{"pageNumber":"4758","pageRowStart":"118925","pageSize":"25","recordCount":165605,"records":[{"id":70168858,"text":"70168858 - 1983 - Earthquakes; November-December 1982","interactions":[],"lastModifiedDate":"2016-03-24T16:04:47","indexId":"70168858","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquakes; November-December 1982","docAbstract":"<p>The months of November and December were quite active, seismically speaking, compared to the preceding months. The most devastating earthquake of the year occurred in Yemen on December 13 and killed hundreds of people. the largest earthquake of the year, a magnitude 7.7, occurred in the Pacific Tonga Islands on December 19.&nbsp;</p>\n<p>Again, a number of earthquakes occurred in the United States, but only minor damage was reported.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1983, Earthquakes; November-December 1982: Earthquake Information Bulletin (USGS), v. 15, no. 3, p. 108-112.","productDescription":"5 p.","startPage":"108","endPage":"112","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318606,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfcfe4b015c306f84c62","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621994,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70168864,"text":"70168864 - 1983 - Earthquakes; May-June 1983","interactions":[],"lastModifiedDate":"2016-03-06T15:02:25","indexId":"70168864","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquakes; May-June 1983","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1983, Earthquakes; May-June 1983: Earthquake Information Bulletin (USGS), v. 15, no. 6, p. 233-235.","productDescription":"3 p.","startPage":"233","endPage":"235","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318612,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dd62c8e4b015c306fa4b9b","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":622017,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70140556,"text":"70140556 - 1983 - Synthesis of geophysical data with space-acquired imagery: a review","interactions":[],"lastModifiedDate":"2017-12-14T16:41:05","indexId":"70140556","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":661,"text":"Advances in Space Research","active":true,"publicationSubtype":{"id":10}},"title":"Synthesis of geophysical data with space-acquired imagery: a review","docAbstract":"<p>Geophysical data obtained from ground and airborne platforms have been used in the development of regional geologic models for many years. Space-acquired data and imagery have a shorter but similar history of applications. All these data may be synthesized either manually or digitally. Manual synthesis methods consist of overlaying and comparing maps, whereas digital synthesis methods consist of computer storage and analysis of registered digital data sets.</p>\n<p>A data base may include topographic, geologic, soils, aeromagnetic, gravity, radiometric, electromagnetic and geochemical data, and Landsat, Seasat, and Heat Capacity Mapping Mission (HCMM) images, all of which can be evaluated individually or compared in multiple layers (overlays).</p>\n<p>Stereographic models, useful in the correlation and interpretation of geophysical data, have been created from Landsat images by using aeromagnetic, gravity, geochemical, or topographic values to offset Landsat pixels, thus introducing parallax and permitting stereoscopic viewing.</p>\n<p>Statistical correlation has been used to determine the applicability of specific data sets to the development of geologic or exploration models. Various arithmetic functions have proven useful in developing models from such data sets.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0273-1177(83)90116-3","usgsCitation":"Hastings, D.A., 1983, Synthesis of geophysical data with space-acquired imagery: a review: Advances in Space Research, v. 3, no. 2, p. 157-168, https://doi.org/10.1016/0273-1177(83)90116-3.","productDescription":"12 p.","startPage":"157","endPage":"168","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":297837,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2c67e4b08de9379b379a","contributors":{"authors":[{"text":"Hastings, David A.","contributorId":138985,"corporation":false,"usgs":true,"family":"Hastings","given":"David","email":"","middleInitial":"A.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":540071,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30050,"text":"wri824100 - 1983 - Land application of wastewater and its effect on ground-water quality in the Livermore-Amador Valley, Alameda County, California","interactions":[],"lastModifiedDate":"2023-03-14T21:05:28.776892","indexId":"wri824100","displayToPublicDate":"1983-01-01T00:00:00","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":"82-4100","title":"Land application of wastewater and its effect on ground-water quality in the Livermore-Amador Valley, Alameda County, California","docAbstract":"<p>Ground-water quality, ground-water level, and rainfall data collected during the 1975 water year through the 1980 water year were analyzed to determine the effects of land application of effluent from wastewater treatment plants on ground-water quality in the Livermore-Amador Valley. Annual rainfall varied markedly during the study: 1976 and 1977 water years had less than one half the normal rainfall; 1978 and 1980 water years had greater than normal rainfall; and 1975 and 1979 water years had nearly normal rainfall. The direction ground-water movement in the valley was found to be generally that of surface water. Dissolved nitrate concentrations were generally much less in areas not receiving wastewater applications than in areas that do. Specific conductance, dissolved solids, dissolved chloride, and dissolved nitrate were substantially less in the lower aquifers than in the upper aquifer in the Livermore wastewater application areas. In the Castlewood, Pleasanton, Veterans Administration Hospital, and Livermore wastewater applications areas ground-water quality was similar to the quality of effluent from wastewater treatment plants in the valley. Rainfall, soil, and geology appeared to be the main determinants of ground-water quality in the Castlewood and Dublin-San Ramon and Camp Parks Military Reservation areas. Wastewater application appeared to be the main determinant of ground-water quality in Pleasanton, Veterans Administration Hospital, and Livermore Municipal Airport areas. Comparison of ground-water quality in wastewater application areas with proposed State water-quality objectives for ground water in the Livermore-Amador Valley showed impaired water quality in all areas.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824100","usgsCitation":"Sylvester, M.A., 1983, Land application of wastewater and its effect on ground-water quality in the Livermore-Amador Valley, Alameda County, California: U.S. Geological Survey Water-Resources Investigations Report 82-4100, Report: vi, 53 p.; 2 Plates: 41.37 x 40.76 inches and 42.24 x 40.61 inches, https://doi.org/10.3133/wri824100.","productDescription":"Report: vi, 53 p.; 2 Plates: 41.37 x 40.76 inches and 42.24 x 40.61 inches","costCenters":[],"links":[{"id":110155,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35608.htm","linkFileType":{"id":5,"text":"html"},"description":"35608"},{"id":58861,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4100/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58860,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4100/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58859,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4100/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124278,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4100/report-thumb.jpg"}],"country":"United States","state":"California","county":"Alameda County","otherGeospatial":"Livermore-Amador Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122,\n              37.5\n            ],\n            [\n              -121.625,\n              37.5\n            ],\n            [\n              -121.625,\n              37.8333\n            ],\n            [\n              -122,\n              37.8333\n            ],\n            [\n              -122,\n              37.