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,{"id":26186,"text":"wri894160 - 1989 - Sedimentation of Lake Taneycomo, Missouri, 1913-1987","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri894160","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":"89-4160","title":"Sedimentation of Lake Taneycomo, Missouri, 1913-1987","docAbstract":"On the basis of the data from a sedimentation survey done by the U.S. Department of Agriculture, Soil Conservation Service, during 1935 and data collected by the U.S. Geological Survey during 1987, the volume of sediment accumulated in Lake Taneycomo from 1913 to 1935 and 1913 to 1987 was determined. Table Rock Dam, built directly upstream from Lake Taneycomo during 1958, eliminated about 92% of the 4,644-sq mi basin from contributing sediment directly to the lake. Cesium-137 isotope was used as a tracer in the sediment to determine the quantity of deposition in the lake after Table Rock Dam was completed. The relation between cross-sectional area and distance upstream from the dam (curve method) was used to determine the 1913 (original), the 1935, and the 1987 volumes of Lake Taneycomo. A total of 910,000,000 cu ft of sediment accumulated between 1913 and 1935, 42% of the original volume of the lake. A total of 1 ,066,000,000 cu ft of sediment accumulated between 1913 and 1987 , 49% of the original volume. Lake Taneycomo seems to be functioning as an alluvial river, responding to the new energy gradient established by the spillway at Ozark Beach Dam, and later to changes in the sediment load. The upper two-thirds of the lake seems to have been scoured after Table Rock Dam greatly decreased the sediment load to the lake. The cesium-137 analysis indicated that sediment is still accumulating in the lower reaches of the lake, with measured accumulation generally ranging from 0.2 to 2.6 ft. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-file report [distributor],","doi":"10.3133/wri894160","usgsCitation":"Berkas, W., 1989, Sedimentation of Lake Taneycomo, Missouri, 1913-1987: U.S. Geological Survey Water-Resources Investigations Report 89-4160, vii, 80 p. :ill. ;28 cm., https://doi.org/10.3133/wri894160.","productDescription":"vii, 80 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":157615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4160/report-thumb.jpg"},{"id":54984,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a1ee","contributors":{"authors":[{"text":"Berkas, W.R.","contributorId":59808,"corporation":false,"usgs":true,"family":"Berkas","given":"W.R.","affiliations":[],"preferred":false,"id":195956,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14259,"text":"ofr89401 - 1989 - Compilation of geohydrologic data collected as part of the areal appraisal of ground-water resources near Branson, Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:06:45","indexId":"ofr89401","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":"89-401","title":"Compilation of geohydrologic data collected as part of the areal appraisal of ground-water resources near Branson, Missouri","docAbstract":"A rapidly developing retirement community and tourist industry in the Branson, Missouri area has created an increased demand for potable water, especially in the summer months. The rapid pace of residential and business expansion has created concerns regarding the future groundwater availability and quality. Water levels measured in the Ozark aquifer during the summer of 1988 and March 1989 show water levels increasing in 22 wells, decreasing in 2 wells, and remaining the same in 1 well. The water level increases ranged from 1 to 111 ft. These measurements and similar measurements during the summer of 1989 will be used to calibrate a three-dimensional model of groundwater flow in the Branson area and estimate the long-term effect of large groundwater withdrawals during the summer tourist season. A reconnaissance of water quality in 34 wells that are open to the Ozark aquifer shows specific conductance ranging from 347 to 841 microsiemens/cm at 25 C and no fecal coliform bacteria present in any well. Chloride and nitrate concentrations in all wells were well below the Missouri Department of Natural Resources recommended maximum concentrations of 250 mg/L and 10 mg/L, respectively. Analysis of 5 water samples for 33 volatile organic compounds failed to detect any concentrations in excess of the detection limits. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/ofr89401","usgsCitation":"Imes, J., 1989, Compilation of geohydrologic data collected as part of the areal appraisal of ground-water resources near Branson, Missouri: U.S. Geological Survey Open-File Report 89-401, v, 24 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89401.","productDescription":"v, 24 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":146304,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0401/report-thumb.jpg"},{"id":42940,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0401/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a984e","contributors":{"authors":[{"text":"Imes, J. L.","contributorId":61428,"corporation":false,"usgs":true,"family":"Imes","given":"J. L.","affiliations":[],"preferred":false,"id":169163,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14907,"text":"ofr89301 - 1989 - Analytical results and sample locality maps for 12 water samples from  springs and domestic wells near the El Dorado, Lime Canyon, and Million Hills Wilderness Study Areas, Clark County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr89301","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":"89-301","title":"Analytical results and sample locality maps for 12 water samples from  springs and domestic wells near the El Dorado, Lime Canyon, and Million Hills Wilderness Study Areas, Clark County, Nevada","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr89301","usgsCitation":"McHugh, J., and Nowlan, G., 1989, Analytical results and sample locality maps for 12 water samples from  springs and domestic wells near the El Dorado, Lime Canyon, and Million Hills Wilderness Study Areas, Clark County, Nevada: U.S. Geological Survey Open-File Report 89-301, 10 p.  :maps ;28 cm., https://doi.org/10.3133/ofr89301.","productDescription":"10 p.  :maps ;28 cm.","costCenters":[],"links":[{"id":146333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0301/report-thumb.jpg"},{"id":43714,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1989/0301/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43715,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0301/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e3ee","contributors":{"authors":[{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":170213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":170214,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27962,"text":"wri864345 - 1989 - Quality of water and bottom material of streams that drain potential lignite mining areas in the outcrop area of the Wilcox Group in Mississippi","interactions":[],"lastModifiedDate":"2022-09-28T20:40:30.562705","indexId":"wri864345","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":"86-4345","title":"Quality of water and bottom material of streams that drain potential lignite mining areas in the outcrop area of the Wilcox Group in Mississippi","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864345","usgsCitation":"Kalkhoff, S., 1989, Quality of water and bottom material of streams that drain potential lignite mining areas in the outcrop area of the Wilcox Group in Mississippi: U.S. Geological Survey Water-Resources Investigations Report 86-4345, v, 34 p., https://doi.org/10.3133/wri864345.","productDescription":"v, 34 p.","costCenters":[],"links":[{"id":407553,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36658.htm","linkFileType":{"id":5,"text":"html"}},{"id":158591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4345/report-thumb.jpg"},{"id":56778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4345/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Mississippi","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90,\n              32.267\n            ],\n            [\n              -88.096,\n              32.267\n            ],\n            [\n              -88.096,\n              35\n            ],\n            [\n              -90,\n              35\n            ],\n            [\n              -90,\n              32.267\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db65178f","contributors":{"authors":[{"text":"Kalkhoff, S. J.","contributorId":28967,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"S. J.","affiliations":[],"preferred":false,"id":198972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16240,"text":"ofr88453 - 1989 - Data on ground-water quality, Carson Valley and Topaz Lake areas, Douglas County, Nevada, for year ending September 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:07:05","indexId":"ofr88453","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":"88-453","title":"Data on ground-water quality, Carson Valley and Topaz Lake areas, Douglas County, Nevada, for year ending September 1986","docAbstract":"Douglas County, Nevada encompasses 708 sq mi and has been one of the fastest growing counties in the Nation, according to the 1980 census. This rapid population growth has led to concern about the present and future impacts of development upon the groundwater. A network of 33 wells was recently established (1985) in the Carson Valley and Topaz Lake areas of Douglas County to characterize the current groundwater quality and its seasonal variability and to monitor temporal responses to changing land-use activities. This report presents data collected from that network during November 1985 through September 1986. The primary drinking water standard was exceeded for fluoride at two domestic wells, for nitrate-nitrogen at one domestic well, and for arsenic in one non-domestic shallow monitoring well. Secondary drinking water standards were exceeded as follows: pH at one public-supply well and one domestic well; sulfate at one shallow monitoring well; and manganese at three shallow monitoring wells and