No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84632","usgsCitation":"Molnia, B.F., Atwood, T.J., Carlson, P., Post, A., and Vath, S.C., 1984, Map of marine geology of Upper Muir and Wachusett Inlets, Glacier Bay, Alaska: Sediment distribution and thickness, bathymetry, and interpreted seismic profiles: U.S. Geological Survey Open-File Report 84-632, 3 Plates: 39.86 × 29.15 inches or smaller, https://doi.org/10.3133/ofr84632.","productDescription":"3 Plates: 39.86 × 29.15 inches or smaller","costCenters":[],"links":[{"id":170830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":83162,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0632/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83161,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0632/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83160,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0632/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391903,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13494.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Glacier Bay, Upper Muir and Wachusett Inlets","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -136.5106201171875,\n 58.876263846088314\n ],\n [\n -135.999755859375,\n 58.876263846088314\n ],\n [\n -135.999755859375,\n 59.16466752496466\n ],\n [\n -136.5106201171875,\n 59.16466752496466\n ],\n [\n -136.5106201171875,\n 58.876263846088314\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a92e4b07f02db657b19","contributors":{"authors":[{"text":"Molnia, Bruce F. bmolnia@usgs.gov","contributorId":4002,"corporation":false,"usgs":true,"family":"Molnia","given":"Bruce","email":"bmolnia@usgs.gov","middleInitial":"F.","affiliations":[{"id":410,"text":"National Center","active":false,"usgs":true}],"preferred":false,"id":232791,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atwood, T. J.","contributorId":25625,"corporation":false,"usgs":true,"family":"Atwood","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":232792,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carlson, P.R.","contributorId":97055,"corporation":false,"usgs":true,"family":"Carlson","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":232795,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":232794,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Vath, S. C.","contributorId":63457,"corporation":false,"usgs":true,"family":"Vath","given":"S.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":232793,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":30317,"text":"wri844267 - 1984 - Hydrology of Yucca Mountain and vicinity, Nevada-California — Investigative results through mid-1983","interactions":[],"lastModifiedDate":"2022-01-10T20:59:45.500688","indexId":"wri844267","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4267","title":"Hydrology of Yucca Mountain and vicinity, Nevada-California — Investigative results through mid-1983","docAbstract":"Yucca Mountain, Nevada, is one of several sites under consideration for construction of the first repository for high-level nuclear waste. The climate is arid; few perennial streams are present in the region. Flash floods occasionally occur. The site is underlain by at least 1,800 meters of volcanic tuffs of Tertiary age; limestones and dolomites of Paleozoic age underlie much of the surrounding region, and, together with alluvial deposits, comprise the major aquifers. Yucca Mountain is in the Alkali Flat-Furnace Creek Ranch ground-water subbasin, which is part of the Death Valley ground-water basin. Discharge occurs at Alkali Flat almost entirely by evapotranspiration, and at Furnace Creek Ranch from small springs and seeps. Beneath Yucca Mountain, depth to water ranges from about 460 to 700 meters; the rock under consideration for construction of the repository is in the unsaturated zone. Rate of recharge at Yucca Mountain is small, perhaps much less than 5 millimeters per year. Within the saturated zone, water movement is principally along fractures. The hydraulic gradient is small east (downgradient) of Yucca Mountain, and increases to the north and west. Lack of effective-porosity data presently precludes accurate calculation of flow velocity and travel times.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844267","usgsCitation":"Waddell, R.K., Robison, J.H., and Blankennagel, R., 1984, Hydrology of Yucca Mountain and vicinity, Nevada-California — Investigative results through mid-1983: U.S. Geological Survey Water-Resources Investigations Report 84-4267, vi, 72 p., https://doi.org/10.3133/wri844267.","productDescription":"vi, 72 p.","costCenters":[],"links":[{"id":394133,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36112.htm"},{"id":59109,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4267/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4267/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Yucca Mountain and vicinity","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118,\n 35.833\n ],\n [\n -114.5670,\n 35.833\n ],\n [\n -114.5670,\n 38.466\n ],\n [\n -118,\n 38.466\n ],\n [\n -118,\n 35.833\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604816","contributors":{"authors":[{"text":"Waddell, R. K.","contributorId":25560,"corporation":false,"usgs":true,"family":"Waddell","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":203045,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robison, J. H.","contributorId":60183,"corporation":false,"usgs":true,"family":"Robison","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":203046,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blankennagel, R. K.","contributorId":65078,"corporation":false,"usgs":true,"family":"Blankennagel","given":"R. K.","affiliations":[],"preferred":false,"id":203047,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":65873,"text":"i1646 - 1984 - Shaded relief map of the Casius Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:08","indexId":"i1646","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1646","subseriesTitle":"NONE","title":"Shaded relief map of the Casius Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1646","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Shaded relief map of the Casius Quadrangle of Mars: U.S. Geological Survey IMAP 1646, 1 remote-sensing image :col. ;46 x 69 cm., on sheet 76 x 78 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1646.","productDescription":"1 remote-sensing image :col. ;46 x 69 cm., on sheet 76 x 78 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189803,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260822,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1646/plate-1.pdf"}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f480b","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534227,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64679,"text":"i1496 - 1984 - Geologic map and cross sections of the San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:53","indexId":"i1496","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1496","subseriesTitle":"NONE","title":"Geologic map and cross sections of the San