The data in the following tables were abstracted from measurements of physical properties of evaporite minerals or of equivalent synthetic compounds. The compounds considered are the halide and sulfate salts which supposedly precipitated from evaporating ocean water and which form very extensive and thick \"rock salt\" beds. These beds are composed almost entirely of NaCl. In places where the beds are deeply buried and where fractures occur in the overlying rocks, the salt is plastically extruded upward as in a pipe to form the \"salt domes\".
\n\nMost of the tables are for NaCl, both the natural (halite) and the synthetic salt, polycrystalline and single crystals. These measurements have been collected for use 1) in studies on storage of radioactive wastes in salt domes or beds, 2) in calculations concerned with nuclear tests in salt domes and beds, and 3) in studies of phenomena in salt of geologic interest.
\n\nRather than an exhaustive compilation of physical property measurements, there tables represent a summary of data from accessible sources. As limitations of time have presented making a more systematic and comprehensive selection, the data given may seem arbitrarily chosen. Some of the data listed are old, and newer, more accurate data are undoubtedly available.
\nHalite (an synthetic NaCl) has been very thoroughly studied because of its relatively simple and highly symmetrical crystal structure, its easy availability naturally or synthetically, both in single crystals and polycrystalline, its useful and scientifically interesting properties, and its role as a compound of almost purely ionic bonding. The measurements of NaCl in the tables, however, represent only a small part of the total number of observations; discrimination was necessary to keep the size of the tabulations manageable. The physical properties of the evaporite minerals other than halite and sylvite have received only desultory attention of experiementalists, and appear in only a few tables.
\nThe effects of temperature, hydrostatic pressure, stress difference, and other mechanical, eletrical, and optical conditions on the physical properties have probably been observed more completely on NaCl than on any other solid substance, which makes it a unique and important substance. Several new and important phenomena have been observed first on it. The mechanical properties of NaCl, for example, depend very strongly on the condition and the composition of the gas or liquid in contact with the sample surface; the data are sparse as yet and are not reported here.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei821","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Robertson, E.C., 1962, Physical properties of evaporite minerals: U.S. Geological Survey Trace Elements Investigations 821, 90 p., https://doi.org/10.3133/tei821.","productDescription":"90 p.","numberOfPages":"90","costCenters":[],"links":[{"id":288266,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288265,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0821/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5385b3fbe4b09e18fc023a7b","contributors":{"authors":[{"text":"Robertson, Eugene C.","contributorId":71139,"corporation":false,"usgs":true,"family":"Robertson","given":"Eugene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":284738,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220651,"text":"70220651 - 1962 - Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid","interactions":[],"lastModifiedDate":"2021-05-24T11:47:18.288311","indexId":"70220651","displayToPublicDate":"1962-01-01T06:43:05","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid","docAbstract":"Geological and experimental evidence indicate that the three-phase field, plagioclase-alkalifeldspar-liquid, may terminate in several different ways. The possible terminations have been developed from Schreinemakers' rules governing the disappearance of three-phase fields. In igncous rocks, these different terminations may arise from variations in the relative amounts of additional components in magmas, or from changes of total pressure, or from structural changes that effect the extent of solid solution in feldspar.The three-phase region originates from the intersection of the solidus and the feldspar solvus. The available evidence regarding this intersection is reviewed, as is the evidence for the existence and form of the boundary curve on the feldspar liquidus. The data are used to project a series of isobaric polythermal and isobaric isothermal diagrams for each possible termination. Subsequent discussions relate the theoretical arguments to the natural evidence, suggest the more probable geological environments of some of the terminations, and indicate characteristic features of each termination.It may be possible to identify the type of termination involved in the crystallization of some rocks. The necessary data are the amounts and compositions of both kinds of coexisting feldspars and of the feldspar components of the coexisting liquid at one or more stages of the crystallization process. Volcanic rocks are most suitable for such studies.The terminations explain many of the compositional relationships possible between feldspar crystals and silicate melt under geological and experimental conditions. These compositional relationships are fundamental to understanding the crystallization of igneous rocks and the formation of melts by partial fusion. Other geological applications include a simple explanation for some resorbed feldspars, the separation, correlation, and comparison of porphyritic rock units, interpretation of compositional changes of successive zones of zoned feldspars, and mantling of one feldspar by another. With all types of termination, extensive fractionation yields a liquid rich in Or and Ab that may crystallize to alkali feldspar or feldspars.
","language":"English","publisher":"Oxford University Press","doi":"10.1093/petrology/3.3.280","usgsCitation":"Stewart, D.B., and Roseboom, E.H., 1962, Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid: Journal of Petrology, v. 3, no. 3, p. 280-315, https://doi.org/10.1093/petrology/3.3.280.","productDescription":"36 p.","startPage":"280","endPage":"315","costCenters":[],"links":[{"id":385877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stewart, D. B.","contributorId":41809,"corporation":false,"usgs":true,"family":"Stewart","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":816300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roseboom, E. H. Jr.","contributorId":40730,"corporation":false,"usgs":true,"family":"Roseboom","given":"E.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":816301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61978,"text":"mr27 - 1962 - Magnesite and brucite in the United States, exclusive of Alaska and Hawaii","interactions":[{"subject":{"id":45985,"text":"ofr6156 - 1961 - Magnesite and brucite in the United States","indexId":"ofr6156","publicationYear":"1961","noYear":false,"title":"Magnesite and brucite in the United States"},"predicate":"SUPERSEDED_BY","object":{"id":61978,"text":"mr27 - 1962 - Magnesite and brucite in the United States, exclusive of Alaska and Hawaii","indexId":"mr27","publicationYear":"1962","noYear":false,"title":"Magnesite and brucite in the United States, exclusive of Alaska and Hawaii"},"id":1}],"lastModifiedDate":"2023-01-24T19:21:38.71232","indexId":"mr27","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"27","title":"Magnesite and brucite in the United States, exclusive of Alaska and Hawaii","docAbstract":"The important deposits of magnesite (MgCO3) and brucite (MgO.H2O) in the United States (exclusive of Alaska and Hawaii) are shown on the accompanying map. Single deposits and groups of deposits are shown by geometric symbols according to four size categories based on estimated production plus reserves. These categories are: less than 10,000 tons, 10,000 to 100,000 tons, 100,000 to 1,000,000 tons, and more than 1,000,000 tons. Occurrences of mineralogic interest only are not shown. All map locations are numbered consecutively in each State and keyed to the locality index. The geographical coordinates in the locality index represent the centers of the geometric symbols. Thus, the same coordinates are assigned to all deposits covered by a group symbol.
The map was compiled from published reports and data in the files of the United States Geological Survey. The names, geographic coordinates, and geologic types of deposits are given in the locality index. The principal published reports used in compiling the map are listed in the selected references.
The main types of commercial deposits of magnesite in the United States are: (1) replacement bodies in limestone and dolomite; (2) replacements and veins in serpentine; and (3) sedimentary beds. Other magnesite deposits of varied origin and less common occurrence include beds associated with talc, chlorite, and mica schists; and veins and lenses in altered tuffs.
Brucite is a relatively rare mineral of secondary origin which usually accompanies other magnesian minerals, particularly magnesite and hydromagnesite, and is associated with carbonate rocks and serpentine.
