{"pageNumber":"4143","pageRowStart":"103550","pageSize":"25","recordCount":166022,"records":[{"id":1271,"text":"wsp2345 - 1989 - Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina","interactions":[{"subject":{"id":13302,"text":"ofr8746 - 1987 - Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina","indexId":"ofr8746","publicationYear":"1987","noYear":false,"title":"Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":1271,"text":"wsp2345 - 1989 - Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina","indexId":"wsp2345","publicationYear":"1989","noYear":false,"title":"Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina"},"id":1}],"lastModifiedDate":"2019-12-30T10:40:13","indexId":"wsp2345","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":"2345","title":"Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina","docAbstract":"Four unsaturated-zone monitoring sites and a meteorologic station were installed at the low-level radioactive-waste burial site near Barnwell, S.C., to investigate the geohydrologic and climatologic factors affecting water movement in the unsaturated zone. The study site is located in the Atlantic Coastal Plain. The unsaturated zone consists of a few centimeters to more than 1 meter of surface sand, underlain by up to 15 meters of clayey sand. Two monitoring sites were installed in experimental trenches, and two were installed in radioactive-waste trenches. Two different trench designs were evaluated at the monitoring sites. \r\n\r\nA meteorologic station was used to measure precipitation and to calculate actual evapotranspiration using the Bowen ratio method. Soil-moisture tensiometers, soil-moisture conductance probes, and temperature sensors were used to monitor soil-water movement in and adjacent to the trenches. Tracer tests using sodium chloride were conducted at each monitoring site. Hydrologic properties of unsaturated-zone materials were also determined. Data collection at the monitoring sites began in January 1982 and continued until early May 1984. \r\n\r\nTensiometer data show that the unsaturated materials had their highest percent saturations in winter and spring. Saturations in the backfill sand varied from 20 to 100 percent, and in the adjacent undisturbed and overlying compacted clayey sand, from about 75 to 100 percent. The same pattern generally was observed at all four monitoring sites. The tracer-test data indicate that water movement occurred mainly during the recharge period, winter and spring. The tracer-test results enabled computation of rates of unsaturated flow in the compacted clayey-sand cap, the compacted clayey-sand barrier, and the backfill sand. \r\n\r\nA micro-scale hydrologic budget was determined for an undisturbed part of the site from July 1983 through June 1984.Total precipitation was 144 centimeters, and actual evapotranspiration was 101 centimeters. Additionally, because tensiometer data indicate negligible water-storage changes in the unsaturated zone, it is estimated that approximately 43 centimeters of recharge reached the water table. \r\n\r\nDuring 1984, the rise and fall of ponded water in an experimental trench was continuously monitored with a digital recorder. This water-level record was used to compute the rate of leakage of ponded water from that trench--1 x 10 -5 centimeter per second. A cross-sectional finite-element model of variably saturated flow was used to test the conceptual model of water movement in the unsaturated zone and to illustrate the effect of trench design on water movement into the experimental trenches. \r\n\r\nMonitoring and model results show that precipitation on trenches infiltrated the trench cap and moved vertically into the trench backfill material. Precipitation on the undisturbed material adjacent to the trenches moved vertically through the surface sand and continued either downward into undisturbed clayey sand or laterally along the sand/clayey-sand interface into the backfill sand, depending on trench design. The trench construction practice of placing a compacted clayey-sand barrier around the trench greatly inhibits soil water from entering the trench.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp2345","usgsCitation":"Dennehy, K.F., and McMahon, P.B., 1989, Water movement in the unsaturated zone at a low-level radioactive-waste burial site near Barnwell, South Carolina: U.S. Geological Survey Water Supply Paper 2345, v, 40 p. , https://doi.org/10.3133/wsp2345.","productDescription":"v, 40 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":26225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2345/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2345/report-thumb.jpg"}],"country":"United States","state":"South Carolina","city":"Barnwell","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.5350341796875,\n              33.13065128220441\n            ],\n            [\n              -81.199951171875,\n              33.13065128220441\n            ],\n            [\n              -81.199951171875,\n              33.348884792201694\n            ],\n            [\n              -81.5350341796875,\n              33.348884792201694\n            ],\n            [\n              -81.5350341796875,\n              33.13065128220441\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db69970a","contributors":{"authors":[{"text":"Dennehy, Kevin F. kdennehy@usgs.gov","contributorId":1128,"corporation":false,"usgs":true,"family":"Dennehy","given":"Kevin","email":"kdennehy@usgs.gov","middleInitial":"F.","affiliations":[{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true}],"preferred":true,"id":143476,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McMahon, Peter B. 0000-0001-7452-2379 pmcmahon@usgs.gov","orcid":"https://orcid.org/0000-0001-7452-2379","contributorId":724,"corporation":false,"usgs":true,"family":"McMahon","given":"Peter","email":"pmcmahon@usgs.gov","middleInitial":"B.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":143475,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28903,"text":"wri894130 - 1989 - Effects of limestone quarrying and cement-plant operations on runoff and sediment yields in the Upper Permanente Creek basin, Santa Clara County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri894130","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":"89-4130","title":"Effects of limestone quarrying and cement-plant operations on runoff and sediment yields in the Upper Permanente Creek basin, Santa Clara County, California","docAbstract":"High sediment loads below headwater areas of the Permanente Creek drainage basin, Santa Clara County, California, have caused flood-control problems in downstream lowland areas. Measured sediment yields in Permanente Creek, which drains areas affected by limestone quarrying and cement-plant operations, were 14 times greater than yields from the West Fork Permanente Creek, which primarily drains parkland. Part of this large disparity in yields is the result of higher runoff/unit of drainage area in the Permanente Creek Basin. Results of rainfall-runoff modeling indicate that the tendency for higher runoff from Permanente Creek results from natural differences in basin physiography. Runoff during periods of high streamflow (when most sediment is transported) is dominated by subsurface flow, which is not affected by human activities. Although artificial features created by human activities seem to have had only minor effects on runoff, they apparently have had major effects on sediment availability. Artificial features accounted for 273 acres (89%) of the 307 acres of active erosional landforms mapped in 1984. Increased availability of sediment in the Permanente Creek basin appears to be indicated by elevated intercepts of sediment-transport curves. A comparison of sediment-transport curves for the West Fork Permanente Creek with similar curves for the Permanente Creek basin under natural conditions suggests that the sediment yield from Permanente Creek is about 3.5 times higher than it would be under natural basin conditions. The increased yield apparently is due to an increase in sediment availability rather than an increase in runoff. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri894130","usgsCitation":"Nolan, K., and Hill, B.R., 1989, Effects of limestone quarrying and cement-plant operations on runoff and sediment yields in the Upper Permanente Creek basin, Santa Clara County, California: U.S. Geological Survey Water-Resources Investigations Report 89-4130, vi, 48 p. :ill. ;28 cm., https://doi.org/10.3133/wri894130.","productDescription":"vi, 48 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":124163,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4130/report-thumb.jpg"},{"id":57776,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4130/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611c78","contributors":{"authors":[{"text":"Nolan, K.M.","contributorId":36151,"corporation":false,"usgs":true,"family":"Nolan","given":"K.M.","affiliations":[],"preferred":false,"id":200590,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, B. R.","contributorId":72833,"corporation":false,"usgs":true,"family":"Hill","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":200591,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44623,"text":"wri884067 - 1989 - Water-level maps of the Mississippi River Valley alluvial aquifer in eastern Arkansas, 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:11:00","indexId":"wri884067","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":"88-4067","title":"Water-level maps of the Mississippi River Valley alluvial aquifer in eastern Arkansas, 1986","docAbstract":"The Mississippi River Valley alluvial