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aeeaa","contributors":{"authors":[{"text":"Sylvester, M. A.","contributorId":10838,"corporation":false,"usgs":true,"family":"Sylvester","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":202595,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185337,"text":"70185337 - 1983 - An isolated population of small Canada geese on Kaliktagik Island, Alaska","interactions":[],"lastModifiedDate":"2017-03-20T15:06:20","indexId":"70185337","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3764,"text":"Wildfowl","onlineIssn":"2052-6458","printIssn":"0954-6324","active":true,"publicationSubtype":{"id":10}},"title":"An isolated population of small Canada geese on Kaliktagik Island, Alaska","docAbstract":"<p>Recently we discovered that a small form of the Canada Goose <i>Branta canadensis</i> breeds on Kaliktagik Island, one of the Semidi Islands, about 80 km south of the Alaska Peninsula near longitude 157°W (Figure 1). The unexpected occurrence of geese on this oceanic island and the possibility that they are closely allied with the endangered Aleutian race of Canada Geese <i>B. c. leucopareia</i> prompt this summary of observations made between 1977 and 1981, in the course of field studies on seabirds of the area. </p>","language":"English","publisher":"Wildfowl & Wetlands Trust","usgsCitation":"Hatch, S.A., and Hatch, M.A., 1983, An isolated population of small Canada geese on Kaliktagik Island, Alaska: Wildfowl, v. 34, p. 130-136.","productDescription":"7 p.","startPage":"130","endPage":"136","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337882,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":337881,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://wildfowl.wwt.org.uk/index.php/wildfowl/article/view/674"}],"country":"United States","state":"Alaska","otherGeospatial":"Kaliktagik Island, Semidi Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.6708755493164,\n              56.08295658599044\n            ],\n            [\n              -156.67259216308594,\n              56.077304816827684\n            ],\n            [\n              -156.6705322265625,\n              56.071460590574574\n            ],\n            [\n              -156.6573143005371,\n              56.0656154780254\n            ],\n            [\n              -156.6408348083496,\n              56.06551964912398\n            ],\n            [\n              -156.6317367553711,\n              56.067819477013636\n            ],\n            [\n              -156.6368865966797,\n              56.075388774724956\n            ],\n            [\n              -156.64752960205078,\n              56.081519774117034\n            ],\n            [\n              -156.6569709777832,\n              56.08448912626121\n            ],\n            [\n              -156.6708755493164,\n              56.08295658599044\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"34","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d0ea1fe4b0236b68f673b1","contributors":{"authors":[{"text":"Hatch, Scott A. 0000-0002-0064-8187 shatch@usgs.gov","orcid":"https://orcid.org/0000-0002-0064-8187","contributorId":2625,"corporation":false,"usgs":true,"family":"Hatch","given":"Scott","email":"shatch@usgs.gov","middleInitial":"A.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":685228,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatch, Martha A.","contributorId":181576,"corporation":false,"usgs":false,"family":"Hatch","given":"Martha","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":685229,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42071,"text":"ofr83137 - 1983 - Altitude of the top of the Matawan Group-Magothy Formation, Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2023-03-01T21:30:31.255374","indexId":"ofr83137","displayToPublicDate":"1983-01-01T00:00:00","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":"83-137","title":"Altitude of the top of the Matawan Group-Magothy Formation, Suffolk County, Long Island, New York","docAbstract":"<p>The Magothy aquifer, with its irregular surface and deeply eroded buried valleys, has become the major source of fresh water in most of Suffolk Country. With the availability of recent data from deep wells and test holes, refinement of the surface-altitude contours has been possible and resulted in substantial revision in some areas. This 1-sheet map delineates the surface altitude of the Magothy aquifer (Matawan Group-Magothy Formation) and includes a brief text and bibliography.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83137","usgsCitation":"Krulikas, R.K., Koszalka, E., and Doriski, T.P., 1983, Altitude of the top of the Matawan Group-Magothy Formation, Suffolk County, Long Island, New York: U.S. Geological Survey Open-File Report 83-137, 1 Plate: 47.05 x 25.51 inches, https://doi.org/10.3133/ofr83137.","productDescription":"1 Plate: 47.05 x 25.51 inches","costCenters":[],"links":[{"id":135569,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79820,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0137/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413560,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13907.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New York","county":"Suffolk County","otherGeospatial":"Long Island, Matawan Group-Magothy Formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.5,\n              41.167\n            ],\n            [\n              -73.5,\n              40.6\n            ],\n            [\n              -71.917,\n              40.6\n            ],\n            [\n              -71.917,\n              41.167\n            ],\n            [\n              -73.5,\n              41.167\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686a7b","contributors":{"authors":[{"text":"Krulikas, Richard K.","contributorId":36910,"corporation":false,"usgs":true,"family":"Krulikas","given":"Richard","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":225905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koszalka, E. J.","contributorId":28949,"corporation":false,"usgs":true,"family":"Koszalka","given":"E. J.","affiliations":[],"preferred":false,"id":225904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doriski, Thomas P.","contributorId":20301,"corporation":false,"usgs":true,"family":"Doriski","given":"Thomas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":225903,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70168593,"text":"70168593 - 1983 - Krakatau 1883","interactions":[],"lastModifiedDate":"2019-11-14T08:26:18","indexId":"70168593","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Krakatau 1883","docAbstract":"<p>This year marks the 100th anniversary of the eruption of Krakatau, perhaps the most famous volcanic event in recorded history. During a 23-hour period on August 26 and 17, 1883, more than 4 cubic miles of volcanic debris exploded upward from Krakatau, resulting in the death of more than 36,000 people and producing catastrophic devastation. The 1883 events at Krakatau caused phenomena that were recorded around the world that lingered for several years after the main eruption. &nbsp;</p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Simkin, T., and Fiske, R., 1983, Krakatau 1883: Earthquake Information Bulletin (USGS), v. 15, no. 4, p. 128-133.","productDescription":"6 p.","startPage":"128","endPage":"133","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318211,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Indonesia","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[120.71561,-10.23958],[120.29501,-10.25865],[118.96781,-9.55797],[119.90031,-9.36134],[120.42576,-9.66592],[120.7755,-9.96968],[120.71561,-10.23958]]],[[[124.43595,-10.14],[123.57998,-10.35999],[123.45999,-10.23999],[123.55001,-9.90002],[123.98001,-9.29003],[124.96868,-8.89279],[125.07002,-9.08999],[125.08852,-9.39317],[124.43595,-10.14]]],[[[117.90002,-8.09568],[118.26062,-8.36238],[118.87846,-8.28068],[119.12651,-8.70582],[117.9704,-8.90664],[117.27773,-9.04089],[116.74014,-9.03294],[117.08374,-8.45716],[117.63202,-8.4493],[117.90002,-8.09568]]],[[[122.90354,-8.09423],[122.75698,-8.64981],[121.25449,-8.93367],[119.92439,-8.81042],[119.92093,-8.44486],[120.71509,-8.23696],[121.34167,-8.53674],[122.00736,-8.46062],[122.90354,-8.09423]]],[[[108.62348,-6.77767],[110.53923,-6.87736],[110.75958,-6.46519],[112.61481,-6.94604],[112.97877,-7.59421],[114.47894,-7.77653],[115.70553,-8.37081],[114.56451,-8.75182],[113.46473,-8.34895],[112.55967,-8.37618],[111.52206,-8.30213],[110.58615,-8.1226],[109.42767,-7.74066],[108.69366,-7.6416],[108.27776,-7.76666],[106.4541,-7.3549],[106.28062,-6.9249],[105.36549,-6.85142],[106.05165,-5.89592],[107.26501,-5.95499],[108.07209,-6.34576],[108.48685,-6.42198],[108.62348,-6.77767]]],[[[134.72462,-6.2144],[134.21013,-6.89524],[134.11278,-6.14247],[134.29034,-5.78306],[134.49963,-5.44504],[134.727,-5.73758],[134.72462,-6.2144]]],[[[127.24922,-3.45907],[126.87492,-3.79098],[126.1838,-3.60738],[125.98903,-3.17727],[127.00065,-3.12932],[127.24922,-3.45907]]],[[[130.47134,-3.09376],[130.83484,-3.85847],[129.99055,-3.4463],[129.15525,-3.36264],[128.59068,-3.42868],[127.89889,-3.39344],[128.13588,-2.84365],[129.371,-2.80215],[130.47134,-3.09376]]],[[[134.14337,-1.15187],[134.42263,-2.76918],[135.4576,-3.36775],[136.29331,-2.30704],[137.44074,-1.70351],[138.32973,-1.70269],[139.18492,-2.0513],[139.92668,-2.40905],[141.00021,-2.60015],[141.01706,-5.85902],[141.03385,-9.11789],[140.14342,-8.29717],[139.12777,-8.09604],[138.88148,-8.38094],[137.61447,-8.41168],[138.0391,-7