No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79623","usgsCitation":"Berge Exploration Inc., 1979, Federal coal resource occurrence and coal development potential maps of the Cuba 7 1/2-minute quadrangle, Sandoval County, New Mexico: U.S. Geological Survey Open-File Report 79-623, Report: 21 p.; 4 Plates: 23.24 × 28.14 inches or smaller, https://doi.org/10.3133/ofr79623.","productDescription":"Report: 21 p.; 4 Plates: 23.24 × 28.14 inches or smaller","costCenters":[],"links":[{"id":68865,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0623/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":68864,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0623/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391021,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_29193.htm"},{"id":169598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0623/report-thumb.jpg"},{"id":68868,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0623/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":68866,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0623/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":68867,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0623/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Mexico","county":"Sandoval County","otherGeospatial":"Cuba 7 1/2-minute quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107,\n 36\n ],\n [\n -106.875,\n 36\n ],\n [\n -106.875,\n 36.125\n ],\n [\n -107,\n 36.125\n ],\n [\n -107,\n 36\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af62e","contributors":{"authors":[{"text":"Berge Exploration Inc.","contributorId":128031,"corporation":true,"usgs":false,"organization":"Berge Exploration Inc.","id":529972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11286,"text":"ofr79774 - 1979 - Interpretation of thermoluminescence patterns around a Wyoming roll-type uranium deposit","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr79774","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-774","title":"Interpretation of thermoluminescence patterns around a Wyoming roll-type uranium deposit","docAbstract":"Thermoluminescence from quartz and feldspar grains in samples collected from the vicinity of a Wyoming roll-type uranium deposit show an increase in the importance of high-temperature thermoluminescence relative to low-temperature thermoluminescence of samples which are believed to be former positions of the migrating mineralized front. This effect is believed to be due to the increased radiation in the ore coupled with the faster rate of fading of low-temperature thermoluminescence compared to high-temperature thermoluminescence. Both the ratios of thermoluminescent responses from any of a variety of temperature ranges and glow curves (plots of intensity of thermoluminescence versus temperature) can be used to detect the increased importance of high-temperature thermoluminescence relative to low-temperature thermoluminescence of previously mineralized samples. Both ratios and glow curves present a systematic pattern around this deposit; these patterns may have application in uranium prospecting.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr79774","usgsCitation":"Spirakis, C.S., 1979, Interpretation of thermoluminescence patterns around a Wyoming roll-type uranium deposit: U.S. Geological Survey Open-File Report 79-774, ii, 22 p. :graphs ;28 cm., https://doi.org/10.3133/ofr79774.","productDescription":"ii, 22 p. :graphs ;28 cm.","costCenters":[],"links":[{"id":143267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0774/report-thumb.jpg"},{"id":39088,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0774/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e00df","contributors":{"authors":[{"text":"Spirakis, Charles S.","contributorId":97111,"corporation":false,"usgs":true,"family":"Spirakis","given":"Charles","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":162869,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4241,"text":"cir796 - 1979 - Biological and microbiological assessment of the upper Chattahoochee River basin, Georgia","interactions":[],"lastModifiedDate":"2017-02-03T11:15:53","indexId":"cir796","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"796","title":"Biological and microbiological assessment of the upper Chattahoochee River basin, Georgia","docAbstract":"Biological and microbiological studies were conducted by the U.S. Geological Survey as a part of the Intensive River-Quality Assessment studies of the upper Chattahoochee River basin, Georgia. Phytoplankton concentrations in cells per milliliter (cells/mL) were generally higher downstream from Atlanta than upstream. The highest concentrations, mostly blue-green algae, occurred in West Point Lake with an average of 90,000 cells/mL for the sampling period. The lowest concentrations, 1,000 cells/mL, occurred upstream of Lake Sidney Lanier. Dissolved orthophosphate and nitrite plus nitrate concentrations were highest in the river reaches and upper reaches of the two lakes and were lowest at the dam pools of both lakes. The high nitrite plus nitrate concentrations downstream from Atlanta were primarily a result of nitrification by Nitrosomonas and Nitrobacter bacteria. Algal growth potential was highest downstream from Atlanta, 25 milligrams per liter (mg/L) at Whitesburg, and was the lowest in the headwaters and at the dam pools of Lake Sidney Lanier and West Point Lake. The rate of nitrification in the Atlanta to Franklin reach of the river was comparatively low, 0.02 mg/L per hour. Nitrification was an important cause of dissolved-oxygen consumption in a 45-mi reach of the river downstream from the Atlanta wastewater treatment facilities. Dissolved-oxygen consumption as a result of nitrification may be greatest during low flow. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir796","usgsCitation":"Lium, B.W., Stamer, J., Ehlke, T.A., Faye, R., and Cherry, R., 1979, Biological and microbiological assessment of the upper Chattahoochee River basin, Georgia: U.S. Geological Survey Circular 796, iv, 22 p. :ill. ;28 cm. , https://doi.org/10.3133/cir796.","productDescription":"iv, 22 p. :ill. ;28 cm. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":126676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1979/0796/report-thumb.jpg"},{"id":31355,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1979/0796/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alabama, Georgia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.59634399414061,\n 34.65213247511267\n ],\n [\n -83.53008270263672,\n 34.66794670701665\n ],\n [\n -83.48613739013672,\n 34.66060476037414\n ],\n [\n -83.45626831054688,\n 34.641117209595805\n ],\n [\n -83.43292236328125,\n 34.58884537801345\n ],\n [\n -83.45386505126953,\n 34.54021718378472\n ],\n [\n -83.48957061767578,\n 34.50344445434755\n ],\n [\n -83.77761840820312,\n 34.25210855909975\n ],\n [\n -83.91014099121094,\n 34.113510052127566\n ],\n [\n -84.08111572265625,\n 33.986071790199205\n ],\n [\n -84.23423767089844,\n 33.92740869431181\n ],\n [\n -84.3255615234375,\n 33.93139678750913\n ],\n [\n -84.39216613769531,\n 33.85159945579106\n ],\n [\n -84.4690704345703,\n 33.780859506378675\n ],\n [\n -84.61601257324219,\n 33.63062889539564\n ],\n [\n -84.71351623535156,\n 33.55627344791359\n ],\n [\n -84.76364135742188,\n 33.49788816685207\n ],\n [\n -84.81376647949219,\n 33.305281685899445\n ],\n [\n -84.95315551757812,\n 33.28748994441748\n ],\n [\n -84.91333007812499,\n 33.19905140349983\n ],\n [\n -84.92843627929688,\n 33.15537344954293\n ],\n [\n -85.04928588867188,\n 32.915908931564864\n ],\n [\n -85.18798828125,\n 32.86747661083543\n ],\n [\n -85.32600402832031,\n 32.91648534731439\n ],\n [\n -85.35072326660155,\n 33.03744943602074\n ],\n [\n -85.3363037109375,\n 33.15594830078649\n ],\n [\n -85.19691467285156,\n 33.247301699949205\n ],\n [\n -85.1605224609375,\n 33.43086829665599\n ],\n [\n -85.00808715820312,\n 33.53223722395908\n ],\n [\n -84.84466552734375,\n 33.75288969455201\n ],\n [\n -84.57481384277344,\n 33.857871948188674\n ],\n [\n -84.4244384765625,\n 34.045263375550654\n ],\n [\n -84.24591064453125,\n 34.081099738028236\n ],\n [\n -84.12986755371094,\n 34.24472995671498\n ],\n [\n -84.03785705566406,\n 34.359308974793564\n ],\n [\n -84.00489807128906,\n 34.44315867450577\n ],\n [\n -83.79478454589844,\n 34.60947549180879\n ],\n [\n -83.72611999511719,\n 34.65410941913741\n ],\n [\n -83.66294860839844,\n 34.649025753526985\n ],\n [\n -83.59634399414061,\n 34.65213247511267\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629e18","contributors":{"authors":[{"text":"Lium, Bruce W.","contributorId":75907,"corporation":false,"usgs":true,"family":"Lium","given":"Bruce","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":148531,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stamer, J. K.","contributorId":47753,"corporation":false,"usgs":true,"family":"Stamer","given":"J. K.","affiliations":[],"preferred":false,"id":148530,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ehlke, T. A.","contributorId":106477,"corporation":false,"usgs":true,"family":"Ehlke","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":148532,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Faye, R.E.","contributorId":106863,"corporation":false,"usgs":true,"family":"Faye","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":148533,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cherry, R.N.","contributorId":20728,"corporation":false,"usgs":true,"family":"Cherry","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":148529,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":46410,"text":"ofr791513 - 1979 - Measured lignite sections in northeastern Montana and northwestern North Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:04:59","indexId":"ofr791513","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1513","title":"Measured lignite sections in northeastern Montana and northwestern North Dakota","language":"ENGLISH","doi":"10.3133/ofr791513","usgsCitation":"Gott, G.B., and Witkind, I.J., 1979, Measured lignite sections in northeastern Montana and northwestern North Dakota: U.S. Geological Survey Open-File Report 79-1513, 1 map and 48 sections ;on sheet 92 x 105 cm. --, https://doi.org/10.3133/ofr791513.","productDescription":"1 map and 48 sections ;on sheet 92 x 105 cm. --","costCenters":[],"links":[{"id":135861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":83363,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1513/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db610b54","contributors":{"authors":[{"text":"Gott, Garland Bayard","contributorId":6420,"corporation":false,"usgs":true,"family":"Gott","given":"Garland","email":"","middleInitial":"Bayard","affiliations":[],"preferred":false,"id":233230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witkind, Irving Jerome","contributorId":87517,"corporation":false,"usgs":true,"family":"Witkind","given":"Irving","email":"","middleInitial":"Jerome","affiliations":[],"preferred":false,"id":233231,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10899,"text":"ofr791675 - 1979 - Fluid inclusions in salt from the Rayburn and Vacherie domes, Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr791675","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1675","title":"Fluid inclusions in salt from the Rayburn and Vacherie domes, Louisiana","docAbstract":"Core samples from the Rayburn and Vacherie salt domes in Louisiana were examined for fluid inclusions, in connection with the possible use of such domes for nuclear waste storage sites. Three types of fluid inclusions were found, brine, compressed gas, and oil (in decreasing volume percent abundance). The total amount of such fluids is small, certainly < 0.1 vol. % and probably in the range 0.01 to 0.001 volume %, but the inclusions are highly erratic in distribution. Unlike many bedded salt deposits, the brine inclusions in this salt contain fluids that are not far from simple NaCl-H2O solutions, with very little of other ions. One of three possible explanations for such fluids is that fresh water penetrated the salt at some unknown time in the past and was trapped; if such entry of fresh water has occurred in the past, it might also occur again in the future.