Magnesite was first mined in California in 1886, and the State was the only domestic producer until the development of the Washington deposits began in 1916. In recent years, the main production of magnesite has been from Stevens County, Washington, and Nye County, Nevada. Production in California has been intermittent since 1945. Magnesite deposits in Texas were mined during and immediately after World War II. At present (1961) the only brucite deposits being worked are those at Gabbs, Nye County, Nevada. They have been mined almost continuously since 1935.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mr27","usgsCitation":"Gildersleeve, B., 1962, Magnesite and brucite in the United States, exclusive of Alaska and Hawaii: U.S. Geological Survey Mineral Investigations Resource Map 27, Report: 4 p.; 1 Plate: 63.55 x 40.06 inches, https://doi.org/10.3133/mr27.","productDescription":"Report: 4 p.; 1 Plate: 63.55 x 40.06 inches","costCenters":[],"links":[{"id":412282,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/27/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":412281,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mr/27/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179997,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mr/27/report-thumb.jpg"}],"scale":"3168000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.25,24.25 ], [ -127.25,49.25 ], [ -66.5,49.25 ], [ -66.5,24.25 ], [ -127.25,24.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64924b","contributors":{"authors":[{"text":"Gildersleeve, Benjamin","contributorId":14468,"corporation":false,"usgs":true,"family":"Gildersleeve","given":"Benjamin","email":"","affiliations":[],"preferred":false,"id":266643,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009799,"text":"70009799 - 1962 - Behaviour of calcium carbonate in sea water","interactions":[],"lastModifiedDate":"2020-09-09T13:46:35.413922","indexId":"70009799","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Behaviour of calcium carbonate in sea water","docAbstract":"Anomalies in the behaviour of calcium carbonate in natural solutions diminish when considered in context. Best values found by traditional oceanographie methods for the apparent solubility product constant K'CaCO3 in sea water at atmospheric pressure are consistent mineralogically—at 36 parts per thousand salinity and T-25°C, K'aragonlte is estimated as 1.12 × 10−6 and K'calcite as 0.61 × 10−6. At 30°C the corresponding values are 0.98 × 10−6 for aragonite and 0.53 × 10−6 for calcite. Because the K' computations do not compensate for ionic activity, however, they cannot give thermodynamically satisfactory results. It is of interest, therefore, that approximate methods and information now available permit the estimation from the same basic data of an activity product constant KCaCO3 close to that found in solutions to which Debye-Hückel theory applies. Such methods indicate approximate Karagonite 7.8 × 10−9 for surface sea water at 29°C; Kcalcite would be proportionately lower.
Field data and experimental results indicate that the mineralogy of precipitated CaCO3 depends primarily on degree of supersaturation, thus also on kinetic or biologic factors that facilitate or inhibit a high degree of supersaturation. The shallow, generally hypersaline bank waters west of Andros Island yield aragonitic sediments with
Aragonitc of marine origin persists in contact with supersaturated interstitial solutions at ordinary temperature and pressure. Conversion to calcite follows transfer to solutions undersaturated with respect to aragonite or upon exposure to the moist atmosphere.
This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources and (2) to supplement an interpretive report that will be published later.
Records were collected during the period 1956-59 by the U.S. Geological Survey in cooperation with the Utah State Engineer as a part of the investigation of the ground-water resources of northern Utah Walley in Utah County, Utah. Some earlier data and other information in the tables are from published reports on the ground-water resources of northern Utah Walley. The interpretive material will be published cooperatively by the U.S. Geological Survey and the Utah State Engineer in a companion report by Seymour Subitzky.
This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells as shown on the tables. From tables 1, 2, and h he can note the type of material that yields water to wells in the vicinity; from table 2 he can note (1) the depth and diameter of wells in the vicinity and the yield of some of those wells, and (2) the depth to water or the feet of water pressure in the vicinity; from table 3 and plate 1 he may note the location of springs and the conditions related to the occurrence of these springs; and from tables 5 and 6 he may note the chemical quality of the water from wells and from some surface sources, and the uses of these waters. If the reader decides from his examination that conditions are favorable, he may place an application to drill a well with the State Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.
The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Subitsky, S., 1962, Records of selected wells and springs, selected drillers' logs of wells, and chemical analyses of ground and surface waters, northern Utah Valley, Utah County, Utah: Utah Basic-Data Report 2, 14 p.","productDescription":"14 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345756,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345754,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-040&Title=Basic+Data+Report+2"}],"country":"United States","state":"Utah","county":"Utah County","otherGeospatial":"Utah Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ce4b091459a57823e","contributors":{"authors":[{"text":"Subitsky, Seymour","contributorId":77227,"corporation":false,"usgs":true,"family":"Subitsky","given":"Seymour","email":"","affiliations":[],"preferred":false,"id":710415,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70045415,"text":"wdrCO621 - 1962 - Surface Water Records of Colorado","interactions":[],"lastModifiedDate":"2013-05-22T14:43:50","indexId":"wdrCO621","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CO-62-1","title":"Surface Water Records of Colorado","docAbstract":"The surface-water records for the 1962 water year for gaging stations and miscellaneous sites within the State of Colorado are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of J. W. Odell, district engineer, Surface Water Branch.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/wdrCO621","collaboration":"Prepared in cooperation with Colorado Water Conservation Board, Office of the State Engineer, Southeastern Colorado Water Conservancy District, Arkansas River Compact Administration, Colorado Agricultural Experiment Station, Colorado River Water Conservation District, County of Boulder, Board of County Cotmnissioners, City and County of Denver Board of Water Conunissioners, City of ·Colorado Springs Department of Public Utilities, U.S. Army Corps of Engineers, U.S. Bureau of Reclamation, U.S. Soil Conservation Service","usgsCitation":"U.S. Geological Survey, W.R., 1962, Surface Water Records of Colorado: U.S. Geological Survey Water Data Report CO-62-1, xii, 335 p., https://doi.org/10.3133/wdrCO621.","productDescription":"xii, 335 p.","numberOfPages":"356","additionalOnlineFiles":"N","temporalStart":"1961-10-01","temporalEnd":"1962-09-30","costCenters":[],"links":[{"id":272538,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1962/co-62/report.pdf"},{"id":270918,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1962/co-62/report-thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.000,37.0000 ], [ -109.000,41.0000 ], [ -102.000,41.0000 ], [ -102.000,37.0000 ], [ -109.000,37.0000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"516d216ce4b0411d430a8a31","contributors":{"authors":[{"text":"U.S. Geological Survey, Water Resources Division","contributorId":102359,"corporation":false,"usgs":true,"family":"U.S. Geological Survey","given":"Water","email":"","middleInitial":"Resources Division","affiliations":[],"preferred":false,"id":477467,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010572,"text":"70010572 - 1962 - Elastic constants of calcite","interactions":[],"lastModifiedDate":"2020-09-17T19:49:47.39236","indexId":"70010572","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2171,"text":"Journal of Applied Physics","active":true,"publicationSubtype":{"id":10}},"title":"Elastic constants of calcite","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":70010573,"text":"70010573 - 1962 - Concentration method for the spectrochemical determination of seventeen minor elements in natural water","interactions":[],"lastModifiedDate":"2020-11-19T17:30:23.631193","indexId":"70010573","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Concentration method for the spectrochemical determination of seventeen minor elements in natural water","docAbstract":"A method for the quantitative spectrochemical determination of microgram amounts of 17 minor elements in water is given. The chelating reagents 8-quinolinol, tannic acid, and thionalide are utilized to concentrate traces (1 to 500 μg.) of aluminum, cobalt, chromium, copper, iron, gallium, germanium, manganese, nickel, titanium, vanadium, bismuth, lead, molybdenum, cadmium, zinc, and beryllium. Indium is added as a buffer, and palladium is used as an internal standard. The ashed oxides of these 17 metals are subsequently subjected to direct current arcing conditions during spectrum analysis. The method can be used to analyze waters with dissolved solids ranging from less than 100 to more than 100,000 p.p.m. There is no limiting concentration range for the determination of the heavy metals since any volume of sample can be used that will contain a heavy metal concentration within the analytical range of the method. Both the chemical and spectrographic procedures are described, and precision and accuracy data are given.
