A statistical analysis is made of the sequences of annual tree ring widths and indices. The expected value of growth during any year is shown to be proportional to the standard deviation of the growth, so that the coefficient of variation is a measure of the sensitivity of the growth of a tree. Tree ring data were found to be non-randomly distributed in time. The large values of serial correlation indicated that the non-randomness cannot be attributed entirely to climatic factors. Correlogram and power spectrum analyses applied to a sequence of tree ring indices for a pinyon pine showed that the data were generated by an autoregressive process. The statistical parameter measuring the sensitivity or complacency of growth is used to derive a growth function.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666209493254","usgsCitation":"Matalas, N., 1962, Statistical properties of tree ring data: International Association of Scientific Hydrology - Bulletin , v. 7, no. 2, p. 39-47, https://doi.org/10.1080/02626666209493254.","productDescription":"9 p.","startPage":"39","endPage":"47","costCenters":[],"links":[{"id":480373,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666209493254","text":"Publisher Index Page"},{"id":385948,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Matalas, N.C.","contributorId":25173,"corporation":false,"usgs":true,"family":"Matalas","given":"N.C.","affiliations":[],"preferred":false,"id":816460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220759,"text":"70220759 - 1962 - The distribution of tritium fallout in precipitation over North America","interactions":[],"lastModifiedDate":"2021-05-25T16:41:45.677086","indexId":"70220759","displayToPublicDate":"1962-06-01T11:38:37","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"The distribution of tritium fallout in precipitation over North America","docAbstract":"In 1958 the U.S. Geological Survey and the U.S. Weather Bureau jointly conducted a study of tritium fallout distribution over the continental United States, Alaska, and Puerto Rico. The observation period extended from early April to late July in most areas. While this was insufficient to cover the decay side of the curve, it was sufficiently long to establish general trends of tritium activity contours. Tritium activities were found to be maximum in the north central part of the country and minimum in coastal areas. The tritium activities show an inverse correlation with chloride concentrations in precipitation. Tritium activities in precipitation appear to be influenced by several “low altitude effects” particularly in storms of brief duration. Ground level tritium activity measurements are not directly representative of tritium in cloud moisture because of these effects.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666209493255","usgsCitation":"Thatcher, L.L., 1962, The distribution of tritium fallout in precipitation over North America: International Association of Scientific Hydrology - Bulletin , v. 7, no. 2, p. 48-58, https://doi.org/10.1080/02626666209493255.","productDescription":"11 p.","startPage":"48","endPage":"58","costCenters":[],"links":[{"id":480374,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666209493255","text":"Publisher Index Page"},{"id":385943,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Thatcher, L. L.","contributorId":23271,"corporation":false,"usgs":true,"family":"Thatcher","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":816454,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220754,"text":"70220754 - 1962 - Progress report on an international decade for hydrology","interactions":[],"lastModifiedDate":"2021-05-25T16:28:24.653044","indexId":"70220754","displayToPublicDate":"1962-06-01T11:25:20","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"title":"Progress report on an international decade for hydrology","docAbstract":"As reported in the Transactions of March 1961 (p. 96), the ad hoc Panel on Hydrology convened to report on ways of stimulating research in scientific hydrology, recommended a program of international cooperation in hydrology—more specifically a plan for an ‘International Decade for Hydrology,’ as drawn for the Panel by R. L. Nace. The proposal for an international program in scientific hydrology was submitted to the Council of the International Association of Scientific Hydrology (IASH), meeting at Athens during October 1961, and was explained to them by Nace. The proposal was endorsed in principle by the country representatives who were present, and further endorsement is being requested of national committees not represented at Athens. The report of the ad hoc Panel on International Cooperation in Hydrology will be published in a forthcoming Bulletin of the International Association of Scientific Hydrology.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR043i001p00009","usgsCitation":"Langbein, W.B., 1962, Progress report on an international decade for hydrology, v. 42, no. 1, p. 9-9, https://doi.org/10.1029/TR043i001p00009.","productDescription":"1 p.","startPage":"9","endPage":"9","costCenters":[],"links":[{"id":385941,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":816450,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010568,"text":"70010568 - 1962 - Hydrology","interactions":[],"lastModifiedDate":"2026-02-25T16:58:59.570241","indexId":"70010568","displayToPublicDate":"1962-03-02T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology","docAbstract":"An understanding of water in relation to earth processes requires the collaboration of many disciplines.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.135.3505.699","issn":"00368075","usgsCitation":"Hendricks, E.L., 1962, Hydrology: Science, v. 135, no. 3505, p. 699-705.","productDescription":"7 p.","startPage":"699","endPage":"705","costCenters":[],"links":[{"id":218970,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"135","issue":"3505","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a36b2e4b0c8380cd6091d","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70185611,"text":"70185611 - 1962 - The Vigil Network","interactions":[],"lastModifiedDate":"2017-03-24T14:24:10","indexId":"70185611","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"The Vigil Network","docAbstract":"Those of us who seek to explain the variations in hydrologic phenomena such as may be observed in the occurrence of floods or in changes in the shape of river channels are painfully aware of the lack of adequate data. Our existing data, collected mainly to serve immediate practical needs for water-resources development, usually are deficient in providing information useful for many kinds of scientific inquiry. Hydrologic records are usually obtained on streams that are highly regulated or otherwise put to use, to the neglect of headwater streams better suited to studies of the details of hydrologic processes.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666209493250","usgsCitation":"Leopold, L.B., 1962, The Vigil Network: International Association of Scientific Hydrology - Bulletin , v. 7, no. 2, p. 5-9, https://doi.org/10.1080/02626666209493250.","productDescription":"5 p.","startPage":"5","endPage":"9","costCenters":[],"links":[{"id":338317,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d6304ce4b05ec799131147","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70176018,"text":"70176018 - 1961 - Geology and ground-water resources of Sumner County, Kansas","interactions":[],"lastModifiedDate":"2018-09-27T11:55:07","indexId":"70176018","displayToPublicDate":"2015-11-16T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Sumner County, Kansas","docAbstract":"This report describes the geography, geology, and ground-water resources of Sumner County in south-central Kansas. The hydrologic and geologic data upon which this report is based were obtained in the field during the summers of 1955 and 1956. Records of 300 wells and 2 springs, chemical analyses of 219 water samples from wells and test holes and of 15 from streams, and logs of 362 wells and test holes are included in tables.
Sumner County has an area of 1,183 square miles and lies in the Wellington Lowland and Arkansas River Lowlands of the Central Lowland physiographic province. It is drained by Arkansas River, Ninnescah River, and Chikaskia River and their tributaries. The land surface in general is a southeastward-sloping, gently rolling plain. The average annual precipitation at Wellington is about 31 inches. Wheat fanning is the principal industry of the county, and oil is the chief natural resource.
The Wellington Formation, of Permian age, crops out in the eastern two-thirds of the county except where it is covered by Pleistocene deposits. The Ninnescah Shale (Permian) overlies the Wellington Formation and crops out in parts of the western third of the county. The Permian rocks yield small quantities of hard water to wells. Pleistocene sand and gravel deposits of Nebraskan age are present in the northwestern corner of the county and yield moderate quantities of good water to wells. Discontinuous deposits of Kansan or Illinoisan age, locally mantled by colluvium, forms terraces in southern and eastern Sumner County, and may yield moderate quantities of water. Wisconsinan terrace deposits and Recent alluvium along the major streams yield large quantities of water. Colluvium and dune sand are unimportant as sources of water but may facilitate recharge.
Maps of Sumner County included in this report show the outcrop areas of the formations, geologic cross sections, the shape and slope of the water table, the locations of wells and test holes for which records are given, and the distribution of chloride in water samples.
The ground-water reservoir is recharged principally from rain and snow that fall within the county, by percolation from streams and other surface bodies of water, and by underflow from adjacent areas. Water is discharged from the ground-water reservoir by seepage into streams, by transpiration and evaporation, by movement into adjacent areas, and by wells. Water is pumped from wells for domestic, stock, municipal, industrial, and irrigation use. Irrigation from wells is most extensive in the valley of Arkansas River, in which area further development is most probable.
Chemical analyses of samples of water from Sumner County indicate that the quality varies greatly from place to place. Sulfate is common in water from the Wellington Formation and Ninnescah Shale. Water from Pleistocene deposits is generally suitable for most uses except in local areas where it contains excessive chloride.
