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Water resources data for the 1973 water year for Mississippi including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, and records of water-quality data on the chemical and physical characteristics of surface water, are given in this report. In Part 1, records are included for 79 gaging stations of which 75 are streamflow discharge stations, and 4 are reservoir or lake stations; also are included records for 58 low-flow partial-record stations, 139 crest-stage partial-record stations, and 79 miscellaneous sites. Locations of gaging stations are shown in Figure 1. In Part 2, data on the quality of surface water (chemical and temperature) were collected from designated sampling sites at predetermined intervals such as monthly, or less frequently. Records are given for 70 sampling stations of which 32 are continuous record stations, 26 are partial-record stations, and 12 are miscellaneous sites. Locations of water-quality stations are shown in Figure 1. A few pertinent stations (not included above) furnished by bordering States are also included in this report. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of L. E. Carroon, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Mississippi.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMS731","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for Mississippi, water year 1973: U.S. Geological Survey Water Data Report MS-73-1, vii, 184 p., https://doi.org/10.3133/wdrMS731.","productDescription":"vii, 184 p.","costCenters":[],"links":[{"id":493095,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1973/ms-73-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175275,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1973/ms-73-1/report-thumb.jpg"}],"country":"United 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in rocks, Coeur d'Alene district, Idaho","language":"ENGLISH","doi":"10.3133/ofr74341","usgsCitation":"Gott, G.B., and Cathrall, J.B., 1974, Geochemical distribution of selected metals in rocks, Coeur d'Alene district, Idaho: U.S. Geological Survey Open-File Report 74-341, 8 sheets, https://doi.org/10.3133/ofr74341.","productDescription":"8 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Water resources data for the 1973 water year for West Virginia including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, records of water-quality data on the chemical and physical characteristics of surface water, and records of ground-water levels at index wells are given in this report. In Part 1, records are included for 126 gaging stations of which 119 are streamflow discharge stations, 1 is stage only streamflow station, and 6 are reservoir or lake stations; also included are records for 2 low-flow partial-record stations, 39 crest-stage partial-record stations and 7 miscellaneous sites. Locations of gaging stations are shown in Figure 1, and location of partial-record stations are shown in Figure 2. In Part 2, data on the quality of surface water (chemical, temperature, and sediment) were collected from designated sampling sites at predetermined intervals, such as once daily, weekly, monthly, or less frequently, and at some sites data were recorded on punched paper tape at 15-, 30-, or 60-minute intervals. Records are given for 28 sampling stations of which 18 are continuous record stations, and 10 are partial-record stations. Locations of water quality stations are shown in Figure 1. A few pertinent stations (not included above) in bordering States are also included in this report. In Part 3, records are included for 46 observation wells of which 8 are equipped with water-level recorders that give a continuous graph of the fluctuations, 3 are equipped with digital recorders that punch the water level on a tape at hourly intervals, at 35 manual reading are made with a steel tape by observers on the days indicated. Locations of index wells are shown in Figure 2. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Edwin E. Harris, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in West Virginia.

Beginning with the 1961 water year, streamflow records and related data have been released by the Geological Survey in annual reports on a State-boundary basis. Water-quality records beginning with the 1964 water year have been similarly released either in separate reports or in conjunction with streamflow records. These reports are for limited distribution and are designed primarily for rapid release of data shortly after the end of the water year.

Records of discharge and stage of streams, and contents and stage of lakes and reservoirs are published in a series of U.S. Geological Survey water-supply papers entitled, \"Surface Water Supply of the United States.\" Through September 30, 1960, these water-supply papers were in an annual series and since then are in a 5-year series. Records of chemical quality, water temperatures, and suspended sediment have been published since 1941 in an annual series of water-supply papers entitled, \"Quality of Surface Waters of the United States.\" More information is given under the headings \"Publications\" on page 21. Records of ground water levels are published in a series of water supply papers entitled, \"Ground-water Levels in the United States\". Through 1955 these were in an annual series but are now in a 5-year series. More information is given under the heading \"Publications\" on page 22.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4724","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532891,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2846,"text":"wsp2027 - 1974 - Analog model study of the ground-water basin of the Upper Coachella Valley, California","interactions":[{"subject":{"id":47981,"text":"ofr71287 - 1971 - Analog model study of the ground-water basin of the upper Coachella Valley, California","indexId":"ofr71287","publicationYear":"1971","noYear":false,"title":"Analog model study of the ground-water basin of the upper Coachella Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":2846,"text":"wsp2027 - 1974 - Analog model study of the ground-water basin of the Upper Coachella Valley, California","indexId":"wsp2027","publicationYear":"1974","noYear":false,"title":"Analog model study of the ground-water basin of the Upper Coachella Valley, California"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"wsp2027","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2027","title":"Analog model study of the ground-water basin of the Upper Coachella Valley, California","docAbstract":"An analog model of the ground-water basin of the upper Coachella Valley was constructed to determine the effects of imported water on ground-water levels. The model was considered verified when the ground-water levels generated by the model approximated the historical change in water levels of the ground-water basin caused by man's activities for the period 1986-67. The ground-water basin was almost unaffected by man's activities until about 1945 when ground-water development caused the water levels to begin to decline. The Palm Springs area has had the largest water-level decline, 75 feet since 1986, because of large pumpage, reduced natural inflow from the San Gorgonio Pass area, and diversions of natural inflows at Snow and Falls Creeks and Chino Canyon starting in 1945. The San Gorgonio Pass inflow had been reduced from about 18,000 acre-feet in 1986 to about 9,000 acre-feet by 1967 because of increased ground-water pumpage in the San Gorgonio Pass area, dewatering of the San Gorgonio Pass area that took place when the tunnel for the Metropolitan Water District of Southern California was drilled, and diversions of surface inflow at Snow and Falls Creeks. In addition, 1944-64 was a period of below-normal precipitation which, in part, contributed to the declines in water levels in the Coachella Valley. The Desert Hot Springs, Garnet Hill, and Mission Creek subbasins have had relatively little development; consequently, the water-level declines have been small, ranging from 5 to 15 feet since 1986. In the Point Happy area a decline of about 2 feet per year continued until 1949 when delivery of Colorado River water to the lower valley through the Coachella Canal was initiated. Since 1949 the water levels in the Point Happy area have been rising and by 1967 were above their 1986 levels. \r\n\r\nThe Whitewater River subbasin includes the largest aquifer in the basin, having sustained ground-water pumpage of about 740,000 acre-feet from 1986 to 1967, and will probably continue to provide the most significant supply of ground water for the upper valley. The total ground-water storage depletion for the entire upper valley for 1986-67 was about 600,000 acre-feet, an average storage decrease of about 25,000 acre-feet per year since 1945. \r\n\r\nTransmissivity for the Whitewater River subbasin ranges from 860,000 gallons per day per foot (near Point Happy) to 50,000 gallons per day per foot, with most of the subbasin about 800,000 gallons per day per foot. In contrast, the transmissivities of the Desert Hot Springs, Mission Creek, and Garnet Hill subbasins generally range from 2,000 to 100,000, but the highest value, beneath the Mission Creek streambed deposits, is 200,000 gallons per day per foot; the transmissivity for most of the area of th6 three subbasins is 80,000 gallons per day per foot.\r\n\r\nThe storage coefficients are representative of water-table conditions, ranging from 0.18 beneath the Mission Creek stream deposits to 0.06 in the Palm Springs area. \r\n\r\nThe model indicated that the outflow at Point Happy decreased from 50,000 acre-feet in 1936 to 30,000 acre-feet by 1967 as a result of the rising water levels in the lower valley. \r\n\r\nThe most logical area to recharge the Colorado River water is the Windy Point-Whitewater area, where adequate percolation rates of 2-4 acre-feet per acre per day are probable. The Whitewater River bed may be the best location to spread the water if the largest part of the imported water can be recharged during low-flow periods. The area in sec. 21, T. 2 S., R. 4 E., would be adequate for the smaller quantities of recharge proposed for the Mission Creek area. \r\n\r\nProjected pumpage for the period 1968-2000 was programmed on the model with the proposed recharge of Colorado River water for the same period. The model indicated a maximum water-level increase of 200 feet above the 1967 water level at Windy Point, the proposed recharge site, by the year 2000, a 130-foot increase by 1990, and a 20-foot increas","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2027","usgsCitation":"Tyley, S.J., 1974, Analog model study of the ground-water basin of the Upper Coachella Valley, California: U.S. Geological Survey Water Supply Paper 2027, v, 77 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp2027.","productDescription":"v, 77 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138697,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2027/report-thumb.jpg"},{"id":29418,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2027/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6837f5","contributors":{"authors":[{"text":"Tyley, Stephen J.","contributorId":35355,"corporation":false,"usgs":true,"family":"Tyley","given":"Stephen","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145897,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25926,"text":"wri7414 - 1974 - Water quality and streamflow characteristics, Raritan River Basin, New Jersey","interactions":[],"lastModifiedDate":"2012-09-11T17:16:26","indexId":"wri7414","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"14-74","title":"Water quality and streamflow characteristics, Raritan River Basin, New Jersey","docAbstract":"The findings of a problem-oriented river-system investigation of the stream-quality and streamflow characteristics of the Raritan River basin (1,105 square miles or 2,862 square kilometers drainage area) are described. The investigation covers mainly the period 1955-72.\r\n