.59788],[138.66862,-7.32022],[138.40791,-6.23285],[137.92784,-5.39337],[135.98925,-4.54654],[135.1646,-4.46293],[133.66288,-3.53885],[133.3677,-4.02482],[132.98396,-4.11298],[132.75694,-3.74628],[132.75379,-3.31179],[131.9898,-2.82055],[133.06684,-2.46042],[133.78003,-2.47985],[133.69621,-2.21454],[132.23237,-2.21253],[131.83622,-1.61716],[130.94284,-1.43252],[130.51956,-0.93772],[131.86754,-0.69546],[132.38012,-0.36954],[133.98555,-0.78021],[134.14337,-1.15187]]],[[[125.2405,1.41984],[124.43704,0.42788],[123.6855,0.23559],[122.72308,0.43114],[121.05672,0.38122],[120.18308,0.23725],[120.04087,-0.51966],[120.93591,-1.40891],[121.47582,-0.95596],[123.34056,-0.61567],[123.2584,-1.07621],[122.82272,-0.93095],[122.38853,-1.51686],[121.50827,-1.90448],[122.45457,-3.18606],[122.2719,-3.5295],[123.17096,-4.68369],[123.16233,-5.3406],[122.62852,-5.63459],[122.23639,-5.28293],[122.71957,-4.46417],[121.73823,-4.85133],[121.48946,-4.57455],[121.61917,-4.18848],[120.89818,-3.60211],[120.97239,-2.62764],[120.30545,-2.9316],[120.39005,-4.09758],[120.43072,-5.52824],[119.79654,-5.6734],[119.36691,-5.37988],[119.65361,-4.45942],[119.49884,-3.49441],[119.07834,-3.48702],[118.76777,-2.802],[119.18097,-2.1471],[119.32339,-1.35315],[119.826,0.15425],[120.0357,0.56648],[120.88578,1.30922],[121.66682,1.01394],[122.92757,0.87519],[124.07752,0.9171],[125.06599,1.64326],[125.2405,1.41984]]],[[[128.68825,1.13239],[128.63595,0.25849],[128.12017,0.35641],[127.96803,-0.25208],[128.38,-0.78],[128.10002,-0.9],[127.69647,-0.2666],[127.39949,1.01172],[127.60051,1.81069],[127.93238,2.1746],[128.00416,1.62853],[128.59456,1.54081],[128.68825,1.13239]]],[[[117.87563,1.82764],[118.99675,0.90222],[117.81186,0.78424],[117.47834,0.10247],[117.52164,-0.80372],[116.56005,-1.48766],[116.5338,-2.48352],[116.14808,-4.01273],[116.00086,-3.65704],[114.8648,-4.10698],[114.46865,-3.4957],[113.75567,-3.43917],[113.25699,-3.11878],[112.06813,-3.47839],[111.70329,-2.99444],[111.04824,-3.04943],[110.22385,-2.93403],[110.07094,-1.59287],[109.57195,-1.31491],[109.09187,-0.45951],[108.95266,0.41538],[109.06914,1.34193],[109.66326,2.00647],[109.83023,1.33814],[110.51406,0.77313],[111.15914,0.97648],[111.79755,0.90444],[112.38025,1.41012],[112.85981,1.49779],[113.80585,1.21755],[114.62136,1.43069],[115.13404,2.82148],[115.51908,3.16924],[115.86552,4.30656],[117.01521,4.30609],[117.88203,4.13755],[117.31323,3.23443],[118.04833,2.28769],[117.87563,1.82764]]],[[[105.81766,-5.85236],[104.71038,-5.87328],[103.86821,-5.03731],[102.58426,-4.22026],[102.15617,-3.61415],[101.39911,-2.79978],[100.9025,-2.05026],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T.","contributorId":45833,"corporation":false,"usgs":true,"family":"Simkin","given":"T.","email":"","affiliations":[],"preferred":false,"id":620994,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fiske, R.S.","contributorId":47783,"corporation":false,"usgs":true,"family":"Fiske","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":620995,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011400,"text":"70011400 - 1983 - Human interactions with ground-water","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70011400","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1746,"text":"GeoJournal","active":true,"publicationSubtype":{"id":10}},"title":"Human interactions with ground-water","docAbstract":"Ground-Water could be considered as an immense reservoir, from which only a certain amount of water can be withdrawn without affecting the quantity and quality of water. This amount is determined by the characteristics of the environment in which ground-water occurs and by the interactions of ground-water with precipitation, surface water, and people. It should be recognized that quantity and quality of ground-water are intimately related and should be considered accordingly. Quantity refers to usable water and water is usable for any specific purpose only so long as its quality has not deteriorated beyond acceptable limits. Thus an overall quantitative and qualitative management of ground water is inevitable, and its should also involve the uses of ground-water reservoirs for purposes other than water supply. The main objective of ground-water management is to ensure that ground-water resources will be available in appropriate time and in appropriate quantity and quality to meet the most important demands of our society. Traditional, and obvious uses of ground-water are the extraction of water for water supplies (domestic, municipal, agricultural, and industrial) and the natural discharge feeding lakes and maintaining base flow of streams. Not so obvious are the uses of ground-water reservoirs, the very framework within which ground-water occurs and moves, and in which other fluids or materials can be stored. In the last two decades, ground-water reservoirs have been intensively considered for many other purposes than water supplies. Diversified and very often conflicting uses need to be evaluated and dealt with in the most efficient way in order to determine the importance of each possible use, and to assign priorities of these uses. With rising competition for the use of ground-water reservoirs, we will also need to increase the potential for effective planning of ground-water development and protection. Man's development and use of ground-water necessarily modifies the natural conditions and the total natural system must be successfully blended with the unnatural stresses placed upon it. This can be accomplished by introducing new methods (such as ground-water zoning) in and by developing alternative strategies for ground-water management and protection. ?? 1983 D. Reidel Publishing Company.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"GeoJournal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00194489","issn":"03432521","usgsCitation":"Zaporozec, A., 1983, Human interactions with ground-water: GeoJournal, v. 7, no. 5, p. 427-433, https://doi.org/10.1007/BF00194489.","startPage":"427","endPage":"433","numberOfPages":"7","costCenters":[],"links":[{"id":205139,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00194489"},{"id":221751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3281e4b0c8380cd5e868","contributors":{"authors":[{"text":"Zaporozec, A.","contributorId":24093,"corporation":false,"usgs":true,"family":"Zaporozec","given":"A.","email":"","affiliations":[],"preferred":false,"id":361007,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011395,"text":"70011395 - 1983 - Petrology and comparative thermal and mechanical histories of clasts in breccia 62236","interactions":[],"lastModifiedDate":"2024-06-28T16:31:21.086666","indexId":"70011395","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Petrology and comparative thermal and mechanical histories of clasts in breccia 62236","docAbstract":"<p><span>Lunar breccia 62236 contains large lithic fragments of troctolite, norite, and anorthosite. The mafic phases, olivine, inverted pigeonite, and augite, fill interstitial areas between larger plagioclases and appear to be cumulate phases with extensive adcumulus growth. Pyroxene compositional homogeneity indicates that cation exchange during cooling was limited to an area of about 1 mm. Primary augite and pigeonite both contain 30 μm-wide lamellae of the other along ‘001’. Pigeonite inverted to orthopyroxene without retaining any crystallographic orientation and subsequently exsolved fine lamellae of augite on (100). Profiles across orthopyroxene-augite interfaces obtained in the analytical transmission electron microscope show an increase of ∼5% wollastonite in augite within 0.5 μm of the interface, suggesting that short-range cation exchange continued to temperatures below 500°C. The entire sample has undergone heterogeneous shock deformation. Shock melting of the troctolitic clast suggests pressures of 200–300 kb and well-developed basal twinning in augite from the norite clasts suggests pressures of 50–300 kbars. The present evidence indicates that 62236 contains parts of a slowly cooled microlayered adcumulate that has been heterogeneously shocked several times and combined into the present breccia.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB088iS02p0A645","issn":"01480227","usgsCitation":"Nord, G.L., and Wandless, M., 1983, Petrology and comparative thermal and mechanical histories of clasts in breccia 62236: Journal of Geophysical Research Solid Earth, v. 88, no. S02, p. A645-A657, https://doi.org/10.1029/JB088iS02p0A645.","productDescription":"13 p.","startPage":"A645","endPage":"A657","costCenters":[],"links":[{"id":221663,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"S02","noUsgsAuthors":false,"publicationDate":"2012-09-21","publicationStatus":"PW","scienceBaseUri":"505a781ae4b0c8380cd78631","contributors":{"authors":[{"text":"Nord, Gordon L. Jr.","contributorId":12498,"corporation":false,"usgs":true,"family":"Nord","given":"Gordon","suffix":"Jr.","middleInitial":"L.","affiliations":[],"preferred":false,"id":360992,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wandless, M.