","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Walters, K., 1961, Geology and ground-water resources of Sumner County, Kansas: Kansas Geological Survey Bulletin, v. 151, 198 p. .","productDescription":"198 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327735,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327734,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/Geology/Sumner/index.html"}],"volume":"151","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dbe4b03fd6b7df2ce7","contributors":{"authors":[{"text":"Walters, K.L.","contributorId":105765,"corporation":false,"usgs":true,"family":"Walters","given":"K.L.","affiliations":[],"preferred":false,"id":646804,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71747,"text":"tei791 - 1961 - Geologic summary of the Appalachian basin, with reference to the subsurface disposal of radioactive waste solutions","interactions":[],"lastModifiedDate":"2018-10-03T09:25:01","indexId":"tei791","displayToPublicDate":"2013-07-16T09:38:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"791","title":"Geologic summary of the Appalachian basin, with reference to the subsurface disposal of radioactive waste solutions","docAbstract":"The Appalachian basin is an elongate depression in the crystalline basement complex which contains a great volume of predominantly sedimentary stratified rocks. As defined in this paper it extends from the Adirondack Mountains in New York to central Alabama. From east to west it extends from the west flank of the Blue Ridge Mountains to the crest of the Findlay and Cincinnati arches and the Nashville dome. It encompasses an area of about 207,000 square miles, including all of West Virginia and parts of New York, New Jersey, Pennsylvania, Ohio, Maryland, Virginia, Kentucky, Tennessee, North Carolina, Georgia, and Alabama.
The stratified rocks that occupy the basin constitute a wedge-shaped mass whose axis of greatest thickness lies close to and parallel to the east edge of the basin. The maximum thickness of stratified rocks preserved in any one part of the basin today is between 35,000 and 40,000 feet. The volume of the sedimentary rocks is approximately 510,000 cubic miles and of volcanic rocks is a few thousand cubic miles. The sedimentary rocks are predominantly Paleozoic in age, whereas the volcanic rocks are predominantly Late Precambrian.
On the basis of gross lithology the stratified rocks overlying the crystalline basement complex can be divided into nine vertically sequential units, which are designated \"sequences\" in this report. The boundaries between contiguous sequences do not necessarily coincide with the commonly recognized boundaries between systems or series. All sequences are grossly wedge shaped, being thickest along the eastern margin of the basin and thinnest along the western margin.
The lowermost unit the Late Precambrian stratified sequence is present only along part of the eastern margin of the basin, where it lies unconformably on the basement complex. It consists largely of volcanic tuffs and flows but contains some interbedded sedimentary rocks. The Late Precambrian sequence is overlain by the Early Cambrian clastic sequence. Where the older sequence is absent, the Early Cambrian sequence rests on the basement complex. Interbedded fine- to coarse-grained noncarbonate detrital rocks comprise the bulk of the sequence, but some volcanic and carbonate rocks are included. Next above is the Cambrian-Ordovician carbonate sequence which consists largely of limestone and dolomite. Some quartzose sandstone is present in the lower part in the western half of the basin, and much shale is present in the upper part in the southeast part of the basin. The next higher sequence is the Late Ordovician clastic sequence, which consists largely of shale, siltstone, and sandstone. Coarse-grained light-gray to red rocks are common in the sequence along the eastern side of the basin, whereas fine-grained dark-gray to black calcareous rocks are common along the west side. The Late Ordovician clastic sequence is overlain unconformably in many places by the Early Silurian clastic sequence. The latter comprises a relatively thin wedge of coarse-grained clastic rocks. Some of the most prolific oil- and gas-producing sandstones in the Appalachian basin are included. Among these are the \"Clinton\" sands of Ohio, the Medina Sandstones of New York and Pennsylvania, and the Keefer or \"Big Six\" Sandstone of West Virginia and Kentucky. Conformably overlying the Early Silurian clastic sequence is the Silurian-Devonian carbonate sequence, which consists predominantly of limestone and dolomite. It also contains a salt-bearing unit in the north-central part of the basin and a thick wedge of coarse-grained red beds in the northeastern part. The sequence is absent in much of the southern part of the basin. Large volumes of gas and much oil are obtained from some of its rocks, especially from the Oriskany Sandstone and the Huntersville Ghert. The Silurian-Devonian carbonate sequence is abruptly overlain by the Devonian clastic sequence a thick succession of interbedded shale, mudrock, siltstone, and sandstone. Colors range from predominantly purple and red in the northeastern part of the basin to predominantly dark gray and black in the southwestern part. Many rocks in the upper part contain hydrocarbons in commercial quantities. The next higher sequence is a heterogeneous succession that comprises most rocks of Mississippian age in the basin. It is composed largely of fine-grained to very coarse-grained noncalcareous clastic rocks in the northern half of the basin, and largely of carbonate rocks in the southern part. Large quantities of oil and gas are produced from the sequence. The youngest sequence consists of coarse-grained clastic rocks largely of Pennsylvanian age. In the center of the basin a relatively small volume of lithologically similar rocks of Permian age are included. The sequence has been intensively mined for coal throughout most of its extent.
The waste-disposal possibilities of the stratified rocks in the Appalachian basin are considered in terms of the following: 1) gross lithology of the sequences; 2) general lithology of the rock units composing the sequences; and 3) the structural attitudes of the sequences in different parts of the basin. The degree of exploitation of economically significant mineral* resources is considered briefly where such exploitation may affect waste-disposal possibilities. Hydrologic aspects are not in general considered. Based largely on consideration of the above geologic factors the following types of reservoirs associated with particular geologic environments offer some prospects for the disposal of radioactive waste solutions. They are: 1) artificially created cavities in thick salt beds; 2) artificially fractured thin lenticular sandstone bodies isolated in shale or mudrock sequences; 3) portions of thick noncarbonate clastic sequences possessing appreciable natural porosity and permeability; 4) thin clastic units (with natural or artificially created openings) in the plate of a thrust fault overlain by impermeable strata.
Considered in its entirety the Late Ordovician clastic sequence appears to have a greater number of favorable geologic factors for waste-disposal purposes than the others. The Early Silurian clastic sequence, the Silurian-Devonian carbonate sequence, and the Devonian clastic sequence offer fewer possibilities. The Late Precambrian stratified sequence, Early Cambrian, and the Cambrian-Ordovician carbonate sequence offer few possibilities. The Mississippian and Pennsylvanian sequences appear to be generally unsuitable.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei791","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Colton, G.W., 1961, Geologic summary of the Appalachian basin, with reference to the subsurface disposal of radioactive waste solutions: U.S. Geological Survey Trace Elements Investigations 791, Report: 121 p.; 15 Maps; 1 Illustration, https://doi.org/10.3133/tei791.","productDescription":"Report: 121 p.; 15 Maps; 1 Illustration","costCenters":[],"links":[{"id":358066,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358065,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0028/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358067,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358068,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358069,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358070,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358071,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358072,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358073,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358074,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358075,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358076,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358077,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358078,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358079,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358080,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358081,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":290249,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0028/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Appalachian Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.71,35.8 ], [ -84.71,43.91 ], [ -74.13,43.91 ], [ -74.13,35.8 ], [ -84.71,35.8 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79ef3e4b0194841642446","contributors":{"authors":[{"text":"Colton, George Willis","contributorId":12015,"corporation":false,"usgs":true,"family":"Colton","given":"George","email":"","middleInitial":"Willis","affiliations":[],"preferred":false,"id":284696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71744,"text":"tei787 - 1961 - Hydrologic significance of six core holes in carbonate rocks of the Nevada test site","interactions":[],"lastModifiedDate":"2014-07-16T09:31:07","indexId":"tei787","displayToPublicDate":"2013-07-16T09:29:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"787","title":"Hydrologic significance of six core holes in carbonate rocks of the Nevada test site","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei787","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission.","usgsCitation":"Schoff, S.L., and Winograd, I.J., 1961, Hydrologic significance of six core holes in carbonate rocks of the Nevada test site: U.S. Geological Survey Trace Elements Investigations 787, 97 p., https://doi.org/10.3133/tei787.","productDescription":"97 p.","costCenters":[],"links":[{"id":290247,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.01,35.0 ], [ -120.01,42.0 ], [ -114.04,42.0 ], [ -114.04,35.0 ], [ -120.01,35.