Precipitation in the basin is classified as ample and averages 47 inches or 120 centimeters per year (3-5 inches or 8-12 centimeters per month). During the study period four general precipitation trends were noted: less than normalin 1955-61 and 1966-70; extreme drought in 1962-66; and above normal in 1971-72.

\r\n

Analyses of streamflow measurements at eight gaging stations indicate a general trend toward lower flows during the study period, which is attributed to generally lower than normal precipitation. Highest flows were observed in 1958, concurrent with maximum annual precipitation; whereas lowest flows were observed in 1965 during extreme drought conditions.

\r\n

Non-tidal streams in the basin are grouped into three general regions of similar chemical quality based upon predominant constituents and dissolved-solids concentration during low-flow conditions. The predominant cations in solution in all regions are calcium and magnesium (usually exceeding 60 percent of total cation content). In headwater streams of the North and South Branch Raritan Rivers, bicarbonate is the predominant anion; a combination of sulfate, chloride, and nitrate are the predominant anions in the other two regions. The dissolved-solids concentration of streams in areas little influenced by man's activities generally range from 40 to 200 mg/L. Those in areas influenced by man often range much higher sometimes exceeding 800 mg/L. Suspended-sediment yields in the basin range from 25 to 500 tons per square mile annually.

\r\n

The water quality of the Raritan River and most tributaries above Manville (784 square miles of 2,030 square kilometers drainage area) generally is good for most industrial, domestic, and recreational uses, although pollution has been reported locally in some areas. A comparison of chemical analyses of water collected at several sampling sites in the 1920's with more recent data, however, indicate that there has been a significant increase in sulfate, chloride, and nitrate ions transported per unit of streamflow. These increases reflect increased waste-water discharges and nutrients in agricultural runoff in the upper basin.

\r\n

Trends in the dissolved-solids and dissolved-oxygen concentation of water in the Raritan and MIllstone Rivers above their confluence at Manville are described. The dissolved solids of the Millstone River are shown to increase, particularly at low streamflows. For example, at a flow of 100 cubic feet per second (2.83 cubic meters per second) this river tansported 13 percent more dissolved solids in 1969-70 than it did in 1957-58. A similar trend, however, was not apparent on the Raritan River. This phenomenon is attributed to dilution provided since 1964 by upstream reservoir releases during low flows.

\r\n

With the exception of low-flow periods on the Raritan River, dissolved-oxygen concentrations showed little or no significant time trends at Manville on either the Raritan or Millstone River. An improvement in dissolved-oxygen content at flows lower than 100 cubic feet per second (2.83 cubic meters per second) is observed with time on the Raritan River. This improvement is attributed to generally better quality water and dilution of nonconservative pollutants by upstream reservoir releases during low flows.

\r\n

The Raritan River between Manville and Perth Amboy flows through a large urban and industrial complex. Much of this reach is tidal. Detrimental activities of man are reflected in higher concentrations of most constituents below Manville than those observed upstream. For example, between Manville and the head of tide near South Bound Brook, the maximum concentration of dissolved solids observed during the study period increased from 464 to 1,520 mg/L; orthophosphates from 0.93 to 2.3 mg/L; phenolic materials from 22 to 312 μg/L; and coliform bacteria from 13,300 to 100,000 colonies per 100 milliliters. A general deterioration in water quality with time in the river below Manville is demonstrated through comparisons of dissolved-oxygen and biochemical-oxygen demand data collected between the late 1920's and early 1970's.

