{"pageNumber":"4521","pageRowStart":"113000","pageSize":"25","recordCount":184743,"records":[{"id":49411,"text":"ofr89400J - 1989 - New information resources of the U.S. Geological Survey Library System, October 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:10:23","indexId":"ofr89400J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-400","chapter":"J","title":"New information resources of the U.S. Geological Survey Library System, October 1989","language":"ENGLISH","doi":"10.3133/ofr89400J","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, New information resources of the U.S. Geological Survey Library System, October 1989: U.S. Geological Survey Open-File Report 89-400, 52 p. ; 28 cm., https://doi.org/10.3133/ofr89400J.","productDescription":"52 p. ; 28 cm.","costCenters":[],"links":[{"id":169874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0400j/report-thumb.jpg"},{"id":86055,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0400j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697631","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":531931,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2083,"text":"wsp2337 - 1989 - Use of temperature profiles beneath streams to determine rates of vertical ground-water flow and vertical hydraulic conductivity","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp2337","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2337","title":"Use of temperature profiles beneath streams to determine rates of vertical ground-water flow and vertical hydraulic conductivity","docAbstract":"The use of temperature profiles beneath streams to determine rates of vertical ground-water flow and effective vertical hydraulic conductivity of sediments was evaluated at three field sites by use of a model that numerically solves the partial differential equation governing simultaneous vertical flow of fluid and heat in the Earth. The field sites are located in Hardwick and New Braintree, Mass., and in Dover, N.J. \r\n\r\nIn New England, stream temperature varies from about 0 to 25 ?C (degrees Celsius) during the year. This stream-temperature fluctuation causes ground-water temperatures beneath streams to fluctuate by more than 0.1 ?C during a year to a depth of about 35 ft (feet) in fine-grained sediments and to a depth of about 50 ft in coarse-grained sediments, if ground-water velocity is 0 ft/d (foot per day). Upward flow decreases the depth affected by stream-temperature fluctuation, and downward flow increases the depth. \r\n\r\nAt the site in Hardwick, Mass., ground-water flow was upward at a rate of less than 0.01 ft/d. The maximum effective vertical hydraulic conductivity of the sediments underlying this site is 0.1 ft/d. Ground-water velocities determined at three locations at the site in New Braintree, Mass., where ground water discharges naturally from the underlying aquifer to the Ware River, ranged from 0.10 to 0.20 ft/d upward. The effective vertical hydraulic conductivity of the sediments underlying this site ranged from 2.4 to 17.1 ft/d. Ground-water velocities determined at three locations at the Dover, N.J., site, where infiltration from the Rockaway River into the underlying sediments occurs because of pumping, were 1.5 ft/d downward. The effective vertical hydraulic conductivity of the sediments underlying this site ranged from 2.2 to 2.5 ft/d. Independent estimates of velocity at two of the three sites are in general agreement with the velocities determined using temperature profiles. The estimates of velocities and conductivities derived from the temperature measurements generally fall within the ranges of expected rates of flow in, and conductivities of, the sediments encountered at the test sites. \r\n\r\nApplication of the method at the three test sites demonstrates the feasibility of using the method to determine the rate of ground-water flow between a stream and underlying sediments and the effective vertical hydraulic conductivity of the sediments.","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nU.S. G.P.O. ;\r\nBooks and Open- File Reports Section, U.S. Geological Survey [distributor],","doi":"10.3133/wsp2337","usgsCitation":"Lapham, W.W., 1989, Use of temperature profiles beneath streams to determine rates of vertical ground-water flow and vertical hydraulic conductivity: U.S. Geological Survey Water Supply Paper 2337, v, 35 p. :ill. ;28 cm., https://doi.org/10.3133/wsp2337.","productDescription":"v, 35 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":138155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2337/report-thumb.jpg"},{"id":27645,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2337/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d1e4b07f02db5dbae2","contributors":{"authors":[{"text":"Lapham, Wayne W.","contributorId":74734,"corporation":false,"usgs":true,"family":"Lapham","given":"Wayne","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144651,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2611,"text":"wsp2302 - 1989 - Alluvial and bedrock aquifers of the Denver Basin — Eastern Colorado's dual ground-water resource","interactions":[],"lastModifiedDate":"2022-01-21T19:56:55.233074","indexId":"wsp2302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2302","title":"Alluvial and bedrock aquifers of the Denver Basin — Eastern Colorado's dual ground-water resource","docAbstract":"Large volumes of ground water are contained in alluvial and bedrock aquifers in the semiarid Denver basin of eastern Colorado. The bedrock aquifer, for example, contains 1.2 times as much water as Lake Erie of the Great Lakes, yet it supplies only about 9 percent of the ground water used in the basin. Although this seems to indicate underutilization of this valuable water supply, this is not necessarily the case, for many factors other than the volume of water in the aquifer affect the use of the aquifer. Such factors as climatic conditions, precipitation runoff, geology and water-yielding character of the aquifers, water-level conditions, volume of recharge and discharge, legal and economic constraints, and water-quality conditions can ultimately affect the decision to use ground water. Knowledge of the function and interaction of the various parts of this hydrologic system is important to the proper management and use of the ground-water resources of the region. \r\n\r\nThe semiarid climatic conditions on the Colorado plains produce flash floods of short duration and large peak-flow rates. However, snowmelt runoff from the Rocky Mountains produces the largest volumes of water and is typically of longer duration with smaller peak-flow rates. The alluvial aquifer is recharged easily from both types of runoff and readily stores and transmits the water because it consists of relatively thin deposits of gravel, sand, and clay located in the valleys of principal streams. The bedrock aquifer is recharged less easily because of its greater thickness (as much as 3,000 feet) and prevalent layers of shale which retard the downward movement of water in the formations. \r\n\r\nAlthough the bedrock aquifer contains more than 50 times as much water in storage as the alluvial aquifer, it does not store and transmit water as readily as the alluvial aquifer. For example, about 91 percent of the water pumped from wells is obtained from the alluvial aquifer, yet water-level declines generally have not exceeded 40 feet. By contrast, only 9 percent of the water pumped from wells is obtained from the bedrock aquifer, yet water-level declines in this aquifer have exceeded 500 feet in some areas. \r\n\r\nDepth to water in the alluvial aquifer generally is less than 40 feet, while depth to water in the bedrock aquifer may exceed 1,000 feet in some areas. Cost of pumping water to the surface and cost of maintaining existing supplies in areas of rapidly declining water levels in the bedrock aquifer affect water use. Water use is also affected by the generally poorer quality water found in the alluvial aquifer and, to a lesser extent, by the greater susceptibility of the alluvial aquifer to pollution from surface sources. \r\n\r\nBecause of these factors, the alluvial aquifer is used primarily as a source of irrigation supply, which is the largest water use in the area. The bedrock aquifer is used primarily as a source of domestic or municipal supply, which is the smaller of the two principal uses, even though the bedrock aquifer contains 50 times more stored ground water than the alluvial aquifer.