aquifer is a major source of water for irrigation in much of eastern Arkansas. Maps of the potentiometric surface, water level change, and depth to water illustrate the effects of large withdrawals for irrigation on water levels in the aquifer. The Mississippi River Valley alluvial aquifer is composed of Quaternary Flood plain and terrace deposits. Water in the aquifer generally is confined by an upper silt and clay layer. The regional direction of groundwater flow is south and southeast, except where affected by large withdrawals for irrigation by stream reaches that are hydraulically connected with the alluvial aquifer. The largest well yields range from 1,000 to 3,000 gal/min. Recharge to the aquifer principally is by infiltration of precipitation and water for surface water bodies. Both the spring and fall potentiometric surface maps show extensive cones of depression that result from large withdrawals for irrigation-one centered beneath Arkansas County, and another beneath western Poinsett and Cross Counties. Average water level differences between the spring and fall indicate a general decline of about 3 ft. The largest declines in water levels between 1981 and 1986 and the deepest water levels in 1986 occurred in areas most affected by large withdrawals for irrigation, as shown by the water level change map and depth to water map. The largest water level declines mainly occurred in central Lonoke County and in western Poinsett County. (USGS)","language":"ENGLISH","doi":"10.3133/wri884067","usgsCitation":"Plafcan, M., and Remsing, L.M., 1989, Water-level maps of the Mississippi River Valley alluvial aquifer in eastern Arkansas, 1986: U.S. Geological Survey Water-Resources Investigations Report 88-4067, 4 maps on 1 sheet ; sheet 94 x 132 cm. folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri884067.","productDescription":"4 maps on 1 sheet ; sheet 94 x 132 cm. folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":168815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81953,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4067/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db54539f","contributors":{"authors":[{"text":"Plafcan, Maria","contributorId":20338,"corporation":false,"usgs":true,"family":"Plafcan","given":"Maria","email":"","affiliations":[],"preferred":false,"id":230135,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Remsing, Larry M.","contributorId":32221,"corporation":false,"usgs":true,"family":"Remsing","given":"Larry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":230136,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29470,"text":"wri874089 - 1989 - Cost effectiveness of the stream-gaging program in West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri874089","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":"87-4089","title":"Cost effectiveness of the stream-gaging program in West Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nAvailable from Books and Open-File Reports,","doi":"10.3133/wri874089","usgsCitation":"Runner, G.S., Bragg, R., and Atkins, J., 1989, Cost effectiveness of the stream-gaging program in West Virginia: U.S. Geological Survey Water-Resources Investigations Report 87-4089, v, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874089.","productDescription":"v, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4089/report-thumb.jpg"},{"id":58316,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4089/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683f42","contributors":{"authors":[{"text":"Runner, G. S.","contributorId":74405,"corporation":false,"usgs":true,"family":"Runner","given":"G.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":201574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bragg, R.L.","contributorId":67905,"corporation":false,"usgs":true,"family":"Bragg","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":201573,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Atkins, J.T.","contributorId":39403,"corporation":false,"usgs":true,"family":"Atkins","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":201572,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17648,"text":"ofr89570 - 1989 - Sample locality maps, analytical data, and statistical summary of analyses of rock samples from the Mount Katmai quadrangle and adjacent portions of the Naknek and Afognak quadrangles, Alaska","interactions":[],"lastModifiedDate":"2022-08-01T21:34:27.835603","indexId":"ofr89570","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":"89-570","title":"Sample locality maps, analytical data, and statistical summary of analyses of rock samples from the Mount Katmai quadrangle and adjacent portions of the Naknek and Afognak quadrangles, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr89570","usgsCitation":"Riehle, J., Bailey, E., Church, S.E., and Yount, M.E., 1989, Sample locality maps, analytical data, and statistical summary of analyses of rock samples from the Mount Katmai quadrangle and adjacent portions of the Naknek and Afognak quadrangles, Alaska: U.S. Geological Survey Open-File Report 89-570, Report: 136 p.; 2 Plates: 39.94 × 30.43 inches and 39.82 × 30.24 inches, https://doi.org/10.3133/ofr89570.","productDescription":"Report: 136 p.; 2 Plates: 39.94 × 30.43 inches and 39.82 × 30.24 inches","costCenters":[],"links":[{"id":46849,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0570/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404608,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19100.htm","linkFileType":{"id":5,"text":"html"}},{"id":46850,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0570/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46851,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0570/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0570/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Afognak quadrangle, Mount Katmai quadrangle, Naknek quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -157,\n              58\n            ],\n            [\n              -153,\n              58\n            ],\n            [\n              -153,\n              59\n            ],\n            [\n              -157,\n              59\n            ],\n            [\n              -157,\n              58\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fde82","contributors":{"authors":[{"text":"Riehle, J.R.","contributorId":73573,"corporation":false,"usgs":true,"family":"Riehle","given":"J.R.","affiliations":[],"preferred":false,"id":177281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bailey, E. A.","contributorId":100399,"corporation":false,"usgs":true,"family":"Bailey","given":"E. A.","affiliations":[],"preferred":false,"id":177283,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Church, S. E.","contributorId":58260,"corporation":false,"usgs":true,"family":"Church","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":177280,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yount, M. E.","contributorId":76748,"corporation":false,"usgs":true,"family":"Yount","given":"M.","middleInitial":"E.","affiliations":[],"preferred":false,"id":177282,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":27453,"text":"wri894077 - 1989 - Flood of September 7-9, 1987, in Lexington and Richland counties in the vicinity of Saint Andrews Road and Irmo, South Carolina","interactions":[],"lastModifiedDate":"2017-01-27T09:49:10","indexId":"wri894077","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":"89-4077","title":"Flood of September 7-9, 1987, in Lexington and Richland counties in the vicinity of Saint Andrews Road and Irmo, South Carolina","docAbstract":"Localized heavy rainfall on September 7, 1987, in Lexington and Richland Counties, South Carolina, caused severe flooding in the basins of Kinley Creek, Rawls Creek, and Stoop Creek, in the vicinity of Saint Andrews Road and the town of Irmo, South Carolina. The flooding damaged homes, furnishings, and landscaping. Rainfall, peak discharges, high-water elevations, and frequency relations of rainfall and discharge are tabulated and plotted for selected streams. The rain was most intense in the area along Rawls Creek, R-2 (tributary to Rawls Creek), Koon Branch (tributary to Rawls Creek), and the upper part of Kinley Creek. A rainfall of about 5.5 inches in 3 hours, which has a recurrence interval in excess of 100 years, was reported by local residents along these streams. High-water marks are presented in this report for Stoop Creek, Kinley Creek, K-1 (tributary to Kinley Creek), K-2 (tributary to Kinley Creek), unnamed tributary to Kinley Creek, Lowery Creek (tributary to Kinley Creek), Rawls Creek, R-2 (tributary to Rawls Creek), and Koon Branch (tributary to Rawls Creek). Peak discharges at the most downstream sites on Rawls Creek and Koon Branch had recurrence intervals of 75 years and 60 years, respectively. Peak discharges on Kinley Creek varied from 20 to 25 years north of K-1 basin to less than 10 years at K-1. The Stoop Creek basin had a recurrence interval of 10 years. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri894077","usgsCitation":"Guimaraes, W., 1989, Flood of September 7-9, 1987, in Lexington and Richland counties in the vicinity of Saint Andrews Road and Irmo, South Carolina: U.S. Geological Survey Water-Resources Investigations Report 89-4077, iv, 37 p. :ill. ;28 cm., https://doi.org/10.3133/wri894077.","productDescription":"iv, 37 p. :ill. ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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W.B.","contributorId":14020,"corporation":false,"usgs":true,"family":"Guimaraes","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":198142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13135,"text":"ofr89460 - 1989 - Landslide deposits in the Duchesne 30' x 60' Quadrangle, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr89460","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":"89-460","title":"Landslide deposits in the Duchesne 30' x 60' Quadrangle, Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89460","usgsCitation":"Colton, R.B., and Bryant, B., 1989, Landslide deposits in the Duchesne 30' x 60' Quadrangle, Utah: U.S. Geological Survey Open-File Report 89-460, 6 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr89460.","productDescription":"6 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":144445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0460/report-thumb.jpg"},{"id":41536,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0460/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41537,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0460/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab7ba","contributors":{"authors":[{"text":"Colton, R. B.","contributorId":40186,"corporation":false,"usgs":true,"family":"Colton","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":167295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bryant, Bruce bbryant@usgs.gov","contributorId":1355,"corporation":false,"usgs":true,"family":"Bryant","given":"Bruce","email":"bbryant@usgs.gov","affiliations":[],"preferred":false,"id":167294,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17535,"text":"ofr89336 - 1989 - Preliminary geologic map of the Turayf Quadrangle, sheet 31C, and part of the An Nabk quadrangle, sheet 31B, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-16T15:36:31","indexId":"ofr89336","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":"89-336","title":"Preliminary geologic map of the Turayf Quadrangle, sheet 31C, and part of the An Nabk quadrangle, sheet 31B, Kingdom of Saudi Arabia","docAbstract":"<p>The An Nabk and Turayf quadrangles lie at the northern border of the Kingdom of Saudi Arabia. Middle and upper Cenozoic sedimentary and volcanic rocks form the surface of the quadrangles, and sedimentary rocks of the Paleozoic, Mesozoic, and lower Cenozoic are found in the subsurface. The Paleozoic and Mesozoic rocks, described from drill hole records, include the Tabuk, Upper Sudair, Lower Jilh and Aruma formations which are mostly of marine origin.</p>\n<p>The map area is part of the Sirhan-Turayf Basin and contains the Thaniyat, China, and Arqah Phosphorite members of the Upper Cretaceous-Tertiary Turayf group. Only the Arqah Phosphorite, the uppermost of the three members, crops out at the surface. From its outcrop along the east border of the area, the Arqah dips westward into the subsurface and passes into an argillaceous deeper water fades. The Thaniyat and China also dip westward in the subsurface and pinch out into a deeper water fades.</p>\n<p>Upper Eocene calcareous claystone and chalk mapped in the Wadi As Sirhan depression on the west side of the map area are named the Rashrashiyah formation, and may be partly equivalent to Eocene bioclastic, chert-bearing carbonate rocks of the Turayf group mapped to the east.</p>\n<p>The Sirhan formation is a new name for rocks of Miocene(?) age occurring in the Wadi As Sirhan area. These rocks are mostly sandstone of probable continental origin, and contain thin beds of fresh water limestone. However, marine limestone beds also occur, indicating periodic incursions by the sea.</p>\n<p>Al Harrah, a large Quaternary-Tertiary basalt field in the Sirhan-Turayf Basin, occupies the central part of the map area. The flows consist of silicic alkali olivine basalt, typical of the Cenozoic lava flows of Saudi Arabia. Volcanism appears to be of the continental rift-type and is related to Red Sea rifting.</p>\n<p>Quaternary calcareous and gypsiferous duricrust is found discontinuously throughout the western part of the map area. At one time it apparently formed a carapace-like cover over all surface rocks, and indicates a much wetter in northern Saudi Arabia than the present climate.</p>\n<p>The Arqah Phosphorite member is exposed in the northeast corner of the map area and contains thin beds of phosphorite grading from 18 to 30 percent P<sub>2</sub>O<sub>5</sub>-</p>\n<p>Oil shows have been reported in Cretaceous rocks of the Wadi As Sirhan depression, and oil has been discovered recently nearby in Jordan. Geologic and geophysical conditions are favorable for the entrapment of oil in the Wadi As Sirhan area and additional exploration is recommended.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr89336","usgsCitation":"Meissner, C.R., Riddler, G., Van Eck, M., Aspinall, N., Farasani, A., and Dini, S., 1989, Preliminary geologic map of the Turayf Quadrangle, sheet 31C, and part of the An Nabk quadrangle, sheet 31B, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 89-336, Report: ii, 29 p., ill.; maps: 28 cm., https://doi.org/10.3133/ofr89336.","productDescription":"Report: ii, 29 p., ill.; maps: 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":46697,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0336/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149265,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0336/report-thumb.jpg"},{"id":46696,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0336/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Saudi Arabia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              37,\n              31\n            ],\n            [\n              37,\n              32\n            ],\n            [\n              39,\n              32\n            ],\n            [\n              39,\n              31\n            ],\n            [\n              37,\n              31\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aa8d","contributors":{"authors":[{"text":"Meissner, C. R. 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,{"id":21410,"text":"ofr89380 - 1989 - Miscellaneous streamflow measurements in the State of Washington, January 1961 to September 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr89380","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":"89-380","title":"Miscellaneous streamflow measurements in the State of Washington, January 1961 to September 1985","docAbstract":"This report is a compilation of previously published miscellaneous streamflow measurements made in Washington State by the U.S. Geological Survey between January 1961 and September 1985. It is a supplement to a volume of similar data for the period 1890 to January 1961. The data include stream name and stream to which it is tributary, latitude and longitude, county code, hydrologic unit code, land-line location, drainage area, and measurement dates and discharges. In general, the data sites are not at gaging stations; however, some data are given for gaging station sites during periods when the stations were not in operation. All data in this report have been entered into a computerized data base that includes the data for the period 1890 to January 1961. The data can be retrieved in a variety of ways, such as by county, by hydrologic unit code, by river basin , or by size of drainage area. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr89380","usgsCitation":"Williams, J., and Riis, S., 1989, Miscellaneous streamflow measurements in the State of Washington, January 1961 to September 1985: U.S. Geological Survey Open-File Report 89-380, iii, 382 p. ;28 cm., https://doi.org/10.3133/ofr89380.","productDescription":"iii, 382 p. ;28 cm.","costCenters":[],"links":[{"id":154119,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0380/report-thumb.jpg"},{"id":50980,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0380/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b94","contributors":{"authors":[{"text":"Williams, John R.","contributorId":41832,"corporation":false,"usgs":true,"family":"Williams","given":"John R.","affiliations":[],"preferred":false,"id":184377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Riis, S.A.","contributorId":79500,"corporation":false,"usgs":true,"family":"Riis","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":184378,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17743,"text":"ofr89588 - 1989 - Summary of water-resources activities of the U.S. Geological Survey in Colorado– Fiscal year 1989","interactions":[],"lastModifiedDate":"2021-12-03T19:39:07.16162","indexId":"ofr89588","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":"89-588","title":"Summary of water-resources activities of the U.S. Geological Survey in Colorado– Fiscal year 1989","docAbstract":"The biennial summary of water resources activities in Colorado is presented for fiscal year 1989. The report includes an introduction of these activities and names of the management personnel to whom information requests may be addressed, a summary of the U.S. Geological Survey mission and of the Water Resources Division mission, and a discussion of the water resources in Colorado in fiscal year 1989, including data collection on surface water and groundwater. All current Colorado hydrologic investigations are listed--their problems, objectives, approaches, progress, and plans for fiscal year 1989. A list of current cooperators, for fiscal year 1989 and a list of reports published or released during fiscal years 1987, 1988, and 1989 also are given. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr89588","usgsCitation":"Griffith, P.A., 1989, Summary of water-resources activities of the U.S. Geological Survey in Colorado– Fiscal year 1989: U.S. Geological Survey Open-File Report 89-588, Report: iv, 58 p.; 1 Plate: 26.97 × 22.06 inches, https://doi.org/10.3133/ofr89588.","productDescription":"Report: iv, 58 p.; 1 Plate: 26.97 × 22.06 inches","costCenters":[],"links":[{"id":392455,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17729.htm"},{"id":46966,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0588/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46965,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0588/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150055,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0588/report-thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.09423828125,\n              36.98500309285596\n            ],\n            [\n              -101.97509765625,\n              36.98500309285596\n            ],\n            [\n              -101.97509765625,\n              40.9964840143779\n            ],\n            [\n              -109.09423828125,\n              40.9964840143779\n            ],\n            [\n              -109.09423828125,\n              36.98500309285596\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698778","contributors":{"authors":[{"text":"Griffith, P. A.","contributorId":20345,"corporation":false,"usgs":true,"family":"Griffith","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":177672,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58390,"text":"mf2071B - 1989 - Geochemical maps showing the distribution and abundance of selected elements in nonmagnetic heavy-mineral-concentrate samples from stream sediment, Solomon and Bendeleben 1° x 3° quadrangles, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2021-11-08T19:12:15.014963","indexId":"mf2071B","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":"B","title":"Geochemical maps showing the distribution and abundance of selected elements in nonmagnetic heavy-mineral-concentrate samples from stream sediment, 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/mf2071B","usgsCitation":"King, H.D., Smith, S., Sutley, S.J., and Greene, K., 1989, Geochemical maps showing the distribution and abundance of selected elements in nonmagnetic heavy-mineral-concentrate samples from stream sediment, Solomon and Bendeleben 1° x 3° quadrangles, Seward Peninsula, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 2071, Report: 13 p.; 1 Plate: 56.29 × 37.65 inches, https://doi.org/10.3133/mf2071B.","productDescription":"Report: 13 p.; 1 Plate: 56.29 × 37.65 inches","costCenters":[],"links":[{"id":100683,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1989/2071b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":105224,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5672.htm","linkFileType":{"id":5,"text":"html"},"description":"5672"},{"id":88370,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1989/2071b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1989/2071b/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Seward Peninsula, Solomon 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":"4f4e4826e4b07f02db4e4f68","contributors":{"authors":[{"text":"King, H. D.","contributorId":89113,"corporation":false,"usgs":true,"family":"King","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":258996,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, S.C.","contributorId":16833,"corporation":false,"usgs":true,"family":"Smith","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":258994,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sutley, S. J.","contributorId":91484,"corporation":false,"usgs":true,"family":"Sutley","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":258997,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Greene, K.R.","contributorId":46615,"corporation":false,"usgs":true,"family":"Greene","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":258995,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":12285,"text":"ofr89331 - 1989 - Seismic study of the Agua de Pau volcano Sao Miguel, Arcores","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr89331","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":"89-331","title":"Seismic study of the Agua de Pau volcano Sao Miguel, Arcores","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89331","usgsCitation":"Dawson, P., daSilva, A., Evans, J., and Iyer, H.M., 1989, Seismic study of the Agua de Pau volcano Sao Miguel, Arcores: U.S. Geological Survey Open-File Report 89-331, 74 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89331.","productDescription":"74 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":143674,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0331/report-thumb.jpg"},{"id":40507,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0331/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e128","contributors":{"authors":[{"text":"Dawson, P.B.","contributorId":75934,"corporation":false,"usgs":true,"family":"Dawson","given":"P.B.","email":"","affiliations":[],"preferred":false,"id":165777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"daSilva, A.M.","contributorId":58276,"corporation":false,"usgs":true,"family":"daSilva","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":165776,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Evans, J.R.","contributorId":50526,"corporation":false,"usgs":true,"family":"Evans","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":165775,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Iyer, H. M.","contributorId":17997,"corporation":false,"usgs":true,"family":"Iyer","given":"H.","middleInitial":"M.","affiliations":[],"preferred":false,"id":165774,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":17474,"text":"ofr89559 - 1989 - Phosphorite potential in the continental shelf off Georgia: Results of the TACTS core studies","interactions":[],"lastModifiedDate":"2019-11-26T06:43:29","indexId":"ofr89559","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":"89-559","title":"Phosphorite potential in the continental shelf off Georgia: Results of the TACTS core studies","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr89559","usgsCitation":"Huddlestun, P., Henry, V.J., Commeau, J.A., Da Silva, J., Manheim, F., Popenoe, P., and Herring, J.R., 1989, Phosphorite potential in the continental shelf off Georgia: Results of the TACTS core studies: U.S. Geological Survey Open-File Report 89-559, 64 p., https://doi.org/10.3133/ofr89559.","productDescription":"64 p.","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":150713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0559/report-thumb.jpg"},{"id":46628,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0559/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.8756103515625,\n              30.670990790779168\n            ],\n            [\n              -80.76599121093749,\n              30.670990790779168\n            ],\n            [\n              -80.76599121093749,\n              32.310348764525806\n            ],\n            [\n              -81.8756103515625,\n              32.310348764525806\n            ],\n            [\n              -81.8756103515625,\n              30.670990790779168\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db687616","contributors":{"editors":[{"text":"Manheim, F.T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":74018,"corporation":false,"usgs":true,"family":"Manheim","given":"F.T.","affiliations":[],"preferred":false,"id":749232,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Huddlestun, Paul","contributorId":9669,"corporation":false,"usgs":true,"family":"Huddlestun","given":"Paul","email":"","affiliations":[],"preferred":false,"id":776154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henry, Vernon J.","contributorId":138788,"corporation":false,"usgs":false,"family":"Henry","given":"Vernon","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":776155,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Commeau, Judith A.","contributorId":32137,"corporation":false,"usgs":true,"family":"Commeau","given":"Judith","email":"","middleInitial":"A.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":776156,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Da Silva, Jana","contributorId":220908,"corporation":false,"usgs":false,"family":"Da Silva","given":"Jana","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":776157,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Manheim, F.T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":55421,"corporation":false,"usgs":true,"family":"Manheim","given":"F.T.","affiliations":[],"preferred":false,"id":776158,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Popenoe, Peter","contributorId":104078,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","affiliations":[],"preferred":false,"id":776159,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Herring, James R.","contributorId":95492,"corporation":false,"usgs":true,"family":"Herring","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":776160,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":27697,"text":"wri894066 - 1989 - Summary of fluvial-sediment studies in Ohio, through 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri894066","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":"89-4066","title":"Summary of fluvial-sediment studies in Ohio, through 1987","docAbstract":"The U.S. Geological Survey, in cooperation with other Federal, State, and local agencies, has been collecting fluvial sediment data from Ohio streams since April 1950. This report summarizes the data collected for the period April 1950 through 1987. In addition, trends in annual suspended-sediment discharge in Ohio streams are examined and discussed, and a technique is presented for estimating discharge at ungaged points on Ohio streams. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri894066","usgsCitation":"Hindall, S.M., 1989, Summary of fluvial-sediment studies in Ohio, through 1987: U.S. Geological Survey Water-Resources Investigations Report 89-4066, vi, 29 p. :ill., map ;28 cm., https://doi.org/10.3133/wri894066.","productDescription":"vi, 29 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":158840,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4066/report-thumb.jpg"},{"id":56546,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4066/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56547,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4066/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699295","contributors":{"authors":[{"text":"Hindall, S. M.","contributorId":59414,"corporation":false,"usgs":true,"family":"Hindall","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":198554,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57514,"text":"wdrAL881 - 1989 - Water resources data for Alabama, water year 1988","interactions":[],"lastModifiedDate":"2022-11-23T19:49:50.191346","indexId":"wdrAL881","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":"AL-88-1","title":"Water resources data for Alabama, water year 1988","docAbstract":"<p>The Water Resources Division of the U.S. Geological Survey, in cooperation with State and Federal agencies, obtains a large amount of data pertaining to the water resources of Alabama each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. To make these data readily available to interested parties outside the Geological Survey, the data are published annually in this report series entitled \"Water Resources Data - Alabama.\"</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrAL881","collaboration":"Prepared in cooperation with the Alabama Department of Environmental Management, the Alabama Highway Department, the Geological Survey of Alabama, and with other State, municipal, and Federal agencies","usgsCitation":"Rollins, H., Pearman, J., Sedberry, F., and Cole, P., 1989, Water resources data for Alabama, water year 1988: U.S. Geological Survey Water Data Report AL-88-1, viii, 324 p., https://doi.org/10.3133/wdrAL881.","productDescription":"viii, 324 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L.","contributorId":76353,"corporation":false,"usgs":true,"family":"Pearman","given":"J. L.","affiliations":[],"preferred":false,"id":257230,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sedberry, F.C.","contributorId":8922,"corporation":false,"usgs":true,"family":"Sedberry","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":257229,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cole, P.W.","contributorId":98795,"corporation":false,"usgs":true,"family":"Cole","given":"P.W.","email":"","affiliations":[],"preferred":false,"id":257231,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":27301,"text":"wri884231 - 1989 - Analysis of water surface and flow distribution for the design flood at a proposed highway crossing of the Sabine River near Tatum, Texas","interactions":[],"lastModifiedDate":"2016-08-10T15:45:08","indexId":"wri884231","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":"88-4231","title":"Analysis of water surface and flow distribution for the design flood at a proposed highway crossing of the Sabine River near Tatum, Texas","docAbstract":"<p>The hydraulic effects of the proposed Texas Highway 43 crossing of the Sabine River near Tatum, Texas, were determined on the basis of results from a two-dimensional finite-element surface-water-flow model. In planning the replacement crossing by the Texas State Department of Highways and Public Transportation, approximations of apportionment of flow among the openings and velocities within the openings were of concern. The model was used to simulate flow in the river floodplain system for the proposed design, an alternate design, and for the natural condition. The proposed bridge design by the State Department of Highways and Public Transportation consisted of a 320-foot main channel opening, four left overflow bridges with widths of 120, 320, 320, and 280 feet, and one right overflow opening with a width of 440 feet. The alternate design consisted of a 950-foot main channel opening, three left overflow bridges with widths of 320, 320, and 280 feet, and one right overflow opening with a width of 200 feet. Preliminary one-dimensional computations were used as an aid in establishing the boundary conditions for the two-dimensional analysis.</p>\n<p>The analysis evaluates the interaction of complex hydraulic characteristics of varied features found at many multiple-opening highway crossings. Valid applications of accepted standard one-dimensional techniques would not reveal some aspects of the overall hydraulics of the crossing.</p>\n<p>The simulation of the proposed design shows, among other things, which openings are the most productive per foot of bridge length. The results of the two-dimensional simulation of the proposed design indicate some differences in the apportionment of flow among the openings when compared to the one-dimensional proposed crossing computations. The alternate design results in computed water-surface altitudes which were slightly lower than those of the proposed design. The alternate design would require less modification to the existing embankment. Velocities computed within the openings and at the bridge abutments, using the two-dimensional model, were within the design specifications of the State Department of Highways and Public Transportation.</p>\n<p>The simulations of the proposed and alternate designs indicate a lateral component of the water-surface slope at the embankment. Redistribution of flow across the floodplain also is indicated in both simulations. Some of the differences in the response between the two designs are affected by geometric features of the floodplain other than the embankment-opening geometry.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri884231","usgsCitation":"Gilbert, J.J., and Myers, D., 1989, Analysis of water surface and flow distribution for the design flood at a proposed highway crossing of the Sabine River near Tatum, Texas: U.S. Geological Survey Water-Resources Investigations Report 88-4231, v, 36 p., https://doi.org/10.3133/wri884231.","productDescription":"v, 36 p.","numberOfPages":"41","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":124166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4231/report-thumb.jpg"},{"id":56174,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4231/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f55d","contributors":{"authors":[{"text":"Gilbert, J. J.","contributorId":12448,"corporation":false,"usgs":true,"family":"Gilbert","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197877,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Myers, D.R.","contributorId":104534,"corporation":false,"usgs":true,"family":"Myers","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":197878,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27466,"text":"wri854283 - 1989 - Surface-water quality in the West Branch Susquehanna River basin, Pennsylvania: An appraisal of areal and temporal variability from 1962 to 1982 in hydrologic accounting unit 020502","interactions":[],"lastModifiedDate":"2021-12-30T21:28:35.535812","indexId":"wri854283","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":"85-4283","title":"Surface-water quality in the West Branch Susquehanna River basin, Pennsylvania: An appraisal of areal and temporal variability from 1962 to 1982 in hydrologic accounting unit 020502","docAbstract":"<p>The West Branch Susquehanna River basin has a drainage area of 6,955 square miles in north-central Pennsylvania and comprises Hydrologic Accounting Unit 020502. A National Stream Quality Accounting Network (NASQAN) waterquality data collection site, maintained by the U.S. Geological Survey, is located on the river near its mouth at Lewisburg, Pennsylvania. Water-quality data are collected at numerous other sites throughout the basin by the Pennsylvania Department of Environmental Resources, Bureau of Water Quality Management. Data collected from the NASQAN site and the sites operated by the Pennsylvania Department of Environmental Resources from 1962 to 1982 were used to evaluate water-quality variability in the basin. The following objectives were addressed: (1) describe the surface-water quality upstream of the NASQAN site on an areal and temporal basis; (2) relate the water-quality variability, on both an areal and temporal basis, to general basin characteristics; and (3) assess the ability of the water-quality data collected at the NASQAN site to represent, on both an areal and temporal basis the water quality for Hydrologic Accounting Unit 020502 upstream from the site. Areally, the water quality varies considerably throughout the basin. Generally, the river was found to have moderately good water quality in the upper reaches, poor water quality in its middle reach, and good water quality near the mouth. Two tributaries, Moshannon Creek (median pH 3.9) and Bald Eagle Creek (median pH 7.8), had the most pronounced effect on the water quality of the river. Temporal trends were found in the concentrations of several of the constituents at most of the stations. Of the constituents analyzed, those which exhibited increasing or decreasing trends most frequently were pH, alkalinity, dissolved sulfate, total ammonia, and total nitrite plus nitrate. The largest trends were in the concentrations of total-recoverable aluminum, manganese, and zinc. Causes of areal variation were attributed to land use and geologic variations throughout the basin. Trends which indicated an improvement in water qualijty are believed to be caused by improvements in the treatment of acid mine drainage and wastewater. Trends which indicated degradation of water quality were generally found in areas where these types of treatment are not yet effective. The NASQAN site at Lewisburg was shown not to represent the water quality of the entire basin, either areally or temporally. It does, however, represent the water quality of the West Branch Susquehanna River at its mouth.