Joaquin Valley, California","language":"ENGLISH","doi":"10.3133/i1496","usgsCitation":"Bartow, J., 1984, Geologic map and cross sections of the San Joaquin Valley, California: U.S. Geological Survey IMAP 1496, 1 map and 7 cross sections on 2 sheets :col. ;78 x 55 cm., sheets 86 x 109 cm. and 84 x 102 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1496.","productDescription":"1 map and 7 cross sections on 2 sheets :col. ;78 x 55 cm., sheets 86 x 109 cm. and 84 x 102 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":101802,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_22.htm","linkFileType":{"id":5,"text":"html"},"description":"22"},{"id":186913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.25,35 ], [ -119.25,35.8675 ], [ -118.5,35.8675 ], [ -118.5,35 ], [ -119.25,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49f0","contributors":{"authors":[{"text":"Bartow, J. A.","contributorId":16389,"corporation":false,"usgs":true,"family":"Bartow","given":"J. A.","affiliations":[],"preferred":false,"id":271973,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29836,"text":"wri844008 - 1984 - Subsurface storage of freshwater in south Florida; evaluation of surface-water discharge data at selected sites","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri844008","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4008","title":"Subsurface storage of freshwater in south Florida; evaluation of surface-water discharge data at selected sites","docAbstract":"Canal discharge in south Florida may consist of a potential source of freshwater for deep-well injection. Discharge data for the 1970-81 water years at 27 canal and river sites were analyzed. Flow was analyzed for 30-, 60-, 90-, 120-, and 183-consecutive-day low-mean discharges during the periods of highest flow to define minimum high-flow-period fresh surface-water discharges at the 27 sites. Curves show the magnitude and frequency of average minimum flows for consecutive-day periods during high-flow periods, and duration curves and tables show the percentage of time that selected discharges were equaled or exceeded. Canal discharge as high as 660 cubic feet per second occurred 70 percent of the time during the high-flow period at one site (Tamiami Canal Outlets, Levee 67A to 40-Mile Bend). At 11 sites, discharges of 110 to 370 cubic feet per second occurred 70 percent of the high-flow periods, while at 9 sites, discharges of 21 to 100 cubic feet per second occurred 70 percent of the time during the high-flow periods. At other sites (those in the Biscayne, Plantation Road, Middle River, C-111, and Cypress Creek Canals), discharges as low as 0.1 cubic foot per second occurred 70 percent of the time during the high-flow periods. Criteria for amounts of surplus freshwater considered adequate to support injection systems cannot be established, as they would vary greatly with water needs to be satisfied and with the efficiency of a particular injection system. However, based upon this analysis of discharge at 27 canal and river sites throughout south Florida, it appears that substantial amounts of water are available for surface injection and storage. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844008","usgsCitation":"Sonntag, W.H., 1984, Subsurface storage of freshwater in south Florida; evaluation of surface-water discharge data at selected sites: U.S. Geological Survey Water-Resources Investigations Report 84-4008, viii, 75 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844008.","productDescription":"viii, 75 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159558,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4008/report-thumb.jpg"},{"id":58635,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4008/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699526","contributors":{"authors":[{"text":"Sonntag, W. H.","contributorId":106127,"corporation":false,"usgs":true,"family":"Sonntag","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":202215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30009,"text":"wri844162 - 1984 - Hydrology of Prairie Dog Creek Valley, Norton Dam to state line, north-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"wri844162","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4162","title":"Hydrology of Prairie Dog Creek Valley, Norton Dam to state line, north-central Kansas","docAbstract":"Development of water resources has been a major factor in the economy of Prairie Dog Creek Valley in north-central Kansas. Releases from Norton Reservoir to the Almena Irrigation District averaged 6,900 acre-feet per year during 1967-76. The number of irrigation wells increased from 4 to 147 during 1947-78. Ground water in the valley is derived mostly from the alluvial aquifer. The effects of irrigation on the aquifer are indicated by water-level changes. The water in storage increased from 130,000 to 136,000 acre-feet during 1947-78 due to recharge from surface-water irrigation. A steady-state model of the aquifer prior to irrigation (1947) indicated that most recharge was from precipitation (88 percent) and most discharge was to streams (54 percent) and reparian transpiration (26 percent). Although aquifer storage increased in this area, storage generally decreased in other areas of western Kansas. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844162","usgsCitation":"Stullken, L., 1984, Hydrology of Prairie Dog Creek Valley, Norton Dam to state line, north-central Kansas: U.S. Geological Survey Water-Resources Investigations Report 84-4162, vi, 49 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844162.","productDescription":"vi, 49 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4162/report-thumb.jpg"},{"id":58814,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4162/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58815,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4162/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58816,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4162/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58817,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4162/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6047de","contributors":{"authors":[{"text":"Stullken, L.E.","contributorId":59049,"corporation":false,"usgs":true,"family":"Stullken","given":"L.E.","affiliations":[],"preferred":false,"id":202523,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30322,"text":"wri844228 - 1984 - A pragmatic approach to evaluating a multipurpose stream-gaging network","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri844228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4228","title":"A pragmatic approach to evaluating a multipurpose stream-gaging network","docAbstract":"A method for evaluating the relative worth of individual streamflow gaging stations in a multipupose network is presented. Each individual gaging station in the network is evaluated on the basis of selected rating factors. The factors relate to the need for information at the gaging stations, accuracy of data, economic aspects of operation, and usefulness of data as a basis for estimates at ungaged sites. The total score for the various factors provides a convenient basis for comparing relative importance of individual gaging stations. The rating-factor method is both flexible and definitive, but the point values that are assigned for each rating factor are somewhat subjective. A table of the point values and guidelines for assigning those values is presented. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844228","usgsCitation":"Wahl, K., and Crippen, J., 1984, A pragmatic approach to evaluating a multipurpose stream-gaging network: U.S. Geological Survey Water-Resources Investigations Report 84-4228, iii, 13 p. :ill. ;28 cm., https://doi.org/10.3133/wri844228.","productDescription":"iii, 13 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4228/report-thumb.jpg"},{"id":59115,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4228/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab5ef","contributors":{"authors":[{"text":"Wahl, K.L.","contributorId":19598,"corporation":false,"usgs":true,"family":"Wahl","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":203054,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crippen, J. R.","contributorId":87985,"corporation":false,"usgs":true,"family":"Crippen","given":"J. R.","affiliations":[],"preferred":false,"id":203055,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30131,"text":"wri834252 - 1984 - Sanitary quality of the Jordan River in Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri834252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4252","title":"Sanitary quality of the Jordan River in Salt Lake County, Utah","docAbstract":"This investigation of the sanitary quality of the Jordan River was conducted from July 1980 to October 1982 using indicator bacteria rather than specific pathogens. A serious sanitary problem was identified. Concentrations of total coliform bacteria often exceeded 5,000 colonies per 100 milliliters and concentrations of fecal coliform bacteria often exceeded 2,000 colonies per 100 milliliters in the lower reaches of the river. At times these levels were greatly exceeded. The most conspicuous aspect of the bacteriological data is its extreme variability. Seven waste-water treatment plants, seven major tributaries, numerous storm conduits, irrigation-return flow, and other sources all contribute to the dynamic system that determines the sanitary quality of the river. Because of this variability the sanitary quality of the river cannot be predicted at any one time. In general, concentrations of all three indicator bacteria increased in a downstream direction. Storm runoff from urban areas contributed large concentrations of indicator bacteria to the river. Regression analysis of 9 years of data collected at 1700 South Street showed a significant positive correlation between both fecal coliform and fecal streptococcal concentrations versus time. Concentrations of fecal coliform and fecal streptococci have both been increasing since 1974 at 1700 South Street. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834252","usgsCitation":"Thompson, K.R., 1984, Sanitary quality of the Jordan River in Salt Lake County, Utah: U.S. Geological Survey Water-Resources Investigations Report 83-4252, vi, 36 p. :ill., map ;28 cm., https://doi.org/10.3133/wri834252.","productDescription":"vi, 36 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":159790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4252/report-thumb.jpg"},{"id":58936,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4252/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648546","contributors":{"authors":[{"text":"Thompson, K. R.","contributorId":92677,"corporation":false,"usgs":true,"family":"Thompson","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202732,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30130,"text":"wri844155 - 1984 - Reconnaissance of toxic substances in the Jordan River, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri844155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4155","title":"Reconnaissance of toxic substances in the Jordan River, Salt Lake County, Utah","docAbstract":"A reconnaissance of toxic substances in the Jordan River, Salt Lake County, Utah, was made during July, 1980 to October, 1982 as part of a larger study of the river that included studies of sanitary quality, dissolved oxygen, and turbidity. Samples for toxic substances were collected at five sites on the Jordan River, at three major tributaries, and at six storm drains. The toxic substance that most frequently exceeded State standards was total mercury. About 78 percent of the 138 samples for total mercury exceeded the State standard of 0.05 microgram per liter. Other toxic substances that exceeded State standards were: Ammonia-18 percent of the samples analyzed, cadmium--9 percent, copper-9 percent, zinc--6 percent, and lead--2 percent. One sample for cyanide and one for iron also exceeded State standards. The diversity of toxic substances with concentrations large enough to cause them to be problems increased from the upstream sampling site at the Jordan Narrows to the next two downstream sites at 9000 South and 5800 South Streets. Concentrations of trace elements in stream-bottom materials also increased in a downstream direction. Substantial increases first were observed at 5800 South Street, and they were sustained throughout the downstream study area. Iron is transported in the greatest quantity of all the trace elements studied, with a mean load of 110 pounds per day. Notable loads of barium, boron, lead , and zinc also are transported by the river. DDD, DDE, DDT, dieldrin, heptachlor, methoxychlor, PCB, and 2,4-D were detected in bottom materials; and DDE, Silvex, and 2,4-D were detected in water samples. Of 112 organic compounds in the Environmental Protection Agency 's priority pollutant list, only chloroform was detected in the storm drains that empty into the Joran River. Several metals and phenol also were detected in the samples for priority pollutants. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844155","usgsCitation":"Thompson, K.R., 1984, Reconnaissance of toxic substances in the Jordan River, Salt Lake County, Utah: U.S. Geological Survey Water-Resources Investigations Report 84-4155, vi, 31 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844155.","productDescription":"vi, 31 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":159781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4155/report-thumb.jpg"},{"id":58935,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4155/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db6241c2","contributors":{"authors":[{"text":"Thompson, Kendall R.","contributorId":100854,"corporation":false,"usgs":true,"family":"Thompson","given":"Kendall","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64928,"text":"i1483 - 1984 - Map showing recently active breaks along the San Andreas fault and associated faults between Salton Sea and Whitewater River-Mission Creek, California","interactions":[],"lastModifiedDate":"2012-02-02T00:13:15","indexId":"i1483","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1483","subseriesTitle":"NONE","title":"Map showing recently active breaks along the San Andreas fault and associated faults between Salton Sea and Whitewater River-Mission Creek, California","language":"ENGLISH","doi":"10.3133/i1483","usgsCitation":"Clark, M.M., 1984, Map showing recently active breaks along the San Andreas fault and associated faults between Salton Sea and Whitewater River-Mission Creek, California: U.S. Geological Survey IMAP 1483, 1 strip map on 2 sheets :col. ;sheets 101 x 127 cm. +1 pamphlet (6 p. ; 28 cm.), https://doi.org/10.3133/i1483.","productDescription":"1 strip map on 2 sheets :col. ;sheets 101 x 127 cm. +1 pamphlet (6 p. ; 28 cm.)","costCenters":[],"links":[{"id":189951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260722,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1483/plate-1.pdf"},{"id":260723,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1483/plate-2.pdf"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a38c6","contributors":{"authors":[{"text":"Clark, M. M.","contributorId":41877,"corporation":false,"usgs":true,"family":"Clark","given":"M.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":272385,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7293,"text":"ofr84523 - 1984 - Lithotectonic terrane maps of the North American Cordillera","interactions":[{"subject":{"id":7293,"text":"ofr84523 - 1984 - Lithotectonic terrane maps of the North American Cordillera","indexId":"ofr84523","publicationYear":"1984","noYear":false,"title":"Lithotectonic terrane maps of the North American Cordillera"},"predicate":"SUPERSEDED_BY","object":{"id":64517,"text":"i2176 - 1992 - Lithotectonic terrane map of the North American Cordillera","indexId":"i2176","publicationYear":"1992","noYear":false,"title":"Lithotectonic terrane map of the North American Cordillera"},"id":1}],"supersededBy":{"id":64517,"text":"i2176 - 1992 - Lithotectonic terrane map of the North American Cordillera","indexId":"i2176","publicationYear":"1992","noYear":false,"title":"Lithotectonic terrane map of the North American Cordillera"},"lastModifiedDate":"2018-01-31T15:57:29","indexId":"ofr84523","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-523","title":"Lithotectonic terrane maps of the North American Cordillera","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84523","collaboration":"Prepared in cooperation with the Geological Survey of Canada and Petroleos Mexicanos","usgsCitation":"1984, Lithotectonic terrane maps of the North American Cordillera: U.S. Geological Survey Open-File Report 84-523, Report: 106 p.; 4 Plates: 40.61 x 35.90 inches or smaller, https://doi.org/10.3133/ofr84523.","productDescription":"Report: 106 p.; 4 Plates: 40.61 x 35.90 inches or smaller","costCenters":[],"links":[{"id":350859,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0523/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350858,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0523/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350860,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0523/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350861,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0523/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350862,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0523/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0523/report-thumb.jpg"}],"scale":"2500000","country":"Canada, Mexico, United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -180.17578125,\n 13.581920900545844\n ],\n [\n -85.95703125,\n 13.581920900545844\n ],\n [\n -85.95703125,\n 71.18775391813158\n ],\n [\n -180.17578125,\n 71.18775391813158\n ],\n [\n -180.17578125,\n 13.581920900545844\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636238","contributors":{"editors":[{"text":"Silberling, N. J.","contributorId":34919,"corporation":false,"usgs":true,"family":"Silberling","given":"N. J.","affiliations":[],"preferred":false,"id":726306,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Jones, D. L.","contributorId":65045,"corporation":false,"usgs":true,"family":"Jones","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":726307,"contributorType":{"id":2,"text":"Editors"},"rank":2}]}} ,{"id":18678,"text":"ofr82818C - 1984 - Geochemical data and airborne radioactivity from parts of west-central Ventura County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:33","indexId":"ofr82818C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-818","chapter":"C","title":"Geochemical data and airborne radioactivity from parts of west-central Ventura County, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82818C","usgsCitation":"Dickinson, K.A., Frizzell, V., and Morrone, J., 1984, Geochemical data and airborne radioactivity from parts of west-central Ventura County, California: U.S. Geological Survey Open-File Report 82-818, i, 12 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82818C.","productDescription":"i, 12 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":151591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0818c/report-thumb.jpg"},{"id":48025,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0818c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48026,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0818c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48027,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0818c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae4e5","contributors":{"authors":[{"text":"Dickinson, K. A.","contributorId":77528,"corporation":false,"usgs":true,"family":"Dickinson","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179547,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frizzell, V.A.","contributorId":6877,"corporation":false,"usgs":true,"family":"Frizzell","given":"V.A.","email":"","affiliations":[],"preferred":false,"id":179546,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morrone, J.F.","contributorId":80704,"corporation":false,"usgs":true,"family":"Morrone","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":179548,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":64813,"text":"i1522E - 1984 - Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States coal, oil and gas wells, seeps and tar sandstone occurrences","interactions":[{"subject":{"id":8034,"text":"ofr83549 - 1983 - Map showing coal deposits, oil and gas wells and seeps, and tar sandstone occurrences in the Basin and Range Provinces","indexId":"ofr83549","publicationYear":"1983","noYear":false,"title":"Map showing coal deposits, oil and gas wells and seeps, and tar sandstone occurrences in the Basin and Range Provinces"},"predicate":"SUPERSEDED_BY","object":{"id":64813,"text":"i1522E - 1984 - Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States coal, oil and gas wells, seeps and tar sandstone occurrences","indexId":"i1522E","publicationYear":"1984","noYear":false,"chapter":"E","title":"Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States coal, oil and gas wells, seeps