\r\n

Several time-of-travel measurements within the basin are reported. These data provide reasonable estimates of the time required for soluble contaminants to pass through particular parts of the river system. For example, the peak concentration of a contaminant injected into the river system at Clinton at a flow of 100 cubic feet per second (2.83 cubic meters per second) would be expected to travel to the head of tide near South Bound Brook, about 34 miles (55 kilometers), in about 70 hours; but at a flow of 50 cubic feet per second (1.42 cubic meters per second) the traveltime would increase to about 125 hours.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Trenton, NJ","doi":"10.3133/wri7414","collaboration":"Prepared in cooperation with the State of New Jersey, Department of Environmental Protection. Originally produced by the USGS New Jersey Water Resources Division.","usgsCitation":"Anderson, P.W., and Faust, S.D., 1974, Water quality and streamflow characteristics, Raritan River Basin, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 14-74, vi, 82 p., https://doi.org/10.3133/wri7414.","productDescription":"vi, 82 p.","numberOfPages":"90","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true}],"links":[{"id":158039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_14_74.gif"},{"id":261813,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wri/1974/0014/","linkFileType":{"id":5,"text":"html"}},{"id":261814,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0014/pdf/wrir14-74.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey","otherGeospatial":"Raritan River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.11666666666666,40.166666666666664 ], [ -75.11666666666666,40.96666666666667 ], [ -74.16666666666667,40.96666666666667 ], [ -74.16666666666667,40.166666666666664 ], [ -75.11666666666666,40.166666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9b4b","contributors":{"authors":[{"text":"Anderson, Peter W.","contributorId":10400,"corporation":false,"usgs":true,"family":"Anderson","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":195492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faust, Samuel Denton","contributorId":70367,"corporation":false,"usgs":true,"family":"Faust","given":"Samuel","email":"","middleInitial":"Denton","affiliations":[],"preferred":false,"id":195493,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66217,"text":"i822 - 1974 - Geologic map of the Purbach Quadrangle of the Moon","interactions":[],"lastModifiedDate":"2023-03-15T11:08:38.682344","indexId":"i822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"822","subseriesTitle":"MOON","title":"Geologic map of the Purbach Quadrangle of the Moon","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i822","usgsCitation":"Holt, H.E., 1974, Geologic map of the Purbach Quadrangle of the Moon: U.S. Geological Survey IMAP 822, 1 Plate: 72.00 × 37.33 inches, https://doi.org/10.3133/i822.","productDescription":"1 Plate: 72.00 × 37.33 inches","costCenters":[],"links":[{"id":439013,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9BFJRQ0","text":"USGS data release","linkHelpText":"Geologic map of the Purbach Quadrangle of the Moon"},{"id":439012,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9ZTWSXJ","text":"USGS data release","linkHelpText":"Interactive Map: USGS IMAP 822 Geologic Map of the Purbach Quadrangle of the Moon"},{"id":101329,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0822/plate-1.pdf","size":"9370","linkFileType":{"id":1,"text":"pdf"}},{"id":189502,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414194,"rank":3,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://doi.org/10.5066/P9ZTWSXJ","text":"Interactive map","linkHelpText":"- Geologic map of the Purbach Quadrangle of the Moon, 1:1M. Holt (1974)"}],"scale":"1000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db6914a3","contributors":{"authors":[{"text":"Holt, H. 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The water-resources investigations program of the Geological Survey has the objective of seeing that the Nation's water resources are appraised and that the necessary water data to develop and manage them efficiently are available when needed. In carrying out this objective, the Survey is the primary source of hydrologic data that are basic not only to the quantification of the water resource but also to its development and conservation. In recent years, the need has developed for the Survey to provide data and technology to predict the impact of man's activities upon the water resource and the water environment.

