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Location information, including distance of nearby towns or other landmarks, latitude and longitude coordinates, county in which the site lies, and the name of the latest topographic maps on which the site is located, are also provided.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83211","usgsCitation":"Meikle, R.L., 1983, Drainage areas of selected sites on streams in North Carolina: U.S. Geological Survey Open-File Report 83-211, iv, 167 p. maps ;28 cm., https://doi.org/10.3133/ofr83211.","productDescription":"iv, 167 p. maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":38147,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0211/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0211/report-thumb.jpg"}],"country":"United States","state":"North 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,{"id":11003,"text":"ofr81918 - 1983 - Geothermal resources of the western arm of the Black Rock Desert, northwestern Nevada: Part I, geology and geophysics","interactions":[],"lastModifiedDate":"2022-10-17T15:30:14.608693","indexId":"ofr81918","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-918","title":"Geothermal resources of the western arm of the Black Rock Desert, northwestern Nevada: Part I, geology and geophysics","docAbstract":"<p>Studies of the geothermal potential of the western arm of the Black Rock Desert in northwestern Nevada included a compilation of existing geologic data on a detailed map, a temperature survey at 1-meter depth, a thermal-scanner survey, and gravity and seismic surveys to determine basin geometry. The temperature survey showed the effects of heating at shallow depths due to rising geothermal fluids near the known hot spring areas. Lower temperatures were noted in areas of probable near-surface ground-water movement. The thermal-scanner survey verified the known geothermal areas and showed relatively high-temperature areas of standing water and ground-water discharge. The upland areas of the desert were found to be distinctly warmer than the playa area, probably due to low thermal diffusivity resulting from low moisture content. The surface geophysical surveys indicated that the maximum thickness of valley-fill deposits in the desert is about 3,200 meters. Gravity data further showed that changes in the trend of the desert axis occurred near thermal areas.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81918","usgsCitation":"Schaefer, D.H., Welch, A., and Mauzer, D.K., 1983, Geothermal resources of the western arm of the Black Rock Desert, northwestern Nevada: Part I, geology and geophysics: U.S. Geological Survey Open-File Report 81-918, Report: v, 37 p.; 4 Plates: 21.24 × 35.96 inches or smaller, https://doi.org/10.3133/ofr81918.","productDescription":"Report: v, 37 p.; 4 Plates: 21.24 × 35.96 inches or smaller","costCenters":[],"links":[{"id":144063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0918/report-thumb.jpg"},{"id":38767,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0918/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38768,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0918/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38769,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0918/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38770,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0918/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38771,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0918/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":408004,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12207.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nevada","otherGeospatial":"Black Rock Desert","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.542,\n              40.584\n            ],\n            [\n              -118.825,\n              40.584\n            ],\n            [\n              -118.825,\n              41.521\n            ],\n            [\n              -119.542,\n              41.521\n            ],\n            [\n              -119.542,\n              40.584\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ad41","contributors":{"authors":[{"text":"Schaefer, Donald H.","contributorId":77507,"corporation":false,"usgs":true,"family":"Schaefer","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welch, Alan H.","contributorId":45286,"corporation":false,"usgs":true,"family":"Welch","given":"Alan H.","affiliations":[],"preferred":false,"id":162358,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mauzer, Douglas K.","contributorId":44922,"corporation":false,"usgs":true,"family":"Mauzer","given":"Douglas","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":162357,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10521,"text":"ofr83865 - 1983 - Hydrologic data for the Great and Denbow heaths in eastern Maine, October 1981 through October 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr83865","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-865","title":"Hydrologic data for the Great and Denbow heaths in eastern Maine, October 1981 through October 1982","docAbstract":"Hydrologic data collected on the Great and Denbow Heaths, Maine, include precipitation, pan evaporation, air temperatures, streamflow, and ground water levels. These data were collected for a peat bog hydrology study conducted in cooperation with the Maine Geological Survey. The data network consisted of climate information from three rain gages, an evaporation pan and two maximum-minimum thermometers; surface water information from two continuous gaging stations and 19 partial record sites; groundwater information from an observation well equipped with a continuous recorder and 106 piezometers. Methods used for the collection and analyses of data included standard Survey techniques modified for the unique hydrologic environment of the study area. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83865","usgsCitation":"Nichols, W.J., 1983, Hydrologic data for the Great and Denbow heaths in eastern Maine, October 1981 through October 1982: U.S. Geological Survey Open-File Report 83-865, 34 p. :maps ;28 cm., https://doi.org/10.3133/ofr83865.","productDescription":"34 p. :maps ;28 cm.","costCenters":[],"links":[{"id":144248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0865/report-thumb.jpg"},{"id":38370,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0865/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c79f","contributors":{"authors":[{"text":"Nichols, Wallace J.","contributorId":81106,"corporation":false,"usgs":false,"family":"Nichols","given":"Wallace","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161536,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8652,"text":"ofr81688 - 1983 - Application of Gauss algorithm and Monte Carlo simulation to the identification of aquifer parameters","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr81688","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"81-688","title":"Application of Gauss algorithm and Monte Carlo simulation to the identification of aquifer parameters","docAbstract":"The Gauss optimization technique can be used to identify the parameters of a model of a groundwater system for which the parameter identification problem is formulated as a least squares comparison between the response of the prototype and the response of the model. Unavoidable uncertainty in the true stress on the prototype and in the true response of the prototype to that stress will introduce errors into the parameter identification problem. A method for evaluating errors in the predictions of future water levels due to errors in recharge estimates was demonstrated. The method involves a Monte Carlo simulation of the parameter identification problem and of the prediction problem. The steps in the method are: (1) to prescribe the distribution of the recharge estimates; (2) to use this distribution to generate random sets of recharge estimates; (3) to use the Gauss optimization technique to identify the corresponding set of parameter estimates for each set of recharge estimates; (4) to make the corresponding set of hydraulic head predictions for each set of parameter estimates; and (5) to examine the distribution of hydraulic head predictions and to draw appropriate conclusions. Similarly, the method can be used independently or simultaneously to estimate the effect on hydraulic head predictions of errors in the measured water levels that are used in the parameter identification problem. The fit of the model to the data that are used to identify parameters is not a good indicator of these errors. A Monte Carlo simulation of the parameter identification problem can be used, however, to evaluate the effects on water level predictions of errors in the recharge (and pumpage) data used in the parameter identification problem. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81688","usgsCitation":"Durbin, T.J., 1983, Application of Gauss algorithm and Monte Carlo simulation to the identification of aquifer parameters: U.S. Geological Survey Open-File Report 81-688, 30 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr81688.","productDescription":"30 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":141229,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0688/report-thumb.jpg"},{"id":36246,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0688/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ac3c","contributors":{"authors":[{"text":"Durbin, Timothy J.","contributorId":63373,"corporation":false,"usgs":true,"family":"Durbin","given":"Timothy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158095,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9544,"text":"ofr82440 - 1983 - Hydrology of area 20, Eastern Coal Province, Tennessee, Georgia and Alabama","interactions":[],"lastModifiedDate":"2024-09-23T22:12:54.319025","indexId":"ofr82440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-440","title":"Hydrology of area 20, Eastern Coal Province, Tennessee, Georgia and Alabama","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82440","usgsCitation":"Hollyday, E., 1983, Hydrology of area 20, Eastern Coal Province, Tennessee, Georgia and Alabama: U.S. Geological Survey Open-File Report 82-440, v, 145 p., https://doi.org/10.3133/ofr82440.","productDescription":"v, 145 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":462159,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13725.htm","linkFileType":{"id":5,"text":"html"}},{"id":94931,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0440/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142669,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0440/report-thumb.jpg"}],"country":"United States","state":"Alabama, Georgia, Tennessee","otherGeospatial":"Eastern Coal Province","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -86.15478515625,\n              34.38877925439021\n            ],\n            [\n              -86.15478515625,\n              35.8356283888737\n            ],\n            [\n              -84.869384765625,\n              35.8356283888737\n            ],\n            [\n              -84.869384765625,\n              34.38877925439021\n            ],\n            [\n              -86.15478515625,\n              34.38877925439021\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602d35","contributors":{"authors":[{"text":"Hollyday, E. F.","contributorId":95062,"corporation":false,"usgs":true,"family":"Hollyday","given":"E. F.","affiliations":[],"preferred":false,"id":159866,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9548,"text":"ofr83688 - 1983 - Ground-water hydrology and projected effects of ground-water withdrawals in the Sevier Desert, Utah","interactions":[{"subject":{"id":9548,"text":"ofr83688 - 1983 - Ground-water hydrology and projected effects of ground-water withdrawals in the Sevier Desert, Utah","indexId":"ofr83688","publicationYear":"1983","noYear":false,"title":"Ground-water hydrology and projected effects of ground-water withdrawals in the Sevier Desert, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043935,"text":"70043935 - 1984 - Ground-water hydrology and projected effects of ground-water withdrawals in the Sevier Desert, Utah","indexId":"70043935","publicationYear":"1984","noYear":false,"title":"Ground-water hydrology and projected effects of ground-water withdrawals in the Sevier Desert, Utah"},"id":1}],"supersededBy":{"id":70043935,"text":"70043935 - 1984 - Ground-water hydrology and projected effects of ground-water withdrawals in the Sevier Desert, Utah","indexId":"70043935","publicationYear":"1984","noYear":false,"title":"Ground-water hydrology and projected effects of ground-water withdrawals in the Sevier Desert, Utah"},"lastModifiedDate":"2021-01-26T20:37:05.014399","indexId":"ofr83688","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-688","title":"Ground-water hydrology and projected effects of ground-water withdrawals in the Sevier Desert, Utah","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83688","usgsCitation":"Holmes, W.F., 1983, Ground-water hydrology and projected effects of ground-water withdrawals in the Sevier Desert, Utah: U.S. Geological Survey Open-File Report 83-688, Report: 54 p.; 1 Plate: 23.62 x 23.57 inches, https://doi.org/10.3133/ofr83688.","productDescription":"Report: 54 p.; 1 Plate: 23.62 x 23.57 inches","costCenters":[],"links":[{"id":141663,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0688/report-thumb.jpg"},{"id":382617,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0688/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382616,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0688/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Sevier Desert","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.0380859375,\n              38.45789034424927\n            ],\n            [\n              -112.0440673828125,\n              38.45789034424927\n            ],\n            [\n              -112.0440673828125,\n              39.436192999314095\n            ],\n            [\n              -114.0380859375,\n              39.436192999314095\n            ],\n            [\n              -114.0380859375,\n              38.45789034424927\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668d50","contributors":{"authors":[{"text":"Holmes, Walter F.","contributorId":31737,"corporation":false,"usgs":true,"family":"Holmes","given":"Walter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":159872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9549,"text":"ofr83271 - 1983 - Ground water in the southeastern Uinta Basin, Utah and Colorado","interactions":[{"subject":{"id":9549,"text":"ofr83271 - 1983 - Ground water in the southeastern Uinta Basin, Utah and Colorado","indexId":"ofr83271","publicationYear":"1983","noYear":false,"title":"Ground water in the southeastern Uinta Basin, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":1903,"text":"wsp2248 - 1987 - Ground water in the southeastern Uinta Basin, Utah and Colorado","indexId":"wsp2248","publicationYear":"1987","noYear":false,"title":"Ground water in the southeastern Uinta Basin, Utah and Colorado"},"id":1}],"supersededBy":{"id":1903,"text":"wsp2248 - 1987 - Ground water in the southeastern Uinta Basin, Utah and Colorado","indexId":"wsp2248","publicationYear":"1987","noYear":false,"title":"Ground water in the southeastern Uinta Basin, Utah and Colorado"},"lastModifiedDate":"2021-03-05T02:11:45.24522","indexId":"ofr83271","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-271","title":"Ground water in the southeastern Uinta Basin, Utah and Colorado","docAbstract":"<p><span>The potential for developing oil-shale resources in the southeastern </span><span>Uinta Basin of Utah and Colorado has created the need for information on the </span><span>quantity and quality of water available in the area. This report describes </span><span>the availability and chemical quality of ground water, which might provide a </span><span>source or supplement of water supply for an oil-shale industry. </span></p><p><span>Ground water in the southeastern Uinta Basin occurs in three major aquifers. Alluvial aquifers of small areal extent are present in valley-fill deposits of six major drainages. Consolidated-rock aquifers include the bird's-nest aquifer in the Parachute Creek Member of the Green River Formation, which is limited to the central part of the study area; and the Douglas Creek aquifer, which includes parts of the Douglas Creek Member of the Green River Formation and parts of the intertonguing Renegade Tongue of the Wasatch Formation; this aquifer underlies most of the study area. </span></p><p><span>The alluvial aquifers are recharged by infiltration of streamflow and leakage from consolidated-rock aquifers. Recharge is estimated to average about 32,000 acre-feet per year. Discharge from alluvial aquifers, primarily by evapotranspiration, also averages about 32,000 acre-feet per year. The estimated volume of recoverable water in storage in alluvial aquifers is about 200,000 acre-feet. Maximum yields to individual wells are less than 1,000 gallons per minute. </span></p><p><span>Recharge to the bird's-nest aquifer, primarily from stream infiltration and downward leakage from the overlying Uinta Formation, is estimated to average 670 acre-feet per year. Discharge from the bird's-nest aquifer, which is primarily by seepage to Bitter Creek and the White River, is estimated to be 670 acre-feet per year. The estimated volume of recoverable water in storage in the bird's-nest aquifer is 1.9 million acre-feet. Maximum yields to individual wells in some areas may be as much as 5,000 gallons per minute. </span></p><p><span>A digital-computer model of the flow system was used to evaluate the effects of oil-shale development on the bird's-nest aquifer at the Federal lease tracts Ua and Ub. Results of model simulations indicate that during construction of a vertical access shaft, a pumping rate of about 900 gallons per minute would be required to dewater the aquifer. The model also indicates that the construction of a proposed reservoir on the White River may raise water levels in the bird's-nest aquifer near the reservoir site by as much as 45 feet. </span></p><p><span>The flow model was used to evaluate the potential ground-water supply available for oil-shale development in the vicinity of the Federal lease tracts Ua and Ub. The results of the simulation indicate that the bird's-nest aquifer could supply about 10,000 acre-feet of water per year at that site, for a period of 20 years. Drawdown after 20 years of pumping would exceed 250 feet near the simulated well field. Based on the results of the model simulation, it is estimated that the aquifer could simultaneously supply another 10,000 acre-feet of water per year in the northern part of the study area, but some interference between well fields could be expected. </span></p><p><span>The Douglas Creek aquifer is recharged by precipitation and stream infiltration at an average rate of about 20,000 acre-feet per year. Discharge is estimated to be about the same and is primarily through springs and diffuse seepage. The estimated volume of recoverable water in storage is 16 million acre-feet. Maximum yields to individual wells are estimated to be less than 500 gallons per minute.