{"pageNumber":"1480","pageRowStart":"36975","pageSize":"25","recordCount":46700,"records":[{"id":70013677,"text":"70013677 - 1988 - Aftershocks of the western Argentina (Caucete) earthquake of 23 November 1977: Some tectonic implications","interactions":[],"lastModifiedDate":"2025-08-25T15:39:57.896156","indexId":"70013677","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Aftershocks of the western Argentina (Caucete) earthquake of 23 November 1977: Some tectonic implications","docAbstract":"<p><span>An aftershock survey, using a network of eight portable and two permanent seismographs, was conducted for the western Argentina (Caucete) earthquake (</span><i>M</i><sub><i>S</i></sub><span>&nbsp;7.3) of November 23, 1977. Monitoring began December 6, almost 2 weeks after the main shock and continued for 11 days. The data set includes 185 aftershock hypocenters that range in the depth from near surface to more than 30 km. The spatial distribution of those events occupied a volume of about 100 km long ×50 km wide ×30 km thick. The volumnar nature of the aftershock distribution is interpreted to be a result of a bimodal distribution of foci that define east- and west-dipping planar zones. Efforts to select which of those zones was associated with the causal faulting include special attention to the determination of the mainshock focal depth and dislocation theory modeling of the coseismic surface deformation in the epicentral region. Our focal depth (25–35 km) and modeling studies lead us to prefer an east-dipping plane as causal. A previous interpretation by other investigators used a shallower focal depth (17 km) and similar modeling calculations in choosing a west-dipping plane. Our selection of the east-dipping plane is physically more appealing because it places fault initiation at the base of the crustal seismogenic layer (rather than in the middle of that layer) which requires fault propagation to be updip (rather than downdip).</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(88)90166-7","issn":"00401951","usgsCitation":"Langer, C., and Bollinger, G.A., 1988, Aftershocks of the western Argentina (Caucete) earthquake of 23 November 1977: Some tectonic implications: Tectonophysics, v. 148, no. 1-2, p. 131-146, https://doi.org/10.1016/0040-1951(88)90166-7.","productDescription":"16 p.","startPage":"131","endPage":"146","costCenters":[],"links":[{"id":220157,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Argentina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -68.31581448033793,\n              -31.101424732207356\n            ],\n            [\n              -68.31581448033793,\n              -31.99657323096657\n            ],\n            [\n              -67.57002983228087,\n              -31.99657323096657\n            ],\n            [\n              -67.57002983228087,\n              -31.101424732207356\n            ],\n            [\n              -68.31581448033793,\n              -31.101424732207356\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"148","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e8d4e4b0c8380cd47ed3","contributors":{"authors":[{"text":"Langer, C.J.","contributorId":31395,"corporation":false,"usgs":true,"family":"Langer","given":"C.J.","email":"","affiliations":[],"preferred":false,"id":366616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bollinger, G. A.","contributorId":55809,"corporation":false,"usgs":true,"family":"Bollinger","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":366617,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70013733,"text":"70013733 - 1988 - An improved dark-object subtraction technique for atmospheric scattering correction of multispectral data","interactions":[],"lastModifiedDate":"2025-07-17T15:54:35.25532","indexId":"70013733","displayToPublicDate":"2003-04-11T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"An improved dark-object subtraction technique for atmospheric scattering correction of multispectral data","docAbstract":"<p><span>Digital analysis of remotely sensed data has become an important component of many earth-science studies. These data are often processed through a set of preprocessing or “clean-up” routines that includes a correction for atmospheric scattering, often called haze. Various methods to correct or remove the additive haze component have been developed, including the widely used dark-object subtraction technique. A problem with most of these methods is that the haze values for each spectral band are selected independently. This can create problems because atmospheric scattering is highly wavelength-dependent in the visible part of the electromagnetic spectrum and the scattering values are correlated with each other. Therefore, multispectral data such as from the Landsat Thematic Mapper and Multispectral Scanner must be corrected with haze values that are spectral band dependent. An improved dark-object subtraction technique is demonstrated that allows the user to select a&nbsp;</span><i>relative</i><span>&nbsp;atmospheric scattering model to predict the haze values for all the spectral bands from a selected starting band haze value. The improved method normalizes the predicted haze values for the different gain and offset parameters used by the imaging system. Examples of haze value differences between the old and improved methods for Thematic Mapper Bands 1, 2, 3, 4, 5, and 7 are 40.0, 13.0, 12.0, 8.0, 5.0, and 2.0 vs. 40.0, 13.2, 8.9, 4.9, 16.7, and 3.3, respectively, using a relative scattering model of a clear atmosphere. In one Landsat multispectral scanner image the haze value differences for Bands 4, 5, 6, and 7 were 30.0, 50.0, 50.0, and 40.0 for the old method vs. 30.0, 34.4, 43.6, and 6.4 for the new method using a relative scattering model of a hazy atmosphere.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0034-4257(88)90019-3","issn":"00344257","usgsCitation":"Chavez, P.S., 1988, An improved dark-object subtraction technique for atmospheric scattering correction of multispectral data: Remote Sensing of Environment, v. 24, no. 3, p. 459-479, https://doi.org/10.1016/0034-4257(88)90019-3.","productDescription":"21 p.","startPage":"459","endPage":"479","costCenters":[],"links":[{"id":220218,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"northern Arizona","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -112.51428402871795,\n              35.76132241917742\n            ],\n            [\n              -112.51428402871795,\n              35.12484483192148\n            ],\n            [\n              -111.06027608212764,\n              35.12484483192148\n            ],\n            [\n              -111.06027608212764,\n              35.76132241917742\n            ],\n            [\n              -112.51428402871795,\n              35.76132241917742\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ea6ee4b0c8380cd48869","contributors":{"authors":[{"text":"Chavez, Pat S. Jr.","contributorId":39870,"corporation":false,"usgs":true,"family":"Chavez","given":"Pat","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":366748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70013680,"text":"70013680 - 1988 - Use of airborne imaging spectrometer data to map minerals associated with hydrothermally altered rocks in the northern Grapevine Mountains, Nevada, and California","interactions":[],"lastModifiedDate":"2025-07-17T16:03:26.450169","indexId":"70013680","displayToPublicDate":"2003-04-11T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3254,"text":"Remote Sensing of Environment","printIssn":"0034-4257","active":true,"publicationSubtype":{"id":10}},"title":"Use of airborne imaging spectrometer data to map minerals associated with hydrothermally altered rocks in the northern Grapevine Mountains, Nevada, and California","docAbstract":"<p><span>Three flightlines of Airborne Imaging Spectrometer (AIS) data, acquired over the northern Grapevine Mountains, Nevada, and California, were used to map minerals associated with hydrothermally altered rocks. The data were processed to remove vertical striping, normalized using an equal area normalization, and reduced to reflectance relative to an average spectrum derived from the data. An algorithm was developed to automatically calculate the absorption band parameters band position, band depth, and band width for the strongest absorption feature in each pixel. These parameters were mapped into an intensity, hue, saturation (IHS) color system to produce a single color image that summarized the absorption band information, This image was used to map areas of potential alteration based upon the predicted relationships between the color image and mineral absorption band. Individual AIS spectra for these areas were then examined to identify specific minerals. Two types of alteration were mapped with the AIS data. Areas of quartz-sericite-pyrite alteration were identified based upon a strong absorption feature near 2.21 μm, a weak shoulder near 2.25 μm, and a weak absorption band near 2.35 μm caused by sericite (fine-grained muscovite). Areas of argillic alteration were defined based on the presence of montmorillonite, identified by a weak to moderate absorption feature near 2.21 μm and the absence of the 2.35 μm band. Montmorillonite could not be identified in mineral mixtures. Calcite and dolomite were identified based on sharp absorption features near 2.34 and 2.32 μm, respectively. Areas of alteration identified using the AIS data corresponded well with areas mapped using field mapping, field reflectance spectra, and laboratory spectral measurements.