one public-supply well. Concentrations of unidentified organic compounds were estimated by gas chromatograph and flame ionization detector for groundwater samples collected from 30 network wells. Seven wells (2 domestic and 5 non-domestic) had concentrations greater than 10 micrograms/L relative to the internal standard compound perdeuteronaphthalene. (Thacker-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nCopies of this report may be purchased from U.S. Geological Survey Books and Open-File Reports Section,","doi":"10.3133/ofr88453","usgsCitation":"Thodal, C.E., 1989, Data on ground-water quality, Carson Valley and Topaz Lake areas, Douglas County, Nevada, for year ending September 1986: U.S. Geological Survey Open-File Report 88-453, v, 55 p. ill. ;28 cm., https://doi.org/10.3133/ofr88453.","productDescription":"v, 55 p. ill. ;28 cm.","costCenters":[],"links":[{"id":148919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0453/report-thumb.jpg"},{"id":45162,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0453/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c821","contributors":{"authors":[{"text":"Thodal, Carl E. 0000-0003-0782-3280 cethodal@usgs.gov","orcid":"https://orcid.org/0000-0003-0782-3280","contributorId":2292,"corporation":false,"usgs":true,"family":"Thodal","given":"Carl","email":"cethodal@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":172473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34526,"text":"b1789 - 1989 - Geology and ground-water hydrology of Spirit Lake blockage, Mount St. Helens, Washington, with implications for lake retention","interactions":[],"lastModifiedDate":"2021-11-04T18:52:23.687525","indexId":"b1789","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":"1789","title":"Geology and ground-water hydrology of Spirit Lake blockage, Mount St. Helens, Washington, with implications for lake retention","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1789","usgsCitation":"Glicken, H.X., Meyer, W., and Sabol, M.A., 1989, Geology and ground-water hydrology of Spirit Lake blockage, Mount St. Helens, Washington, with implications for lake retention: U.S. Geological Survey Bulletin 1789, Report: iv, 33 p.; 3 Plates: 41.00 × 29.50 inches or smaller, https://doi.org/10.3133/b1789.","productDescription":"Report: iv, 33 p.; 3 Plates: 41.00 × 29.50 inches or smaller","costCenters":[],"links":[{"id":62404,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1789/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62403,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1789/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62402,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1789/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62401,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1789/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1789/report-thumb.jpg"},{"id":109796,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21936.htm","linkFileType":{"id":5,"text":"html"},"description":"21936"}],"country":"United States","state":"Washington","otherGeospatial":"Mount St, Helens, Spirit Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.23594665527342,\n              46.22284011773094\n            ],\n            [\n              -122.14530944824217,\n              46.22284011773094\n            ],\n            [\n              -122.14530944824217,\n              46.28503762859978\n            ],\n            [\n              -122.23594665527342,\n              46.28503762859978\n            ],\n            [\n              -122.23594665527342,\n              46.22284011773094\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685dce","contributors":{"authors":[{"text":"Glicken, Harry X.","contributorId":83580,"corporation":false,"usgs":true,"family":"Glicken","given":"Harry","email":"","middleInitial":"X.","affiliations":[],"preferred":false,"id":213113,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":213114,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sabol, Martha A.","contributorId":80334,"corporation":false,"usgs":true,"family":"Sabol","given":"Martha","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":213112,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26413,"text":"wri884214 - 1989 - Calibration and use of an interactive-accounting model to simulate dissolved solids, streamflow, and water-supply operations in the Arkansas River basin, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri884214","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":"88-4214","title":"Calibration and use of an interactive-accounting model to simulate dissolved solids, streamflow, and water-supply operations in the Arkansas River basin, Colorado","docAbstract":"An interactive-accounting model was used to simulate dissolved solids, streamflow, and water supply operations in the Arkansas River basin, Colorado. Model calibration of specific conductance to streamflow relations at three sites enabled computation of dissolved-solids loads throughout the basin. To simulate streamflow only, all water supply operations were incorporated in the regression relations for streamflow. Calibration for 1940-85 resulted in coefficients of determination that ranged from 0.89 to 0.58, and values in excess of 0.80 were determined for 16 of 20 nodes. The model then incorporated 74 water users and 11 reservoirs to simulate the water supply operations for two periods, 1943-74 and 1975-85. For the 1943-74 calibration, coefficients of determination for streamflow ranged from 0.87 to 0.02. Calibration of the water supply operations resulted in coefficients of determination that ranged from 0.87 to negative for simulated irrigation diversions of 37 selected water users. Calibration for 1975-85 was not evaluated statistically, but average values and plots of reservoir contents indicated reasonableness of the simulation. To demonstrate the utility of the model, six specific alternatives were simulated to consider effects of potential enlargement of Pueblo Reservoir. Three general major alternatives were simulated: the 1975-85 calibrated model data, the calibrated model data with an addition of 30 cu ft/sec in Fountain Creek flows, and the calibrated model data plus additional municipal water in storage. These three major alternatives considered the options of reservoir enlargement or no enlargement. A 40,000-acre-foot reservoir enlargement resulted in average increases of 2,500 acre-ft in transmountain diversions, of 800 acre-ft in storage diversions, and of 100 acre-ft in winter-water storage. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884214","usgsCitation":"Burns, A., 1989, Calibration and use of an interactive-accounting model to simulate dissolved solids, streamflow, and water-supply operations in the Arkansas River basin, Colorado: U.S. Geological Survey Water-Resources Investigations Report 88-4214, v, 116 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884214.","productDescription":"v, 116 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4214/report-thumb.jpg"},{"id":55208,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4214/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6892ba","contributors":{"authors":[{"text":"Burns, A.W.","contributorId":65498,"corporation":false,"usgs":true,"family":"Burns","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":196344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28156,"text":"wri854288 - 1989 - Hydrogeology of the southwestern part of the town of Hempstead, Nassau County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri854288","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":"85-4288","title":"Hydrogeology of the southwestern part of the town of Hempstead, Nassau County, New York","docAbstract":"The groundwater resources of the southwestern part of the Town of Hempstead in Nassau County, NY were investigated in 1984. The area studied encompasses 85 sq mi, or 68% of the town 's 125-sq mi area. The groundwater reservoir underlying the area consists of unconsolidated gravel, sand, silt, and clay of Holocene, Pleistocene, and Late Cretaceous age that have been divided into eight geologic units. The maximum total thickness of the unconsolidated deposits is about 1,500 ft. Precipitation is the sole source of groundwater recharge in the area. The average annual precipitation, as recorded at Valley Stream during 1927-83, was 42.62 in. The water table altitude in the 1980 's has recovered and equalled or exceeded that before the regional drought of 1962-66. The potentiometric surfaces in the Magothy and Lloyd aquifers are still somewhat below those before the drought but are recovering throughout most of the area. The report presents 10 maps showing the surface altitude of the geologic units as well as the potentiometric altitudes of the three major aquifers. Also included are six geologic sections, four hydrographs, and several graphs presenting the data that was collected. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nCopies may be purchased from Books and Open-File Reports Section,","doi":"10.3133/wri854288","usgsCitation":"Krulikas, R.K., 1989, Hydrogeology of the southwestern part of the town of Hempstead, Nassau County, New York (Revision): U.S. Geological Survey Water-Resources Investigations Report 85-4288, iv, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854288.","productDescription":"iv, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4288/report-thumb.jpg"},{"id":56986,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4288/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Revision","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614b56","contributors":{"authors":[{"text":"Krulikas, Richard K.","contributorId":36910,"corporation":false,"usgs":true,"family":"Krulikas","given":"Richard","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":199311,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38531,"text":"pp1370A - 1989 - Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste - Basis of characterization and evaluation","interactions":[{"subject":{"id":12310,"text":"ofr84738 - 1985 - Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste; basis of characterization and evaluation","indexId":"ofr84738","publicationYear":"1985","noYear":false,"title":"Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste; basis of characterization and evaluation"},"predicate":"SUPERSEDED_BY","object":{"id":38531,"text":"pp1370A - 1989 - Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste - Basis of characterization and evaluation","indexId":"pp1370A","publicationYear":"1989","noYear":false,"chapter":"A","title":"Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste - Basis of characterization and evaluation"},"id":1}],"lastModifiedDate":"2017-08-31T15:48:37","indexId":"pp1370A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1370","chapter":"A","title":"Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste - Basis of characterization and evaluation","docAbstract":"<p>The geologic and hydrologic factors in selected regions of the Basin and Range province were examined to identify prospective areas for further study that may provide isolation of high-level radioactive waste from the accessible environment. The six regions selected for study were characterized with respect to the following guidelines: (1) Potential repository media; (2) Quaternary tectonic conditions; (3) climatic change and geomorphic processes; (4) ground-water conditions; (5) ground-water quality; and (6) mineral and energy resources.</p><p>The repository medium will function as the first natural barrier to radionuclide travel by virtue of associated slow ground-water velocity. The principal rock types considered as host media include granitic, intermediate, and mafic intrusive rocks; argillaceous rocks; salt and anhydrite; volcanic mudflow (laharic) breccias; some intrusive rhyolitic plugs and stocks; partially zeolitized tuff; and metamorphic rocks. In the unsaturated zone, the permeability and hydrologic properties of the rocks and the hydrologic setting are more important than the rock type. Media ideally should be permeable to provide drainage and should have a minimal water flux</p><p>The ground-water flow path from a repository to the accessible environment needs to present major barriers to the transport of radionuclides. Factors considered in evaluating the ground-water conditions include ground-water traveltimes and quality, confining beds, and earth materials favorable for retardation of radionuclides. </p><p>Ground-water velocities in the regions were calculated from estimated hydraulic properties of the rocks and gradients. Because site-specific data on hydraulic properties are not available, data from the literature were assembled and synthesized to obtain values for use in estimating ground-water velocities. Hydraulic conductivities for many rock types having granular and fracture permeability follow a log-normal distribution. Porosity for granular and very weathered crystalline rock tends to be normally distributed; porosity of fractured crystalline rock probably follows a log-normal distribution.</p><p>The tectonic setting needs to prevent an increase in radionuclides to the accessible environment. Data on historic seismicity and heat flow, Quaternary faults, volcanism, and uplift were used to assess the tectonic conditions. Long-term late Cenozoic rates of vertical crustal movement in the Basin and Range province range from less than 2 meters per 104 years to greater than 20 meters per 104 years. Shortterm rates of vertical movement may be more than an order of magnitude greater, based on geodetic leveling. Changes in tectonic and climatic processes may potentially cause changes in hydrologic conditions and geomorphology that could affect the integrity of a deep, mined repository either adversely or beneficially.</p><p>The transition from a full-glacial climate to the current interglacial condition has occurred within the past 15,000 years. Reconstructions of the last full-glacial climate indicate that, at that time, there was greater water availability for runoff and vegetation growth than there is now. Based on the increased water availability and depending on seasonal distribution of precipitation, on soil characteristics, on topography, and on other characteristics, ground-water recharge during the full-glacial climate is estimated to have been possibly 2 to 10 or more times the modern rate. During the full-glacial climate, more than 100 lakes occupied closed basins in the province. Any increase in ground-water recharge and refilling of Pleistocene lakes will tend to decrease the distance of ground-water flow and its time of travel. The unsaturated zone this zone is considered a potential host medium where the thickness is greater than 150 m will be decreased by these changes. In contrast, incision of streams and other geomorphic, tectonic, or climatically induced changes that lower the ground-water discharge level will tend to increase the thickness of the unsaturated zone. Aggradation in basinal troughs may either decrease or increase the thickness of the unsaturated zone. Aggradation in basins that causes the ground-water discharge level to rise will tend to decrease the thickness of unsaturated zone in the adjacent uplands; aggradation in basins where the ground-water discharge level remains the same or is lowered will increase the unsaturated thickness of basin fill.</p><p>Records show that, throughout late Cenozoic time in the Basin and Range province, continued vertical crustal movements have tended to maintain mountain ranges and closed basins, whereas aggradation of the basins and erosion of the mountain ranges have tended to decrease the topographic relief. Maximum rates of denudation for small basins in areas climatically similar to the Basin and Range province are about 2 meters per 104 years. For sites unaffected by stream incision and scarp retreat, a conservative estimate of erosion affecting long-term changes in depth of burial would appear to be 2 meters per 104 years, or, equal to the long-term rate of vertical crustal movement where greater than 2 meters per 104 years. The response of the ground-water conditions to climatic and geomorphically induced boundary conditions is significant from the points of: (1) The potential maximum change in the ground-water flow system; (2) the time of response of the ground-water system; and (3) the present state of the ground-water system as a result of past changes. Effects of longterm climatic and tectonic changes on hydrologic and geomorphic conditions differ from area to area, and rates of change of geomorphic and hydrologic conditions may vary significantly. Therefore, sitespecific studies need to be made to assess the long-term integrity of deep, mined repositories. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp1370A","collaboration":"Prepared in cooperation with the States of Arizona, California, Idaho, Nevada, New Mexico, Texas, and Utah","usgsCitation":"Bedinger, M.S., Sargent, K.A., Langer, W.H., Sherman, F.B., Reed, J., and Brady, B.T., 1989, Studies of geology and hydrology in the Basin and Range Province, Southwestern United States, for isolation of high-level radioactive waste - Basis of characterization and evaluation: U.S. Geological Survey Professional Paper 1370, Report: vi, 41 p.; Plate: 34.00 in. x 32.00 in., https://doi.org/10.3133/pp1370A.","productDescription":"Report: vi, 41 p.; Plate: 34.00 in. x 32.00 in.","startPage":"A1","endPage":"A41","numberOfPages":"48","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":104611,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4821.htm","linkFileType":{"id":5,"text":"html"},"description":"4821"},{"id":120236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1370a/report-thumb.jpg"},{"id":65293,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1370a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65294,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1370a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona, California, Idaho, Nevada, New Mexico, Texas, Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a24e","contributors":{"authors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":220008,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sargent, K. A.","contributorId":58630,"corporation":false,"usgs":true,"family":"Sargent","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":220007,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langer, William H. blanger@usgs.gov","contributorId":1241,"corporation":false,"usgs":true,"family":"Langer","given":"William","email":"blanger@usgs.gov","middleInitial":"H.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":false,"id":220006,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sherman, Frank B.","contributorId":16495,"corporation":false,"usgs":true,"family":"Sherman","given":"Frank","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":220004,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Reed, J.E.","contributorId":41801,"corporation":false,"usgs":true,"family":"Reed","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":220005,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brady, B. T.","contributorId":93047,"corporation":false,"usgs":true,"family":"Brady","given":"B.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":220009,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":38446,"text":"pp1405D - 1989 - Geochemistry of the Cambrian-Ordovician aquifer system in the northern Midwest, United States: D in <i>Regional aquifer-system analysis</i>","interactions":[],"lastModifiedDate":"2018-04-02T10:36:50","indexId":"pp1405D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1405","chapter":"D","title":"Geochemistry of the Cambrian-Ordovician aquifer system in the northern Midwest, United States: D in <i>Regional aquifer-system analysis</i>","docAbstract":"<p>Distributions of solutes in aquifers of Cambrian and Ordovician age were studied in Minnesota, Wisconsin, Iowa, Illinois, northwestern Indiana, and northern Missouri to determine the sources of solutes and the probable chemical mechanisms that control regional variations in water quality. This work is part of the Northern Midwest Regional Aquifer-System Analysis project, whose objective is to describe and model the regional hydrogeology of the Cambrian- Ordovician aquifer system in the study region. The data base used included more than 3,000 ground-water-quality analyses from all major aquifers, but especially from the St. Peter, Jordan, and Mount Simon Sandstones and their equivalents. Regional variations in the water chemistry of glacial drift and other sedimentary units that overlie the Cambrian-Ordovician aquifer system in recharge areas in Minnesota, Iowa, Wisconsin, and Illinois were also studied, but to a lesser degree.