and tar sandstone occurrences"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:55","indexId":"i1522E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1522","subseriesTitle":"NONE","chapter":"E","title":"Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States coal, oil and gas wells, seeps and tar sandstone occurrences","language":"ENGLISH","doi":"10.3133/i1522E","usgsCitation":"Brady, B.T., 1984, Selected geologic and hydrologic characteristics of the Basin and Range Province, western United States coal, oil and gas wells, seeps and tar sandstone occurrences: U.S. Geological Survey IMAP 1522, 1 map :col. ;76 x 82 cm., on sheet 87 x 88 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1522E.","productDescription":"1 map :col. ;76 x 82 cm., on sheet 87 x 88 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106787,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9290.htm","linkFileType":{"id":5,"text":"html"},"description":"9290"},{"id":187278,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"2500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,29 ], [ -123,44 ], [ -102,44 ], [ -102,29 ], [ -123,29 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa63e","contributors":{"authors":[{"text":"Brady, B. T.","contributorId":93047,"corporation":false,"usgs":true,"family":"Brady","given":"B.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":272198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41997,"text":"ofr84502 - 1984 - Aeromagnetic map of the Eagle Mountains area, Riverside County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:02","indexId":"ofr84502","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-502","title":"Aeromagnetic map of the Eagle Mountains area, Riverside County, California","language":"ENGLISH","doi":"10.3133/ofr84502","usgsCitation":"Grauch, V., 1984, Aeromagnetic map of the Eagle Mountains area, Riverside County, California: U.S. Geological Survey Open-File Report 84-502, 1 map :photocopy ;45 x 73 cm., on sheet 73 x 108 cm., https://doi.org/10.3133/ofr84502.","productDescription":"1 map :photocopy ;45 x 73 cm., on sheet 73 x 108 cm.","costCenters":[],"links":[{"id":135459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79754,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0502/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696799","contributors":{"authors":[{"text":"Grauch, V.J. 0000-0002-0761-3489","orcid":"https://orcid.org/0000-0002-0761-3489","contributorId":70362,"corporation":false,"usgs":true,"family":"Grauch","given":"V.J.","affiliations":[],"preferred":false,"id":225821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":30030,"text":"wri844343 - 1984 - Summary of results of an investigation to define the geohydrology and simulate the effects of large ground-water withdrawals on the Mississippi River alluvial aquifer in northwestern Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:08:59","indexId":"wri844343","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4343","title":"Summary of results of an investigation to define the geohydrology and simulate the effects of large ground-water withdrawals on the Mississippi River alluvial aquifer in northwestern Mississippi","docAbstract":"The 7,000 square-mile Mississippi River alluvial plain in north-western Mississippi (the Delta) is underlain by the prolific Mississippi River alluvial aquifer that currently (1983) yields about 1,100 Mgal/d of water to irrigation wells. Commonly, about 20 feet of clay underlying the Delta land surface is underlain by about 80 to 180 feet of sand and gravel that forms the aquifer. The Mississippi River is in good hydraulic connection with the alluvial aquifer. Generally smaller streams are less likely to have good hydraulic connection with the aquifer. Direct vertical recharge to the alluvial aquifer is small. A two-dimensional finite-difference computer model of the alluvial aquifer was constructed, calibrated, and verified using water levels observed for five dates within the period April 1981 to September 1983. The model shows that the aquifer had a net loss in storage of about 360 Mgal/d for the 2-year period April 1981 to April 1983, when pumpage was about 1,100 Mgal/d. The net inflows from the sources of recharge were: Mississippi River, 390 Mgal/d; recharge along east edge of the Delta, 170 Mgal/d; streams within the Delta, 81 Mgal/d; and areal recharge from infiltration, 180 Mgal/d. The effects of several levels of pumpage by wells were projected 20 years into the future. In 2003, the result of continued pumpage at the 1,100 Mgal/d pumping rate would be lowered ground-water levels of more than 20 feet in a large area in the central part of the Delta, and ground-water levels would continue to decline. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844343","usgsCitation":"Sumner, D.M., and Wasson, B.E., 1984, Summary of results of an investigation to define the geohydrology and simulate the effects of large ground-water withdrawals on the Mississippi River alluvial aquifer in northwestern Mississippi: U.S. Geological Survey Water-Resources Investigations Report 84-4343, iii, 17 p. :maps ;28 cm., https://doi.org/10.3133/wri844343.","productDescription":"iii, 17 p. :maps ;28 cm.","costCenters":[],"links":[{"id":160090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4343/report-thumb.jpg"},{"id":58833,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4343/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f9e","contributors":{"authors":[{"text":"Sumner, D. M.","contributorId":100827,"corporation":false,"usgs":true,"family":"Sumner","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":202561,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wasson, B. E.","contributorId":11204,"corporation":false,"usgs":true,"family":"Wasson","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":202560,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42340,"text":"ofr84390 - 1984 - Reconnaissance geologic map of the Janban Quadrangle, sheet 20/44 B, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-07T18:15:58","indexId":"ofr84390","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-390","title":"Reconnaissance geologic map of the Janban Quadrangle, sheet 20/44 B, Kingdom of Saudi Arabia","docAbstract":"The Janban quadrangle, 20/44B, lies along the eastern margin of the Arabian Shield. The oldest rocks comprise the Precambrian Namtah Formation of the Halaban(?) group, and consist of basalt, dacite, siltstone, and calcareous greywacke metamorphosed in the lower amphibolite facies. Metamorphic rocks of uncertain Precambrian age in the northern part of the quadrangle are amphibolite, gneissic quartz diorite and metarhyolite that occur as roof pendants in plutonic rocks. Precambrian intrusive rocks, in order of decreasing age, are: biotite-hornblende tonalite; the locally gneissic Dawasir granodiorite and granite; the as Sabahah granite, coarse-grained alkaline granite; biotite-muscovite granite forming a small circular stock; the Janban granite, a coarse-grained non-foliated alkali-feldspar rapakiyl granite; aplitic granite; and fine-grained alkali granite that forms a stock, plugs, and dikes. Andesite dikes cut most of the plutonic rock units. Precambrian rocks are unconformably overlain by the Wajid Sandstone of Cambrian and Ordovician age, which covers the southeastern half of the quadrangle and consists of reddish-brown, medium-grained arkosic sandstone. Tertiary lake beds of gray marl, siltstone, and sandstone crop out locally, and lie unconformably on the Wajid. Most of the Wajid sandstone is mantled by an extensive blanket of Quaternary eolian sand and silt.