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2302","usgsCitation":"Robson, S.G., 1989, Alluvial and bedrock aquifers of the Denver Basin — Eastern Colorado's dual ground-water resource: U.S. Geological Survey Water Supply Paper 2302, x, 40 p., https://doi.org/10.3133/wsp2302.","productDescription":"x, 40 p.","costCenters":[],"links":[{"id":394685,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25269.htm"},{"id":28898,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2302/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2302/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Denver Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.2870,\n              38.678\n            ],\n            [\n              -103.7,\n              38.678\n            ],\n            [\n              -103.7,\n              40.4360\n            ],\n            [\n              -105.2870,\n              40.4360\n            ],\n            [\n              -105.2870,\n              38.678\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68763b","contributors":{"authors":[{"text":"Robson, Stanley G.","contributorId":73187,"corporation":false,"usgs":true,"family":"Robson","given":"Stanley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145492,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25588,"text":"wri894033 - 1989 - Hydrologic and geochemical monitoring in Long Valley caldera, Mono County, California, 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri894033","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89-4033","title":"Hydrologic and geochemical monitoring in Long Valley caldera, Mono County, California, 1986","docAbstract":"The U.S. Geological Survey continued to monitor hydrologic and geochemical conditions in the Long Valley caldera during 1986. The monitoring is directed toward detecting changes in the hydrologic system caused by tectonic or magmatic processes. Data collected during 1986 include chemical and isotopic composition of water from selected streams sites, springs, and wells; pumpage from four geothermal wells; flow rates of selected springs and stream sites; mean daily water or gas temperatures at selected sites; mean daily atmospheric pressures and water level at selected wells, and precipitation records for two sites. Seismicity within the caldera persisted at a relatively low level compared with the more active periods of 1978-84. The most significant events of seismicity that affected hydrologic monitoring sites in Long Valley during 1986 occurred during July , in response to the Chalfant Valley earthquakes, centered about 20 miles southeast of the caldera. Water level records for three wells show distinct responses to the Chalfant Valley earthquakes. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri894033","usgsCitation":"Farrar, C.D., Sorey, M., Rojstaczer, S., Steinemann, A., and Clark, M.D., 1989, Hydrologic and geochemical monitoring in Long Valley caldera, Mono County, California, 1986: U.S. Geological Survey Water-Resources Investigations Report 89-4033, vi, 69 p. :ill. ;28 cm., https://doi.org/10.3133/wri894033.","productDescription":"vi, 69 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":118877,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4033/report-thumb.jpg"},{"id":54330,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4033/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611851","contributors":{"authors":[{"text":"Farrar, C. D.","contributorId":71978,"corporation":false,"usgs":true,"family":"Farrar","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":194314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":194315,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rojstaczer, S.A.","contributorId":54620,"corporation":false,"usgs":true,"family":"Rojstaczer","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":194312,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steinemann, A.C.","contributorId":71214,"corporation":false,"usgs":true,"family":"Steinemann","given":"A.C.","affiliations":[],"preferred":false,"id":194313,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Clark, M. D.","contributorId":25202,"corporation":false,"usgs":true,"family":"Clark","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":194311,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":25607,"text":"wri884235 - 1989 - Hydrology of the Goat Lake watershed, Snohomish County, Washington, 1982-87","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"wri884235","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4235","title":"Hydrology of the Goat Lake watershed, Snohomish County, Washington, 1982-87","docAbstract":"The Goat Lake watershed in Snohomish County, Washington, functions as an '  experimental watershed ' for long-term studies to determine the effects of acidic precipitation on water resources. Data have been collected there by the U.S. Geological Survey since 1982. The watershed is in a wilderness area of the Cascade Range and is downwind of an industrial and urban area that produces chemical compounds found in acidic precipitation.  The lake is considered sensitive to acidic inputs from atmospheric deposition and streamflow. The mean annual discharge of the Goat Lake outflow is 35 cu ft/sec; precipitation on the watershed is calculated to be about 170 in/yr. The inflow to Goat Lake is sufficient to replace the entire contents of the lake basin on an average every 21.5 days, or 17 times/year. Water in Goat Lake, and that of the inlet and outlet, is of low ionic strength and of calcium-bicarbonate type. The lake, although considered oligotrophic, is sufficiently deep to stratify thermally, and summer dissolved-oxygen concentrations in the hypolimnion are depressed. Even though alkalinity and specific conductance at Goat Lake are in the range considered sensitive to acidic inputs , the pH of water in the lake has consistently ranged from 6.1 to 7.2, indicating that the lake is not acidified at this time. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri884235","usgsCitation":"Dion, N.P., Ebbert, J., Poole, J., and Peck, B., 1989, Hydrology of the Goat Lake watershed, Snohomish County, Washington, 1982-87: U.S. Geological Survey Water-Resources Investigations Report 88-4235, iv, 44 p. :ill. ;28 cm., https://doi.org/10.3133/wri884235.","productDescription":"iv, 44 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":122974,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4235/report-thumb.jpg"},{"id":54351,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4235/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acbe4b07f02db67e3a4","contributors":{"authors":[{"text":"Dion, N. P.","contributorId":33302,"corporation":false,"usgs":true,"family":"Dion","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":194385,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ebbert, J.C.","contributorId":57451,"corporation":false,"usgs":true,"family":"Ebbert","given":"J.C.","affiliations":[],"preferred":false,"id":194387,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poole, J.E.","contributorId":70764,"corporation":false,"usgs":true,"family":"Poole","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":194388,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peck, B.S.","contributorId":46128,"corporation":false,"usgs":true,"family":"Peck","given":"B.S.","email":"","affiliations":[],"preferred":false,"id":194386,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25624,"text":"wri884072 - 1989 - Low-flow characteristics of streams in West Virginia","interactions":[],"lastModifiedDate":"2022-01-20T20:56:58.219486","indexId":"wri884072","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4072","title":"Low-flow characteristics of streams in West Virginia","docAbstract":"<p>Low-flow characteristics of selected streams in West Virginia were determined at continuous-record and partial-record sites. Daily discharges at 100 continuous-record gaging stations on unregulated streams were used to compute selected low-flow frequency values. Estimates of low-flow frequency values at 296 partial-record sites (ones having only discharge measurements) were made using the relation defined by concurrent flows with a continuous-record station. Low-flow characteristics at continuous-record stations were related to drainage area and a variability index to produce equations which can be used to estimate low-flow characteristics at ungaged sites in West Virginia. The State was divided into two hydrologic regions. Drainage area and a streamflow-variability index were determined to be the most significant. The streamflow variability index was computed from duration curves and was used to account for the integrated effects of geology and other hydrologic characteristics. The standard error of estimate for the 7-day low flow with a 2-year recurrence interval is 43% for Region 1 and 57% for Region 2. The standard error of estimate for the 7-day low flow with a 10-year recurrence interval is 82% for Region 1 and 83% for Region 2.