","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60187a021","usgsCitation":"Silvey, W., and Brennan, R., 1962, Concentration method for the spectrochemical determination of seventeen minor elements in natural water: Analytical Chemistry, v. 34, no. 7, p. 784-786, https://doi.org/10.1021/ac60187a021.","productDescription":"3 p.","startPage":"784","endPage":"786","numberOfPages":"3","costCenters":[],"links":[{"id":219021,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"7","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059f97ee4b0c8380cd4d62b","contributors":{"authors":[{"text":"Silvey, W. D.","contributorId":102914,"corporation":false,"usgs":true,"family":"Silvey","given":"W. D.","affiliations":[],"preferred":false,"id":359203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brennan, R.","contributorId":62572,"corporation":false,"usgs":true,"family":"Brennan","given":"R.","email":"","affiliations":[],"preferred":false,"id":359202,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70217326,"text":"wdrMDDE61 - 1961 - Surface water records of Maryland and Delaware, water year 1961","interactions":[],"lastModifiedDate":"2021-01-22T19:12:04.621675","indexId":"wdrMDDE61","displayToPublicDate":"2021-01-22T14:45:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MD-DE-61","displayTitle":"Surface Water Records of Maryland and Delaware, Water Year 1961","title":"Surface water records of Maryland and Delaware, water year 1961","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE61","usgsCitation":"U.S. Geological Survey, 1961, Surface water records of Maryland and Delaware, water year 1961: U.S. Geological Survey Water Data Report MD-DE-61, 102 p., https://doi.org/10.3133/wdrMDDE61.","productDescription":"102 p.","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia Water Science Center","active":true,"usgs":true}],"links":[{"id":382228,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1961/md-de-61/swrMDDE61_coverthb.jpg"},{"id":382229,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1961/md-de-61/swrMDDE61.pdf","text":"Report","size":"7.98 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Water Data Report MD-DE-61"}],"country":"United States","state":"Delaware, Maryland","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-75.564927,39.583248],[-75.576271,39.588144],[-75.579615,39.598656],[-75.565823,39.590608],[-75.564927,39.583248]]],[[[-75.55587,39.605824],[-75.561934,39.605216],[-75.570798,39.626768],[-75.559446,39.629812],[-75.55587,39.605824]]],[[[-75.594846,39.837286],[-75.539346,39.838211],[-75.498843,39.833312],[-75.45374,39.820312],[-75.405337,39.796213],[-75.437938,39.783413],[-75.459439,39.765813],[-75.474168,39.735473],[-75.47764,39.715013],[-75.488553,39.714833],[-75.496241,39.701413],[-75.509042,39.694513],[-75.509742,39.686113],[-75.529744,39.692613],[-75.562246,39.656712],[-75.587147,39.651012],[-75.614065,39.61832],[-75.611905,39.597568],[-75.563034,39.56224],[-75.570362,39.527223],[-75.560728,39.520472],[-75.566933,39.508273],[-75.576436,39.509195],[-75.587729,39.496353],[-75.593068,39.479186],[-75.589901,39.462022],[-75.570985,39.442486],[-75.57183,39.438897],[-75.538512,39.416502],[-75.512996,39.366153],[-75.494158,39.354613],[-75.491688,39.343963],[-75.439027,39.313384],[-75.435551,39.297546],[-75.427953,39.285049],[-75.402964,39.254626],[-75.405716,39.223834],[-75.396892,39.216141],[-75.393015,39.204512],[-75.39479,39.188354],[-75.408266,39.174625],[-75.410625,39.156246],[-75.401193,39.088762],[-75.402035,39.066885],[-75.387914,39.051174],[-75.345763,39.024857],[-75.318354,38.988191],[-75.311607,38.967637],[-75.311923,38.945917],[-75.302552,38.939002],[-75.312282,38.924594],[-75.304078,38.91316],[-75.190552,38.806861],[-75.160748,38.791224],[-75.134022,38.782242],[-75.113331,38.782998],[-75.097103,38.788703],[-75.093654,38.793992],[-75.097197,38.803101],[-75.093805,38.803812],[-75.089473,38.797198],[-75.082153,38.772157],[-75.06551,38.66103],[-75.048939,38.451263],[-75.06137,38.389466],[-75.085171,38.325096],[-75.092142,38.323252],[-75.102947,38.311525],[-75.192925,38.097819],[-75.241817,38.027802],[-75.624341,37.994211],[-75.633833,37.984519],[-75.628855,37.977798],[-75.630992,37.975667],[-75.638221,37.979397],[-75.648229,37.966775],[-75.647606,37.947027],[-75.655681,37.945435],[-75.669711,37.950796],[-75.663095,37.961195],[-75.671681,37.966576],[-75.71315,37.976623],[-75.737514,37.963705],[-75.759091,37.970663],[-75.783444,37.972565],[-75.831707,37.934789],[-75.860727,37.91831],[-75.885032,37.911717],[-75.892686,37.916848],[-75.898316,37.925114],[-75.894065,37.93079],[-75.890871,37.954847],[-75.898956,37.974514],[-75.875297,38.011965],[-75.87319,38.034375],[-75.858891,38.03839],[-75.847922,38.03437],[-75.830023,38.042845],[-75.812913,38.058932],[-75.819415,38.066606],[-75.844265,38.072272],[-75.858944,38.067323],[-75.859005,38.060717],[-75.871503,38.05887],[-75.880515,38.075011],[-75.86381,38.100968],[-75.837563,38.113753],[-75.827993,38.132803],[-75.843862,38.144599],[-75.868636,38.134381],[-75.900355,38.14115],[-75.936773,38.124355],[-75.936663,38.109956],[-75.945297,38.113091],[-75.958786,38.135572],[-75.947534,38.168274],[-75.951812,38.176053],[-75.942375,38.187066],[-75.888073,38.203813],[-75.878293,38.198407],[-75.864104,38.200858],[-75.848473,38.20934],[-75.851396,38.226432],[-75.874653,38.244514],[-75.887409,38.24208],[-75.885676,38.231006],[-75.894583,38.228439],[-75.90845,38.246648],[-75.911143,38.257951],[-75.938577,38.272329],[-75.954483,38.264366],[-75.954582,38.254108],[-75.940697,38.246902],[-75.946414,38.23889],[-75.970514,38.233668],[-75.964528,38.240692],[-75.963453,38.251793],[-75.984274,38.265155],[-75.990385,38.282915],[-76.007118,38.303994],[-76.016291,38.307206],[-76.009377,38.311997],[-75.969577,38.320044],[-75.964237,38.324285],[-75.961948,38.341431],[-75.973876,38.36585],[-76.001839,38.374343],[-76.011869,38.360582],[-76.010437,38.352504],[-76.016682,38.332429],[-76.041431,38.322163],[-76.049609,38.309348],[-76.05022,38.304101],[-76.030532,38.28796],[-76.028234,38.282035],[-76.043927,38.249712],[-76.032044,38.216684],[-76.05801,38.227079],[-76.069502,38.238455],[-76.074491,38.251148],[-76.09972,38.253647],[-76.107592,38.262525],[-76.102549,38.277153],[-76.111296,38.286946],[-76.137238,38.281648],[-76.166154,38.290431],[-76.180115,38.277019],[-76.175783,38.261551],[-76.164388,38.250061],[-76.146297,38.249678],[-76.126623,38.242949],[-76.125856,38.23888],[-76.131332,38.23288],[-76.151035,38.234215],[-76.17335,38.247037],[-76.188644,38.267434],[-76.190531,38.277139],[-76.211446,38.302656],[-76.226376,38.309988],[-76.243897,38.310313],[-76.258189,38.318373],[-76.266602,38.339502],[-76.264186,38.346436],[-76.259286,38.341619],[-76.238452,38.347986],[-76.23901,38.350738],[-76.249666,38.364214],[-76.273003,38.366483],[-76.281697,38.39147],[-76.28302,38.413512],[-76.331383,38.473323],[-76.33636,38.492235],[-76.327257,38.500121],[-76.318054,38.498199],[-76.289507,38.503906],[-76.263968,38.503452],[-76.247894,38.523019],[-76.244396,38.536966],[-76.253624,38.539393],[-76.278106,38.532468],[-76.281047,38.53613],[-76.275913,38.548809],[-76.27964,38.557231],[-76.289017,38.567982],[-76.308321,38.571769],[-76.273496,38.59139],[-76.268633,38.597753],[-76.279589,38.60952],[-76.271827,38.615661],[-76.264155,38.615109],[-76.23665,38.628598],[-76.231187,38.61401],[-76.212427,38.606738],[-76.174969,38.628791],[-76.160148,38.625452],[-76.147158,38.63684