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,{"id":9817,"text":"ofr804 - 1979 - Machine-independent Fortran coding of the Lehmer random number generators","interactions":[],"lastModifiedDate":"2012-02-02T00:06:17","indexId":"ofr804","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"80-4","title":"Machine-independent Fortran coding of the Lehmer random number generators","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr804","usgsCitation":"Kirby, W., 1979, Machine-independent Fortran coding of the Lehmer random number generators: U.S. Geological Survey Open-File Report 80-4, [i], 13 p.  ;28 cm., https://doi.org/10.3133/ofr804.","productDescription":"[i], 13 p.  ;28 cm.","costCenters":[],"links":[{"id":142787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0004/report-thumb.jpg"},{"id":37602,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0004/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6490a5","contributors":{"authors":[{"text":"Kirby, W.H.","contributorId":65468,"corporation":false,"usgs":true,"family":"Kirby","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":160353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40079,"text":"ofr791120 - 1979 - Coal resource occurrence and coal development potential map of the Pine River quadrangle, Rio Arriba and San Juan Counties, New Mexico","interactions":[],"lastModifiedDate":"2022-10-17T19:39:52.412939","indexId":"ofr791120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1120","title":"Coal resource occurrence and coal development potential map of the Pine River quadrangle, Rio Arriba and San Juan Counties, New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791120","usgsCitation":"Dames & Moore, 1979, Coal resource occurrence and coal development 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,{"id":47639,"text":"wri7910 - 1979 - The effect of nitrification in the oxygen balance of the Upper Chattahoochee River, Georgia","interactions":[],"lastModifiedDate":"2019-07-26T16:03:02","indexId":"wri7910","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-10","title":"The effect of nitrification in the oxygen balance of the Upper Chattahoochee River, Georgia","docAbstract":"Oxygen consumption as a result of nitrification, and carbonaceous bacterial oxidation were compared in a 108 kilometer reach of the Chattahoochee River, Georgia. Nitrogenous and carbonaceous oxygen consumption were separated by using an inhibitor of nitrification 1-allyl-2-thiourea. The comparison was conducted in the laboratory using samples collected from the water column. Nitrification accounted for 38 to 52 percent of the total oxygen consumption. Nitrifying bacteria were enumerated from the same reach of the river. The population of Nitrosomonas ranged from 10 to 1,000 per milliliter in the water column and 100 to 100,000 per gram of benthic sediment. The nitrobacter population ranged from 10 to 100 per milliliter in the water column and 100 to 1,000 per gram in the benthic sediment. The concentration of ammonium, nitrite, and nitrate as N was determined from water samples collected throughout the study reach. The average rate of ammonium disappearance and of nitrate appearance was 0.02 milligram per liter per hour of flow time. 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,{"id":10716,"text":"ofr791604 - 1979 - Thrust fault zones in the Allegheny Plateau of north-central Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr791604","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1604","title":"Thrust fault zones in the Allegheny Plateau of north-central Pennsylvania","docAbstract":"Field investigations in the Williamsport Valley identify lineaments found on Landsat III images, have shown the presence of six discrete fault zones that strike subparallel to the trend of the Appalachian folds. These zones range from 0.5 to 1.75 km in width and from at least 10 km to more than 50 km in length. The individual thrust faults within each zone occur in 'staircase-type' folds and are at a low angle to bedding. Although each individual fault may have 0nly centimeters to displacement, many of these individual faults appear to exist within the six zones. We believe that the stress that produced that Valley and Ridge folds to the south was largely dissipated in faulting in the Williamsport Valley. This dissipation of the stress would explain the presence of only broad open folds to the north on the Allegheny Plateau. The extreme faulting in the Williamsport Valley along with the unique 'staircase' and 'reverse staircase' structures may result in fracture porosity traps at depth.