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0034-4257(88)90004-1","issn":"00344257","usgsCitation":"Kruse, F., 1988, Use of airborne imaging spectrometer data to map minerals associated with hydrothermally altered rocks in the northern Grapevine Mountains, Nevada, and California: Remote Sensing of Environment, v. 24, no. 1, p. 31-51, https://doi.org/10.1016/0034-4257(88)90004-1.","productDescription":"21 p.","startPage":"31","endPage":"51","costCenters":[],"links":[{"id":220213,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"northern Grapevine Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.25035077426466,\n              37.014559377695576\n            ],\n            [\n              -117.25035077426466,\n              36.75769172696985\n            ],\n            [\n              -116.86542089423386,\n              36.75769172696985\n            ],\n            [\n              -116.86542089423386,\n              37.014559377695576\n            ],\n            [\n              -117.25035077426466,\n              37.014559377695576\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"24","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbeaee4b08c986b329711","contributors":{"authors":[{"text":"Kruse, F.A.","contributorId":30676,"corporation":false,"usgs":true,"family":"Kruse","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":366626,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14954,"text":"ofr87549 - 1988 - Post-eruption changes in channel geometry of streams in the Toutle River drainage basin, 1983-85, Mount St. Helens, Washington","interactions":[],"lastModifiedDate":"2022-05-04T17:12:27.532673","indexId":"ofr87549","displayToPublicDate":"2001-09-01T00:00:00","publicationYear":"1988","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":"87-549","title":"Post-eruption changes in channel geometry of streams in the Toutle River drainage basin, 1983-85, Mount St. Helens, Washington","docAbstract":"<p>The May 18, 1980, eruption of Mount St. Helens generated a debris avalanche, lateral blast, lahars and tephra deposits that altered mainstream and tributary channels within the Toutle River drainage basin. Channel cross sections were monumented and surveyed on the North Fork Toutle River and its tributaries, South Fork Toutle River, Green River, and Toutle River in 1980 and 1981. These streams drain the north and west flanks of the volcano. The network of channel cross sections has been resurveyed annually. Selected cross sections were surveyed more frequently following periods of higher flow. The repetitive cross-section surveys provide measurements of hank erosion or accretion and of channel erosion or aggradation. These data can be used to determine erosion rates, and to identify sources and storage sites of sediment in sediment budget computations. This report presents channel cross-section profiles constructed from the survey data collected during water years 1983-85.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87549","usgsCitation":"Meyer, D.F., and Dodge, J., 1988, Post-eruption changes in channel geometry of streams in the Toutle River drainage basin, 1983-85, Mount St. Helens, Washington: U.S. Geological Survey Open-File Report 87-549, v, 226 p., https://doi.org/10.3133/ofr87549.","productDescription":"v, 226 p.","costCenters":[],"links":[{"id":400175,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0549/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145950,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0549/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.29705810546874,\n              46.18743678432541\n            ],\n            [\n              -121.981201171875,\n              46.18743678432541\n            ],\n            [\n              -121.981201171875,\n              46.32417161725691\n            ],\n            [\n              -122.29705810546874,\n              46.32417161725691\n            ],\n            [\n              -122.29705810546874,\n              46.18743678432541\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683acc","contributors":{"authors":[{"text":"Meyer, D. F.","contributorId":21167,"corporation":false,"usgs":true,"family":"Meyer","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":170312,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dodge, J.E.","contributorId":21133,"corporation":false,"usgs":true,"family":"Dodge","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":170311,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38198,"text":"pp1386B - 1988 - Glaciers of Antarctica","interactions":[{"subject":{"id":38198,"text":"pp1386B - 1988 - Glaciers of Antarctica","indexId":"pp1386B","publicationYear":"1988","noYear":false,"chapter":"B","title":"Glaciers of Antarctica"},"predicate":"IS_PART_OF","object":{"id":70042384,"text":"pp1386 - 1988 - Satellite image atlas of glaciers of the world","indexId":"pp1386","publicationYear":"1988","noYear":false,"title":"Satellite image atlas of glaciers of the world"},"id":1}],"isPartOf":{"id":70042384,"text":"pp1386 - 1988 - Satellite image atlas of glaciers of the world","indexId":"pp1386","publicationYear":"1988","noYear":false,"title":"Satellite image atlas of glaciers of the world"},"lastModifiedDate":"2024-10-02T15:16:14.227884","indexId":"pp1386B","displayToPublicDate":"1995-02-01T00:00:00","publicationYear":"1988","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":"1386","chapter":"B","title":"Glaciers of Antarctica","docAbstract":"<p>Of all the world's continents Antarctica is the coldest, the highest, and the least known. It is one and a half times the size of the United States, and on it lies 91 percent (30,109,800 km<sup>3</sup>) of the estimated volume of all the ice on Earth. Because so little is known about Antarctic glaciers compared with what is known about glaciers in populated countries, satellite imagery represents a great leap forward in the provision of basic data. From the coast of Antarctica to about 81?south latitude, there are 2,514 Landsat nominal scene centers (the fixed geographic position of the intersection of orbital paths and latitudinal rows). If there were cloud-free images for all these geographic centers, only about 520 Landsat images would be needed to provide complete coverage. Because of cloud cover, however, only about 70 percent of the Landsat imaging area, or 55 percent of the continent, is covered by good quality Landsat images. To date, only about 20 percent of Antarctica has been mapped at scales of 1:250,000 or larger, but these maps do include about half of the coastline. The area of Antarctica that could be planimetrically mapped at a scale of 1:250,000 would be tripled if the available Landsat images were used in image map production. </p><p>This chapter contains brief descriptions and interpretations of features seen in 62 carefully selected Landsat images or image mosaics. Images were chosen on the basis of quality and interest; for this reason they are far from evenly spaced around the continent. Space limitations allow less than 15 percent of the Landsat imaging area of