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791675","usgsCitation":"Roedder, E., and Belkin, H., 1979, Fluid inclusions in salt from the Rayburn and Vacherie domes, Louisiana: U.S. Geological Survey Open-File Report 79-1675, 26 p. ;28 cm., https://doi.org/10.3133/ofr791675.","productDescription":"26 p. ;28 cm.","costCenters":[],"links":[{"id":143042,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1675/report-thumb.jpg"},{"id":38672,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1675/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de6f2","contributors":{"authors":[{"text":"Roedder, Edwin","contributorId":25571,"corporation":false,"usgs":true,"family":"Roedder","given":"Edwin","affiliations":[],"preferred":false,"id":162166,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Belkin, H. E. 0000-0001-7879-6529","orcid":"https://orcid.org/0000-0001-7879-6529","contributorId":38160,"corporation":false,"usgs":true,"family":"Belkin","given":"H. E.","affiliations":[],"preferred":false,"id":162167,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9576,"text":"ofr79543 - 1979 - Geochemical analyses of rock, soil, and stream sediment samples from the Big Frog Wilderness Study Area, Polk County, Tennessee and Fannin County, Georgia","interactions":[],"lastModifiedDate":"2022-06-27T20:29:36.293164","indexId":"ofr79543","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-543","title":"Geochemical analyses of rock, soil, and stream sediment samples from the Big Frog Wilderness Study Area, Polk County, Tennessee and Fannin County, Georgia","docAbstract":"Semiquantitative spectrographic analyses for 31 elements and atomic absorption analyses for gold and zinc on 43 stream sediments, 5 panned concentrates, 65 soils, and 81 rock samples from the Big Frog Wilderness Study Area and vicinity, Polk County, Tennessee, and Fannin County, Georgia, are reported here in detail. Locations for all 194 samples are given in Universal Transverse Mercator (UTM) coordinates. Rocks analyzed include metasiltstone, metasandstone, metaconglomerate, slate, and vein quartz. The data contain no obviously anomalous values that might be related to economically recoverable mineralization.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79543","usgsCitation":"Hopkins, R., Meir, A., and Slack, J.F., 1979, Geochemical analyses of rock, soil, and stream sediment samples from the Big Frog Wilderness Study Area, Polk County, Tennessee and Fannin County, Georgia: U.S. Geological Survey Open-File Report 79-543, 16 p., https://doi.org/10.3133/ofr79543.","productDescription":"16 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":402560,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0543/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142885,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0543/report-thumb.jpg"}],"country":"United States","state":"Georgia, Tennessee","otherGeospatial":"Big Frog Wilderness Study Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.5580,\n 34.9830\n ],\n [\n -84.4850,\n 34.9830\n ],\n [\n -84.4850,\n 35.058104573869024\n ],\n [\n -84.5580,\n 35.058104573869024\n ],\n [\n -84.5580,\n 34.9830\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae8cf","contributors":{"authors":[{"text":"Hopkins, R.T.","contributorId":80264,"corporation":false,"usgs":true,"family":"Hopkins","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":159936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meir, A.L.","contributorId":93492,"corporation":false,"usgs":true,"family":"Meir","given":"A.L.","email":"","affiliations":[],"preferred":false,"id":159937,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Slack, John F. 0000-0001-6600-3130 jfslack@usgs.gov","orcid":"https://orcid.org/0000-0001-6600-3130","contributorId":1032,"corporation":false,"usgs":true,"family":"Slack","given":"John","email":"jfslack@usgs.gov","middleInitial":"F.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":true,"id":159935,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":30316,"text":"wri7974 - 1979 - Use of the STORM model for estimating the quantity and quality of runoff from the metropolitan area of Houston, Texas","interactions":[],"lastModifiedDate":"2016-08-09T12:15:17","indexId":"wri7974","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-74","title":"Use of the STORM model for estimating the quantity and quality of runoff from the metropolitan area of Houston, Texas","docAbstract":"The \"STORM\" model, developed by the U.S. Army Corps of Engineers, was selected from existing models and adapted to use available data to compute runoff from the Houston, Texas, area and to compute the loads and concentrations of biochemicaloxygen demand, dissolved solids, total phosphorus, total organic carbon, total nitrogen, and fecal-coliform bacteria. The water-quality data simulated by the STORM model will be used by the Texas Department of Water Resources to refine and verify a model of the Calveston Bay estuarine system.
\nDischarge and precipitation data for the 1975 water year and all available waterquality analyses were used to calibrate the model for the Buffalo, Whiteoak, Brays, Sims, Hunting, Greens, and Vince Bayous. Data for the 1974 water year were used to verify the model for discharge. After verification, the calibrations were adjusted to balance the difference between the 1974 and 1975 error predictions for discharge. The adjusted model was used with records of precipitation and evaporation to simulate a 20-vear record of the quantity and quality of runoff from the modeled area.