoff channel near site 1 increased the velocity by 3.2 ft/sec and the elevation by 1 ft for the 100-year flood; however, it would move floodwater away from residential property where bank erosion is a problem. The few other old channels that shortcut river bends where much erosion occurs are apparently already part of the channel during floods. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854316","usgsCitation":"Nelson, L.M., 1986, Effect of bank protection measures, Stehekin River, Chelan County, Washington: U.S. Geological Survey Water-Resources Investigations Report 85-4316, iv, 22 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854316.","productDescription":"iv, 22 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118926,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4316/report-thumb.jpg"},{"id":57742,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4316/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6256b7","contributors":{"authors":[{"text":"Nelson, L. M.","contributorId":39773,"corporation":false,"usgs":true,"family":"Nelson","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":200525,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27479,"text":"wri854102 - 1986 - Ground-water movement and effects of coal strip mining on water quality of high-wall lakes and aquifers in the Macon-Huntsville area, north-central Missouri","interactions":[],"lastModifiedDate":"2022-02-18T21:17:42.217943","indexId":"wri854102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4102","title":"Ground-water movement and effects of coal strip mining on water quality of high-wall lakes and aquifers in the Macon-Huntsville area, north-central Missouri","docAbstract":"Glacial drift and Pennsylvanian bedrock were mixed together forming spoil during pre-reclamation strip mining for coal in north-central Missouri. This restructuring of the land increases the porosity of the material, and increases aqueous concentrations of many dissolved constituents. Median sodium and bicarbonate concentrations were slightly greater, calcium 5 times greater, magnesium 6 times greater, manganese 15 times greater, iron 19 times greater, and sulfate 24 times greater in water from spoil than in water from glacial drift. Median potassium concentrations were slightly greater, and chloride concentrations were two times greater in water from glacial drift than in water from spoil. Water types in glacial drift and bedrock were mostly sodium bicarbonate and calcium bicarbonate; in spoil and lakes in the spoil, the water types were mostly calcium sulfate. Median pH values in water from spoil were 6.6, as compared to 7.4 in water from glacial drift and 9.0 in water from bedrock. Neutralization of acid by carbonate rocks causes the moderate pH values in water from spoil; a carbonate system closed to the atmosphere may result in alkaline pH values in bedrock. Transmissivities generally are greatest for spoil, and decrease in the following order: alluvium, glacial drift, and bedrock. Recharge to spoil is from precipitation, lateral flow from glacial drift, and lateral and vertical flow from bedrock. The rate of recharge to the aquifers is unknown, but probably is small. Groundwater discharge from the glacial drift, bedrock, and spoil is to alluvium. The direction of flow generally was from high-wall lakes in the spoil toward East Fork Little Chariton River or South Fork Claybank Creek. Significant differences (95% confidence level) in values and concentrations of aqueous constituents between spoil areas mined at different times (1940, 1952, and 1968) were obtained for pH, calcium, magnesium, manganese, sulfate, chloride, and dissolved solids, but not for iron. These differences are attributed to local variations in the geohydrologic system rather than spoil age. (Lantz-PTT)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854102","usgsCitation":"Hall, D.C., and Davis, R.E., 1986, Ground-water movement and effects of coal strip mining on water quality of high-wall lakes and aquifers in the Macon-Huntsville area, north-central Missouri: U.S. Geological Survey Water-Resources Investigations Report 85-4102, viii, 102 p., https://doi.org/10.3133/wri854102.","productDescription":"viii, 102 p.","costCenters":[],"links":[{"id":56330,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4102/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126660,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4102/report-thumb.jpg"},{"id":396201,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36271.htm"}],"country":"United States","state":"Missouri","otherGeospatial":"Macon-Huntsville area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.583,\n              39.625\n            ],\n            [\n              -92.493,\n              39.625\n            ],\n            [\n              -92.493,\n              39.708\n            ],\n            [\n              -92.583,\n              39.708\n            ],\n            [\n              -92.583,\n              39.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4995e4b07f02db5b637f","contributors":{"authors":[{"text":"Hall, D. C.","contributorId":7291,"corporation":false,"usgs":true,"family":"Hall","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":198191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, R. E.","contributorId":77153,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198192,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27477,"text":"wri864160 - 1986 - A description of the hydrologic system and the effects of coal mining on water quality in the East Fork Little Chariton River and the alluvial aquifer between Macon and Huntsville, north-central Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:08:27","indexId":"wri864160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4160","title":"A description of the hydrologic system and the effects of coal mining on water quality in the East Fork Little Chariton River and the alluvial aquifer between Macon and Huntsville, north-central Missouri","docAbstract":"The quality of surface and groundwater has been affected by abandoned strip mines and by abandoned underground mines in a 110-sq mi subbasin of the East Fork Little Chariton River. More than 14% of the area was strip mined for coal before 1979. The hydrologic system in the area was investigated and the effects of coal mining on quality of water in the river and alluvial aquifer were analyzed, with major emphasis on defining strip-mining effects. The groundwater gradient was from glacial drift or coal spring to alluvium to the East Fork Little Chariton River, and was greatest in spring and least in fall. Seepage from alluvium to the East Fork Little Chariton River occurs throughout the year, except during drought conditions when the only river flow is water released from Long Branch Lake. In the East Fork Little Chariton River median dissolved-solids concentrations increased from 153 mg/L near Macon to 630 mg/L near Huntsville and median sulfate concentrations increased from 36 mg/L near Macon to 360 mg/L near Huntsville. The median dissolved-solids concentration in water from the alluvium increased from 408 mg/L upstream from the strip mines to 641 mg/L near the mines and median dissolved-sulfate concentration increased from 140 to 350 mg/L. The sulfate-to-chloride ratio, used as the most sensitive indicator of strip-mining effects, increased markedly downstream in the East Fork Little Chariton River and nearby Middle Fork Little Chariton River, which also is affected by strip mining. There were no significant increases in sulfate-to-chloride ratio and dissolved-solids concentrations in comparable nearby subbasins of the Grand, Thompson, and Chariton Rivers where there was no mining. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864160","usgsCitation":"Hall, D.C., 1986, A description of the hydrologic system and the effects of coal mining on water quality in the East Fork Little Chariton River and the alluvial aquifer between Macon and Huntsville, north-central Missouri: U.S. Geological Survey Water-Resources Investigations Report 86-4160, iv, 66 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864160.","productDescription":"iv, 66 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4160/report-thumb.jpg"},{"id":56328,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af045","contributors":{"authors":[{"text":"Hall, D. C.","contributorId":7291,"corporation":false,"usgs":true,"family":"Hall","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":198188,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27464,"text":"wri854025 - 1986 - Areal and temporal variability of selected water-quality characteristics in two hydrologic-benchmark basins in the northeastern United States","interactions":[],"lastModifiedDate":"2017-07-07T08:23:20","indexId":"wri854025","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4025","title":"Areal and temporal variability of selected water-quality characteristics in two hydrologic-benchmark basins in the northeastern United States","docAbstract":"Two U.S. Geological Survey National Hydrologic Benchmark stations--Young Womans Creek near Renovo, Pennsylvania and Esopus Creek at Shandaken, New York--were studied to (1) define, both areally and temporally, variations of stream acidity and other water quality characteristics within the basins; (2) evaluate how well the data collected at the Benchmark station represent the water quality conditions upstream; (3) define relations between streamflow acidity or pH; and (4) provide a data base to detect trends in quality of headwater streams. Samples were collected at nine sites, including the Benchmark station, in each basin for three series of measurements over a range of streamflows. Along with streamflow, samples were analyzed for water temperature, specific conductance, pH, dissolved oxygen, acidity, alkalinity, dissolved sulfate, and dissolved nitrite plus nitrate. The results of the measurements indicated little water quality variation in the Young Womans Creek basin. Therefore, the data collected at the Benchmark station can be used to reflect upstream changes in water quality. The data collected at the Esopus Creek station did not reflect upstream conditions as well as the Young Womans Creek data because the water quality varied throughout the basin. Few strong relations were found between streamflow and the water quality characteristics examined in this study. The Esopus Creek data indicated the possibility of relationships between streamflow and alkalinity, dissolved nitrite plus nitrate, and specific conductance. No relations were found between streamflow and the Young Womans Creek water quality data. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854025","usgsCitation":"Hainly, R., and Ritter, J., 1986, Areal and temporal variability of selected water-quality characteristics in two hydrologic-benchmark basins in the northeastern United States: U.S. Geological Survey Water-Resources Investigations Report 85-4025, v, 22 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854025.","productDescription":"v, 22 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":118709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4025/report-thumb.jpg"},{"id":56321,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4025/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673694","contributors":{"authors":[{"text":"Hainly, R.A.","contributorId":45732,"corporation":false,"usgs":true,"family":"Hainly","given":"R.A.","affiliations":[],"preferred":false,"id":198164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ritter, J.R.","contributorId":22350,"corporation":false,"usgs":true,"family":"Ritter","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":198163,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28834,"text":"wri854334 - 1986 - Hydrogeology of sand-plain aquifers in Carlton, Kanabec, and Pine Counties, east-central Minnesota","interactions":[],"lastModifiedDate":"2022-02-03T19:27:52.356527","indexId":"wri854334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4334","title":"Hydrogeology of sand-plain aquifers in Carlton, Kanabec, and Pine Counties, east-central Minnesota","docAbstract":"<p>Sand-plain aquifers in parts of Carlton, Kanabec, and Pine Counties in east-central Minnesota constitute a major aquifer system. They consist predominantly of fine to medium outwash sand with a combined areal extent of nearly 500 square miles. Saturated thickness in localized areas is as much as 90 feet. Depth to water generally is less than 20 feet. Transmissivities range from about 100 to 25,000 feet squared per day. Yields to properly constructed wells locally may exceed 2,000 gallons per minute. A reconnaissance of sandstone units underlying the outwash indicates that transmissivities of the sandstone aquifers range from 1,850 to 2,200 feet squared per day, and specific capacities range from 9 to 12 gallons per minute per foot of drawdown. Locally, wells may be capable of supplying several hundred gallons per minute. Regionally, the sand-plain and sandstone aquifers are poorly connected hydraulically at all locations tested except in a small localized area near Quamba in Kanabec County.</p>\n<p>Ground water in the sand-plain aquifers can be classified chemically, based on predominant ions, as a calcium bicarbonate type that is moderately hard. Concentrations of dissolved solids range from 30 to 610 milligrams per liter. Except for locally high concentrations of iron and manganese, the quality of water is within State drinking-water standards and is suitable for most uses. There are no major differences between the quality of water in the sand-plain and sandstone aquifers.</p>\n<p>Ground-water flow, aquifer response, aquifer development, and drought conditions were simulated for sand-plain aquifers areally extensive enough to be hydrologically significant. Simulation of expanded ground-water development and drought in northern Pine County indicates that regional ground-water levels may be lowered as much as 12 feet and ground-water discharge to streams may be reduced as much as 42 percent. Simulation of expanded development and drought in southern Pine County indicates that regional ground-water levels may be lowered as much as 25 feet and ground-water discharge to streams may be reduced as much as 65 percent. The simulations also indicate that each area, especially the northern Pine County area, will support substantial additional development without dewatering the aquifer or reducing streamflow significantly.