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791604","usgsCitation":"Pohn, H.A., and Purdy, T.L., 1979, Thrust fault zones in the Allegheny Plateau of north-central Pennsylvania: U.S. Geological Survey Open-File Report 79-1604, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr791604.","productDescription":"16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1604/report-thumb.jpg"},{"id":38527,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1604/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b832","contributors":{"authors":[{"text":"Pohn, Howard A.","contributorId":66681,"corporation":false,"usgs":true,"family":"Pohn","given":"Howard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161847,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Purdy, Terri L.","contributorId":87950,"corporation":false,"usgs":true,"family":"Purdy","given":"Terri","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161848,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11795,"text":"ofr791695 - 1979 - Some reconnaissance-type electrical surveys of Timber Mountain Caldera, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:34","indexId":"ofr791695","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1695","title":"Some reconnaissance-type electrical surveys of Timber Mountain Caldera, Nye County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr791695","usgsCitation":"Zablocki, C.J., 1979, Some reconnaissance-type electrical surveys of Timber Mountain Caldera, Nye County, Nevada: U.S. Geological Survey Open-File Report 79-1695, 10, [12] leaves :ill., maps, graphs ;28 cm.; (23 p. - PGS), https://doi.org/10.3133/ofr791695.","productDescription":"10, [12] leaves :ill., maps, graphs ;28 cm.; (23 p. - PGS)","costCenters":[],"links":[{"id":144801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1695/report-thumb.jpg"},{"id":39685,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1695/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685b06","contributors":{"authors":[{"text":"Zablocki, Charles J.","contributorId":48961,"corporation":false,"usgs":true,"family":"Zablocki","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":163742,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10628,"text":"ofr79448 - 1979 - The subsurface geology of the Florida-Hatteras shelf, slope, and inner Blake Plateau","interactions":[],"lastModifiedDate":"2022-09-02T20:24:12.862875","indexId":"ofr79448","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-448","title":"The subsurface geology of the Florida-Hatteras shelf, slope, and inner Blake Plateau","docAbstract":"The structure and stratigraphy of the Florida-Hatteras Slope and inner Blake Plateau was studied by means of 4,780 km of single-channel air gun seismic reflection profiles. Control for the seismic stratigraphy is provided by correlating reflecting units and paleontologically dated stratigraphic units identified in offshore wells and dredge hauls. Many Tertiary unconformities exist, and major regional unconformities at the end of the Oligocene and in the late Paleocene are mapped. Reflecting surfaces believed to represent the tops of the Cretaceous, Paleocene, and Oligocene extend throughout the region. Upper Cretaceous (pre-Maastrichtian) rocks on the southeastern side of the Carolina Platform form a large seaward-facing progradational wedge. The Upper Cretaceous rocks in the Southeast Georgia Embayment, are seismically transparent and on the inner Blake Plateau are cut by numerous small faults, perhaps due to compaction. \r\n\r\nWithin the survey area relatively flat-lying Maastrichtian and Paleocene strata show no evidence that a feature similar to the present Florida-Hatteras Slope existed at the beginning of the Tertiary. Late Paleocene erosion, related to the initiation of the Gulf Stream flow, probably developed this regional unconformity. Eocene and Oligocene sediments landward of the present Gulf Stream form a thick sequence of seaward-dipping progradational beds. A seaward progradational wedge of Miocene to Holocene age covers a regionally traceable unconformity, which separates the Oligocene from the Miocene sediments. Under and seaward of the present Gulf Stream, the Eocene and younger sediment supply was much smaller and the buildup is comparatively insignificant. The difference in accumulation rates in the Eocene and younger sediments, landward and seaward of the Gulf Stream, is responsible for the Florida-Hatteras Slope. Tertiary isopach maps suggest that there is a well developed triangular depocenter under the shelf. The edges of the depocenter correspond with magnetic anomalies and it is suggested that the depocenter is related to differential subsidence during the Tertiary across older crustal structures. The Eocene and Oligocene units contain the aquifer onshore, and the aquifer probably remains in these units offshore. With this assumption the potential aquifer has been identified and traced under the shelf and slope.