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri7974","usgsCitation":"Waddell, K.M., Massey, B.C., and Jennings, M.E., 1979, Use of the STORM model for estimating the quantity and quality of runoff from the metropolitan area of Houston, Texas: U.S. Geological Survey Water-Resources Investigations Report 79-74, iv, 29 p., https://doi.org/10.3133/wri7974.","productDescription":"iv, 29 p.","numberOfPages":"35","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":59108,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0074/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":160405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0074/report-thumb.jpg"}],"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 -95.8941650390625,\n 29.463514026304715\n ],\n [\n -95.8941650390625,\n 30.197366063272245\n ],\n [\n -94.8944091796875,\n 30.197366063272245\n ],\n [\n -94.8944091796875,\n 29.463514026304715\n ],\n [\n -95.8941650390625,\n 29.463514026304715\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49cce4b07f02db5d9248","contributors":{"authors":[{"text":"Waddell, Kidd M.","contributorId":20720,"corporation":false,"usgs":true,"family":"Waddell","given":"Kidd","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":203043,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Massey, Bernard C.","contributorId":173558,"corporation":false,"usgs":false,"family":"Massey","given":"Bernard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":203044,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jennings, Marshall E.","contributorId":55813,"corporation":false,"usgs":true,"family":"Jennings","given":"Marshall","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":203042,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":4233,"text":"cir758 - 1979 - The Alaskan Mineral Resource Assessment Program: Guide to information contained in the folio of geologic and mineral resource maps of the Chandalar quadrangle, Alaska","interactions":[],"lastModifiedDate":"2021-10-28T21:20:35.184532","indexId":"cir758","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"758","title":"The Alaskan Mineral Resource Assessment Program: Guide to information contained in the folio of geologic and mineral resource maps of the Chandalar quadrangle, Alaska","docAbstract":"The Chandalar quadrangle in east-central Alaska was investigated by a multidisciplinary research group to assess the mineral resource potential of the quadrangle. This circular serves as a guide to and integrates with a folio of 10 miscellaneous field study (MF) maps and 2 open-file (OF) reports (table 1) concerned with the geology, geophysics, geochemistry, Landsat imagery, and mineral resources of the area. \r\n\r\nRevisions to the previously published Chandalar quadrangle geologic map, a new radiometric age determination, and a bibliography are also included.","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/cir758","usgsCitation":"Reiser, H.N., Brosge, W., DeYoung, J.H., Marsh, S., Hamilton, T.D., Cady, J.W., and Albert, N.R., 1979, The Alaskan Mineral Resource Assessment Program: Guide to information contained in the folio of geologic and mineral resource maps of the Chandalar quadrangle, Alaska: U.S. Geological Survey Circular 758, iii, 23 p., https://doi.org/10.3133/cir758.","productDescription":"iii, 23 p.","costCenters":[],"links":[{"id":31347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1979/0758/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1979/0758/report-thumb.jpg"},{"id":391120,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23883.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Chandalar quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -150,\n 68\n ],\n [\n -147,\n 68\n ],\n [\n -147,\n 67\n ],\n [\n -150,\n 67\n ],\n [\n -150,\n 68\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683460","contributors":{"authors":[{"text":"Reiser, H. N.","contributorId":13199,"corporation":false,"usgs":true,"family":"Reiser","given":"H.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":148503,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brosge, W. P.","contributorId":58248,"corporation":false,"usgs":true,"family":"Brosge","given":"W. P.","affiliations":[],"preferred":false,"id":148506,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeYoung, J. H.","contributorId":75908,"corporation":false,"usgs":true,"family":"DeYoung","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":148508,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Marsh, S.P.","contributorId":32913,"corporation":false,"usgs":true,"family":"Marsh","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":148504,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hamilton, T. D.","contributorId":36921,"corporation":false,"usgs":true,"family":"Hamilton","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":148505,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cady, J. W.","contributorId":81892,"corporation":false,"usgs":true,"family":"Cady","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":148509,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Albert, N. R. D.","contributorId":63789,"corporation":false,"usgs":true,"family":"Albert","given":"N.","email":"","middleInitial":"R. D.","affiliations":[],"preferred":false,"id":148507,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":11107,"text":"ofr791624 - 1979 - Principal facts for gravity stations of the Broadwater, Montana geothermal area","interactions":[],"lastModifiedDate":"2024-03-25T19:19:28.051022","indexId":"ofr791624","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1624","title":"Principal facts for gravity stations of the Broadwater, Montana geothermal area","docAbstract":"On October 31, November 1 and 3, 1978, forty-eight gravity stations were established near Helena, in the Broadwater geothermal area, west-central Montana (fig. 1).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791624","usgsCitation":"Senterfit, R.M., 1979, Principal facts for gravity stations of the Broadwater, Montana geothermal area: U.S. Geological Survey Open-File Report 79-1624, 7 p., https://doi.org/10.3133/ofr791624.","productDescription":"7 p.","costCenters":[],"links":[{"id":427058,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1624/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143488,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1624/report-thumb.jpg"}],"country":"United States","state":"Montana","city":"Helena","otherGeospatial":"Broadwater geothermal area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -112.86634659331804,\n 47.097587251123485\n ],\n [\n -112.86634659331804,\n 46.65915069903153\n ],\n [\n -112.19218858451427,\n 46.65915069903153\n ],\n [\n -112.19218858451427,\n 47.097587251123485\n ],\n [\n -112.86634659331804,\n 47.097587251123485\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667657","contributors":{"authors":[{"text":"Senterfit, R. Michael","contributorId":10791,"corporation":false,"usgs":true,"family":"Senterfit","given":"R.