],[-76.154889,38.656268],[-76.174611,38.672811],[-76.199722,38.671127],[-76.212808,38.681892],[-76.237818,38.711762],[-76.238685,38.735434],[-76.255093,38.736476],[-76.270277,38.724385],[-76.271553,38.713576],[-76.275015,38.712714],[-76.298499,38.718005],[-76.298186,38.726255],[-76.316146,38.729586],[-76.330149,38.714682],[-76.333532,38.705063],[-76.321865,38.689512],[-76.322418,38.679304],[-76.33861,38.672023],[-76.34322,38.67688],[-76.347998,38.686234],[-76.340543,38.730338],[-76.341288,38.751505],[-76.334619,38.772911],[-76.323768,38.779287],[-76.310743,38.795996],[-76.308922,38.813346],[-76.301886,38.824595],[-76.277854,38.831256],[-76.271575,38.851771],[-76.264221,38.851572],[-76.265759,38.847638],[-76.250364,38.825438],[-76.221162,38.813052],[-76.198138,38.81444],[-76.19109,38.82966],[-76.202598,38.862616],[-76.200082,38.882885],[-76.205063,38.892726],[-76.203638,38.928382],[-76.213731,38.937269],[-76.232038,38.942518],[-76.250157,38.938667],[-76.249163,38.9218],[-76.255819,38.919008],[-76.262226,38.919976],[-76.273022,38.94184],[-76.29558,38.928855],[-76.299431,38.918542],[-76.293255,38.902582],[-76.308425,38.898404],[-76.317947,38.911312],[-76.336104,38.905977],[-76.338501,38.892474],[-76.331103,38.864686],[-76.340587,38.85574],[-76.348826,38.857134],[-76.35996,38.852586],[-76.368164,38.836194],[-76.375086,38.839474],[-76.376031,38.848777],[-76.364678,38.873831],[-76.365658,38.907477],[-76.361727,38.939175],[-76.353828,38.957234],[-76.323293,38.998767],[-76.320277,39.022998],[-76.311766,39.035257],[-76.302029,39.039571],[-76.302846,39.025828],[-76.29409,39.004263],[-76.278058,38.983246],[-76.258813,38.983664],[-76.229993,38.977728],[-76.218929,38.970538],[-76.20236,38.973079],[-76.164004,38.99953],[-76.163616,39.010057],[-76.184207,39.046264],[-76.175284,39.058805],[-76.15896,39.065486],[-76.145174,39.092824],[-76.183908,39.096344],[-76.203333,39.085654],[-76.212563,39.041641],[-76.208502,39.024818],[-76.200666,39.01452],[-76.209114,39.01001],[-76.231765,39.018518],[-76.242687,39.028926],[-76.231212,39.060769],[-76.233457,39.091385],[-76.260343,39.142722],[-76.278527,39.145764],[-76.274741,39.164961],[-76.251032,39.199214],[-76.219338,39.261997],[-76.211306,39.269761],[-76.203031,39.269871],[-76.181496,39.291797],[-76.176804,39.306229],[-76.186024,39.312462],[-76.186001,39.317814],[-76.170588,39.331954],[-76.159673,39.335909],[-76.145524,39.334399],[-76.133225,39.340491],[-76.136971,39.344414],[-76.13495,39.35107],[-76.116698,39.360744],[-76.110598,39.372119],[-76.049846,39.370644],[-76.02299,39.361896],[-76.002408,39.367501],[-76.002514,39.384805],[-76.035464,39.386176],[-76.040854,39.393594],[-76.035298,39.401609],[-76.00688,39.414527],[-75.996697,39.430549],[-75.982585,39.435287],[-75.977751,39.44302],[-75.976698,39.44569],[-75.990005,39.458646],[-75.998276,39.457182],[-76.002497,39.450231],[-76.009071,39.449256],[-76.01188,39.452524],[-75.99657,39.476658],[-75.986298,39.510398],[-75.976105,39.529876],[-75.966955,39.53865],[-75.970337,39.557637],[-75.992633,39.563098],[-75.999669,39.560488],[-76.006213,39.550546],[-76.063379,39.546638],[-76.096072,39.536912],[-76.116831,39.496882],[-76.11461,39.488619],[-76.100218,39.476918],[-76.073119,39.475331],[-76.060988,39.447775],[-76.081176,39.436712],[-76.102232,39.435659],[-76.146373,39.40531],[-76.157108,39.406176],[-76.171134,39.392588],[-76.180057,39.377638],[-76.226976,39.349908],[-76.243377,39.361808],[-76.266365,39.353352],[-76.253928,39.336768],[-76.262008,39.334708],[-76.276078,39.322908],[-76.281578,39.302108],[-76.296546,39.302383],[-76.291078,39.318108],[-76.298778,39.329208],[-76.295678,39.350008],[-76.322687,39.357092],[-76.341443,39.354217],[-76.334401,39.335222],[-76.338898,39.325783],[-76.327579,39.314108],[-76.339817,39.304216],[-76.355495,39.312155],[-76.36439,39.31184],[-76.380662,39.299161],[-76.384901,39.275928],[-76.395136,39.269293],[-76.402047,39.258783],[-76.386937,39.249216],[-76.38138,39.249508],[-76.38438,39.242708],[-76.393626,39.232012],[-76.41762,39.219838],[-76.425281,39.205708],[-76.441411,39.196049],[-76.46156,39.204947],[-76.488883,39.202208],[-76.497977,39.204697],[-76.519804,39.222946],[-76.535885,39.211008],[-76.533103,39.20763],[-76.534185,39.190608],[-76.525785,39.177908],[-76.508384,39.169408],[-76.500926,39.161286],[-76.484023,39.164407],[-76.475983,39.161109],[-76.471483,39.154709],[-76.428681,39.131709],[-76.432481,39.126709],[-76.432981,39.113209],[-76.42186,39.081442],[-76.423081,39.07421],[-76.438845,39.0529],[-76.405081,39.033211],[-76.394699,39.0132],[-76.421535,38.989524],[-76.448928,38.982823],[-76.454581,38.974512],[-76.474198,38.972647],[-76.471281,38.956512],[-76.451695,38.94249],[-76.46188,38.924013],[-76.459479,38.907113],[-76.46938,38.907613],[-76.46948,38.911513],[-76.475761,38.914469],[-76.49368,38.910013],[-76.49068,38.884814],[-76.519442,38.863135],[-76.516944,38.851157],[-76.509285,38.848388],[-76.496579,38.853115],[-76.489878,38.838715],[-76.509314,38.802328],[-76.525531,38.794043],[-76.535207,38.778298],[-76.559697,38.767443],[-76.557535,38.744687],[-76.544561,38.727784],[-76.52718,38.727062],[-76.532409,38.680064],[-76.525007,38.647568],[-76.511278,38.615745],[-76.51634,38.590229],[-76.517506,38.539149],[-76.506023,38.50461],[-76.492699,38.482849],[-76.455799,38.451233],[-76.450937,38.442422],[-76.415384,38.414682],[-76.40271,38.396003],[-76.388348,38.387781],[-76.386229,38.382013],[-76.387408,38.360811],[-76.40494,38.341089],[-76.409291,38.325891],[-76.402894,38.311402],[-76.382163,38.303389],[-76.374517,38.296556],[-76.394171,38.278233],[-76.399313,38.259398],[-76.385244,38.217751],[-76.353799,38.178606],[-76.329711,38.15519],[-76.320492,38.138966],[-76.337342,38.120696],[-76.329165,38.071247],[-76.319476,38.043315],[-76.321499,38.03805],[-76.332812,38.049938],[-76.350656,38.053277],[-76.361237,38.059542],[-76.370845,38.077771],[-76.393121,38.103142],[-76.405368,38.106974],[-76.421066,38.105989],[-76.439841,38.138933],[-76.459236,38.139471],[-76.469798,38.119264],[-76.46533,38.10583],[-76.473266,38.103035],[-76.501258,38.137744],[-76.514824,38.141219],[-76.52899,38.134708],[-76.54038,38.152991],[-76.552957,38.187209],[-76.588683,38.21295],[-76.673462,38.234401],[-76.740055,38.235227],[-76.752017,38.222409],[-76.778625,38.22847],[-76.79659,38.236531],[-76.811647,38.250129],[-76.805949,38.252275],[-76.802347,38.280743],[-76.824834,38.30113],[-76.845846,38.297783],[-76.846221,38.29196],[-76.841703,38.289768],[-76.834908,38.274299],[-76.842038,38.254657],[-76.864292,38.268945],[-76.920778,38.291529],[-76.922161,38.311086],[-76.929554,38.321088],[-76.975092,38.347067],[-76.983582,38.362999],[-76.98828,38.394975],[-77.016371,38.445572],[-77.042879,38.443607],[-77.074174,38.425479],[-77.091073,38.407546],[-77.106571,38.406237],[-77.123325,38.410646],[-77.128872,38.399692],[-77.139968,38.390102],[-77.184917,38.366559],[-77.205009,38.360511],[-77.216729,38.363159],[-77.250172,38.382781],[-77.264238,38.414282],[-77.259962,38.435821],[-77.274021,38.481127],[-77.263599,38.512344],[-77.237724,38.55187],[-77.221117,38.555217],[-77.183767,38.600699],[-77.169968,38.60674],[-77.148651,38.6056],[-77.129213,38.614306],[-77.12463,38.619778],[-77.135901,38.649817],[-77.132501,38.673816],[-77.1059,38.696815],[-77.079499,38.709515],[-77.053199,38.709915],[-77.045498,38.714315],[-77.041398,38.724515],[-77.040098,38.789913],[-76.910795,38.891712],[-77.040999,38.99511],[-77.1199,38.934311],[-77.146601,38.96421],[-77.221