-V.","contributorId":54611,"corporation":false,"usgs":true,"family":"Wandless","given":"M.-V.","email":"","affiliations":[],"preferred":false,"id":360993,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011411,"text":"70011411 - 1983 - Solubility relations in the ternary system NaCl-CsCl-H2O at 1 atm. 1. Solubilities of halite from 20 to 100 °C","interactions":[],"lastModifiedDate":"2024-04-16T22:49:29.051405","indexId":"70011411","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2209,"text":"Journal of Chemical and Engineering Data","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Solubility relations in the ternary system NaCl-CsCl-H<sub>2</sub>O at 1 atm. 1. Solubilities of halite from 20 to 100 °C","title":"Solubility relations in the ternary system NaCl-CsCl-H2O at 1 atm. 1. Solubilities of halite from 20 to 100 °C","docAbstract":"<p>Solubilities of halite in the ternary system NaCl-CsCl-H<sub>2</sub>O have been determined by the visual polythermal method at 1 atm from 20 to 100 °C along five constant CsCl/(CsCl + H<sub>2</sub>O) weight ratio lines. These five constant weight ratios are 0.1, 0.2, 0.3, 0.4, and 0.5. The maximum uncertainties in these measurements are <span>±</span>0.02 wt % NaCl and <span>±</span>0.15 °C. The data along each constant CsCl/(CsCl + H<sub>2</sub>O) weight ratio line were regressed to a smooth curve. The maximum deviation of the measured solubilities from the smooth curves is 0.06 wt % NaCl. Isothermal solubilities of halite were calculated from smoothed curves at 25, 50, and 75 °C.</p>","language":"English","publisher":"American Chemical Society Publications","doi":"10.1021/je00034a012","issn":"00219568","usgsCitation":"Chou, I., and Lee, R., 1983, Solubility relations in the ternary system NaCl-CsCl-H2O at 1 atm. 1. Solubilities of halite from 20 to 100 °C: Journal of Chemical and Engineering Data, v. 28, no. 4, p. 390-393, https://doi.org/10.1021/je00034a012.","productDescription":"4 p.","startPage":"390","endPage":"393","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":220834,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505b9249e4b08c986b319df7","contributors":{"authors":[{"text":"Chou, I.-M. 0000-0001-5233-6479","orcid":"https://orcid.org/0000-0001-5233-6479","contributorId":44283,"corporation":false,"usgs":true,"family":"Chou","given":"I.-M.","affiliations":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":361020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, R.D.","contributorId":83664,"corporation":false,"usgs":true,"family":"Lee","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":361021,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011619,"text":"70011619 - 1983 - Lead-isotopic compositions of diverse igneous rocks and ore deposits from southwestern New Mexico and their implications for early Proterozoic crustal evolution in the western United States","interactions":[],"lastModifiedDate":"2024-01-03T12:13:02.946684","indexId":"70011619","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Lead-isotopic compositions of diverse igneous rocks and ore deposits from southwestern New Mexico and their implications for early Proterozoic crustal evolution in the western United States","docAbstract":"<div id=\"15238645\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>U-Pb zircon measurements from some of the basement rocks in southwestern New Mexico have ages that range from 1,650 to 1,450 m.y.</p><p>The largest ore deposits occur near Silver City in the southwest part of the region studied. They are associated with Laramide alkali to calc-alkaline plutons, and their lead-isotopic compositions are the least radiogenic in the region. This lead exhibits lower-crustal-upper-mantle characteristics, and for the major producing porphyry copper deposits, the<span>&nbsp;</span><sup>206</sup>Pb/<sup>204</sup>Pb ratios are less than 18.0.</p><p>Lead from more silicic mid-Tertiary volcanic rocks and associated ore deposits has somewhat higher<span>&nbsp;</span><sup>208</sup>Pb/<sup>204</sup>Pb ratios that reflect a greater crustal involvement in their origin. In a regional trend to the northeast, ore lead becomes more radiogenic, and at Hansonburg, 200 km from Silver City, lead in the Mississippi-type deposits is clearly derived from upper-crustal sources.</p><p>On the<span>&nbsp;</span><sup>207</sup>Pb/<sup>204</sup>Pb-<sup>206</sup>Pb/<sup>204</sup>Pb plot, data from all of the rocks and ores that we have analyzed form an array that lies below the average orogene curve of Doe and Zartman (1979). A common source is implied for the lead, the isotopic composition of which was similar to that found in 1,750-m.y.-old stratiform deposits as far apart as Pecos, New Mexico, and Jerome, Arizona. Such a composition indicates that over a large region of the southwestern United States, continental crust developed between 1,750 and 1,450 m.y. ago, possibly in an island-arc environment.</p><p>Basement rocks that are ∼ 1,750 m.y. old extend northward through Colorado to Utah. Galena data obtained in previous studies show that the fraction of older sialic lead in those rocks increases toward the Archean craton in Wyoming. The crust apparently developed southward from Wyoming in stages at 2,400 m.y. ago or before, 2,100 m.y. ago, and 1,750 m.y. ago, with incorporation of older sialic material in each stage as far south as Milford, Utah.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1983)94<43:LCODIR>2.0.CO;2","usgsCitation":"Stacey, J.S., and Hedlund, D.C., 1983, Lead-isotopic compositions of diverse igneous rocks and ore deposits from southwestern New Mexico and their implications for early Proterozoic crustal evolution in the western United States: Geological Society of America Bulletin, v. 94, no. 1, p. 43-57, https://doi.org/10.1130/0016-7606(1983)94<43:LCODIR>2.0.CO;2.","productDescription":"15 p.","startPage":"43","endPage":"57","numberOfPages":"15","costCenters":[],"links":[{"id":220986,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a45dee4b0c8380cd674f8","contributors":{"authors":[{"text":"Stacey, J. S.","contributorId":72785,"corporation":false,"usgs":true,"family":"Stacey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":361558,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedlund, D. C.","contributorId":101624,"corporation":false,"usgs":true,"family":"Hedlund","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":361559,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011601,"text":"70011601 - 1983 - Statistical evaluation of oil and gas prospects in the outer continental shelf of the U.S. Gulf Coast","interactions":[],"lastModifiedDate":"2012-03-12T17:18:31","indexId":"70011601","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2554,"text":"Journal of the International Association for Mathematical Geology","active":true,"publicationSubtype":{"id":10}},"title":"Statistical evaluation of oil and gas prospects in the outer continental shelf of the U.S. Gulf Coast","docAbstract":"Areas of the U.S. Gulf Coast, both onshore and offshore, are among the petroliferous regions of the United States. In offshore Louisiana and Texas, most oil and gas is associated with structurally controlled traps on the crest or flanks of domes created by the diapiric movement of salt. These structures can be detected and mapped by seismic techniques that directly indicate favorable prospective areas. The characteristics of seismically defined structures provide information in advance of drilling about the probable size of reservoirs contained within these structures. Simple statistical relationships can be determined between the size, shape, and other attributes of structures detected by seismic mapping and the presence and size of petroleum and natural gas reservoirs. Gulf Coast OCS lease tracts presently are evaluated by the U.S. government using a Monte Carlo simulation procedure adapted from reservoir analysis. Specification of the parameters of the Monte Carlo model are obtained subjectively in advance of drilling and thus are highly uncertain. Comparisons of predrill predictions with postdiscovery reservoir evaluations show very low correlations. In contrast, predrill predictions based on regressions between seismic structural properties and reservoir volumes show highly significant correlations. In addition, statistical analysis of seismic structure is much simpler than the Monte Carlo procedure, and can be applied rapidly and inexpensively. A statistical analysis of the \"Pleistocene Trend\" of offshore Louisiana and Texas, an area of about 3 million acres, yielded results that are sufficiently encouraging to suggest that similar evaluations be made of the remaining Gulf Coast OCS and of OCS regions off of other coasts of the United States. ?? 