</p>\n<p>The most important chemical variation in the aquifer is the change in water type from calcium-sodium-sulfate-bicarbonate water to sodium-calcium-sulfate-bicarbonate and sodium-chloride waters along the longest regional flow path from northwestern Iowa to the Illinois basin. Sodium predominance downgradient from the recharge area is probably related to mechanisms of ion exchange and shalemembrane filtration near the Illinois and Forest City basins.</p>\n<p>The most striking aspect of the distribution of dissolved solids and carbon isotopic content of bicarbonate is the increase in concentration and isotopic enrichment from southwestern Wisconsin, southern Minnesota, and northwestern Illinois south toward Missouri. This trend is perpendicular to the present hydraulic gradient that trends from northwestern Iowa southeastward to the Illinois basin. The distribution of dissolved solids defines a \"plume\" of dilute water having a dissolved-solids concentration of about 500 milligrams per liter, compared with surrounding concentrations more than twice as large. Distribution of the isotopic content of oxygen (&lt;518O) and hydrogen (5D) in water closely parallels that of dissolved solids and shows covariance similar to modern meteoric water. The isotopic contents are more depleted (lighter) toward the south, perpendicular to the direction of current hydraulic gradients. The degree of depletion, compared with the isotopic content of modern recharge water, indicates that the plume and a significant fraction of the ground water in Iowa, northern Missouri, and possibly central Illinois may have originated as recharge during Pleistocene time.</p>\n<p>Distributions of dissolved trace constituents in the aquifers probably are related to the proximity to mineralogic sources as well as chemical and hydraulic mechanisms. For example, concentrations of some constituents, such as cadmium and arsenic, are largest in the vicinity of the Dakota Formation in northwestern Iowa. Other constituents, such as beryllium and vanadium, have larger concentrations near the edge of the Forest City basin in southwestern Iowa and northwestern Missouri. Strontium and fluoride concentrations generally increase from north to south, which suggests the input of these trace constituents during the recharge events. However, concentrations of bromide, radium-226, and lithium show distribution patterns similar to the \"plume\" defined by dissolved solids and isotopes of water, suggesting dilution of concentrations of trace constituents by Pleistocene recharge. Concentrations of other constituents are partly controlled by aquifer temperature, such as silica in south-central Iowa, and solubility controls, such as barium in northeastern Illinois. Additional information on the chemical and mineralogical composition of the aquifer matrix and the isotopically lightest ground water is needed to evaluate the hypothesis of Pleistocene mixing before more quantitative studies can be done to evaluate the different proposed mechanisms that have controlled and modified the water chemistry over time. This study, however, indicates that the ground water in the region is thousands of years old. The study also indicates that the major chemical trends in the aquifers probably are related as much to paleohydrogeologic flow systems during Pleistocene time as to the present flow system, which may postdate the retreat of the last ice sheet about 12,000 years ago.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Regional aquifer-system analysis","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp1405D","usgsCitation":"Siegel, D.I., 1989, Geochemistry of the Cambrian-Ordovician aquifer system in the northern Midwest, United States: D in <i>Regional aquifer-system analysis</i>: U.S. Geological Survey Professional Paper 1405, vii, 76 p., https://doi.org/10.3133/pp1405D.","productDescription":"vii, 76 p.","numberOfPages":"87","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":64921,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1405d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1405d/report-thumb.jpg"}],"country":"United States","state":"Iowa, Indiana, Illinois, Michigan, Minnesota, Missouri, Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.044921875,\n              45.9511496866914\n            ],\n            [\n              -88.330078125,\n              46.042735653846506\n            ],\n            [\n              -90.3955078125,\n              46.31658418182218\n            ],\n            [\n              -92.59277343749999,\n              46.34692761055676\n            ],\n            [\n              -93.603515625,\n              46.13417004624326\n            ],\n            [\n              -94.7021484375,\n              45.24395342262324\n            ],\n            [\n              -95.8447265625,\n              43.644025847699496\n            ],\n            [\n              -96.6796875,\n              42.553080288955826\n            ],\n            [\n              -96.7236328125,\n              41.83682786072714\n            ],\n            [\n              -96.328125,\n              40.78054143186031\n            ],\n            [\n              -95.2734375,\n              39.16414104768742\n            ],\n            [\n              -94.8779296875,\n              38.37611542403604\n            ],\n            [\n              -93.8232421875,\n              37.996162679728116\n            ],\n            [\n              -90.7470703125,\n              37.54457732085582\n            ],\n            [\n              -89.69238281249999,\n              37.71859032558816\n            ],\n            [\n              -88.1982421875,\n              38.03078569382294\n            ],\n            [\n              -87.01171875,\n              38.685509760012\n            ],\n            [\n              -85.78125,\n              39.16414104768742\n            ],\n            [\n              -86.4404296875,\n              42.45588764197166\n            ],\n            [\n              -86.8798828125,\n              43.29320031385282\n            ],\n            [\n              -87.099609375,\n              44.15068115978091\n            ],\n            [\n              -86.044921875,\n              45.9511496866914\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa604","contributors":{"authors":[{"text":"Siegel, D. I.","contributorId":77562,"corporation":false,"usgs":true,"family":"Siegel","given":"D.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":219837,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12684,"text":"ofr88711 - 1989 - Water supply and demand in Sedgwick County, Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr88711","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":"88-711","title":"Water supply and demand in Sedgwick County, Kansas","docAbstract":"Water supplies in Sedgwick County, Kansas, are derived from surface--and groundwater resources. During 1985, public supply, irrigation, and self-supplied industry required 38% of the 56 ,500 acre-ft of appropriated surface water and 57% of the 187 ,800 acre-ft of appropriated groundwater. If the historic (1920-80) annual population growth rate (2.8%) continues, the 126,100 acre ft of water appropriated for public-water supplies should meet demand until 2015. The quantity of potentially available water supplies was estimated by summing those resources having less than 1.00 mg/L dissolved solids. Surface water resources that meet this criterion are the Little Arkansas and Ninnescah Rivers and Cheney Reservoir. Subtracting legislated minimum streamflows for the rivers from their mean annual streamflow volumes leaves 532,000 acre-ft, which combined with the annual sustained yield of Cheney Reservoir (40,000 acre-ft) provides an estimated 572,000 acre-ft of surface water annually. Groundwater that meets the criterion was estimated by summing the annual precipitation recharge available to unconsolidated deposits in the county (78,400 acre-ft) and in the Harvey County part of the Wichita well field (13,000 acre-ft). Although more groundwater is available, withdrawals exceeding annual precipitation recharge would cause water level declines. Because less than 4% of the potentially available surface water was used for supplies in 1985 and because about 120% of the groundwater recharge was used, surface water resources have a greater potential for meeting future water use demands. (USGS)","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/ofr88711","usgsCitation":"Bevans, H.E., 1989, Water supply and demand in Sedgwick County, Kansas: U.S. Geological Survey Open-File Report 88-711, 2 p. 1 map ;28 cm., https://doi.org/10.3133/ofr88711.","productDescription":"2 p. 1 map ;28 cm.","costCenters":[],"links":[{"id":972,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://ks.water.usgs.gov/pubs/fact-sheets/ofr.88-711.bevans.html","linkFileType":{"id":5,"text":"html"}},{"id":145718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0711/report-thumb.jpg"},{"id":41094,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0711/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e33df","contributors":{"authors":[{"text":"Bevans, Hugh E.","contributorId":11589,"corporation":false,"usgs":true,"family":"Bevans","given":"Hugh","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":166539,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22497,"text":"ofr8944 - 1989 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","interactions":[{"subject":{"id":12701,"text":"ofr87469 - 1987 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr87469","publicationYear":"1987","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"predicate":"SUPERSEDED_BY","object":{"id":22497,"text":"ofr8944 - 1989 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr8944","publicationYear":"1989","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"id":1},{"subject":{"id":22497,"text":"ofr8944 - 1989 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr8944","publicationYear":"1989","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"predicate":"SUPERSEDED_BY","object":{"id":18169,"text":"ofr90141 - 1990 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr90141","publicationYear":"1990","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"id":2}],"supersededBy":{"id":18169,"text":"ofr90141 - 1990 - Directory of member organizations of the National Water Data Exchange (NAWDEX)","indexId":"ofr90141","publicationYear":"1990","noYear":false,"title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)"},"lastModifiedDate":"2012-02-02T00:08:07","indexId":"ofr8944","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":"89-44","title":"Directory of member organizations of the National Water Data Exchange (NAWDEX)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8944","issn":"0094-9140","usgsCitation":"Blackwell, C.D., 1989, Directory of member organizations of the National Water Data Exchange (NAWDEX): U.S. Geological Survey Open-File Report 89-44, x, 81 p. ;28 cm., https://doi.org/10.3133/ofr8944.","productDescription":"x, 81 p. ;28 cm.","costCenters":[],"links":[{"id":155605,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ab4e","contributors":{"authors":[{"text":"Blackwell, Cassandra D.","contributorId":25562,"corporation":false,"usgs":true,"family":"Blackwell","given":"Cassandra","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":188355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12725,"text":"ofr89411 - 1989 - Senegal River Valley Ground-Water Monitoring Project; summary report on piezometer evaluation, February-March 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:06:39","indexId":"ofr89411","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":"89-411","title":"Senegal River Valley Ground-Water Monitoring Project; summary report on piezometer evaluation, February-March 1989","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr89411","usgsCitation":"Bolke, E., and Stephens, J., 1989, Senegal River Valley Ground-Water Monitoring Project; summary report on piezometer evaluation, February-March 1989: U.S. Geological Survey Open-File Report 89-411, iii, 11 p. :map ;28 cm., https://doi.org/10.3133/ofr89411.","productDescription":"iii, 11 p. :map ;28 cm.","costCenters":[],"links":[{"id":145745,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0411/report-thumb.jpg"},{"id":41135,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0411/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a1d7","contributors":{"authors":[{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":166604,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, J.C.","contributorId":74010,"corporation":false,"usgs":true,"family":"Stephens","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":166605,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16079,"text":"ofr86140 - 1989 - Water quality data for precipitation and storm runoff in Pennypack Creek Basin, Philadelphia, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-09T08:47:13","indexId":"ofr86140","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":"86-140","title":"Water quality data for precipitation and storm runoff in Pennypack Creek Basin, Philadelphia, Pennsylvania","docAbstract":"This report presents data on the chemistry of precipitation and storm runoff that were collected during 29 storms from July 1979 through November 1980, in an urban environment in the Pennypack Creek basin, Philadelphia, Pennsylvania. Daily mean and instantaneous stream discharge data were collected at two U.S. Geological Survey gaging stations. Water-quality data collected from these sites and from one storm-sewer sampling site included nutrients, chemical and biochemical oxygen demands, solids, metals, major anions, other constituents, and pH. Instantaneous loads of selected constituents were computed.\r\n\r\n      Chemical oxygen demand, biochemical oxygen demand, sulfate, alkalinity, chloride, and dissolved solids generally were low in precipitation and runoff. During the November 5, 1980 storm at Pine Road, dissolved nitrate concentrations equaled or exceeded 10 milligrams per liter in 17 percent of the samples analyzed and dissolved ammonia nitrogen concentrations exceeded 2.5 milligrams per liter. Generally, a comparison of median concentration of copper, lead, or zinc in precipitation and runoff at the Tustin Street storm-sewer site showed that median concentrations in precipitation were greater than those in runoff.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr86140","usgsCitation":"Speight, D., 1989, Water quality data for precipitation and storm runoff in Pennypack Creek Basin, Philadelphia, Pennsylvania: U.S. Geological Survey Open-File Report 86-140, iv, 34 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86140.","productDescription":"iv, 34 p. :ill. ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":45011,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0140/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0140/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699657","contributors":{"authors":[{"text":"Speight, D.W.","contributorId":71563,"corporation":false,"usgs":true,"family":"Speight","given":"D.W.","affiliations":[],"preferred":false,"id":172202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20750,"text":"ofr88470 - 1989 - Hydrologic data for Indian Creek basin, Fayette and Westmoreland counties, Pennsylvania, 1985-87","interactions":[],"lastModifiedDate":"2017-06-13T15:04:01","indexId":"ofr88470","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":"88-470","title":"Hydrologic data for Indian Creek basin, Fayette and Westmoreland counties, Pennsylvania, 1985-87","docAbstract":"<p>Hydrologic data were collected in the Indian Creek basin, Fayette and Westmoreland Counties, Pennsylvania. Since the early 1900's, coal in the basin has been extensively mined by both underground and surface-mining techniques. Data-collection sites were located in mined and unmined areas of the basin. The hydrologic data presented are from 5 continuous-record surfacewater data-collection sites, 1 ground-water well, 23 partial-record surfacewater sites, and 2 continuous-record precipitation gages. Data from the five continuous-record surface-water sites include discharge, specific conductance, temperature, pH, and suspended-sediment concentration. Results of laboratory analyses are reported. Benthic macroinvertebrates collected at 23 sites are listed. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88470","usgsCitation":"Sams, J.I., and Witt, E., 1989, Hydrologic data for Indian Creek basin, Fayette and Westmoreland counties, Pennsylvania, 1985-87: U.S. Geological Survey Open-File Report 88-470, vi, 124 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88470.","productDescription":"vi, 124 p. :ill. ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":50306,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0470/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152393,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0470/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ed62","contributors":{"authors":[{"text":"Sams, J. I. III","contributorId":50548,"corporation":false,"usgs":true,"family":"Sams","given":"J.","suffix":"III","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":183181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witt, E. C. III","contributorId":105746,"corporation":false,"usgs":true,"family":"Witt","given":"E. C.","suffix":"III","affiliations":[],"preferred":false,"id":183182,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56273,"text":"wdrWA881 - 1989 - Water resources data, Washington, water year 1988","interactions":[],"lastModifiedDate":"2023-03-10T21:17:13.291619","indexId":"wdrWA881","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":"WA-88-1","title":"Water resources data, Washington, water year 1988","docAbstract":"<p>Water-resources data for the 1988 water year for Washington consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels of wells. This report contains discharge records for 202 gaging stations; stage only records for 6 gaging stations; stage and (or) contents for 38 lakes and reservoirs; water quality for 28 streamflow-gaging stations, and 9 ungaged streamsites; water levels for 77 observation wells; and water quality for 1 observation well. Also included are data for 13 crest-stage partial-record stations and 112 partial-record or miscellaneous streamflow stations. Locations of these sites are shown on figures 4a, 4b, 5, 6a, 6b, 35a, and 35b. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Washington.