To accomplish its mission, the Geological Survey determines the source, quantity, quality, distribution, movement, and availability of both surface and ground water. This work includes the assessment of the chemical, physical, and biological quality of water resources and its relation to various parts of the hydrologic cycle; research to improve the scientific basis of investigations and techniques; design and operation of a national water-data network; and publication of its investigations.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f39","contributors":{"authors":[{"text":"Manigold, Douglas B.","contributorId":60265,"corporation":false,"usgs":true,"family":"Manigold","given":"Douglas","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":190729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3459,"text":"cir692 - 1974 - Selenium, fluorine, and arsenic in surficial materials of the conterminous United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"cir692","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"692","title":"Selenium, fluorine, and arsenic in surficial materials of the conterminous United States","docAbstract":"Concentrations of selenium, fluorine, and arsenic in 912, 911, and 910 samples, respectively, of soils and other regoliths from sites approximately 50 miles (80 km) apart throughout the United States are represented on maps by symbols showing five ranges of values. Histograms of the concentrations of these elements are also given. The geometric-mean concentrations (ppm) in the samples, grouped by area, are as follows: \r\n\r\nSelenium-- Entire United States, 0.31; Western United States, 0.25; and Eastern United States, 0.39. \r\n\r\nFluorine-- Entire United States, 180; Western United States, 250; and Eastern United States, 115. \r\n\r\nArsenic-- Entire United States, 5.8; Western United States, 6.1; and Eastern United States, 5.4.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey],","doi":"10.3133/cir692","usgsCitation":"Shacklette, H.T., Boerngen, J.G., and Keith, J.R., 1974, Selenium, fluorine, and arsenic in surficial materials of the conterminous United States: U.S. Geological Survey Circular 692, iii, 14 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir692.","productDescription":"iii, 14 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":120811,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1974/0692/report-thumb.jpg"},{"id":30471,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1974/0692/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7b2b","contributors":{"authors":[{"text":"Shacklette, Hansford T.","contributorId":43339,"corporation":false,"usgs":true,"family":"Shacklette","given":"Hansford","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":146967,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boerngen, Josephine G.","contributorId":31750,"corporation":false,"usgs":true,"family":"Boerngen","given":"Josephine","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":146966,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keith, John R. 0000-0002-4665-227X jkeith@usgs.gov","orcid":"https://orcid.org/0000-0002-4665-227X","contributorId":4252,"corporation":false,"usgs":true,"family":"Keith","given":"John","email":"jkeith@usgs.gov","middleInitial":"R.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":146965,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":13560,"text":"ofr74369 - 1974 - Bootstrap Window, Elko and Eureka Counties, Nevada; geological summary and analyses of rock samples","interactions":[],"lastModifiedDate":"2012-02-02T00:06:56","indexId":"ofr74369","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-369","title":"Bootstrap Window, Elko and Eureka Counties, Nevada; geological summary and analyses of rock samples","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr74369","usgsCitation":"Evans, J.G., 1974, Bootstrap Window, Elko and Eureka Counties, Nevada; geological summary and analyses of rock samples: U.S. Geological Survey Open-File Report 74-369, i, 10 leaves :ill. ;27 cm.; (19 p. - PGS), https://doi.org/10.3133/ofr74369.","productDescription":"i, 10 leaves :ill. ;27 cm.; (19 p. - PGS)","costCenters":[],"links":[{"id":146814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0369/report-thumb.jpg"},{"id":42037,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0369/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602aac","contributors":{"authors":[{"text":"Evans, James George","contributorId":73578,"corporation":false,"usgs":true,"family":"Evans","given":"James","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":168025,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13444,"text":"ofr7456 - 1974 - Stratigraphy and nahcolite resources of the saline facies of the Green River Formation, Rio Blanco County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:45","indexId":"ofr7456","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-56","title":"Stratigraphy and nahcolite resources of the saline facies of the Green River Formation, Rio Blanco County, Colorado","docAbstract":"Based on a study of 10 drill cores, a sequence of oil shale and associated nahcolite, nearly 2,000 feet thick, in the lacustrine Green River Formation (Eocene) in the Piceance Creek basin, Rio Blanco County, Colo., was divided in ascending order into zones 1 to 13, B-groove, Mahogany zone (with lower, middle, and upper parts), and A-groove at the top. The odd-numbered zones and the Mahogany zone are mappable subsurface units of relatively thick oil shale and are distinguished from the even-numbered zones and A- and B-grooves which are thinner units of oil shale of lower grade. \r\n\r\nLarge amounts of nahcolite found in zones 5 to 12 occur in (1) coarse-grained crystalline aggregates scattered through oil shale, (2) laterally continuous units of fine-grained crystals disseminated in oil shale, (3) brown microcrystalline beds, and (4) white coarse-grained beds that grade laterally into halitic rocks toward basin center. The original .upper limit of the nahcolite and halitic rocks is not yet completely known, but the present top is marked by a dissolution surface. Above this surface the rocks, extending from zones 11 or 12 upward into the Mahogany zone, form a water-saturated 'leached zone,' a geohydrologic unit in which large amounts of water-soluble minerals probably mostly nahcolite, and halite, were removed by ground-water dissolution. Rocks in the leached zone, mostly oil shale, are commonly broken and fractured and contain crystal cavities and solution breccias. Several solution breccias can be traced laterally into unleached beds of nahcolite and halite. Although evidence of salines is found in rocks above A-groove, the original saline facies that includes most of the bedded deposits extends from zone 5 upward into A-groove. \r\n\r\nPotentially ruinable beds of white nahcolite as much as 12 feet thick are found at depths of 1,560 or more feet below the surface. Some thicker beds of high-grade nahcolite are believed to be too close to the dissolution surface for safe room-and-pillar mining. Probably the most economical method of mining nahcolite would be as a coproduct of a shale-oil industry. Removal of nahcolite prior to retorting increases significantly the grade of oil shale by as much as 1.6 times, Several zones are more than 300 feet thick and average 30 or more weight percent nahcolite. Resources of nahcolite per square mile range as high as 489 million short tons. The total nahcolite resource in the basin is conservatively estimated at 32 billion short tons, which makes it the secondlargest deposit of sodium carbonate known .in the world.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr7456","usgsCitation":"Dyni, J.R., 1974, Stratigraphy and nahcolite resources of the saline facies of the Green River Formation, Rio Blanco County, Colorado: U.S. Geological Survey Open-File Report 74-56, ii, 28 leaves, 2 sheets, :ill ;29 cm., https://doi.org/10.3133/ofr7456.","productDescription":"ii, 28 leaves, 2 sheets, :ill ;29 cm.","costCenters":[],"links":[{"id":146399,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0056/report-thumb.jpg"},{"id":41886,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0056/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9179","contributors":{"authors":[{"text":"Dyni, John R. jdyni@usgs.gov","contributorId":756,"corporation":false,"usgs":true,"family":"Dyni","given":"John","email":"jdyni@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":167815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13427,"text":"ofr757 - 1974 - Chalcopyrite in rocks associated with magnetic iron-formation in Wisconsin","interactions":[],"lastModifiedDate":"2012-02-02T00:06:45","indexId":"ofr757","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"75-7","title":"Chalcopyrite in rocks associated with magnetic iron-formation in Wisconsin","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr757","usgsCitation":"Dutton, C.E., 1974, Chalcopyrite in rocks associated with magnetic iron-formation in Wisconsin: U.S. Geological Survey Open-File Report 75-7, [i, 9] leaves :map ;28 cm., https://doi.org/10.3133/ofr757.","productDescription":"[i, 9] leaves :map ;28 cm.","costCenters":[],"links":[{"id":146485,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6df0","contributors":{"authors":[{"text":"Dutton, Carl E.","contributorId":27418,"corporation":false,"usgs":true,"family":"Dutton","given":"Carl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":167794,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13409,"text":"ofr74188 - 1974 - Effect of irrigation pumping on desert pupfish habitats in Ash Meadows, Nye County, Nevada","interactions":[{"subject":{"id":13409,"text":"ofr74188 - 1974 - Effect of irrigation pumping on desert pupfish habitats in Ash Meadows, Nye County, Nevada","indexId":"ofr74188","publicationYear":"1974","noYear":false,"title":"Effect of irrigation pumping on desert pupfish habitats in Ash Meadows, Nye County, Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":5910,"text":"pp927 - 1976 - Effect of irrigation pumping on desert pupfish habitats in the Ash Meadows, Nye County, Nevada","indexId":"pp927","publicationYear":"1976","noYear":false,"title":"Effect of irrigation pumping on desert pupfish habitats in the Ash Meadows, Nye County, Nevada"},"id":1}],"supersededBy":{"id":5910,"text":"pp927 - 1976 - Effect of irrigation pumping on desert pupfish habitats in the Ash Meadows, Nye County, Nevada","indexId":"pp927","publicationYear":"1976","noYear":false,"title":"Effect of irrigation pumping on desert pupfish habitats in the Ash Meadows, Nye County, Nevada"},"lastModifiedDate":"2017-06-18T21:53:23","indexId":"ofr74188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-188","title":"Effect of irrigation pumping on desert pupfish habitats in Ash Meadows, Nye County, Nevada","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74188","usgsCitation":"Dudley, W., and Larson, J.D., 1974, Effect of irrigation pumping on desert pupfish habitats in Ash Meadows, Nye County, Nevada: U.S. Geological Survey Open-File Report 74-188, xi, 142 p. :ill. (some folded), maps ;27 cm., https://doi.org/10.3133/ofr74188.","productDescription":"xi, 142 p. :ill. (some folded), maps ;27 cm.","costCenters":[],"links":[{"id":145939,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62560f","contributors":{"authors":[{"text":"Dudley, William W.","contributorId":6064,"corporation":false,"usgs":true,"family":"Dudley","given":"William W.","affiliations":[],"preferred":false,"id":167760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larson, J. D.","contributorId":83084,"corporation":false,"usgs":true,"family":"Larson","given":"J.","middleInitial":"D.","affiliations":[],"preferred":false,"id":167761,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13637,"text":"ofr74348 - 1974 - Atlantic OCS resource and leasing potential","interactions":[],"lastModifiedDate":"2024-02-23T19:40:15.304656","indexId":"ofr74348","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-348","title":"Atlantic OCS resource and leasing potential","docAbstract":"

