{"pageNumber":"4768","pageRowStart":"119175","pageSize":"25","recordCount":165609,"records":[{"id":10385,"text":"ofr82409 - 1982 - Three-dimensional modeling of the Nevada Test Site and vicinity from teleseismic P-wave residuals","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82409","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-409","title":"Three-dimensional modeling of the Nevada Test Site and vicinity from teleseismic P-wave residuals","docAbstract":"A teleseismic P-wave travel-time residual study is described which reveals the regional compressional-velocity structure of southern Nevada and neighboring parts of California to a depth of 280 km. During 1980, 98 teleseismic events were recorded at as many as 53 sites in this area. P-wave residuals were calculated relative to a network-wide average residual for each event and are displayed on maps of the stations for each of four event-azimuth quadrants. Fluctuations in these map-patterns of residuals with approach azimuth combined with results of linear, three-dimensional inversions of some 2887 residuals indicate the following characteristics of the velocity structure of the southern Nevada region: 1) a low-velocity body exists in the upper crust 50 km northeast of Beatty, Nevada, near the Miocene Timber Mountain-Silent Canyon caldera complex. Another highly-localized low-velocity anomaly occurs near the southwest corner of the Nevada Test Site (NTS). These two anomalies seem to be part of a low-velocity trough extending from Death Valley, California, to about 50 km north of NTS. 2) There is a high-velocity body in the mantle between 81 and 131 km deep centered about i0 km north of the edge of the Timber Mountain caldera, 3) a broad low-velocity body is delineated between 81 and 131 km deep centered about 30 km north of Las Vegas, 4) there is a monotonic increase in travel-time delays from west to east across the region, probably indicating an eastward decrease in velocity, and lower than average velocities in southeastern Nevada below 31 km, and 5) considerable complexity in three-dimensional velocity structure exists in this part of the southern Great Basin. \r\n\r\nInversions of teleseismic P-wave travel-time residuals were also performed on data from 12 seismometers in the immediate vicinity of the Nevada Test Site to make good use of the closer station spacing i in that area. Results of these inversions show more details of the velocity structure but generally the same features as those found in the regional study.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82409","usgsCitation":"Monfort, M.E., and Evans, J.R., 1982, Three-dimensional modeling of the Nevada Test Site and vicinity from teleseismic P-wave residuals: U.S. Geological Survey Open-File Report 82-409, 70 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82409.","productDescription":"70 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":142336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0409/report-thumb.jpg"},{"id":38215,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0409/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b857","contributors":{"authors":[{"text":"Monfort, Mary E.","contributorId":93491,"corporation":false,"usgs":true,"family":"Monfort","given":"Mary","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, John R. jrevans@usgs.gov","contributorId":529,"corporation":false,"usgs":true,"family":"Evans","given":"John","email":"jrevans@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":161295,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8361,"text":"ofr82103 - 1982 - Quality of surface water at selected sites in the Suwannee River basin, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"ofr82103","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-103","title":"Quality of surface water at selected sites in the Suwannee River basin, Florida","docAbstract":"This report presents the results of analyses of water-quality samples collected from 14 surface-water sites in the Suwannee River basin in Florida from January through December 1980. The analyses of samples collected routinely included: nutrients, total organic carbon, and 5-day biochemical oxygen demand, bimonthly; and trace metals, annually. The array of constituents sampled was expanded in October 1978 at three of the original nine stations to provide quality-of-water information for streams draining an industrial area: Rocky Creek near Belmont, Hunter Creek near Belmont, and Swift Creek at Facil. Data collected at these three sites now include: major chemical constituents, six times per year: radium-226, two times per year; and trace metals, one time per year. These constituents are determined in addition to nutrients, total organic carbon, and bio-chemical oxygen demand which continue to be analyzed six times per year. All results of analyses of the water-quality samples collected from January through December 1980 remained within, or near, previously measured ranges and water-quality fluctuations were similar to those noted from data collected since 1971. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82103","usgsCitation":"Coffin, J., 1982, Quality of surface water at selected sites in the Suwannee River basin, Florida: U.S. Geological Survey Open-File Report 82-103, x, 117 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr82103.","productDescription":"x, 117 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":140310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0103/report-thumb.jpg"},{"id":35934,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0103/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db640ffd","contributors":{"authors":[{"text":"Coffin, J.E.","contributorId":75913,"corporation":false,"usgs":true,"family":"Coffin","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":157596,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8363,"text":"ofr82361 - 1982 - Summary of ground-water and surface-water data for city of Pensacola and Escambia County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"ofr82361","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-361","title":"Summary of ground-water and surface-water data for city of Pensacola and Escambia County, Florida","docAbstract":"Hydrologic, geologic, and water-quality data collected in Escambia County, Florida, October 1962 through September 1980 are presented. The data were collected by the U.S. Geological Survey as part of a cooperative investigation with the city of Pensacola and Escambia County to provide information on the quality and quantity of water available from the sand-and-gravel aquifer and selected surface-water sites in Escambia County. Ground-water data include records of 440 wells, chemical and physical analyses of water quality for 325 wells, 6 long-term hydrographs, and 19 lithologic logs. Surface-water data include streamflow measurements and analyses of water collected at 9 sites. Maps of the county show the locations of the data-collection sites. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82361","usgsCitation":"Coffin, J., 1982, Summary of ground-water and surface-water data for city of Pensacola and Escambia County, Florida: U.S. Geological Survey Open-File Report 82-361, 136 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82361.","productDescription":"136 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0361/report-thumb.jpg"},{"id":35935,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0361/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980e9","contributors":{"authors":[{"text":"Coffin, J.E.","contributorId":75913,"corporation":false,"usgs":true,"family":"Coffin","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":157598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8378,"text":"ofr8218 - 1982 - Alaska index (December 1980 - November 1981)","interactions":[],"lastModifiedDate":"2024-04-04T22:20:33.17103","indexId":"ofr8218","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-18","title":"Alaska index (December 1980 - November 1981)","docAbstract":"