502,38.97131],[-77.228395,38.978404],[-77.231601,38.979917],[-77.234803,38.97631],[-77.249803,38.985909],[-77.248303,38.992309],[-77.255703,39.002409],[-77.244603,39.020109],[-77.246003,39.024909],[-77.274706,39.034091],[-77.293105,39.046508],[-77.340287,39.062991],[-77.38568,39.061987],[-77.46145,39.075151],[-77.4858,39.109303],[-77.519929,39.120925],[-77.524559,39.127821],[-77.527282,39.146236],[-77.510631,39.178484],[-77.478596,39.189168],[-77.47361,39.208407],[-77.457943,39.222023],[-77.46021,39.228359],[-77.486813,39.247586],[-77.540581,39.264947],[-77.560854,39.286152],[-77.561826,39.301913],[-77.566596,39.306121],[-77.592739,39.30129],[-77.615939,39.302722],[-77.650997,39.310784],[-77.675846,39.324192],[-77.692984,39.31845],[-77.727379,39.321666],[-77.759615,39.337331],[-77.759315,39.345314],[-77.74593,39.353221],[-77.743874,39.359947],[-77.753389,39.382094],[-77.738084,39.386211],[-77.735905,39.389665],[-77.740012,39.401694],[-77.75872,39.42681],[-77.792751,39.430593],[-77.802866,39.439285],[-77.786052,39.444224],[-77.798144,39.455981],[-77.798468,39.46067],[-77.777815,39.461924],[-77.795634,39.471259],[-77.797787,39.47876],[-77.769125,39.490281],[-77.765993,39.495724],[-77.781608,39.499067],[-77.791765,39.490789],[-77.80183,39.489395],[-77.845666,39.498628],[-77.845103,39.505845],[-77.82565,39.516895],[-77.825357,39.529177],[-77.836935,39.53217],[-77.84192,39.51847],[-77.86368,39.515032],[-77.866518,39.520039],[-77.865351,39.538381],[-77.888945,39.55595],[-77.878451,39.563493],[-77.83633,39.56637],[-77.829753,39.59105],[-77.831813,39.601105],[-77.838008,39.606125],[-77.885124,39.615775],[-77.886959,39.613329],[-77.880993,39.602852],[-77.888477,39.597343],[-77.923298,39.604852],[-77.932862,39.617676],[-77.94194,39.61879],[-77.944622,39.616772],[-77.93545,39.608076],[-77.936371,39.594508],[-77.93905,39.587139],[-77.946182,39.584814],[-77.951955,39.592709],[-77.950599,39.603944],[-77.957642,39.608614],[-77.966223,39.607435],[-77.976686,39.599744],[-78.009985,39.602893],[-78.035992,39.63572],[-78.08226,39.671166],[-78.088592,39.671211],[-78.107834,39.682137],[-78.176625,39.695967],[-78.191107,39.690262],[-78.201081,39.677866],[-78.231564,39.674382],[-78.233012,39.670471],[-78.223864,39.662607],[-78.225075,39.658878],[-78.254077,39.640089],[-78.262189,39.630464],[-78.265088,39.619274],[-78.283039,39.62047],[-78.355218,39.640576],[-78.358735,39.635589],[-78.353878,39.627722],[-78.358343,39.625581],[-78.380504,39.629359],[-78.382959,39.622246],[-78.372404,39.612297],[-78.378181,39.608178],[-78.420549,39.624021],[-78.43025,39.62329],[-78.433002,39.61652],[-78.425581,39.607599],[-78.397471,39.590232],[-78.395317,39.584215],[-78.408031,39.578593],[-78.443175,39.591155],[-78.457187,39.587379],[-78.458338,39.580426],[-78.454376,39.574319],[-78.426537,39.559155],[-78.418777,39.548953],[-78.424053,39.546315],[-78.433828,39.548953],[-78.436378,39.539302],[-78.449499,39.542281],[-78.45105,39.536695],[-78.461911,39.532971],[-78.462899,39.52084],[-78.468639,39.516789],[-78.5032,39.518652],[-78.521388,39.52479],[-78.565929,39.519444],[-78.587079,39.52802],[-78.595603,39.535483],[-78.600511,39.533434],[-78.623037,39.539512],[-78.655984,39.534695],[-78.675629,39.540371],[-78.689455,39.54577],[-78.694626,39.553251],[-78.72501,39.563973],[-78.733979,39.586618],[-78.746421,39.579544],[-78.760196,39.582154],[-78.778141,39.601364],[-78.77686,39.604027],[-78.760497,39.609984],[-78.751514,39.609947],[-78.747063,39.60569],[-78.733759,39.613931],[-78.736189,39.621708],[-78.748499,39.626262],[-78.763171,39.618897],[-78.777516,39.621712],[-78.76584,39.648487],[-78.775241,39.645687],[-78.781341,39.636787],[-78.795941,39.637287],[-78.801741,39.627488],[-78.795857,39.606934],[-78.809347,39.608063],[-78.812215,39.597717],[-78.818899,39.59037],[-78.824788,39.590233],[-78.82636,39.577333],[-78.815114,39.571351],[-78.816764,39.561691],[-78.838553,39.5673],[-78.851196,39.559924],[-78.851016,39.554044],[-78.874744,39.522611],[-78.885996,39.522581],[-78.891197,39.5189],[-78.916488,39.486544],[-78.933613,39.48618],[-78.942293,39.480987],[-78.939164,39.475267],[-78.941969,39.469959],[-78.953333,39.463645],[-78.955483,39.442277],[-78.965484,39.438455],[-78.978826,39.448678],[-79.017147,39.466977],[-79.028159,39.46506],[-79.046276,39.483801],[-79.05388,39.480094],[-79.056583,39.471014],[-79.068627,39.474515],[-79.098059,39.472073],[-79.095428,39.462548],[-79.104217,39.448358],[-79.116369,39.440482],[-79.117932,39.434412],[-79.129047,39.429542],[-79.129816,39.419901],[-79.140699,39.416649],[-79.145453,39.407767],[-79.16134,39.411895],[-79.16722,39.393256],[-79.197937,39.386132],[-79.213961,39.36532],[-79.25227,39.356663],[-79.253891,39.337222],[-79.282037,39.323048],[-79.283723,39.30964],[-79.290236,39.299323],[-79.314768,39.304381],[-79.33238,39.299919],[-79.344344,39.293534],[-79.343625,39.287148],[-79.35375,39.278039],[-79.376154,39.273154],[-79.387023,39.26554],[-79.412051,39.240546],[-79.42035,39.23888],[-79.425059,39.233686],[-79.424413,39.228171],[-79.43983,39.217074],[-79.476037,39.203728],[-79.486862,39.205959],[-79.476662,39.721078],[-75.788359,39.721811],[-75.773558,39.722411],[-75.744394,39.767855],[-75.701208,39.802606],[-75.641518,39.828363],[-75.594846,39.837286]]],[[[-76.048373,38.12055],[-76.061,38.127002],[-76.089018,38.115287],[-76.095548,38.125123],[-76.089017,38.141033],[-76.092334,38.151355],[-76.088639,38.192649],[-76.07147,38.203502],[-76.050511,38.203714],[-76.02217,38.177882],[-76.021941,38.171976],[-76.032767,38.169154],[-76.034038,38.157902],[-76.022515,38.133453],[-76.012487,38.131731],[-76.011916,38.122214],[-76.020496,38.117044],[-76.021305,38.108608],[-76.008168,38.095385],[-76.005904,38.07717],[-76.011544,38.072312],[-76.0233,38.07076],[-76.036676,38.076509],[-76.05831,38.094906],[-76.050156,38.107758],[-76.03962,38.11199],[-76.048373,38.12055]]],[[[-76.022325,37.953878],[-76.045561,37.953669],[-76.049608,37.983628],[-76.048617,38.014843],[-76.041668,38.032148],[-76.013128,38.039762],[-75.991846,38.025497],[-75.973432,38.018841],[-75.970345,38.008222],[-75.98502,38.001855],[-75.99473,37.974694],[-75.988879,37.960337],[-75.993905,37.953489],[-76.022325,37.953878]]]]},\"properties\":{\"name\":\"Delaware\",\"nation\":\"USA \"}}]}","contact":"","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":127955,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":808363,"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":71743,"text":"tei786 - 1961 - Test holes drilled in support of ground-water investigations, Project GNOME, Eddy County, New Mexico: basic data report","interactions":[],"lastModifiedDate":"2014-07-16T09:28:02","indexId":"tei786","displayToPublicDate":"2013-07-16T09:25:00","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":"786","title":"Test holes drilled in support of ground-water investigations, Project GNOME, Eddy County, New Mexico: basic data report","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei786","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission.","usgsCitation":"Cooper, J.B., 1961, Test holes drilled in support of ground-water investigations, Project GNOME, Eddy County, New Mexico: basic data report: U.S. Geological Survey Trace Elements Investigations 786, Report: 27 p.; 6 Illustrations, https://doi.org/10.3133/tei786.","productDescription":"Report: 27 p.; 6 Illustrations","costCenters":[],"links":[{"id":290245,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"New