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79efce4b019484164245f","contributors":{"authors":[{"text":"Schoff, Stuart Leeson","contributorId":57951,"corporation":false,"usgs":true,"family":"Schoff","given":"Stuart","email":"","middleInitial":"Leeson","affiliations":[],"preferred":false,"id":284693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winograd, Isaac Judah","contributorId":9233,"corporation":false,"usgs":true,"family":"Winograd","given":"Isaac","email":"","middleInitial":"Judah","affiliations":[],"preferred":false,"id":284692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047041,"text":"70047041 - 1961 - Water utilization in the Anchorage area, Alaska, 1958-59","interactions":[{"subject":{"id":52142,"text":"ofr60150 - 1960 - Water utilization in the Anchorage area, Alaska, 1958-59","indexId":"ofr60150","publicationYear":"1960","noYear":false,"title":"Water utilization in the Anchorage area, Alaska, 1958-59"},"predicate":"SUPERSEDED_BY","object":{"id":70047041,"text":"70047041 - 1961 - Water utilization in the Anchorage area, Alaska, 1958-59","indexId":"70047041","publicationYear":"1961","noYear":false,"title":"Water utilization in the Anchorage area, Alaska, 1958-59"},"id":1}],"lastModifiedDate":"2013-07-15T15:10:16","indexId":"70047041","displayToPublicDate":"2013-01-01T15:05:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":258,"text":"Hydrological Data","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"12","title":"Water utilization in the Anchorage area, Alaska, 1958-59","language":"English","publisher":"Alaska Department of Health and Welfare","collaboration":"Issued in cooperation with the U.S. Geological Survey, Water Resources Division","usgsCitation":"Waller, R., 1961, Water utilization in the Anchorage area, Alaska, 1958-59: Hydrological Data 12, 19 p.","productDescription":"19 p.","costCenters":[],"links":[{"id":275007,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","city":"Anchorage","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -153.25,59.75 ], [ -153.25,62.5 ], [ -145.75,62.5 ], [ -145.75,59.75 ], [ -153.25,59.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51e519f5e4b069f8d27ccb72","contributors":{"authors":[{"text":"Waller, R.M.","contributorId":13659,"corporation":false,"usgs":true,"family":"Waller","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":480917,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70040438,"text":"70040438 - 1961 - Hydrology of the shallow ground-water reservoir of the Town of Southold, Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2012-10-19T17:16:26","indexId":"70040438","displayToPublicDate":"2012-01-01T13:59:30","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"GW-45","title":"Hydrology of the shallow ground-water reservoir of the Town of Southold, Suffolk County, Long Island, New York","language":"English","publisher":"New York State Water Resources Commission","publisherLocation":"Albany, NY","usgsCitation":"Hoffman, J., 1961, Hydrology of the shallow ground-water reservoir of the Town of Southold, Suffolk County, Long Island, New York: Bulletin GW-45, 49 p., 1 Plate.","productDescription":"49 p., 1 Plate","numberOfPages":"49","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.760000,40.480000 ], [ -79.760000,45.020000 ], [ -71.860000,45.020000 ], [ -71.860000,40.480000 ], [ -79.760000,40.480000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50df0563e4b0dfbe79e686de","contributors":{"authors":[{"text":"Hoffman, J.F.","contributorId":37413,"corporation":false,"usgs":true,"family":"Hoffman","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":468327,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71752,"text":"tei796 - 1961 - Preliminary evaluation of the seismicity, geology, and hydrology of the northern Sand Springs Range, Churchill County, Nevada, as a possible site for Project Shoal","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"tei796","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"796","title":"Preliminary evaluation of the seismicity, geology, and hydrology of the northern Sand Springs Range, Churchill County, Nevada, as a possible site for Project Shoal","language":"ENGLISH","doi":"10.3133/tei796","usgsCitation":"Twenhofel, W., Moore, J.E., and Black, R.A., 1961, Preliminary evaluation of the seismicity, geology, and hydrology of the northern Sand Springs Range, Churchill County, Nevada, as a possible site for Project Shoal: U.S. Geological Survey Trace Elements Investigations 796, 21 p. : ill., maps ; 27 cm.; 10 figs.; 1 table, https://doi.org/10.3133/tei796.","productDescription":"21 p. : ill., maps ; 27 cm.; 10 figs.; 1 table","costCenters":[],"links":[{"id":191640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/796/report-thumb.jpg"},{"id":90982,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/796/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c36b","contributors":{"authors":[{"text":"Twenhofel, William S.","contributorId":47876,"corporation":false,"usgs":true,"family":"Twenhofel","given":"William S.","affiliations":[],"preferred":false,"id":284704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, John Ezra","contributorId":93582,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"Ezra","affiliations":[],"preferred":false,"id":284706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Black, Rudolph Allen","contributorId":60724,"corporation":false,"usgs":true,"family":"Black","given":"Rudolph","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":284705,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68325,"text":"ha42 - 1961 - Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells","interactions":[],"lastModifiedDate":"2022-06-03T20:40:02.242302","indexId":"ha42","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"42","title":"Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha42","usgsCitation":"Herrick, E.H., 1961, Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells: U.S. Geological Survey Hydrologic Atlas 42, 1 Plate: 27.50 × 21.00 inches, https://doi.org/10.3133/ha42.","productDescription":"1 Plate: 27.50 × 21.00 inches","costCenters":[],"links":[{"id":185963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":401720,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15804.htm"},{"id":89786,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/042/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"680","country":"United States","state":"New Mexico","county":"Dona Ana County","otherGeospatial":"White Sands Missile Range headquarters area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.622314453125,\n 32.287132632616384\n ],\n [\n -106.383,\n 32.287132632616384\n ],\n [\n -106.383,\n 32.465743313283596\n ],\n [\n -106.622314453125,\n 32.465743313283596\n ],\n [\n -106.622314453125,\n 32.287132632616384\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2aef","contributors":{"authors":[{"text":"Herrick, Eugene H.","contributorId":80360,"corporation":false,"usgs":true,"family":"Herrick","given":"Eugene","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278031,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52211,"text":"ofr61152 - 1961 - Hydrologic significance of six core holes in carbonate rocks of the Nevada Test Site","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr61152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-152","title":"Hydrologic significance of six core holes in carbonate rocks of the Nevada Test Site","language":"ENGLISH","doi":"10.3133/ofr61152","usgsCitation":"Schoff, S., and Winograd, I., 1961, Hydrologic significance of six core holes in carbonate rocks of the Nevada Test Site: U.S. Geological Survey Open-File Report 61-152, 97 p., https://doi.org/10.3133/ofr61152.","productDescription":"97 p.","costCenters":[],"links":[{"id":177343,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6052ed","contributors":{"authors":[{"text":"Schoff, S.L.","contributorId":107365,"corporation":false,"usgs":true,"family":"Schoff","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":244976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winograd, I.J.","contributorId":10408,"corporation":false,"usgs":true,"family":"Winograd","given":"I.J.","affiliations":[],"preferred":false,"id":244975,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68452,"text":"ha40 - 1961 - Floods at Mount Vernon, Ohio","interactions":[],"lastModifiedDate":"2022-04-29T20:48:06.30266","indexId":"ha40","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"40","title":"Floods at Mount Vernon, Ohio","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha40","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Floods at Mount Vernon, Ohio: U.S. Geological Survey Hydrologic Atlas 40, 1 Plate: 22.50 × 29.00 inches, https://doi.org/10.3133/ha40.","productDescription":"1 Plate: 22.50 × 29.00 inches","costCenters":[],"links":[{"id":186274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":399951,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15782.htm"},{"id":89989,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"12000","country":"United States","state":"Ohio","city":"Mount Vernon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.517,\n 40.358\n ],\n [\n -82.45,\n 40.358\n ],\n [\n -82.45,\n 40.425\n ],\n [\n -82.517,\n 40.425\n ],\n [\n -82.517,\n 40.358\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df767","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":534511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57721,"text":"ofr61177 - 1961 - Ground water in the alluvial deposits of the Canadian River valley near Norman, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:12:12","indexId":"ofr61177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-177","title":"Ground water in the alluvial deposits of the Canadian River valley near Norman, Oklahoma","docAbstract":"Unconsolidated water-bearing alluvial deposits border the Canadian River in the vicinity of Norman, Oklahoma. These Quaternary materials are divided on the basis of topgraphic position into 'high terrace deposits' and 'alluvium.' The high terrace lies at an elevation of 50 to 60 feet above the alluvium, which in turn lies 7 to 15 feet above the channel of the Canadian River. Southwest of Norman a relatively thick section of these deposits occur as a hydrologic unit and overlie impermeable Permian shale. The high terrace deposits contain thick beds of clay, silt, and fine sand, whereas the alluvium contains a higher percentage of coarse sand and gravel.\r\nGround-water recharge is estimated to be 23 percent of the normal annual precipitation of 33.22 inches; the specific yield is about 15 percent, and the coefficient of permeability is about 1,000 gpd/ft2. Using these figures 17,000 acre-feet of water is computed to be in storage within the area acting as a hydrologic unit. About 3.6 million gallons of water is discharged daily from the high terrace deposits through a 16,000-foot section of alluvium having a saturated thickness of 40 feet along the river.\r\n\r\nThe quality of water in the high terrace deposits meets the standards of the U.S. Public Health Service for domestic water used by Interstate carriers but nitrate content of one well is higher than recommended by the Oklahoma Department of Public Health. Water in the alluvium is of poorer quality because the water is concentrated by evapotranspiration.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr61177","usgsCitation":"Stacy, B.L., 1961, Ground water in the alluvial deposits of the Canadian River valley near Norman, Oklahoma: U.S. Geological Survey Open-File Report 61-177, 61 p., https://doi.org/10.3133/ofr61177.","productDescription":"61 p.","costCenters":[],"links":[{"id":184149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d7fe","contributors":{"authors":[{"text":"Stacy, Bill L.","contributorId":99637,"corporation":false,"usgs":true,"family":"Stacy","given":"Bill","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":257637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52156,"text":"ofr6128 - 1961 - Floods in Pennsylvania, frequency and magnitude","interactions":[],"lastModifiedDate":"2016-06-23T10:52:55","indexId":"ofr6128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-28","title":"Floods in Pennsylvania, frequency and magnitude","docAbstract":"This report outlines a method of determining the magnitude of floods having frequencies up to 50 years for any stream in Pennsylvania except regulated streams and streams whose drainage basins are smaller than 10 square miles. On the main stems of the Schuylkill, Delaware, Susquehanna, and Chemung Rivers the magnitude of floods can be determined for frequencies up to 100 years.
