Water logging and flooding of some roads and agricultural lands have become a problem in the Lake Nettie area of eastern McLean County. Part of the flooding is caused by the raising of Lake Audubon about 13 feet from an elevation of about 1,835 feet to 1,848 feet and its effect on ground-water levels in the upper unit of the Lake Nettie aquifer by way of leakage from the lower unit. The major part of the flooding is caused by the greater than normal precipitation and the resulting runoff.
Recharge to the aquifer is from the direct infiltration of precipitation and snowmelt, the lateral percolation of water from the adjacent Fort Union Formation and glacial-drift aquifers, and from Lake Audubon. Discharge is by evapotranspiration and by ground-water movement into undrained surface-water basins in the Lake Holmes-Lake Williams area and southward through Lake Ordway or westward to Lake Audubon.
Trends shown on hydrographs indicate that near equilibrium between recharge and discharge has been reestablished in the lower unit of the Lake Nettie aquifer in the area between Lake Audubon and Lake Nettie, but east of Lake Nettie water levels are still rising. As of 1982, water-level rises caused by the raising of Lake Audubon are as much as 4 feet in the lower unit of the Lake Nettie aquifer and are between 1 and 2 feet in the upper unit of the Lake Nettie aquifer, which is hydraulically connected to Lake Nettie, Crooked Lake, and Slough No. 1. There is a rise in Slough No. 1, about 2 miles east of Lake Audubon, that can be attributed to the higher levels of Lake Audubon. Apparently rises also have occurred in many other sloughs.
Water levels have risen in the Turtle Lake aquifer both as a result of raising the water level in Lake Audubon to an elevation of about 1,848 feet and the McClusky Canal to an elevation of about 1,844 feet. Water levels have risen as much as 6 feet near the canal, but generally less than 1 foot at distances of about 0.5 mile.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834242","usgsCitation":"Armstrong, C.A., 1983, Evaluation of the effects of Lake Audubon on ground- and surface-water levels in the Lake Nettie area, eastern McLean County, North Dakota: U.S. Geological Survey Water-Resources Investigations Report 83-4242, iv, 41 p., https://doi.org/10.3133/wri834242.","productDescription":"iv, 41 p.","numberOfPages":"45","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":396042,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49181.htm"},{"id":54716,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4242/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121745,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4242/report-thumb.jpg"}],"country":"United States","state":"North Dakota","county":"McLean County","otherGeospatial":"Lake Nettie area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -101.0833,\n 47.5\n ],\n [\n -100.75,\n 47.5\n ],\n [\n -100.75,\n 47.6667\n ],\n [\n -101.0833,\n 47.6667\n ],\n [\n -101.0833,\n 47.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa49f","contributors":{"authors":[{"text":"Armstrong, C. A.","contributorId":66231,"corporation":false,"usgs":true,"family":"Armstrong","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":195564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":17252,"text":"ofr83223 - 1983 - Hydrology of Area 1, eastern coal province, Pennsylvania [West Branch Susquehanna River, Sinnemahoning Creek, Upper Juniata River, Clearfield Creek]","interactions":[],"lastModifiedDate":"2022-02-07T21:20:37.876385","indexId":"ofr83223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-223","title":"Hydrology of Area 1, eastern coal province, Pennsylvania [West Branch Susquehanna River, Sinnemahoning Creek, Upper Juniata River, Clearfield Creek]","docAbstract":"Provisions of the Surface Mining Control and Reclamation Act of 1977 recognized a nationwide need for hydrologic information in mined and potentially mined areas. This report is designed to be useful to mine owners, operators, regulatory authorities, citizens groups, and others by presenting information on existing hydrologic conditions and by identifying additional sources of hydrologic information. General hydrologic information is presented in a brief text accompanied by a map, chart, graph, or other illustration for each of a series of water resources-related topics. The summation of the topical discussions provides a description of the hydrology of the area.
The Eastern Coal Province has been divided into 24 hydrologic study areas which are shown on the cover of this report. The divisions are based on hydrologic factors, location, and size. Hydrologic units (surface drainage basins) or parts of units are combined to form each study area.
Area 1 covers 7,400 square miles of the Eastern Coal Province in part or all of 18 counties in west-central Pennsylvania. The major streams in the area are the West Branch Susquehanna and Juniata Rivers. Area 1 counties produced more than 20,000,000 tons of coal during 1979. About 66,000 acres of disturbed coal land in Area 1 counties are in need of reclamation.
Streamflow data have been collected at 146 locations in the area, and water-quality data have been collected at 123 locations. Interpretations of water quality in this report are generally based on a series of four water-quality samples collected at each of 113 locations during the 1979-80 water years. Water-quality data collected at these sites included: specific conductance; dissolved solids; pH; acidity; alkalinty; total and dissolved iron; total and dissolved manganese; sulfate; and bed-material iron, manganese, coal, and organic carbon. Most sites had benthic invertebrate populations sampled and analyses of bed-material constituents. A smaller set of sites was sampled for common constituents and minor elements.
Streams in Clearfield and Cambria Counties, the two leading coal producers in the area, had median specific conductances and dissolved-solids concentrations three to five times greater than those from other area counties. Clearfield County streams had the lowest median stream pH in the area. Most streams sampled in the area had acidity in excess of alkalinity. Streams in the three major coal producing counties in the area had median total-iron concentrations two to three times higher than those for other area counties, and the same general pattern was found for total manganese. The median sulfate concentration of a county's streams showed a close positive correlation with the amount of coal mined in the county. Iron and coal concentrations in bed material were higher in coal-producing counties, but manganese concentrations in bed material were not higher. Twenty-eight streams did not have a benthic biological community as defined by the Office of Surface Mining. Three-fourths of the sites with no biological community had levels of pH, acidity, iron, manganese, and sulfate indicative of acid mine drainage.
Statistics on low flow, mean flow, peak flow, and flow-duration can be computed from gaging station records for gaged streams. The same statistics can be estimated for ungaged streams through the use of regression or graphical techniques. This information may be useful in preparing and evaluating mine-permit applications.