In an effort to develop the oil and gas resources of the Outer Continental Shelf (OCS), the United States currently conducts a leasing program for these resources. The Secretary of the Department of the Interior (DOI) has been designated by the Outer Continental Shelf Lands Act of 1953 (43 U.S.C. 1331-1343), as amended by the Outer Continental Shelf Lands Act Amendments of 1978 (43 U.S.C. 1801-1866), to manage and regulate many of the activities that relate to the leasing, exploration, development, and production of the OCS mineral resources. Many of the Secretary's responsibilities have been delegated to the Bureau of Land Management (BLM) and the Minerals Management Service (MMS). Responsibilities of the Minerals Management Service were formerly delegated to the Conservation Division of the U.S. Geological Survey (USGS).

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8218","usgsCitation":"Collignon, M.A., 1982, Alaska index (December 1980 - November 1981): U.S. Geological Survey Open-File Report 82-18, vii, 81 p., https://doi.org/10.3133/ofr8218.","productDescription":"vii, 81 p.","costCenters":[],"links":[{"id":141313,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0018/report-thumb.jpg"},{"id":427424,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0018/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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Mary Ann","contributorId":91490,"corporation":false,"usgs":true,"family":"Collignon","given":"Mary","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":157628,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10373,"text":"ofr82123 - 1982 - Preliminary evaluation of the potential for artificial ground-water recharge in eastern San Joaquin County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-123","title":"Preliminary evaluation of the potential for artificial ground-water recharge in eastern San Joaquin County, California","docAbstract":"In response to increasing demand on water supplies and declining water levels in San Joaquin County, the U. S. Geological Survey, in cooperation with the San Joaquin County Flood Control and Water Conservation District, is evaluating the potential for artificially recharging the aquifer system in eastern San Joaquin County, California. Through a well canvass and analyses of existing data on geology, soils, and drillers logs, this study (phase one of three phases) resulted in identification of 20 sites for exploratory test drilling in areas potentially favorable for artificial recharge. Ten of the sites are in areas adjacent to the Mokelumne River, six are in areas adjacent to the Calaveras River and Mormon Slough, and four are north of Littlejohns Creek. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82123","usgsCitation":"Mitten, H., 1982, Preliminary evaluation of the potential for artificial ground-water recharge in eastern San Joaquin County, California: U.S. Geological Survey Open-File Report 82-123, viii, 46 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82123.","productDescription":"viii, 46 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":142619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0123/report-thumb.jpg"},{"id":38206,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669096","contributors":{"authors":[{"text":"Mitten, H. T.","contributorId":88735,"corporation":false,"usgs":true,"family":"Mitten","given":"H. T.","affiliations":[],"preferred":false,"id":161276,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8388,"text":"ofr82558 - 1982 - Compendium of available surface-water data in the upper Tombigbee River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:06:06","indexId":"ofr82558","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-558","title":"Compendium of available surface-water data in the upper Tombigbee River basin","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82558","usgsCitation":"Colson, B., and Gardner, R.A., 1982, Compendium of available surface-water data in the upper Tombigbee River basin: U.S. Geological Survey Open-File Report 82-558, 324 p. , https://doi.org/10.3133/ofr82558.","productDescription":"324 p. ","costCenters":[],"links":[{"id":141523,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa3e7","contributors":{"authors":[{"text":"Colson, B.E.","contributorId":71546,"corporation":false,"usgs":true,"family":"Colson","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":157643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gardner, Richard Alfred","contributorId":89134,"corporation":false,"usgs":true,"family":"Gardner","given":"Richard","email":"","middleInitial":"Alfred","affiliations":[],"preferred":false,"id":157644,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10366,"text":"ofr82586 - 1982 - A summary of U.S. Geological Survey marine geological data collected in the Beaufort Sea, Alaska, July through August 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr82586","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-586","title":"A summary of U.S. Geological Survey marine geological data collected in the Beaufort Sea, Alaska, July through August 1981","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82586","usgsCitation":"Minkler, P., Reimnitz, E., and Barnes, P.W., 1982, A summary of U.S. Geological Survey marine geological data collected in the Beaufort Sea, Alaska, July through August 1981: U.S. Geological Survey Open-File Report 82-586, 10 p., maps ;28 cm., https://doi.org/10.3133/ofr82586.","productDescription":"10 p., maps ;28 cm.","costCenters":[],"links":[{"id":143557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0586/report-thumb.jpg"},{"id":38203,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0586/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a60cf","contributors":{"authors":[{"text":"Minkler, P.W.","contributorId":87933,"corporation":false,"usgs":true,"family":"Minkler","given":"P.W.","affiliations":[],"preferred":false,"id":161264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":161263,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barnes, P. W.","contributorId":8819,"corporation":false,"usgs":true,"family":"Barnes","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":161262,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":8392,"text":"ofr82250 - 1982 - The economic feasibility of operational earth sensing from space","interactions":[],"lastModifiedDate":"2022-08-22T20:46:50.824266","indexId":"ofr82250","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-250","title":"The economic feasibility of operational earth sensing from space","docAbstract":"

Earth-sensing satellites designed to follow Landsat involve spatial resolution in the order of 10 to 30 m as compared to the 80 m of the Landsat Multispectral Scanner (MSS). At these higher resolutions such satellites will perform inspection functions of high importance to government agencies and which are beyond the capabilities of the Landsat MSS.