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854283","usgsCitation":"Hainly, R., Truhlar, J., and Wetzel, K.L., 1989, Surface-water quality in the West Branch Susquehanna River basin, Pennsylvania: An appraisal of areal and temporal variability from 1962 to 1982 in hydrologic accounting unit 020502: U.S. Geological Survey Water-Resources Investigations Report 85-4283, vi, 50 p., https://doi.org/10.3133/wri854283.","productDescription":"vi, 50 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":393707,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36421.htm"},{"id":56322,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4283/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4283/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"West Branch Susquehanna River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.9170,\n              40.462\n            ],\n            [\n              -76.25,\n              40.462\n            ],\n            [\n              -76.25,\n              41.917\n            ],\n            [\n              -78.9170,\n              41.917\n            ],\n            [\n              -78.9170,\n              40.462\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a5e0","contributors":{"authors":[{"text":"Hainly, R.A.","contributorId":45732,"corporation":false,"usgs":true,"family":"Hainly","given":"R.A.","affiliations":[],"preferred":false,"id":198167,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Truhlar, J.F.","contributorId":107738,"corporation":false,"usgs":true,"family":"Truhlar","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":198168,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wetzel, K. L.","contributorId":14418,"corporation":false,"usgs":true,"family":"Wetzel","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":198166,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":17633,"text":"ofr88318 - 1989 - Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois","interactions":[{"subject":{"id":17633,"text":"ofr88318 - 1989 - Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois","indexId":"ofr88318","publicationYear":"1989","noYear":false,"title":"Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois"},"predicate":"SUPERSEDED_BY","object":{"id":2635,"text":"wsp2367 - 1991 - Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois","indexId":"wsp2367","publicationYear":"1991","noYear":false,"title":"Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois"},"id":1}],"supersededBy":{"id":2635,"text":"wsp2367 - 1991 - Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois","indexId":"wsp2367","publicationYear":"1991","noYear":false,"title":"Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois"},"lastModifiedDate":"2021-03-05T19:30:36.120435","indexId":"ofr88318","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":"88-318","title":"Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois","docAbstract":"<p>Ten years of hydrologic research have been conducted by the U.S. Geological Survey at a commercial low-level radioactive-waste disposal site near Sheffield, Illinois. Research included studies of microclimate, evapotranspiration, and tritium release by plants; runoff and land modification; water movement through a trench cover; water and tritium movement in the unsaturated zone; gases in the unsaturated zone; water and tritium movement in the saturated zone; and water chemistry. Implications specific to each research topic and those based on overlapping research topics are summarized as to their potential effect on the selection, characterization, design, operation, and decommissioning processes of future low-level radioactive-waste disposal sites. </p><p>Unconsolidated deposits at the site are diverse in lithologic character and are spatially and stratigraphically complex. Thickness of these Quaternary deposits ranges from 3 to 27 meters and averages 17 meters. The unconsolidated deposits overlay 140 meters of Pennsylvanian shale, mudstone, siltstone, and coal. </p><p>Approximately 90,500 cubic meters of waste were buried from August 1967 through August 1978, in 21 trenches that were constructed in glacial materials by using a cut-and-fill process. Trenches generally were constructed below grade and ranged from 11 to 180 meters long, 2.4 to 21 meters wide, and 2.4 to about 7.9 meters deep. </p><p>Research on microclimate and evapotranspiration at the site was conducted from July 1982 through June 1984. Continuous measurements were made of precipitation, incoming and reflected solar (shortwave) radiation, incoming and emitted terrestrial (longwave) radiation, horizontal windspeed and direction, wet- and dry-bulb air temperature, barometric pressure, soil-heat fluxes, and soil temperature. Soil-moisture content, for this research phase, was measured approximately biweekly. Evapotranspiration rates were estimated by using three techniques--energy budget, aerodynamic profile, and water budget. Although monthly totals for each method differed, estimated annual evapotranspiration averages ranged from 630 to 693 millimeters or about 70 percent of precipitation. </p><p>Tritium concentrations in leaf water from on-site plants were determined for 125 vegetation samples collected during the summers of 1982 through 1986. Concentrations varied significantly among some locations and plant types. Tritium concentrations ranged from the detection limit of 0 .2 to 1,330 nanocuries per liter, with alfalfa (Medicago sativa) having the highest concentrations, followed by brome grass (Bromus inermis), and then red clover (Trifoleum pratense); these variations in concentration are most likely a result of root depth. </p><p>Runoff and sediment transport were measured from July 1982 through December 1985 in four basins--three comprising almost two-thirds of the 8.1-hectare site and one comprising a 1.4-hectare undisturbed area. Volumes and equivalent weights of collapses were estimated from records of site surficial conditions from October 1978 through December 1985. Runoff showed a direct relation to degree of land modification; lowest mean yields were measured at the undisturbed area, and highest mean yields were measured from the basin composed wholly of trench and intertrench areas. Sediment yield measured onsite averaged 3.4 megagrams per hectare. A total of 315 collapse cavities, corresponding to a cumulative volume of about 500 cubic meters, were documented. Most collapses were recorded after periods of rainfall or snowmelt when soil moisture was near maximum. Almost two-thirds of the collapses, corresponding to 63 percent of the cumulative cavity volume, occurred during February through April. </p><p>Data for the study of water movement through a trench cover were collected from July 1982 through June 1934. Pressure-head data were collected at four different clusters at depths ranging from 50 to 1,850 millimeters within a selected trench cover. Soil-moisture content for this research phase was measured weekly with a gamma-attenuation moisture probe. The amount of water stored within the trench cover fluctuated in an annual cycle. Moisture contents were greatest in late March or early April, decreased steadily from late spring through the summer, reached a minimum in late August or early September, and then increased gradually from midfall through the winter. Depths of wetting-front movements were a function of initial soil-moisture content and total storm precipitation. Seepage to the trench was estimated by use of four different methods: the Darcy method, the zero-flux phase method, the surface-based water-budget method, and the ground-water based water-budget method. Estimates by the different methods differed considerably. </p><p>Investigation of the unsaturated zone at the site began in 1981 and is ongoing (1987). Water movement was measured along a generalized vertical section through four trenches. A 120-meter-long, 2-meter-diameter horizontal tunnel provided access below the trenches. The timing of water movement varied temporally and spatially. Vertical flow was inhibited at interfaces between lithologic units of contrasting hydraulic conductivities. Data also indicate that water movement through the sand of the Toulon Member of the Glasford Formation occurs along localized partially saturated to saturated flow paths. Average velocities of water movement through the extent of the unsaturated zone, as estimated by a saturation-tracking method, ranged from 0.04 to 0.34 meter per day. </p><p>Tritium concentrations in the unsaturated zone varied spatially reflecting the heterogeneity of wastes in the overlying trenches and local hydrogeologic conditions. Tritium concentrations at all lysimeter locations increased with time; however, the increases usually were of small magnitude. Tritium concentrations increased abruptly, from five to nine times previous concentrations, at only 3 of 14 locations. </p><p>Gas samples were collected from a network of soil-gas piezometers located in the undisturbed unsaturated zone near a waste trench at approximately 70-day intervals during 1984-86. Relative proportions of nitrogen, oxygen plus argon, carbon dioxide, methane, ethane, propane, butane, tritiated water vapor, carbon dioxide, and 222radon