Aquifers in the area receive most recharge from precipitation on outcrop areas. Highest ground-water levels generally occur in spring, decline during the summer, and begin to rise again during the fall. Water levels in valleys generally show less fluctuation than on hills. Median well yields in the area range from 5 to 50 gallons per minute. Ground-water supplies are obtained from more than 40 formations. Ground-water quality is generally suitable for most uses.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83223","usgsCitation":"Herb, W.J., Brown, D.E., Shaw, L.C., and Becher, A.E., 1983, Hydrology of Area 1, eastern coal province, Pennsylvania [West Branch Susquehanna River, Sinnemahoning Creek, Upper Juniata River, Clearfield Creek]: U.S. Geological Survey Open-File Report 83-223, vi, 89 p., https://doi.org/10.3133/ofr83223.","productDescription":"vi, 89 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":149364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0223/report-thumb.jpg"},{"id":94516,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0223/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.31579589843749,\n 39.87601941962116\n ],\n [\n -77.47558593749999,\n 39.87601941962116\n ],\n [\n -77.47558593749999,\n 41.93088998442502\n ],\n [\n -79.31579589843749,\n 41.93088998442502\n ],\n [\n -79.31579589843749,\n 39.87601941962116\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604b72","contributors":{"authors":[{"text":"Herb, William J.","contributorId":79454,"corporation":false,"usgs":true,"family":"Herb","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":175611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Deborah E.","contributorId":92255,"corporation":false,"usgs":true,"family":"Brown","given":"Deborah","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":175614,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shaw, Lewis C.","contributorId":84433,"corporation":false,"usgs":true,"family":"Shaw","given":"Lewis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":175612,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Becher, Albert E.","contributorId":82979,"corporation":false,"usgs":true,"family":"Becher","given":"Albert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":175613,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7195,"text":"ofr83186 - 1983 - Geology report for proposed oil and gas lease sale No. 90; continental margin off the southeastern United States","interactions":[],"lastModifiedDate":"2022-12-01T20:16:31.213544","indexId":"ofr83186","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-186","title":"Geology report for proposed oil and gas lease sale No. 90; continental margin off the southeastern United States","docAbstract":"This report summarizes our general knowledge of the geology and petroleum potential, as well as potential problems and hazards associated with development of petroleum resources, within the area proposed for nominations for lease sale number 90. This area includes the U.S. eastern continental margin from Raleigh Bay, just south of Cape Hatteras, to southern Florida, including the upper Continental Slope and inner Blake Plateau. The area for possible sales for lease sale number 90, as well as the area for lease sale number 78 and the previous areas leased are shown in figure 1; physiographic features of the region are shown in figure 2.
Six exploration wells have been drilled within the proposed lease area (figs. 3 and 4), but no commercial discoveries have been made. All six wells were drilled on the Continental Shelf. No commercial production has been obtained onshore in the region. The areas already drilled have thin sedimentary rock sections, and the deeper strata are dominantly of continental facies. Petroleum formation may have been hindered by a lack of organic material and lack of sufficient burial for thermal maturation. However, analyses of drilling and seismic profiling data presented here indicate that a much thicker section of sedimentary rocks containing a much higher proportion of marine deposits, exists seaward of the Continental Shelf. These geologic conditions imply that the basins farther offshore may be more favorable environments for generating petroleum.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83186","usgsCitation":"Dillon, W.P., 1983, Geology report for proposed oil and gas lease sale No. 90; continental margin off the southeastern United States: U.S. Geological Survey Open-File Report 83-186, Report: 125 p.; 2 Plates: 8.10 x 10.88 inches and 10.80 x 13.29 inches, https://doi.org/10.3133/ofr83186.","productDescription":"Report: 125 p.; 2 Plates: 8.10 x 10.88 inches and 10.80 x 13.29 inches","costCenters":[{"id":132,"text":"Atlantic Marine Geology","active":false,"usgs":true}],"links":[{"id":34584,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0186/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":34583,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0186/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":34585,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0186/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":409945,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13929.htm","linkFileType":{"id":5,"text":"html"}},{"id":140159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0186/report-thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -81.50357992821841,\n 29.56282563875409\n ],\n [\n -76.99516298385373,\n 29.56282563875409\n ],\n [\n -76.99516298385373,\n 34.177210082895485\n ],\n [\n -81.50357992821841,\n 34.177210082895485\n ],\n [\n -81.50357992821841,\n 29.56282563875409\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6e5","contributors":{"authors":[{"text":"Dillon, William P. bdillon@usgs.gov","contributorId":79820,"corporation":false,"usgs":true,"family":"Dillon","given":"William","email":"bdillon@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":154708,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1098,"text":"wsp2210 - 1983 - Connector well experiment to recharge the Floridan aquifer, east Orange County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp2210","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2210","title":"Connector well experiment to recharge the Floridan aquifer, east Orange County, Florida","docAbstract":"An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in east Orange County, Fla., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiomettic surface of the Floridan aquifer; hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well 'connecting' the two aquifers. Continuous flow measurement over 10 months shows the well discharge varies seasonally and averages slightly more than 50 gallons per minute. Observation wells show that, except for seasonal variation, water levels within the area of influence have reached steady state within measurable limits. Vertical anisotropy in the shallow aquifer is apparently caused by the shape and (or) arrangement of the sand grains that comprise the shallow aquifer, rather than because of distinct confining layers of different lithology. Transmissivity of the shallow aquifer at the site is about 600 square feet per clay. Extensive dewatering of wetlands in east Orange County by connector wells alone probably is not feasible. Nevertheless, large amounts of water could be channeled to the Floridan aquifer by connector wells. The results of the connector well experiment imply that water is being captured from evapotranspiration and interception of water that would have discharged to swamps in the vicinity of the connector well. However, the data available from this experiment do not permit a quantitative expression of the net gain in recharge to the Floridan aquifer resulting from operation of the connector well.