There is considerable evidence that nations that cannot afford their own Earth-sensing satellites are willing to pay a suitable price for the capability of inspecting their own land and adjacent sea areas. A unit price of 25 cents per square km per year is suggested as a reasonable fee which would provide economic viability to a well defined satellite system such as the Mapsat defined by the U.S. Geological Survey.

This concept and pricing involve only the satellite and its data acquisition and transmission capability. Data reception, processing and distribution would remain a separate function to be implemented on a local or regional basis as is now done.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82250","usgsCitation":"Colvocoresses, A.P., 1982, The economic feasibility of operational earth sensing from space: U.S. Geological Survey Open-File Report 82-250, 6 p., https://doi.org/10.3133/ofr82250.","productDescription":"6 p.","costCenters":[],"links":[{"id":405412,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0250/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142086,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0250/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668174","contributors":{"authors":[{"text":"Colvocoresses, Alden P.","contributorId":72779,"corporation":false,"usgs":true,"family":"Colvocoresses","given":"Alden","email":"","middleInitial":"P.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":157648,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8404,"text":"ofr82680 - 1982 - Support by the U.S. Geological Survey for adjudications, compacts, and treaties","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr82680","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-680","title":"Support by the U.S. Geological Survey for adjudications, compacts, and treaties","docAbstract":"The U.S. Geological Survey supports interstate compacts, treaties, and court decrees by providing hydrologic data and analysis needed in their administration and by providing Federal representation on compact commissions. As part of this program, in fiscal year 1982 the Geological Survey operated 171 streamflow stations, 3 sediment stations, and 13 water-quality stations, and conducted ground-water studies at a cost of $1,014,000. Funding for Federal representation to i0 interstate compacts is presently budgeted at $56,000.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82680","usgsCitation":"Condes de la Torre, A., 1982, Support by the U.S. Geological Survey for adjudications, compacts, and treaties: U.S. Geological Survey Open-File Report 82-680, iv, 28 p. :maps ;28 cm., https://doi.org/10.3133/ofr82680.","productDescription":"iv, 28 p. :maps ;28 cm.","costCenters":[],"links":[{"id":142166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0680/report-thumb.jpg"},{"id":35968,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0680/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697cbd","contributors":{"authors":[{"text":"Condes de la Torre, Alberto","contributorId":73570,"corporation":false,"usgs":true,"family":"Condes de la Torre","given":"Alberto","email":"","affiliations":[],"preferred":false,"id":157662,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10343,"text":"ofr82347 - 1982 - Appraisal of the Pelican River sand-plain aquifer, western Minnesota","interactions":[],"lastModifiedDate":"2021-10-26T19:51:21.499199","indexId":"ofr82347","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-347","title":"Appraisal of the Pelican River sand-plain aquifer, western Minnesota","docAbstract":"

The Pelican River sand-plain area includes approximately 200 square miles of outwash deposits in parts of Decker, Otter Tail, and Clay Counties in west-central Minnesota. Saturated thickness of the outwash is as much as 140 feet and yields of properly constructed wells locally may exceed 1,200 gallons per minute.

\n

Recharge to the outwash from snowmelt and rain ranged from 3.2 to 6.1 inches during 1979-80. Discharge from the aquifer, as base flow of the Pelican River, averaged 2.0 inches during 1979-80. Evapotranspiration is 22.4 inches per year. The chemical quality of ground water is suitable for irrigation, as measured by sodium-adsorption ratios, but locally high concentrations of calcium, magnesium, and bicarbonate may cause clogging of well screens.

\n

Mathematical models of parts of the ground-water-flow system indicate that lake levels and streamflow may decline because of pumping wells. The exact water-level decline depends on the total number of wells, pumping rates, location of pumping wells with respect to one another and to surface-water bodies, duration of pumping, and the quantity of ground-water recharge. Sensitivity analyses of the models indicates that additional data on hydraulic conductivity, evapotranspiration, and recharge may increase the reliability of model results.