were converted to partial pressures, based on a mean atmospheric pressure of 98.6 kilopascals. Methane and 14 carbon dioxide were identified as originating in the waste and having mean partial pressures that generally decreased with horizontal distance from the trench and with vertical distance to the land surface. Partial-pressure gradients for other radioactive gases were not detected in the gas sampling network; definable gradients may occur much nearer to the waste source. </p><p>Ground-water flow has been studied at the site since 1976. The spatial, stratigraphic, and lithologic complexity of the unconsolidated deposits that compose the shallow aquifer result in the free water surface intersecting nine different lithologic units at the site. Saturated hydraulic conductivities of these units range from about 4x10-12 to 8x10-6 centimeters per second. Three ground-water basins were defined within the shallow aquifer, with flow generally from west to east. Ground-water velocities are highly variable. A tracer test conducted in a pebbly-sand unit resulted in velocities in the range of 640 to 770 meters per year. Estimated velocities for the other units ranged from 2 to 490 meters per year. </p><p>Tritium was detected in observation wells on-site in 1976 and off-site in 1982. Concentrations ranged from the analytical detection limit of 0.2 to over 300 nanocuries per liter. Seasonal variations in tritium concentrations were observed in most wells, and dilution caused by infiltrating rainfall was observed. </p><p>Water-chemistry research included the collection and analysis of precipitation, geologic materials, and unsaturated- and saturated-zone water, both on-site and off-site, and in all geologic units, during 1978 to 1984. Precipitation was a calcium-zinc-sulfate type water. Calcium and bicarbonate were the most abundant cation and anion, respectively, in the geologic materials. Mean dissolved organic carbon and tritium concentrations (45 milligrams per liter and 290 nanocuries per liter, respectively) were greater in samples from six lysimeters located directly below waste trenches and one located within a trench, than in samples from all other lysimeters (8.4 milligrams per liter and 17 nanocuries per liter, respectively). Water in the saturated zone was generally a magnesium-bicarbonate type. Tritium was the only radionuclide detected in the saturated zone.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr88318","usgsCitation":"1989, Results of hydrologic research at a low-level radioactive-waste disposal site near Sheffield, Illinois: U.S. Geological Survey Open-File Report 88-318, x, 114 p., https://doi.org/10.3133/ofr88318.","productDescription":"x, 114 p.","costCenters":[],"links":[{"id":149804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0318/report-thumb.jpg"},{"id":384153,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0318/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Illinois","city":"Sheffield","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.76242065429688,\n              41.33660710626423\n            ],\n            [\n              -89.67727661132811,\n              41.33660710626423\n            ],\n            [\n              -89.67727661132811,\n              41.3675335097313\n            ],\n            [\n              -89.76242065429688,\n              41.3675335097313\n            ],\n            [\n              -89.76242065429688,\n              41.33660710626423\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673fe8","contributors":{"editors":[{"text":"Ryan, Barbara J.","contributorId":53397,"corporation":false,"usgs":true,"family":"Ryan","given":"Barbara J.","affiliations":[],"preferred":false,"id":749494,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":14497,"text":"ofr88722 - 1989 - Arsenic and chloride data for five stream sites in the Madison River drainage, Montana, 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:06:53","indexId":"ofr88722","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":"88-722","title":"Arsenic and chloride data for five stream sites in the Madison River drainage, Montana, 1988","docAbstract":"Enriched geothermal waters in Yellowstone National Park contribute large quantities of arsenic to the Madison River. Because arsenic may be acutely or chronically toxic to humans when ingested, it is of concern in the upper Missouri River basin where the water is used for domestic purposes. In passage of water downstream, concentrations of arsenic in the Madison and Missouri Rivers are diluted by tributary inflows. However, insufficient information existed to describe concentrations during runoff at specific locations. As a result, a monitoring network was established to better define arsenic concentrations during the 1988 peak runoff and during periods prior to and following the runoff. In addition to arsenic, samples were analyzed for chloride because of its association with geothermal water and specific conductance because it is a surrogate measure of dissolved-solids concentration. This report presents data acquired during 1988 at five sampling stations in the Madison River drainage. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88722","usgsCitation":"Knapton, J.R., and Brosten, T.M., 1989, Arsenic and chloride data for five stream sites in the Madison River drainage, Montana, 1988: U.S. Geological Survey Open-File Report 88-722, iii, 12 p. ill., map ;28 cm., https://doi.org/10.3133/ofr88722.","productDescription":"iii, 12 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":147354,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0722/report-thumb.jpg"},{"id":43189,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0722/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672e08","contributors":{"authors":[{"text":"Knapton, J. R.","contributorId":84385,"corporation":false,"usgs":true,"family":"Knapton","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":169558,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brosten, Tordis M.","contributorId":72790,"corporation":false,"usgs":true,"family":"Brosten","given":"Tordis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":169557,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34757,"text":"b1905 - 1989 - Arizona's industrial rock and mineral resources; workshop proceedings","interactions":[],"lastModifiedDate":"2018-03-02T15:43:21","indexId":"b1905","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1905","title":"Arizona's industrial rock and mineral resources; workshop proceedings","language":"ENGLISH","publisher":"U.S. G.P.O. ; Books and Open-File Reports Section [distributor],","doi":"10.3133/b1905","usgsCitation":"1989, Arizona's industrial rock and mineral resources; workshop proceedings: U.S. Geological Survey Bulletin 1905, vii, 93 p. ill. ;28 cm., https://doi.org/10.3133/b1905.","productDescription":"vii, 93 p. ill. ;28 cm.","costCenters":[],"links":[{"id":62631,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1905/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167209,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1905/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db672e9a","contributors":{"compilers":[{"text":"Tooker, Edwin Wilson","contributorId":33295,"corporation":false,"usgs":true,"family":"Tooker","given":"Edwin","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":730114,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"editors":[{"text":"Tooker, Edwin Wilson","contributorId":33295,"corporation":false,"usgs":true,"family":"Tooker","given":"Edwin","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":730113,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":11980,"text":"ofr88717 - 1989 - Climatic data for Mirror Lake, West Thornton, New Hampshire, 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:06:31","indexId":"ofr88717","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":"88-717","title":"Climatic data for Mirror Lake, West Thornton, New Hampshire, 1987","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88717","usgsCitation":"Sturrock, A.M., Buso, D., Oberley, M., and Winter, T.C., 1989, Climatic data for Mirror Lake, West Thornton, New Hampshire, 1987: U.S. Geological Survey Open-File Report 88-717, 69 p. ill. ;28 cm., https://doi.org/10.3133/ofr88717.","productDescription":"69 p. ill. ;28 cm.","costCenters":[],"links":[{"id":143762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0717/report-thumb.jpg"},{"id":39973,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0717/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de1ab","contributors":{"authors":[{"text":"Sturrock, Alex M.","contributorId":48948,"corporation":false,"usgs":true,"family":"Sturrock","given":"Alex","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":164506,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buso, D.C.","contributorId":31392,"corporation":false,"usgs":true,"family":"Buso","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":164505,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oberley, M.J.","contributorId":81104,"corporation":false,"usgs":true,"family":"Oberley","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":164507,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Winter, T. C.","contributorId":23485,"corporation":false,"usgs":true,"family":"Winter","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":164504,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":21304,"text":"ofr89488 - 1989 - Petroleum source rock potential of the Upper Ordovician black shale sequence, northern Appalachian basin","interactions":[],"lastModifiedDate":"2012-02-02T00:07:55","indexId":"ofr89488","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":"89-488","title":"Petroleum