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wsp2210","usgsCitation":"Bush, P.W., 1983, Connector well experiment to recharge the Floridan aquifer, east Orange County, Florida: U.S. Geological Survey Water Supply Paper 2210, iii, 26 p. :ill., map ;28 cm., https://doi.org/10.3133/wsp2210.","productDescription":"iii, 26 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":138094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2210/report-thumb.jpg"},{"id":25828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2210/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f59","contributors":{"authors":[{"text":"Bush, Peter W.","contributorId":57820,"corporation":false,"usgs":true,"family":"Bush","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143173,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11729,"text":"ofr83747 - 1983 - Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California","interactions":[],"lastModifiedDate":"2022-09-23T20:16:56.047888","indexId":"ofr83747","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-747","title":"Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California","docAbstract":"Hydration-rind ages based on hydration-rind thicknesses of obsidian and an assumed hydration rate of 5 microns /1000 yrs have been determined for the 26 exposed Mono domes and coulees. Hydration-rind thickness data give good estimates of relative age differences between the domes, but determination of absolute ages will depend upon calibration to radiometric ages. \r\n\r\nThe first extrusion of highly differentiated, sparsely porphyritic rhyolite occurred an estimated 32,000 to 40,000 yrs ago and consists of a small dome at the northwest end of the contiguous chain. The next major extrusive event occurred about 24,000 yrs ago and is represented by two domes and a major tephra. About 10,000 yrs ago the frequency of eruptive activity increases and rhyolite lave was extruded at an average rate of 0.2 km3/1000 yrs; periods of dormancy ranging in length from 300 to 2000 yrs. About 2000 to 3000 yrs ago the rate of extrusion increased dramatically to 0.8 km3/1000 yrs beginning with the eruption of the South Coulee and its associated tephra. At the same time, the nature of erupted magma changed from sparsely porphyritic (3 to 10 per cent sanidine) to aphyric rhyolite. All eruptions since 2000 radiocarbon yrs BP have produced magma that is aphyric but is of the same chemical composition as the earlier porphyritic magma. Volumes of porphyritic and aphyric extrusives, each of which includes volumes of lava and volumes of pumiceous pyroclastics reduced for porosity, are nearly equal and together total about 4 km3. Projecting the recent rate of extrusion over the time since the last major eruption, 1185 radiocarbon yrs ago suggests that a future eruption in the Mono Chain could release as much as 1 km 3 of magma. The recent increase in extrusion rate and the contemporaneous change in the nature of the magma are attributed to an event in the magma chamber that allowed the release of hotter, more fluid, crystal-free magma. The young age for the beginning of rhyolite volcanism from the mono magma chamber suggests that rhyolite magma may have been emplaced in the shallow crust as recently as 32,000 to 40,000 yrs ago. Calculations by Lachenbruch et al. (1976, Jour. Geophys. Research, v. 81, p. 769-784) that a thermal disturbance at this age would have propagated upward by solid conduction only 4 km and offer an explanation for the lack of a heat-flow anomaly and surface indications of hydrothermal activity over the Mono magma chamber and its associated ring-fracture system. This report also contains new information on the age and chemistry of volcanics on the Mono Lake island, the Inyo domes, and tephras within the Long Valley Caldera. \r\n\r\nA newly discovered rhyolite tuff ring of late Quaternary age in the Toowa volcanic field of the southern Sierra Nevada is briefly described for it represents a new area that should be examined for potential as a geothermal area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83747","usgsCitation":"Wood, S.H., 1983, Chronology of late Pleistocene and Holocene volcanics, Long Valley and Mono Basin geothermal areas, eastern California: U.S. Geological Survey Open-File Report 83-747, vii, 76 p., https://doi.org/10.3133/ofr83747.","productDescription":"vii, 76 p.","costCenters":[],"links":[{"id":407293,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14207.htm","linkFileType":{"id":5,"text":"html"}},{"id":143964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0747/report-thumb.jpg"},{"id":39615,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0747/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Long Valley and Mono Basin geothermal area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.129,\n 37.681\n ],\n [\n -118.922,\n 37.681\n ],\n [\n -118.922,\n 38.046\n ],\n [\n -119.129,\n 38.046\n ],\n [\n -119.129,\n 37.681\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e073f","contributors":{"authors":[{"text":"Wood, S. H.","contributorId":66261,"corporation":false,"usgs":true,"family":"Wood","given":"S.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":163631,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11271,"text":"ofr83123 - 1983 - General characteristics and availability of Landsat 3 and heat capacity mapping mission thermal infrared data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr83123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-123","title":"General characteristics and availability of Landsat 3 and heat capacity mapping mission thermal infrared data","docAbstract":"Two satellite systems launched by the National Aeronautics and Space Administration (NASA) in 1978 carried sensors which operated in the thermal infrared (IR) region of the electromagnetic spectrum, The final IR radiation data provide spectral information about the physical properties of the Earth's surficial materials not duplicated in either the visible or reflective IR wavelength regions. Landsat 3, launched on March 5, 1978, contained a thermal sensor as part of the multispectral scanner (MSS) system. The sensor operated in the 10.4- to 12.6-?m (band 8) wavelength region and produced imagery with a ground resolution of approximately 235 m. \r\n\r\nLaunched on April 26) 1978) the Heat Capacity Mapping Mission (HCMM) spacecraft carried a sensor, the heat capacity mapping radiometer (HCMR) which operated in the 10.5- to 12.5?m wavelength region and produced imagery with a ground resolution of approximately 600 m at nadir. The HCMM satellite acquired over 6,600 data passes of visible (0.55-1.1 ?m), as well as thermal IR data, over North America, Europe, and Australia. \r\n\r\nGeneral characteristics and availability of Landsat 3 and HCMM thermal IR data are discussed. Landsat 3 reflected IR band 7 (0.55-1.1 ?m) and Landsat 3 band 8 thermal data acquired over the eastern and western United States are analyzed and compared with HCMM visible, thermal IR, thermal inertia, and day-night temperature difference imagery for geologic applications. Digitally processed and enhanced HCMM data (high-pass filters, diagonal derivatives, and band ratios), produced by the U.S. Geological Survey, Flagstaff) Ariz., are presented for geologic interpretation.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83123","usgsCitation":"Southworth, C.S., 1983, General characteristics and availability of Landsat 3 and heat capacity mapping mission thermal infrared data: U.S. Geological Survey Open-File Report 83-123, 30 p. maps (some col.) ;28 cm., https://doi.org/10.3133/ofr83123.","productDescription":"30 p. maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":142961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0123/report-thumb.jpg"},{"id":39063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec45","contributors":{"authors":[{"text":"Southworth, C. Scott 0000-0002-7976-7807 ssouthwo@usgs.gov","orcid":"https://orcid.org/0000-0002-7976-7807","contributorId":1608,"corporation":false,"usgs":true,"family":"Southworth","given":"C.","email":"ssouthwo@usgs.gov","middleInitial":"Scott","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":162841,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11987,"text":"ofr83710 - 1983 - Comparative anatomy of epithermal precious- and base-metal districts hosted by volcanic rocks: A talk presented at the GAC/MSC/GGU Joint Annual Meeting, May 11-13, 1983, Victoria, British Columbia","interactions":[],"lastModifiedDate":"2018-10-22T08:47:25","indexId":"ofr83710","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-710","title":"Comparative anatomy of epithermal precious- and base-metal districts hosted by volcanic rocks: A talk presented at the GAC/MSC/GGU Joint Annual Meeting, May 11-13, 1983, Victoria, British Columbia","docAbstract":"In order to distinguish dissimilar from similar features of epithermal districts, lithotectonic, mineralogical and geochemical traits are compiled for 15 such districts. The districts occur in structurally complex settings associated with silicic to intermediate volcanics. Affiliation with subduction environments on a continental scale and caldera settings on a regional scale is common but is not demonstrable for all districts. Most deposits formed near the end of major volcanism, but some formed considerably later. Paleodepth to the top of the ore is 300-600m for most districts, although Au-rich districts appear to be shallower. The lateral extent of the ore zone is highly variable and far exceeds the limited vertical range (300-800m). Most ore was deposited from dominantly meteoric fluids ranging in temperature from 220°-290°C. Salinities ranged from 0-13 wt% NaCl equiv., and typical values were 1-3 wt%. Although noted for eight deposits, boiling is clearly associated with precious-metal deposition in only two deposits. Four districts, typified by Goldfield, Nev., are characterized by a highly sulfidized mineral assemblage, advanced argillic alteration, and ore deposition closely following emplacement of the host rock. The remaining eleven districts highlight a second, discrete type of deposit. They contain adularia, exhibit sericitic ± argillic alteration, and were mineralized significantly after emplacement of the host rock. The latter category includes two subgroups: Ag- and base-metal-rich deposits (e.g., Creede, Colo.), and Au-rich, base-metal-poor deposits (e.g., Round Mtn., Nev.).