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri854334","collaboration":"Prepared in cooperation with the Onanegozie Resource Conservation and Development Project and the Minnesota Department of Natural Resources","usgsCitation":"Myette, C., 1986, Hydrogeology of sand-plain aquifers in Carlton, Kanabec, and Pine Counties, east-central Minnesota: U.S. Geological Survey Water-Resources Investigations Report 85-4334, Report: vi, 66 p.; 4 Plates: 20.31 x 36.55 inches or smaller, https://doi.org/10.3133/wri854334.","productDescription":"Report: vi, 66 p.; 4 Plates: 20.31 x 36.55 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":26678,"text":"wri844356 - 1986 - Wastewater movement near four treatment and disposal sites in Yellowstone National Park, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:32","indexId":"wri844356","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"84-4356","title":"Wastewater movement near four treatment and disposal sites in Yellowstone National Park, Wyoming","docAbstract":"The U.S. Geological Survey, in cooperation with the National Park Service, studied the effects on nearby streams and lakes of treated wastewater effluents that percolate from sewage lagoons at four sites in Yellowstone National Park. A network of observation wells has been established near the sites, and water level and water quality data were collected from 1974 through 1982. Groundwater mounds occur under the lagoons as percolation of effluents occurs. The percolating effluents mix with groundwater and form plumes of water that contain chemical constituents from the effluents. These plumes move down the hydraulic gradient toward groundwater discharge areas. The directions of movement of percolating effluents have been determined by analyzing water samples from wells near the lagoons for specific conductance, chloride concentration, and nitrite plus nitrate concentration. Other constituents and properties also were determined. The percolating effluents are diluted by groundwater and have no discernible effects on the quality of water in the nearby streams and lakes. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844356","usgsCitation":"Cox, E., 1986, Wastewater movement near four treatment and disposal sites in Yellowstone National Park, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 84-4356, vi, 81 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844356.","productDescription":"vi, 81 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158117,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4356/report-thumb.jpg"},{"id":55540,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4356/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd454","contributors":{"authors":[{"text":"Cox, E.R.","contributorId":6094,"corporation":false,"usgs":true,"family":"Cox","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":196816,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67969,"text":"ha694B - 1986 - Ground-water levels in the Great Basin region of Nevada, Utah, and adjacent states","interactions":[],"lastModifiedDate":"2017-02-21T10:43:27","indexId":"ha694B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"694","chapter":"B","title":"Ground-water levels in the Great Basin region of Nevada, Utah, and adjacent states","docAbstract":"<p>The Great Basin Regional Aquifer-System Analysis (RASA) is the tenth study in a national program b the U.S. Geological Survey to analyze regional ground-water systems that comprise a major part of the Nation’s water supply. The main objectives of RASA studies are to: (1) Describe the ground-water systems as they exist today, (2) analyze the changes that have led to the system’s present condition, (3) combine the results of previous studies in a regional analysis, and (4) provide means by which effects of future ground-water development can be estimated (G.D. Bennett, U.S. Geological Survey, written comm., 1978).</p><p>This atlas is Chapter B of a three-part series. Chapter A delineates and describes hydrogeologic units in the Great Basin, and Chapter C shows inferred directions of ground-water flow and individual flow systems.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha694B","usgsCitation":"Thomas, J., Mason, J.L., and Crabtree, J.D., 1986, Ground-water levels in the Great Basin region of Nevada, Utah, and adjacent states: U.S. Geological Survey Hydrologic Atlas 694, 2 Sheets: 32.00 x 42.00 inches and 32.00 x 41.79 inches , https://doi.org/10.3133/ha694B.","productDescription":"2 Sheets: 32.00 x 42.00 inches and 32.00 x 41.79 inches ","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":89198,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/694b/plate-1.pdf","text":"Sheet 1","size":"15.05 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Water levels in basin-fill deposits"},{"id":89199,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/694b/plate-2.pdf","text":"Sheet 2","size":"10.15 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Potentiometric surface in consolidated rocks of the carbonate-rock province"},{"id":185812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":335843,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/ha694A","text":"HA-694-A","linkHelpText":"Hydrogeology of the Great Basin region of Nevada, Utah, and adjacent states"},{"id":335844,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/ha694C","text":"HA-694-C","linkHelpText":"Major ground-water flow systems in the Great Basin region of Nevada, Utah, and adjacent states"}],"scale":"1000000","country":"United States","state":"Nevada, Utah","otherGeospatial":"Great Basin region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120.32226562500001,\n              42.24478535602799\n            ],\n            [\n              -120.32226562500001,\n              38.77121637244273\n            ],\n            [\n              -114.86206054687499,\n              34.867904962568716\n            ],\n            [\n              -113.983154296875,\n              37.01132594307015\n            ],\n            [\n              -111.24755859375,\n              40.136890695345905\n            ],\n            [\n              -111.060791015625,\n              42.293564192170095\n            ],\n            [\n              -120.32226562500001,\n              42.24478535602799\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667539","contributors":{"authors":[{"text":"Thomas, James M.","contributorId":97880,"corporation":false,"usgs":true,"family":"Thomas","given":"James M.","affiliations":[],"preferred":false,"id":277422,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mason, James L.","contributorId":14397,"corporation":false,"usgs":true,"family":"Mason","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277420,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crabtree, James