Thick marine sedimentary sections and geologic structures favorable for the accumulation of petroleum are indicated in Georges Bank basin, the Baltimore Canyon trough, and the Southeast Georgia embayment. Undiscovered recoverable resources of petroleum on the Atlantic OCS are estimated to be 10 billion to 20 billion barrels of oil and 55 trillion to 110 trillion cubic feet of gas. Such estimates carry a high degree of uncertainty. Preliminary results suggest that the most favorable areas for leasing are under the deeper waters of the shelf.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74348","usgsCitation":"Foote, R.Q., Mattick, R.E., and Behrendt, J.C., 1974, Atlantic OCS resource and leasing potential: U.S. Geological Survey Open-File Report 74-348, 33 p., https://doi.org/10.3133/ofr74348.","productDescription":"33 p.","costCenters":[],"links":[{"id":425965,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0348/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146771,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0348/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Atlantic OCS, Baltimore Canyon trough, Georges Bank basin, Southeast Georgia embayment","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -67.39486458992656,\n 44.39864915712985\n ],\n [\n -81.54908500998866,\n 44.39864915712985\n ],\n [\n -81.54908500998866,\n 26.50609859114779\n ],\n [\n -67.39486458992656,\n 26.50609859114779\n ],\n [\n -67.39486458992656,\n 44.39864915712985\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaee4b07f02db66c578","contributors":{"authors":[{"text":"Foote, Richard Q.","contributorId":19171,"corporation":false,"usgs":true,"family":"Foote","given":"Richard","email":"","middleInitial":"Q.","affiliations":[],"preferred":false,"id":168147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mattick, Robert E.","contributorId":44130,"corporation":false,"usgs":true,"family":"Mattick","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":168148,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Behrendt, John Charles jbehrendt@usgs.gov","contributorId":74747,"corporation":false,"usgs":true,"family":"Behrendt","given":"John","email":"jbehrendt@usgs.gov","middleInitial":"Charles","affiliations":[],"preferred":false,"id":168149,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":46955,"text":"ofr741086 - 1974 - Geologic and structure contour maps of the Ute Creek 1 SE quadrangle, Colfax County, New Mexico","interactions":[],"lastModifiedDate":"2022-05-06T19:29:04.700553","indexId":"ofr741086","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-1086","title":"Geologic and structure contour maps of the Ute Creek 1 SE quadrangle, Colfax County, New Mexico","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741086","usgsCitation":"Pillmore, C., 1974, Geologic and structure contour maps of the Ute Creek 1 SE quadrangle, Colfax County, New Mexico: U.S. Geological Survey Open-File Report 74-1086, 2 Plates: 28.38 × 29.31 inches and 21.62 × 27.61 inches, https://doi.org/10.3133/ofr741086.","productDescription":"2 Plates: 28.38 × 29.31 inches and 21.62 × 27.61 inches","costCenters":[],"links":[{"id":171035,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":108584,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14993.htm","linkFileType":{"id":5,"text":"html"},"description":"14993"},{"id":83872,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/1086/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83871,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/1086/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New Mexico","county":"Colfax County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -105.125,\n 36.75\n ],\n [\n -105,\n 36.75\n ],\n [\n -105,\n 36.875\n ],\n [\n -105.125,\n 36.875\n ],\n [\n -105.125,\n 36.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a807e","contributors":{"authors":[{"text":"Pillmore, Charles L.","contributorId":27123,"corporation":false,"usgs":true,"family":"Pillmore","given":"Charles L.","affiliations":[],"preferred":false,"id":234391,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13520,"text":"ofr72109_Englund - 1974 - Availability of low-sulphur coal in McDowell County, West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:44","indexId":"ofr72109_Englund","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"72-109","title":"Availability of low-sulphur coal in McDowell County, West Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr72109_Englund","usgsCitation":"Englund, K.J., 1974, Availability of low-sulphur coal in McDowell County, West Virginia: U.S. Geological Survey Open-File Report 72-109, iii, 19 leaves :ill., folded map ;29 cm., https://doi.org/10.3133/ofr72109_Englund.","productDescription":"iii, 19 leaves :ill., folded map ;29 cm.","costCenters":[],"links":[{"id":145305,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d83c","contributors":{"authors":[{"text":"Englund, Kenneth John","contributorId":59023,"corporation":false,"usgs":true,"family":"Englund","given":"Kenneth","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":167938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13642,"text":"ofr74307 - 1974 - Geology of the Zwedru Quadrangle, Liberia","interactions":[{"subject":{"id":13642,"text":"ofr74307 - 1974 - Geology of the Zwedru Quadrangle, Liberia","indexId":"ofr74307","publicationYear":"1974","noYear":false,"title":"Geology of the Zwedru Quadrangle, Liberia"},"predicate":"SUPERSEDED_BY","object":{"id":65208,"text":"i777D - 1977 - Geologic map of the Zwedru Quadrangle, Liberia","indexId":"i777D","publicationYear":"1977","noYear":false,"chapter":"D","title":"Geologic map of the Zwedru Quadrangle, Liberia"},"id":1}],"supersededBy":{"id":65208,"text":"i777D - 1977 - Geologic map of the Zwedru Quadrangle, Liberia","indexId":"i777D","publicationYear":"1977","noYear":false,"title":"Geologic map of the Zwedru Quadrangle, Liberia"},"lastModifiedDate":"2023-08-28T16:38:31.59172","indexId":"ofr74307","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-307","title":"Geology of the Zwedru Quadrangle, Liberia","docAbstract":"