</span></p><div class=\"page\" data-page-number=\"16\" data-loaded=\"true\"><div class=\"textLayer\"><span>A model of the flow system in the Douglas Creek aquifer indicates that </span><span>the aquifer could supply about 700 acre-feet of water per year for oil-shale </span><span>development at Federal lease tracts Ua and Ub and at the TOSCO Corp. site. </span><span>After 20 years of pumping, water levels in production wells would be near the </span><span>base of the aquifer. Based on the results of the model simulation, it is </span><span>estimated that the aquifer could supply another 700 acre-feet of water per </span><span>year in the southern part of the modeled area, but some interference between </span><span>wells could be expected.</span></div><div class=\"textLayer\"><span><br data-mce-bogus=\"1\"></span></div></div><div class=\"page\" data-page-number=\"17\" data-loaded=\"true\"><div class=\"textLayer\"><span>Chemical quality of the ground water in the southeastern Uinta Basin </span><span>varies considerably. Water from alluvial wells ranges from about 440 to </span><span>27,800 milligrams per liter of dissolved solids. Water from two consolidated-</span><span>rock aquifers has dissolved-solids concentrations ranging from 870 to 5,810 </span><span>milligrams per liter in the bird's-nest aquifer, and from 640 to 6,100 </span><span>milligrams per liter in the Douglas Creek aquifer. Water from alluvial wells </span><span>generally is a sodium sulfate type, whereas water in both the consolidated-</span><span>rock aquifers generally changes from a sodium sulfate type to a sodium </span><span>bicarbonate type. All ground water is very alkaline, and the alluvial </span><span>aquifers contain very hard water. None of the water is suitable for public </span><span>supply, but all the water could be used for industrial purposes such as </span><span>washing and cooling.</span></div><div class=\"textLayer\"><span><br data-mce-bogus=\"1\"></span></div></div><div class=\"page\" data-page-number=\"18\" data-loaded=\"true\"><div class=\"textLayer\"><span>Changes in chemical composition of the ground water can be attributed to </span><span>several physiochemical processes, including mineral precipitation and </span><span>dissolution, oxidation and reduction, mixing, ion exchange, and evaporative </span><span>concentration. Mass-transfer modeling of these processes shows how they can </span><span>account for the variability in the ground-water quality. The mass-transfer </span><span>model of the Bitter Creek alluvial aquifer shows that evaporative </span><span>concentration, combined with precipitation of calcite, dolomite, gypsum, and </span><span>release of carbon dioxide to the atmosphere results in the documented changes </span><span>in pH and dissolved solids in the water. The water-quality changes in the </span><span>consolidated-rock aquifers are a result of precipitation of calcium carbonate </span><span>and perhaps dolomite (calcium magnesium carbonate) with the reduction of </span><span>sulfate by organic carbon, as well as ion exchange of magnesium for sodium. </span><span>These processes result in large values of pH and alkalinity in the water. </span></div></div><div class=\"page\" data-page-number=\"19\" data-loaded=\"true\"></div><div class=\"page\" data-page-number=\"20\" data-loaded=\"true\"><div class=\"textLayer\"><br data-mce-bogus=\"1\"></div></div>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83271","usgsCitation":"Holmes, W.F., and Kimball, B.A., 1983, Ground water in the southeastern Uinta Basin, Utah and Colorado: U.S. Geological Survey Open-File Report 83-271, Report: 138 p.; 1 Plate: 21.65 x 29.42 inches, https://doi.org/10.3133/ofr83271.","productDescription":"Report: 138 p.; 1 Plate: 21.65 x 29.42 inches","costCenters":[],"links":[{"id":384043,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1983/0271/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":384042,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0271/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141682,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0271/report-thumb.jpg"}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Uinta Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.77490234375,\n              37.90953361677018\n            ],\n            [\n              -102.7880859375,\n              37.90953361677018\n            ],\n            [\n              -102.7880859375,\n              39.70718665682654\n            ],\n            [\n              -111.77490234375,\n              39.70718665682654\n            ],\n            [\n              -111.77490234375,\n              37.90953361677018\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d77f","contributors":{"authors":[{"text":"Holmes, Walter F.","contributorId":31737,"corporation":false,"usgs":true,"family":"Holmes","given":"Walter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":159874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kimball, Briant A. bkimball@usgs.gov","contributorId":533,"corporation":false,"usgs":true,"family":"Kimball","given":"Briant","email":"bkimball@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":159873,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11375,"text":"ofr82700 - 1983 - Occurrence and use of ground water in the Venice-Englewood area, Sarasota and Charlotte counties, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82700","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-700","title":"Occurrence and use of ground water in the Venice-Englewood area, Sarasota and Charlotte counties, Florida","docAbstract":"In a 75-square-mile area of coastal Sarasota and Charlotte Counties, demand for water is increasing. Groundwater, the principal source of supply, is distributed largely by public water systems. Principal water-bearing formations in descending order, include the surficial aquifer, artesian zone 1 in the Tamiami Formation, zone 2 in the upper part of the Hawthorn Formation, zone 3 in the lower part of the Hawthorn Formation and upper part of the Tampa Limestone, and zones 4 and 5 which comprise the Floridan aquifer. The surficial aquifer, except near tidewater, provides limited supplies of freshwater to wells. Artesian zone 1 is the major aquifer for public supply. It is contaminated by saline water in some areas, either as a result of inundation by storm-driven tides or by upwar leakage of mineralized water from underlying aquifers through uncased or improperly constructed wells. The city of Venice obtains some water from zone 2, but the water is brackish in much of the area. The water is suitable for irrigation in parts of the area. Except for local use of water for watering livestock and maintaining ponds, the water from zones 3, 4, and 5 is little used because of its poor quality. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82700","usgsCitation":"Sutcliffe, H., and Thompson, T., 1983, Occurrence and use of ground water in the Venice-Englewood area, Sarasota and Charlotte counties, Florida: U.S. Geological Survey Open-File Report 82-700, v, 64 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82700.","productDescription":"v, 64 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0700/report-thumb.jpg"},{"id":39200,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0700/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696304","contributors":{"authors":[{"text":"Sutcliffe, Horace","contributorId":28598,"corporation":false,"usgs":true,"family":"Sutcliffe","given":"Horace","affiliations":[],"preferred":false,"id":163025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, Thomas H.","contributorId":20748,"corporation":false,"usgs":true,"family":"Thompson","given":"Thomas H.","affiliations":[],"preferred":false,"id":163024,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11425,"text":"ofr83311 - 1983 - Chemical analyses of thermal and nonthermal springs in Lassen Volcanic National Park and vicinity, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr83311","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-311","title":"Chemical analyses of thermal and nonthermal springs in Lassen Volcanic National Park and vicinity, California","docAbstract":"Most thermal waters issuing in Lassen Volcanic National Park (LVNP) are acidic (pH =3.5), low-Cl (concentrations =30 mg/L) hot springs which are characteristic of vapor-dominated hydrothermal systems and, as such, are not useful for liquid chemical geothermometry. Thermal waters at Drakesbad and in Little Hot Springs Valley, hot spring localities characterized by neutral pH and low Cl containing water, may have equilibrated in shallow aquifers so that temperatures estimated by both the Na-K-Ca and Na-Li geothermometers approach the measured spring temperatures of 65? to 95?C. Waters rich in chloride (>2000 mg/L), such as those at Growler Hot Spring and Morgan Hot Springs, situated south of LVNP, are the most appropriate springs for liquid chemical geothermometry and indicate subsurface temperatures between 220? and 230?C. The chemical and thermal characteristics of these springs may result either from boiling at depth and subsequent mixing with meteoric water or from conductive cooling during lateral flow. In either case ~220? to 230?C thermal water probably originates inside LVNP and flows south to Morgan Hot Springs.