D.","contributorId":73278,"corporation":false,"usgs":false,"family":"Crabtree","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":277421,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61558,"text":"mf1183J - 1986 - Geochemical maps showing distribution and abundance of manganese in two fractions of stream-sediment concentrates, Silver City 1 degree by 2 degrees Quadrangle, New Mexico and Arizona","interactions":[],"lastModifiedDate":"2016-08-23T10:45:06","indexId":"mf1183J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1183","chapter":"J","title":"Geochemical maps showing distribution and abundance of manganese in two fractions of stream-sediment concentrates, Silver City 1 degree by 2 degrees Quadrangle, New Mexico and Arizona","docAbstract":"<p><span>These maps (Maps A and B) show the distribution and abundance of&nbsp;maganese in the nonmagnetic and magnetic fractions&nbsp;of heavy-mineral concentrates from stream sediments collected in the Silver City 1</span><sup><span>o</span></sup><span>&nbsp;x 2</span><span><sup>o</sup>&nbsp;</span><span>quadrangle, New Mexico and Arizona. Geochemical maps showing the distribution and abundance of 10 other selected key elements and the mineral fluorite in the Silver City quadrangle are also part of this folio (Watts and Hassemer, 1980; Watts and others 1986a-i). These maps contribute to the assessment of mineral resources within Silver City&nbsp;1</span><sup><span>o</span></sup><span>&nbsp;x 2</span><span><sup>o</sup>&nbsp;</span><span>quadrangle by (1) showing regional patterns of elements enriched in heavy-mineral concentrates, thereby providing clues to regional patterns of mineralization; (2) showing new areas containing enriched metals, not previously known from mining activity; and (3) providing supportive data to the interpretive and summary maps (Watts and Hassmer, 1986) and the mineral resource assessment (Richter and others, 1983). Background information that pertains to published components of the Silver City Folio is also available (Richter and others, in press).&nbsp;</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1183J","usgsCitation":"Watts, K., Hassemer, J.R., Forn, C.L., and Siems, D.F., 1986, Geochemical maps showing distribution and abundance of manganese in two fractions of stream-sediment concentrates, Silver City 1 degree by 2 degrees Quadrangle, New Mexico and Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1183, 45.30 x 39.71 inches, https://doi.org/10.3133/mf1183J.","productDescription":"45.30 x 39.71 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1183J.PNG"},{"id":327618,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1183-J/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Arizona, New Mexico","city":"Silver City","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110,32 ], [ -110,33 ], [ -108,33 ], [ -108,32 ], [ -110,32 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adfd0","contributors":{"authors":[{"text":"Watts, Kenneth C.","contributorId":101180,"corporation":false,"usgs":true,"family":"Watts","given":"Kenneth C.","affiliations":[],"preferred":false,"id":266038,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hassemer, Jerry R.","contributorId":173451,"corporation":false,"usgs":false,"family":"Hassemer","given":"Jerry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":266036,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forn, Carl L.","contributorId":173452,"corporation":false,"usgs":false,"family":"Forn","given":"Carl","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":266037,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Siems, David F.","contributorId":100835,"corporation":false,"usgs":true,"family":"Siems","given":"David","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":266039,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":61611,"text":"gq1590 - 1986 - Geologic map of the Koosharem quadrangle, Sevier and Piute Counties, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:51","indexId":"gq1590","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1590","title":"Geologic map of the Koosharem quadrangle, Sevier and Piute Counties, Utah","language":"ENGLISH","doi":"10.3133/gq1590","usgsCitation":"Rowley, P.D., Williams, P., and Kaplan, A.M., 1986, Geologic map of the Koosharem quadrangle, Sevier and Piute Counties, Utah: U.S. Geological Survey Geologic Quadrangle 1590, 1 map :col. ;58 x 45 cm., on sheet 82 x 89 cm., folded in envelope 30 x 23 cm., https://doi.org/10.3133/gq1590.","productDescription":"1 map :col. ;58 x 45 cm., on sheet 82 x 89 cm., folded in envelope 30 x 23 cm.","costCenters":[],"links":[{"id":102666,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1116.htm","linkFileType":{"id":5,"text":"html"},"description":"1116"},{"id":247917,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1590/report.pdf","size":"70","linkFileType":{"id":1,"text":"pdf"}},{"id":252342,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1590/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,38.5 ], [ -112,38.6175 ], [ -111.86749999999999,38.6175 ], [ -111.86749999999999,38.5 ], [ -112,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db6970ce","contributors":{"authors":[{"text":"Rowley, Peter D.","contributorId":27435,"corporation":false,"usgs":true,"family":"Rowley","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":266134,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Paul L.","contributorId":91086,"corporation":false,"usgs":true,"family":"Williams","given":"Paul L.","affiliations":[],"preferred":false,"id":266135,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaplan, Allan M.","contributorId":13319,"corporation":false,"usgs":true,"family":"Kaplan","given":"Allan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":266133,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28856,"text":"wri844144 - 1986 - Investigation of the need for discharge adjustments for unsteady flow at selected gaging stations on streams in Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri844144","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"84-4144","title":"Investigation of the need for discharge adjustments for unsteady flow at selected gaging stations on streams in Tennessee","docAbstract":"Measured discharges made during rising or falling stages generally require adjustments to refine constant-stage rating curves (stage-discharge relations) for gaged sites. Measurements at 42 gaging stations on Tennessee streams were selected for adjustment. Two methods, generally accepted by the U.S. Geological Survey, were tested: (1) the slope method adjusts the discharge for changing slope during the measurement, and (2) the storage method adjusts for change in channel storage. Both methods are related to the rate of change in stage. The initial results of the storage method of adjustments were unsatisfactory because of uncertainty in determining channel storage at each site, and a specific trend in the results could not be defined. Consequently, the storage method of adjustment was deleted from successive analyses. Maximum adjustments in measured discharge using the slope method were less than 5 percent at 28 of the 42 stations and less than 10 percent at 39 of the 42 stations used in the analyses. The adjustments were small because most of the measurements were made during nearly stable stage. Adjustments of measurements made during stage changes of several feet per hour could be considerably larger than 10 percent. Stage records at 10 stations showed that maximum change in stage during rises were considerably higher than the change in stage observed during the measurements. Large adjustments are usually required for a short period of time on the rising side of a hydrograph and smaller adjustments are required for a longer period of time on the falling side. Maximum adjustments in discharge using the slope method were less than 5 percent at three of the 10 stations and less than 30 percent at eight of the 10 stations used in the analyses. The mean discharge for the adjusted and unadjusted hydrographs are about the same. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844144","usgsCitation":"Neely, B., and Bingham, R., 1986, Investigation of the need for discharge adjustments for unsteady flow at selected gaging stations on streams in Tennessee: U.S. Geological Survey Water-Resources Investigations Report 84-4144, iv, 21 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844144.","productDescription":"iv, 21 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":2339,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri844144","linkFileType":{"id":5,"text":"html"}},{"id":123970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_84_4144.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4284","contributors":{"authors":[{"text":"Neely, B.L.","contributorId":90344,"corporation":false,"usgs":true,"family":"Neely","given":"B.L.","affiliations":[],"preferred":false,"id":200513,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bingham, R.H.","contributorId":37301,"corporation":false,"usgs":true,"family":"Bingham","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":200512,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61608,"text":"gq1589 - 1986 - Geologic map of the Greenwich quadrangle, Piute County, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:51","indexId":"gq1589","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1589","title":"Geologic map of the Greenwich quadrangle, Piute County, Utah","language":"ENGLISH","doi":"10.3133/gq1589","usgsCitation":"Rowley, P.D., Williams, P., and Kaplan, A.M., 1986, Geologic map of the Greenwich quadrangle, Piute County, Utah: U.S. Geological Survey Geologic Quadrangle 1589, 1 map :col. ;58 x 45 cm., on sheet 84 x 93 cm., folded in envelope 30 x 23 cm., https://doi.org/10.3133/gq1589.","productDescription":"1 map :col. ;58 x 45 cm., on sheet 84 x 93 cm., folded in envelope 30 x 23 cm.","costCenters":[],"links":[{"id":102665,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1115.htm","linkFileType":{"id":5,"text":"html"},"description":"1115"},{"id":247914,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1589/report.pdf","size":"72","linkFileType":{"id":1,"text":"pdf"}},{"id":252339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1589/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,38.3675 ], [ -112,38.5 ], [ -111.86749999999999,38.5 ], [ -111.86749999999999,38.3675 ], [ -112,38.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69803f","contributors":{"authors":[{"text":"Rowley, Peter D.","contributorId":27435,"corporation":false,"usgs":true,"family":"Rowley","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":266126,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Paul L.","contributorId":91086,"corporation":false,"usgs":true,"family":"Williams","given":"Paul L.","affiliations":[],"preferred":false,"id":266127,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaplan, Allan M.","contributorId":13319,"corporation":false,"usgs":true,"family":"Kaplan","given":"Allan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":266125,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61561,"text":"mf1807 - 1986 - Free-air gravity anomaly map of the Long Island Platform","interactions":[],"lastModifiedDate":"2016-08-23T10:42:56","indexId":"mf1807","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1807","title":"Free-air gravity anomaly map of the Long Island Platform","docAbstract":"<p>The U.S. Geological Survey (USGS) has collected marine gravity data along the U.S. Atlantic continental margin during the last decade. This map of the Long Island platform combines the data used to make the preliminary free-air gravity anomaly map of the Atlantic continental margin (Grow and others, 1976) with the new gravity values collected aboard the RV <i>Gilliss</i> in 1979 and the RV <i>Gyre</i> in 1981.</p>\n<p>Carl Bowin provided the USNS <i>Kealthley</i> data from the Woods Hole Oceanographic Institution gravity data-base. We thank Bab Bowles (USGS) for his advice on editing the navigation and gravity data.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1807","usgsCitation":"Hutchinson, D.R., Leeds, W., Bell, R., and Grow, J.A., 1986, Free-air gravity anomaly map of the Long Island Platform: U.S. Geological Survey Miscellaneous Field Studies Map 1807, Plate: 49.01 x 31.77 inches or smaller, https://doi.org/10.3133/mf1807.","productDescription":"Plate: 49.01 x 31.77 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326196,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1807.JPG"},{"id":327612,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1807/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","otherGeospatial":"Long Island","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75,39 ], [ -75,42 ], [ -69,42 ], [ -69,39 ], [ -75,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8701","contributors":{"authors":[{"text":"Hutchinson, D. R.","contributorId":31770,"corporation":false,"usgs":true,"family":"Hutchinson","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":266047,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leeds, W.D.","contributorId":43432,"corporation":false,"usgs":true,"family":"Leeds","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":266049,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bell, Robin","contributorId":41515,"corporation":false,"usgs":true,"family":"Bell","given":"Robin","affiliations":[],"preferred":false,"id":266048,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grow, J. A.","contributorId":27858,"corporation":false,"usgs":true,"family":"Grow","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":266046,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":61562,"text":"mf1878 - 1986 - Geologic map of the Beck Mountain, Crestone Peak, and Crestone quadrangles, Custer, Huerfano, and Saguache counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:35","indexId":"mf1878","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1878","title":"Geologic map of the Beck Mountain, Crestone Peak, and Crestone quadrangles, Custer, Huerfano, and Saguache counties, Colorado","language":"ENGLISH","doi":"10.3133/mf1878","usgsCitation":"Lindsey, D.A., Johnson, B., Soulliere, S.J., Bruce, R., and