Antarctica to be shown in the illustrations reproduced in this chapter. Unfortunately, a wealth of glaciological and other features of compelling interest is present in the many hundreds of images that could not be included. To help show some important features beyond the limit of Landsat coverage, and as an aid to the interpretation of certain features seen in the images, 38 oblique aerial photographs have been included. Again, these represent only a small fraction of the large number of aerial photographs now available in various national collections. </p><p>The chapter is divided into five geographic sections. The first is the Transantarctic Mountains in the Ross Sea area. Some very large outlet glaciers flow from the East Antarctic ice sheet through the Transantarctic Mountains to the Ross Ice Shelf. Byrd Glacier, one of the largest in the world, drains an area of more than 1,000,000 km<sup>2</sup>. Next, images from the Indian Ocean sector are discussed. These include the Lambert Glacier- Amery Ice Shelf system, so large that about 25 images must be mosaicked to cover its complex system of tributary glaciers. Shirase Glacier, a tidal outlet glacier in the sector, flows at a speed of 2.5 km a<sup>-l</sup>. About 200 km inland and 200 km west of Shirase Glacier lie the Queen Fabiola (\"Yamato\") Mountains, whose extensive exposures of `blue ice' lay claim to being the world's most important meteorite-collecting locality, with more than 4,700 meteorite fragments discovered since 1969. </p><p>The Atlantic Ocean sector is fringed by ice shelves into which flow large ice streams like Jutulstraumen, Stancomb-Wills, Slessor, and Recovery Glaciers. Filchner and Ronne Ice Shelves together cover an area two-thirds the size of Texas. From the western margin of the Ronne Ice Shelf, the north-trending arc of the Antarctic Peninsula, with its fjord and alpine landscape and fringing ice shelves, stretches towards South America. The Pacific Ocean sector begins with the Ellsworth Mountains, which include the highest peaks (Vinson Massif at 4,897 m) in Antarctica. The area between the Ellsworth Mountains and the eastern margin of the Ross Ice Shelf is fringed with small ice shelves and some major outlet glaciers. One of these, Pine Island Glacier, was found from comparing 1973 and 1975 images to have an average ice-front velocity of 2.4 km a<sup>-1</sup>. This part of Antarctica contains many dormant volcanoes; the summits of servers, such as Mount Takahe with its 8-km-wide summit caldera, protrude through the West Antarctic ice sheet.&nbsp;</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Satellite image atlas of glaciers of the World (Professional Paper1386)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1386B","usgsCitation":"Swithinbank, C., Chinn, T.J., Williams, R.S., and Ferrigno, J.G., 1988, Glaciers of Antarctica (Version 1.0): U.S. Geological Survey Professional Paper 1386, Report: xi, 278 p.; 2 Plates: 30.00 x 24.00 inches and 35.00 x 26.00 inches, https://doi.org/10.3133/pp1386B.","productDescription":"Report: xi, 278 p.; 2 Plates: 30.00 x 24.00 inches and 35.00 x 26.00 inches","costCenters":[],"links":[{"id":122088,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp_1386_b.jpg"},{"id":3486,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/p1386b/","linkFileType":{"id":5,"text":"html"}}],"otherGeospatial":"Antarctica","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -179.9,\n              -60\n            ],\n            [\n              -179.9,\n              -90\n            ],\n            [\n             179.9,\n              -90\n            ],\n            [\n              179.9,\n              -60\n            ],\n            [\n              -179.9,\n              -60\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abee4b07f02db674ff3","contributors":{"editors":[{"text":"Williams, Richard S. Jr.","contributorId":17355,"corporation":false,"usgs":true,"family":"Williams","given":"Richard S.","suffix":"Jr.","affiliations":[],"preferred":false,"id":914634,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Ferrigno, Jane G. jferrign@usgs.gov","contributorId":39825,"corporation":false,"usgs":true,"family":"Ferrigno","given":"Jane","email":"jferrign@usgs.gov","middleInitial":"G.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":false,"id":914635,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Swithinbank, Charles","contributorId":60145,"corporation":false,"usgs":true,"family":"Swithinbank","given":"Charles","affiliations":[],"preferred":false,"id":914632,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chinn, Trevor J.","contributorId":344745,"corporation":false,"usgs":false,"family":"Chinn","given":"Trevor","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":914633,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williams, Richard S. Jr.","contributorId":19946,"corporation":false,"usgs":true,"family":"Williams","given":"Richard","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":219310,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ferrigno, Jane G. jferrign@usgs.gov","contributorId":39825,"corporation":false,"usgs":true,"family":"Ferrigno","given":"Jane","email":"jferrign@usgs.gov","middleInitial":"G.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":false,"id":219311,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":3186,"text":"wsp2325 - 1988 - National water summary 1986: Hydrologic events and ground-water quality","interactions":[],"lastModifiedDate":"2024-06-28T20:58:06.584628","indexId":"wsp2325","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1988","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":"2325","title":"National water summary 1986: Hydrologic events and ground-water quality","docAbstract":"<p>Ground water is one of the most important natural resources of the United States and degradation of its quality could have a major effect on the welfare of the Nation. Currently (1985), ground water is the source of drinking water for 53 percent of the Nation's population and for more than 97 percent of its rural population. It is the source of about 40 percent of the Nation's public water supply, 33 percent of water for irrigation, and 17 percent of freshwater for selfsupplied industries.</p><p>Ground water also is the source of about 40 percent of the average annual streamflow in the United States, although during long periods of little or no precipitation, ground-water discharges provide nearly all of the base streamflow. This hydraulic connection between aquifers and streams implies that if a persistent pollutant gets into an aquifer, it eventually could discharge into a stream.</p><p>Information presented in the 1986 National Water Summary clearly shows that the United States has very large amounts of potable ground water available for use. Although naturally occurring constituents, such as nitrate, and human-induced substances, such as synthetic organic chemicals, frequently are detected in ground water, their concentrations usually do not exceed existing Federal or State standards or guidelines for maximum concentrations in drinking water.</p><p>Troublesome contamination of ground water falls into two basic categories related to the source or sources of the contamination. Locally, high concentrations of a variety of toxic metals, organic chemicals, and petroleum products have been detected in ground water associated with point sources such as wastedisposal sites, storage-tank leaks, and hazardous chemical spills. These types of local problems commonly occur in densely populated urban areas and industrialized areas. Larger, multicounty areas also have been identified where contamination frequently is found in shallow wells. These areas generally are associated with broad-scale, or nonpoint, sources of contamination such as agricultural activities or highdensity domestic waste disposal (septic systems) in urban centers. At present, only a very small percentage of the total volume of potable ground water in the United States is contaminated from both point and nonpoint sources; however, available data, especially data about the occurrence of synthetic organic and toxic substances, generally are inadequate to determine the full extent of ground-water contamination in the Nation's aquifers or to define trends in groundwater quality. Most information about the occurrence of these substances has come from the study of individual sites or areas where contamination had already been detected or suspected.