As part of a program undertaken cooperatively by the Liberian Geological Survey (LGS) and the U. S. Geological Survey (USGS), under the sponsorship of the Government of Liberia and the Agency for International Development, U. S. Department of State, Liberia was mapped by geologic and geophysical methods during the period 1965 to 1972. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74307","usgsCitation":"Force, E.R., and Beikman, H.M., 1974, Geology of the Zwedru Quadrangle, Liberia: U.S. Geological Survey Open-File Report 74-307, Report: 12 p.; 1 Plate: 35.08 x 24.38 inches, https://doi.org/10.3133/ofr74307.","productDescription":"Report: 12 p.; 1 Plate: 35.08 x 24.38 inches","costCenters":[],"links":[{"id":420190,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0307/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":420189,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0307/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147274,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0307/report-thumb.jpg"}],"scale":"250000","country":"Liberia","otherGeospatial":"Zwedru Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 7.75,6 ], [ 7.75,7 ], [ 9,7 ], [ 9,6 ], [ 7.75,6 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c90b","contributors":{"authors":[{"text":"Force, Eric R.","contributorId":32916,"corporation":false,"usgs":true,"family":"Force","given":"Eric","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":168160,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beikman, Helen Marie","contributorId":65075,"corporation":false,"usgs":true,"family":"Beikman","given":"Helen","email":"","middleInitial":"Marie","affiliations":[],"preferred":false,"id":168161,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13550,"text":"ofr74224 - 1974 - A stochastic model for predicting the probability distribution of the dissolved oxygen deficit in streams","interactions":[{"subject":{"id":13550,"text":"ofr74224 - 1974 - A stochastic model for predicting the probability distribution of the dissolved oxygen deficit in streams","indexId":"ofr74224","publicationYear":"1974","noYear":false,"title":"A stochastic model for predicting the probability distribution of the dissolved oxygen deficit in streams"},"predicate":"SUPERSEDED_BY","object":{"id":5893,"text":"pp913 - 1976 - A stochastic model for predicting the probability distribution of the dissolved-oxygen deficit in streams","indexId":"pp913","publicationYear":"1976","noYear":false,"title":"A stochastic model for predicting the probability distribution of the dissolved-oxygen deficit in streams"},"id":1}],"supersededBy":{"id":5893,"text":"pp913 - 1976 - A stochastic model for predicting the probability distribution of the dissolved-oxygen deficit in streams","indexId":"pp913","publicationYear":"1976","noYear":false,"title":"A stochastic model for predicting the probability distribution of the dissolved-oxygen deficit in streams"},"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr74224","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-224","title":"A stochastic model for predicting the probability distribution of the dissolved oxygen deficit in streams","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr74224","usgsCitation":"Esen, I., and Rathbun, R.E., 1974, A stochastic model for predicting the probability distribution of the dissolved oxygen deficit in streams: U.S. Geological Survey Open-File Report 74-224, 177 leaves ; 28 cm., https://doi.org/10.3133/ofr74224.","productDescription":"177 leaves ; 28 cm.","costCenters":[],"links":[{"id":146234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a62d0","contributors":{"authors":[{"text":"Esen, I.I.","contributorId":10790,"corporation":false,"usgs":true,"family":"Esen","given":"I.I.","email":"","affiliations":[],"preferred":false,"id":167991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":167992,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13788,"text":"ofr74222 - 1974 - Effects of local geology on ground motion in the San Francisco Bay region, California: A continued study","interactions":[],"lastModifiedDate":"2024-12-02T20:32:01.027343","indexId":"ofr74222","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-222","title":"Effects of local geology on ground motion in the San Francisco Bay region, California: A continued study","docAbstract":"

Measurements of ground motion generated by nuclear explosions in Nevada have been completed for 99 locations in the San Francisco Bay region, California. The seismograms, Fourier amplitude spectra, spectral amplification curves for the signal, and the Fourier amplitude spectra of the seismic noise are presented for 60 locations. Analog amplifications, based on the maximum signal amplitude, are computed for an additional 39 locations. The recordings of the nuclear explosions show marked amplitude variations which are consistently related to the local geologic conditions of the recording site. The average spectral amplifications observed for vertical and horizontal ground motions are, respectively: (1, 1) for granite, (1.5, 1.6) for the Franciscan Formation, (2.3, 2.3), for other pre-Tertiary and Tertiary rocks, (3.0, 2.7) for the Santa Clara Formation, (3.3, 4.4) for older bay sediments, and (3.7, 11.3) for younger bay mud. Spectral amplification curves define predominant ground frequencies for younger bay mud sites and for some older bay sediment sites. The predominant frequencies for most sites were not clearly defined by the amplitude spectra computed from the seismic background noise.

The intensities ascribed to various sites in the San Francisco Bay region for the California earthquake of April 18, 1906, are strongly dependent on distance from the zone of surface faulting and the geological character of the ground. Considering only those sites (approximately one square city block in size) for which there is good evidence for the degree of ascribed intensity, the intensities for 917 sites on Franciscan rocks generally decrease with the logarithm of distance as

Intensity = 2.69 - 1.90 log (Distance Km).

For sites on other geologic units, intensity increments, derived from this empirical rela.tion, correlate strongly with the Average Horizontal Spectral Amplifications (MISA) according to the empirical relation

Intensity Increment= 0.27 + 2.70 log(AHSA).

Average intensity increments predicted for various geologic units are -0.3 for granite, 0.2 for Franciscan Formation, 0.6 for other pre-Tertiary, Tertiary bedrock, 0.8 for Santa Clara Formation, 1 .3 for older bay sediments, 2.4 for younger bay mud. These empirical relations, together with detailed geologic maps, delineate areas in the San Francisco Bay region of potentially high intensity from future earthquakes on either the San Andreas fault or the Hayward fault.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr74222","usgsCitation":"Gibbs, J., and Borcherdt, R.D., 1974, Effects of local geology on ground motion in the San Francisco Bay region, California: A continued study: U.S. Geological Survey Open-File Report 74-222, Report: 132 p.; 3 Figures: 121.50 × 113.44 inches or smaller, https://doi.org/10.3133/ofr74222.","productDescription":"Report: 132 p.; 3 Figures: 121.50 × 113.44 inches or smaller","numberOfPages":"146","onlineOnly":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":116806,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_74_222.jpg"},{"id":410085,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15033.htm","linkFileType":{"id":5,"text":"html"}},{"id":111131,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1974/0222/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay Region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.617,\n 37.421\n ],\n [\n -122.617,\n 37.875\n ],\n [\n -121.75,\n 37.875\n ],\n [\n -121.75,\n 37.421\n ],\n [\n -122.617,\n 37.421\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611c82","contributors":{"authors":[{"text":"Gibbs, James F.","contributorId":95880,"corporation":false,"usgs":true,"family":"Gibbs","given":"James F.","affiliations":[],"preferred":false,"id":168389,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Borcherdt, Roger D. 0000-0002-8668-0849 borcherdt@usgs.gov","orcid":"https://orcid.org/0000-0002-8668-0849","contributorId":2373,"corporation":false,"usgs":true,"family":"Borcherdt","given":"Roger","email":"borcherdt@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":168388,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":38678,"text":"pp758B - 1974 - Geology and mineral deposits of the Upper Chulitna district, Alaska","interactions":[],"lastModifiedDate":"2022-03-31T18:39:59.139606","indexId":"pp758B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"758","chapter":"B","title":"Geology and mineral deposits of the Upper Chulitna district, Alaska","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp758B","usgsCitation":"Hawley, C.C., and Clark, A.L., 1974, Geology and mineral deposits of the Upper Chulitna district, Alaska: U.S. Geological Survey Professional Paper 758, Report: iv, 47 p.; 2 Plates: 30.00 × 33.00 inches and 41.00 × 28.00 inches, https://doi.org/10.3133/pp758B.","productDescription":"Report: iv, 47 p.; 2 Plates: 30.00 × 33.00 inches and 41.00 × 28.00 inches","costCenters":[],"links":[{"id":65518,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0758b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65517,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0758b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65519,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0758b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397945,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5035.htm"},{"id":120105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0758b/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"Alaska","otherGeospatial":"Upper Chulitna district","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -149.4042,\n 63.0056\n ],\n [\n -150.0431,\n 63.0056\n ],\n [\n -150.0431,\n 63.3319\n ],\n [\n -149.4042,\n 63.3319\n ],\n [\n -149.4042,\n 63.0056\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db68517f","contributors":{"authors":[{"text":"Hawley, C. C.","contributorId":102070,"corporation":false,"usgs":true,"family":"Hawley","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":220271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, A. L.","contributorId":89502,"corporation":false,"usgs":true,"family":"Clark","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":220270,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13640,"text":"ofr74306 - 1974 - Geologic map of the Gbanka Quadrangle, Liberia","interactions":[{"subject":{"id":13640,"text":"ofr74306 - 1974 - Geologic map of the Gbanka Quadrangle, Liberia","indexId":"ofr74306","publicationYear":"1974","noYear":false,"title":"Geologic map of the Gbanka Quadrangle, Liberia"},"predicate":"SUPERSEDED_BY","object":{"id":65182,"text":"i776D - 1977 - Geologic map of the Gbanka Quadrangle, Liberia","indexId":"i776D","publicationYear":"1977","noYear":false,"chapter":"D","title":"Geologic map of the Gbanka Quadrangle, Liberia"},"id":1}],"supersededBy":{"id":65182,"text":"i776D - 1977 - Geologic map of the Gbanka Quadrangle, Liberia","indexId":"i776D","publicationYear":"1977","noYear":false,"title":"Geologic map of the Gbanka Quadrangle, Liberia"},"lastModifiedDate":"2018-01-24T16:48:16","indexId":"ofr74306","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-306","title":"Geologic map of the Gbanka Quadrangle, Liberia","docAbstract":"