Mexico","county":"Eddy County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.8496,32.0001 ], [ -104.8496,32.9665 ], [ -103.7154,32.9665 ], [ -103.7154,32.0001 ], [ -104.8496,32.0001 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79f18e4b01948416424bc","contributors":{"authors":[{"text":"Cooper, James Blair","contributorId":25084,"corporation":false,"usgs":true,"family":"Cooper","given":"James","email":"","middleInitial":"Blair","affiliations":[],"preferred":false,"id":284691,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70038392,"text":"wdrCA611 - 1961 - Surface Water Records of California, 1961; Volume 1: Colorado River Basin, Southern Great Basin and Pacific Slope Basins excluding Central Valley","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA611","displayToPublicDate":"2012-05-13T11:07:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-61-1","title":"Surface Water Records of California, 1961; Volume 1: Colorado River Basin, Southern Great Basin and Pacific Slope Basins excluding Central Valley","docAbstract":"The surface-water records for the 1961 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of California are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Walter Hofmann, district engineer, Surface Water Branch.
\nThis report marks the beginning of a new method of presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in California were contained in Parts 9, 10, and 11 of that series.
\nBeginning with the 1961 water year, streamflow records and related data will be released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basicdata reports will be limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of conterminous United States will be further subdivided.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA611","collaboration":"Prepared in cooperation with the State of California and other agencies","usgsCitation":"U.S. Geological Survey, 1961, Surface Water Records of California, 1961; Volume 1: Colorado River Basin, Southern Great Basin and Pacific Slope Basins excluding Central Valley: U.S. Geological Survey Water Data Report CA-61-1, xvi, 448 p., https://doi.org/10.3133/wdrCA611.","productDescription":"xvi, 448 p.","temporalStart":"1960-10-01","temporalEnd":"1961-09-30","costCenters":[],"links":[{"id":256909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256904,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1961/ca-61/WDR-1961-vol1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Colorado River Basin;Southern Great Basin;Pacific Slope Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9f8ce4b08c986b31e66b"} ,{"id":70046318,"text":"wdrNM61 - 1961 - Surface water records of New Mexico, water year 1961","interactions":[],"lastModifiedDate":"2025-04-23T16:24:23.441285","indexId":"wdrNM61","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NM-61","title":"Surface water records of New Mexico, water year 1961","docAbstract":"The surface-water records for the 1961 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of New Mexico are given in this report. For convenience there are also included for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U. S. Geological Survey, under the direction of W. L. Heckler, district engineer, Surface Water Branch.
This report marks the beginning of a new method of presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U. S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there has been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in New Mexico were contained in Parts 7, 8, and 9 of that series.
Beginning with the 1961 water year, streamflow records and related data will be released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports will be limited and primarily for local needs. The records later will be published in Geological Survey water-supply paper at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of conterminous United States will be further subdivided.
The records for New Mexico will be published in water-supply papers covering Part 7 for stations in the Lower Mississippi River drainage, Part 8 for Western Gulf of Mexico drainage, and Part 9 for Colorado River drainage. For 1960 water year, the WSP Numbers for these parts were 1711, 1712, 1713 respectively. A compilation of records for these parts through 1950 water year is contained in WSP Nos. 1311, 1312, 1313 respectively; a 1951-60 compilation is currently being prepared, and WSP Nos. will be 1731, 1732, 1733.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Santa Fe, NM","doi":"10.3133/wdrNM61","collaboration":"Prepared in cooperation with the State of New Mexico and other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Surface water records of New Mexico, water year 1961: U.S. Geological Survey Water Data Report NM-61, vii, 211 p., https://doi.org/10.3133/wdrNM61.","productDescription":"vii, 211 p.","numberOfPages":"224","costCenters":[],"links":[{"id":484919,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1961/nm-61/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":273447,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1961/nm-61/report-thumb.jpg"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.052,31.3322 ], [ -109.052,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.052,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b300e7e4b01368e589e400","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":535528,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71750,"text":"tei794 - 1961 - Geophysical data on the Climax stock, Nevada test site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"tei794","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":"794","title":"Geophysical data on the Climax stock, Nevada test site, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/tei794","usgsCitation":"Allingham, J.W., and Zietz, I., 1961, Geophysical data on the Climax stock, Nevada test site, Nye County, Nevada: U.S. Geological Survey Trace Elements Investigations 794, 24 p., 12 fig., https://doi.org/10.3133/tei794.","productDescription":"24 p., 12 fig.","costCenters":[],"links":[{"id":191639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/794/report-thumb.jpg"},{"id":90981,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/794/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c1e8","contributors":{"authors":[{"text":"Allingham, John W.","contributorId":91848,"corporation":false,"usgs":true,"family":"Allingham","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":284702,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":284701,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71755,"text":"tei800 - 1961 - Ground water test well A, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and construction","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"tei800","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":"800","title":"Ground water test well A, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and construction","language":"ENGLISH","doi":"10.3133/tei800","usgsCitation":"Price, C., and Thordarson, W., 1961, Ground water test well A, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and construction: U.S. Geological Survey Trace Elements Investigations 800, 60 p., 4 fig. , https://doi.org/10.3133/tei800.","productDescription":"60 p., 4 