\nSix composite frequency curves show the relation of the mean annual flood to floods having recurrence interval up to 50 to 100 years. Curves for fourteen hydrologic areas show the variation of mean annual flood with drainage area. This report explains how to select the proper curves for any chosen point in the State and how to compute a flood-frequency curve for that point.
\nA tabulation of peak gage heights and discharges for most gaging stations in the State is included. In general, the tabulations contain all peaks above a specific base discharge, although for some stations only annual peaks are shown.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/ofr6128","usgsCitation":"Busch, W.F., and Shaw, E., 1961, Floods in Pennsylvania, frequency and magnitude: U.S. Geological Survey Open-File Report 61-28, Report: v, 231 p.; 2 Sheets: 15.86 x 9.71 inches and 16.10 x 9.63 inches, https://doi.org/10.3133/ofr6128.","productDescription":"Report: v, 231 p.; 2 Sheets: 15.86 x 9.71 inches and 16.10 x 9.63 inches","numberOfPages":"240","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":178746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr6128.jpg"},{"id":324286,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1961/0028/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":324287,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0028/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":324288,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0028/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-79.916171,39.720893],[-80.075947,39.72135],[-80.421388,39.721189],[-80.519342,39.721403],[-80.519423,39.806181],[-80.518891,39.890964],[-80.519248,39.936967],[-80.51896,40.078089],[-80.519039,40.342101],[-80.517991,40.367968],[-80.51769,40.462467],[-80.51899,40.473667],[-80.519002,40.877543],[-80.519891,40.906661],[-80.519091,40.921061],[-80.518928,41.070954],[-80.519144,41.171203],[-80.518693,41.248855],[-80.518993,41.268155],[-80.518794,41.305509],[-80.519129,41.312408],[-80.519345,41.340145],[-80.518993,41.435454],[-80.519339,41.539297],[-80.519425,41.977522],[-80.435451,42.005611],[-80.409776,42.011578],[-80.373066,42.024102],[-80.371869,42.023966],[-80.363251,42.027973],[-80.349169,42.030243],[-80.329976,42.036168],[-80.296758,42.049076],[-80.230486,42.077957],[-80.188085,42.094257],[-80.165884,42.105857],[-80.154084,42.114757],[-80.136213,42.149937],[-80.13043,42.156331],[-80.117368,42.166341],[-80.088512,42.173184],[-80.077388,42.171262],[-80.073381,42.168658],[-80.080028,42.163625],[-80.071981,42.155357],[-80.078781,42.151457],[-80.076281,42.147857],[-80.07198,42.146057],[-80.06108,42.144857],[-79.989186,42.177051],[-79.931324,42.206737],[-79.923924,42.207546],[-79.90105,42.216701],[-79.886187,42.224933],[-79.867979,42.230999],[-79.844661,42.235486],[-79.798447,42.255939],[-79.761951,42.26986],[-79.762152,42.243054],[-79.761759,42.162675],[-79.762122,42.131246],[-79.761709,42.11899],[-79.761798,42.019042],[-79.761374,41.999067],[-79.670128,41.999335],[-79.472472,41.998255],[-79.249772,41.998807],[-79.17857,41.999458],[-79.061265,41.999259],[-78.983065,41.998949],[-78.874759,41.997559],[-78.749754,41.998109],[-78.59665,41.999877],[-78.308128,41.999415],[-78.271204,41.998968],[-78.12473,42.000452],[-78.031177,41.999415],[-77.997508,41.998758],[-77.83203,41.998524],[-77.505308,42.00007],[-77.124693,41.999395],[-77.063676,42.000461],[-76.920784,42.001774],[-76.749675,42.001689],[-76.558118,42.000155],[-76.462155,41.998934],[-76.343722,41.998346],[-76.131201,41.998954],[-75.98025,41.999035],[-75.870677,41.998828],[-75.742217,41.997864],[-75.610316,41.99896],[-75.359579,41.999445],[-75.353504,41.99711],[-75.346568,41.995324],[-75.341125,41.992772],[-75.337602,41.9867],[-75.337791,41.984386],[-75.34246,41.974303],[-75.342204,41.972872],[-75.339488,41.970786],[-75.335771,41.970315],[-75.329318,41.968232],[-75.322384,41.961693],[-75.32004,41.960867],[-75.318168,41.954236],[-75.312817,41.950182],[-75.310358,41.949012],[-75.303966,41.948216],[-75.301664,41.94838],[-75.301233,41.9489],[-75.301593,41.952811],[-75.300409,41.953871],[-75.29858,41.954521],[-75.293713,41.954593],[-75.29143,41.952477],[-75.291762,41.947092],[-75.290966,41.945039],[-75.289383,41.942891],[-75.279094,41.938917],[-75.277243,41.933598],[-75.276501,41.926679],[-75.276552,41.922208],[-75.275368,41.919564],[-75.269736,41.911363],[-75.267562,41.907054],[-75.267773,41.901971],[-75.272778,41.897112],[-75.272581,41.893168],[-75.271292,41.88736],[-75.267789,41.885982],[-75.263005,41.885109],[-75.260623,41.883783],[-75.257564,41.877108],[-75.258439,41.875087],[-75.261488,41.873277],[-75.263815,41.870757],[-75.263673,41.868105],[-75.262802,41.866213],[-75.260527,41.8638],[-75.257825,41.862154],[-75.251197,41.86204],[-75.248045,41.8633],[-75.243345,41.866875],[-75.241134,41.867118],[-75.238743,41.865699],[-75.234565,41.861569],[-75.231612,41.859459],[-75.22572,41.857481],[-75.223734,41.857456],[-75.220125,41.860534],[-75.21497,41.867449],[-75.209741,41.86925],[-75.204002,41.869867],[-75.197836,41.868807],[-75.194382,41.867287],[-75.191441,41.865063],[-75.190203,41.862454],[-75.188888,41.861264],[-75.186993,41.860109],[-75.185254,41.85993],[-75.183937,41.860515],[-75.182271,41.862198],[-75.180497,41.86568],[-75.179134,41.869935],[-75.176633,41.872371],[-75.174574,41.87266],[-75.170565,41.871608],[-75.169142,41.87029],[-75.168053,41.867043],[-75.168733,41.859258],[-75.166217,41.853862],[-75.164168,41.851586],[-75.161541,41.849836],[-75.156512,41.848327],[-75.152898,41.848564],[-75.143824,41.851737],[-75.140241,41.852078],[-75.130983,41.845145],[-75.127913,41.844903],[-75.118789,41.845819],[-75.115598,41.844638],[-75.114399,41.843583],[-75.113369,41.840698],[-75.113441,41.836298],[-75.114998,41.8303],[-75.115147,41.827285],[-75.114837,41.82567],[-75.113334,41.822782],[-75.100024,41.818347],[-75.093537,41.813375],[-75.089484,41.811576],[-75.085789,41.811626],[-75.079818,41.814815],[-75.078063,41.815112],[-75.074409,41.815088],[-75.072172,41.813732],[-75.071751,41.811901],[-75.072168,41.808327],[-75.074412,41.802191],[-75.076889,41.798509],[-75.07827,41.797467],[-75.081415,41.796483],[-75.088328,41.797534],[-75.092876,41.796386],[-75.101463,41.787941],[-75.102329,41.786503],[-75.103548,41.782008],[-75.10464,41.774203],[-75.104334,41.772693],[-75.103492,41.771238],[-75.10099,41.769121],[-75.095451,41.768366],[-75.09281,41.768361],[-75.079478,41.771205],[-75.075942,41.771518],[-75.074231,41.770518],[-75.072664,41.768807],[-75.068567,41.767298],[-75.064901,41.766686],[-75.060759,41.764638],[-75.053431,41.752538],[-75.052808,41.744725],[-75.054818,41.735168],[-75.053527,41.72715],[-75.049699,41.715093],[-75.049862,41.713309],[-75.050689,41.711969],[-75.052226,41.711396],[-75.061174,41.712935],[-75.06663,41.712588],[-75.068642,41.710146],[-75.06883,41.708161],[-75.067278,41.705434],[-75.059829,41.699716],[-75.056745,41.695703],[-75.052736,41.688393],[-75.051234,41.682439],[-75.051285,41.679961],[-75.052653,41.678436],[-75.058765,41.674412],[-75.059332,41.67232],[-75.05843,41.669653],[-75.057251,41.668933],[-75.053991,41.668194],[-75.04992,41.662556],[-75.048683,41.656317],[-75.049281,41.641862],[-75.048658,41.633781],[-75.048199,41.632011],[-75.043562,41.62364],[-75.044224,41.617978],[-75.045508,41.616203],[-75.047298,41.615791],[-75.048385,41.615986],[-75.051856,41.618157],[-75.05385,41.618655],[-75.060098,41.617482],[-75.06156,41.616429],[-75.061675,41.615468],[-75.059956,41.612306],[-75.059725,41.610801],[-75.062716,41.609639],[-75.067795,41.610143],[-75.071667,41.609501],[-75.074626,41.607905],[-75.074613,41.605711],[-75.066955,41.599428],[-75.063677,41.594739],[-75.060012,41.590813],[-75.052858,41.587772],[-75.04676,41.583258],[-75.043879,41.575094],[-75.04049,41.569688],[-75.036989,41.567049],[-75.033162,41.565092],[-75.029211,41.564637],[-75.027343,41.563541],[-75.018524,41.551802],[-75.016328,41.546501],[-75.016144,41.544246],[-75.017626,41.542734],[-75.022828,41.541456],[-75.024798,41.539801],[-75.024757,41.535099],[-75.024206,41.534018],[-75.023018,41.533147],[-75.016616,41.53211],[-75.014919,41.531399],[-75.009