As part of a program undertaken cooperatively by the Liberian Geological Survey (LGS) and the U. S. Geological Survey (USGS), under the sponsorship of the Government of Liberia and the Agency for International Development, U. S. Department of State, Liberia was mapped by geologic and geophysical methods during the period 1965 to 1972. The resulting geologic and geophysical maps are published in ten folios, each covering one quadrangle (see index map). 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74306","usgsCitation":"Force, E.R., and Dunbar, J., 1974, Geologic map of the Gbanka Quadrangle, Liberia: U.S. Geological Survey Open-File Report 74-306, Report: 14 p.; 1 Plate: 31.95 x 24.69 inches, https://doi.org/10.3133/ofr74306.","productDescription":"Report: 14 p.; 1 Plate: 31.95 x 24.69 inches","costCenters":[],"links":[{"id":147272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0306/report-thumb.jpg"},{"id":350588,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0306/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":350589,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0306/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"Liberia","otherGeospatial":"Gbanka Quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -9,\n 6\n ],\n [\n -8,\n 6\n ],\n [\n -8,\n 7\n ],\n [\n -9,\n 7\n ],\n [\n -9,\n 6\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698947","contributors":{"authors":[{"text":"Force, E. R.","contributorId":28235,"corporation":false,"usgs":true,"family":"Force","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":168156,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunbar, J.D.N.","contributorId":35398,"corporation":false,"usgs":true,"family":"Dunbar","given":"J.D.N.","email":"","affiliations":[],"preferred":false,"id":168157,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":38693,"text":"pp813C - 1974 - Summary appraisals of the nation's ground-water resources – Upper Colorado region","interactions":[],"lastModifiedDate":"2025-05-23T18:17:05.336995","indexId":"pp813C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"C","title":"Summary appraisals of the nation's ground-water resources – Upper Colorado region","docAbstract":"

The Upper Colorado Region covers about 113,500 square miles (293,965 km2) in parts of Arizona, Colorado, New Mexico, Utah, and Wyoming. Drainage from about 97 percent of the region is to the Colorado River. About 60 percent of the land is owned or administered by the Federal Government, and another 15 percent is in Indian trust. The predominantly arid to semiarid region is sparsely populated (averaging about three persons per square mile, or about two and one-half persons per km2) and is used chiefly for grazing, recreation, and mineral development.

\n

The water supply for the region comes from precipitation within the region, which averages about 95 million acre-feet (117,182.5 hm3) per year. Development of the region's water supply has been limited almost entirely to surface water. Only about 2 percent of the total estimated volume of water withdrawn (about 5.7 million acre-ft, or 7,030.9 hm3) and consumed (about 3.6 million acre-ft, or 4,440.6 hm3) in the region in 1970 came directly from ground-water sources.

\n

By the year 2020 consumptive use of water within the region and water exports to adjacent regions are expected to total more than 6.5 million acre-feet (8,017.8 hm3) per year. Use of the ground-water resources of the Upper Colorado Region in water-resources management can help to meet these water needs.

\n

A tremendous amount of water is stored in the rocks (ground-water reservoirs) of the Upper Colorado Region. Recoverable water in just the upper 100 feet (30.5 m) of saturated rocks is estimated to be as much as 115 million acre-feet (141,852.5 hm3). That amount is nearly four times the total active storage capacity of all surface-water reservoirs in the region. The average annual replenishable supply of the ground-water reservoir is about 4 million acre-feet (4,934 hm3). This amount of water could irrigate about 1.3 million acres (526,1,10 ha) of crops having an annual water requirement of 3 feet per acre (0.9 m/ha), or it could provide about 3,600 million gallons (13,627,440 m3) per day for industrial use.

\n

Most of the ground water is in consolidated rocks, which generally yield water to wells slowly. Much of the ground water is saline and, in some places, occurs at great depths. Nevertheless, the ground water is more uniformly distributed than is surface water, both areally and with time; therefore, it can be used advantageously in overall waterresources management. Recent advancements in the field of demineralization and in evaluation and development of ground water make this possible.