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84390","usgsCitation":"Brock, M.R., 1984, Reconnaissance geologic map of the Janban Quadrangle, sheet 20/44 B, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 84-390, 2 maps :photocopy ;55 x 52 cm., on sheets 76 x 106 cm. and 76 x 77 cm. folded in envelope 28 x 22 cm., https://doi.org/10.3133/ofr84390.","productDescription":"2 maps :photocopy ;55 x 52 cm., on sheets 76 x 106 cm. and 76 x 77 cm. folded in envelope 28 x 22 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":135633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80105,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0390/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80106,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0390/plate-2.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 45,\n 21.5 \n ],\n [\n 45,\n 21\n ],\n [\n 44.5,\n 21\n ],\n [\n 44.5,\n 21.5 \n ],\n [\n 45,\n 21.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a71e4b07f02db6421e1","contributors":{"authors":[{"text":"Brock, M. R.","contributorId":96230,"corporation":false,"usgs":true,"family":"Brock","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":226321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":36600,"text":"fwsobs82_08 - 1984 - The ecology of the South Florida coral reefs: a community profile","interactions":[],"lastModifiedDate":"2012-02-02T00:09:53","indexId":"fwsobs82_08","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/08","title":"The ecology of the South Florida coral reefs: a community profile","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Japp, W.C., 1984, The ecology of the South Florida coral reefs: a community profile: FWS/OBS 82/08, xii, 138 p. : ill. (some col.), maps; 28 cm.","productDescription":"xii, 138 p. : ill. (some col.), maps; 28 cm.","costCenters":[],"links":[{"id":165616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6681e3","contributors":{"authors":[{"text":"Japp, Walter C.","contributorId":86639,"corporation":false,"usgs":true,"family":"Japp","given":"Walter","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":216618,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41258,"text":"ofr84814 - 1984 - Potentiometric surface of the upper Floridan Aquifer in central Sumter County, Florida, May 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:11:10","indexId":"ofr84814","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-814","title":"Potentiometric surface of the upper Floridan Aquifer in central Sumter County, Florida, May 1984","docAbstract":"This map presents the potentiometric surface of the upper Floridan aquifer in central Sumter County, Florida, for May 1984. The Floridan aquifer system is the principal source of potable water in the area. The focus of the map is the potentiometric surface in the Jumper Creek Canal area. Water level measurements were made on approximately 60 wells. The potentiometric surface ranged in altitude from more than 90 feet in the southeastern part of the county to less than 40 feet northwest of lake Panasoffkee in the west-central area. (USGS)","language":"ENGLISH","doi":"10.3133/ofr84814","usgsCitation":"Bradner, L.A., 1984, Potentiometric surface of the upper Floridan Aquifer in central Sumter County, Florida, May 1984: U.S. Geological Survey Open-File Report 84-814, 1 map :photocopy ;52 x 73 cm., on sheet 76 x 87 cm., https://doi.org/10.3133/ofr84814.","productDescription":"1 map :photocopy ;52 x 73 cm., on sheet 76 x 87 cm.","costCenters":[],"links":[{"id":176695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79054,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0814/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682dab","contributors":{"authors":[{"text":"Bradner, L. A.","contributorId":21925,"corporation":false,"usgs":true,"family":"Bradner","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":224725,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18545,"text":"ofr84174 - 1984 - Factor analysis of the chemistry of Spanish moss","interactions":[],"lastModifiedDate":"2012-02-02T00:07:27","indexId":"ofr84174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-174","title":"Factor analysis of the chemistry of Spanish moss","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84174","usgsCitation":"Connor, J.J., and Shacklette, H., 1984, Factor analysis of the chemistry of Spanish moss: U.S. Geological Survey Open-File Report 84-174, ii, 39 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84174.","productDescription":"ii, 39 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":150855,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0174/report-thumb.jpg"},{"id":47894,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0174/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a05e4b07f02db5f883d","contributors":{"authors":[{"text":"Connor, J. J.","contributorId":56224,"corporation":false,"usgs":true,"family":"Connor","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":179313,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shacklette, H.T.","contributorId":61813,"corporation":false,"usgs":true,"family":"Shacklette","given":"H.T.","affiliations":[],"preferred":false,"id":179314,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":64866,"text":"i1447 - 1984 - Reconnaissance geologic map of the Precambrian Farmington Canyon complex and surrounding rocks in the Wasatch Mountains between Ogden and Bountiful, Utah","interactions":[{"subject":{"id":42845,"text":"ofr79709 - 1979 - Reconnaissance geologic map of the Precambrian Farmington Canyon complex and surrounding rocks in the Wasatch Mountains between Ogden and Bountiful, Utah","indexId":"ofr79709","publicationYear":"1979","noYear":false,"title":"Reconnaissance geologic map of the Precambrian Farmington Canyon complex and surrounding rocks in the Wasatch Mountains between Ogden and Bountiful, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":64866,"text":"i1447 - 1984 - Reconnaissance geologic map of the Precambrian Farmington Canyon complex and surrounding rocks in the Wasatch Mountains between Ogden and Bountiful, Utah","indexId":"i1447","publicationYear":"1984","noYear":false,"title":"Reconnaissance geologic map of the Precambrian Farmington Canyon complex and surrounding rocks in the Wasatch Mountains between Ogden and Bountiful, Utah"},"id":1}],"lastModifiedDate":"2025-08-04T18:41:15.57252","indexId":"i1447","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1447","title":"Reconnaissance geologic map of the Precambrian Farmington Canyon complex