fig. ","costCenters":[],"links":[{"id":191641,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/800/report-thumb.jpg"},{"id":90983,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/800/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90984,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/800/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d703","contributors":{"authors":[{"text":"Price, C.E.","contributorId":19642,"corporation":false,"usgs":true,"family":"Price","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":284712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":284713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71101,"text":"wdrWI611 - 1961 - Surface water records of Wisconsin, 1961","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"wdrWI611","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WI-61-1","title":"Surface water records of Wisconsin, 1961","language":"ENGLISH","doi":"10.3133/wdrWI611","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Surface water records of Wisconsin, 1961: U.S. Geological Survey Water Data Report WI-61-1, vi, 143 p., https://doi.org/10.3133/wdrWI611.","productDescription":"vi, 143 p.","numberOfPages":"149","costCenters":[],"links":[{"id":192934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696723","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":534720,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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}]}} ,{"id":14107,"text":"ofr6163 - 1961 - Gravity survey in the western Snake River Plain, Idaho-a progress report","interactions":[],"lastModifiedDate":"2012-02-02T00:06:54","indexId":"ofr6163","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":"61-63","title":"Gravity survey in the western Snake River Plain, Idaho-a progress report","docAbstract":"From June 24 through August 16, 1960, a regional gravity survey was made in 3,600 square miles of the Snake River Plain in southwestern Idaho. Six hundred and seventy-two gravity stations were established between latitudes 42?30\u0019N and 43?30\u0019N and between longitudes 115?15\u0019W and 116?15\u0019W at an average density of one station per 5.4 square miles. The data were reduced to simple-Bouguer gravity by standard methods and plotted as a gravity contour map.\r\n\r\nThree major anomalies were defined by the survey; two 30-mile long, en echelon gravity highs with amplitudes of 15 and 50 milligals, and one elongated gravity low with an amplitude of -10 milligals. A two-dimensional graticule analysis suggests that the highs are caused by vertical slabs of dense rock (probably basalt), the larges about 4 miles wide, about 30 miles long, and extending from about 1,000 feet (0.3 kilometer) below sea level to about 66,000 feet (20 kilometers) below sea level. A possible geological interpretation is that the vertical slabs are large, en echelon, basalt-filled fissures or zones of fissures in the earth\u0019s crust. The gravity low is attributed to an alluvium-filled trough about 5,000 feet (1.5 kilometers) deep.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6163","usgsCitation":"Hill, D.P., and Jacobson, J.J., 1961, Gravity survey in the western Snake River Plain, Idaho-a progress report: U.S. Geological Survey Open-File Report 61-63, 20 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr6163.","productDescription":"20 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":147041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0063/report-thumb.jpg"},{"id":42752,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0063/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42753,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1961/0063/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671ffd","contributors":{"authors":[{"text":"Hill, David P. hill@usgs.gov","contributorId":2600,"corporation":false,"usgs":true,"family":"Hill","given":"David","email":"hill@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":false,"id":168938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacobson, Jimmy J.","contributorId":36571,"corporation":false,"usgs":true,"family":"Jacobson","given":"Jimmy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":168939,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":52160,"text":"ofr6144 - 1961 - Floods in Wisconsin: Magnitude and frequency","interactions":[],"lastModifiedDate":"2017-09-21T15:03:10","indexId":"ofr6144","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":"61-44","title":"Floods in Wisconsin: Magnitude and frequency","docAbstract":"Flood data from gaging stations on Wisconsin rivers and streams are listed in this report. From these data, composite frequency curves were defined which express the ratio of floods of various recurrence intervals to the mean annual flood. Multiple correlation techniques were used to obtain formulas that relate the basin parameters of drainage area, main channel slope, and lake and reservoir surface area to the mean annual flood. By combining the results from the mean annual flood formulas with the regional frequency curves, the flood-frequency relationship can be determined for most sites in the State where the drainage basin exceeds 20 square miles. The curves and formulas are not applicable to: main stem of several of the larger rivers, highly regulated streams where it is possible for man to alter flood peaks, and drainage basins under 70 square miles in a part of west-central Wisconsin.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Madison, WI","doi":"10.3133/ofr6144","collaboration":"Prepared in cooperation with the State Highway Commission of Wisconsin","usgsCitation":"Ericson, D., 1961, Floods in Wisconsin: Magnitude and frequency: U.S. Geological Survey Open-File Report 61-44, iv, 109 p., https://doi.org/10.3133/ofr6144.","productDescription":"iv, 109 p.","numberOfPages":"124","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":178750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0044/report-thumb.jpg"},{"id":86673,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1961/0044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-90.403306,47.026693],[-90.411972,47.014958],[-90.425351,47.007526],[-90.464079,46.994636],[-90.465465,47.002593],[-90.457688,47.012484],[-90.4553,47.02375],[-90.455502,47.051331],[-90.449572,47.064965],[-90.438734,47.072557],[-90.417272,47.07757],[-90.395367,47.077175],[-90.393342,47.066204],[-90.403306,47.026693]]],[[[-90.730883,46.873096],[-90.677989,46.897527],[-90.667776,46.890037],[-90.675239,46.881029],[-90.718547,46.864531],[-90.745356,46.83566],[-90.756052,46.830595],[-90.760991,46.838277],[-90.749816,46.861806],[-90.730883,46.873096]]],[[[-90.764857,46.946524],[-90.741417,46.9636],[-90.71511,46.957332],[-90.694487,46.93671],[-90.689302,46.918563],[-90.737107,46.914712],[-90.764857,46.946524]]],[[[-90.568938,46.847391],[-90.58505,46.839789],[-90.613569,46.837958],[-90.673838,46.819684],[-90.683356,46.813275],[-90.685753,46.805003],[-90.652916,46.797755],[-90.65892,46.7885],[-90.696465,46.78204],[-90.716456,46.785418],[-90.7625,46.755547],[-90.787751,46.753301],[-90.783086,46.772939],[-90.790965,46.781373],[-90.790231,46.786103],[-90.733231,46.800183],[-90.720932,46.815897],[-90.656946,46.843476],[-90.622048,46.872872],[-90.602619,46.872715],[-90.568938,46.847391]]],[[[-90.572383,46.958835],[-90.528182,46.968396],[-90.508157,46.956836],[-90.524018,46.935714],[-90.539947,46.92785],[-90.543852,46.918289],[-90.549104,46.915461],[-90.569169,46.920309],[-90.637124,46.906724],