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA881","usgsCitation":"Miles, M., Wiggins, W., Ruppert, G., Blazs, R., Reed, L., and Hubbard, L., 1989, Water resources data, Washington, water year 1988: U.S. Geological Survey Water Data Report WA-88-1, xvi, 471 p., https://doi.org/10.3133/wdrWA881.","productDescription":"xvi, 471 p.","costCenters":[],"links":[{"id":174638,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1988/wa-88-1/report-thumb.jpg"},{"id":413974,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1988/wa-88-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":14415,"text":"ofr89468 - 1989 - An assessment of the ground-water resources of Kaho'olawe, Hawaii using transient electromagnetic and Schlumberger soundings","interactions":[],"lastModifiedDate":"2012-02-02T00:07:03","indexId":"ofr89468","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":"89-468","title":"An assessment of the ground-water resources of Kaho'olawe, Hawaii using transient electromagnetic and Schlumberger soundings","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr89468","usgsCitation":"Kauahikaua, J.P., 1989, An assessment of the ground-water resources of Kaho'olawe, Hawaii using transient electromagnetic and Schlumberger soundings: U.S. Geological Survey Open-File Report 89-468, 51 p. ill. ;28 cm., https://doi.org/10.3133/ofr89468.","productDescription":"51 p. ill. ;28 cm.","costCenters":[],"links":[{"id":147702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0468/report-thumb.jpg"},{"id":43095,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0468/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684d33","contributors":{"authors":[{"text":"Kauahikaua, James P. 0000-0003-3777-503X jimk@usgs.gov","orcid":"https://orcid.org/0000-0003-3777-503X","contributorId":2146,"corporation":false,"usgs":true,"family":"Kauahikaua","given":"James","email":"jimk@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":169419,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47478,"text":"b1875C - 1989 - North American Datum of 1983, map data conversion tables; Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:47","indexId":"b1875C","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":"1875","chapter":"C","title":"North American Datum of 1983, map data conversion tables; Alaska","language":"ENGLISH","doi":"10.3133/b1875C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1989, North American Datum of 1983, map data conversion tables; Alaska: U.S. Geological Survey Bulletin 1875, p. C1-C355, https://doi.org/10.3133/b1875C.","productDescription":"p. C1-C355","costCenters":[],"links":[{"id":94032,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1875c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1875c/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a857c","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":531746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38437,"text":"pp1404D - 1989 - The occurrence and geochemistry of salty ground water in the northern Atlantic Coastal Plain","interactions":[{"subject":{"id":10298,"text":"ofr8171 - 1980 - Preliminary delineation of salty ground water in the northern Atlantic Coastal Plain","indexId":"ofr8171","publicationYear":"1980","noYear":false,"title":"Preliminary delineation of salty ground water in the northern Atlantic Coastal Plain"},"predicate":"SUPERSEDED_BY","object":{"id":38437,"text":"pp1404D - 1989 - The occurrence and geochemistry of salty ground water in the northern Atlantic Coastal Plain","indexId":"pp1404D","publicationYear":"1989","noYear":false,"chapter":"D","title":"The occurrence and geochemistry of salty ground water in the northern Atlantic Coastal Plain"},"id":1}],"lastModifiedDate":"2025-04-17T19:20:32.652041","indexId":"pp1404D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1404","chapter":"D","title":"The occurrence and geochemistry of salty ground water in the northern Atlantic Coastal Plain","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1404D","usgsCitation":"Meisler, H., 1989, The occurrence and geochemistry of salty ground water in the northern Atlantic Coastal Plain: U.S. Geological Survey Professional Paper 1404, Report: 51 p.; 6 Plates: 23.50 x 13.00 inches or smaller, https://doi.org/10.3133/pp1404D.","productDescription":"Report: 51 p.; 6 Plates: 23.50 x 13.00 inches or smaller","costCenters":[],"links":[{"id":64874,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404d/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64873,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404d/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64872,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404d/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64871,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64870,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119286,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1404d/report-thumb.jpg"},{"id":484734,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4844.htm","linkFileType":{"id":5,"text":"html"}},{"id":64876,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1404d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64875,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404d/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Atlantic Coastal Plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -79.1667,\n              40.8333\n            ],\n            [\n              -79.1667,\n              33.8333\n            ],\n            [\n              -72.6667,\n              33.8333\n            ],\n            [\n              -72.6667,\n              40.8333\n            ],\n            [\n              -79.1667,\n              40.8333\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627c1e","contributors":{"authors":[{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":219821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28207,"text":"wri884157 - 1989 - Continuous seismic-reflection survey of the Great Salt Lake, Utah– East of Antelope and Fremont Islands","interactions":[],"lastModifiedDate":"2022-02-14T21:51:43.898039","indexId":"wri884157","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":"88-4157","title":"Continuous seismic-reflection survey of the Great Salt Lake, Utah– East of Antelope and Fremont Islands","docAbstract":"<p>A continuous seismic-reflection survey of the Great Salt Lake, Utah, was conducted east of Fremont and Antelope Islands in 1984 by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources and produced data along approximately 80 miles of seismic lines. The survey was conducted to determine depth to consolidated rock, and definition and continuity of overlying basin fill under the lake. Interpretation of the data indicates the presence of faulted rock dipping away from Fremont and Antelope Islands. A north-south-trending consolidated-rock ridge is identified 200 ft below lake bottom, 275 miles east of Fremont Island. Shallow rock is also inferred 380 ft below lake bottom, near Hooper Hot Springs, and 520 ft below lake bottom approximately 4 miles east of the south end of Antelope Island. Interpretation of reflections from overlying basin fill indicates fine-grained, thinly-bedded deposits that become coarser with depth. Strong reflectors in the basin fill can be correlated with water-bearing strata penetrated by wells near the north end of Antelope Island and along the east shore of the lake. Many continuous, high-amplitude reflections can be identified in data from basin fill and may represent sedimentary sections or aquifer boundaries but cannot be defined because of a lack of subsurface control in the area.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884157","usgsCitation":"Lambert, P., and West, J.C., 1989, Continuous seismic-reflection survey of the Great Salt Lake, Utah– East of Antelope and Fremont Islands: U.S. Geological Survey Water-Resources Investigations Report 88-4157, Report: iv, 17 p.; 1 Plate: 36.74 × 25.62 inches, https://doi.org/10.3133/wri884157.","productDescription":"Report: iv, 17 p.; 1 Plate: 36.74 × 25.62 inches","costCenters":[],"links":[{"id":395949,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47065.htm"},{"id":57044,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4157/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57043,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4157/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4157/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.35992431640625,\n              40.83043687764923\n            ],\n            [\n              -111.9012451171875,\n              40.83043687764923\n            ],\n            [\n              -111.9012451171875,\n              41.20758898181025\n            ],\n            [\n              -112.35992431640625,\n              41.20758898181025\n            ],\n            [\n              -112.35992431640625,\n              40.83043687764923\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689c9d","contributors":{"authors":[{"text":"Lambert, P. M.","contributorId":74380,"corporation":false,"usgs":true,"family":"Lambert","given":"P. M.","affiliations":[],"preferred":false,"id":199395,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"West, J. C.","contributorId":63017,"corporation":false,"usgs":true,"family":"West","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":199394,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38435,"text":"pp1404B - 1989 - Hydrogeologic framework of the New Jersey Coastal Plain","interactions":[{"subject":{"id":16692,"text":"ofr84730 - 1984 - Hydrogeologic framework of the New Jersey coastal plain","indexId":"ofr84730","publicationYear":"1984","noYear":false,"title":"Hydrogeologic framework of the New Jersey coastal plain"},"predicate":"SUPERSEDED_BY","object":{"id":38435,"text":"pp1404B - 1989 - Hydrogeologic framework of the New Jersey Coastal Plain","indexId":"pp1404B","publicationYear":"1989","noYear":false,"chapter":"B","title":"Hydrogeologic framework of the New Jersey Coastal Plain"},"id":1}],"lastModifiedDate":"2025-04-18T13:43:49.49535","indexId":"pp1404B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1404","chapter":"B","title":"Hydrogeologic framework of the New Jersey Coastal Plain","docAbstract":"This report presents the results of a water-resources, oriented subsurface mapping program within the Coastal Plain of New Jersey.  The occurrence and configuration of 15 regional  hydrogeologic units have been defined, primarily on the basis of an interpretation of borehole geophysical data.  The nine aquifers and six confining beds are composed of unconsolidated clay, silt, sand, and gravel and range in age from Cretaceous to Quaternary.\r\n\r\nElectric and gamma-ray logs from more than 1,000 Coastal Plain wells were examined.  Of these, interpretive data for 302 sites were selected, on the basis of logged depth, quality of data, and data distribution, to prepare structure contour and thickness maps for each aquifer and a thickness map for each confining bed.  These maps, together with 14 hydrogeologic sections, show the geometry, lateral extent, and vertical and horizontal relationships among the 15 hydrogeologic units.  \r\n\r\nThe hydrogeologic maps and sections show that distinct lower, middle, and upper aquifers are present within the Potomac, Raritan-Magothy aquifer system near the Delaware River from Burlington County to Salem County.  