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884072","usgsCitation":"Friel, E., Embree, W., Jack, A.R., and Atkins, J.T., 1989, Low-flow characteristics of streams in West Virginia: U.S. Geological Survey Water-Resources Investigations Report 88-4072, Report: iv, 34 p.; 2 Plates: 18.32 × 16.40 inches and 18.38 × 16.57 inches, https://doi.org/10.3133/wri884072.","productDescription":"Report: iv, 34 p.; 2 Plates: 18.32 × 16.40 inches and 18.38 × 16.57 inches","costCenters":[],"links":[{"id":54369,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4072/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394616,"rank":5,"type":{"id":36,"text":"NGMDB Index 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R.","contributorId":48597,"corporation":false,"usgs":true,"family":"Jack","given":"A.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":194456,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Atkins, J. T. Jr.","contributorId":29474,"corporation":false,"usgs":true,"family":"Atkins","given":"J.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":194455,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25130,"text":"cir930H - 1989 - International strategic minerals inventory summary report; natural graphite","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"cir930H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"930","chapter":"H","title":"International strategic minerals inventory summary report; natural graphite","docAbstract":"Natural graphite is a crystalline mineral of pure carbon which normally occurs in the form of platelet-shaped crystals. It has important properties, such as chemical inertness, low thermal expansion, and lubricity, that make it almost irreplaceable for certain uses such as refractories and steelmaking. Graphite ore types are crystalline (flake and lump} or 'amorphous' (cryptocrystalline}. Refractory applications use the largest total amount of natural graphite, while the most important use of crystalline graphite is in crucibles for handling molten metals. All graphite deposits being mined today are found in the following metamorphic environments: (1) contact metamorphosed coal generally is a source of amorphous graphite; (2)disseminated crystalline flake graphite comes from syngenetic metasediments; and (3) crystalline lump graphite is found in epigenetic veins in high-grade metamorphic regions. Graphite may also occur as a trace mineral in ultrabasic rocks and pegmatites, but these are economically insignificant. The world's identified economically exploitable resources of crystalline graphite in major deposits are estimated to be about 9.7 million metric tons of concentrate. In-place resources of amorphous graphite are about 11.5 million metric tons. Of these, less than 2 percent of the crystalline ore and less than 1 percent of the amorphous ore are in western industrial countries. World mining production of natural graphite rose from 347,000 metric tons in 1973 to 659,000 metric tons in 1986, while the proportion produced by central economy countries increased from about 50 percent for the period from 1973 to 1978 to more than 64 percent in 1979 to 1986. It is estimated that crystalline flake graphite accounts for at least 180,000 metric tons of total annual world mining production of natural graphite, and amorphous graphite makes up the rest.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir930H","usgsCitation":"Krauss, U., Schmidt, H., Taylor, H., and Sutphin, D.M., 1989, International strategic minerals inventory summary report; natural graphite: U.S. Geological Survey Circular 930, v. :ill. ;26 cm.; 29 p., https://doi.org/10.3133/cir930H.","productDescription":"v. :ill. ;26 cm.; 29 p.","costCenters":[],"links":[{"id":124484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1989/0930h/report-thumb.jpg"},{"id":54110,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1989/0930h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cde4b07f02db544d63","contributors":{"authors":[{"text":"Krauss, U.H.","contributorId":47404,"corporation":false,"usgs":true,"family":"Krauss","given":"U.H.","email":"","affiliations":[],"preferred":false,"id":193269,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmidt, H.W.","contributorId":103710,"corporation":false,"usgs":true,"family":"Schmidt","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":193271,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, H.A. Jr.","contributorId":100024,"corporation":false,"usgs":true,"family":"Taylor","given":"H.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":193270,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sutphin, D. M.","contributorId":27424,"corporation":false,"usgs":true,"family":"Sutphin","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":193268,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":55702,"text":"wdrMO881 - 1989 - Water resources data, Missouri, water year 1988","interactions":[],"lastModifiedDate":"2019-11-22T14:18:47","indexId":"wdrMO881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"MO-88-1","title":"Water resources data, Missouri, water year 1988","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrMO881","usgsCitation":"Waite, L., Davis, J.V., Reed, H., Hatten, D., and Perkins, T., 1989, Water resources data, Missouri, water year 1988: U.S. Geological Survey Water Data Report MO-88-1, x, 290 p., https://doi.org/10.3133/wdrMO881.","productDescription":"x, 290 p.","costCenters":[],"links":[{"id":369476,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1988/mo-88-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1988/mo-88-1/report-thumb.jpg"}],"country":"United States","state":"Missouri","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.7568359375,\n              35.94243575255426\n            ],\n            [\n              -89.14306640625,\n              35.94243575255426\n            ],\n            [\n              -89.14306640625,\n              40.56389453066509\n            ],\n            [\n              -95.7568359375,\n              40.56389453066509\n            ],\n            [\n              -95.7568359375,\n              35.94243575255426\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f1119","contributors":{"authors":[{"text":"Waite, L.A.","contributorId":40995,"corporation":false,"usgs":true,"family":"Waite","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":254060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Jerri V. jdavis@usgs.gov","contributorId":99149,"corporation":false,"usgs":true,"family":"Davis","given":"Jerri","email":"jdavis@usgs.gov","middleInitial":"V.","affiliations":[],"preferred":false,"id":254062,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, H.L.","contributorId":14886,"corporation":false,"usgs":true,"family":"Reed","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":254058,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hatten, D.O.","contributorId":29057,"corporation":false,"usgs":true,"family":"Hatten","given":"D.O.","email":"","affiliations":[],"preferred":false,"id":254059,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Perkins, T.J.","contributorId":76815,"corporation":false,"usgs":true,"family":"Perkins","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":254061,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":25934,"text":"wri894065 - 1989 - Stratigraphy of the unsaturated zone at the radioactive waste management complex, Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri894065","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89-4065","title":"Stratigraphy of the unsaturated zone at the radioactive waste management complex, Idaho National Engineering Laboratory, Idaho","docAbstract":"A complex sequence of layered basalt flows, cinders, and sediment underlies the Radioactive Waste Management Complex at the Idaho National Engineering Laboratory in southeastern Idaho. Wells drilled to 700 ft penetrate a sequence of 10 basalt-flow groups and 7 major sedimentary interbeds that range in age from about 100,000 to 600,000 years old. The 10 flow groups consist of 22 separate lava flows and flow-units. Each flow group is made up of from one to five petrographically similar flows that erupted from common source areas during periods of less than 200 years. Sedimentary interbeds consist of fluvial, lacustrine, and wind-blown deposits of clay, silt, sand, and gravel that accumulated during periods of volcanic inactivity ranging from thousands to hundreds of thousands of years. Flows and sediment are unsaturated to a depth of about 600 ft. Flows and sediment below a depth of 600 ft are saturated and make up the uppermost part of the Snake River Plain aquifer. The areal extent of flow groups and interbeds was determined from well cuttings, cores, geophysical logs, potassium-argon ages, and geomagnetic properties. Stratigraphical control was provided by four sequential basalt flows near the base of the unsaturated zone that have reversed geomagnetic polarity and high emission of natural gamma radiation compared to other flows. Natural gamma logs were used as a primary correlation tool. Natural-gamma emissions, which are generally uniform in related, petrographically similar flows, increase or decrease between petrographically dissimilar flows of different age and source. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nCopies of this report can be purchased from Books and Open-File Reports Section,","doi":"10.3133/wri894065","usgsCitation":"Anderson, S.R., and Lewis, B.D., 1989, Stratigraphy of the unsaturated zone at the radioactive waste management complex, Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 89-4065, v, 54 p. :ill ;28 cm., https://doi.org/10.3133/wri894065.","productDescription":"v, 54 p. :ill ;28 cm.","costCenters":[],"links":[{"id":158056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4065/report-thumb.jpg"},{"id":54691,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4065/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a5492","contributors":{"authors":[{"text":"Anderson, S. R.","contributorId":93518,"corporation":false,"usgs":true,"family":"Anderson","given":"S.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":195508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, B. D.","contributorId":85965,"corporation":false,"usgs":true,"family":"Lewis","given":"B.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":195507,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26231,"text":"wri884211 - 1989 - Relation of ground-water quality to land use in the Philadelphia, Pennsylvania-Camden, New Jersey area","interactions":[],"lastModifiedDate":"2022-08-29T18:40:14.749232","indexId":"wri884211","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4211","title":"Relation of ground-water quality to land use in the Philadelphia, Pennsylvania-Camden, New Jersey area","docAbstract":"The distributions of common dissolved constituents, trace metals, and volatile organic compounds in ground water near Philadelphia, Pennsylvania, and Camden, New Jersey, are influenced by local geology and land use. Many common dissolved constituents are more concentrated in ground water beneath urban and industrial areas than in water beneath suburban and undeveloped and agricultural areas. Industrial and urban land uses commonly are situated in the outcrop of the aquifer where vulnerability of ground water to contamination is increased by the lack of overlying confining strata. Ground water beneath undeveloped and agricultural lands is least affected by trace metal or volatile organic contamination, but differences in water quality as related to other land-use categories are less clear and vary according to the chemical constituent considered.\r\n\r\n      Only about 20 percent of all water samples contained detectable concentrations of trace metals or volatile organic compounds; as a result, determinations of relations between water quality and land use are difficult. Variations in detection limits further complicated data interpretation. The proportion of water samples in which concentrations of constituents were below detection compared to water samples in which concentrations were present in detectable amounts is the most useful statistic in determining relations based on trace-metal or volatile organic-compound data. Iron and Manganese concentrations are elevated in water throughout the Coastal Plain aquifer in Pennsylvania, but the elevated concentrations cannot be adequately explained on the basis of land use alone.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884211","usgsCitation":"Blickwedel, R.S., and Wood, C.R., 1989, Relation of ground-water quality to land use in the Philadelphia, Pennsylvania-Camden, New Jersey area: U.S. Geological Survey Water-Resources Investigations Report 88-4211, vi, 58 p., https://doi.org/10.3133/wri884211.","productDescription":"vi, 58 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":405825,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47110.htm","linkFileType":{"id":5,"text":"html"}},{"id":55030,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4211/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4211/report-thumb.jpg"}],"country":"United States","state":"New Jersey, Pennsylvania","city":"Camden, Philadelphia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.42938232421875,\n              39.70296052957233\n            ],\n            [\n              -74.84161376953125,\n              39.70296052957233\n            ],\n            [\n              -74.84161376953125,\n              40.143189742924406\n            ],\n            [\n              -75.42938232421875,\n              40.143189742924406\n            ],\n            [\n              -75.42938232421875,\n              39.70296052957233\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606740","contributors":{"authors":[{"text":"Blickwedel, Ray S.","contributorId":23984,"corporation":false,"usgs":true,"family":"Blickwedel","given":"Ray","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":196024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, C. R.","contributorId":100386,"corporation":false,"usgs":true,"family":"Wood","given":"C.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":196025,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2572,"text":"wsp2334 - 1989 - Evapotranspiration estimates using remote-sensing data, Parker and Palo Verde valleys, Arizona and California","interactions":[{"subject":{"id":15575,"text":"ofr8667 - 1986 - Evapotranspiration estimates using remote-sensing data, Parker and Palo Verde Valleys, Arizona and California","indexId":"ofr8667","publicationYear":"1986","noYear":false,"title":"Evapotranspiration estimates using remote-sensing data, Parker and Palo Verde Valleys, Arizona and California"},"predicate":"SUPERSEDED_BY","object":{"id":2572,"text":"wsp2334 - 1989 - Evapotranspiration estimates using remote-sensing data, Parker and Palo Verde valleys, Arizona and California","indexId":"wsp2334","publicationYear":"1989","noYear":false,"title":"Evapotranspiration estimates using remote-sensing data, Parker and Palo Verde valleys, Arizona and California"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"wsp2334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2334","title":"Evapotranspiration estimates using remote-sensing data, Parker and Palo Verde valleys, Arizona and California","docAbstract":"In 1981 the U.S. Geological Survey established an experimental project to assess the possible and practical use of remote-sensing data to estimate evapotranspiration as an approximation of consumptive use of water in the lower Colorado River flood plain. The project area was in Parker Valley, Arizona. The approach selected was to measure the areas covered by each type of vegetation, using remote-sensing data in various types of analyses, and to multiply each area by a predetermined water-use rate. \r\n\r\nTwo calibration and six remote-sensing methods of classifying crop types were compared for cost, accuracy, consistency, and labor requirements. Included were one method each for field reconnaissance using 1982 data, low-altitude (less than 5,000 feet) aerial photography using 1982 data, and visual photointerpretation of Landsat satellite images using 1981 and 1982 data; two methods for medium-altitude (15,000-18,000 feet) aerial photography using 1982 data; and three methods for digital Landsat satellite images using 1981 data. A test of the most promising digital-processing method, which used three image dates, was made in part of Palo Verde Valley, California, where 1981 crop data were more complete than in Parker Valley. \r\n\r\nOf the eight methods studied, the two-date digital-processing method was the most consistent and least labor intensive for identifying two or three major crops; visual photointerpretation of Landsat images was the least expensive. Evapotranspiration estimates from crop classifications by all methods differed by a maximum of 6 percent. Total evapotranspiration calculated from crop data and phreatophyte maps in 1981 ranged from 11 percent lower in Palo Verde Valley to 17 percent lower in Parker Valley than consumptive use calculated by water budgets. The difference was greater in Parker Valley because the winter crop data were not included.","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nFor sale by the Books and Open-File Reports Section,","doi":"10.3133/wsp2334","usgsCitation":"Raymond, L.H., and Rezin, K.V., 1989, Evapotranspiration estimates using remote-sensing data, Parker and Palo Verde valleys, Arizona and California: U.S. Geological Survey Water Supply Paper 2334, iv, 18 p. :ill. (some col.), maps ;28 cm., https://doi.org/10.3133/wsp2334.","productDescription":"iv, 18 p. :ill. (some col.), maps ;28 cm.","costCenters":[],"links":[{"id":138599,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2334/report-thumb.jpg"},{"id":28843,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2334/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9b71","contributors":{"authors":[{"text":"Raymond, Lee H.","contributorId":83501,"corporation":false,"usgs":true,"family":"Raymond","given":"Lee","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145422,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rezin, Kelly