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":162554,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63685,"text":"gp925 - 1979 - Bouguer gravity and geologic map of northeast Arkansas","interactions":[],"lastModifiedDate":"2021-11-02T21:35:25.449042","indexId":"gp925","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"925","title":"Bouguer gravity and geologic map of northeast Arkansas","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp925","usgsCitation":"Hendricks, J.D., 1979, Bouguer gravity and geologic map of northeast Arkansas: U.S. Geological Survey Geophysical Investigations Map 925, 1 Plate: 44.04 × 30.00 inches, https://doi.org/10.3133/gp925.","productDescription":"1 Plate: 44.04 × 30.00 inches","costCenters":[],"links":[{"id":391294,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6269.htm"},{"id":260535,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0925/plate-1.pdf"},{"id":187230,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","country":"United States","state":"Arkansas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92,35 ], [ -92,36.5 ], [ -90.5083,36.5 ], [ -90.5083,35 ], [ -92,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601e91","contributors":{"authors":[{"text":"Hendricks, J. D.","contributorId":40187,"corporation":false,"usgs":true,"family":"Hendricks","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":269377,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4228,"text":"cir783 - 1979 - The Alaskan Mineral Resource Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Big Delta quadrangle, Alaska","interactions":[],"lastModifiedDate":"2021-10-28T21:08:43.149578","indexId":"cir783","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"783","title":"The Alaskan Mineral Resource Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Big Delta quadrangle, Alaska","docAbstract":"The geology, geochemistry, geophysics, and Landsat imagery of the Big Delta quadrangle, 16,335 km 2 in the Yukon-Tanana Upland of east-central Alaska, were investigated, and maps and reports were prepared by an interdisciplinary research team for the purpose of assessing the mineral potential. The quadrangle is dominantly a complex terrane of greenschist- to amphibolitefacies metamorphic rocks that have been intruded by Mesozoic and Tertiary dioritic to granitic rocks and are overlain by Tertiary sedimentary and volcanic rocks. Serpentinized peridotite and associated greenstone, graywacke, and chert crop out in some places. \r\n\r\nThe quadrangle is bisected by the northeastward-trending Shaw Creek fault, which, on the basis of aeromagnetic interpretation and geologic data, is postulated to have left-lateral offset of as much as 48 km. On the northwest side of the Shaw Creek fault, metamorphic rock units have a northwesterly regional trend, and the oldest rocks could be Precambrian in age. Gneiss and schist in the southwestern part of the quadrangle are derived from both igneous and sedimentary protoliths, some of which may be as old as Precambrian. Other rock units, which include calcareous schist and thin-layered marble, black quartzite, semischist, and cataclastic rocks, are considered to be of probable Paleozoic age, although no fossils have yet been found in these rocks. Radiolarians and conodonts in chert associated with greenstone and ultramafic rocks indicate that the chert is of Permian age. \r\n\r\nPotassium-argon ages on igneous rocks of the Big Delta quadrangle fall into two groups: those with biotite, muscovite, hornblende, and sanidine ages between 50 to 69 m.y.; and those with biotite, hornblende, and sanidine ages between 88 to 105 m.y. The younger of these two groups appears to indicate the time of a plutonic event marked by intrusion of mostly small, isolated plutons, including hypabyssal stocks, and the eruption of silicic volcanic rocks. Most of the plutons are quartz monzonite to granite. \r\n\r\nThe older group of ages (88 to 105 m.y.) on igneous rocks includes ages on the largest plutons of the Yukono-Tanana Upland. The rocks range from diorite to quartz monzonite in composition. The potassium-argon ages on the metamorphic rocks of the Big Delta quadrangle, like those obtained elsewhere in the Yukon-Tanana Upland, appear to have been partly or completely reset by subsequent thermal events. \r\n\r\nVein and placer gold deposits have been mined in the Big Delta quadrangle, and although indications of mineralization are widespread, no other mineral deposits have yet been identified. The geologic, geochemical, and geophysical data are compatible with several types of deposits, including porphyry copper, massive sulfide, and skarn deposits. In certain aspects, the geology of the quadrangle is similar to areas in the eastern part of the Yukon-Tanana Upland and Canada where mineral deposits are known.","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/cir783","usgsCitation":"Foster, H.L., Albert, N.R., Griscom, A., Hessin, T., Menzie, W., Turner, D.L., and Wilson, F.H., 1979, The Alaskan Mineral Resource Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Big Delta quadrangle, Alaska: U.S. Geological Survey Circular 783, iii, 19 p., https://doi.org/10.3133/cir783.","productDescription":"iii, 19 p.","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":31342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1979/0783/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139243,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1979/0783/report-thumb.jpg"},{"id":391117,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23992.