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83311","usgsCitation":"Thompson, J., 1983, Chemical analyses of thermal and nonthermal springs in Lassen Volcanic National Park and vicinity, California: U.S. Geological Survey Open-File Report 83-311, 27 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83311.","productDescription":"27 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":144142,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0311/report-thumb.jpg"},{"id":39277,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0311/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e496d","contributors":{"authors":[{"text":"Thompson, J. M.","contributorId":77142,"corporation":false,"usgs":true,"family":"Thompson","given":"J. M.","affiliations":[],"preferred":false,"id":163118,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11492,"text":"ofr83746 - 1983 - Sand-wave movement on Little Georges Bank","interactions":[],"lastModifiedDate":"2012-02-02T00:06:45","indexId":"ofr83746","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-746","title":"Sand-wave movement on Little Georges Bank","docAbstract":"A 1-x-1.5-km area on Little Georges Bank (centered at 41?08?N., 68?04?W.) was mapped three times during a ten-month period by sidescan sonar and echo-sounding techniques to assess the morphology and mobility of sand waves on Georges Bank. Sand-wave amplitudes in the survey area ranged from 1-11 m although most were 5-7 m. Wavelengths were not constant as the crests were sinuous and in places, even bifurcated. The sand waves are asymmetrical with their steepest sides facing northwest; however, gradients of their steep sides mostly are 4?-10? which is well below the angle of repose for sand in water. Sand waves tended to have greater relief and a sharper asymmetry during the survey in September than during those in June or April. \r\n\r\nDuring the survey period the sand waves moved but the direction and rate of motion was variable. Even along an individual sand wave some parts moved as much as 60 m between surveys while other parts apparently remained stationary. The sand waves were asymmetrical, but movement was not consistently in the direction that the steep sides faced. Along the same sand wave, parts moved to the northwest while other parts moved to the southeast. Despite the complex pattern of sand motion, the mean displacement of the sand waves was below the resolution of the survey technique; to resolve it, a longer survey is needed.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83746","usgsCitation":"Twichell, D.C., 1983, Sand-wave movement on Little Georges Bank: U.S. Geological Survey Open-File Report 83-746, ii, 22 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83746.","productDescription":"ii, 22 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":146581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0746/report-thumb.jpg"},{"id":39361,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0746/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdae2","contributors":{"authors":[{"text":"Twichell, David C.","contributorId":37730,"corporation":false,"usgs":true,"family":"Twichell","given":"David","email":"","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":163234,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11502,"text":"ofr82769 - 1983 - Evaluation of water-quality characteristics of part of the Spokane Aquifer, Washington and Idaho, using a solute-transport digital model","interactions":[],"lastModifiedDate":"2012-02-02T00:06:41","indexId":"ofr82769","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-769","title":"Evaluation of water-quality characteristics of part of the Spokane Aquifer, Washington and Idaho, using a solute-transport digital model","docAbstract":"The principal dissolved constituents in water in the Spokane aquifer are calcium and bicarbonate. These constituents (as well as dissolved solids, hardness, and magnesium) each correlate well with specific conductance, whereas chloride, sodium, and nitrate each do not. Specific conductance ranges from 73 to 820 micromhos per centimeter throughout the study area. Short-term variations in water quality in the Spokane aquifer are generally greater than long-term variations. \r\n\r\nVertical variations in concentration of chemical constituents occurred in four of 15 wells used to sample the upper 50 feet of the aquifer along several cross sections. Changes in water quality from one cross section to another could not be directly related to land-use activities. \r\n\r\nA digital model was developed and used to simulate solute transport of conservative ions in the Spokane aquifer. Specifically, the model was used to estimate the impact of the chloride ion from recharge through septic tanks and from irrigation on the water quality of the aquifer. Analysis shows that the estimated impact on the aquifer from these two source loadings was less than a 1-milligram-per-liter increase throughout approximately 80 percent of the aquifer, but increases averaging about 3 milligrams per liter occurred in some peripheral areas. Various water-quality-management schemes based on manmade or natural stresses can be tested with the model.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82769","usgsCitation":"Vaccaro, J.J., and Bolke, E., 1983, Evaluation of water-quality characteristics of part of the Spokane Aquifer, Washington and Idaho, using a solute-transport digital model: U.S. Geological Survey Open-File Report 82-769, vi, 75 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82769.","productDescription":"vi, 75 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145736,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0769/report-thumb.jpg"},{"id":39368,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0769/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1cce","contributors":{"authors":[{"text":"Vaccaro, J. J.","contributorId":48173,"corporation":false,"usgs":true,"family":"Vaccaro","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":163259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":163260,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8449,"text":"ofr83550 - 1983 - Nonparametric tests for trends in water-quality data using the statistical analysis system","interactions":[],"lastModifiedDate":"2016-06-01T15:43:25","indexId":"ofr83550","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-550","title":"Nonparametric tests for trends in water-quality data using the statistical analysis system","docAbstract":"<p>Two nonparametric procedures to test for trends in water-quality data (SEASKEN AND SEASRS) have been developed for the Statistical Analysis System* (SAS). The procedure SEASKEN tests for a monotonic trend in time by a modified form of Kendall's tau, the Seasonal Kendall test. The procedure SEASRS tests for a step trend between two different periods in a time series using a modified form of the Wilcoxon (Mann-Whitney) rank sum test, the Mann-WhitneyWilcoxon rank sum test for seasonal data. Examples are presented using the two procedures. The source code and user's guide for each of the two procedures are also presented.</p>\n<p>Procedures for flow adjusting water-quality data by the SAS procedures REG and SYSREG and techniques for plotting water-quality data as a time series by the SAS procedure PLOT are presented.</p>\n<p>Additionally, examples are presented to demonstrate the use of the U.S. Geological Survey procedures QWRETR, DVRETR, QWSAS, and DVINPUT to retrieve data from the Geological Survey WATSTORE system and make it available to SAS.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83550","usgsCitation":"Crawford, C.G., Slack, J.R., and Hirsch, R.M., 1983, Nonparametric tests for trends in water-quality data using the statistical analysis system: U.S. Geological Survey Open-File Report 83-550, iv, 102 p., https://doi.org/10.3133/ofr83550.","productDescription":"iv, 102 p.","numberOfPages":"106","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":140525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0550/report-thumb.jpg"},{"id":36022,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0550/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684672","contributors":{"authors":[{"text":"Crawford, Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":157734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slack, James R.","contributorId":43778,"corporation":false,"usgs":true,"family":"Slack","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":157736,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hirsch, Robert M. 0000-0002-4534-075X rhirsch@usgs.gov","orcid":"https://orcid.org/0000-0002-4534-075X","contributorId":2005,"corporation":false,"usgs":true,"family":"Hirsch","given":"Robert","email":"rhirsch@usgs.gov","middleInitial":"M.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":37316,"text":"WMA - Integrated Information Dissemination Division","active":true,"usgs":true}],"preferred":true,"id":157735,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9609,"text":"ofr83753 - 1983 - Ground-water data for Michigan 1982","interactions":[],"lastModifiedDate":"2016-12-29T10:58:52","indexId":"ofr83753","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-753","title":"Ground-water data for Michigan 1982","docAbstract":"<p>Water levels, locations, depths, and aquifers tapped are given for 117 observation wells. Tabulated data include extremes of water levels for 1982 and for the period of record, pumpage of most major ground-water users in the State, and quality data on selected wells. The largest reported user of ground-water, the city of Lansing, pumped 8.2 billion gallons from the Saginaw Formation and glacial deposits.