","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83710","usgsCitation":"Heald-Wetlaufer, P., Hayba, D.O., Foley, N.K., and Goss, J., 1983, Comparative anatomy of epithermal precious- and base-metal districts hosted by volcanic rocks: A talk presented at the GAC/MSC/GGU Joint Annual Meeting, May 11-13, 1983, Victoria, British Columbia: U.S. Geological Survey Open-File Report 83-710, 20 p., https://doi.org/10.3133/ofr83710.","productDescription":"20 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":145580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0710/report-thumb.jpg"},{"id":39981,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0710/report.pdf","text":"Report","size":"1.00 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"Mexico, Peru, United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -101.3,\n 21\n ],\n [\n -101.3,\n 21.1\n ],\n [\n -101.2,\n 21.1\n ],\n [\n -101.2,\n 21\n ],\n [\n -101.3,\n 21\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -98.7,\n 20\n ],\n [\n -98.7,\n 20.1\n ],\n [\n -98.8,\n 20.1\n ],\n [\n -98.8,\n 20\n ],\n [\n -98.7,\n 20\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -76.4,\n -11.5\n ],\n [\n -76.4,\n -11.6\n ],\n [\n -76.5,\n -11.6\n ],\n [\n -76.5,\n -11.5\n ],\n [\n -76.4,\n -11.5\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n 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37.77831314799669\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.75050735473633,\n 43.002387443860826\n ],\n [\n -116.75050735473633,\n 43.030753001428344\n ],\n [\n -116.71634674072266,\n 43.030753001428344\n ],\n [\n -116.71634674072266,\n 43.002387443860826\n ],\n [\n -116.75050735473633,\n 43.002387443860826\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.09204101562501,\n 38.14319750166766\n ],\n [\n -118.09204101562501,\n 39.57182223734374\n ],\n [\n -116.71874999999999,\n 39.57182223734374\n ],\n [\n -116.71874999999999,\n 38.14319750166766\n ],\n [\n -118.09204101562501,\n 38.14319750166766\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae552","contributors":{"authors":[{"text":"Heald-Wetlaufer, Pamela","contributorId":21164,"corporation":false,"usgs":true,"family":"Heald-Wetlaufer","given":"Pamela","email":"","affiliations":[],"preferred":false,"id":164538,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayba, Daniel O. 0000-0003-4092-1894 dhayba@usgs.gov","orcid":"https://orcid.org/0000-0003-4092-1894","contributorId":396,"corporation":false,"usgs":true,"family":"Hayba","given":"Daniel","email":"dhayba@usgs.gov","middleInitial":"O.","affiliations":[],"preferred":true,"id":164539,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foley, Nora K. 0000-0003-0124-3509 nfoley@usgs.gov","orcid":"https://orcid.org/0000-0003-0124-3509","contributorId":4010,"corporation":false,"usgs":true,"family":"Foley","given":"Nora","email":"nfoley@usgs.gov","middleInitial":"K.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":164537,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Goss, J.A.","contributorId":62222,"corporation":false,"usgs":true,"family":"Goss","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":164540,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":11552,"text":"ofr83417 - 1983 - Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:44","indexId":"ofr83417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-417","title":"Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado","docAbstract":"The Schwartzwalder uranium deposit, in the Front Range west of Denver, Colorado, is the largest vein-type uranium deposit in the United States. The deposit is situated in a steeply dipping fault system that cuts Proterozoic metamorphic rocks. The host rocks represent a submarine volcanic system with associated chert and iron- and sulfide-rich pelitic rocks. Where faulted, the more competent garnetiferous and quartzitic units behaved brittlely and created a deep, narrow conduit. \r\n\r\nThe ores formed 70-72 m.y. ago beneath 3 km of Phanerozoic sedimentary rocks. Mineralization included two episodes of alteration and three stages of vein-mineralization. Early carbonate-sericite alteration pseudomorphically replaced mafic minerals, whereas the ensuing hematite-adularia episode replaced only the earlier alteration assemblage. Early vein mineralization produced a minor sulfide-adularia-carbonate assemblage. Later vein mineralization generated the uranium ores in two successive stages. Carbonates, sulfides, and adularia filled the remaining voids. Clastic dikes composed of fault gouge and, locally, ore were injected into new and existing fractures. \r\n\r\nGeologic and chemical evidence suggest that virtually all components of the deposit were derived from major hornblende gneiss units and related rocks. The initial fluids were evolved connate/metamorphic water that infiltrated and resided along the extensive fault zones. Complex fault movements in the frontal zone of the eastern Front Range caused the fluids to migrate to the most permeable segments of the fault zones. Heat was supplied by increased crustal heat flow related to igneous activity in the nearby Colorado mineral belt. Temperatures decreased from 225?C to 125?C during later mineralization, and the pressure episodically dropped from 1000 bars. The CO2 fugacity was initially near 100 bars, and uranium was carried as a dicarbonate complex. Sudden decreases in confining pressure during fault movement caused evolution of CO2 and a consequent increase in pH. Uranium was released with destruction of the uranyl complexes; it was subsequently reduced by aqueous sulfur species, thereby leading to the precipitation of pitchblende.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83417","usgsCitation":"Wallace, A.R., 1983, Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado: U.S. Geological Survey Open-File Report 83-417, 186 p. ill. ;28 cm., https://doi.org/10.3133/ofr83417.","productDescription":"186 p. ill. ;28 cm.","costCenters":[],"links":[{"id":145473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0417/report-thumb.jpg"},{"id":39426,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0417/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68751b","contributors":{"authors":[{"text":"Wallace, Alan R.","contributorId":6024,"corporation":false,"usgs":true,"family":"Wallace","given":"Alan","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":163345,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28087,"text":"wri824122 - 1983 - Artificial recharge in the northern part of Chino ground-water basin, upper Santa Ana Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:43","indexId":"wri824122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4122","title":"Artificial recharge in the northern part of Chino ground-water basin, upper Santa Ana Valley, California","docAbstract":"This study was made to help management design and implement a recharge-recapture system for State Water Project water in Chino Basin. Nine test holes were drilled in the study area. Analyses of data from these test holes and drillers ' logs of water wells indicate the presence of clay deposits. The clay deposits cannot be correlated between holes which indicates that they are in the form of discontinuous beds or lenses. The existence and location of two ground-water barriers (Barrier ' J ' and Red Hill Barrier) have been postulated in previous reports. Water-level data indicate that Barrier ' J ' is probably not effectively stopping the movement of ground water. Data are insufficient to determine the effectiveness of the Red Hill barrier. Five existing recharge facilities in the study area were previously constructed to control floodflow. Infiltration tests were conducted at three of the facilities, and results of these tests indicate infiltration rates of 2.6 feet per day at Day Creek, 2.0 feet per day at East Etiwanda, and 1.3 feet per day at San Sevaine. A total of about 9,000 acre-feet of State Water Project water was recharged between June 1980 and July 1981. Rising water levels in wells indicate that recharge water is percolating down to the water table. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824122","usgsCitation":"Koehler, J.H., 1983, Artificial recharge in the northern part of Chino ground-water basin, upper Santa Ana Valley, California: U.S. Geological Survey Water-Resources Investigations Report 82-4122, iv, 27 p. :ill., maps ;26 cm., https://doi.org/10.3133/wri824122.","productDescription":"iv, 27 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":123868,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4122/report-thumb.jpg"},{"id":56907,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4122/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672bfe","contributors":{"authors":[{"text":"Koehler, J. H.","contributorId":108108,"corporation":false,"usgs":true,"family":"Koehler","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":199196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18705,"text":"ofr83739 - 1983 - Analyses of heavy-mineral-concentrate samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire","interactions":[],"lastModifiedDate":"2022-05-04T21:23:22.720667","indexId":"ofr83739","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-739","title":"Analyses of heavy-mineral-concentrate samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83739","usgsCitation":"Domenico, J.A., Howd, F.H., and Nowlan, G., 1983, Analyses of heavy-mineral-concentrate samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire: U.S. Geological Survey Open-File Report 83-739, i, 25 p., https://doi.org/10.3133/ofr83739.","productDescription":"i, 25 p.","costCenters":[],"links":[{"id":48063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0739/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48062,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0739/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0739/report-thumb.jpg"},{"id":400191,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14203.htm"}],"country":"United States","state":"Maine, New Hampshire","otherGeospatial":"Lewiston 1° x 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.063,\n 44\n ],\n [\n -70,\n 44\n ],\n [\n -70,\n 45\n ],\n [\n -71.063,\n 45\n ],\n [\n -71.063,\n 44\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683838","contributors":{"authors":[{"text":"Domenico, J. A.","contributorId":12028,"corporation":false,"usgs":true,"family":"Domenico","given":"J.","middleInitial":"A.","affiliations":[],"preferred":false,"id":179592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howd, F. H.","contributorId":52965,"corporation":false,"usgs":true,"family":"Howd","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":179593,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":179594,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3568,"text":"cir760 - 1983 - Petroleum geology and resources of southeastern Mexico, northern Guatemala, and Belize","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir760","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"760","title":"Petroleum geology and resources of southeastern Mexico, northern Guatemala, and Belize","docAbstract":"Petroleum deposits in southeastern Mexico and Guatemala occur in two main basinal provinces, the Gulf Coast Tertiary basin area, which includes the Reforma and offshore Campeche Mesozoic fields, and the Peten basin of eastern Chiapas State (Mexico) and Guatemala. Gas production is mainly from Tertiary sandstone reservoirs of Miocene age. Major oil production, in order of importance, is from Cretaceous, Paleocene, and Jurassic carbonate reservoirs in the Reforma and offshore Campeche areas. Several small oil fields have been discovered in Cretaceous carbonate reservoirs in west-central Guatemala, and one major discovery has been reported in northwestern Guatemala. Small- to medium-sized oil accumulations also occur in Miocene sandstone reservoirs on salt structures in the Isthmus Saline basin of western Tabasco State, Mexico. Almost all important production is in salt structure traps or on domes and anticlines that may be related to deep-seated salt structures. Some minor oil production has occurred in Cretaceous carbonate reservoirs in a buried overthrust belt along the west flank of the Veracruz basin. \r\n\r\nThe sedimentary cover of Paleozoic through Tertiary rocks ranges in thickness from about 6,000 m (20,000 ft) to as much as 12,000 m (40,000 ft) or more in most of the region. Paleozoic marine carbonate and clastic rocks 1,000 to 2,000 m (3,300 to 6,500 ft) thick overlie the metamorphic and igneous basement in part of the region; Triassic through Middle Jurassic red beds and evaporite deposits, including halite, apparently are present throughout the region, deposited in part in a Triassic graben system. Upper Jurassic (Oxfordian) through Cretaceous rocks make up the bulk of the Mesozoic regional carbonate bank complex, which dominates most of the area. Tertiary marine and continental clastic rocks, some of deep water origin, 3,000 to 10,000 m (10,000 to 35,000 ft) thick, are present in the coastal plain Tertiary basins. These beds grade eastward into a carbonate sequence that overlies the Mesozoic carbonate complex on the Yucatan platform. \r\n\r\nDuring the past 10 years, about 50 large oil fields were discovered in the Reforma and offshore Campeche areas. Oil is produced from intensely microfractured Cretaceous, Paleocene, and Upper Jurassic dolomite reservoirs on blockfaulted salt swells or domes. Most fields are located in the \r\n\r\nMesozoic carbonate-bank margin and forebank talus (Tamabra) facies, which passes through the offshore Campeche and onshore Reforma areas. Oil source rocks are believed to be organic-rich shales and shaly carbonate rocks of latest Jurassic and possibly Early Cretaceous age. At least six of the Mesozoic discoveries are giant or supergiant fields. The largest is the Cantarell complex (about 8 billion to 10 billion barrels (BB)) in the offshore Campeche area and the Bermudez complex (about 8 BB) in the Reforma onshore area. Oil columns are unusually large (from 50 m to as much as 1,000 m, or 160 ft to 3,300 ft). Production rates are extremely high, averaging at least 3,000 to 5,000 barrels of oil per day (bo/d); some wells produce more than 20,000 bo/d, particularly in the offshore Campeche area, where 30,000- to 60,000-bo/d wells are reported. \r\n\r\nTertiary basin fields produce primarily from Miocene sandstone reservoirs. About 50 of these are oil fields ranging from 1 million barrels (MMB) to 200 MMB in size, located on faulted salt structures in the Isthmus Saline basin. Another 30 are gas or gas-condensate fields of a few billion cubic feet to 3 trillion to 4 trillion cubic feet (Tcf) located on salt structures or probable salt structures in the Macuspana, Comalcalco, Isthmus Saline, and Veracruz basins. Source rocks for the gas are believed to be carbonaceous shales interbedded with the sandstone reservoir bodies. \r\nIdentified reserves in the southeastern Mexico-Guatemala \r\narea, almost all in the Mesozoic fields, are about 53 BB of oil, \r\n3 BB of natural gas liquids, and 65 Tcf of gas. The estimat","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir760","usgsCitation":"Peterson, J.A., 1983, Petroleum geology and resources of southeastern Mexico, northern Guatemala, and Belize: U.S. Geological Survey Circular 760, vi, 44 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir760.","productDescription":"vi, 44 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":123013,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0760/report-thumb.jpg"},{"id":30596,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0760/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687e8e","contributors":{"authors":[{"text":"Peterson, James A.","contributorId":106872,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147168,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19790,"text":"ofr83931 - 1983 - Public-supply pumpage in Wisconsin","interactions":[],"lastModifiedDate":"2015-10-08T13:30:56","indexId":"ofr83931","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-931","title":"Public-supply pumpage in Wisconsin","docAbstract":"This report summarizes the amounts and distribution of the pumpage of ground water for public supplies from four aquifers in Wisconsin. The data are for 1979 and reflect the pumpage from about 1,100 wells in 485 communities. The distribution and amount of pumpage is estimated to be similar for subsequent years.