1983 Plenum Publishing Corporation.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of the International Association for Mathematical Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers-Plenum Publishers","doi":"10.1007/BF01030086","issn":"00205958","usgsCitation":"Davis, J., and Harbaugh, J., 1983, Statistical evaluation of oil and gas prospects in the outer continental shelf of the U.S. Gulf Coast: Journal of the International Association for Mathematical Geology, v. 15, no. 1, https://doi.org/10.1007/BF01030086.","startPage":"217","costCenters":[],"links":[{"id":205058,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01030086"},{"id":220713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b972be4b08c986b31b911","contributors":{"authors":[{"text":"Davis, J.C.","contributorId":72121,"corporation":false,"usgs":true,"family":"Davis","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":361518,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harbaugh, J.W.","contributorId":43912,"corporation":false,"usgs":true,"family":"Harbaugh","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":361517,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012103,"text":"70012103 - 1983 - Use of reflectance spectra of native plant species for interpreting airborne multispectral scanner data in the East Tintic Mountains, Utah","interactions":[],"lastModifiedDate":"2024-01-11T16:52:21.107163","indexId":"70012103","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Use of reflectance spectra of native plant species for interpreting airborne multispectral scanner data in the East Tintic Mountains, Utah","docAbstract":"<p><span>Representative spectra from three plant species were used to interpret the color components on a color ratio composite image. Most of the vegetation unit coincided with an altered rock unit, but many altered areas were not within the vegetation unit.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.78.4.761","issn":"03610128","usgsCitation":"Milton, N., 1983, Use of reflectance spectra of native plant species for interpreting airborne multispectral scanner data in the East Tintic Mountains, Utah: Economic Geology, v. 78, no. 4, p. 761-769, https://doi.org/10.2113/gsecongeo.78.4.761.","productDescription":"9 p.","startPage":"761","endPage":"769","numberOfPages":"9","costCenters":[],"links":[{"id":221867,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"78","issue":"4","noUsgsAuthors":false,"publicationDate":"1983-07-01","publicationStatus":"PW","scienceBaseUri":"505bbf6ae4b08c986b329b46","contributors":{"authors":[{"text":"Milton, N.M.","contributorId":29415,"corporation":false,"usgs":true,"family":"Milton","given":"N.M.","email":"","affiliations":[],"preferred":false,"id":362736,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011443,"text":"70011443 - 1983 - Fission track dating of kimberlitic zircons","interactions":[],"lastModifiedDate":"2023-12-10T22:01:13.156211","indexId":"70011443","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Fission track dating of kimberlitic zircons","docAbstract":"<p>The only reliable method for dating kimberlites at present is the lengthy and specialized hydrothermal procedure that extracts<sup>206</sup>Pb and<sup>238</sup>U from low-uranium zircons. This paper describes a second successful method by fission track dating of large single-crystal zircons, 1.0–1.5 cm in dimension. The use of large crystals overcomes the limitations imposed in conventional fission track analysis which utilizes crushed fragments. Low track densities, optical track dispersion, and the random orientation of polished surfaces in the etch and irradiation cycle are effectively overcome.</p><p>Fission track ages of zircons from five African kimberlites are reported, from the Kimberley Pool (90.3 ± 6.5 m.y.), Orapa (87.4 ± 5.7 and 92.4 ± 6.1 m.y.), Nzega (51.1 ± 3.8 m.y.), Koffiefontein (90.0 ± 8.2 m.y.), and Val do Queve (133.4 ± 11.5 m.y.). In addition we report the first radiometric ages (707.9 ± 59.6 and 705.5 ± 61.0 m.y.) of crustal zircons from kimberlites in northwest Liberia. The fission track ages agree well with earlier age estimates. Most of the zircons examined in this study are zoned with respect to uranium but linear correlations are established (by regression analysis) between zones of variable uranium content, and within zones of constant uranium content (by analysis of variance). Concordance between the fission track method and the U/Pb technique is established and we concluded that track fading from thermal annealing has not taken place. Kimberlitic zircons dated in this study, therefore, record the time of eruption.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(83)90020-1","issn":"0012821X","usgsCitation":"Haggerty, S., Raber, E., and Naeser, C.W., 1983, Fission track dating of kimberlitic zircons: Earth and Planetary Science Letters, v. 63, no. 1, p. 41-50, https://doi.org/10.1016/0012-821X(83)90020-1.","productDescription":"10 p.","startPage":"41","endPage":"50","numberOfPages":"10","costCenters":[],"links":[{"id":221364,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a10bde4b0c8380cd53db3","contributors":{"authors":[{"text":"Haggerty, S.E.","contributorId":75681,"corporation":false,"usgs":true,"family":"Haggerty","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":361107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raber, E.","contributorId":12620,"corporation":false,"usgs":true,"family":"Raber","given":"E.","email":"","affiliations":[],"preferred":false,"id":361105,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Naeser, C. W.","contributorId":17582,"corporation":false,"usgs":true,"family":"Naeser","given":"C.","middleInitial":"W.","affiliations":[],"preferred":false,"id":361106,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011275,"text":"70011275 - 1983 - Faulting arrested by control of ground-water withdrawal in Houston, Texas","interactions":[],"lastModifiedDate":"2021-02-26T13:07:46.02718","indexId":"70011275","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Faulting arrested by control of ground-water withdrawal in Houston, Texas","docAbstract":"<p>More than 86 historically active faults with an aggregate length of 150 miles have been identified within and adjacent to the Houston, Texas, metropolitan area. Although scarps of these faults grow gradually and without causing damaging earthquakes, historical fault offset has cost millions of dollars in damage to houses and other buildings, utilities, and highways that were built on or across the faults. The historical fault activity results from renewed movement along preexisting faults and appears to be caused principally by withdrawal of ground water for municipal, industrial, and agricultural uses in the Houston area. Approximately one-half of the area's water supply is obtained from local ground water. Monitoring by the US Geological Survey of heights of fault scarps indicates that many of the scarps have recently stopped increasing in height. The area where faulting has ceased coincides with the area where ground-water pumping was cut back in the mid-1970s to slow the damage caused by land subsidence along Galveston Bay and the Houston Ship Channel. Thus, it appears that efforts to halt land subsidence in the coastal area have provided the additional benefit of arresting damaging surface faulting. -from Authors</p>","language":"English","publisher":"U.S. Geological Survey","usgsCitation":"Holzer, T., Gabrysch, R., and Verbeek, E., 1983, Faulting arrested by control of ground-water withdrawal in Houston, Texas: Earthquake Information Bulletin (USGS), v. 15, no. 6, p. 204-209.","productDescription":"6 p.","startPage":"204","endPage":"209","numberOfPages":"6","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":220968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70011275/report-thumb.jpg"},{"id":282969,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70011275/report.pdf","text":"Report","size":"2.97 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","city":"Houston","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96,\n              29\n            ],\n            [\n              -96,\n              30\n            ],\n            [\n              -94.5,\n              30\n            ],\n            [\n              -94.5,\n              29\n            ],\n            [\n              -96,\n              29\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"15","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0f24e4b0c8380cd537be","contributors":{"authors":[{"text":"Holzer, T.","contributorId":17368,"corporation":false,"usgs":true,"family":"Holzer","given":"T.","email":"","affiliations":[],"preferred":false,"id":360727,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":360729,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Verbeek, E.R.","contributorId":61439,"corporation":false,"usgs":true,"family":"Verbeek","given":"E.R.","affiliations":[],"preferred":false,"id":360728,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011338,"text":"70011338 - 1983 - Euler-Lagrangian computation for estuarine hydrodynamics","interactions":[],"lastModifiedDate":"2016-07-27T10:37:23","indexId":"70011338","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Euler-Lagrangian computation for estuarine hydrodynamics","docAbstract":"<p>The transport of conservative and suspended matter in fluid flows is a phenomenon of Lagrangian nature because the process is usually convection dominant. Nearly all numerical investigations of such problems use an Eulerian formulation for the convenience that the computational grids are fixed in space and because the vast majority of field data are collected in an Eulerian reference frame. Several examples are given in this paper to illustrate a modeling approach which combines the advantages of both the Eulerian and Lagrangian computational techniques.