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr83753","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources","usgsCitation":"Huffman, G., 1983, Ground-water data for Michigan 1982: U.S. Geological Survey Open-File Report 83-753, iv, 54 p., https://doi.org/10.3133/ofr83753.","productDescription":"iv, 54 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":141716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0753/report-thumb.jpg"},{"id":37339,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0753/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":8617,"text":"ofr83425 - 1983 - Shallow structure and stratigraphy of the carbonate West Florida continental slope and their implications to sedimentation and geohazards","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr83425","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-425","title":"Shallow structure and stratigraphy of the carbonate West Florida continental slope and their implications to sedimentation and geohazards","docAbstract":"An 1800-joule sparker survey of the West Florida continental slope between about 26?N and 29?15?N showed a top bed of Pleistocene age forming an irregular drape over a surface that is probably Pliocene. The contact between the top two layers is unconformable in the south and, in some places, shows karst collapse and solution features. Karst topography grades into a more hummocky erosional surface to the north, which in turn smoothes out; the contact become conformable still further north. A period of folding, which is widespread over the outer portion of the study area and which may be related to large scale mass wasting, occurred at about the same time represented by the unconformity. Significant subsidence has occurred as late as Pleistocene. \r\n\r\nThe surface layer thins to a minimum (0 in the south) at about 525-meters water depth and then thickens again dramatically to the west, downslope. This thinning is interpreted to be due to the Loop Current, which flows from north to south in the area and which acts to block deposition and scour the bottom. \r\n\r\nDespite the fact that the margin is dominated by carbonates, usually associated with low sedimentation rates, there is widespread evidence of mass wasting affecting ancient and surficial deposits on the outer part of the upper slope. \r\n\r\nThree potential groups of geohazards identified are: \r\n\r\n1. Potential bottom failure in areas where a thin top layer overlies the karst surface. \r\n2. Potential for sliding and slumping. \r\n3. Scour due to currents which could also affect drilling and engineering activities.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83425","usgsCitation":"Doyle, L.J., 1983, Shallow structure and stratigraphy of the carbonate West Florida continental slope and their implications to sedimentation and geohazards: U.S. Geological Survey Open-File Report 83-425, 21 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83425.","productDescription":"21 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0425/report-thumb.jpg"},{"id":36208,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0425/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f40a9","contributors":{"authors":[{"text":"Doyle, Larry J.","contributorId":43352,"corporation":false,"usgs":true,"family":"Doyle","given":"Larry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158035,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10321,"text":"ofr82771 - 1983 - Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr82771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-771","title":"Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982","docAbstract":"The rockslide/debris avalanche from the north face of Mount St. Helens that precipitated the volcano 's eruption on May 18, 1980 , blocked outflow from Spirit Lake, Washington. There has been no surface outflow since that time. From May 21, 1980, when the first measurement of lake level was made, to August 1, 1982, Spirit Lake has increased its volume from 122,800 acre-ft to 264 ,000 acre-ft, an increase of 115%. Lake level has risen approximately 54 ft during this period. Hydrologic and geologic properties of the debris dam are unknown, but the materials obviously are easily erodible. Steep walled channels up to 60 ft deep have been eroded into the dam and are extending headward toward the lowest points on the crest. In addition, it appears that the lower areas on the crest of the dam are underlain by ash cloud deposits of low density. Indications are that the debris dam could fail by headward erosion, by overtopping with rapid downcutting, or by ' piping ' and rapid erosion. Each type of failure can produce rapid release of stored lake water with very high discharge rates. On the basis of observed filling rates of the lake over the last two yr and precipitation records at four long-term, low altitude National Weather Service stations, it is expected that normal precipitation will fill the lake to the dam crest in December 1985. This estimate is also based on the assumption that loss of water from the lake by seepage continues at the present rate until December 1985. With normal precipitation during the coming yr (August 1982 through July 1983 the lake will fill to a level 50 ft below the lowest existing point on the crest of the debris dam, which is at 3,532 ft altitude. If precipitation exceeds normal by 1.5 times during this coming year, the lake level will be 40 ft below the 3 ,532-ft crest of the debris dam by the end of July 1983. This same lake level can be reached by the end of March 1983 if precipitation from October through March is twice the winter mean. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82771","usgsCitation":"Meyer, W., and Carpenter, P.J., 1983, Filling of Spirit Lake, Washington, May 18, 1980 to July 31, 1982: U.S. Geological Survey Open-File Report 82-771, iv, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82771.","productDescription":"iv, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0771/report-thumb.jpg"},{"id":38172,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0771/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f481e","contributors":{"authors":[{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":161195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carpenter, Philip J.","contributorId":85034,"corporation":false,"usgs":true,"family":"Carpenter","given":"Philip","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161194,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11534,"text":"ofr83252 - 1983 - Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah","interactions":[{"subject":{"id":11534,"text":"ofr83252 - 1983 - Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah","indexId":"ofr83252","publicationYear":"1983","noYear":false,"title":"Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":2868,"text":"wsp2247 - 1985 - Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah","indexId":"wsp2247","publicationYear":"1985","noYear":false,"title":"Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah"},"id":1}],"supersededBy":{"id":2868,"text":"wsp2247 - 1985 - Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah","indexId":"wsp2247","publicationYear":"1985","noYear":false,"title":"Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah"},"lastModifiedDate":"2021-03-05T02:04:08.849089","indexId":"ofr83252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-252","title":"Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83252","usgsCitation":"Waddell, K., Darby, D., and Theobald, S., 1983, Chemical and physical characteristics of water and sediment in Scofield Reservoir, Carbon County, Utah: U.S. Geological Survey Open-File Report 83-252, 74 p., https://doi.org/10.3133/ofr83252.","productDescription":"74 p.","costCenters":[],"links":[{"id":384039,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0252/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144553,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0252/report-thumb.jpg"}],"country":"United States","state":"Utah","county":"Carbon County","otherGeospatial":"Scofield Reservoir","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.18713378906249,\n              39.74732195489861\n            ],\n            [\n              -111.11709594726561,\n              39.74732195489861\n            ],\n            [\n              -111.11709594726561,\n              39.82013946676259\n            ],\n            [\n              -111.18713378906249,\n              39.82013946676259\n            ],\n            [\n              -111.18713378906249,\n              39.74732195489861\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e480e","contributors":{"authors":[{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":163318,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Darby, D.W.","contributorId":49333,"corporation":false,"usgs":true,"family":"Darby","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":163316,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Theobald, S.M.","contributorId":51270,"corporation":false,"usgs":true,"family":"Theobald","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":163317,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11542,"text":"ofr83219 - 1983 - Ground-water data for selected coal areas in western North Dakota","interactions":[],"lastModifiedDate":"2018-03-15T16:47:54","indexId":"ofr83219","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-219","title":"Ground-water data for selected coal areas in western North Dakota","docAbstract":"<p>Ground-water data are provided in this report for the Sand Creek-Hanks, New England-Mott, Dickinson, and Bowman-Gascoyne coal areas, western North Dakota. The report contains the following: (1) Maps showing the location of wells, springs, and test holes; the location of wells and test holes where drillers' logs are available; and the location of wells with chemical analyses; and (2) tables showing well, spring, and testhole records; logs; and chemical analyses of water. Descriptions of the location of data-collection sites and methods used to collect data are included.