\nOf the water pumped for public supplies, 95 percent comes from two major aquifers--the sand-and-gravel and the sandstone aquifers. Lesser amounts of water come from the Silurian dolomite, which is present onlyl in a narrow band in eastern Wisconsin, and from the generally low-yielding Precambrian basement rock that underlies the entire state.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83931","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Lawrence, C., Ellefson, B., and Cotter, R.D., 1983, Public-supply pumpage in Wisconsin: U.S. Geological Survey Open-File Report 83-931, iv, 40 p., https://doi.org/10.3133/ofr83931.","productDescription":"iv, 40 p.","numberOfPages":"44","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":49269,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0931/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0931/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f934","contributors":{"authors":[{"text":"Dyer, Kenneth L.","contributorId":82353,"corporation":false,"usgs":true,"family":"Dyer","given":"Kenneth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197221,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":19847,"text":"ofr83816 - 1983 - The Emma Bell deposit, Siskiyou Co., California: A possible low-grade source of chromite","interactions":[],"lastModifiedDate":"2021-11-16T20:29:28.488564","indexId":"ofr83816","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-816","title":"The Emma Bell deposit, Siskiyou Co., California: A possible low-grade source of chromite","docAbstract":"The Emma Bell chromite deposit in Siskiyou County, California contains over 5 million tons of dunite averaging about 4 percent Cr2O3. Chromite is not evenly disseminated throughout the dunite, however. For the most part the deposit consists of many chromite-rich bands in sharp contact with, and separated by, common dunite containing 1 to 2 percent accessory chromite. Electron microprobe and petrographic analysis of accessory chromite shows that it is fine grained (average grain size 0.14 mm), generally lower in Cr2O3, and has a lower Cr/Fe ratio than segregated chromite. In addition, unusual patchy zoning is exhibited by some accessory chromite. These patchy zones are extremely rich in iron (>60 percent total iron oxide). The negative factors such as the fine-grained nature of the accessory chromite and high iron content compared to segregated chromite, could be overcome by the very large tonnage in the deposit.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83816","usgsCitation":"Lipin, B., Wetzel, N., and Heinrich, S.M., 1983, The Emma Bell deposit, Siskiyou Co., California: A possible low-grade source of chromite: U.S. Geological Survey Open-File Report 83-816, i, 16 p., https://doi.org/10.3133/ofr83816.","productDescription":"i, 16 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":391761,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14237.htm"},{"id":152420,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0816/report-thumb.jpg"},{"id":49326,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0816/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Siskiyou County","otherGeospatial":"Emma Bell deposit","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.176,\n 41.905\n ],\n [\n -123.125,\n 41.905\n ],\n [\n -123.125,\n 41.95\n ],\n [\n -123.176,\n 41.95\n ],\n [\n -123.176,\n 41.905\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c8b5","contributors":{"authors":[{"text":"Lipin, B. 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M.","contributorId":95892,"corporation":false,"usgs":true,"family":"Heinrich","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":181622,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7937,"text":"ofr83440 - 1983 - Central and Eastern United States; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-440","title":"Central and Eastern United States; basic data for thermal springs and wells as recorded in Geotherm","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83440","usgsCitation":"Bliss, J.D., 1983, Central and Eastern United States; basic data for thermal springs and wells as recorded in Geotherm: U.S. Geological Survey Open-File Report 83-440, iv, 87 p. ;28 cm., https://doi.org/10.3133/ofr83440.","productDescription":"iv, 87 p. ;28 cm.","costCenters":[],"links":[{"id":140806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0440/report-thumb.jpg"},{"id":35508,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0440/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6e35","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156865,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23793,"text":"ofr83207 - 1983 - Summary of water withdrawals in the United States, 1950-80","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr83207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-207","title":"Summary of water withdrawals in the United States, 1950-80","docAbstract":"Estimated use of water in the United States increased from 180 bgd (billion gallons per day) in 1950 to 450 bgd in 1980. During this same time population increased from about 150 million to about 230 million. Data on consumptive use are not available for the first decade of the period; however, from 1960 to 1980, consumptive use increased from 61 bgd to 100 bgd. \r\n\r\nFrom 1950 to 1980, fresh surface-water withdrawals increased from 140 bgd to 290 bgd and fresh ground-water withdrawals increased from 34 bgd to 88 bgd. Withdrawals of saline surface water increased from 10 bgd in 1950 to 71 bgd in 1980. In 1980, 91 percent of the saline surface water withdrawn was used in thermoelectric power plants. \r\n\r\nWithdrawals of water for domestic purposes nationwide increased from 16 bgd in 1960 to 25 bgd in 1980. The Northeastern States still are the largest users of water for domestic purposes; however, domestic withdrawals in that region declined from 9.6 bgd in 1975 to 8.8 bgd in 1980. Population in that region also showed a slight decline from 1970 to 1980. \r\n\r\nIrrigation withdrawals nationwide increased from 89 bgd in 1950 to 150 bgd in 1980. The Western States continue to be the largest user of irrigation water, 136 bgd in 1980. Irrigation accounted for 81 percent of the total consumptive use for the Nation in 1980. \r\n\r\nIndustrial withdrawals (exclusive of thermoelectric power generation) increased from 44 bgd in 1960 to about 56 bgd in 1980. The Northeast Region continues to withdraw the largest amount of water for industrial purposes, although withdrawals declined steadily from 33 bgd in 1965 to 27 bgd in 1980. \r\n\r\nTotal withdrawals for thermoelectric power generation increased from about 99 bgd in 1960 to about 210 bgd in 1980. During that period, saline surface water withdrawals increased from 26 bgd to 71 bgd. Thermoelectric plants accounted for 84 percent of saline surface water withdrawals in 1960 compared to 91 percent in 1980. Withdrawals for thermoelectric power generation continue to be the largest in the Northeast, ll3 bgd in 1980, where many of the major industrial and population centers are located. \r\n\r\nAgriculture (nonirrigation) water withdrawals nationwide increased from 1.6 bgd in 1960 to about 2.2 bgd in 1980. Withdrawals for this purpose in 1980 were about evenly divided between the West and East.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83207","issn":"0094-9140","usgsCitation":"Mann, W., Solley, W.B., and Chase, E.B., 1983, Summary of water withdrawals in the United States, 1950-80: U.S. Geological Survey Open-File Report 83-207, 22 p. ill., 1 map ;28 cm., https://doi.org/10.3133/ofr83207.","productDescription":"22 p. ill., 1 map ;28 cm.","costCenters":[],"links":[{"id":156847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0207/report-thumb.jpg"},{"id":53015,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0207/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4881e4b07f02db51670d","contributors":{"authors":[{"text":"Mann, William B.","contributorId":21985,"corporation":false,"usgs":true,"family":"Mann","given":"William B.","affiliations":[],"preferred":false,"id":190735,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Solley, Wayne B.","contributorId":61409,"corporation":false,"usgs":true,"family":"Solley","given":"Wayne","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":190736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chase, Edith B.","contributorId":11192,"corporation":false,"usgs":true,"family":"Chase","given":"Edith","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":190734,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":9931,"text":"ofr83592 - 1983 - Eastern Gulf of Alaska seismicity: Final report to the National Oceanic and Atmospheric Administration for July 1, 1975, through September 30, 1981","interactions":[],"lastModifiedDate":"2022-12-12T22:32:38.805937","indexId":"ofr83592","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-592","title":"Eastern Gulf of Alaska seismicity: Final report to the National Oceanic and Atmospheric Administration for July 1, 1975, through September 30, 1981","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83592","usgsCitation":"Lahr, J.C., and Stephens, C., 1983, Eastern Gulf of Alaska seismicity: Final report to the National Oceanic and Atmospheric Administration for July 1, 1975, through September 30, 1981: U.S. Geological Survey Open-File Report 83-592, 48 p., https://doi.org/10.3133/ofr83592.","productDescription":"48 p.","costCenters":[],"links":[{"id":410335,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14119.htm","linkFileType":{"id":5,"text":"html"}},{"id":37713,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0592/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144046,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0592/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"eastern Gulf of Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -136.50699581919312,\n 