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"Big Delta quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -147,\n 64\n ],\n [\n -144,\n 64\n ],\n [\n -144,\n 65\n ],\n [\n -147,\n 65\n ],\n [\n -147,\n 64\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a276","contributors":{"authors":[{"text":"Foster, Helen Laura","contributorId":21936,"corporation":false,"usgs":true,"family":"Foster","given":"Helen","email":"","middleInitial":"Laura","affiliations":[],"preferred":false,"id":148472,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Albert, N. R. D.","contributorId":63789,"corporation":false,"usgs":true,"family":"Albert","given":"N.","email":"","middleInitial":"R. D.","affiliations":[],"preferred":false,"id":148477,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":148473,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hessin, T. D.","contributorId":42181,"corporation":false,"usgs":true,"family":"Hessin","given":"T. D.","affiliations":[],"preferred":false,"id":148474,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Menzie, W. D.","contributorId":52916,"corporation":false,"usgs":true,"family":"Menzie","given":"W. D.","affiliations":[],"preferred":false,"id":148475,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Turner, D. L.","contributorId":53776,"corporation":false,"usgs":true,"family":"Turner","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":148476,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":148471,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":1142,"text":"wsp1757O - 1979 - The corrosive well waters of Egypt's western desert","interactions":[{"subject":{"id":18481,"text":"ofr78892 - 1978 - The corrosive well waters of Egypt's Western Desert","indexId":"ofr78892","publicationYear":"1978","noYear":false,"title":"The corrosive well waters of Egypt's Western Desert"},"predicate":"SUPERSEDED_BY","object":{"id":1142,"text":"wsp1757O - 1979 - The corrosive well waters of Egypt's western desert","indexId":"wsp1757O","publicationYear":"1979","noYear":false,"chapter":"O","title":"The corrosive well waters of Egypt's western desert"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1757O","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"1757","chapter":"O","title":"The corrosive well waters of Egypt's western desert","docAbstract":"The discovery that ground waters of Egypt's Western Desert are highly corrosive is lost in antiquity. Inhabitants of the oases have been aware of the troublesome property for many decades and early investigators mention it in their reports concerning the area. Introduction of modern well-drilling techniques and replacements of native wood casing with steel during the 20th century increased corrosion problems and, in what is called the New Valley Project, led to an intense search for causes and corrective treatments. This revealed that extreme corrosiveness results from combined effects of relatively acidic waters with significant concentrations of destructive sulfide ion; unfavorable ratios of sulfate and chloride to less aggressive ions; mineral equilibria and electrode potential which hinder formation of protective films; relative high chemical reaction rates because of abnormal temperatures, and high surface velocities related to well design. \r\n\r\nThere is general agreement among investigators that conventional corrosion control methods such as coating metal surfaces, chemical treatment of the water, and electrolytic protection with impressed current and sacrificial electrodes are ineffective or impracticable for wells in the Western Desert's New Valley. Thus, control must be sought through the use of materials more resistant to corrosion than plain carbon steel wherever well screens and casings are necessary. Of the alternatives considered, stainless steel appears to. be the most promising where high strength and long-term services are required and the alloy's relatively high cost is acceptable. Epoxy resin-bonded fiberglass and wood appear to be practicable, relatively inexpensive alternatives for installations which do. not exceed their strength limitations. Other materials such as high strength aluminum and Monel Metal have shown sufficient promise to. merit their consideration in particular locations and uses. The limited experience with pumping in these desert wells leaves uncertainties concerning the durability of conventional pump designs. \r\n\r\nEgypt's New Valley Project provides an excellent opportunity for continuing study of the corrosion problems that concern ground-water developers in many parts of the world.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1757O","usgsCitation":"Clarke, F., 1979, The corrosive well waters of Egypt's western desert: U.S. Geological Survey Water Supply Paper 1757, v, 55 p. : ill., maps ; 24 cm., https://doi.org/10.3133/wsp1757O.","productDescription":"v, 55 p. : ill., maps ; 24 cm.","costCenters":[],"links":[{"id":137610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1757o/report-thumb.jpg"},{"id":25923,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1757o/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db66890d","contributors":{"authors":[{"text":"Clarke, Frank Eldridge","contributorId":107255,"corporation":false,"usgs":true,"family":"Clarke","given":"Frank Eldridge","affiliations":[],"preferred":false,"id":143248,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26434,"text":"wri7873 - 1979 - Connector well experiment to recharge the Floridan Aquifer, East Orange County, Florida","interactions":[],"lastModifiedDate":"2019-11-07T11:25:09","indexId":"wri7873","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"78-73","title":"Connector well experiment to recharge the Floridan Aquifer, East Orange County, Florida","docAbstract":"An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer, and cased through the confining layer between the two aquifers, was drilled in east Orange County, Florida, to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiometric surface of the Floridan aquifer; hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well ' connecting ' the two aquifers. Continuous flow measurement over 10 months shows the well discharge varies seasonally and averages slightly more than 50 gallons per minute. Observation wells show that, except for seasonal variation water levels within the area of influence have reached steady state within measurable limits. Vertical anisotrophy in the shallow aquifer is apparently caused by the shape and (or) arrangement of the sand grains that comprise the shallow aquifer , rather than distinct confining layers of different lithology. Transmissivity of the shallow aquifer at the site is about 600 square feet per day. Extensive dewatering of wetlands in east Orange County by connector wells alone is probably not feasible. Nevertheless, large amounts of water could be channeled to the Floridan aquifer by connector wells. The results of the connector well experiment imply that water is being captured from evapotranspiration and runoff in the vicinity of the connector well. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7873","usgsCitation":"Bush, P.W., 1979, Connector well experiment to recharge the Floridan Aquifer, East Orange County, Florida: U.S. Geological Survey Water-Resources Investigations Report 78-73, iv, 40 p. , https://doi.org/10.3133/wri7873.","productDescription":"iv, 40 p. ","costCenters":[],"links":[{"id":158122,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0073/report-thumb.jpg"},{"id":369036,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Orange County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.25350952148438,\n 28.365422796841774\n ],\n [\n -80.89508056640625,\n 28.365422796841774\n ],\n [\n -80.89508056640625,\n 28.612856636438657\n ],\n [\n -81.25350952148438,\n 28.612856636438657\n ],\n [\n -81.25350952148438,\n 28.365422796841774\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69740b","contributors":{"authors":[{"text":"Bush, P. W.","contributorId":14826,"corporation":false,"usgs":true,"family":"Bush","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":196386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40324,"text":"ofr79143 - 1979 - Coal resource occurrence and coal development potential maps of the Thayer Junction Quadrangle, Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:06","indexId":"ofr79143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-143","title":"Coal resource occurrence and coal development potential maps of the Thayer Junction Quadrangle, Sweetwater County, Wyoming","language":"ENGLISH","doi":"10.3133/ofr79143","usgsCitation":"Dames & Moore, 1979, Coal resource occurrence and coal development potential maps of the Thayer Junction Quadrangle, Sweetwater County, Wyoming: U.S. Geological Survey Open-File Report 79-143, 8 maps and 1 data sheet ;58 x 44 cm.; 21 p., https://doi.org/10.3133/ofr79143.","productDescription":"8 maps and 1 data sheet ;58 x 44 cm.; 21 p.","costCenters":[],"links":[{"id":136807,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0143/report-thumb.jpg"},{"id":72575,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0143/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72576,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0143/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72577,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0143/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72578,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0143/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72579,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0143/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72580,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0143/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72581,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0143/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72582,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0143/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72583,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72574,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0143/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6afc08","contributors":{"authors":[{"text":"Dames & Moore","contributorId":127975,"corporation":true,"usgs":false,"organization":"Dames & Moore","id":530130,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11189,"text":"ofr791209 - 1979 - Mineral resources of the Big Frog Wilderness Study Area, Polk County, Tennessee and Fannin County, Georgia","interactions":[],"lastModifiedDate":"2023-11-21T22:01:17.934418","indexId":"ofr791209","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1209","title":"Mineral resources of the Big Frog Wilderness Study Area, Polk County, Tennessee and Fannin County, Georgia","docAbstract":"The proposed Big Frog Wilderness is comprised of approximately 1820 hectares (18.2 km2) of mountainous terrain in the Cherokee and Chattahoochee National Forests south of the Ocoee River in Polk County, Tennessee, and Fannin County, Georgia. Rocks of the study area are greenschist-facies metasandstone, meta-arkose, metagraywacke, and dark slate of the Ocoee Supergroup of late Precambrian age. A major thrust fault, correlated with the Greenbrier Fault, separates fine-grained slaty rocks of the Snowbird Group on the northwest side, from coarse clastic sediments and interbedded slates of the Great Smoky Group on the southeast. North- and northeast-trending folds are common in the map area. Minor deposits of Quaternary sand and gravel occur locally in the lower parts of large streams.
Semiquantitative spectrographic, atomic absorption, and selected fire assay analyses were done on more than 200 samples of rock, soil, and stream sediment. No significant metal anomalies were found for 31 major, minor, and trace elements. In many places, metasiltstone and metasandstone contain trace amounts of chalcopyrite and sphalerite as microscopic intergrowths with the chief sulfide minerals, pyrite and pyrrhotite. Sulfides make up as much as 5 to 10 percent of some rocks and provide concentrations of Cu, Zn, and As slightly higher than background in samples of rock and soil. Rocks containing these disseminated base-metal sulfides are of insufficient grade to have current economic potential, however.