</p><p>Management and protection of ground water present a major challenge to the Nation. Current and projected costs of detection and cleanup of existing ground-water contamination are staggering and, even so, complete removal of pollutants from ground water in the vicinity of some waste sites might not be technically feasible. At all levels of government, the task of protecting the resource for its most beneficial uses is difficult and controversial.</p><p>Despite increasing awareness that some of the Nation's ground water is contaminated with a variety of toxic metals, synthetic organic chemicals, radionuclides, pesticides, and other contaminants that might present a long-term risk to human health, public policy towards ground-water protection is still in the formative stages. Despite increasing efforts devoted to ground-water protection by State and Federal regulatory and resource-management agencies, the extent of ground-water contamination is likely to appear to increase over the next few years because more agencies will be searching for evidence of contamination, and they will be using increasingly sensitive analytical procedures. Increased technology and expanded monitoring activities probably will detect the effects of past contamination and land uses on water quality. The significant time lag between a waterquality change in one part of an aquifer system and the effects of that change at a downgradient site, such as a well, results from the generally slow movement of ground water. This lag between cause and observed effect needs to be considered in evaluating the effectiveness of current and future ground-water policies and remedial measures.</p><p>Conclusive answers to questions about the location, extent, and severity of ground-water contamination, and about trends in ground-water quality, must await further collection and analysis of data from the Nation's aquifers. Generalizations, however, can be made, and the 1986 National Water Summary, which describes the natural quality of ground-water resources in each State and the major contamination problems that have been identified as of 1986, provides a national perspective of the ground-water-quality situation.</p><p>The 1986 <i>National Water Summary</i> follows the format of previous volumes. 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,{"id":14593,"text":"ofr88182 - 1988 - Selected ground-water information for the Columbia Plateau Regional Aquifer System, Washington and Oregon, 1982-1985; Volume I. Geohydrology","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr88182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-182","title":"Selected ground-water information for the Columbia Plateau Regional Aquifer System, Washington and Oregon, 1982-1985; Volume I. Geohydrology","docAbstract":"This data report presents groundwater information collected and analyzed as part of the U.S. Geological Survey 's Columbia Plateau Regional Aquifer System Analysis study. The information was gathered from July 1982 through September 1985 in the part of the aquifer system in central and eastern Washington, and north-central and eastern Oregon. The report consists of three volumes: volume I, geohydrology; volume II, water levels; and volume III, groundwater quality. (See also W89-02573) (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88182","usgsCitation":"Lane, R.C., 1988, Selected ground-water information for the Columbia Plateau Regional Aquifer System, Washington and Oregon, 1982-1985; Volume I. Geohydrology: U.S. Geological Survey Open-File Report 88-182, iii, 236 p. ill., map ;28 cm., https://doi.org/10.3133/ofr88182.","productDescription":"iii, 236 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":148211,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0182/report-thumb.jpg"},{"id":43260,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0182/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa2d1","contributors":{"authors":[{"text":"Lane, R. C.","contributorId":6421,"corporation":false,"usgs":true,"family":"Lane","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":169708,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13608,"text":"ofr88499 - 1988 - Hydrologic data for the Salt Bayou estuary near Sabine Pass, Texas, October 1984 to March 1986","interactions":[],"lastModifiedDate":"2016-08-12T15:25:33","indexId":"ofr88499","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-499","title":"Hydrologic data for the Salt Bayou estuary near Sabine Pass, Texas, October 1984 to March 1986","docAbstract":"<p>The Salt Bayou estuary, located in extreme southeast Texas near Sabine Pass, has been altered by construction of the Gulf Intracoastal Waterway. The waterway has interrupted the historical saltwater-freshwater exchange in this important estuary. This alteration may have had a detrimental effect on fish production because of increased salinity, and on waterfowl production because of lower water levels.</p>\n<p>There have been proposals to develop water control structures in the major channels that would enable some regulation of the saltwater in order to restore the estuary to its approximate historic state. A cooperative effort was initiated by the Louisiana Cooperative Fish and Wildlife Research Unit, the U.S. Fish and Wildlife Service, the Texas Parks and Wildlife Department, and the U.S. Geological Survey to identify the fish species and their transport mechanisms. The U.S. Geological Survey's part of this effort was to describe the present hydrology of Salt Bayou.</p>\n<p>The purpose of this report is to present the hydrologic data that were collected during October 1984 through March 1986. The initial data-collection network consisted of stage gages at Keith Lake Pass, the mouth of Salt Bayou, Ten Mile Cut, the Intracoastal Waterway, and Star Lake. A stage gage at the Alligator Bayou pumping plant became available later in the study. After 6 months of data were collected, the Ten Mile Cut gage was moved to Wildcow Bayou. The gages at Keith Lake Pass, the mouth of Salt Bayou, Ten Mile Cut, and Wildcow Bayou were equipped with water-velocity recording equipment. The Keith Lake Pass gage also had temperature and specific-conductance recording equipment.</p>\n<p>Six 24-hour flow investigations were performed to calibrate the velocity recording equipment and to determine the flow at ungaged sites. Before and after these investigations, specific conductance was measured at 43 sites within the estuary.</p>\n<p>Precipitation data were obtained from National Oceanic and Atmospheric Administration stations at Port Arthur, Anahuac, and Sea Rim State Park and were used to estimate the contribution of freshwater from rainfall. Evaporation data were obtained from Beaumont Research Station and were used to make estimates of water consumption from evapotranspiration. Wind speed and direction were obtained from the National Oceanic and Atmospheric Administration weather station at Sea Rim State Park.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr88499","usgsCitation":"Fisher, J., 1988, Hydrologic data for the Salt Bayou estuary near Sabine Pass, Texas, October 1984 to March 1986: U.S. Geological Survey Open-File Report 88-499, v, 128 p., https://doi.org/10.3133/ofr88499.","productDescription":"v, 128 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":42125,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0499/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147613,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0499/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db6085e4","contributors":{"authors":[{"text":"Fisher, J.C.","contributorId":99974,"corporation":false,"usgs":true,"family":"Fisher","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":168101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14872,"text":"ofr88681 - 1988 - Catalog of heat-flow and other pertinent data for the eastern United States and selected adjacent areas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr88681","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-681","title":"Catalog of heat-flow and other pertinent data for the eastern United States and selected adjacent areas","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88681","usgsCitation":"McCartan, L., and Architzel, R.J., 1988, Catalog of heat-flow and other pertinent data for the eastern United States and selected adjacent areas: U.S. Geological Survey Open-File Report 88-681, 5 p.  ;28 cm.; also in ASCII on IBM-compatible diskette; supplement to MF-2057, https://doi.org/10.3133/ofr88681.","productDescription":"5 p.  ;28 cm.; also in ASCII on IBM-compatible diskette; supplement to MF-2057","costCenters":[],"links":[{"id":147100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0681/report-thumb.jpg"},{"id":43681,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0681/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef8c3","contributors":{"authors":[{"text":"McCartan, Lucy","contributorId":87960,"corporation":false,"usgs":true,"family":"McCartan","given":"Lucy","affiliations":[],"preferred":false,"id":170158,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Architzel, Rebecca J.","contributorId":107706,"corporation":false,"usgs":true,"family":"Architzel","given":"Rebecca","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":170159,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13394,"text":"ofr88654 - 1988 - Pliocene planktonic foraminifer census data from Deep Sea Drilling Project holes 366A, 410, 606, and 646B","interactions":[],"lastModifiedDate":"2012-02-02T00:06:42","indexId":"ofr88654","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-654","title":"Pliocene planktonic foraminifer census data from Deep Sea Drilling Project holes 366A, 410, 606, and 646B","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88654","usgsCitation":"Dowsett, H.J., Gosnell, L.B., and Poore, R.Z., 1988, Pliocene planktonic foraminifer census data from Deep Sea Drilling Project holes 366A, 410, 606, and 646B: U.S. Geological Survey Open-File Report 88-654, 14 p. ill. ;28 cm., https://doi.org/10.3133/ofr88654.","productDescription":"14 p. ill. ;28 cm.","costCenters":[],"links":[{"id":145459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0654/report-thumb.jpg"},{"id":41826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0654/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684d8f","contributors":{"authors":[{"text":"Dowsett, Harry J. 0000-0003-1983-7524 hdowsett@usgs.gov","orcid":"https://orcid.org/0000-0003-1983-7524","contributorId":949,"corporation":false,"usgs":true,"family":"Dowsett","given":"Harry","email":"hdowsett@usgs.gov","middleInitial":"J.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":167739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gosnell, Linda B.","contributorId":106909,"corporation":false,"usgs":true,"family":"Gosnell","given":"Linda","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":167740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poore, Richard Z. rpoore@usgs.gov","contributorId":345,"corporation":false,"usgs":true,"family":"Poore","given":"Richard","email":"rpoore@usgs.gov","middleInitial":"Z.","affiliations":[{"id":574,"text":"St. Petersburg Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":167738,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14238,"text":"ofr8887 - 1988 - Ground-water data for Michigan 1986","interactions":[],"lastModifiedDate":"2016-12-29T10:47:08","indexId":"ofr8887","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-87","title":"Ground-water data for Michigan 1986","docAbstract":"<p>Water levels, locations, depths, and aquifers tapped are given for 112 observation wells. Tabulated data include extremes of water levels for calendar year 1986 and for the period of record, pumpage of most major groundwater users in the State, and water-quality data from selected wells. The largest reported user of ground-water, the city of Lansing, pumped 7.6 billion gallons from the Saginaw Formation and glacial deposits in 1986. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr8887","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources","usgsCitation":"Huffman, G., 1988, Ground-water data for Michigan 1986: U.S. Geological Survey Open-File Report 88-87, iv, 52 p., https://doi.org/10.3133/ofr8887.","productDescription":"iv, 52 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":42917,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0087/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144372,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0087/report-thumb.jpg"}],"country":"United 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,{"id":27872,"text":"wri874170 - 1988 - Techniques for estimating the magnitude and frequency of floods in Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T12:16:00","indexId":"wri874170","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4170","title":"Techniques for estimating the magnitude and frequency of floods in Minnesota","docAbstract":"<p>Log-Pearson type III flood-frequency analyses were made of annual series peak-flow records from 246 gaging stations on unregulated streams in Minnesota having watersheds ranging in area from 0.08 to 2,520 square miles. These flood discharges were related to watershed and climatic characteristics by using multiple-regression techniques. On the basis of this preliminary regression analysis of the frequency-analysis results, the data from these stations were grouped into four hydrologically distinct regions for the State. Regression analyses were performed on data from each region relating the 2-, 5-, 10-, 25-, 50-, and 100-year recurrence interval flood discharges to basin characteristics. The resulting regression equations, which may be used to estimate flood flows at ungaged sites, relate basin characteristics (contributing drainage area, main-channel slope, percent of basin covered by water, percent of basin covered by lakes, and mean annual runoff) to estimated flood flows. Different basin characteristics are significant for each of the four regions. Drainage area was found to be most significant and is included in all regional equations. Standard errors of estimate of the regression equations ranged from 33 to 60 percent.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri874170","collaboration":"Prepared in cooperation with the Minnesota Department of Transportation","usgsCitation":"Jacques, J., and Lorenz, D., 1988, Techniques for estimating the magnitude and frequency of floods in Minnesota: U.S. Geological Survey Water-Resources Investigations Report 87-4170, iv, 48 p., https://doi.org/10.3133/wri874170.","productDescription":"iv, 48 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":56696,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4170/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158983,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4170/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685bf8","contributors":{"authors":[{"text":"Jacques, J.E.","contributorId":79929,"corporation":false,"usgs":true,"family":"Jacques","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":198822,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lorenz, D. 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,{"id":55211,"text":"wdrIA871 - 1988 - Water resources data Iowa, water year 1987","interactions":[],"lastModifiedDate":"2016-03-09T12:22:54","indexId":"wdrIA871","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"IA-87-1","title":"Water resources data Iowa, water year 1987","docAbstract":"<p>Water resources data for the 1987 water year for Iowa consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; ground water levels and water quality of ground-water wells. This report contains records of water discharge for 112 stream-gaging stations; stage or j contents for 8 lakes and reservoirs; water quality for 8 stream-gaging stations; sediment! records for 10 stream-gaging stations; water levels for 112 observation wells; and chemical analyses for 197 municipal wells. Also included are 113 crest-stage partial record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements and analyses. These data represent that part of the National Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Iowa.