58.25683134476469\n ],\n [\n -141.03281680066513,\n 59.80148318152371\n ],\n [\n -145.59090741484098,\n 60.788650974736555\n ],\n [\n -147.08261119524425,\n 61.00000324280887\n ],\n [\n -145.7721746037704,\n 56.60939795810589\n ],\n [\n -136.0653342871446,\n 56.852428007950806\n ],\n [\n -136.50699581919312,\n 58.25683134476469\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db629522","contributors":{"authors":[{"text":"Lahr, John C.","contributorId":20328,"corporation":false,"usgs":true,"family":"Lahr","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":160531,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, C.D.","contributorId":18752,"corporation":false,"usgs":true,"family":"Stephens","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":160530,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":20306,"text":"ofr83848 - 1983 - Analytical results for 2244 stream-sediment samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire","interactions":[],"lastModifiedDate":"2021-10-22T19:01:13.844526","indexId":"ofr83848","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-848","title":"Analytical results for 2244 stream-sediment samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83848","usgsCitation":"Nowlan, G., Howd, F.H., and Nakagawa, H.M., 1983, Analytical results for 2244 stream-sediment samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire: U.S. Geological Survey Open-File Report 83-848, Report: i, 117 p.; 1 Plate: 30.53 × 47.40 inches, https://doi.org/10.3133/ofr83848.","productDescription":"Report: i, 117 p.; 1 Plate: 30.53 × 47.40 inches","costCenters":[],"links":[{"id":152191,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0848/report-thumb.jpg"},{"id":49840,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0848/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49841,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0848/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390840,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14244.htm"}],"country":"United States","state":"Maine, New Hampshire","otherGeospatial":"Lewiston 1° x 2° quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.211,\n 44\n ],\n [\n -70,\n 44\n ],\n [\n -70,\n 45\n ],\n [\n -71.211,\n 45\n ],\n [\n -71.211,\n 44\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca6d","contributors":{"authors":[{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":182426,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howd, F. H.","contributorId":52965,"corporation":false,"usgs":true,"family":"Howd","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":182425,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nakagawa, H. M.","contributorId":106475,"corporation":false,"usgs":true,"family":"Nakagawa","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":182427,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":29871,"text":"wri824109 - 1983 - Appraisal of the interconnection between the St Johns River and the surficial aquifer, east-central Duval County, Florida","interactions":[],"lastModifiedDate":"2024-01-08T23:01:11.323275","indexId":"wri824109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4109","title":"Appraisal of the interconnection between the St Johns River and the surficial aquifer, east-central Duval County, Florida","docAbstract":"The proposed deepening of the navigation channel in the St. Johns River to about 46-48 feet below sea level (45 feet below mean low water) may breach up to 11 feet of limestone unit of the lower part of the surficial aquifer along a 25-mile channel. The limestone supplies water to numerous domestic wells along the river in the Jacksonville area. Recent channel improvements to about 39 feet below sea level have already breached the limestone at many locations. Where breaching has not yet occurred, less than 1 to 6 feet of undifferentiated sediments overlie the limestone. These sediments, consisting predominantly of sand, are generally too permeable to form an effective confining layer. Chloride concentrations determined from water in wells tapping the limestone unit range from 8 to 6,600 milligrams per liter. However, chloride concentrations in water from wells located more than 500 feet from the river, were generally less than 30 milligrams per liter. The proposed dredging operation is not expected to alter significantly the present hydrologic system. The current position of the interface most likely represents conditions that will be present after future channel improvements. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824109","usgsCitation":"Spechler, R., and Stone, R.B., 1983, Appraisal of the interconnection between the St Johns River and the surficial aquifer, east-central Duval County, Florida: U.S. Geological Survey Water-Resources Investigations Report 82-4109, iv, 38 p., https://doi.org/10.3133/wri824109.","productDescription":"iv, 38 p.","costCenters":[],"links":[{"id":424204,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35616.htm","linkFileType":{"id":5,"text":"html"}},{"id":58685,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4109/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123308,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4109/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Duval County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -81.72156565133055,\n 30.471947232313866\n ],\n [\n -81.72156565133055,\n 30.27618396890138\n ],\n [\n -81.39844829812067,\n 30.27618396890138\n ],\n [\n -81.39844829812067,\n 30.471947232313866\n ],\n [\n -81.72156565133055,\n 30.471947232313866\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a369","contributors":{"authors":[{"text":"Spechler, R. M.","contributorId":85961,"corporation":false,"usgs":true,"family":"Spechler","given":"R. M.","affiliations":[],"preferred":false,"id":202279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stone, R. B. Jr.","contributorId":71598,"corporation":false,"usgs":true,"family":"Stone","given":"R.","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":202278,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":18803,"text":"ofr82864 - 1983 - Hydrology of area 10, Eastern Coal Province, West Virginia and Virginia","interactions":[],"lastModifiedDate":"2023-12-13T21:02:30.442332","indexId":"ofr82864","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-864","title":"Hydrology of area 10, Eastern Coal Province, West Virginia and Virginia","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82864","usgsCitation":"Ehlke, T.A., McCauley, S.D., Schultz, R.A., Bader, J., Runner, G.S., and Downs, S.C., 1983, Hydrology of area 10, Eastern Coal Province, West Virginia and Virginia: U.S. Geological Survey Open-File Report 82-864, v, 73 p., https://doi.org/10.3133/ofr82864.","productDescription":"v, 73 p.","costCenters":[],"links":[{"id":95416,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0864/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152920,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0864/report-thumb.jpg"},{"id":423532,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13845.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Virginia, West Virginia","otherGeospatial":"Area 10","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -81.2305875752171,\n 37.237962508166916\n ],\n [\n -81.07592965369068,\n 37.00253435336218\n ],\n [\n -80.09174288034123,\n 37.21277309392809\n ],\n [\n -79.61370930471458,\n 37.40288462880359\n ],\n [\n -80.13743726624699,\n 37.86218294165562\n ],\n [\n -79.49420064369879,\n 38.6790003602099\n ],\n [\n -79.73673238427408,\n 38.80785124653647\n ],\n [\n -80.17961643228112,\n 38.409585365316985\n ],\n [\n -81.2868289170625,\n 37.45033682465838\n ],\n [\n -81.34658311401566,\n 37.32745615996632\n ],\n [\n -81.43094198030279,\n 37.25195244255953\n ],\n [\n -81.2305875752171,\n 37.237962508166916\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6046e7","contributors":{"authors":[{"text":"Ehlke, T. A.","contributorId":106477,"corporation":false,"usgs":true,"family":"Ehlke","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCauley, S. D.","contributorId":63036,"corporation":false,"usgs":true,"family":"McCauley","given":"S.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":179767,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schultz, R. A.","contributorId":108126,"corporation":false,"usgs":true,"family":"Schultz","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179771,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bader, J. S.","contributorId":65830,"corporation":false,"usgs":true,"family":"Bader","given":"J. S.","affiliations":[],"preferred":false,"id":179768,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Runner, G. S.","contributorId":74405,"corporation":false,"usgs":true,"family":"Runner","given":"G.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":179769,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Downs, S. C.","contributorId":36956,"corporation":false,"usgs":true,"family":"Downs","given":"S.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":179766,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":27380,"text":"wri811108 - 1983 - Ground-water resources in the Hood Basin, Oregon","interactions":[],"lastModifiedDate":"2016-10-21T10:33:36","indexId":"wri811108","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"81-1108","title":"Ground-water resources in the Hood Basin, Oregon","docAbstract":"The Hood Basin, an area of 1,035 square miles in north-central Oregon, includes the drainage basins of all tributaries of the Columbia River between Eagle Creek and Fifteenmile Creek. The physical characteristics and climate of the basin are diverse. The Wasco subarea, in the eastern half of the basin, has moderate relief, mostly intermittent streams, and semiarid climate. The Hood subarea, in the western half, has rugged topography, numerous perennial streams, and a humid climate.