552,41.528461],[-75.00385,41.524052],[-75.001297,41.52065],[-75.000911,41.519292],[-75.000935,41.517638],[-75.002592,41.51456],[-75.003706,41.511118],[-75.003694,41.509295],[-75.003151,41.508101],[-74.999612,41.5074],[-74.993893,41.508754],[-74.987645,41.508738],[-74.985653,41.507926],[-74.984372,41.506611],[-74.982385,41.500981],[-74.982168,41.498486],[-74.982463,41.496467],[-74.985247,41.489113],[-74.985595,41.485863],[-74.985004,41.483703],[-74.983341,41.480894],[-74.981652,41.479945],[-74.969887,41.477438],[-74.95826,41.476396],[-74.956411,41.476735],[-74.94808,41.480625],[-74.945634,41.483213],[-74.941798,41.483542],[-74.932585,41.482323],[-74.926835,41.478327],[-74.924092,41.477138],[-74.917282,41.477041],[-74.912517,41.475605],[-74.909181,41.472436],[-74.908133,41.468117],[-74.908103,41.464639],[-74.906887,41.461131],[-74.9042,41.459806],[-74.895069,41.45819],[-74.892114,41.456959],[-74.890358,41.455324],[-74.889116,41.452534],[-74.889075,41.451245],[-74.894931,41.446099],[-74.896399,41.442179],[-74.896025,41.439987],[-74.893913,41.43893],[-74.888691,41.438259],[-74.876721,41.440338],[-74.864688,41.443993],[-74.858578,41.444427],[-74.8542,41.443166],[-74.848602,41.440179],[-74.845572,41.437577],[-74.836915,41.431625],[-74.834635,41.430796],[-74.830671,41.430503],[-74.828592,41.430698],[-74.826031,41.431736],[-74.82288,41.436792],[-74.817995,41.440505],[-74.812123,41.442982],[-74.807582,41.442847],[-74.805655,41.442101],[-74.801225,41.4381],[-74.80037,41.43606],[-74.800095,41.432661],[-74.799546,41.43129],[-74.795396,41.42398],[-74.793856,41.422671],[-74.790417,41.42166],[-74.784339,41.422397],[-74.778029,41.425104],[-74.773239,41.426352],[-74.77065,41.42623],[-74.763701,41.423612],[-74.758587,41.423287],[-74.754359,41.425147],[-74.75068,41.427984],[-74.743821,41.430635],[-74.740932,41.43116],[-74.738455,41.430641],[-74.736688,41.429228],[-74.735519,41.427465],[-74.734893,41.425818],[-74.734731,41.422699],[-74.738684,41.413463],[-74.741086,41.411413],[-74.741717,41.40788],[-74.740963,41.40512],[-74.738554,41.401191],[-74.736103,41.398398],[-74.73364,41.396975],[-74.730384,41.39566],[-74.720891,41.39469],[-74.715979,41.392584],[-74.713411,41.389814],[-74.710391,41.382102],[-74.708458,41.378901],[-74.703282,41.375093],[-74.694968,41.370431],[-74.691129,41.367324],[-74.689516,41.363843],[-74.689767,41.361558],[-74.691076,41.36034],[-74.696398,41.357339],[-74.694914,41.357423],[-74.700595,41.354553],[-74.704429,41.354043],[-74.708514,41.352734],[-74.720923,41.347384],[-74.730373,41.345983],[-74.735622,41.346518],[-74.753239,41.346122],[-74.755971,41.344953],[-74.760325,41.340325],[-74.763499,41.331568],[-74.766714,41.328558],[-74.771588,41.325079],[-74.774887,41.324326],[-74.781584,41.324229],[-74.789095,41.323281],[-74.792116,41.322465],[-74.79504,41.320407],[-74.795822,41.318516],[-74.792377,41.314088],[-74.791991,41.311639],[-74.792558,41.310628],[-74.806858,41.303155],[-74.812033,41.298157],[-74.815703,41.296151],[-74.821884,41.293838],[-74.830057,41.2872],[-74.834067,41.281111],[-74.838366,41.277286],[-74.841137,41.27098],[-74.846319,41.263077],[-74.846506,41.261576],[-74.845031,41.258055],[-74.845883,41.254945],[-74.846932,41.253318],[-74.848987,41.251192],[-74.854669,41.25051],[-74.856003,41.250094],[-74.857151,41.248975],[-74.861678,41.241575],[-74.862049,41.237609],[-74.866182,41.232132],[-74.867405,41.22777],[-74.866839,41.226865],[-74.860837,41.222317],[-74.859323,41.220507],[-74.859632,41.219077],[-74.860398,41.217454],[-74.867287,41.208754],[-74.874034,41.198543],[-74.878275,41.190489],[-74.878492,41.187504],[-74.882139,41.180836],[-74.889424,41.1736],[-74.899701,41.166181],[-74.901172,41.16387],[-74.90178,41.161394],[-74.905256,41.155668],[-74.923169,41.138146],[-74.931141,41.133387],[-74.945067,41.129052],[-74.947714,41.126292],[-74.947334,41.124439],[-74.947912,41.12356],[-74.964294,41.114237],[-74.966298,41.113669],[-74.969312,41.113869],[-74.972917,41.113327],[-74.979873,41.110423],[-74.982212,41.108245],[-74.991718,41.092284],[-74.991815,41.089132],[-74.991013,41.088578],[-74.988263,41.088222],[-74.984782,41.088545],[-74.981314,41.08986],[-74.975298,41.094073],[-74.972036,41.095562],[-74.969434,41.096074],[-74.967464,41.095327],[-74.966759,41.093425],[-74.968389,41.087797],[-74.970987,41.085293],[-74.98259,41.079172],[-74.989332,41.078319],[-74.994847,41.076556],[-74.999617,41.073943],[-75.006376,41.067546],[-75.011133,41.067521],[-75.01257,41.066281],[-75.015271,41.061215],[-75.015867,41.05821],[-75.017239,41.055491],[-75.019186,41.052968],[-75.025702,41.046482],[-75.026376,41.04444],[-75.02543,41.04071],[-75.025777,41.039806],[-75.030701,41.038416],[-75.034496,41.036755],[-75.040668,41.031755],[-75.070532,41.01862],[-75.074999,41.01713],[-75.081101,41.016838],[-75.089787,41.014549],[-75.090312,41.013302],[-75.095556,41.008874],[-75.100682,41.006716],[-75.109114,41.004102],[-75.110595,41.002174],[-75.123423,40.996129],[-75.127196,40.993954],[-75.130575,40.991093],[-75.131619,40.9889],[-75.13153,40.984914],[-75.132106,40.982566],[-75.133086,40.980179],[-75.135521,40.976865],[-75.135526,40.973807],[-75.13378,40.970973],[-75.131364,40.969277],[-75.129074,40.968976],[-75.122603,40.970152],[-75.120514,40.968369],[-75.11977,40.96651],[-75.12065,40.964028],[-75.119893,40.961646],[-75.118904,40.956361],[-75.117764,40.953023],[-75.111683,40.948111],[-75.106153,40.939671],[-75.105524,40.936294],[-75.095526,40.924152],[-75.079279,40.91389],[-75.076956,40.90988],[-75.076092,40.907042],[-75.075188,40.900154],[-75.075957,40.895694],[-75.07534,40.894162],[-75.07392,40.892176],[-75.065438,40.885682],[-75.062149,40.882289],[-75.058655,40.877654],[-75.053664,40.87366],[-75.051508,40.870224],[-75.050839,40.868067],[-75.051029,40.865662],[-75.053294,40.8599],[-75.060491,40.85302],[-75.064328,40.848338],[-75.066014,40.847591],[-75.07083,40.847392],[-75.073544,40.84894],[-75.076684,40.849875],[-75.090962,40.849187],[-75.095784,40.847082],[-75.097221,40.844672],[-75.097586,40.843042],[-75.097572,40.840967],[-75.097006,40.839336],[-75.09494,40.837103],[-75.085517,40.830085],[-75.083822,40.827805],[-75.083929,40.824471],[-75.085387,40.821972],[-75.090518,40.815913],[-75.096147,40.812211],[-75.098279,40.810286],[-75.100277,40.807578],[-75.100739,40.805488],[-75.100165,40.803],[-75.100277,40.801176],[-75.1008,40.799797],[-75.108505,40.791094],[-75.111343,40.789896],[-75.116842,40.78935],[-75.123088,40.786746],[-75.125867,40.784026],[-75.131465,40.77595],[-75.133303,40.774124],[-75.1344,40.773765],[-75.139106,40.773606],[-75.149378,40.774786],[-75.16365,40.778386],[-75.169523,40.778473],[-75.171587,40.777745],[-75.173349,40.776129],[-75.17562,40.772923],[-75.176855,40.768721],[-75.177477,40.764225],[-75.17904,40.761897],[-75.183037,40.759344],[-75.191796,40.75583],[-75.196533,40.751631],[-75.196861,40.750097],[-75.196325,40.747137],[-75.195349,40.745473],[-75.18578,40.737266],[-75.182804,40.73365],[-75.182084,40.731522],[-75.1825,40.729922],[-75.186372,40.72397],[-75.189412,40.71797],[-75.192612,40.715874],[-75.19442,40.714018],[-75.19872,40.705298],[-75.20392,40.691498],[-75.20092,40.685498],[-75.19692,40.681299],[-75.19058,40.679379],[-75.184516,40.679971],[-75.180564,40.679363],[-75.177587,40.677731],[-75.176803,40.675715],[-75.177491,40.672595],[-75.182756,40.665971],[-75.18794,40.663811],[-75.190852,40.661939],[-75.196676,40.655123],[-75.200452,40.649219],[-75.200468,40.646899],[-75.193492,40.642275],[-75.192276,40.640803],[-75.191059,40.637971],[-75.188579,40.624628],[-75.189283,40.621492],[-75.190691,40.619956],[-75.197891,40.619332],[-75.200708,40.618356],[-75.201812,40.617188],[-75.201348,40.614628],[-75.198499,40.611492],[-75.195923,40.606788],[-75.192291,40.602676],[-75.190146,40.590359],[-75.190796,40.586838],[-75.194656,40.58194],[-75.195114,40.579689],[-75.194046,40.576256],[-75.192352,40.574257],[-75.186737,40.569406],[-75.183151,40.567354],[-75.175307,40.564996],[-75.168609,40.564111],[-75.162871,40.564096],[-75.158446,40.565286],[-75.147368,40.573152],[-75.141906,40.575273],[-75.136748,40.575731],[-75.117292,40.573211],[-75.110903,40.570671],[-75.100325,40.567811],[-75.0