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79448","usgsCitation":"Paull, C.K., and Dillon, W.P., 1979, The subsurface geology of the Florida-Hatteras shelf, slope, and inner Blake Plateau: U.S. Geological Survey Open-File Report 79-448, 94 p., https://doi.org/10.3133/ofr79448.","productDescription":"94 p.","costCenters":[],"links":[{"id":406184,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_29112.htm","linkFileType":{"id":5,"text":"html"}},{"id":38458,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0448/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0448/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Florida-Hatteras shelf, slope, and inner Blake Plateau","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.6064453125,\n              28.459033019728043\n            ],\n            [\n              -75.05859375,\n              28.459033019728043\n            ],\n            [\n              -75.05859375,\n              34.08906131584994\n            ],\n            [\n              -81.6064453125,\n              34.08906131584994\n            ],\n            [\n              -81.6064453125,\n              28.459033019728043\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634ad0","contributors":{"authors":[{"text":"Paull, Charles K. 0000-0001-5940-3443","orcid":"https://orcid.org/0000-0001-5940-3443","contributorId":55825,"corporation":false,"usgs":false,"family":"Paull","given":"Charles","email":"","middleInitial":"K.","affiliations":[{"id":7043,"text":"University of North Carolina","active":true,"usgs":false}],"preferred":true,"id":161707,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dillon, William P. bdillon@usgs.gov","contributorId":79820,"corporation":false,"usgs":true,"family":"Dillon","given":"William","email":"bdillon@usgs.gov","middleInitial":"P.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":161706,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28915,"text":"wri79100 - 1979 - Monthly and annual water budgets of Lake Wingra, Madison, Wisconsin, 1972-77","interactions":[],"lastModifiedDate":"2024-01-11T17:41:15.771569","indexId":"wri79100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-100","title":"Monthly and annual water budgets of Lake Wingra, Madison, Wisconsin, 1972-77","docAbstract":"<p>This report presents estimated annual and monthly water budgets for Lake Wingra and the adjacent wetland area for January 1972 through September 1972. Annually, inputs from precipitation, surface runoff, and groundwater inflow are approximately equal (31, 34, and 35 percent, respectively). Outputs include outflow from the lake into Murphy Creek (70 percent), evapotranspiration from the lake and wetland (26 percent), and ground-water outflow (4 percent).</p>\n<p>The inputs and outputs vary seasonally. In months when snowmelt occurs, surface runoff is a major input (56 percent in March; 46 percent in April). In fall and winter ground-water inflow is a major input (57 percent in November). Precipitation comprises 41 percent of the input in August but only 18 percent in January. Lake outflow is the major output except from July through September. Combined evaporation and evapotranspiration is a major output in summer (45 to 58 percent) but minor in winter (less than 13 percent). Ground-water outflow is a small part of the budget each month, ranging from 2 percent in March and April to a maximum of 7 percent in September.</p>\n<p>The water budget is based on field data collected from January 1972 through June 1973, and on fragmentary data and estimates for July 1973 through September 1977. The budget terms differ from those published by Oakes, Hendrickson, and Zuehls (1975, table 10) because springflow has been included in total ground-water inflow and estimated on a monthly basis in this report. Previously only annual estimates were provided.</p>\n<p>&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri79100","collaboration":"Prepared in cooperation with the University of Wisconsin Institute for Environmental Studies","usgsCitation":"Novitzki, R., and Holmstrom, B.K., 1979, Monthly and annual water budgets of Lake Wingra, Madison, Wisconsin, 1972-77: U.S. Geological Survey Water-Resources Investigations Report 79-100, iv, 31 p., https://doi.org/10.3133/wri79100.","productDescription":"iv, 31 p.","numberOfPages":"37","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":57787,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0100/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124135,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0100/report-thumb.jpg"},{"id":424338,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35285.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wisconsin","county":"Dane County","city":"Madison","otherGeospatial":"Lake Wingra","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.47917938232422,\n              43.03426640603482\n            ],\n            [\n              -89.47917938232422,\n              43.09697190802465\n            ],\n            [\n              -89.29515838623045,\n              43.09697190802465\n            ],\n            [\n              -89.29515838623045,\n              43.03426640603482\n            ],\n            [\n              -89.47917938232422,\n              43.03426640603482\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db698fef","contributors":{"authors":[{"text":"Novitzki, R.P.","contributorId":73986,"corporation":false,"usgs":true,"family":"Novitzki","given":"R.P.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":200612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Holmstrom, B. K.","contributorId":90728,"corporation":false,"usgs":true,"family":"Holmstrom","given":"B.