V.","contributorId":18744,"corporation":false,"usgs":true,"family":"Rezin","given":"Kelly","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":145421,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60923,"text":"mf2071A - 1989 - Geochemical maps showing the distribution and abundance of selected elements in stream-sediment samples, Solomon and Bendeleben 1° x 3° quadrangles, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2021-11-08T19:16:33.493326","indexId":"mf2071A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"2071","chapter":"A","title":"Geochemical maps showing the distribution and abundance of selected elements in stream-sediment samples, Solomon and Bendeleben 1° x 3° quadrangles, Seward Peninsula, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf2071A","usgsCitation":"Smith, S., King, H.D., and O’Leary, R.M., 1989, Geochemical maps showing the distribution and abundance of selected elements in stream-sediment samples, Solomon and Bendeleben 1° x 3° quadrangles, Seward Peninsula, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 2071, 14 p., https://doi.org/10.3133/mf2071A.","productDescription":"14 p.","costCenters":[],"links":[{"id":179782,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1989/2071a/report-thumb.jpg"},{"id":105223,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5671.htm","linkFileType":{"id":5,"text":"html"},"description":"5671"},{"id":88901,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1989/2071a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Seward PeninsulaSolomon and Bendeleben 1° x 3° quadrangles","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -165,64.25 ], [ -165,66 ], [ -162,66 ], [ -162,64.25 ], [ -165,64.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf1f","contributors":{"authors":[{"text":"Smith, S.C.","contributorId":16833,"corporation":false,"usgs":true,"family":"Smith","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":264623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":264625,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O’Leary, R. M.","contributorId":44894,"corporation":false,"usgs":true,"family":"O’Leary","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":264624,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26371,"text":"wri894152 - 1989 - Geology and ground-water resources of the San Carlos Indian Reservation, Gila, Graham, and Pinal counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:32","indexId":"wri894152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89-4152","title":"Geology and ground-water resources of the San Carlos Indian Reservation, Gila, Graham, and Pinal counties, Arizona","docAbstract":"The San Carlos Indian Reservation includes about 2,900 sq mi in east- central Arizona. Relatively impermeable pre-Tertiary rocks are exposed in about 23% of the reservation and underlie water-bearing Tertiary and quaternary basin fill and Quaternary stream alluvium in much of the southern part of the reservation. About 9,000 members of the San Carlos Apache Tribe live on the reservation and rely on groundwater to meet public supply, irrigation, and other needs. Basin fill is widespread in the valley of the San Carlos and Gila Rivers and consists of fine sand, silt, limestone, clay, and pyroclastic volcanics that may attain a total maximum thickness of more than 3,200 ft in the reservation. Quaternary stream alluvium overlies the basin fill along many streams and washes. Stream alluvium consists of poorly sorted, unconsolidated, gravelly, muddy, sand; and sandy gravel and reaches a maximum thickness of 100 ft along the San Carlos and Gila Rivers. The volume of recoverable water stored in the basin fill to a depth of 1,200 ft is estimated to be about 20 million acre-ft. The volume of recoverable water stored in the stream alluvium on the reservation is estimated to be more than 100,000 acre-ft. The stream alluvium along the San Carlos River supplies most of the water used for drinking. Water throughout much of the reservation is suitable for most uses except for that in the alluvium along the Gila River, which contains large concentrations of dissolved solids. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri894152","usgsCitation":"Brown, J.G., 1989, Geology and ground-water resources of the San Carlos Indian Reservation, Gila, Graham, and Pinal counties, Arizona: U.S. Geological Survey Water-Resources Investigations Report 89-4152, v, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri894152.","productDescription":"v, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":110254,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47240.htm","linkFileType":{"id":5,"text":"html"},"description":"47240"},{"id":122881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4152/report-thumb.jpg"},{"id":55163,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4152/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55164,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4152/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55165,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4152/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6835de","contributors":{"authors":[{"text":"Brown, J. G.","contributorId":28263,"corporation":false,"usgs":true,"family":"Brown","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":196273,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26323,"text":"wri894094 - 1989 - Contrasts of vegetation, soils, microclimates, and geomorphic processes between north- and south-facing slopes on Green Mountain near Denver, Colorado","interactions":[],"lastModifiedDate":"2019-08-20T12:25:19","indexId":"wri894094","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89-4094","title":"Contrasts of vegetation, soils, microclimates, and geomorphic processes between north- and south-facing slopes on Green Mountain near Denver, Colorado","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri894094","usgsCitation":"Branson, F.A., and Shown, L.M., 1989, Contrasts of vegetation, soils, microclimates, and geomorphic processes between north- and south-facing slopes on Green Mountain near Denver, Colorado: U.S. Geological Survey Water-Resources Investigations Report 89-4094, v, 18 p. , https://doi.org/10.3133/wri894094.","productDescription":"v, 18 p. ","costCenters":[],"links":[{"id":157654,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4094/report-thumb.jpg"},{"id":366724,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4094/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","city":"Denver","otherGeospatial":"Green Mountain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.19203186035155,\n              39.678126804900295\n            ],\n            [\n              -105.14911651611328,\n              39.678126804900295\n            ],\n            [\n              -105.14911651611328,\n              39.71537404178252\n            ],\n            [\n              -105.19203186035155,\n              39.71537404178252\n            ],\n            [\n              -105.19203186035155,\n              39.678126804900295\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69859c","contributors":{"authors":[{"text":"Branson, Farrel Allen","contributorId":53823,"corporation":false,"usgs":true,"family":"Branson","given":"Farrel","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":196180,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shown, Lynn M.","contributorId":7326,"corporation":false,"usgs":true,"family":"Shown","given":"Lynn","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":196179,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26778,"text":"wri884077 - 1989 - Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 10","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri884077","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4077","title":"Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 10","docAbstract":"This report delineates and describes the geohydrology and susceptibility of major aquifers to contamination in Area 10--Choctaw, Clarke, and Washington Counties in southwest Alabama. The major aquifers in the study area are the Nanafalia-Clayton, Lisbon, and Pliocene-Miocene aquifers of Tertiary age. The recharge areas for these aquifers generally coincide with their areas of use. Each aquifer is a source of public water supply in one or more of the three counties. All recharge areas for the major aquifers are susceptible to contamination from the surface. However, large parts of the recharge areas are rural areas that are used for timberlands, farms, and pastures; these areas have low potential for contamination and are several miles from pumping centers. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/wri884077","usgsCitation":"DeJarnette, S., 1989, Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 10: U.S. Geological Survey Water-Resources Investigations Report 88-4077, v, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884077.","productDescription":"v, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4077/report-thumb.jpg"},{"id":55661,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4077/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55662,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4077/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae053","contributors":{"authors":[{"text":"DeJarnette, S.S.","contributorId":6896,"corporation":false,"usgs":true,"family":"DeJarnette","given":"S.S.","affiliations":[],"preferred":false,"id":196988,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41742,"text":"ofr8957 - 1989 - Approximate water-level changes in wells completed in the Chicot and Evangeline aquifers, 1977-89 and 1988-89, and measured compaction, 1973-89, in the Houston-Galveston region, Texas","interactions":[],"lastModifiedDate":"2016-08-15T08:14:04","indexId":"ofr8957","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-57","title":"Approximate water-level changes in wells completed in the Chicot and Evangeline aquifers, 1977-89 and 1988-89, and measured compaction, 1973-89, in the Houston-Galveston region, Texas","docAbstract":"<p>This report presents data on water-level changes in the Chinot and Evangeline aquifers during 1977-89 and 1988-89 and data on measured compaction during 1973-89.</p>\n<p>Measurements of water level in 307 wells were used to construct the maps showing water-level changes. Compaction data were obtained from 12 wells equipped with compaction monitors at 11 sites.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr8957","collaboration":"Prepared in cooperation with the City of Houston and the Harris-Galveston Coastal Subsidence District","usgsCitation":"Barbie, D.L., Coplin, L., and Bonnet, C., 1989, Approximate water-level changes in wells completed in the Chicot and Evangeline aquifers, 1977-89 and 1988-89, and measured compaction, 1973-89, in the Houston-Galveston region, Texas: U.S. Geological Survey Open-File Report 89-57, 8 p., https://doi.org/10.3133/ofr8957.","productDescription":"8 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":79450,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0057/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":176585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0057/report-thumb.jpg"}],"country":"United States","state":"Texas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a263","contributors":{"authors":[{"text":"Barbie, Dana L.","contributorId":64632,"corporation":false,"usgs":true,"family":"Barbie","given":"Dana","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":225458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coplin, L.S.","contributorId":49366,"corporation":false,"usgs":true,"family":"Coplin","given":"L.S.","affiliations":[],"preferred":false,"id":225457,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bonnet, C.W.","contributorId":44535,"corporation":false,"usgs":true,"family":"Bonnet","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":225456,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20030,"text":"ofr89641 - 1989 - Geologic evidence for triggered slip on the Calaveras fault during the magnitude 7.1 Loma Prieta earthquake of October 17, 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:07:45","indexId":"ofr89641","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-641","title":"Geologic evidence for triggered slip on the Calaveras fault during the magnitude 7.1 Loma Prieta earthquake of October 17, 1989","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89641","usgsCitation":"McClellan, P., and Hay, E., 1989, Geologic evidence for triggered slip on the Calaveras fault during the magnitude 7.1 Loma Prieta earthquake of October 17, 1989: U.S. Geological Survey Open-File Report 89-641, 37 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89641.","productDescription":"37 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":153159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0641/report-thumb.jpg"},{"id":49560,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0641/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a61fe","contributors":{"authors":[{"text":"McClellan, P.H.","contributorId":62611,"corporation":false,"usgs":true,"family":"McClellan","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":181933,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hay, E.A.","contributorId":41851,"corporation":false,"usgs":true,"family":"Hay","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":181932,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29566,"text":"wri884170 - 1989 - Effects of three highway-runoff detention methods on water quality of the surficial aquifer system in central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:09:02","indexId":"wri884170","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4170","title":"Effects of three highway-runoff detention methods on water quality of the surficial aquifer system in central Florida","docAbstract":"Water quality of the surficial aquifer system in central Florida was evaluated at one exfiltration pipe, two ponds (detention and retention), and two swales in central Florida, representing three runoff-detention methods, to detect any effect from infiltrating highway runoff. Concentrations of major ions, metals, and nutrients in groundwater and bottom sediments were measured from 1984 through 1986. At each study area, constituent concentrations in groundwater near the structure were compared to concentrations in groundwater from an upgradient control site. Groundwater quality data were also pooled by detention method and statistically compared to detect any significant differences between methods. Significantly greater mean phosphorus concentrations in groundwater near the exfiltration pipe than those in the control well was the only evidence of increasing constituent concentrations in groundwater near structures. The quality of water was more variable, and had greater constituent concentrations in the unsaturated zone than in the saturated zone near the exfiltration pipe. Values of water quality variables measured in groundwater at all study areas generally were within State drinking water standards. The main exception was dissolved iron, which commonly exceeded 300 micrograms/L at one swale and the detention pond. Results of the study indicate that natural processes occurring in soils attenuate inorganic constituent concentrations prior to reaching the receiving groundwater. However, organic compounds detected in bottom sediments at the retention pond indicate a potential problem that may eventually affect the quality of the receiving groundwater. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri884170","usgsCitation":"Schiffer, D., 1989, Effects of three highway-runoff detention methods on water quality of the surficial aquifer system in central Florida: U.S. Geological Survey Water-Resources Investigations Report 88-4170, vi, 79 p. :ill. ;28 cm., https://doi.org/10.3133/wri884170.","productDescription":"vi, 79 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":2388,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri884170/","linkFileType":{"id":5,"text":"html"}},{"id":123321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4170/report-thumb.jpg"},{"id":58395,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4170/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae9ea","contributors":{"authors":[{"text":"Schiffer, D. M.","contributorId":102103,"corporation":false,"usgs":true,"family":"Schiffer","given":"D. M.","affiliations":[],"preferred":false,"id":201728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15745,"text":"ofr89110 - 1989 - Statistical summaries of elemental constituents in streambed-sediments in the lower Kansas River basin; Nebraska, Kansas, and Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:06:47","indexId":"ofr89110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-110","title":"Statistical summaries of elemental constituents in streambed-sediments in the lower Kansas River basin; Nebraska, Kansas, and Missouri","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89110","usgsCitation":"Ryder, J.L., and Sanzolone, R.F., 1989, Statistical summaries of elemental constituents in streambed-sediments in the lower Kansas River basin; Nebraska, Kansas, and Missouri: U.S. Geological Survey Open-File Report 89-110, ii, 28 p. ill., maps ;29 cm., https://doi.org/10.3133/ofr89110.","productDescription":"ii, 28 p. ill., maps ;29 cm.","costCenters":[],"links":[{"id":146516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0110/report-thumb.jpg"},{"id":44761,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e1d6f","contributors":{"authors":[{"text":"Ryder, Jean