957,40.564401],[-75.078503,40.548296],[-75.068615,40.542223],[-75.067257,40.539584],[-75.066426,40.536619],[-75.06509,40.526148],[-75.065853,40.519495],[-75.066001,40.510716],[-75.065275,40.504682],[-75.062373,40.491689],[-75.061937,40.486362],[-75.062227,40.481391],[-75.064327,40.476795],[-75.067776,40.472827],[-75.06805,40.468578],[-75.067302,40.464954],[-75.070568,40.456348],[-75.070568,40.455165],[-75.067425,40.448323],[-75.062923,40.433407],[-75.061489,40.422848],[-75.058848,40.418065],[-75.056102,40.416066],[-75.046473,40.413792],[-75.043071,40.411603],[-75.041651,40.409894],[-75.036616,40.406796],[-75.028315,40.403883],[-75.024775,40.403455],[-75.017221,40.404638],[-75.003351,40.40785],[-74.998651,40.410093],[-74.996378,40.410528],[-74.988901,40.408773],[-74.985467,40.405935],[-74.982735,40.404432],[-74.969597,40.39977],[-74.965508,40.397337],[-74.963997,40.395246],[-74.953697,40.376081],[-74.948722,40.364768],[-74.946006,40.357306],[-74.945088,40.347332],[-74.943776,40.342564],[-74.939711,40.338006],[-74.933111,40.333106],[-74.92681,40.329406],[-74.91741,40.322406],[-74.90831,40.316907],[-74.90331,40.315607],[-74.896409,40.315107],[-74.891609,40.313007],[-74.887109,40.310307],[-74.880609,40.305607],[-74.868209,40.295207],[-74.860492,40.284584],[-74.856508,40.277407],[-74.853108,40.269707],[-74.846608,40.258808],[-74.842308,40.250508],[-74.836307,40.246208],[-74.823907,40.241508],[-74.819507,40.238508],[-74.795306,40.229408],[-74.781206,40.221508],[-74.77136,40.215399],[-74.770406,40.214508],[-74.766905,40.207709],[-74.760605,40.198909],[-74.756905,40.189409],[-74.755605,40.186709],[-74.754305,40.185209],[-74.751705,40.183309],[-74.744105,40.181009],[-74.737205,40.177609],[-74.733804,40.174509],[-74.722304,40.160609],[-74.721504,40.158409],[-74.721604,40.15381],[-74.722604,40.15001],[-74.724304,40.14701],[-74.725663,40.145495],[-74.740605,40.13521],[-74.742905,40.13441],[-74.745905,40.13421],[-74.755305,40.13471],[-74.758882,40.134036],[-74.762864,40.132541],[-74.769488,40.129145],[-74.782106,40.12081],[-74.785106,40.12031],[-74.788706,40.12041],[-74.800607,40.12281],[-74.812807,40.12691],[-74.816307,40.12761],[-74.819007,40.12751],[-74.822307,40.12671],[-74.825907,40.12391],[-74.828408,40.12031],[-74.832808,40.11171],[-74.835108,40.10391],[-74.838008,40.10091],[-74.843408,40.09771],[-74.851108,40.09491],[-74.854409,40.09311],[-74.856509,40.09131],[-74.858209,40.08881],[-74.859809,40.08491],[-74.860909,40.08371],[-74.863809,40.08221],[-74.880209,40.07881],[-74.88781,40.07581],[-74.909011,40.07021],[-74.911911,40.06991],[-74.920811,40.07111],[-74.925311,40.07071],[-74.932211,40.068411],[-74.944412,40.063211],[-74.974713,40.048711],[-74.983913,40.042711],[-74.989914,40.037311],[-75.007914,40.023111],[-75.011115,40.021311],[-75.015515,40.019511],[-75.039316,40.013012],[-75.047016,40.008912],[-75.051217,40.004512],[-75.059017,39.992512],[-75.072017,39.980612],[-75.088618,39.975212],[-75.093718,39.974412],[-75.108119,39.970312],[-75.11922,39.965412],[-75.12692,39.961112],[-75.13012,39.958712],[-75.13352,39.954412],[-75.13572,39.947112],[-75.13612,39.933912],[-75.13502,39.927312],[-75.13282,39.921612],[-75.13012,39.917013],[-75.12792,39.911813],[-75.13082,39.900213],[-75.13342,39.896213],[-75.140221,39.888213],[-75.145421,39.884213],[-75.150721,39.882713],[-75.183023,39.882013],[-75.189323,39.880713],[-75.195324,39.877013],[-75.210425,39.865913],[-75.221025,39.861113],[-75.235026,39.856613],[-75.243431,39.854597],[-75.271159,39.84944],[-75.293376,39.848782],[-75.309674,39.850179],[-75.323232,39.849812],[-75.330433,39.849012],[-75.341765,39.846082],[-75.3544,39.839917],[-75.371835,39.827612],[-75.390536,39.815312],[-75.403737,39.807512],[-75.415041,39.801786],[-75.428038,39.809212],[-75.45374,39.820312],[-75.463341,39.823812],[-75.481242,39.829112],[-75.498843,39.833312],[-75.518444,39.836311],[-75.539346,39.838211],[-75.570464,39.839007],[-75.579849,39.838526],[-75.593666,39.837455],[-75.617251,39.833999],[-75.634706,39.830164],[-75.641518,39.828363],[-75.662822,39.82115],[-75.685991,39.811054],[-75.701208,39.802606],[-75.716969,39.791998],[-75.727049,39.784126],[-75.736489,39.775759],[-75.744394,39.767855],[-75.753066,39.757631],[-75.760346,39.747231],[-75.766058,39.737811],[-75.773558,39.722411],[-75.788359,39.721811],[-75.998649,39.721576],[-76.013067,39.72192],[-76.233259,39.721305],[-76.715594,39.721103],[-76.8901,39.720401],[-76.936601,39.720701],[-76.990903,39.7198],[-77.058204,39.7202],[-77.534758,39.720134],[-77.724115,39.720894],[-77.874719,39.722219],[-78.330715,39.722689],[-78.337111,39.722461],[-78.438839,39.722481],[-78.461422,39.722869],[-78.537702,39.72249],[-78.546415,39.722869],[-78.575893,39.722561],[-78.723529,39.723043],[-79.045548,39.722883],[-79.548465,39.720778],[-79.610623,39.721245],[-79.763774,39.720776],[-79.916171,39.720893]]]},\"properties\":{\"name\":\"Pennsylvania\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4826","contributors":{"authors":[{"text":"Busch, W. F.","contributorId":67968,"corporation":false,"usgs":true,"family":"Busch","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":244886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaw, E.C.","contributorId":94737,"corporation":false,"usgs":true,"family":"Shaw","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":244887,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":52183,"text":"ofr6180 - 1961 - Hydrology of radioactive waste disposal at the Idaho Chemical Processing Plant National Reactor Testing Station, Idaho","interactions":[],"lastModifiedDate":"2013-11-26T11:28:10","indexId":"ofr6180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-80","title":"Hydrology of radioactive waste disposal at the Idaho Chemical Processing Plant National Reactor Testing Station, Idaho","language":"English","doi":"10.3133/ofr6180","usgsCitation":"Jones, P., 1961, Hydrology of radioactive waste disposal at the Idaho Chemical Processing Plant National Reactor Testing Station, Idaho: U.S. Geological Survey Open-File Report 61-80, 8 p., https://doi.org/10.3133/ofr6180.","productDescription":"8 p.","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":176727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Idaho","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f22","contributors":{"authors":[{"text":"Jones, P.H.","contributorId":50963,"corporation":false,"usgs":true,"family":"Jones","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":244923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52188,"text":"ofr6192 - 1961 - Studies of the hydrology of the lower Colorado River area","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr6192","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-92","title":"Studies of the hydrology of the lower Colorado River area","language":"ENGLISH","doi":"10.3133/ofr6192","usgsCitation":"McDonald, C.C., 1961, Studies of the hydrology of the lower Colorado River area: U.S. Geological Survey Open-File Report 61-92, 8 p., https://doi.org/10.3133/ofr6192.","productDescription":"8 p.","costCenters":[],"links":[{"id":176827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dc9","contributors":{"authors":[{"text":"McDonald, C. C.","contributorId":69204,"corporation":false,"usgs":true,"family":"McDonald","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":244929,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68695,"text":"ha41 - 1961 - Floods at Boulder, Colorado","interactions":[{"subject":{"id":52181,"text":"ofr6177 - 1961 - Preliminary report on floods on Boulder Creek below Boulder, Colorado","indexId":"ofr6177","publicationYear":"1961","noYear":false,"title":"Preliminary report on floods on Boulder Creek below Boulder, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":68695,"text":"ha41 - 1961 - Floods at Boulder, Colorado","indexId":"ha41","publicationYear":"1961","noYear":false,"title":"Floods at Boulder, Colorado"},"id":1}],"lastModifiedDate":"2012-02-02T00:13:36","indexId":"ha41","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"41","title":"Floods at Boulder, Colorado","language":"ENGLISH","doi":"10.3133/ha41","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Floods