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/wdrIA871","collaboration":"Prepared in cooperation with the Iowa Department of Natural Resources (Geological Survey Bureau), Iowa Department of Transportation and with Federal agencies","usgsCitation":"Melcher, N., Baebenroth, R., Detroy, M., Karsten, R., and Matthes, W., 1988, Water resources data Iowa, water year 1987: U.S. Geological Survey Water Data Report IA-87-1, xv, 345 p., https://doi.org/10.3133/wdrIA871.","productDescription":"xv, 345 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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,{"id":55227,"text":"wdrME881 - 1988 - Water resources data, Maine, water year 1988","interactions":[],"lastModifiedDate":"2025-08-18T16:27:56.776624","indexId":"wdrME881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"ME-88-1","title":"Water resources data, Maine, water year 1988","docAbstract":"<p>The Water Resources Division of the U.S. Geological Survey, in cooperation with State, Federal, and other local governmental agencies, obtains a large amount of data pertaining to the water resources of Maine each water year. These data, accumulated during many water years, constitute a valuable data base for developing animproved understanding of the water resources of the State.</p><p>Water resources data for the 1987 water year for Maine consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of ground-water wells. This report contains discharge records for 51 gaging stations; stage only for 2 gaging stations; contents for 17 lakes and reservoirs; water quality for 12 gaging stations; and water-levels for 31 ground-water wells. Additional water data were collected at other sites, not part of the systematic data collection program, and are published as miscellaneous measurements.</p>","language":"English","publisher":"U.S Geological Survey","doi":"10.3133/wdrME881","collaboration":"Prepared in cooperation with the State of Maine and other agencies","usgsCitation":"Bartlett, W., Higgins, W., and Nichols, W., 1988, Water resources data, Maine, water year 1988: U.S. Geological Survey Water Data Report ME-88-1, vii, 183 p., https://doi.org/10.3133/wdrME881.","productDescription":"vii, 183 p.","costCenters":[],"links":[{"id":494260,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1988/me-88-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174493,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1988/me-88-1/report-thumb.jpg"}],"country":"United 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,{"id":14594,"text":"ofr88183 - 1988 - Selected ground-water information for the Columbia Plateau Regional Aquifer System, Washington and Oregon, 1982-1985; Volume II. Water levels","interactions":[],"lastModifiedDate":"2012-02-02T00:06:59","indexId":"ofr88183","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-183","title":"Selected ground-water information for the Columbia Plateau Regional Aquifer System, Washington and Oregon, 1982-1985; Volume II. Water levels","docAbstract":"This data report presents groundwater information collected and analyzed as part of the U.S. Geological Survey 's Columbia Plateau Regional Aquifer System Analysis study. The information was gathered from July 1982 through September 1985 in the part of the aquifer system in central and eastern Washington, and north-central and eastern Oregon. The report consists of three volumes: volume I, geohydrology; volume II, water levels; and volume III, groundwater quality. (See also W89-02572) (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88183","usgsCitation":"Lane, R.C., 1988, Selected ground-water information for the Columbia Plateau Regional Aquifer System, Washington and Oregon, 1982-1985; Volume II. Water levels: U.S. Geological Survey Open-File Report 88-183, iii, 136 p. ill., map ;28 cm., https://doi.org/10.3133/ofr88183.","productDescription":"iii, 136 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":148234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0183/report-thumb.jpg"},{"id":43261,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0183/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa3a8","contributors":{"authors":[{"text":"Lane, R. C.","contributorId":6421,"corporation":false,"usgs":true,"family":"Lane","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":169709,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":12890,"text":"ofr88241 - 1988 - Processed strong-motion data for the El Salvador earthquake of June 19, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:54","indexId":"ofr88241","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-241","title":"Processed strong-motion data for the El Salvador earthquake of June 19, 1982","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr88241","usgsCitation":"Campbell, K.W., and Algermissen, S.T., 1988, Processed strong-motion data for the El Salvador earthquake of June 19, 1982: U.S. Geological Survey Open-File Report 88-241, 32 p. ill ;28 cm., https://doi.org/10.3133/ofr88241.","productDescription":"32 p. ill ;28 cm.","costCenters":[],"links":[{"id":147315,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0241/report-thumb.jpg"},{"id":41304,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0241/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ce4b07f02db65e788","contributors":{"authors":[{"text":"Campbell, Kenneth W.","contributorId":74391,"corporation":false,"usgs":false,"family":"Campbell","given":"Kenneth","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":166901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Algermissen, Sylvester Theodore","contributorId":94300,"corporation":false,"usgs":true,"family":"Algermissen","given":"Sylvester","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":166902,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18080,"text":"ofr88691 - 1988 - Geologic map of the northwestern Caliente Range, San Luis Obispo County, California","interactions":[],"lastModifiedDate":"2018-11-21T10:55:29","indexId":"ofr88691","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-691","title":"Geologic map of the northwestern Caliente Range, San Luis Obispo County, California","docAbstract":"<p>The map area lies in the southern Coast Ranges of California, north of the Transverse Ranges and west of the southern San Joaquin Valley. This region is part of the Salinia-Tujunga composite terrane that is bounded on the northeast by the San Andreas fault (fig. 1) and on the southwest by the Nacimiento fault zone (Vedder and others, 1983). The Chimineas fault of this map is inferred to be the boundary between the Salinia and the Tujunga terranes (Ross, 1972; Vedder and others, 1983).</p><p>Geologic mapping in the region of the California Coast Ranges that includes the area of this map has been largely the work of T.W. Dibblee, Jr. Compilations of geologic mapping at a scale of 1:125,000 (Dibblee, 1962, 1973a) provide the regional setting for this map, the northeast border of which lies about 6 to 7 km southwest of the San Andreas fault. Ross (1972) mapped the crystalline basement rocks in the vicinity of Barrett Creek, along the northeast side of the Chimineas fault (\"Barrett Ridge\" of Ross, 1972). Recent 1:24,000-scale mapping in the La Panza Range (fig. 1) (Vedder and others 1986a,b) overlaps onto the southwest edge of this map and provides useful information about the older rocks, mostly southwest of San Juan Creek.</p><p>Stratigraphic knowledge of the area, which lies in the northern part of the middle Tertiary Cuyama basin, has evolved over a period of years beginning with the molluscan biostratigraphic work of Anderson and Martin (1914) and Loel and Corey (1932). Hill and others (1958) described the Tertiary stratigraphy of the region and proposed stratigraphic names. This stratigraphy was discussed further by Dibblee (1973b), and his revised nomenclature is used here. Stratigraphic studies in the southeastern Caliente Range (fig. 1) (Repenning and Vedder, 1961; Vedder, 1973) provided valuable information on the interrelations of continental, shallow-marine, and deeper marine facies in the southern part of the Cuyama basin, which have basinwide application. More recent stratigraphic studies by Lagoe (1984, 1985, 1987, 1988) further elaborate on aspects of Miocene basin history and paleogeography.