\n

Buried aquifers are known to be present in the area. Aquifer-test results showed that pumping from a buried aquifer had no effect on water levels in the unconfined aquifer.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr82347","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources, the Western Minnesota Resources Conservation and Development Commission, and the Pelican River Sands Steering Committee","usgsCitation":"Miller, R.T., 1982, Appraisal of the Pelican River sand-plain aquifer, western Minnesota: U.S. Geological Survey Open-File Report 82-347, Report: v, 44 p.; 3 Plates: 29.60 x 42.14 inches or smaller, https://doi.org/10.3133/ofr82347.","productDescription":"Report: v, 44 p.; 3 Plates: 29.60 x 42.14 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":390982,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13703.htm"},{"id":94968,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0347/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":94969,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0347/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":94970,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0347/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":94971,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0347/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0347/report-thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Pelican River sand-plain aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -96.32400512695312,\n 46.321326452271464\n ],\n [\n -96.32400512695312,\n 46.969945150264635\n ],\n [\n -95.78979492187499,\n 46.969945150264635\n ],\n [\n -95.78979492187499,\n 46.321326452271464\n ],\n [\n -96.32400512695312,\n 46.321326452271464\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a360","contributors":{"authors":[{"text":"Miller, R. T.","contributorId":15209,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":161224,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10340,"text":"ofr82744 - 1982 - Documentation and user's guide for interactive spectral analysis and filter program package useful in the processing of seismic reflection data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr82744","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-744","title":"Documentation and user's guide for interactive spectral analysis and filter program package useful in the processing of seismic reflection data","docAbstract":"The spectral analysis and filter program package is written in the BASIC language for the HP-9845T desktop computer. The program's main purpose is to perform spectral analyses on digitized time-domain data. In addition, band-pass filtering of the data can be performed in the time domain. Various other processes such as autocorrelation can be performed to the time domain data in order to precondition them for spectral analyses. The frequency domain data can also be transformed back into the time domain if desired. Any data can be displayed on the CRT in graphic form using a variety of plot routines. A hard copy can be obtained immediately using the internal thermal printer. Data can also be displayed in tabular form on the CRT or internal thermal printer or it can be stored permanently on a mass storage device like a tape or disk. A list of the processes performed in the order in which they occurred can be displayed at any time.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82744","usgsCitation":"Miller, J.J., 1982, Documentation and user's guide for interactive spectral analysis and filter program package useful in the processing of seismic reflection data: U.S. Geological Survey Open-File Report 82-744, 55 p., ill. ;28 cm., https://doi.org/10.3133/ofr82744.","productDescription":"55 p., ill. ;28 cm.","costCenters":[],"links":[{"id":143662,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0744/report-thumb.jpg"},{"id":38191,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0744/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d7a6","contributors":{"authors":[{"text":"Miller, J. J.","contributorId":54588,"corporation":false,"usgs":true,"family":"Miller","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161220,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10339,"text":"ofr82774 - 1982 - Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota","interactions":[{"subject":{"id":10339,"text":"ofr82774 - 1982 - Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota","indexId":"ofr82774","publicationYear":"1982","noYear":false,"title":"Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":2314,"text":"wsp2243 - 1984 - Changes in flood response of the Red River of the North basin, North Dakota-Minnesota","indexId":"wsp2243","publicationYear":"1984","noYear":false,"title":"Changes in flood response of the Red River of the North basin, North Dakota-Minnesota"},"id":1}],"supersededBy":{"id":2314,"text":"wsp2243 - 1984 - Changes in flood response of the Red River of the North basin, North Dakota-Minnesota","indexId":"wsp2243","publicationYear":"1984","noYear":false,"title":"Changes in flood response of the Red River of the North basin, North Dakota-Minnesota"},"lastModifiedDate":"2018-03-09T13:58:25","indexId":"ofr82774","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-774","title":"Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota","docAbstract":"

The magnitude and frequency of large floods that have occurred in recent years in the basin of the Red River of the North have caused concern that land-use changes and manmade drainage have increased flooding. This study was undertaken to determine if any changes in flood response of the Red River basin can be documented. A review of the hydrologic setting, previous floods, flood-control measures, and probable effects of land-use changes shows that the flooding problem of the Red River basin is complex hydrologically, highly variable historically, and follows a regional pattern. Therefore, a change in flood response of the basin is difficult to identify. The flood-frequency, regression, normalized-hydrograph, and double-mass analyses show little indication of significant change in flood response of the Red River basin at locations on the main stem. However, the large variation in flood discharges may mask or dwarf small changes in response of the basin.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82774","usgsCitation":"Miller, J.E., and Frink, D.L., 1982, Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota: U.S. Geological Survey Open-File Report 82-774, viii, 166 p., https://doi.org/10.3133/ofr82774.","productDescription":"viii, 166 p.","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":94967,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0774/report.pdf","size":"8340","linkFileType":{"id":1,"text":"pdf"}},{"id":143661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0774/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6cdb","contributors":{"authors":[{"text":"Miller, Jeffrey E.","contributorId":76717,"corporation":false,"usgs":true,"family":"Miller","given":"Jeffrey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frink, Dale L.","contributorId":59421,"corporation":false,"usgs":true,"family":"Frink","given":"Dale","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8426,"text":"ofr82625 - 1982 - Sonobuoy seismic data collected during 1982 in the Bering Sea","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr82625","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-625","title":"Sonobuoy seismic data collected during 1982 in the Bering Sea","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82625","usgsCitation":"Cooper, A.K., Marlow, M.S., and O'Brien, T., 1982, Sonobuoy seismic data collected during 1982 in the Bering Sea: U.S. Geological Survey Open-File Report 82-625, 8 p., map ;28 cm., https://doi.org/10.3133/ofr82625.","productDescription":"8 p., map ;28 cm.","costCenters":[],"links":[{"id":141530,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0625/report-thumb.jpg"},{"id":35998,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0625/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e77d2","contributors":{"authors":[{"text":"Cooper, A. K.","contributorId":50149,"corporation":false,"usgs":true,"family":"Cooper","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":157695,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marlow, M. S.","contributorId":76743,"corporation":false,"usgs":true,"family":"Marlow","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":157697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O'Brien, Thomas","contributorId":75924,"corporation":false,"usgs":true,"family":"O'Brien","given":"Thomas","affiliations":[],"preferred":false,"id":157696,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10336,"text":"ofr8231 - 1982 - Water for western oil shale development: Potential local supplies","interactions":[],"lastModifiedDate":"2022-09-23T20:26:58.565482","indexId":"ofr8231","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-31","title":"Water for western oil shale development: Potential local supplies","docAbstract":"