at Boulder, Colorado: U.S. Geological Survey Hydrologic Atlas 41, 3 col. maps ;30 x 52 cm. on sheet 74 x 105 cm. folded to 26 x 19 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/ha41.","productDescription":"3 col. maps ;30 x 52 cm. on sheet 74 x 105 cm. folded to 26 x 19 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":188615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90417,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"6000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e7097","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":534515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52204,"text":"ofr61120 - 1961 - Hydrology of the Babylon-Islip area, Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr61120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-120","title":"Hydrology of the Babylon-Islip area, Suffolk County, Long Island, New York","language":"ENGLISH","doi":"10.3133/ofr61120","usgsCitation":"Pluhowski, E., and Kantrowitz, I., 1961, Hydrology of the Babylon-Islip area, Suffolk County, Long Island, New York: U.S. Geological Survey Open-File Report 61-120, 118 p., https://doi.org/10.3133/ofr61120.","productDescription":"118 p.","costCenters":[],"links":[{"id":175698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601eef","contributors":{"authors":[{"text":"Pluhowski, E.J.","contributorId":52244,"corporation":false,"usgs":true,"family":"Pluhowski","given":"E.J.","affiliations":[],"preferred":false,"id":244966,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kantrowitz, I.H.","contributorId":15646,"corporation":false,"usgs":true,"family":"Kantrowitz","given":"I.H.","affiliations":[],"preferred":false,"id":244965,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68391,"text":"ha43 - 1961 - Floods at Springfield, Ohio, in 1913 and 1959","interactions":[],"lastModifiedDate":"2012-02-10T00:11:27","indexId":"ha43","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"43","title":"Floods at Springfield, Ohio, in 1913 and 1959","language":"ENGLISH","doi":"10.3133/ha43","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Floods at Springfield, Ohio, in 1913 and 1959: U.S. Geological Survey Hydrologic Atlas 43, 1 map :col. ;76 x 78 cm., https://doi.org/10.3133/ha43.","productDescription":"1 map :col. ;76 x 78 cm.","costCenters":[],"links":[{"id":185620,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89891,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/043/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.86749999999999,39.8675 ], [ -83.86749999999999,40 ], [ -83.75,40 ], [ -83.75,39.8675 ], [ -83.86749999999999,39.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7221","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":534508,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52228,"text":"ofr6228 - 1961 - Geologic summary of the Appalachian Basin, with reference to the subsurface disposal of radioactive waste solutions","interactions":[],"lastModifiedDate":"2018-10-03T09:24:58","indexId":"ofr6228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"62-28","title":"Geologic summary of the Appalachian Basin, with reference to the subsurface disposal of radioactive waste solutions","docAbstract":"The Appalachian basin is an elongate depression in the crystalline basement complex which contains a great volume of predominantly sedimentary stratified rocks. As defined in this paper it extends from the Adirondack Mountains in New York to central Alabama. From east to west it extends from the west flank of the Blue Ridge Mountains to the crest of the Findlay and Cincinnati arches and the Nashville dome. It encompasses an area of about 207,000 square miles, including all of West Virginia and parts of New York, New Jersey, Pennsylvania, Ohio, Maryland, Virginia, Kentucky, Tennessee, North Carolina, Georgia, and Alabama.
The stratified rocks that occupy the basin constitute a wedge-shaped mass whose axis of greatest thickness lies close to and parallel to the east edge of the basin. The maximum thickness of stratified rocks preserved in any one part of the basin today is between 35,000 and 40,000 feet. The volume of the sedimentary rocks is approximately 510,000 cubic miles and of volcanic rocks is a few thousand cubic miles. The sedimentary rocks are predominantly Paleozoic in age, whereas the volcanic rocks are predominantly Late Precambrian.
On the basis of gross lithology the stratified rocks overlying the crystalline basement complex can be divided into nine vertically sequential units, which are designated \"sequences\" in this report. The boundaries between contiguous sequences do not necessarily coincide with the commonly recognized boundaries between systems or series. All sequences are grossly wedge shaped, being thickest along the eastern margin of the basin and thinnest along the western margin.
The lowermost unit the Late Precambrian stratified sequence is present only along part of the eastern margin of the basin, where it lies unconformably on the basement complex. It consists largely of volcanic tuffs and flows but contains some interbedded sedimentary rocks. The Late Precambrian sequence is overlain by the Early Cambrian clastic sequence. Where the older sequence is absent, the Early Cambrian sequence rests on the basement complex. Interbedded fine- to coarse-grained noncarbonate detrital rocks comprise the bulk of the sequence, but some volcanic and carbonate rocks are included. Next above is the Cambrian-Ordovician carbonate sequence which consists largely of limestone and dolomite. Some quartzose sandstone is present in the lower part in the western half of the basin, and much shale is present in the upper part in the southeast part of the basin. The next higher sequence is the Late Ordovician clastic sequence, which consists largely of shale, siltstone, and sandstone. Coarse-grained light-gray to red rocks are common in the sequence along the eastern side of the basin, whereas fine-grained dark-gray to black calcareous rocks are common along the west side. The Late Ordovician clastic sequence is overlain unconformably in many places by the Early Silurian clastic sequence. The latter comprises a relatively thin wedge of coarse-grained clastic rocks. Some of the most prolific oil- and gas-producing sandstones in the Appalachian basin are included. Among these are the \"Clinton\" sands of Ohio, the Medina Sandstones of New York and Pennsylvania, and the Keefer or \"Big Six\" Sandstone of West Virginia and Kentucky. Conformably overlying the Early Silurian clastic sequence is the Silurian-Devonian carbonate sequence, which consists predominantly of limestone and dolomite. It also contains a salt-bearing unit in the north-central part of the basin and a thick wedge of coarse-grained red beds in the northeastern part. The sequence is absent in much of the southern part of the basin. Large volumes of gas and much oil are obtained from some of its rocks, especially from the Oriskany Sandstone and the Huntersville Ghert. The Silurian-Devonian carbonate sequence is abruptly overlain by the Devonian clastic sequence a thick succession of interbedded shale, mudrock, siltstone, and sandstone. Colors range from predominantly purple and red in the northeastern part of the basin to predominantly dark gray and black in the southwestern part. Many rocks in the upper part contain hydrocarbons in commercial quantities. The next higher sequence is a heterogeneous succession that comprises most rocks of Mississippian age in the basin. It is composed largely of fine-grained to very coarse-grained noncalcareous clastic rocks in the northern half of the basin, and largely of carbonate rocks in the southern part. Large quantities of oil and gas are produced from the sequence. The youngest sequence consists of coarse-grained clastic rocks largely of Pennsylvanian age. In the center of the basin a relatively small volume of lithologically similar rocks of Permian age are included. The sequence has been intensively mined for coal throughout most of its extent.