</p><p>Contributions to the tectonic history of the area have been made by Schwade and others (1958), on the basis of oil exploration in the Cuyama Valley area (fig. 1) in the 1940's and 1950's; by Bartow (1974), as part of a regional stratigraphic study; by Ballance and others (1983), on the basis of a study of Oligocene and early Miocene sedimentation; and most recently by Davis and others (1988) and Yeats and others (1988), who utilized a variety of new data from seismic reflection and from stratigraphic and structural studies.</p><p>Field work for this map was done mostly in 1969-73 as part of a regional study of the Simmler and Vaqueros Formations (Bartow, 1974). Detailed field mapping was, therefore, concentrated on those units; other parts of the area were mapped by geologic reconnaissance and air-photo interpretation that were supplemented by data from published maps (Dibblee, 1973a; Vedder and others, 1986a,h). Mapping of the crystalline basement rocks at \"Barrett Ridge\" is from Ross (1972, plate 1). The structural style depicted in the accompanying cross sections favors the thrust belt concepts of Davis and others (1988) over the older interpretations of Dibblee (1962) or Cross (1962).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr88691","usgsCitation":"Bartow, J.A., 1988, Geologic map of the northwestern Caliente Range, San Luis Obispo County, California: U.S. Geological Survey Open-File Report 88-691, Report: 16 p.; 2 Plates: 46.94 x 25.69 inches and 41.64 x 24.24 inches, https://doi.org/10.3133/ofr88691.","productDescription":"Report: 16 p.; 2 Plates: 46.94 x 25.69 inches and 41.64 x 24.24 inches","costCenters":[],"links":[{"id":359634,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0691/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":359635,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0691/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0691/report-thumb.jpg"},{"id":359636,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1988/0691/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"36000","country":"United States","state":"California","county":"San Luis Obispo County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6889cc","contributors":{"authors":[{"text":"Bartow, J. Alan","contributorId":84373,"corporation":false,"usgs":true,"family":"Bartow","given":"J.","email":"","middleInitial":"Alan","affiliations":[],"preferred":false,"id":178508,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13400,"text":"ofr88642 - 1988 - Petrographic and chemical data for the Quien Sabe volcanic rocks in the Mariposa Peak Quadrangle, central Diablo Range, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:50","indexId":"ofr88642","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-642","title":"Petrographic and chemical data for the Quien Sabe volcanic rocks in the Mariposa Peak Quadrangle, central Diablo Range, California","language":"ENGLISH","publisher":"U.S Geological Survey,","doi":"10.3133/ofr88642","usgsCitation":"Drinkwater, J.L., Weigand, P., and Sorg, D.H., 1988, Petrographic and chemical data for the Quien Sabe volcanic rocks in the Mariposa Peak Quadrangle, central Diablo Range, California: U.S. Geological Survey Open-File Report 88-642, 32 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr88642.","productDescription":"32 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":145892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0642/report-thumb.jpg"},{"id":41830,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0642/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f32bf","contributors":{"authors":[{"text":"Drinkwater, J. L.","contributorId":27856,"corporation":false,"usgs":true,"family":"Drinkwater","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":167746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weigand, P.W.","contributorId":59807,"corporation":false,"usgs":true,"family":"Weigand","given":"P.W.","email":"","affiliations":[],"preferred":false,"id":167747,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sorg, D. H.","contributorId":63380,"corporation":false,"usgs":true,"family":"Sorg","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":167748,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14485,"text":"ofr88448 - 1988 - Seismic station data for Northern California and surrounding areas","interactions":[],"lastModifiedDate":"2012-02-02T00:07:04","indexId":"ofr88448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-448","title":"Seismic station data for Northern California and surrounding areas","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88448","usgsCitation":"Klein, F.W., Eaton, J.P., and Lester, F., 1988, Seismic station data for Northern California and surrounding areas: U.S. Geological Survey Open-File Report 88-448, 131 p. ;28 cm., https://doi.org/10.3133/ofr88448.","productDescription":"131 p. ;28 cm.","costCenters":[],"links":[{"id":148885,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0448/report-thumb.jpg"},{"id":43179,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0448/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb667","contributors":{"authors":[{"text":"Klein, F. W.","contributorId":88371,"corporation":false,"usgs":true,"family":"Klein","given":"F.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":169538,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eaton, J. P.","contributorId":105313,"corporation":false,"usgs":true,"family":"Eaton","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":169539,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lester, F.W.","contributorId":10767,"corporation":false,"usgs":true,"family":"Lester","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":169537,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":13797,"text":"ofr88174 - 1988 - The U.S. Geological Survey Federal-State cooperative water- resources program; fiscal year 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:06:49","indexId":"ofr88174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-174","title":"The U.S. Geological Survey Federal-State cooperative water- resources program; fiscal year 1987","docAbstract":"The U.S. Geological Survey 's Federal-State Cooperative Water Resources Program (50-50 matching of funds) started in Kansas in 1895. During fiscal year (FY) 1987, hydrologic data collection, investigations, and research are being conducted in every state, Puerto Rico, and several territories in cooperation with 940 state, regional and local agencies. Federal funding of $55.3 million was matched by cooperating agencies; cooperators also provided $4.6 million unmatched, for a program total of about $115 million. The Cooperative Program accounted for almost 45% of the FY 1987 obligations of the Geological Survey 's Water Resources Division. The principal areas of emphasis during the year included groundwater contamination, stream quality, water supply and demand, and hydrologic hazards. Information is presented on program functions and priorities. Data collection activities are also described as is work related to water resources contamination. Several examples of current (1987) investigations are provided. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88174","usgsCitation":"Gilbert, B., and Mann, W.B., 1988, The U.S. Geological Survey Federal-State cooperative water- resources program; fiscal year 1987: U.S. Geological Survey Open-File Report 88-174, v, 36 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr88174.","productDescription":"v, 36 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":146032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0174/report-thumb.jpg"},{"id":42367,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0174/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66c98e","contributors":{"authors":[{"text":"Gilbert, B.K.","contributorId":32167,"corporation":false,"usgs":true,"family":"Gilbert","given":"B.K.","email":"","affiliations":[],"preferred":false,"id":168409,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mann, William B. IV","contributorId":8838,"corporation":false,"usgs":true,"family":"Mann","given":"William","suffix":"IV","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":168408,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17204,"text":"ofr88323 - 1988 - Ground-water data for Georgia, 1987","interactions":[],"lastModifiedDate":"2024-12-17T19:39:52.774728","indexId":"ofr88323","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-323","title":"Ground-water data for Georgia, 1987","docAbstract":"This