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":200613,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10295,"text":"ofr791642 - 1979 - K-Ar age of alunite alteration at Red Mountain, Lake City area, western San Juan Mountains, Colorado","interactions":[{"subject":{"id":10295,"text":"ofr791642 - 1979 - K-Ar age of alunite alteration at Red Mountain, Lake City area, western San Juan Mountains, Colorado","indexId":"ofr791642","publicationYear":"1979","noYear":false,"title":"K-Ar age of alunite alteration at Red Mountain, Lake City area, western San Juan Mountains, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70043067,"text":"70043067 - 1980 - K-Ar age of alunite alteration at Red Mountain, Lake City area, western San Juan Mountains, Colorado","indexId":"70043067","publicationYear":"1980","noYear":false,"title":"K-Ar age of alunite alteration at Red Mountain, Lake City area, western San Juan Mountains, Colorado"},"id":1}],"supersededBy":{"id":70043067,"text":"70043067 - 1980 - K-Ar age of alunite alteration at Red Mountain, Lake City area, western San Juan Mountains, Colorado","indexId":"70043067","publicationYear":"1980","noYear":false,"title":"K-Ar age of alunite alteration at Red Mountain, Lake City area, western San Juan Mountains, Colorado"},"lastModifiedDate":"2023-08-21T18:53:36.275695","indexId":"ofr791642","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1642","title":"K-Ar age of alunite alteration at Red Mountain, Lake City area, western San Juan Mountains, Colorado","docAbstract":"<p>The San Juan Mountains of southwestern Colorado are famous for rich vein deposits of base and precious metals and for patterns of conspicuous hydrothermal alteration. Areas of acid-sulfate alteration, characterized by extensive base leaching of volcanic rocks or hypabyssal plutons, are of current interest because of their local association with Au, Ag, and, in some cases, U mineralization (Lipman and others, 1976; Cunningham and others, 1978; Steven and others, 1979). Potential may also exist for recovery of aluminum from altered rocks rich in alunite (Hall, 1978). Alunite has been shown to be suitable for K-Ar dating in other mining districts (Mehnert and others, 1973b; Ashley and Silberman, 1976). We report here two concordant K-Ar ages determined on hydrothermal alunite from Red Mountain, in the Lake City area of the western San Juan Mountains.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791642","usgsCitation":"Mehnert, H.H., Slack, J.F., and Cebula, G.T., 1979, K-Ar age of alunite alteration at Red Mountain, Lake City area, western San Juan Mountains, Colorado: U.S. Geological Survey Open-File Report 79-1642, 8 p., https://doi.org/10.3133/ofr791642.","productDescription":"8 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":419984,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1642/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144084,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1642/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Lake City","otherGeospatial":"Red Mountain, San Juan Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.36220553780169,\n              38.037420680809646\n            ],\n            [\n              -107.36220553780169,\n              37.958594813260376\n            ],\n            [\n              -107.29532240114737,\n              37.958594813260376\n            ],\n            [\n              -107.29532240114737,\n              38.037420680809646\n            ],\n            [\n              -107.36220553780169,\n              38.037420680809646\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b489f","contributors":{"authors":[{"text":"Mehnert, Harald H.","contributorId":56221,"corporation":false,"usgs":true,"family":"Mehnert","given":"Harald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":161155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slack, John F. 0000-0001-6600-3130 jfslack@usgs.gov","orcid":"https://orcid.org/0000-0001-6600-3130","contributorId":1032,"corporation":false,"usgs":true,"family":"Slack","given":"John","email":"jfslack@usgs.gov","middleInitial":"F.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":true,"id":161153,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cebula, Gerald T.","contributorId":43775,"corporation":false,"usgs":true,"family":"Cebula","given":"Gerald","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":161154,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":47642,"text":"wri7925 - 1979 - Chemical analyses of surface water in Illinois, 1975-77--Volume III, Ohio River tributaries and Mississippi River tributaries south of Illinois River basin","interactions":[],"lastModifiedDate":"2020-10-29T13:22:44.350094","indexId":"wri7925","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-25","displayTitle":"Chemical Analyses of Surface Water in Illinois, 1975–77—Volume III, Ohio River Tributaries and Mississippi River Tributaries South of the Illinois River Basin","title":"Chemical analyses of surface water in Illinois, 1975-77--Volume III, Ohio River tributaries and Mississippi River tributaries south of Illinois River basin","docAbstract":"<p>Samples of surface water were collected and analyzed by the Illinois Environmental Protection Agency. The results from water years 1975 to 1977 are presented in three volumes. The history of sampling and analytical methods used during that period are summarized. Stream discharge data from records of the U.S. Geological Survey are included for all sites where samples were collected at gaging stations or near enough that reliable discharge estimates could be made. Volume III includes Ohio River tributaries and Mississippi River tributaries south of Illinois River basin.