L.","contributorId":80709,"corporation":false,"usgs":true,"family":"Ryder","given":"Jean","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sanzolone, R. F.","contributorId":64199,"corporation":false,"usgs":true,"family":"Sanzolone","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":171633,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15723,"text":"ofr89204 - 1989 - Magnetic susceptibilities of modally analyzed granitic rocks from the southern Sierra Nevada, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr89204","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-204","title":"Magnetic susceptibilities of modally analyzed granitic rocks from the southern Sierra Nevada, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89204","usgsCitation":"Ross, D., 1989, Magnetic susceptibilities of modally analyzed granitic rocks from the southern Sierra Nevada, California: U.S. Geological Survey Open-File Report 89-204, v, 53 p. ill. ;28 cm., https://doi.org/10.3133/ofr89204.","productDescription":"v, 53 p. ill. ;28 cm.","costCenters":[],"links":[{"id":148606,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0204/report-thumb.jpg"},{"id":44745,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0204/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649374","contributors":{"authors":[{"text":"Ross, Donald Clarence","contributorId":49768,"corporation":false,"usgs":true,"family":"Ross","given":"Donald Clarence","affiliations":[],"preferred":false,"id":171601,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20255,"text":"ofr88641 - 1989 - Chemistry of Lake Tahoe, California-Nevada, and nearby springs","interactions":[],"lastModifiedDate":"2012-02-02T00:07:43","indexId":"ofr88641","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-641","title":"Chemistry of Lake Tahoe, California-Nevada, and nearby springs","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr88641","usgsCitation":"Nathenson, M., 1989, Chemistry of Lake Tahoe, California-Nevada, and nearby springs: U.S. Geological Survey Open-File Report 88-641, 27 p. ill., map ;28 cm., https://doi.org/10.3133/ofr88641.","productDescription":"27 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":153400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0641/report-thumb.jpg"},{"id":49795,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0641/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e31b0","contributors":{"authors":[{"text":"Nathenson, Manuel 0000-0002-5216-984X mnathnsn@usgs.gov","orcid":"https://orcid.org/0000-0002-5216-984X","contributorId":1358,"corporation":false,"usgs":true,"family":"Nathenson","given":"Manuel","email":"mnathnsn@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":182337,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26935,"text":"wri884118 - 1989 - Reconnaissance of water quality of Pueblo Reservoir, Colorado: May through December 1985","interactions":[],"lastModifiedDate":"2022-12-22T19:32:21.832056","indexId":"wri884118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4118","title":"Reconnaissance of water quality of Pueblo Reservoir, Colorado: May through December 1985","docAbstract":"<p>Pueblo Reservoir is the farthest upstream, main-stream reservoir constructed on the Arkansas River and is located in Pueblo County approximately 6 miles upstream from the city of Pueblo, Colorado. During the 1985 sampling period, the reservoir was stratified, and underflow from the Arkansas River occurred that resulted in stratification with respect to specific conductance. Concentrations of dissolved solids decreased markedly below the thermocline during June. Later in the summer, dissolved-solids concentrations increased substantially below the thermocline. Substantial depletion of dissolved oxygen occurred near the bottom of the reservoir. The dissolved oxygen minimum of 0.1 mg/L occurred during August near the reservoir bottom at transect 7 (near the dam). The average total-inorganic-nitrogen concentration near the reservoir surface was about 0.2 mg/L; near the reservoir bottom, the average concentration was about 0.3 mg/L. Concentrations of total phosphorus ranged from less than 0.01 to 0.05 mg/L near the reservoir surface, and from less than 0.01 to 0.22 mg/L near the reservoir bottom. At transect 2 (about 7 miles upstream from the dam) near the bottom of the reservoir, concentrations of total iron exceeded aquatic-life standards, and dissolved-manganese concentrations exceeded standards for public water supply. Diatoms, green algae, blue-green algae, and cryptomonads comprised the majority of phytoplankton in Pueblo Reservoir in 1985. The maximum average of 41,000 cells/ml occurred in July. Blue-green algae dominated from June to September; diatoms were the dominant group of algae in October. The average concentrations of phytoplankton decreased from July to October.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884118","usgsCitation":"Edelmann, P., 1989, Reconnaissance of water quality of Pueblo Reservoir, Colorado: May through December 1985: U.S. Geological Survey Water-Resources Investigations Report 88-4118, Report: v, 53 p.; 1 Plate: 16.69 × 18.61 inches, https://doi.org/10.3133/wri884118.","productDescription":"Report: v, 53 p.; 1 Plate: 16.69 × 18.61 inches","costCenters":[],"links":[{"id":410959,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47034.htm","linkFileType":{"id":5,"text":"html"}},{"id":55826,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4118/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158434,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4118/report-thumb.jpg"},{"id":55825,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4118/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Pueblo Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.6833,\n              39.3667\n            ],\n            [\n              -106.5333,\n              39.3667\n            ],\n            [\n              -106.5333,\n              37.8917\n            ],\n            [\n              -104.6833,\n              37.8917\n            ],\n            [\n              -104.6833,\n              39.3667\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db545bcf","contributors":{"authors":[{"text":"Edelmann, Patrick","contributorId":86305,"corporation":false,"usgs":true,"family":"Edelmann","given":"Patrick","affiliations":[],"preferred":false,"id":197275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61310,"text":"mf1964 - 1989 - Map showing late Quaternary faults and 1978-84 seismicity of the Los Angeles region, California","interactions":[],"lastModifiedDate":"2022-05-10T14:31:20.709024","indexId":"mf1964","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1964","title":"Map showing late Quaternary faults and 1978-84 seismicity of the Los Angeles region, California","docAbstract":"<p>The Los Angeles region of California faces the greatest seismic risk of any part of the United States. The region is inhabited by more than 11 million people and is one of the Nation's key commercial and industrial centers. It lies astride a web of potentially active faults, including those segments of the San Andreas fault with the highest probability for generating a great earthquake during the next 30 years (Lindh, 1983; Sykes and Nishenko, 1984; Wesson and Wallace, 1985; U.S. Geological Survey, 1988). Moreover, many potentially active faults that can generate moderate-size, but damaging earthquakes lie within the metropolitan areas. Earthquakes along some of these faults—for example, a magnitude 6.5 event on the Newport-Inglewood zone—could produce losses exceeding those from a great earthquake on the more distant San Andreas fault (Evernden and Thomson, 1985).</p><p>This map shows, at 1:250,000 scale, known or suspected late Quaternary faults of the Los Angeles region, the ages of their most recent surface movements, and the associated earthquake activity for a recent 7-year period (1978 through 1984). The geologic and seismologic character of these faults and their potential for generating damaging earthquakes recently were evaluated by Ziony and Yerkes (1985). The map is intended primarily to inform scientists, engineers, and planners of the distribution of those faults that may have a potential for generating damaging earthquakes and (or) displacements of the Earth's surface. The map data also should contribute to further investigations of the seismotectonic setting of the Los Angeles region.</p><p>The mapped area extends from lat 33°15' N. to 34°45' N. and from long 116°45' W. to 120°00' W. This region encompasses parts of the Transverse Ranges (including the Santa Ynez, Santa Susana, Santa Monica, San Gabriel, and San Bernardino Mountains), the Los Angeles basin, part of the Mojave Desert, and segments of the Peninsular Ranges (including the Puente Hills, Santa Ana Mountains, and the northern San Jacinto Mountains). Offshore, it includes the eastern Santa Barbara Channel, several of the Channel Islands, the Santa Monica and San Pedro basins, Santa Catalina Island, and part of the Gulf of Santa Catalina.