Although the lower aquifer is recognized only in this area, the middle aquifer extends into the northeastern Coastal Plain of New Jersey, where it is stratigraphically equivalent to the Farrington aquifer.  The upper aquifer extends throughout most of the New Jersey Coastal Plain and is stratigraphically equivalent to the Old Bridge aquifer in the northeastern Coastal Plain.  The overlying Merchantville-Woodbury confining bed is the most regionally extensive confining bed within the New Jersey Coastal Plain.  Its thickness ranges from less than 100 feet near the outcrop to more than 450 feet along the coast.  The Englishtown aquifer system acts as a single aquifer throughout most of its subsurface extent, but it contains two water-bearing sands in pars of Monmouth and Ocean Counties.  The overlying Marshalltown-Wenonah confining bed is a thin, leaky unit ranging in thickness from approximately 20 to 80 feet.  The Wenonah-Mount Laurel aquifer is identified in the subsurface throughout the New Jersey Coastal Plain southeast of its outcrop  area.  \r\n\r\nSediments that overlie the Wenonah-Mount Lauren aquifer and that are subjacent to the major aquifers within the Kirkwood Formation and the Cohansey Sand are described hydrologically as a composite confining bed.  These include the Navesink Formation, Red Bank Sand, Tinton Sand, Hornerstown Sand, Vincentown Formation, Manasquan Formation, Shark River Formation, and Piney Point Formation and the basal clay of the Kirkwood Formation.. The Vincentown Formation functions as n aquifer within 3 to 10 miles downdip of its outcrop area.  In areas farther downdip the Vincentown Formation functions as a confining bed.  The Piney Point aquifer is laterally persistent from the southern New Jersey Coastal Plain northward into parts of Burlington and Ocean Counties.  The Atlantic City 800-foot sand of the Kirkwood Formation can be recognized in the subsurface along coastal areas of Cape May, Atlantic, and southern Ocean Counties, but inland only as far west as the extent of the overlying confining bed.  In areas west of the extent of the overlying confining bed, the Kirkwood Formation is in hydraulic connection with the overlying Cohansey Sand and younger surficial deposits and functions as an unconfined aquifer.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Regional aquifer-system analysis - Northern Atlantic coastal plain (Professional Paper 1404)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1404B","usgsCitation":"Zapecza, O.S., 1989, Hydrogeologic framework of the New Jersey Coastal Plain: U.S. Geological Survey Professional Paper 1404, Report: vi, 49 p.; 24 plates: 20.25 x 27.68 inches or smaller, https://doi.org/10.3133/pp1404B.","productDescription":"Report: vi, 49 p.; 24 plates: 20.25 x 27.68 inches or smaller","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":104627,"rank":27,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4842.htm","linkFileType":{"id":5,"text":"html"},"description":"4842"},{"id":64867,"rank":25,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-23.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64866,"rank":24,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-22.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64861,"rank":19,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64860,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64859,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64858,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64857,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64856,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64855,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64854,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64853,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64852,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64851,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64847,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64846,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64845,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64869,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1404b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124942,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1404b/report-thumb.jpg"},{"id":64850,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64849,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64848,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64862,"rank":20,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64863,"rank":21,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64864,"rank":22,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-20.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64865,"rank":23,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-21.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":64868,"rank":26,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1404b/plate-24.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"New Jersey Coastal Plain","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.6167,\n              40.5678\n            ],\n            [\n              -75.6167,\n              38.8869\n            ],\n            [\n              -74,\n              38.8869\n            ],\n            [\n              -74,\n              40.5678\n            ],\n            [\n              -75.6167,\n              40.5678\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628dd7","contributors":{"authors":[{"text":"Zapecza, Otto S. ozapecza@usgs.gov","contributorId":3687,"corporation":false,"usgs":true,"family":"Zapecza","given":"Otto","email":"ozapecza@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":219818,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38422,"text":"pp1492 - 1989 - Debris flows from tributaries of the Colorado River, Grand Canyon National Park, Arizona","interactions":[{"subject":{"id":16460,"text":"ofr87118 - 1987 - Debris flows from tributaries of the Colorado River, Grand Canyon National Park, Arizona","indexId":"ofr87118","publicationYear":"1987","noYear":false,"title":"Debris flows from tributaries of the Colorado River, Grand Canyon National Park, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":38422,"text":"pp1492 - 1989 - Debris flows from tributaries of the Colorado River, Grand Canyon National Park, Arizona","indexId":"pp1492","publicationYear":"1989","noYear":false,"title":"Debris flows from tributaries of the Colorado River, Grand Canyon National Park, Arizona"},"id":1}],"lastModifiedDate":"2012-02-02T00:09:53","indexId":"pp1492","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1492","title":"Debris flows from tributaries of the Colorado River, Grand Canyon National Park, Arizona","docAbstract":"A reconnaissance of 36 tributaries of the Colorado River indicates that debris flows are a major process by which sediment is transported to the Colorado River in Grand Canyon National Park. Debris flows are slurries of sediment and water that have a water content of less than about 40 percent by volume. Debris flows occur frequently in arid and semiarid regions. Slope failures commonly trigger debris flows, which can originate from any rock formation in the Grand Canyon. The largest and most frequent flows originate from the Permian Hermit Shale, the underlying Esplanade Sandstone of the Supai Group, and other formations of the Permian and Pennsylvanian Supai Group. Debris flows also occur in the Cambrian Muav Limestone and underlying Bright Angel Shale and the Quaternary basalts in the western Grand Canyon. \r\n\r\nDebris-flow frequency and magnitude were studied in detail in the Lava-Chuar Creek drainage at Colorado River mile 65.5; in the Monument Creek drainage at mile 93.5; and in the Crystal Creek drainage at mile 98.2. Debris flows have reached the Colorado River on an average of once every 20 to 30 years in the Lava-Chuar Creek drainage since about 1916. Two debris flows have reached the Colorado River in the last 25 years in Monument Creek. The Crystal Creek drainage has had an average of one debris flow reaching the Colorado River every 50 years, although the debris flow of 1966 has been the only flow that reached the Colorado River since 1900. Debris flows may actually reach the Colorado River more frequently in these drainages because evidence for all debris flows may not have been preserved in the channel-margin stratigraphy. \r\n\r\nDischarges were estimated for the peak flow of three debris flows that reached the Colorado River. The debris flow of 1966 in the Lava-Chuar Creek drainage had an estimated discharge of 4,000 cubic feet per second. The debris flow of 1984 in the Monument Creek drainage had a discharge estimated between 3,600 and 4,200 cubic feet per second. The debris flow of 1966 in the Crystal Creek drainage had a discharge estimated between 9,200 and 14,000 cubic feet per second. Determination of the effective cross-sectional area was a problem in all calculations involving superelevations on bends because areas near superelevation marks were 1.5 to 3.5 times larger than areas of upstream or downstream cross sections. \r\n\r\nDebris flows in the Grand Canyon generally are composed of 10 to 40 percent sand by weight and may represent a significant source of beach-building sand along the Colorado River. The particle-size distributions are very poorly sorted and the largest transported boulders were in the Crystal Creek drainage. The large boulders transported into the Colorado River by debris flows create or change hydraulic controls (rapids); these controls appear to be governed by the magnitude and frequency of tributary-flow events and the history of discharges on the Colorado River. Reworking of debris fans by the Colorado River creates debris bars that constrain the size of eddy systems and forms secondary rapids and riffles below tributary mouths.","language":"ENGLISH","doi":"10.3133/pp1492","usgsCitation":"Webb, R., Pringle, P.T., and Rink, G.R., 1989, Debris flows from tributaries of the Colorado River, Grand Canyon National Park, Arizona: U.S. Geological Survey Professional Paper 1492, 39 p., https://doi.org/10.3133/pp1492.","productDescription":"39 