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7925","collaboration":"Prepared in cooperation with the Illinois Environmental Protection Agency","usgsCitation":"Grason, D., and Healy, R.W., 1979, Chemical analyses of surface water in Illinois, 1975-77--Volume III, Ohio River tributaries and Mississippi River tributaries south of Illinois River basin: U.S. Geological Survey Water-Resources Investigations Report 79-25, v. III, iv, 242 p., https://doi.org/10.3133/wri7925.","productDescription":"iv, 242 p.","costCenters":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"links":[{"id":361728,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://doi.org/10.3133/wri7923","text":"WRI 79–23","description":"WRI 79–23","linkHelpText":"Chemical Analyses of Surface Water in Illinois, 1975–77—Volume I, Des Plaines River Basin and Lake Michigan"},{"id":361721,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0025/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 79–25"},{"id":361729,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://doi.org/10.3133/wri7924","text":"WRI 79–24","description":"WRI 79–24","linkHelpText":"Chemical Analyses of Surface Water in Illinois, 1975–77—Volume II, Illinois River Basin and Mississippi River Tributaries North of Illinois River Basin"},{"id":169422,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0025/coverthb.jpg"}],"country":"United States","state":"Illinois","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.366031,42.500274],[-88.786681,42.491983],[-88.115285,42.496219],[-87.800561,42.49192],[-87.79823,42.473054],[-87.80537,42.384721],[-87.820858,42.361584],[-87.834769,42.301522],[-87.828569,42.269922],[-87.800066,42.208024],[-87.741662,42.128227],[-87.712206,42.096455],[-87.682359,42.075729],[-87.671462,42.058334],[-87.668982,42.029142],[-87.630953,41.933132],[-87.624052,41.904232],[-87.611659,41.892216],[-87.616537,41.882396],[-87.616251,41.868933],[-87.60945,41.845233],[-87.600549,41.826833],[-87.580948,41.804334],[-87.576347,41.786034],[-87.560646,41.766034],[-87.542845,41.752135],[-87.530745,41.748235],[-87.524141,41.72399],[-87.526376,40.491574],[-87.533227,39.883127],[-87.531646,39.347888],[-87.544013,39.352907],[-87.5544,39.340488],[-87.578331,39.340343],[-87.589084,39.333831],[-87.600397,39.312904],[-87.597545,39.296388],[-87.61005,39.282232],[-87.605543,39.261122],[-87.593486,39.247452],[-87.583535,39.243579],[-87.574558,39.218404],[-87.588614,39.197824],[-87.620796,39.17479],[-87.640435,39.166727],[-87.64599,39.1449],[-87.643145,39.128562],[-87.632245,39.118702],[-87.630376,39.104305],[-87.619134,39.100557],[-87.613513,39.085568],[-87.596373,39.079639],[-87.572588,39.057286],[-87.575027,39.034062],[-87.569696,39.019413],[-87.579117,39.001607],[-87.578319,38.988786],[-87.529496,38.971925],[-87.512187,38.954417],[-87.518826,38.923205],[-87.527645,38.907688],[-87.544089,38.895093],[-87.553384,38.863344],[-87.525893,38.848795],[-87.521681,38.826576],[-87.527342,38.818121],[-87.496537,38.778571],[-87.496494,38.742728],[-87.516707,38.716333],[-87.519609,38.697198],[-87.531231,38.684036],[-87.593678,38.667402],[-87.62012,38.639489],[-87.627348,38.60544],[-87.62389,38.593984],[-87.637752,38.588512],[-87.651529,38.568166],[-87.650704,38.55624],[-87.660732,38.541092],[-87.653802,38.517382],[-87.657084,38.507169],[-87.714047,38.47988],[-87.739522,38.475069],[-87.74317,38.459019],[-87.730134,38.446518],[-87.74104,38.435576],[-87.745254,38.408996],[-87.779996,38.370842],[-87.806075,38.363143],[-87.822721,38.346912],[-87.832723,38.324853],[-87.831972,38.307241],[-87.838243,38.29375],[-87.853046,38.289264],[-87.875476,38.301376],[-87.88041,38.299581],[-87.887849,38.285299],[-87.908223,38.274012],[-87.92168,38.289712],[-87.928858,38.292404],[-87.938727,38.289264],[-87.952125,38.273763],[-87.945904,38.256966],[-87.950838,38.247097],[-87.960225,38.237118],[-87.975511,38.232742],[-87.982688,38.221527],[-87.984234,38.20996],[-87.975819,38.197834],[-87.9595,38.184376],[-87.928858,38.168594],[-87.922577,38.160071],[-87.92168,38.148407],[-87.945472,38.126616],[-87.974272,38.121981],[-87.999734,38.100857],[-87.998389,38.090091],[-87.984931,38.069008],[-87.990314,38.056447],[-88.020369,38.046578],[-88.02979,38.025046],[-88.012574,37.977062],[-88.012929,37.966544],[-88.036124,37.942746],[-88.044145,37.926805],[-88.031584,37.901685],[-88.033378