Hafner, K., 1986, Geologic map of the Beck Mountain, Crestone Peak, and Crestone quadrangles, Custer, Huerfano, and Saguache counties, Colorado: U.S. Geological Survey Miscellaneous Field Studies Map 1878, 1 map ;58 x 137 cm., on sheet 104 x 143 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1878.","productDescription":"1 map ;58 x 137 cm., on sheet 104 x 143 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":106019,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7435.htm","linkFileType":{"id":5,"text":"html"},"description":"7435"},{"id":179864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.75,37.86666666666667 ], [ -105.75,38 ], [ -105.36749999999999,38 ], [ -105.36749999999999,37.86666666666667 ], [ -105.75,37.86666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ee4b07f02db69fe01","contributors":{"authors":[{"text":"Lindsey, D. A.","contributorId":49814,"corporation":false,"usgs":true,"family":"Lindsey","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":266051,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, B. R.","contributorId":73995,"corporation":false,"usgs":true,"family":"Johnson","given":"B. R.","affiliations":[],"preferred":false,"id":266054,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Soulliere, S. J.","contributorId":12861,"corporation":false,"usgs":true,"family":"Soulliere","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":266050,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bruce, R.M.","contributorId":60314,"corporation":false,"usgs":true,"family":"Bruce","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":266052,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hafner, Katrin","contributorId":68344,"corporation":false,"usgs":true,"family":"Hafner","given":"Katrin","affiliations":[],"preferred":false,"id":266053,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":38510,"text":"pp1338 - 1986 - Effects of organic wastes on water quality from processing of oil shale from the Green River Formation, Colorado, Utah, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:14","indexId":"pp1338","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1338","title":"Effects of organic wastes on water quality from processing of oil shale from the Green River Formation, Colorado, Utah, and Wyoming","docAbstract":"A series of investigations were conducted during a 6-year research project to determine the nature and effects of organic wastes from processing of Green River Formation oil shale on water quality. Fifty percent of the organic compounds in two retort wastewaters were identified as various aromatic amines, mono- and dicarboxylic acids phenols, amides, alcohols, ketones, nitriles, and hydroxypyridines. Spent shales with carbonaceous coatings were found to have good sorbent properties for organic constituents of retort wastewaters. However, soils sampled adjacent to an in situ retort had only fair sorbent properties for organic constituents or retort wastewater, and application of retort wastewater caused disruption of soil structure characteristics and extracted soil organic matter constituents. Microbiological degradation of organic solutes in retort wastewaters was found to occur preferentially in hydrocarbons and fatty acid groups of compounds. Aromatic amines did not degrade and they inhibited bacterial growth where their concentrations were significant. Ammonia, aromatic amines, and thiocyanate persisted in groundwater contaminated by in situ oil shale retorting, but thiosulfate was quantitatively degraded one year after the burn. Thiocyanate was found to be the best conservative tracer for retort water discharged into groundwater. Natural organic solutes, isolated from groundwater in contact with Green River Formation oil shale and from the White River near Rangely, Colorado, were readily distinguished from organic constituents in retort wastewaters by molecular weight and chemical characteristic differences. (USGS)","language":"ENGLISH","doi":"10.3133/pp1338","usgsCitation":"Leenheer, J., and Noyes, T., 1986, Effects of organic wastes on water quality from processing of oil shale from the Green River Formation, Colorado, Utah, and Wyoming: U.S. Geological Survey Professional Paper 1338, 56 p., https://doi.org/10.3133/pp1338.","productDescription":"56 p.","costCenters":[],"links":[{"id":123902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1338/report-thumb.jpg"},{"id":65229,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1338/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611abf","contributors":{"authors":[{"text":"Leenheer, J.A.","contributorId":75123,"corporation":false,"usgs":true,"family":"Leenheer","given":"J.A.","affiliations":[],"preferred":false,"id":219962,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Noyes, T.I.","contributorId":54971,"corporation":false,"usgs":true,"family":"Noyes","given":"T.I.","email":"","affiliations":[],"preferred":false,"id":219961,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15234,"text":"ofr86427 - 1986 - Analytical and stratigraphic data on the Retort Phosphatic Shale Member of the Phosphoria Formation in the Hawley Creek area, Lehmi County, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:57","indexId":"ofr86427","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-427","title":"Analytical and stratigraphic data on the Retort Phosphatic Shale Member of the Phosphoria Formation in the Hawley Creek area, Lehmi County, Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86427","usgsCitation":"Oberlindacher, H., and Hovland, R.D., 1986, Analytical and stratigraphic data on the Retort Phosphatic Shale Member of the Phosphoria Formation in the Hawley Creek area, Lehmi County, Idaho: U.S. Geological Survey Open-File Report 86-427, 12 p. :map ;28 cm., https://doi.org/10.3133/ofr86427.","productDescription":"12 p. :map ;28 cm.","costCenters":[],"links":[{"id":146741,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0427/report-thumb.jpg"},{"id":44182,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0427/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f4e8","contributors":{"authors":[{"text":"Oberlindacher, H.P.","contributorId":44928,"corporation":false,"usgs":true,"family":"Oberlindacher","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":170788,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hovland, R. D.","contributorId":17620,"corporation":false,"usgs":false,"family":"Hovland","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":7217,"text":"Bureau of Land Management","active":true,"usgs":false}],"preferred":false,"id":170787,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":31056,"text":"ofr86501 - 1986 - Analytical results and sample locality map of heavy-mineral-concentrate and rock samples from the Black Rock Desert Wilderness Study Area (NV-020-620), Humboldt County, Nevada","interactions":[],"lastModifiedDate":"2022-01-10T19:57:15.630634","indexId":"ofr86501","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-501","title":"Analytical results and sample locality map of heavy-mineral-concentrate and