Commercial-scale development of western oil shale resources will require a supply of water for both extraction and reclamation purposes. This paper summarizes some of the information on the occurrence of potential local supplies of water in the Piceance Creek Basin-Uinta Basin areas of northwest Colorado and northeast Utah. The discussion is somewhat hypothetical in that it is restricted to the physical occurrence of water with emphasis on water resources in each basin. Of course, the many potential constraints on water use (including economics, water quality, legal and other institutional factors) are necessarily secondary to the ultimate constraint, its physical occurrence. Perhaps the most obvious constraint is that of water rights and water laws. For example, \"mining\" of some of the ground water is herein assumed to be necessary for technically sound management and utilization of the water resource, but the hydrologic effects of such \"mining\" would require accommodation under water laws and agreements.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8231","usgsCitation":"Miller, G., 1982, Water for western oil shale development: Potential local supplies: U.S. Geological Survey Open-File Report 82-31, 6 p., https://doi.org/10.3133/ofr8231.","productDescription":"6 p.","costCenters":[],"links":[{"id":143503,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0031/report-thumb.jpg"},{"id":407297,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Piceance Creek Basin, Uinta Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.9893798828125,\n 40.17047886718109\n ],\n [\n -108.2537841796875,\n 40.17047886718109\n ],\n [\n -108.2537841796875,\n 40.925964939514294\n ],\n [\n -110.9893798828125,\n 40.925964939514294\n ],\n [\n -110.9893798828125,\n 40.17047886718109\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa1f2","contributors":{"authors":[{"text":"Miller, G.A.","contributorId":107671,"corporation":false,"usgs":true,"family":"Miller","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":161215,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10334,"text":"ofr821062 - 1982 - Preliminary geologic map of the Continental Mountain area","interactions":[],"lastModifiedDate":"2024-01-08T22:46:34.71488","indexId":"ofr821062","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1062","title":"Preliminary geologic map of the Continental Mountain area","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821062","usgsCitation":"Miller, F.K., 1982, Preliminary geologic map of the Continental Mountain area: U.S. Geological Survey Open-File Report 82-1062, Report: 33 p.; 1 Plate: 27.98 x 32.54 inches, https://doi.org/10.3133/ofr821062.","productDescription":"Report: 33 p.; 1 Plate: 27.98 x 32.54 inches","costCenters":[],"links":[{"id":424202,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13636.htm","linkFileType":{"id":5,"text":"html"}},{"id":38186,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1062/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38185,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1062/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143501,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1062/report-thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Continental Mountain area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117,\n 49\n ],\n [\n -117,\n 48.75\n ],\n [\n -116.75,\n 48.75\n ],\n [\n -116.75,\n 49\n ],\n [\n -117,\n 49\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db6548df","contributors":{"authors":[{"text":"Miller, Fred K.","contributorId":89503,"corporation":false,"usgs":true,"family":"Miller","given":"Fred","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":161213,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8160,"text":"ofr82454 - 1982 - Sketch maps, sections and laboratory analyses of peat resources in deposits in and near Piscataquis and Somerset counties and northeastern Aroostook County, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:06:07","indexId":"ofr82454","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-454","title":"Sketch maps, sections and laboratory analyses of peat resources in deposits in and near Piscataquis and Somerset counties and northeastern Aroostook County, Maine","docAbstract":"Peat deposits in and near Piscataquis and Somerset Counties and northeastern Aroostook County, Maine, were investigated for their estimated potential as peat resources suitable for energy, horticultural, and agricultural uses. Fifty sketch maps with sections and laboratory analyses illustrate the amount and quality of peat resources. The total yield of commercial quality peat is estimated at 23,670,000 short tons air-dried peat.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82454","usgsCitation":"Cameron, C., and Mullen, M., 1982, Sketch maps, sections and laboratory analyses of peat resources in deposits in and near Piscataquis and Somerset counties and northeastern Aroostook County, Maine: U.S. Geological Survey Open-File Report 82-454, ix, 169 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82454.","productDescription":"ix, 169 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141550,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0454/report-thumb.jpg"},{"id":35769,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0454/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eec8c","contributors":{"authors":[{"text":"Cameron, C. C.","contributorId":94299,"corporation":false,"usgs":true,"family":"Cameron","given":"C. C.","affiliations":[],"preferred":false,"id":157250,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mullen, M.K.","contributorId":30228,"corporation":false,"usgs":true,"family":"Mullen","given":"M.K.","email":"","affiliations":[],"preferred":false,"id":157249,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8434,"text":"ofr82933 - 1982 - Aeromagnetic measurements in the Cascade Range and Modoc Plateau of northern California; report on work done from December 1, 1980, to May 31, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:06","indexId":"ofr82933","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-933","title":"Aeromagnetic measurements in the Cascade Range and Modoc Plateau of northern California; report on work done from December 1, 1980, to May 31, 1981","docAbstract":"Spectral analysis of aeromagnetic data collected over 6orth-central California during the summer of 1980 aided in determining magnetic-source bottom depths beneath the survey area. Five regions of shallow magnetic source bottom depths were detected: 1) Secret Spring Mountain and National Lava Beds Monument area, 2) the Mount Shasta area, 3) the Eddys Mountain area, 4) the Big Valley Mountains area, and 5) an area northeast of Lassen Peak. Except for the Eddys Mountain area, all regions exhibiting shallow depths are suggested to be due to elevated Curie-point isotherms. \r\n\r\nThe elevated Curie-point depth