\n

Options available for use of ground water in water-resources management·in the·region include conjunctive use with surface water or development of ground water as an independent supply. The latter option could be for & perennial supply or for a time-limited supply (mining ground water), depending on the need and the existing ground-water conditions. All options can be carried out so as to meet the requirements of the Colorado River Compact. The options could be implemented to optimally develop the Upper Colorado River Basin's allocation of Colorado River water while meeting the Compact commitments to the Lower Basin.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813C","usgsCitation":"Price, D., and Arnow, T., 1974, Summary appraisals of the nation's ground-water resources – Upper Colorado region: U.S. Geological Survey Professional Paper 813, Report: vi, 40 p.; 2 Plates: 40.00 x 27.75 inches and 20.50 x 27.84 inches, https://doi.org/10.3133/pp813C.","productDescription":"Report: vi, 40 p.; 2 Plates: 40.00 x 27.75 inches and 20.50 x 27.84 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":65543,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813c/plate-2.pdf","text":"Plate 2","size":"7.75 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":65544,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813c/report.pdf","text":"Report","size":"8.68 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":65542,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813c/plate-1.pdf","text":"Plate 1","size":"13.83 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":392909,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5058.htm"},{"id":119914,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813c/report-thumb.jpg"}],"country":"United States","state":"Arizona, Colorado, New Mexico, Utah, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.74316406249999,\n 44.84029065139799\n ],\n [\n -106.14990234375,\n 43.197167282501276\n ],\n [\n -105.79833984375,\n 42.90816007196054\n ],\n [\n -104.9853515625,\n 42.76314586689494\n ],\n [\n -104.765625,\n 42.21224516288584\n ],\n [\n -104.47998046875,\n 41.65649719441145\n ],\n [\n -104.34814453125,\n 41.02964338716638\n ],\n [\n -103.68896484375,\n 40.6306300839918\n ],\n [\n -103.3154296875,\n 40.195659093364654\n ],\n [\n -103.60107421874999,\n 39.7240885773337\n ],\n [\n -103.95263671874999,\n 39.36827914916014\n ],\n [\n -104.12841796875,\n 38.87392853923629\n ],\n [\n -104.21630859375,\n 38.06539235133249\n ],\n [\n -104.21630859375,\n 37.70120736474139\n ],\n [\n -103.99658203125,\n 37.35269280367274\n ],\n [\n -103.95263671874999,\n 36.66841891894786\n ],\n [\n -104.17236328125,\n 35.585851593232356\n ],\n [\n -105.00732421875,\n 35.17380831799959\n ],\n [\n -105.88623046874999,\n 34.95799531086792\n ],\n [\n -106.94091796875,\n 34.79576153473033\n ],\n [\n -109.599609375,\n 34.79576153473033\n ],\n [\n -110.61035156249999,\n 34.75966612466248\n ],\n [\n -111.90673828125,\n 34.84987503195418\n ],\n [\n -113.0712890625,\n 35.567980458012094\n ],\n [\n -113.18115234375,\n 36.35052700542763\n ],\n [\n -113.5546875,\n 37.89219554724437\n ],\n [\n -112.03857421875,\n 40.44694705960048\n ],\n [\n -111.70898437499999,\n 41.343824581185686\n ],\n [\n -110.6982421875,\n 41.73852846935917\n ],\n [\n -110.23681640625,\n 42.66628070564928\n ],\n [\n -109.88525390624999,\n 43.97700467496408\n ],\n [\n -109.44580078125,\n 44.69989765840318\n ],\n [\n -108.720703125,\n 44.793530904744074\n ],\n [\n -107.64404296875,\n 44.809121700077355\n ],\n [\n -106.74316406249999,\n 44.84029065139799\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699642","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":220296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":220297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13572,"text":"ofr74195 - 1974 - First EROS/AID International Course on remote sensing","interactions":[],"lastModifiedDate":"2023-11-24T19:37:10.368522","indexId":"ofr74195","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-195","title":"First EROS/AID International Course on remote sensing","docAbstract":"

The First International Training Course on Remote Sensing held at the Earth Resources Observations Systems (EROS) Data Center in Sioux Falls, South Dakota, was sponsored by the Agency for International Development (AID), U.S. Department of State, from June 4 to 27, 1973. This course was conducted by the U.S. Geological Survey (USGS) under Participating Agency Services Agreement (PASA) TA (IC) 2-72, 931-11-995-902-72-3138905, as part of the AID program to provide training in remote sensing technology for earth scientists in the less developed countries.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74195","usgsCitation":"Fary, R., 1974, First EROS/AID International Course on remote sensing: U.S. Geological Survey Open-File Report 74-195, i, 40 p., https://doi.org/10.3133/ofr74195.","productDescription":"i, 40 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":147202,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0195/report-thumb.jpg"},{"id":422930,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0195/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Dakota","city":"Sioux Falls","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -96.8840064794897,\n 43.60178466198457\n ],\n [\n -96.8840064794897,\n 43.43491272557935\n ],\n [\n -96.57907298944068,\n 43.43491272557935\n ],\n [\n -96.57907298944068,\n 43.60178466198457\n ],\n [\n -96.8840064794897,\n 43.60178466198457\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f443a","contributors":{"authors":[{"text":"Fary, Raymond W.","contributorId":79112,"corporation":false,"usgs":true,"family":"Fary","given":"Raymond W.","affiliations":[],"preferred":false,"id":168043,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46347,"text":"ofr74153 - 1974 - Map showing mineral resources of Montgomery County, Maryland","interactions":[{"subject":{"id":46347,"text":"ofr74153 - 1974 - Map showing mineral resources of Montgomery County, Maryland","indexId":"ofr74153","publicationYear":"1974","noYear":false,"title":"Map showing mineral resources of Montgomery County, Maryland"},"predicate":"SUPERSEDED_BY","object":{"id":65238,"text":"i920E - 1975 - Map showing mineral resources of Montgomery County, Maryland","indexId":"i920E","publicationYear":"1975","noYear":false,"chapter":"E","title":"Map showing mineral resources of Montgomery County, Maryland"},"id":1}],"supersededBy":{"id":65238,"text":"i920E - 1975 - Map showing mineral resources of Montgomery County, Maryland","indexId":"i920E","publicationYear":"1975","noYear":false,"title":"Map showing mineral resources of Montgomery County, Maryland"},"lastModifiedDate":"2012-02-02T00:04:59","indexId":"ofr74153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-153","title":"Map showing mineral resources of Montgomery County, Maryland","language":"ENGLISH","doi":"10.3133/ofr74153","usgsCitation":"Froelich, A., 1974, Map showing mineral resources of Montgomery County, Maryland: U.S. Geological Survey Open-File Report 74-153, 1 map; scale = 1:62500, https://doi.org/10.3133/ofr74153.","productDescription":"1 map; scale = 1:62500","costCenters":[],"links":[{"id":135795,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649fb0","contributors":{"authors":[{"text":"Froelich, A.J.","contributorId":13593,"corporation":false,"usgs":true,"family":"Froelich","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":233137,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}