,37.894059],[-88.054462,37.877461],[-88.058499,37.865349],[-88.053116,37.847854],[-88.043247,37.836639],[-88.051771,37.813761],[-88.045939,37.807481],[-88.029382,37.803601],[-88.02803,37.799224],[-88.035827,37.791917],[-88.042602,37.76712],[-88.059588,37.742608],[-88.122412,37.709685],[-88.151646,37.675098],[-88.160187,37.657592],[-88.156827,37.632801],[-88.142225,37.603737],[-88.139973,37.586451],[-88.13341,37.574273],[-88.105585,37.55618],[-88.088049,37.535124],[-88.069018,37.525297],[-88.061342,37.505327],[-88.064234,37.484548],[-88.072386,37.483563],[-88.087664,37.471059],[-88.132628,37.471555],[-88.281667,37.452596],[-88.312585,37.440591],[-88.333183,37.42721],[-88.348405,37.410726],[-88.365471,37.401663],[-88.408808,37.425216],[-88.450127,37.411717],[-88.470224,37.396255],[-88.476592,37.386875],[-88.484462,37.345609],[-88.515939,37.284043],[-88.506942,37.266656],[-88.509328,37.26213],[-88.487277,37.244077],[-88.471753,37.220155],[-88.447764,37.203527],[-88.431488,37.160298],[-88.424403,37.152428],[-88.444605,37.098601],[-88.458948,37.073796],[-88.504437,37.065265],[-88.545403,37.070003],[-88.576718,37.085852],[-88.589207,37.099655],[-88.625889,37.119458],[-88.693983,37.141155],[-88.732105,37.143956],[-88.80572,37.188595],[-88.916934,37.224291],[-88.942111,37.228811],[-88.98326,37.228685],[-89.029981,37.211144],[-89.076221,37.175125],[-89.092934,37.156439],[-89.111189,37.119052],[-89.134931,37.103278],[-89.14132,37.093865],[-89.154504,37.088907],[-89.168087,37.074218],[-89.181369,37.046305],[-89.178975,37.020928],[-89.166447,37.003337],[-89.132685,36.9822],[-89.170008,36.970298],[-89.185491,36.973518],[-89.192097,36.979995],[-89.200793,37.016164],[-89.234053,37.037277],[-89.25493,37.072014],[-89.259936,37.064071],[-89.307726,37.069654],[-89.310819,37.057897],[-89.304752,37.047565],[-89.277715,37.03614],[-89.260003,37.023288],[-89.257608,37.015496],[-89.263527,37.00005],[-89.278628,36.98867],[-89.29213,36.992189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 \"}}]}","volume":"III","contact":"<p>Director,&nbsp;<a href=\"https://www.usgs.gov/centers/cm-water\" data-mce-href=\"https://www.usgs.gov/centers/cm-water\">Central Midwest Water Science Center</a><br>U.S. Geological Survey<br>405 North Goodwin<br>Urbana, IL 61801</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Acknowledgment</li><li>Definition of Terms</li><li>Methods</li><li>Presentation of Data</li><li>References</li><li>Index</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e49e7","contributors":{"authors":[{"text":"Grason, David","contributorId":29819,"corporation":false,"usgs":true,"family":"Grason","given":"David","email":"","affiliations":[],"preferred":false,"id":235943,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, R. W.","contributorId":89872,"corporation":false,"usgs":true,"family":"Healy","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":235944,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69350,"text":"l28 - 1979 - Land use and land cover, 1974, Pratt, Kansas","interactions":[],"lastModifiedDate":"2012-02-10T00:11:32","indexId":"l28","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":321,"text":"Land Use and Land Cover","code":"L","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"28","title":"Land use and land cover, 1974, Pratt, Kansas","language":"ENGLISH","doi":"10.3133/l28","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Land use and land cover, 1974, Pratt, Kansas: U.S. Geological Survey Land Use and Land Cover 28, -, https://doi.org/10.3133/l28.","productDescription":"-","costCenters":[],"links":[{"id":191021,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":261175,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/028/plate-1.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100,37 ], [ -100,38 ], [ -98,38 ], [ -98,37 ], [ -100,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae301","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":534559,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10292,"text":"ofr791478 - 1979 - The quality of surface water on Sanibel Island, Florida, 1976-77","interactions":[],"lastModifiedDate":"2023-11-21T22:39:48.500896","indexId":"ofr791478","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1478","title":"The quality of surface water on Sanibel Island, Florida, 1976-77","docAbstract":"<p>The quality of surface water in parts of the interior of Sanibel Island has been periodically degraded by high concentrations of salt or macronutrients and by low concentrations of dissolved oxygen. In 1976 the chloride concentration of surface water ranged from about 500 milligrams per liter to almost that of seawater, 19,000 milligrams per liter. The highest salinities were during the dry season of 1976 in the Sanibel River near the Tarpon Bay control structure and are attributed to leakage of saline water past the structure. The highest concentrations of macronutrients occurred during the dry season in the eastern reach of the Sanibel River, where concentrations generally exceeded 4.0 milligrams per liter total nitrogen and 0.9 