rock samples from the Black Rock Desert Wilderness Study Area (NV-020-620), Humboldt County, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86501","usgsCitation":"Day, G., Turner, R.L., Gent, C.A., Crock, J., Bradley, L.A., and Fey, D., 1986, Analytical results and sample locality map of heavy-mineral-concentrate and rock samples from the Black Rock Desert Wilderness Study Area (NV-020-620), Humboldt County, Nevada: U.S. Geological Survey Open-File Report 86-501, Report: 15 p.; 1 Plate: 15.60 × 29.61 inches, https://doi.org/10.3133/ofr86501.","productDescription":"Report: 15 p.; 1 Plate: 15.60 × 29.61 inches","costCenters":[],"links":[{"id":59612,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0501/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59611,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0501/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164072,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0501/report-thumb.jpg"},{"id":394121,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17084.htm"}],"country":"United States","state":"Nevada","county":"Humboldt County","otherGeospatial":"Black Rock Desert Wilderness Study Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119,\n              40.75\n            ],\n            [\n              -118.5,\n              40.75\n            ],\n            [\n              -118.5,\n              41.5\n            ],\n            [\n              -119,\n              41.5\n            ],\n            [\n              -119,\n              40.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f525","contributors":{"authors":[{"text":"Day, G.W.","contributorId":63363,"corporation":false,"usgs":true,"family":"Day","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":204758,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turner, R. L.","contributorId":93903,"corporation":false,"usgs":true,"family":"Turner","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":204759,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gent, C. A.","contributorId":17955,"corporation":false,"usgs":true,"family":"Gent","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":204754,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crock, J.G.","contributorId":58236,"corporation":false,"usgs":true,"family":"Crock","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":204757,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bradley, L. A.","contributorId":35738,"corporation":false,"usgs":true,"family":"Bradley","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":204755,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Fey, D.L.","contributorId":44537,"corporation":false,"usgs":true,"family":"Fey","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":204756,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":30478,"text":"wri864320 - 1986 - Hydrologic and climatologic factors affecting water levels of Devils Lake, North Dakota","interactions":[],"lastModifiedDate":"2018-03-14T16:35:11","indexId":"wri864320","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4320","title":"Hydrologic and climatologic factors affecting water levels of Devils Lake, North Dakota","docAbstract":"<p>High water levels of Devils Lake, North Dakota, and other terminal lakes, have, in recent years, threatened highways, agricultural land, recreational cabins, and communities located near these lakes. This study was undertaken to describe the hydrology of the Devils Lake basin and to determine how to estimate future water level probabilities. </p><p>Analysis of the available hydrologic and climatologic data indicates the water level of Devils Lake fluctuates largely in response to climatic variability. Average annual net storage gain has varied from 70 ,000 acre-feet for 1969-83 to as little as 4,530 acre-feet for 1931-40. In addition to the influence of climatic variability on the inflow to Devils Lake, an interconnected chain of lakes upstream of Devils Lake retains runoff and acts as an evaporation basin for runoff from the Devils Lake basin. During 1965-67, at least 112,000 acre-feet of water was stored in this upstream chain of lakes. </p><p>A review of research conducted on other terminal lakes indicated that the water level in these lakes fluctuated primarily in response to climate variability. There is agreement between water level fluctuations of terminal lakes in Western North America and water level fluctuations of Devils lake during times of climatic extremes. </p><p>No standardized methods are available for computing water level probabilities of terminal lakes. Most of the development of a method for determining future water level probabilities has been focused on Great Salt Lake, Utah. A number of techniques have been used to estimate the future water-level probabilities for Great Salt Lake; however, they provide a wide range in probability of occurrence for any given water level. (Author 's abstract)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864320","usgsCitation":"Wiche, G.J., 1986, Hydrologic and climatologic factors affecting water levels of Devils Lake, North Dakota: U.S. Geological Survey Water-Resources Investigations Report 86-4320, iv, 62 p., https://doi.org/10.3133/wri864320.","productDescription":"iv, 62 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":59261,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4320/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4320/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611886","contributors":{"authors":[{"text":"Wiche, Gregg J. gjwiche@usgs.gov","contributorId":1675,"corporation":false,"usgs":true,"family":"Wiche","given":"Gregg","email":"gjwiche@usgs.gov","middleInitial":"J.","affiliations":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":203318,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30637,"text":"wri864109 - 1986 - Effects on ground water of spray irrigation using treated municipal sewage southwest of Tallahassee, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:09:00","indexId":"wri864109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4109","title":"Effects on ground water of spray irrigation using treated municipal sewage southwest of Tallahassee, Florida","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864109","usgsCitation":"Yurewicz, M., and Rosenau, J., 1986, Effects on ground water of spray irrigation using treated municipal sewage southwest of Tallahassee, Florida: U.S. Geological Survey Water-Resources Investigations Report 86-4109, v, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864109.","productDescription":"v, 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4109/report-thumb.jpg"},{"id":59402,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4109/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fa60","contributors":{"authors":[{"text":"Yurewicz, M.C.","contributorId":40237,"corporation":false,"usgs":true,"family":"Yurewicz","given":"M.C.","email":"","affiliations":[],"preferred":false,"id":203582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenau, J.C.","contributorId":99192,"corporation":false,"usgs":true,"family":"Rosenau","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":203583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12306,"text":"ofr864 - 1986 - Standards for digital elevation models","interactions":[],"lastModifiedDate":"2021-03-18T21:17:35.939521","indexId":"ofr864","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4","title":"Standards for digital elevation models","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr864","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Standards for digital elevation models: U.S. Geological Survey Open-File Report 86-4, 61 p., https://doi.org/10.3133/ofr864.","productDescription":"61 p.","costCenters":[],"links":[{"id":384468,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0004/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0004/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e47e2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528937,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69222,"text":"coal102 - 1986 - Surficial materials map of the Kemmerer 30' x 60' Quadrangle, Lincoln, Uinta, and Sweetwater counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:11:12","indexId":"coal102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":309,"text":"Coal Map","code":"COAL","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"102","title":"Surficial materials map of the Kemmerer 30' x 60' Quadrangle, Lincoln, Uinta, and Sweetwater counties, Wyoming","language":"ENGLISH","doi":"10.3133/coal102","usgsCitation":"Gibbons, A.B., 1986, Surficial materials map of the Kemmerer 30' x 60' Quadrangle, Lincoln, Uinta, and Sweetwater counties, Wyoming: U.S. Geological Survey Coal Map 102, 1 map :col. ;56 x 82 cm., on sheet 83 x 137 cm., https://doi.org/10.3133/coal102.","productDescription":"1 map :col. ;56 x 82 cm., on sheet 83 x 137 cm.","costCenters":[],"links":[{"id":111078,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19671.htm","linkFileType":{"id":5,"text":"html"},"description":"19671"},{"id":115489,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/coal/102/report.pdf","size":"22","linkFileType":{"id":1,"text":"pdf"}},{"id":115490,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/coal/102/plate-1.pdf","size":"15867","linkFileType":{"id":1,"text":"pdf"}},{"id":190197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/coal/102/report-thumb.jpg"}],"scale":"1","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,41.5 ], [ -111,42 ], [ -110,42 ], [ -110,41.5 ], [ -111,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68889e","contributors":{"authors":[{"text":"Gibbons, A. B.","contributorId":12016,"corporation":false,"usgs":true,"family":"Gibbons","given":"A.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":279839,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55817,"text":"wdrNM851 - 1986 - Water resources data, New Mexico, water year 1985","interactions":[],"lastModifiedDate":"2013-07-12T13:21:32","indexId":"wdrNM851","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NM-85-1","title":"Water resources data, New Mexico, water year 1985","docAbstract":"Water resources data for the 1985 water year for New Mexico consist of records of discharge and water quality of streams; stage, contents and water quality of lakes and reservoirs; and water levels and water quality in wells and springs. This report contains discharge records for 168 gaging stations; stage and contents for\n25 lakes and reservoirs; water quality for 65 gaging stations and 179 wells; and water levels at 111 observation wells. Also included are 138 crest-stage partial-record stations. Additional water data were collected at various sites, not involved in the systematic data collection program, and are published as miscellaneous measurements.  Also, one seepage investigation is published this year. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in New Mexico.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNM851","usgsCitation":"Denis, L.P., Beal, L.V., and Allen, H.R., 1986, Water resources data, New Mexico, water year 1985: U.S. Geological Survey Water Data Report NM-85-1, 496 p., https://doi.org/10.3133/wdrNM851.","productDescription":"496 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":185369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":270296,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/nm-85-1/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0502,31.3322 ], [ -109.0502,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.0502,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0d73","contributors":{"authors":[{"text":"Denis, Louis P.","contributorId":69654,"corporation":false,"usgs":true,"family":"Denis","given":"Louis","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":254314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beal, Linda V.","contributorId":26367,"corporation":false,"usgs":true,"family":"Beal","given":"Linda","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":254313,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allen, Harriet R.","contributorId":94683,"corporation":false,"usgs":true,"family":"Allen","given":"Harriet","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":254315,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15231,"text":"ofr86360 - 1986 - Summary of vitrinite reflectance and rock-eval pyrolysis data, Eagle Basin, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:55","indexId":"ofr86360","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-360","title":"Summary of vitrinite reflectance and rock-eval pyrolysis data, Eagle Basin, northwestern Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86360","usgsCitation":"Nuccio, V., Schenk, C.J., and Daws, T., 1986, Summary of vitrinite reflectance and rock-eval pyrolysis data, Eagle Basin, northwestern Colorado: U.S. Geological Survey Open-File Report 86-360, 5 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr86360.","productDescription":"5 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":146678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0360/report-thumb.jpg"},{"id":44179,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0360/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44180,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0360/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698893","contributors":{"authors":[{"text":"Nuccio, V. F.","contributorId":7713,"corporation":false,"usgs":true,"family":"Nuccio","given":"V. F.","affiliations":[],"preferred":false,"id":170782,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schenk, Christopher J. 0000-0002-0248-7305","orcid":"https://orcid.org/0000-0002-0248-7305","contributorId":72344,"corporation":false,"usgs":true,"family":"Schenk","given":"Christopher","email":"","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":170784,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Daws, T.A.","contributorId":56651,"corporation":false,"usgs":true,"family":"Daws","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":170783,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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