p.","costCenters":[],"links":[{"id":124324,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1492/report-thumb.jpg"},{"id":64815,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1492/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db6727dc","contributors":{"authors":[{"text":"Webb, Robert H. rhwebb@usgs.gov","contributorId":1573,"corporation":false,"usgs":false,"family":"Webb","given":"Robert H.","email":"rhwebb@usgs.gov","affiliations":[{"id":12625,"text":"School of Natural Resources and the Environment, University of Arizona, Tucson, AZ, 85721, USA","active":true,"usgs":false}],"preferred":false,"id":219792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pringle, Patrick T.","contributorId":105744,"corporation":false,"usgs":true,"family":"Pringle","given":"Patrick","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":219794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rink, Glenn R.","contributorId":8339,"corporation":false,"usgs":true,"family":"Rink","given":"Glenn","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":219793,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20759,"text":"ofr89658 - 1989 - Quality assessment program and results for the NAWQA surface water pilot studies","interactions":[],"lastModifiedDate":"2012-02-02T00:07:35","indexId":"ofr89658","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":"89-658","title":"Quality assessment program and results for the NAWQA surface water pilot studies","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89658","usgsCitation":"Sanzolone, R.F., and Ryder, J.L., 1989, Quality assessment program and results for the NAWQA surface water pilot studies: U.S. Geological Survey Open-File Report 89-658, 22 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89658.","productDescription":"22 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":152604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0658/report-thumb.jpg"},{"id":50314,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0658/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db6552f7","contributors":{"authors":[{"text":"Sanzolone, R. F.","contributorId":64199,"corporation":false,"usgs":true,"family":"Sanzolone","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":183198,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryder, J. L.","contributorId":30997,"corporation":false,"usgs":true,"family":"Ryder","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":183197,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38427,"text":"pp1442 - 1989 - Tectonically controlled fan delta and submarine fan sedimentation of late Miocene age, southern Temblor Range, California","interactions":[],"lastModifiedDate":"2017-04-25T15:06:07","indexId":"pp1442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1442","title":"Tectonically controlled fan delta and submarine fan sedimentation of late Miocene age, southern Temblor Range, California","docAbstract":"<p>The Santa Margarita Formation in the southern Temblor Range, composed of conglomerate and subordinate sandstone, evolved as a large complex of fan deltas and submarine fans in late Miocene time. An 80 to 90-m.y.-old granitic basement of the Salinian block and an accompanying 23.5-m.y.-old volcanic field now located in the northern Gabilan Range and the Pinnacles area, respectively, were the primary source terranes. In general, the fan deltas crop out along the west side of the southern Temblor Range, whereas the proximal parts of the submarine fans crop out along the east side of the range. The fan deltas consist of subaerial topset beds and low-angle basinward-dipping subaqueous foreset beds. Strata interpreted to be topset beds are composed largely of conglomerate with thick to very thick horizontal beds and matrix-supported clasts. Most of the thick to very thick conglomerate beds are internally massive and disorganized. Strata interpreted as foreset beds are composed of thick-bedded, large-scale, low-angle, cross-stratified conglomerate and sandstone units which commonly are internally massive. Abundant molluskan macrofossils such as <i>Ostrea</i> and <i>Pecten</i> are present in the subaqueous foreset beds; many have been displaced downslope from their original site of deposition. Conglomerate- and sandstone-filled submarine canyons, through which coarse-grained detritus was transported to the adjacent submarine fans, locally have cut into the foreset beds of the fan deltas. These submarine canyon deposits are generally better stratified than adjacent foreset-bed deposits, and they consist of thick horizontal beds, internally massive or normally graded, arranged in fining- and thinning-upward sequences. Isolated and composite conglomerate- and sandstone-filled channels, which crop out on the east flank of the southern Temblor Range, are interpreted as proximal submarine-fan channel deposits. These channel-form conglomerate and sandstone deposits are characterized by thick, horizontal beds which are internally massive or normally graded containing division T<i>a</i>, and locally T<i>b</i>, of the Bouma sequence. Sparse calcareous foraminifers collected from diatomaceous interbeds suggest that these fan channels were deposited in upper bathyal water depths. Subaerial and regenerated subaqueous debris flows probably formed the bulk of the Santa Margarita fan delta and submarine fan system. Santa Margarita debris flows ranged from the mudflow variety to the cataclysmic debris-avalanche variety.</p><p>The cogenetic Republic and Williams sandstones of local usage, located on the east side of the southern Temblor Range, are slightly older and finer grained than the Santa Margarita Formation. These units, containing well-graded sandstones, fining- and thinning-upward and coarsening- and thickening-upward sandstone sequences, thick-bedded tabular and channel-shaped sandstones, a mixture of shallow- and deep-water foraminifers, and a fan-shaped geometry in the subsurface, are interpreted as submarine fan deposits.</p><p>Sedimentation associated with the Santa Margarita Formation was intimately related to the growing southern Temblor Range anticlinorium and the right-laterally shifting Salinian block along the San Andreas fault. Examples of control exerted on Santa Margarita sedimentation by the southern Temblor Range anticlinorium include the preferential accumulation of sediments along the flanks of the anticlinorium, thickening of strata on the downthrown side of the Recruit Pass fault and on flanks of selected anticlines, intraformational unconformities, and possible partial blockage of the eastward-prograding fan deltas by the Recruit Pass fault. East of the growing southern Temblor Range anticlinorium, the distal ends of the Santa Margarita submarine fans were deflected northwestward by the growing Buena Vista Hills anticline. Several examples of well-defined diachronous sedimentation, where conglomerates and sandstones of the Santa Margarita Formation occupy progressively higher stratigraphic levels in a northwest direction subparallel to the trace of the San Andreas fault, strongly imply that the Salinian basement terrane was shifting in a right-lateral sense during Santa Margarita sedimentation.</p><p>Regional factors of importance in focusing conglomerate sedimentation on the southern Temblor Range locale for a 2- to 3-m.y. period in the late Mohnian were right-lateral oblique slip on the San Andreas fault, formation of the \"big bend\" in the San Andreas fault by left-lateral slip along the Garlock and White Wolf faults, and the partial overlap of the Salinian and Franciscan assemblage basement rocks.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1442","usgsCitation":"Ryder, R.T., and Thomson, A., 1989, Tectonically controlled fan delta and submarine fan sedimentation of late Miocene age, southern Temblor Range, California: U.S. Geological Survey Professional Paper 1442, Report: vii, 59 p.; 5 Plates: 56.10 x 40.00 inches or smaller, https://doi.org/10.3133/pp1442.","productDescription":"Report: vii, 59 p.; 5 Plates: 56.10 x 40.00 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326960,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1442/plate-3.pdf","text":"Plate 3","size":"5.85 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":326961,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1442/plate-4.pdf","text":"Plate 4","size":"7.32 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 4"},{"id":326962,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1442/plate-5.pdf","text":"Plate 5","size":"5.36 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 5"},{"id":165529,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1442/report-thumb.jpg"},{"id":326959,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1442/plate-2.pdf","text":"Plate 2","size":"11.83 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":326958,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1442/plate-1.pdf","text":"Plate 1","size":"42.33 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":340347,"rank":7,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1442/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120,\n              34.5\n            ],\n            [\n              -119,\n              34.5\n            ],\n            [\n              -119,\n              35.5\n            ],\n            [\n              -120,\n              35.5\n            ],\n            [\n              -120,\n              34.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6858e1","contributors":{"authors":[{"text":"Ryder, Robert T. rryder@usgs.gov","contributorId":119319,"corporation":false,"usgs":true,"family":"Ryder","given":"Robert","email":"rryder@usgs.gov","middleInitial":"T.","affiliations":[{"id":596,"text":"U.S. Geological Survey National Center","active":false,"usgs":true},{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":219809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomson, Alan","contributorId":189669,"corporation":false,"usgs":false,"family":"Thomson","given":"Alan","email":"","affiliations":[],"preferred":false,"id":685646,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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