No metallic mineral resources are known within the proposed Big Frog Wilderness. Nonmetallic resources, including slate and phyllite, stone, and sand and gravel are present locally, but are not presently a value because similar resources exist closer to markets outside the study area. These deposits therefore would have only marginal use in the region.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791209","usgsCitation":"Slack, J.F., Gazdik, G.C., and Dunn, M., 1979, Mineral resources of the Big Frog Wilderness Study Area, Polk County, Tennessee and Fannin County, Georgia: U.S. Geological Survey Open-File Report 79-1209, iv, 39 p., https://doi.org/10.3133/ofr791209.","productDescription":"iv, 39 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":144688,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1209/report-thumb.jpg"},{"id":422792,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1209/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia, Tennessee","county":"Fannin County, Polk County","otherGeospatial":"Big Frog Wilderness Study Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.5580,\n 34.9830\n ],\n [\n -84.4850,\n 34.9830\n ],\n [\n -84.4850,\n 35.058104573869024\n ],\n [\n -84.5580,\n 35.058104573869024\n ],\n [\n -84.5580,\n 34.9830\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b2f5","contributors":{"authors":[{"text":"Slack, John F. 0000-0001-6600-3130 jfslack@usgs.gov","orcid":"https://orcid.org/0000-0001-6600-3130","contributorId":1032,"corporation":false,"usgs":true,"family":"Slack","given":"John","email":"jfslack@usgs.gov","middleInitial":"F.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":162697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gazdik, Gertrude C.","contributorId":56220,"corporation":false,"usgs":true,"family":"Gazdik","given":"Gertrude","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":162699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunn, Maynard L.","contributorId":40225,"corporation":false,"usgs":true,"family":"Dunn","given":"Maynard L.","affiliations":[],"preferred":false,"id":162698,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":40321,"text":"ofr79312 - 1979 - Coal resource occurrence and coal development potential maps of the Teckla Quadrangle, Campbell County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:06","indexId":"ofr79312","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-312","title":"Coal resource occurrence and coal development potential maps of the Teckla Quadrangle, Campbell County, Wyoming","language":"ENGLISH","doi":"10.3133/ofr79312","usgsCitation":"IntraSearch Inc., 1979, Coal resource occurrence and coal development potential maps of the Teckla Quadrangle, Campbell County, Wyoming: U.S. Geological Survey Open-File Report 79-312, 13 maps and 2 data sheets ;58 x 43 cm.; 28 p., https://doi.org/10.3133/ofr79312.","productDescription":"13 maps and 2 data sheets ;58 x 43 cm.; 28 p.","costCenters":[],"links":[{"id":136804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0312/report-thumb.jpg"},{"id":72519,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72520,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72521,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72522,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72523,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72524,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72525,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72526,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72527,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72528,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72529,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72530,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72531,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72532,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72533,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/0312/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":72534,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0312/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6afb0d","contributors":{"authors":[{"text":"IntraSearch Inc.","contributorId":128289,"corporation":true,"usgs":false,"organization":"IntraSearch Inc.","id":530127,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10994,"text":"ofr79768 - 1979 - A model of the strain response of Barre Granite to wetting and drying","interactions":[],"lastModifiedDate":"2022-01-03T18:27:28.382312","indexId":"ofr79768","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-768","title":"A model of the strain response of Barre Granite to wetting and drying","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79768","usgsCitation":"Savage, W.Z., 1979, A model of the strain response of Barre Granite to wetting and drying: U.S. Geological Survey Open-File Report 79-768, i, 17 p., https://doi.org/10.3133/ofr79768.","productDescription":"i, 17 p.","costCenters":[],"links":[{"id":143363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0768/report-thumb.jpg"},{"id":393764,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0768/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf69","contributors":{"authors":[{"text":"Savage, William Z.","contributorId":107686,"corporation":false,"usgs":true,"family":"Savage","given":"William","email":"","middleInitial":"Z.","affiliations":[],"preferred":false,"id":162346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11758,"text":"ofr791126 - 1979 - Stratigraphic sections of Jurassic San Rafael Group and adjacent rocks in Wayne County, Utah","interactions":[],"lastModifiedDate":"2023-11-24T17:57:17.06326","indexId":"ofr791126","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","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":"79-1126","title":"Stratigraphic sections of Jurassic San Rafael Group and adjacent rocks in Wayne County, Utah","docAbstract":"These sections were measured prior to 1960, before adoption of the metric system. Publication was delayed by other assignments of the authors and later by the untimely death of J. C. Wright. They are being released at this time because of the increased interest in the uranium potential of Jurassic rocks. The Summerville, Curtis, Entrada, and Carmel Formations are the formations of the San Rafael Group present in these sections.
No abstract available.
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The purpose of this experiment is to search for possible premonitory radon signals that may be useful for earthquake prediction.
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