and surrounding rocks in the Wasatch Mountains between Ogden and Bountiful, Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1447","usgsCitation":"Bryant, B., 1984, Reconnaissance geologic map of the Precambrian Farmington Canyon complex and surrounding rocks in the Wasatch Mountains between Ogden and Bountiful, Utah: U.S. Geological Survey IMAP 1447, 1 Plate: 34.57 x 40.50 inches, https://doi.org/10.3133/i1447.","productDescription":"1 Plate: 34.57 x 40.50 inches","costCenters":[],"links":[{"id":255249,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1447/report-thumb.jpg"},{"id":255248,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1447/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":493477,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9246.htm","linkFileType":{"id":5,"text":"html"}},{"id":255247,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1447/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"50000","state":"Utah","city":"Bountiful, Ogden","otherGeospatial":"Precambrian Farmington Canyon complex and surrounding rocks in the Wasatch Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -111.933,\n 41.25\n ],\n [\n -111.933,\n 40.817\n ],\n [\n -111.7,\n 40.817\n ],\n [\n -111.7,\n 41.25\n ],\n [\n -111.933,\n 41.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682ef0","contributors":{"authors":[{"text":"Bryant, Bruce bbryant@usgs.gov","contributorId":1355,"corporation":false,"usgs":true,"family":"Bryant","given":"Bruce","email":"bbryant@usgs.gov","affiliations":[],"preferred":false,"id":272281,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29639,"text":"wri844118 - 1984 - Hydrology of the Tertiary-Cretaceous aquifer system in the vicinity of Fort Rucker Aviation Center, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri844118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4118","title":"Hydrology of the Tertiary-Cretaceous aquifer system in the vicinity of Fort Rucker Aviation Center, Alabama","docAbstract":"Fort Rucker Aviation Center, built in 1941-42, uses ground water for its water supply. The demand for water began to exceed the capacity of the well field in 1976. The Tertiary-Cretaceous aquifer system in the Fort Rucker area consists of an upper and lower aquifer. The upper aquifer consists of the basal part of the Tuscahoma Sand, the Nanafalia and Clayton Formations, and the upper part of the Providence Sand. The lower aquifer consists of the lower part of the Providence Sand and the Ripley Formation. Most large capacity (greater than 100 gal/min (gallons per minute)) wells in the Fort Rucker area are developed in one of these aquifers, and produce 500 gal/min or more. An aquifer test made at Fort Rucker during the study indicates that the transmissivity of the upper aquifer is about 7,000 ft sq/d (feet squared per day). This test and a potentiometric map of the area indicate that wells spaced too closely together is a major problem at pumping centers in the study area. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844118","usgsCitation":"Scott, J.C., Law, L., and Cobb, R., 1984, Hydrology of the Tertiary-Cretaceous aquifer system in the vicinity of Fort Rucker Aviation Center, Alabama: U.S. Geological Survey Water-Resources Investigations Report 84-4118, v, 221 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844118.","productDescription":"v, 221 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4118/report-thumb.jpg"},{"id":58462,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4118/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdb2b","contributors":{"authors":[{"text":"Scott, J. C.","contributorId":75901,"corporation":false,"usgs":true,"family":"Scott","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201863,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Law, L.R.","contributorId":71596,"corporation":false,"usgs":true,"family":"Law","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":201862,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cobb, Riley","contributorId":107325,"corporation":false,"usgs":true,"family":"Cobb","given":"Riley","email":"","affiliations":[],"preferred":false,"id":201864,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30134,"text":"wri834117B - 1984 - Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range Province, Idaho","interactions":[],"lastModifiedDate":"2021-12-21T19:43:06.193494","indexId":"wri834117B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4117","chapter":"B","title":"Maps showing distribution of dissolved solids and dominant chemical type in ground water, Basin and Range Province, Idaho","docAbstract":"This map report is one of a series of geologic and hydrologic maps of States in the Basin and Range Province. These map reports contain information on ground-water hydrology, ground-water quality, surface distribution of selected rock types, data on tectonic conditions, areal geophysical data, Pleistocene lakes and marshes and natural resources. This information is the basis tor a summary report that characterizes the Basin and Range Province. The geologic and hydrologic characterization will be used to evaluate the Province for prospective regions for further study relative to isolation of high-level radioactive waste. (Bedinger, Sargent and Reed, 1984).
A variety of land uses affects water quality of streams at the Indiana Dunes National Lakeshore. Discharge from storm sewers and runoff from roads contributed lead, zinc, and chlorinated hydrocarbons (chlordane, DOT, ODD, DDE, and PCB's) to all streams except Derby ditch. In addition, the Little Calumet River received ammonia from industrial discharges, and organic materials, nitrogen, phosphorus, and fecal coliform from wastewater-treatment-plant and combinedsanitary- and storm-sewer discharges. As a result, water at some sites in the lower reaches of the Little Calumet River contained dissolved-ammonium-nitrogen concentrations exceeding 0.10 milligram per liter, dissolved-oxygen concentrations less than 3.0 milligrams per liter, and fecal coliform populations exceeding 2,000 colonies per 100 milliliters.
\nSeepage from two landfills may have caused the concentration of dissolved solids in the west Grand Calumet River lagoon to exceed that in the east lagoon. Ammonium concentrations in the west lagoon ranged from 13 to 16 milligrams per liter as nitrogen.
\nPesticides used in agricultural areas were the major source of DOT, ODD, DDE, and dieldrin on streambed materials. Runoff from residential areas was a major source of nitrate, organic materials, and chlordane in Derby ditch and Dunes Creek.