source rock potential of the Upper Ordovician black shale sequence, northern Appalachian basin","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr89488","usgsCitation":"Wallace, L., and Roen, J., 1989, Petroleum source rock potential of the Upper Ordovician black shale sequence, northern Appalachian basin: U.S. Geological Survey Open-File Report 89-488, 66 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89488.","productDescription":"66 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154307,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0488/report-thumb.jpg"},{"id":50854,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0488/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50855,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0488/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50856,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0488/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50857,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0488/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50858,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0488/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50859,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0488/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50860,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0488/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":50861,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0488/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687714","contributors":{"authors":[{"text":"Wallace, L.G.","contributorId":31423,"corporation":false,"usgs":true,"family":"Wallace","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":184180,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roen, J.B.","contributorId":85564,"corporation":false,"usgs":true,"family":"Roen","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":184181,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13131,"text":"ofr89319 - 1989 - Geologic map of the Opheim 1° x 30' quadrangle, Valley and Daniels counties, Montana","interactions":[],"lastModifiedDate":"2021-09-13T22:00:29.296973","indexId":"ofr89319","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":"89-319","title":"Geologic map of the Opheim 1° x 30' quadrangle, Valley and Daniels counties, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89319","usgsCitation":"Colton, R.B., Whitaker, S.T., and Ehler, W., 1989, Geologic map of the Opheim 1° x 30' quadrangle, Valley and Daniels counties, Montana: U.S. Geological Survey Open-File Report 89-319, Report: 10 p.; 1 Plate: 32.69 × 28.74 inches, https://doi.org/10.3133/ofr89319.","productDescription":"Report: 10 p.; 1 Plate: 32.69 × 28.74 inches","costCenters":[],"links":[{"id":41530,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0319/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41531,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0319/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144442,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0319/report-thumb.jpg"},{"id":108795,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17633.htm","linkFileType":{"id":5,"text":"html"},"description":"17633"}],"country":"United States","state":"Montana","county":"Daniels County, Valley County","otherGeospatial":"Opheim 1° x 30' quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106,\n              48.5\n            ],\n            [\n              -107.0,\n              48.5\n            ],\n            [\n              -107.0,\n              49.0\n            ],\n            [\n              -106,\n              49.0\n            ],\n            [\n              -106,\n              48.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af6e4b07f02db692b65","contributors":{"authors":[{"text":"Colton, R. B.","contributorId":40186,"corporation":false,"usgs":true,"family":"Colton","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":167289,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitaker, S. T.","contributorId":38124,"corporation":false,"usgs":true,"family":"Whitaker","given":"S.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":167288,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ehler, W. C.","contributorId":50875,"corporation":false,"usgs":true,"family":"Ehler","given":"W. C.","affiliations":[],"preferred":false,"id":167290,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":12298,"text":"ofr8945 - 1989 - Sources of dissolved and particulate substances to the Sacramento River near Sacramento, California, summer, 1985","interactions":[],"lastModifiedDate":"2016-07-27T12:04:26","indexId":"ofr8945","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":"89-45","title":"Sources of dissolved and particulate substances to the Sacramento River near Sacramento, California, summer, 1985","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8945","usgsCitation":"Schemel, L.E., Ota, A.Y., Hager, S., and Swithenbank, A., 1989, Sources of dissolved and particulate substances to the Sacramento River near Sacramento, California, summer, 1985: U.S. Geological Survey Open-File Report 89-45, 62 p. ill., map ;28 cm., https://doi.org/10.3133/ofr8945.","productDescription":"62 p. ill., map ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":143719,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0045/report-thumb.jpg"},{"id":40526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7681","contributors":{"authors":[{"text":"Schemel, Laurence E. lschemel@usgs.gov","contributorId":4085,"corporation":false,"usgs":true,"family":"Schemel","given":"Laurence","email":"lschemel@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":165828,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ota, Allan Y.","contributorId":85192,"corporation":false,"usgs":true,"family":"Ota","given":"Allan","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":165831,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hager, S.W.","contributorId":51746,"corporation":false,"usgs":true,"family":"Hager","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":165829,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swithenbank, A.M.","contributorId":74005,"corporation":false,"usgs":true,"family":"Swithenbank","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":165830,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":27308,"text":"wri884232 - 1989 - Ground-water flow and quality near the Upper Great Lakes connecting channels, Michigan","interactions":[],"lastModifiedDate":"2025-01-10T19:49:11.566193","indexId":"wri884232","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":"88-4232","title":"Ground-water flow and quality near the Upper Great Lakes connecting channels, Michigan","docAbstract":"<p>The Upper Great Lakes connecting channels are the St. Marys, St. Clair and Detroit Rivers, and Lake St. Clair. The effect of ground water on the connecting channels is largely unknown, and the controls on its movement and quality are undefined. Geologic, hydrologic, and environmental conditions near the channels have been examined.for this investigation. Included in the study area is a 50-mile reach of channel beginning at Whitefish Bay and extending to Neebish Island, and a 90-mile reach of channel between Port Huron and Pointe Mouillee in Lake Erie. </p><p>Glacial deposits, which transmit most ground water to the channels, range from less than 100 feet in thickness in the southern part of the St. Clair-Detroit River area to more than 250 feet in thickness in the northern part. Marine seismic surveys were used at some locations to determine the thickness of deposits. Glacial deposits in the St. Marys River area range from less than 10 feet to more than 300 feet in thickness. Permeable bedrock in the southern reach of the Detroit River area and throughout most of the St. Marys River area may contribute substantial amounts of water to the channels. Total ground-water discharge to the channels, by area, is estimated as follows! St. Marys area, 76 cubic feet per second; St. Clair area, 11 cubic feet per second; Lake St. Clair area, 46 cubic feet per second; and Detroit area, 54 cubic feet per second. </p><p>Analyses of water from 31 wells, 25 of which were installed by the U.S. Geological Survey, were made for organic compounds, trace metals, and other substances. Volatile hydrocarbons, and base neutral, acid extractable, and chlorinated neutral compounds were not detectable in water at most locations. Concentrations of trace metals, however, were higher than common in natural waters at some locations. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri884232","collaboration":"Prepared in cooperation with U.S. Environmental Protection Agency","usgsCitation":"Gillespie, J., and Dumouchelle, D., 1989, Ground-water flow and quality near the Upper Great Lakes connecting channels, Michigan: U.S. Geological Survey Water-Resources Investigations Report 88-4232, Report: vii, 82 p.; 5 Plates: 20.96 x 17.54 inches or smaller, https://doi.org/10.3133/wri884232.","productDescription":"Report: vii, 82 p.; 5 Plates: 20.96 x 17.54 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":393248,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4232/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":466035,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47127.htm","text":"St. Mary's study area","linkFileType":{"id":5,"text":"html"}},{"id":119851,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4232/report-thumb.jpg"},{"id":466034,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47126.htm","text":"St. Clair - 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