Water-bearing geologic units that underlie the basin include volcanic, volcaniclastic, and sedimentary rocks of Miocene to Holocene age, and unconsolidated surficial deposits of Pleistocene and Holocene age. The most important water-bearing unit, the Columbia River Basalt Group, underlies almost the entire basin. Total thickness probably exceeds 2,000 feet, but by 1980 only the upper 1,000 feet or less had been developed by wells. Wells in this unit generally yield from 15 to 1,000 gallons per minute and a few yield as much as 3,300 gallons per minute.
The most productive aquifer in the Columbia River Basalt Group is The Dalles Ground Water Reservoir, a permeable zone of fractured basalt about 25 to 30 square miles in extent that underlies the city of The Dalles. During the late 1950's and mid-1960's, withdrawals of 15,000 acre-feet per year or more caused water levels in the aquifer to decline sharply. Pumpage had diminished to about 5,000 acre-feet per year in 1979 and water levels have stabilized, indicating that ground water recharge and discharge, including the pumping, are in balance.
The other principal geologic units in the basin have more limited areal distribution and less saturated thickness than the Columbia River Basalt Group. Generally, these units are capable of yielding from a few to a hundred gallons per minute to wells.
Most of the ground water in the basin is chemically suitable for domestic, irrigation, or other uses. Some ground water has objectionable concentrations of iron (0.3 to 6.4 milligrams per liter) and manganese (0.05 to 1.2 milligrams per liter) or is moderately hard to very hard (60 to 260 milligrams per liter as CaCO3).
The principal use of ground water in the Hood Basin is for irrigation of crops, with an estimated withdrawal of 7,700 acre-feet in 1979. Additional ground-water withdrawals in 1979 were estimated as: Industrial, 2,600 acre-feet; public supply, 2,100 acre-feet; and domestic and stock supply, 200 acre-feet.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/wri811108","collaboration":"Prepared in cooperation with Wasco and Hood River Counties","usgsCitation":"Grady, S.J., 1983, Ground-water resources in the Hood Basin, Oregon: U.S. Geological Survey Water-Resources Investigations Report 81-1108, Report: viii, 58 p.; 2 Plates: 36.05 x 37.78 inches and 30.57 x 37.96 inches, https://doi.org/10.3133/wri811108.","productDescription":"Report: viii, 58 p.; 2 Plates: 36.05 x 37.78 inches and 30.57 x 37.96 inches","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":159039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri811108.JPG"},{"id":330293,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/1108/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330295,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/1108/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330294,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/1108/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Hood Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122,\n 45.733333\n ],\n [\n -122,\n 45.5\n ],\n [\n -120.875,\n 45.5\n ],\n [\n -120.875,\n 45.733333\n ],\n [\n -122,\n 45.733333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696dbb","contributors":{"authors":[{"text":"Grady, Stephen J.","contributorId":101636,"corporation":false,"usgs":true,"family":"Grady","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198013,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9544,"text":"ofr82440 - 1983 - Hydrology of area 20, Eastern Coal Province, Tennessee, Georgia and Alabama","interactions":[],"lastModifiedDate":"2024-09-23T22:12:54.319025","indexId":"ofr82440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-440","title":"Hydrology of area 20, Eastern Coal Province, Tennessee, Georgia and Alabama","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82440","usgsCitation":"Hollyday, E., 1983, Hydrology of area 20, Eastern Coal Province, Tennessee, Georgia and Alabama: U.S. Geological Survey Open-File Report 82-440, v, 145 p., https://doi.org/10.3133/ofr82440.","productDescription":"v, 145 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":462159,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13725.htm","linkFileType":{"id":5,"text":"html"}},{"id":94931,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0440/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142669,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0440/report-thumb.jpg"}],"country":"United States","state":"Alabama, Georgia, Tennessee","otherGeospatial":"Eastern Coal Province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.15478515625,\n 34.38877925439021\n ],\n [\n -86.15478515625,\n 35.8356283888737\n ],\n [\n -84.869384765625,\n 35.8356283888737\n ],\n [\n -84.869384765625,\n 34.38877925439021\n ],\n [\n -86.15478515625,\n 34.38877925439021\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602d35","contributors":{"authors":[{"text":"Hollyday, E. F.","contributorId":95062,"corporation":false,"usgs":true,"family":"Hollyday","given":"E. F.","affiliations":[],"preferred":false,"id":159866,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9477,"text":"ofr83359 - 1983 - Regional magnetic and gravity features of the Gibson Dome area and surrounding region, Paradox Basin, Utah: A preliminary report","interactions":[],"lastModifiedDate":"2022-02-22T22:13:46.493453","indexId":"ofr83359","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-359","title":"Regional magnetic and gravity features of the Gibson Dome area and surrounding region, Paradox Basin, Utah: A preliminary report","docAbstract":"Analyses of regional gravity and magnetic anomaly maps have been carried out to assist in the evaluation of the Gibson Dome area as a possible repository site for high-level radioactive waste. Derivative, wavelength-filtered, and trend maps were compiled to aid in properly locating major geophysical trends corresponding to faults, folds, and lithologic boundaries. The anomaly maps indicate that Paradox Basin is characterized by a heterogeneous Precambrian basement, essentially a metamorphic complex of gneisses and schist intruded by granitic rocks and mafic to ultramafic bodies. Interpreted Precambrian structures trend predominantly northwest and northeast although east-west trending features are evident. Prominent gravity lows define the salt anticlines. Structural and lithologic trends in the Gibson Dome area are closely examined. Of greatest interest is a series of circular magnetic highs trending west-northwest into the Gibson Dome area. Further study of the exact definition and geologic significance of this series of anomalies is warranted.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83359","usgsCitation":"Hildenbrand, T., and Kucks, R., 1983, Regional magnetic and gravity features of the Gibson Dome area and surrounding region, Paradox Basin, Utah: A preliminary report: U.S. Geological Survey Open-File Report 83-359, Report: 34 p.; 3 Plates: 32.79 × 40.67 inches or smaller, https://doi.org/10.3133/ofr83359.","productDescription":"Report: 34 p.; 3 Plates: 32.79 × 40.67 inches or smaller","costCenters":[],"links":[{"id":396292,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13996.htm"},{"id":37186,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0359/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37185,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0359/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37184,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0359/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37183,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0359/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0359/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Gibson Dome area, Paradox Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.7130,\n 37.388\n ],\n [\n -108.617,\n 37.388\n ],\n [\n -108.617,\n 39.045\n ],\n [\n -110.7130,\n 39.045\n ],\n [\n -110.7130,\n 37.388\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4ae","contributors":{"authors":[{"text":"Hildenbrand, T.G.","contributorId":83892,"corporation":false,"usgs":true,"family":"Hildenbrand","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":159757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kucks, R.P.","contributorId":53758,"corporation":false,"usgs":true,"family":"Kucks","given":"R.P.","affiliations":[],"preferred":false,"id":159756,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}