beneath Secret Spring Mountain and the National Lava Beds Monument area was found to be 4-7 km BSL (Below Sea Level) and is an extension of a zone mapped beneath an area immediately to the north in Oregon. A similar depth was detected for the Mount Shasta area and the area northeast of Lassen Peak. A depth of 4-6 km BSL was detected beneath the Big Valley Mountains area. The shallow Curie-point depths beneath Secret Spring Mountain, Mount Shasta, Big Valley Mountains, and the area northeast of Lassen Peak appear to form a segmented Zone of elevated Curie-point isotherm depths which underlies the High Cascade Mountains and Modoc Plateau in north-central California. A small area of shallow depths to magnetic-source bottoms, 4-5 km BSL, beneath the Eddys Mountain area is attributed to a lithologic boundary rather than an elevated Curie-point isotherm. \r\n\r\nDeeper magnetic source bottom depths were mapped throughout the remainder of the study area, with depths greater than 9 km BSL indicated beneath Lassen Peak and greater than ii km BSL indicated beneath the Western Cascades, Eastern Klamath Mountains, and Great Valley.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82933","usgsCitation":"Couch, R.W., and Gemperle, M., 1982, Aeromagnetic measurements in the Cascade Range and Modoc Plateau of northern California; report on work done from December 1, 1980, to May 31, 1981: U.S. Geological Survey Open-File Report 82-933, 34 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82933.","productDescription":"34 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0933/report-thumb.jpg"},{"id":36001,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0933/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689ba4","contributors":{"authors":[{"text":"Couch, Richard W.","contributorId":22351,"corporation":false,"usgs":true,"family":"Couch","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gemperle, Michael","contributorId":47786,"corporation":false,"usgs":true,"family":"Gemperle","given":"Michael","email":"","affiliations":[],"preferred":false,"id":157709,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10328,"text":"ofr82834 - 1982 - Preliminary geologic map of Patterson Pass and Crater Island NW quadrangles, Box Elder County, Utah, and Elko County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr82834","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-834","title":"Preliminary geologic map of Patterson Pass and Crater Island NW quadrangles, Box Elder County, Utah, and Elko County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82834","usgsCitation":"Miller, D., Lush, A., and Schneyer, J., 1982, Preliminary geologic map of Patterson Pass and Crater Island NW quadrangles, Box Elder County, Utah, and Elko County, Nevada: U.S. Geological Survey Open-File Report 82-834, 23 p., 2 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr82834.","productDescription":"23 p., 2 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":108442,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13837.htm","linkFileType":{"id":5,"text":"html"},"description":"13837"},{"id":143477,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0834/report-thumb.jpg"},{"id":38177,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0834/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38178,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0834/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38179,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0834/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6993f6","contributors":{"authors":[{"text":"Miller, D. M. 0000-0003-3711-0441","orcid":"https://orcid.org/0000-0003-3711-0441","contributorId":104422,"corporation":false,"usgs":true,"family":"Miller","given":"D. M.","affiliations":[],"preferred":false,"id":161205,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lush, A.P.","contributorId":23010,"corporation":false,"usgs":true,"family":"Lush","given":"A.P.","affiliations":[],"preferred":false,"id":161203,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schneyer, J.D.","contributorId":93762,"corporation":false,"usgs":true,"family":"Schneyer","given":"J.D.","affiliations":[],"preferred":false,"id":161204,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":10318,"text":"ofr82475 - 1982 - Geophysical logs of nine holes drilled in 1978 in the Yampa coal field, Hamilton and Pagoda quadrangles, Moffat County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr82475","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-475","title":"Geophysical logs of nine holes drilled in 1978 in the Yampa coal field, Hamilton and Pagoda quadrangles, Moffat County, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82475","usgsCitation":"Meyer, R.F., and Brown, R., 1982, Geophysical logs of nine holes drilled in 1978 in the Yampa coal field, Hamilton and Pagoda quadrangles, Moffat County, Colorado: U.S. Geological Survey Open-File Report 82-475, i, 34 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82475.","productDescription":"i, 34 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":143256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0475/report-thumb.jpg"},{"id":38171,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0475/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b58b","contributors":{"authors":[{"text":"Meyer, R. F.","contributorId":52167,"corporation":false,"usgs":true,"family":"Meyer","given":"R.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":161188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, R.R.","contributorId":83126,"corporation":false,"usgs":true,"family":"Brown","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":161189,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8445,"text":"ofr8235 - 1982 - Environmental geology of Harrison Bay, northern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr8235","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-35","title":"Environmental geology of Harrison Bay, northern Alaska","docAbstract":"The surficial and shallow subsurface geology of Harrison Bay on the Beaufort Sea coast was mapped as part of the U.S. Geological Survey's prelease evaluation for Outer Continental Shelf (OCS) Oil and Gas Lease Sale 71. During the 1980 summer season, approximately 1600 km of multisensored, high-resolution geophysical profile data were collected along a rectangular grid with 4.8 km line spacing. Interpretation of these data is presented on five maps showing bathymetry, sea-floor microrelief, ice-gouge characteristics, Holocene sediment thickness, and geologic structure to depths of approximately 1000 m. \r\n\r\nOn a broad scale, the seafloor is shallow and almost flat, although microrelief features produced by sediment transport and ice-gouge processes typically vary up to several meters in amplitude. Microrelief bedforms related to hydraulic processes are predominant in water depths less than 12 