The waste-disposal possibilities of the stratified rocks in the Appalachian basin are considered in terms of the following: 1) gross lithology of the sequences; 2) general lithology of the rock units composing the sequences; and 3) the structural attitudes of the sequences in different parts of the basin. The degree of exploitation of economically significant mineral* resources is considered briefly where such exploitation may affect waste-disposal possibilities. Hydrologic aspects are not in general considered. Based largely on consideration of the above geologic factors the following types of reservoirs associated with particular geologic environments offer some prospects for the disposal of radioactive waste solutions. They are: 1) artificially created cavities in thick salt beds; 2) artificially fractured thin lenticular sandstone bodies isolated in shale or mudrock sequences; 3) portions of thick noncarbonate clastic sequences possessing appreciable natural porosity and permeability; 4) thin clastic units (with natural or artificially created openings) in the plate of a thrust fault overlain by impermeable strata.
Considered in its entirety the Late Ordovician clastic sequence appears to have a greater number of favorable geologic factors for waste-disposal purposes than the others. The Early Silurian clastic sequence, the Silurian-Devonian carbonate sequence, and the Devonian clastic sequence offer fewer possibilities. The Late Precambrian stratified sequence, Early Cambrian, and the Cambrian-Ordovician carbonate sequence offer few possibilities. The Mississippian and Pennsylvanian sequences appear to be generally unsuitable.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ofr6228","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Colton, G.W., 1961, Geologic summary of the Appalachian Basin, with reference to the subsurface disposal of radioactive waste solutions: U.S. Geological Survey Open-File Report 62-28, Report: 121 p.; 15 Maps; 1 Illustration, https://doi.org/10.3133/ofr6228.","productDescription":"Report: 121 p.; 15 Maps; 1 Illustration","costCenters":[],"links":[{"id":86729,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86730,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0028/report-thumb.jpg"},{"id":86731,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86732,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86733,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86734,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86735,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86736,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86737,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86738,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86739,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86740,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86741,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86742,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86743,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86744,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86745,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0028/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Appalachian Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.71,35.8 ], [ -84.71,43.91 ], [ -74.13,43.91 ], [ -74.13,35.8 ], [ -84.71,35.8 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688132","contributors":{"authors":[{"text":"Colton, George Willis","contributorId":12015,"corporation":false,"usgs":true,"family":"Colton","given":"George","email":"","middleInitial":"Willis","affiliations":[],"preferred":false,"id":244999,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68664,"text":"ha11 - 1961 - Precipitation, water loss, and runoff in the Delaware River basin and New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:13:41","indexId":"ha11","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"11","title":"Precipitation, water loss, and runoff in the Delaware River basin and New Jersey","language":"ENGLISH","doi":"10.3133/ha11","usgsCitation":"Hely, A.G., Nordenson, T.J., and and others, 1961, Precipitation, water loss, and runoff in the Delaware River basin and New Jersey: U.S. Geological Survey Hydrologic Atlas 11, 1 map :illus., maps (part col.) ;69 cm., https://doi.org/10.3133/ha11.","productDescription":"1 map :illus., maps (part col.) ;69 cm.","costCenters":[],"links":[{"id":186048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db6808b8","contributors":{"authors":[{"text":"Hely, Allen Grant","contributorId":41902,"corporation":false,"usgs":true,"family":"Hely","given":"Allen","email":"","middleInitial":"Grant","affiliations":[],"preferred":false,"id":278668,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nordenson, T. J.","contributorId":95116,"corporation":false,"usgs":true,"family":"Nordenson","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":534512,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":66034,"text":"i330 - 1961 - Geology of the Moses Lake North quadrangle, Washington","interactions":[],"lastModifiedDate":"2013-12-13T16:26:47","indexId":"i330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"330","title":"Geology of the Moses Lake North quadrangle, Washington","docAbstract":"The geology of the Moses Lake North quadrangle was mapped in 1954 and 1958 by the U.S. Geological Survey. Some of the basic hydrologic data has been collected by the Geological Survey during the early investigations of ground-water conditions in the Quincy Basin (Henshaw, written communication, 1917; Schwennesen and Meinzer, 1918). Most of the data, however, were obtained by the Geological Survey since 1941, in cooperation with the U.S. Bureau of Reclamation and the Washington State Department of Conservation under continuing programs in the area of the Columbia Basin Project of the Bureau of Reclamation. Some preliminary geologic field work in the Moses Lake North quadrangle was done by the Geological Survey in 1954 in cooperation with the Washington State Department of Conservation.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/i330","collaboration":"Prepared in cooperation with the Washington State Department of Conservation","usgsCitation":"Grolier, M.J., and Foxworthy, B.L., 1961, Geology of the Moses Lake North quadrangle, Washington: U.S. Geological Survey IMAP 330, Plate: 37.73 x 40.60 inches, https://doi.org/10.3133/i330.","productDescription":"Plate: 37.73 x 40.60 inches","costCenters":[],"links":[{"id":102912,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1379.htm","linkFileType":{"id":5,"text":"html"},"description":"1379"},{"id":189540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0330/report-thumb.jpg"},{"id":279958,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0330/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Washington","otherGeospatial":"Moses Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.375,47.125 ], [ -119.375,47.25 ], [ -119.25,47.25 ], [ -119.25,47.125 ], [ -119.375,47.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e98d","contributors":{"authors":[{"text":"Grolier, Maurice J.","contributorId":98292,"corporation":false,"usgs":true,"family":"Grolier","given":"Maurice","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":273889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foxworthy, Bruce L.","contributorId":88815,"corporation":false,"usgs":true,"family":"Foxworthy","given":"Bruce","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":273888,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2372,"text":"wsp1587 - 1961 - Water resources of the Raft River basin, Idaho-Utah","interactions":[{"subject":{"id":51728,"text":"ofr54219 - 1954 - Ground-water resources of the Raft River basin, Cassia County, Idaho - a summary of unpublished data","indexId":"ofr54219","publicationYear":"1954","noYear":false,"title":"Ground-water resources of the Raft River basin, Cassia County, Idaho - a summary of unpublished data"},"predicate":"SUPERSEDED_BY","object":{"id":2372,"text":"wsp1587 - 1961 - Water resources of the Raft River basin, Idaho-Utah","indexId":"wsp1587","publicationYear":"1961","noYear":false,"title":"Water resources of the Raft River basin, Idaho-Utah"},"id":1}],"lastModifiedDate":"2022-12-19T21:20:39.37645","indexId":"wsp1587","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1587","title":"Water resources of the Raft River basin, Idaho-Utah","docAbstract":"Much arable land in the Raft River basin of Idaho lacks water for irrigation, and the potentially irrigable acreage far exceeds the amount that could be irrigated with the estimated total supply of water. Therefore, the amount of uncommitted water that could be intercepted and used within the basin is the limiting factor in further development of its native water supply. Water for additional irrigation might be obtained by constructing surface-storage works, by pumping ground water, or by importing surface water. Additional groundwater development is feasible. As an aid to orderly development and use of the water supplies, the report summarizes available geologic and hydrologic data and, by analysis and interpretation, derives an estimate of the recoverable water yield of the basin.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1587","collaboration":"Prepared in cooperation with the Idaho Department of Reclamation","usgsCitation":"Nace, R.L., 1961, Water resources of the Raft River basin, Idaho-Utah: U.S. Geological Survey Water Supply Paper 1587, Report: vi, 138 p.; 6 Plates: 29.00 x 60.00 inches or smaller, https://doi.org/10.3133/wsp1587.","productDescription":"Report: vi, 138 p.; 6 Plates: 29.00 x 60.00 inches or smaller","numberOfPages":"144","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":410736,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24773.htm","linkFileType":{"id":5,"text":"html"}},{"id":28323,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Provisional water-yield map of the Raft River basin, Idaho-Utah"},{"id":28322,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Provisional isohyetal map of the Raft River basin, Idaho-Utah"},{"id":28321,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Generalized geologic map of Raft River basin, Idaho-Utah"},{"id":28327,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1587/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1587/report-thumb.jpg"},{"id":28326,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Pumping rates, in cubic feet per second, of irrigation wells in the Raft River valley, Idaho"},{"id":28325,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Water table contours in the Raft River valley and northern plains section, October-November 1952"},{"id":28324,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1587/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Location of wells and stream-measuring stations in the Raft River basin, Idaho-Utah"}],"country":"United States","state":"Idaho, Utah","otherGeospatial":"Raft River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -113,\n 42.683\n ],\n [\n -113.844,\n 42.683\n ],\n [\n -113.844,\n 41.76\n ],\n [\n -113,\n 41.76\n ],\n [\n -113,\n 42.683\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fab62","contributors":{"authors":[{"text":"Nace, Raymond L.","contributorId":93460,"corporation":false,"usgs":true,"family":"Nace","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}