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83219","usgsCitation":"Wald, J.D., and Norbeck, S.W., 1983, Ground-water data for selected coal areas in western North Dakota: U.S. Geological Survey Open-File Report 83-219, Report: 244 p.; 9 Plates, https://doi.org/10.3133/ofr83219.","productDescription":"Report: 244 p.; 9 Plates","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":39411,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39412,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39413,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145332,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0219/report-thumb.jpg"},{"id":39405,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39406,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39407,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39408,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39409,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39410,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0219/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":39414,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0219/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce32","contributors":{"authors":[{"text":"Wald, James D.","contributorId":64263,"corporation":false,"usgs":true,"family":"Wald","given":"James","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":163329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Norbeck, Steven W.","contributorId":29824,"corporation":false,"usgs":true,"family":"Norbeck","given":"Steven","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":163328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8452,"text":"ofr83526 - 1983 - Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80: Variability, loads, and trends of selected constituents","interactions":[],"lastModifiedDate":"2022-12-06T22:28:21.895193","indexId":"ofr83526","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-526","title":"Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80: Variability, loads, and trends of selected constituents","docAbstract":"Water-quality data for selected sites in the Cape Fear River basin collected by the U.S. Geological Survey, the North Carolina Department of Natural Resources and Community Development and the University of North Carolina at Chapel Hill are analyzed and interpreted in this report. Emphasis is given to the Cape Fear River at Lock 1 near Kelly, where data are most complete. Other data included in the report were collected from the Cape Fear River at Lillington, the Haw River near the Jordan Dam, and the Deep River at Moncure. \r\n\r\nAvailable data indicate that concentrations of dissolved oxygen at study sites are almost always within U.S. Environmental Protection Agency criteria; however, on two sampling dates, the concentration of dissolved oxygen in the Cape Fear at Lock 1 fell slightly below the 5.0 mg/L recommended for fish populations. Measurements of pH from all stations were frequently below the lower limit of 6.5 pH units recommended for protection of freshwater aquatic life. \r\n\r\nMajor dissolved ions detected are sodium and bicarbonate. Sodium concentration averages 8.6 mg/L and bicarbonate averages 17.5 mg/L at Lock 1. Concentrations of dissolved substances and suspended sediment decrease in the downstream direction, presumably because the more heavily populated part of the basin is near the headwaters of the system. \r\n\r\nHeavy metals, with the exceptions of cadmium and mercury, rarely exceed Environmental Protection Agency criteria for the protection of aquatic life. Concentrations of mercury in the Haw River, which exceed the recommended 0.20 mg/L needed to protect aquatic life, have frequently been reported by other authors. Several of the most toxic metals, arsenic, cadmium, and cobalt, are about five times more concentrated in water from the Haw River site than from other study sites in the basin. Iron and manganese frequently exceed North Carolina water-quality standards. \r\n\r\nAvailable nitrogen averages 1.21 mg/L and available phosphorus averages 0.21 mg/L at Lock 1. Nuisance algal growths have not been identified as a problem in the river. \r\n\r\nComparisons of water-quality data for baseline (natural) and present conditions indicate that more than 50 percent of most dissolved substances and over 80 percent of certain forms of nitrogen and phosph6rus result from development.\r\n\r\nOver the past 25 years, increases in concentrations of specific conductance, dissolved magnesium, dissolved sodium, dissolved potassium, dissolved sulfate, dissolved solids, and total nitrite plus nitrate nitrogen were detected in the Cape Fear River at Lock 1. Values for pH and dissolved silica are decreasing. Concentrations of most dissolved constituents at Lock 1 are increasing. These increases are statistically related to increases in population and manufacturing employment in the basin but are unrelated to agricultural activity.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83526","usgsCitation":"Crawford, J.K., 1983, Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80: Variability, loads, and trends of selected constituents: U.S. Geological Survey Open-File Report 83-526, vi, 66 p., https://doi.org/10.3133/ofr83526.","productDescription":"vi, 66 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":140544,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0526/report-thumb.jpg"},{"id":36023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0526/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":410128,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14090.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina","otherGeospatial":"Cape Fear River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.904052734375,\n              33.75174787568194\n            ],\n            [\n              -77.8546142578125,\n              33.988918483762156\n            ],\n            [\n              -77.7996826171875,\n              34.17090836352573\n            ],\n            [\n              -77.53051757812499,\n              34.384246040152185\n            ],\n            [\n              -77.464599609375,\n              34.43409789359469\n            ],\n            [\n              -77.882080078125,\n              35.02099970111467\n            ],\n            [\n              -78.20068359374999,\n              35.133386854253075\n            ],\n            [\n              -78.519287109375,\n              35.209721645221386\n            ],\n            [\n              -78.7335205078125,\n              35.51881428123057\n            ],\n            [\n              -78.83239746093749,\n              35.82226734114509\n            ],\n            [\n              -78.88732910156249,\n              36.01800375871416\n            ],\n            [\n              -79.4366455078125,\n              36.146746777814364\n            ],\n            [\n              -80.03814697265625,\n              36.02189133007692\n            ],\n            [\n              -80.0628662109375,\n              35.957443980673595\n            ],\n            [\n              -80.06904602050781,\n              35.78941187118459\n            ],\n            [\n              -79.815673828125,\n              35.382332329032984\n            ],\n            [\n              -79.5684814453125,\n              35.22991591449646\n            ],\n            [\n              -79.46685791015625,\n              35.074964853989556\n            ],\n            [\n              -79.22515869140625,\n              34.9895035675793\n            ],\n            [\n              -78.88732910156249,\n              34.77545980961412\n            ],\n            [\n              -78.78021240234375,\n              34.70549341022544\n            ],\n            [\n              -78.42041015625,\n              34.31621838080741\n            ],\n            [\n              -78.22265625,\n              33.988918483762156\n            ],\n            [\n              -77.904052734375,\n              33.75174787568194\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d552","contributors":{"authors":[{"text":"Crawford, J. Kent","contributorId":54176,"corporation":false,"usgs":true,"family":"Crawford","given":"J.","email":"","middleInitial":"Kent","affiliations":[],"preferred":false,"id":157743,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8586,"text":"ofr83500 - 1983 - Survey of helium in natural water wells and springs in southwest Montana and Imperial Valley, California; Part V, Jan. 1-Dec. 31, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:09","indexId":"ofr83500","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-500","title":"Survey of helium in natural water wells and springs in southwest Montana and Imperial Valley, California; Part V, Jan. 1-Dec. 31, 1982","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83500","usgsCitation":"Doering, W.P., and Friedman, I., 1983, Survey of helium in natural water wells and springs in southwest Montana and Imperial Valley, California; Part V, Jan. 1-Dec. 31, 1982: U.S. Geological Survey Open-File Report 83-500, 32 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83500.","productDescription":"32 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":141051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0500/report-thumb.jpg"},{"id":36181,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0500/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688689","contributors":{"authors":[{"text":"Doering, Willis P.","contributorId":9650,"corporation":false,"usgs":true,"family":"Doering","given":"Willis","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":157986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Irving","contributorId":90664,"corporation":false,"usgs":true,"family":"Friedman","given":"Irving","email":"","affiliations":[],"preferred":false,"id":157987,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9692,"text":"ofr83736 - 1983 - Rock property measurements and analysis of selected igneous, sedimentary, and metamorphic rocks from worldwide localities","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr83736","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-736","title":"Rock property measurements and analysis of selected igneous, sedimentary, and metamorphic rocks from worldwide localities","docAbstract":"Dry bulk density and grain density measurements were made on 182 samples of igneous, sedimentary, and metamorphic rocks from various world-wide localities. Total porosity values and both water-accessible and helium-accessible porosities were calculated from the density data. Magnetic susceptibility measurements were made on the solid samples and permeability and streaming potentials were concurrently measured on most samples. Dry bulk densities obtained using two methods of volume determination, namely direct measurement and Archlmedes principle, were nearly equivalent for most samples. Grain densities obtained on powdered samples were typically greater than grain densities obtained on solid samples, but differences were usually small. Sedimentary rocks had the highest percentage of occluded porosity per rock volume whereas metamorphic rocks had the highest percentage of occluded porosity per total porosity. There was no apparent direct relationship between permeability and streaming potential for most samples, although there were indications of such a relationship in the rock group consisting of granites, aplites, and syenites. Most rock types or groups of similar rock types of low permeability had, when averaged, comparable levels of streaming potential per unit of permeability. Three calcite samples had negative streaming potentials.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83736","usgsCitation":"Johnson, G.R., 1983, Rock property measurements and analysis of selected igneous, sedimentary, and metamorphic rocks from worldwide localities: U.S. Geological Survey Open-File Report 83-736, 37 p. ill. ;28 cm., https://doi.org/10.3133/ofr83736.","productDescription":"37 p. ill. ;28 cm.","costCenters":[],"links":[{"id":141012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0736/report-thumb.jpg"},{"id":37411,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0736/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5679","contributors":{"authors":[{"text":"Johnson, Gordon R.","contributorId":90725,"corporation":false,"usgs":true,"family":"Johnson","given":"Gordon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":160136,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9694,"text":"ofr83727 - 1983 - Assessment of gray whale feeding grounds and sea floor interaction in the northeastern Bering Sea","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr83727","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-727","title":"Assessment of gray whale feeding grounds and sea floor interaction in the northeastern Bering Sea","docAbstract":"A dense ampeliscid amphipod community in Chirikov Basin and around St. Lawrence Island in the northeastern Bering Sea has been outlined by summarizing biological studies, analyzing bioturbation in sediment samples, and examining sea floor photos and videotapes. The amphipod population is associated with a homogeneous, relict fine-grained sand body 0.10-1.5 m thick that is deposited during the marine transgression over the Bering land bridge 8,000-10,000 yr B.P. Modern current and water mass movements and perhaps whale feeding activity prevent modern deposition in this area. \r\n\r\nThe distribution of the transgressive sand sheet, associated amphipod community and feeding gray whales mapped by aerial survey correlate closely with three types of sea-floor pits observed on high (500 kHz) and low (105 kHz) resolution side-scan sonar; they are attributed to gray whale feeding traces and their subsequent current scour modification. The fresh and modified feeding pits are present in 22,000 km2 of the basin and they cover a total of 2 to 18% of the sea floor in different areas of the feeding region. The smallest size class of pits approximates whale mouth gape size and is assumed to represent fresh whale feeding pits. Fresh feeding disturbance of the sea floor is estimated to average about 5.7% for a full feeding season. Combined with information that 34% of the measured benthic biomass is amphipod prey species, and calculating the number of gray whale feeding days in the Alaskan waters plus amount consumed per day, it can be estimated that Chirikov Basin, 2% of the feeding area, supplies a minimum of 5.3 to 7.1% of the gray whale's food resource in the Bering Sea and Arctic Ocean. If a maximum of 50% of the fresh feeding features are assumed to be missed because they parallel side-scan beam paths, then a maximum whale food resource of 14.2% is possible in northeastern Bering Sea. Because of side-scan techniques and possible higher amphipod biomass estimates, a reasonable minimum estimate of the total whale food resource in northeastern Bering Sea is 10%. \r\n\r\nThese data show that side-scan sonar is a powerful new technique for analyzing marine mammal benthic feeding grounds. Sonographs reveal that the gray whales profoundly disturb the substrate and initiate substantial further erosion by bottom currents, all of which enhances productivity of the prey species and results in a 'farming of the sea floor'. In turn, because of the high concentration of whale prey species in a prime feeding ground that is vulnerable to the development of petroleum and mining for sand, great care is required in the exploitation of these resources in the Chirikov Basin.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83727","usgsCitation":"Nelson, C., Johnson, K., and Barber, J., 1983, Assessment of gray whale feeding grounds and sea floor interaction in the northeastern Bering Sea: U.S. Geological Survey Open-File Report 83-727, 112 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83727.","productDescription":"112 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0727/report-thumb.jpg"},{"id":37413,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0727/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671f9e","contributors":{"authors":[{"text":"Nelson, C.H.","contributorId":88346,"corporation":false,"usgs":true,"family":"Nelson","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":160141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, K.R.","contributorId":28599,"corporation":false,"usgs":true,"family":"Johnson","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":160140,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barber, John H.","contributorId":90305,"corporation":false,"usgs":true,"family":"Barber","given":"John H.","affiliations":[],"preferred":false,"id":160142,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":11552,"text":"ofr83417 - 1983 - Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:44","indexId":"ofr83417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-417","title":"Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado","docAbstract":"The Schwartzwalder uranium deposit, in the Front Range west of Denver, Colorado, is the largest vein-type uranium deposit in the United States. The deposit is situated in a steeply dipping fault system that cuts Proterozoic metamorphic rocks. The host rocks represent a submarine volcanic system with associated chert and iron- and sulfide-rich pelitic rocks. Where faulted, the more competent garnetiferous and quartzitic units behaved brittlely and created a deep, narrow conduit. \r\n\r\nThe ores formed 70-72 m.y. ago beneath 3 km of Phanerozoic sedimentary rocks. Mineralization included two episodes of alteration and three stages of vein-mineralization. Early carbonate-sericite alteration pseudomorphically replaced mafic minerals, whereas the ensuing hematite-adularia episode replaced only the earlier alteration assemblage. Early vein mineralization produced a minor sulfide-adularia-carbonate assemblage. Later vein mineralization generated the uranium ores in two successive stages. Carbonates, sulfides, and adularia filled the remaining voids. Clastic dikes composed of fault gouge and, locally, ore were injected into new and existing fractures. \r\n\r\nGeologic and chemical evidence suggest that virtually all components of the deposit were derived from major hornblende gneiss units and related rocks. The initial fluids were evolved connate/metamorphic water that infiltrated and resided along the extensive fault zones. Complex fault movements in the frontal zone of the eastern Front Range caused the fluids to migrate to the most permeable segments of the fault zones. Heat was supplied by increased crustal heat flow related to igneous activity in the nearby Colorado mineral belt. Temperatures decreased from 225?C to 125?C during later mineralization, and the pressure episodically dropped from 1000 bars. The CO2 fugacity was initially near 100 bars, and uranium was carried as a dicarbonate complex. Sudden decreases in confining pressure during fault movement caused evolution of CO2 and a consequent increase in pH. Uranium was released with destruction of the uranyl complexes; it was subsequently reduced by aqueous sulfur species, thereby leading to the precipitation of pitchblende.