report was prepared in cooperation with the State of Georgia;  Chatham County; Glynn County; the cities of Brunswick and Valdosta; and  the Albany Water, Gas, and Light Commission. This report is the culmination of a concerted effort by dedicated  personnel of the U.S. Geological Survey who collected, compiled, analyzed, verified, and organized the data, and who edited and assembled the report. In addition to the authors, who had primary responsibility for assuring that the information contained herein is accurate, complete, and adheres to Geological Survey policy and established guidelines, the following individuals contributed significantly to the collection, processing, and tabulation of the data:","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Doraville, GA","doi":"10.3133/ofr88323","collaboration":"Prepared in cooperation with the Georgia Department OF Natural Resources Environmental Protection Division and the Georgia Geologic Survey","usgsCitation":"Joiner, C.N., Reynolds, M., Stayton, W., and Boucher, F., 1988, Ground-water data for Georgia, 1987: U.S. Geological Survey Open-File Report 88-323, xvi, 172 p., https://doi.org/10.3133/ofr88323.","productDescription":"xvi, 172 p.","additionalOnlineFiles":"N","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":279467,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0323/report.pdf"},{"id":149902,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0323/report-thumb.jpg"},{"id":465211,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17399.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Georgia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.61,30.36 ], [ -85.61,35.00 ], [ -80.75,35.00 ], [ -80.75,30.36 ], [ -85.61,30.36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cfa3","contributors":{"authors":[{"text":"Joiner, C. N.","contributorId":17615,"corporation":false,"usgs":true,"family":"Joiner","given":"C.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":175389,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, M.S.","contributorId":35338,"corporation":false,"usgs":true,"family":"Reynolds","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":175390,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stayton, W.L.","contributorId":65487,"corporation":false,"usgs":true,"family":"Stayton","given":"W.L.","affiliations":[],"preferred":false,"id":175392,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boucher, F.G.","contributorId":53821,"corporation":false,"usgs":true,"family":"Boucher","given":"F.G.","email":"","affiliations":[],"preferred":false,"id":175391,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":14518,"text":"ofr88255 - 1988 - Data report for the 1979 seismic-refraction experiment in the Imperial Valley Region, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr88255","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-255","title":"Data report for the 1979 seismic-refraction experiment in the Imperial Valley Region, California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr88255","usgsCitation":"Kohler, W., and Fuis, G., 1988, Data report for the 1979 seismic-refraction experiment in the Imperial Valley Region, California: U.S. Geological Survey Open-File Report 88-255, 96 p. :ill. ;28 cm., https://doi.org/10.3133/ofr88255.","productDescription":"96 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":146589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1988/0255/report-thumb.jpg"},{"id":43207,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1988/0255/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679dc2","contributors":{"authors":[{"text":"Kohler, W.M.","contributorId":62999,"corporation":false,"usgs":true,"family":"Kohler","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":169593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fuis, G. S.","contributorId":83131,"corporation":false,"usgs":true,"family":"Fuis","given":"G. S.","affiliations":[],"preferred":false,"id":169594,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13657,"text":"ofr88331 - 1988 - Annual maximum and minimum lake levels for Indiana, 1942-85","interactions":[],"lastModifiedDate":"2016-05-16T12:42:31","indexId":"ofr88331","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","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":"88-331","title":"Annual maximum and minimum lake levels for Indiana, 1942-85","docAbstract":"<p>Indiana has many natural and manmade lakes. Lake-level data are available for 217 lakes. These data were collected during water years 1942-85 by use of staff gages and, more recently, continuous recorders. The period of record at each site ranges from 1 to 43 years. Data from the lake stations have been compiled, and maximum and minimum lake levels for each year of record are reported. In addition to annual maximum and minimum lake levels, each lake station is described by gage location, surface area, drainage area, period of record, datum of gage, gage type, established legal level, lake level control, inlets and outlets, and extremes for the period of record.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey,","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr88331","usgsCitation":"Fowler, K.K., 1988, Annual maximum and minimum lake levels for Indiana, 1942-85: U.S. Geological Survey Open-File Report 88-331, iv, 363 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr88331.","productDescription":"iv, 363 p. ill., maps ;28 cm.","startPage":"1","endPage":"363","numberOfPages":"367","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science 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,{"id":28014,"text":"wri874283 - 1988 - Hydrogeology and water-supply potential of the water-table aquifer on Dauphin Island, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:08:38","indexId":"wri874283","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1988","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4283","title":"Hydrogeology and water-supply potential of the water-table aquifer on Dauphin Island, Alabama","docAbstract":"The water table aquifer on Dauphin Island, Alabama, consists of a thin veneer of Holocene sand and an underlying Pleistocene unit locally known as the Gulfport Formation. The aquifer is from 28 to 35 ft thick with a thick marine clay at its base. Water in the aquifer generally is low in chloride content except near the coast. Excessively high iron concentrations in groundwater were found locally. A two-dimensional finite-difference groundwater flow model of the water table aquifer on Dauphin Island was used in the steady-state mode to evaluate the flow system under steady-state conditions. Model input data were obtained primarily from 40 test wells, 2 aquifer tests, continuous recording of groundwater levels, and rainfall. The model was calibrated to the low water-table conditions of July 1985 and high water table conditions of April 1985. The model was also used to simulate pumpage from the aquifer under transient conditions with no rainfall. Patterns of computed head changes compared favorably to the natural recession of water levels for the periods of April to May 1985 and May to June 1985. Simulation of groundwater withdrawals in the transient model showed the feasibility of producing 0.6 million gallons/day from eight wells that tap the water table aquifer without inducing lateral seawater encroachment. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874283","usgsCitation":"Kidd, R.E., 1988, Hydrogeology and water-supply potential of the water-table aquifer on Dauphin Island, Alabama: U.S. Geological Survey Water-Resources Investigations Report 87-4283, vii, 49 p. :ill., (some col.), maps ;28 cm., https://doi.org/10.3133/wri874283.","productDescription":"vii, 49 p. :ill., (some col.), maps ;28 cm.","costCenters":[],"links":[{"id":120060,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4283/report-thumb.jpg"},{"id":56841,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4283/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ade77","contributors":{"authors":[{"text":"Kidd, R. E.","contributorId":91145,"corporation":false,"usgs":true,"family":"Kidd","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":199069,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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