</p>","largerWorkTitle":"Numerical Methods in Laminar and Turbulent Flow, Proceedings of the International Conference","conferenceTitle":"Numerical Methods in Laminar and Turbulent Flow, Proceedings of the Third International Conference.","conferenceLocation":"Seattle, WA","language":"English","publisher":"Pineridge Press","publisherLocation":"Swansea, Wa","isbn":"0906674220","usgsCitation":"Cheng, R.T., 1983, Euler-Lagrangian computation for estuarine hydrodynamics, <i>in</i> Numerical Methods in Laminar and Turbulent Flow, Proceedings of the International Conference, Seattle, WA, p. 341-352.","startPage":"341","endPage":"352","numberOfPages":"12","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":220766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0469e4b0c8380cd50980","contributors":{"authors":[{"text":"Cheng, Ralph T.","contributorId":69134,"corporation":false,"usgs":true,"family":"Cheng","given":"Ralph","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":360866,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011282,"text":"70011282 - 1983 - Automated determination of bromide in waters by ion chromatography with an amperometric detector","interactions":[],"lastModifiedDate":"2023-03-07T16:30:37.566048","indexId":"70011282","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":760,"text":"Analytica Chimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Automated determination of bromide in waters by ion chromatography with an amperometric detector","docAbstract":"<p><span>An automated ion chromatograph, including a program controller, an automatic sampler, an integrator, and an amperometric detector, was used to develop a procedure for the determination of bromide in rain water and many ground waters. Approximately 10 min is required to obtain a chromatogram. The detection limit for bromide is 0.01 mg l</span><sup>−1</sup><span>&nbsp;and the relative standard deivation is &lt;5% for bromide concentrations between 0.05 and 0.5 mg l</span><sup>−1</sup><span>. Chloride interferes if the chloride-to-bromide ratio is greater than 1 000:1 for a range of 0.01–0.1 mg l</span><sup>−1</sup><span>&nbsp;bromide; similarly, chloride interferes in the 0.1–1.0 mg l</span><sup>−1</sup><span>&nbsp;range if the ratio is greater than 5 000:1. In the latter case, a maximum of 2 000 mg l</span><sup>−1</sup><span>&nbsp;of chloride can be tolerated. Recoveries of known concentrations of bromide added to several samples, ranged from 97 to 110%.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0003-2670(00)83193-1","usgsCitation":"Pyen, G., and Erdmann, D.E., 1983, Automated determination of bromide in waters by ion chromatography with an amperometric detector: Analytica Chimica Acta, v. 149, no. C, p. 355-358, https://doi.org/10.1016/S0003-2670(00)83193-1.","productDescription":"4 p.","startPage":"355","endPage":"358","numberOfPages":"4","costCenters":[],"links":[{"id":221101,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"149","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eef4e4b0c8380cd4a06c","contributors":{"authors":[{"text":"Pyen, G. S.","contributorId":105049,"corporation":false,"usgs":true,"family":"Pyen","given":"G. S.","affiliations":[],"preferred":false,"id":360743,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erdmann, D. E.","contributorId":30264,"corporation":false,"usgs":true,"family":"Erdmann","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":360742,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70135744,"text":"70135744 - 1983 - Site 534: Blake-Bahama Basin","interactions":[],"lastModifiedDate":"2023-01-02T17:31:29.866937","indexId":"70135744","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"4","title":"Site 534: Blake-Bahama Basin","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Initial reports of the deep sea drilling project","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Ocean Drilling Program","doi":"10.2973/dsdp.proc.76.104.1983","usgsCitation":"Shipboard Scientific Party, 1983, Site 534: Blake-Bahama Basin, chap. 4 <i>of</i> Initial reports of the deep sea drilling project, v. 76, p. 141-340, https://doi.org/10.2973/dsdp.proc.76.104.1983.","productDescription":"200 p.","startPage":"141","endPage":"340","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":296706,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Bahamas, United States","otherGeospatial":"Atlantic Ocean, Blake-Bahama Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.94445914057093,\n              25.865257557482607\n            ],\n            [\n              -73.44985798492627,\n              23.244603058208213\n            ],\n            [\n              -67.65288772112154,\n              28.10508733325615\n            ],\n            [\n              -65.02100684182419,\n              32.84901595793383\n            ],\n            [\n              -64.4805143076793,\n              38.193077007563545\n            ],\n            [\n              -66.8608093492573,\n              40.73970936537094\n            ],\n            [\n              -71.53419952235211,\n              40.13343039492969\n            ],\n            [\n              -74.89541581254684,\n              37.390779900594325\n            ],\n            [\n              -74.76788161867582,\n              35.23012315707604\n            ],\n            [\n              -76.84691384447717,\n              33.24715047243495\n            ],\n            [\n              -76.97076118285693,\n              30.06801119266224\n            ],\n            [\n              -76.72014811197283,\n              27.250619616661993\n            ],\n            [\n              -76.94445914057093,\n              25.865257557482607\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"76","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"549165d4e4b0d0759afaad9b","contributors":{"authors":[{"text":"Shipboard Scientific Party","contributorId":130994,"corporation":true,"usgs":false,"organization":"Shipboard Scientific Party","id":536794,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70135757,"text":"70135757 - 1983 - Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling","interactions":[],"lastModifiedDate":"2017-08-24T12:56:52","indexId":"70135757","displayToPublicDate":"1982-12-27T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling","docAbstract":"<p><span>Gravity models computed for a profile across the long-wavelength paired negative-positive Bouguer anomalies of the southern Appalachian Mountains show that the large negative anomaly can be explained by a crustal root zone, whereas the steep gradient and positive anomaly east of the root may be explained equally well by three different geometries: a suture zone, a mantle upwarp, or a shallow body. Seismic data support the existence of a mountain root but are inadequate to resolve differences among the three possible geometries for the positive anomaly. The presence of outcropping mafic and ultramafic rocks in the southern Appalachians and the inferred tectonic history of the Appalachian orogen are most consistent with the suture-zone model. Crust similar to continental crust probably exists beneath the Coastal Plain and inner continental shelf where the gravity anomalies return to near-zero values.