m. Microrelief caused by ice gouging generally increases with water depth, reaching a maximum of 2 m or more in water depths beyond the 20 m isobath. This intensely gouged area lies beneath the shear zone between the seasonal landfast ice and the mobile polar ice pack. \r\n\r\nThe thickness of recent (Holocene) sediment increases offshore, from 2 m near the Colville River delta to 30 m or more on the outer shelf. The thin Holocene layer is underlain by a complex horizon interpreted to be the upper surface of a Pleistocene deposit similar in composition to the present Arctic Coastal Plain. The base of the inferred Pleistocene section is interpreted to be a low-angle unconformity 100 m below sea level. Beneath this Tertiary-Quaternary unconformity, strata are interpreted to be alluvial fan-delta plain deposits corresponding to the Colville Group and younger formations of Late Cretaceous to Tertiary age. Numerous high-angle faults downthrown to the north trend across the survey area. With few exceptions, these faults terminate at or below the 100 m unconformity, suggesting that most tectonism occurred before Quaternary time. Acoustic anomalies suggesting gas accumulation are rare, and where identified typically occur adjacent to faults. A laterally continuous zone of poor seismic data occurs in the nearshore area and is interpreted to be caused by subsea permafrost. This report describes these geologic conditions in Harrison Bay and discusses potential hazards that they may pose for future oil and gas operations in Sale 71 and adjacent Beaufort Sea shelf areas.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8235","usgsCitation":"Craig, J., and Thrasher, G.P., 1982, Environmental geology of Harrison Bay, northern Alaska: U.S. Geological Survey Open-File Report 82-35, iii, 28 p., 6 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr8235.","productDescription":"iii, 28 p., 6 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":140504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0035/report-thumb.jpg"},{"id":36009,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36010,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36011,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36012,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36013,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36014,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0035/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36015,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db6723d7","contributors":{"authors":[{"text":"Craig, J.D.","contributorId":14405,"corporation":false,"usgs":true,"family":"Craig","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":157726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thrasher, G. P.","contributorId":42939,"corporation":false,"usgs":true,"family":"Thrasher","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":157727,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8447,"text":"ofr82222 - 1982 - Uranium potential of the Burro Canyon Formation in western Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr82222","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-222","title":"Uranium potential of the Burro Canyon Formation in western Colorado","docAbstract":"The Burro Canyon Formation of Early Cretaceous age overlies the Morrison Formation (Late Jurassic) and underlies the Dakota Sandstone (Late Cretaceous) over most of southeastern Utah and southwestern Colorado. It consists mainly of alternating beds of fluvial sandstone and overbank mudstone with sandstone dominating in the lower part of the formation and mudstone in the upper part. At the outcrop, the sandstones in the formation exhibit almost all the characteristics that are considered favorable for the occurrence of sandstone-type uranium deposits, but only a few small deposits have been discovered in the Colorado-Utah area. The major deficiency of the Burro Canyon in these outcrop areas is the absence of a reductant such as carbonaceous debris, humic or humate materials, or pyrite. Reductants were probably removed during a period of extensive oxidation at the time of deposition and during a subsequent erosional episode prior to deposition of the Dakota Sandstone. \r\n\r\nThe formation reaches a lobate, inexactly located eastern margin that extends from near Meeker, Colorado, southward through the Piceance basin to near Aztec, New Mexico, in the northwestern part of the San Juan Basin. Along much of this distance, the formation is in the subsurface and has been penetrated by only a few drill holes. Along this eastern margin, the lobes project eastward where fluvial distributary streams built minor alluvial fans of relatively high-energy deposits out from the main axis of Burro Canyon stream deposition. The lower and distal reaches of these lobes may have survived the period of post depositional erosion and oxidation in a reduced condition because of low relief and the protection of a high water table. If so, the peripheral and distal parts of these lobes may have retained the precipitants necessary to form a uranium deposit. Two of the lobes extend into the southwest margin of the Piceance Basin and are considered the possible location of uranium deposits. Two additional lobes extend into the northwestern part of the San Juan Basin but have not been evaluated in this study.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82222","usgsCitation":"Craig, L., 1982, Uranium potential of the Burro Canyon Formation in western Colorado: U.S. Geological Survey Open-File Report 82-222, 27 p., 4 over-size sheets, maps ;28 cm., https://doi.org/10.3133/ofr82222.","productDescription":"27 p., 4 over-size sheets, maps ;28 cm.","costCenters":[],"links":[{"id":140506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0222/report-thumb.jpg"},{"id":36016,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0222/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36017,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0222/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36018,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0222/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36019,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0222/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36020,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0222/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688016","contributors":{"authors":[{"text":"Craig, L.C.","contributorId":61419,"corporation":false,"usgs":true,"family":"Craig","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":157731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10302,"text":"ofr82650 - 1982 - Water quality of Belton Lake, central Texas","interactions":[],"lastModifiedDate":"2016-08-11T15:16:38","indexId":"ofr82650","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-650","title":"Water quality of Belton Lake, central Texas","docAbstract":"