</p><p>In addition to the Los Angeles metropolitan area, the cities of Santa Barbara, Ventura, Riverside, and San Bernardino are within the map area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1964","usgsCitation":"Ziony, J., and Jones, L.M., 1989, Map showing late Quaternary faults and 1978-84 seismicity of the Los Angeles region, California: U.S. Geological Survey Miscellaneous Field Studies Map 1964, Report: 23 p.; 1 Plate: 50.06 x 33.90 inches, https://doi.org/10.3133/mf1964.","productDescription":"Report: 23 p.; 1 Plate: 50.06 x 33.90 inches","numberOfPages":"24","costCenters":[],"links":[{"id":400390,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1964/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":400389,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1964/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1964/report-thumb.jpg"}],"scale":"250000","projection":"National Geodetic Vertical Datum of 1929","country":"United States","state":"California","city":"Los Angeles","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120,33.25 ], [ -120,34.75 ], [ -116.75,34.75 ], [ -116.75,33.25 ], [ -120,33.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b42fb","contributors":{"authors":[{"text":"Ziony, Joseph I.","contributorId":16829,"corporation":false,"usgs":true,"family":"Ziony","given":"Joseph I.","affiliations":[],"preferred":false,"id":265367,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Lucile M. jones@usgs.gov","contributorId":1014,"corporation":false,"usgs":true,"family":"Jones","given":"Lucile","email":"jones@usgs.gov","middleInitial":"M.","affiliations":[{"id":508,"text":"Office of the AD Hazards","active":true,"usgs":true}],"preferred":true,"id":265368,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63316,"text":"gq1614 - 1989 - Geologic map of the Diamond Peak quadrangle, Larimer County, Colorado, and Albany County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq1614","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"1614","title":"Geologic map of the Diamond Peak quadrangle, Larimer County, Colorado, and Albany County, Wyoming","language":"ENGLISH","doi":"10.3133/gq1614","usgsCitation":"Braddock, W.A., Cole, J., and Eggler, D.H., 1989, Geologic map of the Diamond Peak quadrangle, Larimer County, Colorado, and Albany County, Wyoming: U.S. Geological Survey Geologic Quadrangle 1614, 1 map :col. ;58 x 44 cm. on sheet 76 x 91 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1614.","productDescription":"1 map :col. ;58 x 44 cm. on sheet 76 x 91 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102688,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1138.htm","linkFileType":{"id":5,"text":"html"},"description":"1138"},{"id":249419,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1614/report.pdf","size":"71","linkFileType":{"id":1,"text":"pdf"}},{"id":252818,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1614/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.61749999999999,40.8675 ], [ -105.61749999999999,41 ], [ -105.5,41 ], [ -105.5,40.8675 ], [ -105.61749999999999,40.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6996ff","contributors":{"authors":[{"text":"Braddock, William A.","contributorId":61010,"corporation":false,"usgs":true,"family":"Braddock","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":268669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cole, J. C.","contributorId":21539,"corporation":false,"usgs":true,"family":"Cole","given":"J. C.","affiliations":[],"preferred":false,"id":268668,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eggler, David H.","contributorId":83601,"corporation":false,"usgs":true,"family":"Eggler","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":268670,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17212,"text":"ofr89645 - 1989 - Guidebook for field trip to the Mount Bachelor-South Sister-Bend area, central Oregon High Cascades","interactions":[],"lastModifiedDate":"2024-01-11T01:00:00.639611","indexId":"ofr89645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"89-645","title":"Guidebook for field trip to the Mount Bachelor-South Sister-Bend area, central Oregon High Cascades","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr89645","usgsCitation":"Scott, W.E., Gardner, C.A., Lundstrom, S.A., Hill, B.E., Taylor, E.M., Sarna-Wojcicki, A.M., Meyer, C.E., Nakata, J.K., Slate, J., and Russell, P., 1989, Guidebook for field trip to the Mount Bachelor-South Sister-Bend area, central Oregon High Cascades: U.S. Geological Survey Open-File Report 89-645, 66 p., https://doi.org/10.3133/ofr89645.","productDescription":"66 p.","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":424302,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_37214.htm","linkFileType":{"id":5,"text":"html"}},{"id":149354,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0645/report-thumb.jpg"},{"id":46352,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0645/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Mount Bachelor-South Sister-Bend area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.231,\n              44.2\n            ],\n            [\n              -121.917,\n              44.2\n            ],\n            [\n              -121.917,\n              43.65\n            ],\n            [\n              -121.231,\n              43.65\n            ],\n            [\n              -121.231,\n              44.2\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64affe","contributors":{"editors":[{"text":"Scott, W.E.","contributorId":16033,"corporation":false,"usgs":true,"family":"Scott","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":749522,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Gardner, Cynthia A. 0000-0002-6214-6182 cgardner@usgs.gov","orcid":"https://orcid.org/0000-0002-6214-6182","contributorId":1959,"corporation":false,"usgs":true,"family":"Gardner","given":"Cynthia","email":"cgardner@usgs.gov","middleInitial":"A.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":891924,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Sarna-Wojcicki, Andrei M. 0000-0002-0244-9149 asarna@usgs.gov","orcid":"https://orcid.org/0000-0002-0244-9149","contributorId":1046,"corporation":false,"usgs":true,"family":"Sarna-Wojcicki","given":"Andrei","email":"asarna@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":891925,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Scott, William E. 0000-0001-8156-979X wescott@usgs.gov","orcid":"https://orcid.org/0000-0001-8156-979X","contributorId":1725,"corporation":false,"usgs":true,"family":"Scott","given":"William","email":"wescott@usgs.gov","middleInitial":"E.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":891926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gardner, Cynthia A. 0000-0002-6214-6182 cgardner@usgs.gov","orcid":"https://orcid.org/0000-0002-6214-6182","contributorId":1959,"corporation":false,"usgs":true,"family":"Gardner","given":"Cynthia","email":"cgardner@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":891927,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lundstrom, Scott A.","contributorId":333098,"corporation":false,"usgs":false,"family":"Lundstrom","given":"Scott","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":891928,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hill, Brittain E.","contributorId":333099,"corporation":false,"usgs":false,"family":"Hill","given":"Brittain","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":891929,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Taylor, Edward M.","contributorId":65932,"corporation":false,"usgs":true,"family":"Taylor","given":"Edward","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":891930,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Sarna-Wojcicki, Andrei M. 0000-0002-0244-9149 asarna@usgs.gov","orcid":"https://orcid.org/0000-0002-0244-9149","contributorId":1046,"corporation":false,"usgs":true,"family":"Sarna-Wojcicki","given":"Andrei","email":"asarna@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":891931,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Meyer, Charles E.","contributorId":84007,"corporation":false,"usgs":true,"family":"Meyer","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":891932,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Nakata, John K.","contributorId":32518,"corporation":false,"usgs":true,"family":"Nakata","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":891933,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Slate, J.L.","contributorId":101695,"corporation":false,"usgs":true,"family":"Slate","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":891934,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Russell, P.C.","contributorId":102856,"corporation":false,"usgs":true,"family":"Russell","given":"P.C.","email":"","affiliations":[],"preferred":false,"id":891935,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
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