milligrams per liter total phosphorus. Organic nitrogen accounted for about 95 percent of the total nitrogen, and ammonia accounted for most of the remainder. Concentrations of ammonia exceeded 0.1 milligrams per liter in 31 percent of the wet-season samples and 14 percent of the dry-season samples. Nighttime concentrations of ammonia exceeded those in daytime by several orders of magnitude; concentration of dissolved oxygen fluctuated inversely to that of ammonia. The concentration of dissolved oxygen and the magnitude of the day-night fluctuation decreased with depth. In 1976 the median concentration of dissolved oxygen near the surface was 7.5 milligrams per liter in the dry season and 3.5 milligrams per liter in the wet season. Concentrations were lowest in the wet season along an eastern reach of the Sanibel River and in several nearby ponds and canals where near-anaerobic conditions prevailed. The high concentrations of macronutrients and the low concentrations of dissolved oxygen at some surface-water sites are attributed, in part, to urban runoff and sewage effluent that flow directly into the surface water or seep through the shallow water-table aquifer into surface-water bodies.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791478","collaboration":"Prepared in cooperation with Lee County, City of Sanibel; Lee County, Florida and the Island Water Association","usgsCitation":"McPherson, B.F., and O’Donnell, T., 1979, The quality of surface water on Sanibel Island, Florida, 1976-77: U.S. Geological Survey Open-File Report 79-1478, vi, 50 p., https://doi.org/10.3133/ofr791478.","productDescription":"vi, 50 p.","costCenters":[],"links":[{"id":144081,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1478/report-thumb.jpg"},{"id":422799,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1478/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"Sanibel Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.08721351532877,\n              26.467371950617917\n            ],\n            [\n              -82.08721351532877,\n              26.420799203743798\n            ],\n            [\n              -82.00740949000107,\n              26.420799203743798\n            ],\n            [\n              -82.00740949000107,\n              26.467371950617917\n            ],\n            [\n              -82.08721351532877,\n              26.467371950617917\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641959","contributors":{"authors":[{"text":"McPherson, Benjamin F.","contributorId":17965,"corporation":false,"usgs":true,"family":"McPherson","given":"Benjamin","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":161147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Donnell, T.H.","contributorId":69970,"corporation":false,"usgs":true,"family":"O’Donnell","given":"T.H.","email":"","affiliations":[],"preferred":false,"id":161148,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26021,"text":"wri7992 - 1979 - Evaluation of methods for estimating ground-water withdrawals in western Kansas","interactions":[],"lastModifiedDate":"2018-11-19T12:17:44","indexId":"wri7992","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"79-92","title":"Evaluation of methods for estimating ground-water withdrawals in western Kansas","docAbstract":"<p>During 1978, methods of estimating ground-water withdrawals in western Kansas were examined and evaluated, using both existing data from the files of the U.S. Geological Survey and newly collected data.</p><p>Values for annual ground-water withdrawals reported to the Division of Water Resources, Kansas State Board of Agriculture, by water users probably contain substantial errors because most individual users do not possess the means to measure or accurately estimate the discharge rates of their wells. Such reported values are estimated to average 10 to 15 percent higher than the actual discharge rate. Values obtained from discharge-totaling meters are reasonably accurate, but few wells are equipped with these meters, and the cost of equipping all wells with meters may be prohibitive. Measured rates of power consumption can give good estimates of total withdrawal from wells where the power consumption is measured. However, power-consumption values cannot be extrapolated reliably from one well to another.</p><p>Three techniques are regarded as promising for estimating areal ground-water withdrawals from readily collected data:</p><ol><li>Examination of a small sample of withdrawal values from metered wells indicates that the statistical approach used by Luckey (1972) may be applied to western Kansas to estimate total withdrawal with acceptable accuracy in a large area from a statistical sample of measured values.<br></li><li>Measured values of irrigation application at a small number of selected wells might be used to compute total withdrawal for irrigation by crop type and precipitation zone. Evaluation of reported values of irrigation-water application for selected crops in zones of generally similar precipitation showed that, although the reported values are judged to be erroneously high, the reported values were consistent with each other and with average precipitation.