The concentrations of dissolved solids, chloride, and sulfate in Belton Lake on the Leon River in central Texas average about 240 milligrams per liter, 40 milligrams per liter, and 30 milligrams per liter, respectively. The water is hard or very hard, averaging 170 milligrams per liter as calcium carbonate. The average concentrations of these constituents and hardness are least during late summer and early fall after periods of sustained high inflow.

\n

Thermal stratification begins to develop in Belton Lake in late February or early March. The water usually is stratified into three fairly distinct layers by early June, and stratification usually persists until September or October. Thermal stratification and seasonal variations in the concentrations of dissolved constituents in inflow result in stratification of the principal dissolved constituents. Dissolved solids in water at the surface of deep sites during summer differ from those at the bottom by about 40 milligrams per liter. Thermal stratification also results in significant seasonal and areal variations in dissolved oxygen, dissolved iron, dissolved manganese, total inorganic nitrogen, and total phosphorus.

\n

Oxygen used in the oxidation of dead organisms and other organic material near the bottom of the lake is not replaced during periods of summer stagnation. Consequently, water below depths of 35 to 40 feet (10.7 to 12.2 meters) usually contains less than 1.0 milligram per liter of dissolved oxygen during these periods.

\n

Water near the surface at most sites in the lake throughout the year usually contains less than 30 micrograms per liter of dissolved iron and 20 micrograms per liter of dissolved manganese. Reducing conditions during periods of summer stagnation result in tile dissolution of iron and manganese from the sediments in deep areas of the lake. The concentrations of both constituents are greatest near the bottom at site Ac, a deep site near Belton Dam. Iron concentrations at this site during the summer have ranged from 0 to 600 micrograms per liter and have averaged about 290 micrograms per liter; manganese concentrations have ranged from 0 to 540 micrograms per liter and have averaged about 320 micrograms per liter.

\n

Concentrations of total inorganic nitrogen and total phosphorus are greatest at deep sites during periods of summer stagnation when decay of aquatic organisms and chemical reduction of bottom sediments release the constituents to the water. The concentrations of total inorganic nitrogen and total phosphorus in the bottom stratum of water at site A c during the summer average about 0.75 milligram per liter of nitrogen and 0.10 milligram per liter of phosphorus. The concentrations of these constituents in the surface stratum at site A C during the summer average about 0.02 milligram per liter of nitrogen and 0.01 milligram per liter of phosphorus.

\n

The maximum concentrations of chlorinated hydrocarbon insecticides or their degradation products detected in bottom sediments collected from the lake during four lake surveys included 1.1 micrograms per kilogram of DDT, 3.0 micrograms per kilogram of DDD, 11 micrograms per kilogram of DDE, and 2 micrograms per kilogram of chlordane.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr82650","usgsCitation":"Mendieta, H., and Pate, D.L., 1982, Water quality of Belton Lake, central Texas: U.S. Geological Survey Open-File Report 82-650, Report: vi, 70 p.; Plate: 10.52 x 16.63 inches, https://doi.org/10.3133/ofr82650.","productDescription":"Report: vi, 70 p.; Plate: 10.52 x 16.63 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":38160,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0650/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38161,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0650/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0650/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478fe4b07f02db48a09f","contributors":{"authors":[{"text":"Mendieta, H.B.","contributorId":38965,"corporation":false,"usgs":true,"family":"Mendieta","given":"H.B.","email":"","affiliations":[],"preferred":false,"id":161164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pate, Dale L.","contributorId":55007,"corporation":false,"usgs":true,"family":"Pate","given":"Dale","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161165,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10286,"text":"ofr82753 - 1982 - Water-quality reconnaissance of the north Dade County solid-waste facility, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:06:22","indexId":"ofr82753","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-753","title":"Water-quality reconnaissance of the north Dade County solid-waste facility, Florida","docAbstract":"A water-quality sampling reconnaissance of the north Dade County solid-waste disposal facility (landfill) near Carol City, Florida, was conducted during 1977-78. The purpose of the reconnaissance was to determine selected quality characteristics of the surface- and ground-water of the landfill and contiguous area; and to assess, generally, if leachate produced by the decomposition of landfill wastes was adversely impacting the downgradient water quality. Sampling results indicated that several water-quality characteristics were present in landfill ground water at significantly higher levels than in ground water upgradient or downgradient from the landfill. Moreover, many of these water-quality characteristics were found at slightly higher levels at down gradient site 5 than at upgradient site 1 which suggested that some downgradient movement of landfill leachate had occurred. For example, chloride and alkalinity in ground water had average concentrations of 20 and 290 mg/L at background wells (site 1), 144 and 610 mg/L at landfill wells (sites 2 and 4), and 29 and 338 mg/L at downgradient wells (site 5). A comparison of the 1977-78 sampling results with the National Primary and Secondary Drinking Water Regulations indicated that levels of iron and color in ground water of the study area frequently exceeded national maximum contaminant levels, dissolved solids, turbidity, lead, and manganese occasionally exceeded regulations. Concentrations of iron and levels of color and turbidity in some surface water samples also exceeded National maximum contaminant levels. 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