</span></p>","language":"English","publisher":"Geological Society of  America","doi":"10.1130/0091-7613(1983)11<611:CSBTSA>2.0.CO;2","usgsCitation":"Hutchinson, D.R., Grow, J., and Klitgord, K.D., 1983, Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling: Geology, v. 11, no. 10, p. 611-615, https://doi.org/10.1130/0091-7613(1983)11<611:CSBTSA>2.0.CO;2.","productDescription":"5 p.","startPage":"611","endPage":"615","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":296724,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Appalachian Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -69.01611328125,\n              47.502358951968596\n            ],\n            [\n              -66.6650390625,\n              45.336701909968106\n            ],\n            [\n              -86.484375,\n              31.82156451492074\n            ],\n            [\n              -88.2861328125,\n              33.65120829920497\n            ],\n            [\n              -69.01611328125,\n              47.502358951968596\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"11","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"549165bfe4b0d0759afaad80","contributors":{"authors":[{"text":"Hutchinson, Deborah R. 0000-0002-2544-5466 dhutchinson@usgs.gov","orcid":"https://orcid.org/0000-0002-2544-5466","contributorId":521,"corporation":false,"usgs":true,"family":"Hutchinson","given":"Deborah","email":"dhutchinson@usgs.gov","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":536831,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grow, John A.","contributorId":51739,"corporation":false,"usgs":true,"family":"Grow","given":"John A.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":536832,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klitgord, Kim D.","contributorId":82307,"corporation":false,"usgs":true,"family":"Klitgord","given":"Kim","email":"","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":536833,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70231503,"text":"70231503 - 1983 - Response: Uranium series ages of the Del Mar Man and Sunnyvale skeletons","interactions":[],"lastModifiedDate":"2022-05-11T16:50:39.202911","indexId":"70231503","displayToPublicDate":"1982-08-20T11:49:11","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Response: Uranium series ages of the Del Mar Man and Sunnyvale skeletons","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"AAAS","doi":"10.1126/science.217.4561.756","usgsCitation":"Bischoff, J.L., and Rosenbauer, R.J., 1983, Response: Uranium series ages of the Del Mar Man and Sunnyvale skeletons: Science, v. 217, no. 4561, https://doi.org/10.1126/science.217.4561.756.","productDescription":"1 p.","startPage":"576","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":400517,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"217","issue":"4561","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bischoff, James L. jbischoff@usgs.gov","contributorId":1389,"corporation":false,"usgs":true,"family":"Bischoff","given":"James","email":"jbischoff@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":842797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosenbauer, Robert J. brosenbauer@usgs.gov","contributorId":204,"corporation":false,"usgs":true,"family":"Rosenbauer","given":"Robert","email":"brosenbauer@usgs.gov","middleInitial":"J.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":842798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70195580,"text":"70195580 - 1983 - A Canada goose project in Connecticut","interactions":[],"lastModifiedDate":"2023-10-11T01:10:16.48669","indexId":"70195580","displayToPublicDate":"1981-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1320,"text":"The Connecticut Warbler","printIssn":"1077-0283","active":true,"publicationSubtype":{"id":10}},"title":"A Canada goose project in Connecticut","docAbstract":"<p>It wasn't so long ago that the wild cries of Canada geese overhead were enough to draw most people out of their homes to look skyward. It was a rare sound heard only in the spring and fall when migrating flocks of these magnificent birds marked the change of the seasons. But today the sound is less delightful to growing numbers of people as goose populations have become permanent residents of the Northeast and caused numerous problems.</p><p>Non-migratory flocks of Canada geese are now present from Cape Cod to Virginia. According to the Atlantic Flyway Council, these geese have provoked nuisance complaints from local communities in every one of the states involved, except Delaware. Delaware has had problems in the past but they are presently under control. These resident populations cause numerous sanitation problems in local communities. Examples are accumulations of feathers and droppings, odor, noise, landscape and crop destruction, the decoying-in of additional geese, and overfertilization of ponds, thus causing algal growth and concerns about health problems, especially in swimming and other recreational areas. </p>","language":"English","publisher":"Connecticut Ornithological Association","usgsCitation":"Converse, K.A., 1983, A Canada goose project in Connecticut: The Connecticut Warbler, v. 1, no. 3, p. 36-38.","productDescription":"3 p.","startPage":"36","endPage":"38","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":351893,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.ctbirding.org/publications/the-connecticut-warbler/"},{"id":351894,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Connecticut","county":"Fairfield 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Kathryn A. kathy_converse@usgs.gov","contributorId":16802,"corporation":false,"usgs":true,"family":"Converse","given":"Kathryn","email":"kathy_converse@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":false,"id":729349,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30342,"text":"wri8159 - 1982 - Effects of land use on surface-water quality in the East Everglades, Dade County, Florida","interactions":[],"lastModifiedDate":"2021-12-13T12:29:37.561555","indexId":"wri8159","displayToPublicDate":"2021-12-12T20:45:00","publicationYear":"1982","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":"81-59","title":"Effects of land use on surface-water quality in the East Everglades, Dade County, Florida","docAbstract":"Water-quality characteristics were determined at five developed areas in the East Everglades, Dade County, Florida, during the 1978 wet season (June through October). These areas are designated as: Coopertown; Chekika Hammock State Park; residential area; rock-plowed tomato field; and Cracker Jack Slough agricultural area. Data from the developed areas were compared with data from four baseline sites in undeveloped areas to determine the effects of land use on the surface-water quality. The rock-plowed tomato field was the only area where surface-water quality was affected. Water quality at this field is affected by agricultural activities and chemical applications as indicated by increased concentrations of orthophosphate, organic nitrogen, organic carbon, copper, manganese, mercury, and potassium. The remaining four areas of land use had water-quality characteristics typical of baseline sites in nearby Northeast Shark River Slough or Taylor Slough. Chemical analyses of soil indicated chlorinated-hydrocarbon insecticide residues at Coopertown and the two agricultural areas, Cracker Jack Slough and the rock-plowed tomato field. Trace elements in concentrations greater than base level occurred at both agricultural areas (manganese), Chekika Hammock State Park (manganese), and at Coopertown (lead and zinc). (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8159","collaboration":"Prepared in cooperation with the Metropolitan Dade County Planning Department","usgsCitation":"Waller, B.G., 1982, Effects of land use on surface-water quality in the East Everglades, Dade County, Florida: U.S. Geological Survey Water-Resources Investigations Report 81-59, Report: v, 37 p.; 2 Plates: 32.88 x 30.00 inches or smaller, https://doi.org/10.3133/wri8159.","productDescription":"Report: v, 37 p.; 2 Plates: 32.88 x 30.00 inches or smaller","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":159305,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0059/coverthb.jpg"},{"id":59135,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/0059/wri8159_plate1.pdf","text":"Plate 1","size":"4.17 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":59136,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/0059/wri8159_plate2.pdf","text":"Plate 2","size":"3.94 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":2480,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0059/wri8159.pdf","text":"Report","size":"1.56 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 81-59"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.66162109375,\n              25.18505888358067\n            ],\n            [\n              -79.98046875,\n              25.18505888358067\n            ],\n            [\n              -79.98046875,\n              25.997549919572112\n            ],\n            [\n              -80.66162109375,\n              25.997549919572112\n            ],\n            [\n              -80.66162109375,\n              25.18505888358067\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611cd1","contributors":{"authors":[{"text":"Waller, Bradley G.","contributorId":83492,"corporation":false,"usgs":true,"family":"Waller","given":"Bradley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203089,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30341,"text":"wri824093 - 1982 - Effects of land use on ground-water quality in the East Everglades, Dade County, Florida","interactions":[],"lastModifiedDate":"2021-12-13T12:30:20.981613","indexId":"wri824093","displayToPublicDate":"2021-12-12T20:45:00","publicationYear":"1982","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":"82-4093","title":"Effects of land use on ground-water quality in the East Everglades, Dade County, Florida","docAbstract":"Groundwater quality characteristics of the Biscayne aquifer from September 1978 through June 1979 were determined for seven land use areas within the East Everglades in Dade County, Florida. Four agricultural areas, two low-density residential areas, and Chekika Hammock State Park were investigated. The effects of land use on the groundwater were minimal in all areas; only iron , which occurs naturally in high concentrations in the Everglades, exceeded potable groundwater standards. Potassium and nitrate concentrations in certain samples increased over background concentrations in the agricultural areas. Groundwater at Chekika Hammock State Park and at a citrus grove is contaminated by brackish water flowing from an artesian well. The soil at the agricultural areas had higher concentrations of chromium, copper, and manganese than at the two residential areas or at Chekika Hammock State Park. One residential area (Coopertown) had the highest concentrations of lead and zinc and detectable polychlorinated biphenyls. Chlorinated-hydrocarbon insecticide residues in soil at three agricultural areas were higher than background concentrations. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri824093","collaboration":"Prepared in cooperation with the Metropolitan Dade County Planning Department","usgsCitation":"Waller, B., 1982, Effects of land use on ground-water quality in the East Everglades, Dade County, Florida: U.S. Geological Survey Water-Resources Investigations Report 82-4093, viii, 75 p., https://doi.org/10.3133/wri824093.","productDescription":"viii, 75 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":124279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4093/coverthb.jpg"},{"id":59134,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4093/wri824093.pdf","text":"Report","size":"1.56 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 82-4093"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.66162109375,\n              25.18505888358067\n            ],\n            [\n              -79.98046875,\n              25.18505888358067\n            ],\n            [\n              -79.98046875,\n              25.997549919572112\n            ],\n            [\n              -80.66162109375,\n              25.997549919572112\n            ],\n            [\n              -80.66162109375,\n              25.18505888358067\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611e41","contributors":{"authors":[{"text":"Waller, B.G.","contributorId":75970,"corporation":false,"usgs":true,"family":"Waller","given":"B.G.","email":"","affiliations":[],"preferred":false,"id":203088,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30334,"text":"wri8220 - 1982 - Areal extent of a plume of mineralized water from a flowing artesian well in Dade County, Florida","interactions":[],"lastModifiedDate":"2021-12-13T12:32:19.881544","indexId":"wri8220","displayToPublicDate":"2021-12-12T20:45:00","publicationYear":"1982","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":"82-20","title":"Areal extent of a plume of mineralized water from a flowing artesian well in Dade County, Florida","docAbstract":"A flowing artesian well that taps the Floridan aquifer at Chekika Hammock State Park is contaminating the overlying Biscayne aquifer with saline water. The plume of mineralized water extends approximately 7 miles southeast of the well and ranges in width from 1 to 2 miles. The areal extent of contamination in the primary plume is approximately 12 square miles. The principal ions contaminating the Biscayne aquifer are chloride, sodium, and sulfate. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8220","collaboration":"Prepared in cooperation with the Metropolitan Dade County Planning Department","usgsCitation":"Waller, B.G., 1982, Areal extent of a plume of mineralized water from a flowing artesian well in Dade County, Florida: U.S. Geological Survey Water-Resources Investigations Report 82-20, v, 20 p., https://doi.org/10.3133/wri8220.","productDescription":"v, 20 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":122747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0020/coverthb.jpg"},{"id":59131,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0020/wri8220.pdf","text":"Report","size":"582 KB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 82-20"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.71655273437499,\n              25.095548539604227\n            ],\n            [\n              -80.03540039062499,\n              25.095548539604227\n            ],\n            [\n              -80.03540039062499,\n              25.90864446329127\n            ],\n            [\n              -80.71655273437499,\n              25.90864446329127\n            ],\n            [\n              -80.71655273437499,\n              25.095548539604227\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673491","contributors":{"authors":[{"text":"Waller, Bradley G.","contributorId":83492,"corporation":false,"usgs":true,"family":"Waller","given":"Bradley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203077,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30335,"text":"wri823 - 1982 - Assessment of water quality in canals of eastern Broward County, Florida, 1969-74","interactions":[],"lastModifiedDate":"2021-12-13T12:31:24.026004","indexId":"wri823","displayToPublicDate":"2021-12-12T20:45:00","publicationYear":"1982","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":"82-3","title":"Assessment of water quality in canals of eastern Broward County, Florida, 1969-74","docAbstract":"An intensive water-quality monitoring program was started in 1969 to determine the effects of man-induced contaminants on the water quality in the primary canal system of eastern Broward County, Florida. This report covers the first 6 years of the program and provides a data base that can be used to compare future changes in water-quality conditions. Most data indicate that beyond the small seasonal fluctuation in constituent level, the greatest adverse effect on the quality of water is caused by discharge of sewage and treated sewage effluent to the canals. The areas affected by sewage have greater concentrations of macronutrients, trace metals, and pesticides than unaffected areas. Major-ion concentrations were affected only by season and local lithology. Over the 6-year study a gradual decrease in macronutrient concentration and an increase in dissolved oxygen have occurred. This improvement in water quality is attributed to a decrease of sewage discharge into canals and better treatment of sewage effluents. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri823","collaboration":"Prepared in cooperation with the Broward County Environmental Quality Control Board and the South Florida Water Management District","usgsCitation":"Waller, B.G., and Miller, W.L., 1982, Assessment of water quality in canals of eastern Broward County, Florida, 1969-74: U.S. Geological Survey Water-Resources Investigations Report 82-3, vii, 70 p., https://doi.org/10.3133/wri823.","productDescription":"vii, 70 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":159296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0003/coverthb.jpg"},{"id":2470,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0003/wri823.pdf","text":"Report","size":"1.72 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 82-3"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.60668945312499,\n              25.651430347039724\n            ],\n            [\n              -79.92553710937499,\n              25.651430347039724\n            ],\n            [\n              -79.92553710937499,\n              26.46073804319089\n            ],\n            [\n              -80.60668945312499,\n              26.46073804319089\n            ],\n            [\n              -80.60668945312499,\n              25.651430347039724\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667245","contributors":{"authors":[{"text":"Waller, Bradley G.","contributorId":83492,"corporation":false,"usgs":true,"family":"Waller","given":"Bradley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203078,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Wesley L.","contributorId":91859,"corporation":false,"usgs":true,"family":"Miller","given":"Wesley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":203079,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}