<br></li><li>Power-consumption coefficients may be used to calculate an average coefficient for an area. The method described by Luckey (1972) was used to calculate the number of power-consumption coefficients that would have to be determined to estimate the mean power consumption of wells pumped by electric or natural-gas engines. The results indicate that as few as 100 values would produce results accurate to within 10 percent of the true average at the 95-percent confidence level. Thus, power coefficients for a particular type of irrigation system in any given area can be used even though values of power coefficients have little transfer value from well to well.<br></li></ol><p>Efforts by the Instrument Development Laboratofy of the U.S. Geological Survey to design improved instruments for measuring ground-water withdrawals have produced two promising results:</p><ol><li>An electronic running-time meter (Running-time Sentry) that was tested during 1978 in western Kansas and Florida appears to give accurate values of total pumping time. Large-scale testing of this prototype running-time meter is planned for 1979.<br></li><li>A low-cost discharge-totaling meter (REELTOT), based on the concept of sensing the velocity head in a pipe with differential-pressure transducers permanently installed in the pipe, is nearly complete. Early prototypes of this instrument may be tested in western Kansas during 1979.<br></li></ol><p>For the remainder of this study, the three techniques for estimating areal ground-water withdrawals described above will be tested on a larger scale in Groundwater Management District No. 1, an area of about 1,800 square miles in west-central Kansas. About 150 randomly selected wells will be equipped with Running-time Sentry units and monitored for total withdrawal, instantaneous discharge, and power consumption. A few wells will be equipped with prototype discharge-totaling meters. The performance of the Sentry units and discharge-totaling meters will be evaluated. Areal estimates of withdrawal from measured withdrawal values, from average power-consumption coefficients, and from irrigation application by crop will be calculated and compared with each other and with reported values of withdrawal.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7992","usgsCitation":"Baker, C.H., 1979, Evaluation of methods for estimating ground-water withdrawals in western Kansas: U.S. Geological Survey Water-Resources Investigations Report 79-92, iv, 70 p., https://doi.org/10.3133/wri7992.","productDescription":"iv, 70 p.","costCenters":[],"links":[{"id":359560,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0092/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0092/report-thumb.jpg"}],"country":"United 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,{"id":10238,"text":"ofr791245 - 1979 - Statistics and earth sciences; a challenge for the 80's; the geologists viewpoint","interactions":[],"lastModifiedDate":"2024-03-11T18:33:07.01155","indexId":"ofr791245","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"79-1245","title":"Statistics and earth sciences; a challenge for the 80's; the geologists viewpoint","docAbstract":"<p>It used to be that university students took up geology because they were attracted to the outdoors. This attraction developed perhaps because of a weekend field trip, or a summer field camp, or, for the lucky ones, a field season with an oil company. Whatever the reason, to be a geologist was to be among rocks. Traditionally, the role of the geologist has been to unravel the Earth's past. It has not been easy. Ask anyone who has taken a close look at a rock. Invariably, there is a multiplicity of explanations of how any rock came into existence. What is recorded in all probability is a multiplicity of past events, the evidence being only partly preserved; the rest has been obliterated. As a consequence, the rock record is largely incomplete. This is what has made the science of geology so interesting. It is also what has made it so difficult. Interpreting the past has more than its share of uncertainty.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791245","usgsCitation":"McCammon, R.B., 1979, Statistics and earth sciences; a challenge for the 80's; the geologists viewpoint: U.S. Geological Survey Open-File Report 79-1245, 16 p., https://doi.org/10.3133/ofr791245.","productDescription":"16 p.","costCenters":[],"links":[{"id":144342,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1245/report-thumb.jpg"},{"id":426520,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1245/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a223","contributors":{"authors":[{"text":"McCammon, Richard B.","contributorId":107674,"corporation":false,"usgs":true,"family":"McCammon","given":"Richard","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":161059,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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