\nWetland drainage contributed significant amounts of organic materials to streams and at times increased concentrations of dissolved sulfate and iron. Dissolved-iron concentrations correlated with dissolved-organic-carbon concentrations in yellow-brown water of Kintzele and Derby ditches.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri834208","collaboration":"National Park Service","usgsCitation":"Hardy, M.A., 1984, Chemical and biological quality of streams at the Indiana Dunes National Lakeshore, Indiana, 1978-80: U.S. Geological Survey Water-Resources Investigations Report 83-4208, viii, 95 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834208.","productDescription":"viii, 95 p. :ill., maps ;28 cm.","startPage":"1","endPage":"95","numberOfPages":"105","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":123388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4208/report-thumb.jpg"},{"id":56400,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4208/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","otherGeospatial":"Indiana Dunes National Lakeshore","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.28869438171387,\n 41.621923034123846\n ],\n [\n -87.26963996887207,\n 41.621730547188456\n ],\n [\n -87.26912498474121,\n 41.60806250618307\n ],\n [\n -87.24603652954102,\n 41.608511736657555\n ],\n [\n -87.24303245544434,\n 41.609859409312534\n ],\n [\n -87.24311828613281,\n 41.61306804041503\n ],\n [\n -87.23959922790527,\n 41.61313221140915\n ],\n [\n -87.23779678344727,\n 41.61396642852365\n ],\n [\n -87.23367691040039,\n 41.61441561788573\n ],\n [\n -87.23221778869629,\n 41.61249049859493\n ],\n [\n -87.2306728363037,\n 41.61531398722544\n ],\n [\n -87.2303295135498,\n 41.61614817612265\n ],\n [\n -87.22672462463377,\n 41.61499314246908\n ],\n [\n -87.22346305847167,\n 41.618329849922084\n ],\n [\n -87.22466468811035,\n 41.62558017672615\n ],\n [\n -87.17668533325195,\n 41.63578058345409\n ],\n [\n -87.17471122741699,\n 41.62301378257129\n ],\n [\n -87.17968940734863,\n 41.62275713753768\n ],\n [\n -87.18063354492188,\n 41.621923034123846\n ],\n [\n -87.1805477142334,\n 41.61807318624671\n ],\n [\n -87.18818664550781,\n 41.616725685192804\n ],\n [\n -87.1889591217041,\n 41.61634067972058\n ],\n [\n -87.18844413757324,\n 41.61364557706411\n ],\n [\n -87.18973159790039,\n 41.61358140658068\n ],\n [\n -87.19127655029297,\n 41.60799833014563\n ],\n [\n -87.19874382019043,\n 41.605174521299304\n ],\n [\n -87.19951629638672,\n 41.60645808609603\n ],\n [\n -87.20681190490723,\n 41.607677449000946\n ],\n [\n -87.2068977355957,\n 41.60273567783677\n ],\n [\n -87.21256256103516,\n 41.59978327031246\n ],\n [\n -87.21359252929686,\n 41.603698390215456\n ],\n [\n -87.22123146057129,\n 41.60286404031713\n ],\n [\n -87.22294807434082,\n 41.600040006763784\n ],\n [\n -87.23161697387695,\n 41.600681843423565\n ],\n [\n -87.23153114318848,\n 41.59644560350027\n ],\n [\n -87.25247383117676,\n 41.59792190049485\n ],\n [\n -87.25273132324217,\n 41.60061766004485\n ],\n [\n -87.25496292114258,\n 41.60074602673845\n ],\n [\n -87.2548770904541,\n 41.60382675078074\n ],\n [\n -87.27805137634276,\n 41.60389093096761\n ],\n [\n -87.27865219116211,\n 41.59914142471562\n ],\n [\n -87.34139442443848,\n 41.605880485097465\n ],\n [\n -87.32903480529784,\n 41.60645808609603\n ],\n [\n -87.31126785278319,\n 41.60594466324155\n ],\n [\n -87.30174064636229,\n 41.609153489052005\n ],\n [\n -87.28517532348633,\n 41.609602711929725\n ],\n [\n -87.28526115417479,\n 41.61640484745891\n ],\n [\n -87.28963851928711,\n 41.616854019839494\n ],\n [\n -87.29006767272949,\n 41.62205135842823\n ],\n [\n -87.28869438171387,\n 41.621923034123846\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bcbb8","contributors":{"authors":[{"text":"Hardy, M. A.","contributorId":54223,"corporation":false,"usgs":true,"family":"Hardy","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198295,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28129,"text":"wri834197 - 1984 - Preliminary estimate of possible flood elevations in the Columbia River at Trojan Nuclear Power Plant due to failure of debris dam blocking Spirit Lake, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri834197","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4197","title":"Preliminary estimate of possible flood elevations in the Columbia River at Trojan Nuclear Power Plant due to failure of debris dam blocking Spirit Lake, Washington","docAbstract":"Failure of the debris dam, blocking the outflow of Spirit Lake near Mount St. Helens, could result in a mudflow down the Toutle and Cowlitz Rivers into the Columbia River. Flood elevations at the Trojan Nuclear Power Plant on the Columbia River, 5 mi upstream from the Cowlitz River, were simulated with a hydraulic routing model. The simulations are made for four Columbia River discharges in each of two scenarios, one in which Columbia River floods coincide with a mudflow and the other in which Columbia River floods follow a mudflow sediment deposit upstream from the Cowlitz River. In the first scenario, Manning 's roughness coefficients for clear water and for mudflow in the Columbia River are used; in the second scenario only clear water coefficients are used. The grade elevation at the power plant is 45 ft above sea level. The simulated elevations exceed 44 ft if the mudflow coincides with a Columbia River discharge that has a recurrence interval greater than 10 years (610,000 cu ft/sec); the mudflow is assumed to extend downstream from the Cowlitz River to the mouth of the Columbia River, and Manning 's roughness coefficients for a mudflow are used. The simulated elevation is 32 ft if the mudflow coincides with a 100-yr flood (820,000 cu ft/sec) and clear-water Manning 's coefficients are used throughout the entire reach of the Columbia River. The elevations exceed 45 ft if a flow exceeding the 2-yr peak discharge in the Columbia River (410,000 cu ft/sec) follows the deposit of 0.5 billion cu yd of mudflow sediment upstream of the Cowlitz River before there has been any appreciable scour or dredging of the deposit. In this simulation it is assumed that: (1) the top of the sediment deposited in the Columbia River is at an elevation of 30 ft at the mouth of the Cowlitz River, (2) the surface elevation of the sediment deposit decreases in an upstream direction at a rate of 2.5 ft/mi, and (3) clear water Manning 's coefficients apply to the entire modeled reach of the Columbia River. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834197","usgsCitation":"Kresch, D., and Laenen, A., 1984, Preliminary estimate of possible flood elevations in the Columbia River at Trojan Nuclear Power Plant due to failure of debris dam blocking Spirit Lake, Washington: U.S. Geological Survey Water-Resources Investigations Report 83-4197, iv, 11 p. :map ;28 cm., https://doi.org/10.3133/wri834197.","productDescription":"iv, 11 p. :map ;28 cm.","costCenters":[],"links":[{"id":158616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4197/report-thumb.jpg"},{"id":56962,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4197/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d45","contributors":{"authors":[{"text":"Kresch, D. L.","contributorId":52559,"corporation":false,"usgs":true,"family":"Kresch","given":"D. L.","affiliations":[],"preferred":false,"id":199267,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laenen, Antonius","contributorId":107673,"corporation":false,"usgs":true,"family":"Laenen","given":"Antonius","email":"","affiliations":[],"preferred":false,"id":199268,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}