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83417","usgsCitation":"Wallace, A.R., 1983, Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado: U.S. Geological Survey Open-File Report 83-417, 186 p. ill. ;28 cm., https://doi.org/10.3133/ofr83417.","productDescription":"186 p. ill. ;28 cm.","costCenters":[],"links":[{"id":145473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0417/report-thumb.jpg"},{"id":39426,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0417/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68751b","contributors":{"authors":[{"text":"Wallace, Alan R.","contributorId":6024,"corporation":false,"usgs":true,"family":"Wallace","given":"Alan","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":163345,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9719,"text":"ofr83262 - 1983 - Directory of assistance centers of the National Water Data Exchange (NAWDEX)","interactions":[{"subject":{"id":8702,"text":"ofr79423 - 1979 - Directory of local assistance centers of the National Water Data Exchange (NAWDEX)","indexId":"ofr79423","publicationYear":"1979","noYear":false,"title":"Directory of local assistance centers of the National Water Data Exchange (NAWDEX)"},"predicate":"SUPERSEDED_BY","object":{"id":9719,"text":"ofr83262 - 1983 - Directory of assistance centers of the National Water Data Exchange (NAWDEX)","indexId":"ofr83262","publicationYear":"1983","noYear":false,"title":"Directory of assistance centers of the National Water Data Exchange (NAWDEX)"},"id":1},{"subject":{"id":48608,"text":"ofr801193 - 1980 - Directory of assistance centers of the National Water Data Exchange (NAWDEX)","indexId":"ofr801193","publicationYear":"1980","noYear":false,"title":"Directory of assistance centers of the National Water Data Exchange (NAWDEX)"},"predicate":"SUPERSEDED_BY","object":{"id":9719,"text":"ofr83262 - 1983 - Directory of assistance centers of the National Water Data Exchange (NAWDEX)","indexId":"ofr83262","publicationYear":"1983","noYear":false,"title":"Directory of assistance centers of the National Water Data Exchange (NAWDEX)"},"id":2},{"subject":{"id":49347,"text":"ofr78162 - 1978 - Directory of local assistance centers of the National Water Data Exchange (NAWDEX)","indexId":"ofr78162","publicationYear":"1978","noYear":false,"title":"Directory of local assistance centers of the National Water Data Exchange (NAWDEX)"},"predicate":"SUPERSEDED_BY","object":{"id":9719,"text":"ofr83262 - 1983 - Directory of assistance centers of the National Water Data Exchange (NAWDEX)","indexId":"ofr83262","publicationYear":"1983","noYear":false,"title":"Directory of assistance centers of the National Water Data Exchange (NAWDEX)"},"id":3}],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr83262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-262","title":"Directory of assistance centers of the National Water Data Exchange (NAWDEX)","docAbstract":"The National Water Data Exchange (NAWDEX), managed by the U.S. Geological Survey, has established a network of Assistance Centers throughout the United States and Puerto Rico to assist users of water data in identifying and locating the data they need. This Directory provides the information needed to contact any of the established Centers.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83262","usgsCitation":"Josefson, B.M., and Blackwell, C.D., 1983, Directory of assistance centers of the National Water Data Exchange (NAWDEX): U.S. Geological Survey Open-File Report 83-262, iv, 37 p. ;28 cm., https://doi.org/10.3133/ofr83262.","productDescription":"iv, 37 p. ;28 cm.","costCenters":[],"links":[{"id":142331,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0262/report-thumb.jpg"},{"id":37464,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0262/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b463b","contributors":{"authors":[{"text":"Josefson, Beverly M.","contributorId":94306,"corporation":false,"usgs":true,"family":"Josefson","given":"Beverly","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160180,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blackwell, Cassandra D.","contributorId":25562,"corporation":false,"usgs":true,"family":"Blackwell","given":"Cassandra","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":160179,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9728,"text":"ofr83257 - 1983 - Background hydrologic information in potential lignite mining areas in Mississippi, July 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:30","indexId":"ofr83257","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-257","title":"Background hydrologic information in potential lignite mining areas in Mississippi, July 1982","docAbstract":"A water-quality sampling program was initiated in 1980 to determine background hydrologic data in potential lignite mining areas of Mississippi. This report is the third in a planned five-part series to provide data to assess future impacts of mining on small streams. The data indicates that most streams in the study area have a dissolved-solids concentration less than 100 mg/. The major ion concentrations were generally less than 10 mg/. Concentrations of arsenic, cadmium, mercury, and selenium in bottom material samples were below detectable limits. Cobalt, lead, zinc, copper, and chromium concentrations exceeded 10 micro-/g at all sites and maganese exceeded 1000 micro-/g at five sites. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83257","usgsCitation":"Kalkhoff, S.J., 1983, Background hydrologic information in potential lignite mining areas in Mississippi, July 1982: U.S. Geological Survey Open-File Report 83-257, 25 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83257.","productDescription":"25 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":144227,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0257/report-thumb.jpg"},{"id":37473,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0257/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64adb1","contributors":{"authors":[{"text":"Kalkhoff, Stephen J. 0000-0003-4110-1716 sjkalkho@usgs.gov","orcid":"https://orcid.org/0000-0003-4110-1716","contributorId":1731,"corporation":false,"usgs":true,"family":"Kalkhoff","given":"Stephen","email":"sjkalkho@usgs.gov","middleInitial":"J.","affiliations":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true},{"id":35680,"text":"Illinois-Iowa-Missouri Water Science Center","active":true,"usgs":true}],"preferred":true,"id":160198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11565,"text":"ofr83215 - 1983 - Water and streambed-material data, Eagle Creek watershed, Indiana, August 1980-December 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:06:42","indexId":"ofr83215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-215","title":"Water and streambed-material data, Eagle Creek watershed, Indiana, August 1980-December 1982","docAbstract":"Water quality studies within the Eagle Creek watershed, Indiana, were done by the U.S. Geological Survey in August 1980, October 1982, and December 1982 in cooperation with the city of Indianapolis, Department of Public Works. Streambed-material and water samples were collected from Finley and Eagle Creeks at various flow rates and were analyzed for selected metals, non-metals, insecticides, and acid-extractable and base-neutral-extractable compounds. Water samples also were analyzed for volatile organics. This report lists all the data collected and analyzed by the U.S. Geological Survey during the 1980 and 1982 surveys but does not interpret the data. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83215","usgsCitation":"Wangsness, D.J., 1983, Water and streambed-material data, Eagle Creek watershed, Indiana, August 1980-December 1982: U.S. Geological Survey Open-File Report 83-215, 48 p. maps ;28 cm., https://doi.org/10.3133/ofr83215.","productDescription":"48 p. maps ;28 cm.","costCenters":[],"links":[{"id":145828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0215/report-thumb.jpg"},{"id":39435,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0215/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa351","contributors":{"authors":[{"text":"Wangsness, David J.","contributorId":81475,"corporation":false,"usgs":true,"family":"Wangsness","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":163365,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}