[-90.64412,46.908373],[-90.654796,46.919249],[-90.634507,46.942944],[-90.572383,46.958835]]],[[[-87.335299,45.211327],[-87.331962,45.199251],[-87.33622,45.173174],[-87.327284,45.157363],[-87.376777,45.177298],[-87.375403,45.199296],[-87.335299,45.211327]]],[[[-90.962901,46.962028],[-90.980316,46.971578],[-90.98222,46.985417],[-90.949383,46.991208],[-90.939866,47.001321],[-90.928563,47.000726],[-90.923764,46.987928],[-90.932132,46.962655],[-90.962901,46.962028]]],[[[-90.757147,47.03372],[-90.688544,47.043347],[-90.643623,47.041177],[-90.608824,47.007558],[-90.560936,47.037013],[-90.544875,47.017383],[-90.552867,46.999686],[-90.609715,46.991208],[-90.634105,46.970983],[-90.671581,46.948973],[-90.712032,46.98526],[-90.767985,47.002327],[-90.776921,47.024324],[-90.757147,47.03372]]],[[[-87.405658,44.860098],[-87.384821,44.865532],[-87.385396,44.889964],[-87.406199,44.90449],[-87.393752,44.933751],[-87.374805,44.956631],[-87.360288,44.987643],[-87.322117,45.034201],[-87.264877,45.081361],[-87.257449,45.121644],[-87.240813,45.137559],[-87.242924,45.149377],[-87.238426,45.166492],[-87.224065,45.174551],[-87.21437,45.165735],[-87.195876,45.163201],[-87.17517,45.173],[-87.163169,45.185331],[-87.13303,45.192843],[-87.119972,45.191103],[-87.122708,45.221786],[-87.109541,45.255397],[-87.078316,45.265723],[-87.071035,45.280355],[-87.057627,45.292838],[-87.0517,45.285888],[-87.043895,45.284767],[-87.017036,45.299254],[-86.994112,45.298061],[-86.97778,45.290684],[-86.970355,45.278455],[-86.984938,45.259036],[-86.983066,45.250764],[-86.973287,45.246381],[-86.985973,45.215872],[-87.002806,45.211773],[-87.00754,45.222127],[-87.032521,45.222274],[-87.040909,45.211535],[-87.045242,45.158798],[-87.030225,45.147382],[-87.03292,45.141963],[-87.045748,45.134987],[-87.054282,45.120074],[-87.049346,45.110122],[-87.048213,45.089124],[-87.057415,45.087472],[-87.064864,45.078427],[-87.079552,45.070783],[-87.081866,45.059103],[-87.090849,45.055465],[-87.121156,45.058311],[-87.139384,45.012565],[-87.163477,45.004913],[-87.189134,44.969078],[-87.188399,44.94856],[-87.17524,44.939753],[-87.1717,44.931476],[-87.204238,44.916819],[-87.215808,44.906744],[-87.217171,44.898013],[-87.206285,44.885928],[-87.204815,44.877199],[-87.267061,44.847025],[-87.282561,44.814729],[-87.304824,44.804603],[-87.313363,44.794237],[-87.320397,44.784963],[-87.319903,44.769672],[-87.353789,44.701915],[-87.401629,44.631191],[-87.437751,44.604559],[-87.467089,44.553557],[-87.483696,44.511354],[-87.490024,44.477224],[-87.498662,44.460686],[-87.506362,44.423804],[-87.517965,44.394356],[-87.517597,44.375696],[-87.533583,44.351111],[-87.545382,44.321385],[-87.541382,44.294018],[-87.508457,44.229755],[-87.507419,44.210803],[-87.512903,44.192808],[-87.51966,44.17987],[-87.53994,44.15969],[-87.563181,44.144195],[-87.603572,44.13039],[-87.6458,44.105222],[-87.654935,44.082552],[-87.656062,44.051919],[-87.683361,44.020139],[-87.695053,43.990715],[-87.69892,43.965936],[-87.71817,43.939498],[-87.735436,43.882219],[-87.728698,43.852524],[-87.726408,43.810454],[-87.700251,43.76735],[-87.702985,43.749695],[-87.709885,43.735795],[-87.702685,43.687596],[-87.789105,43.564844],[-87.797608,43.52731],[-87.793239,43.492783],[-87.807799,43.461136],[-87.855608,43.405441],[-87.872504,43.380178],[-87.882392,43.352099],[-87.889207,43.307652],[-87.901847,43.284117],[-87.911787,43.250406],[-87.896286,43.197108],[-87.881085,43.170609],[-87.900285,43.13731],[-87.900496,43.126],[-87.893185,43.114011],[-87.876084,43.099011],[-87.866487,43.074419],[-87.870184,43.064412],[-87.894813,43.042497],[-87.898184,43.030689],[-87.896157,43.017486],[-87.887789,43.000715],[-87.857182,42.978015],[-87.845181,42.962015],[-87.842786,42.944865],[-87.847745,42.889595],[-87.824,42.836649],[-87.766675,42.784896],[-87.781949,42.74857],[-87.778824,42.728432],[-87.783489,42.705164],[-87.802377,42.676651],[-87.814674,42.64402],[-87.819407,42.617327],[-87.819374,42.60662],[-87.810873,42.58732],[-87.812273,42.52982],[-87.800477,42.49192],[-88.115285,42.496219],[-88.786681,42.491983],[-89.690088,42.505191],[-90.640927,42.508302],[-90.636727,42.518702],[-90.645627,42.5441],[-90.654127,42.5499],[-90.661527,42.567999],[-90.685487,42.589614],[-90.693999,42.614509],[-90.709204,42.636078],[-90.769495,42.651443],[-90.88743,42.67247],[-90.921155,42.685406],[-90.949213,42.685573],[-90.977735,42.696816],[-91.000128,42.716189],[-91.026786,42.724228],[-91.035418,42.73734],[-91.053733,42.738238],[-91.056297,42.747341],[-91.065783,42.753387],[-91.060261,42.761847],[-91.069549,42.769628],[-91.078097,42.806526],[-91.078665,42.827678],[-91.09406,42.830813],[-91.091402,42.84986],[-91.097656,42.859871],[-91.100565,42.883078],[-91.115512,42.894672],[-91.14556,42.90798],[-91.144315,42.926592],[-91.149784,42.940244],[-91.14655,42.963345],[-91.156562,42.978226],[-91.15749,42.991475],[-91.174692,43.038713],[-91.179457,43.067427],[-91.175193,43.103771],[-91.177932,43.128875],[-91.175253,43.134665],[-91.1562,43.142945],[-91.1462,43.152405],[-91.12217,43.197255],[-91.066398,43.239293],[-91.059684,43.248566],[-91.058644,43.257679],[-91.072649,43.262129],[-91.07371,43.274746],[-91.107237,43.313645],[-91.137343,43.329757],[-91.181115,43.345926],[-91.201847,43.349103],[-91.21477,43.365874],[-91.19767,43.395334],[-91.203144,43.419805],[-91.22875,43.445537],[-91.233367,43.455168],[-91.216035,43.481142],[-91.217353,43.512474],[-91.232941,43.523967],[-91.243183,43.540309],[-91.24382,43.54913],[-91.232812,43.564842],[-91.231865,43.581822],[-91.268748,43.615348],[-91.268457,43.627352],[-91.262397,43.64176],[-91.270767,43.65308],[-91.273252,43.666623],[-91.268455,43.709824],[-91.255932,43.729849],[-91.255431,43.744876],[-91.243955,43.773046],[-91.262436,43.792166],[-91.277695,43.837741],[-91.284138,43.847065],[-91.310991,43.867381],[-91.320605,43.888491],[-91.338141,43.897664],[-91.346271,43.910074],[-91.356741,43.916564],[-91.366642,43.937463],[-91.385785,43.954239],[-91.406011,43.963929],[-91.43738,43.999962],[-91.463515,44.009041],[-91.478498,44.00803],[-91.507121,44.01898],[-91.580019,44.026925],[-91.59207,44.031372],[-91.610487,44.04931],[-91.638115,44.063285],[-91.647873,44.064109],[-91.667006,44.086964],[-91.68153,44.0974],[-91.707491,44.103906],[-91.710597,44.12048],[-91.721552,44.130342],[-91.751747,44.134786],[-91.774486,44.147539],[-91.808064,44.159262],[-91.817302,44.164235],[-91.829167,44.17835],[-91.875158,44.200575],[-91.877429,44.212921],[-91.892698,44.231105],[-91.88704,44.251772],[-91.896008,44.262871],[-91.895652,44.273008],[-91.924613,44.291815],[-91.913534,44.311392],[-91.918625,44.322671],[-91.92559,44.333548],[-91.941311,44.340978],[-91.9636,44.362112],[-92.038147,44.388731],[-92.056486,44.402729],[-92.078605,44.404869],[-92.111085,44.413948],[-92.124513,44.422115],[-92.195378,44.433792],[-92.232472,44.445434],[-92.291005,44.485464],[-92.302215,44.500298],[-92.302466,44.516487],[-92.314071,44.538014],[-92.336114,44.554004],[-92.361518,44.558935],[-92.399281,44.558292],[-92.431101,44.565786],[-92.455105,44.561886],[-92.481001,44.568276],[-92.493808,44.566063],[-92.518358,44.575183],[-92.54806,44.567792],[-92.55151,44.571607],[-92.549777,44.58113],[-92.569434,44.603539],[-92.577148,44.605054],[-92.584711,44.599861],[-92.601516,44.612052],[-92.621456,44.615017],[-92.619779,44.634195],[-92.632105,44.649027],[-92.660988,44.660884],[-92.700948,44.693751],[-92.737259,44.717155],[-92.787906,44.737432],[-92.807317,44.750364],[-92.805287,44.768361],[-92.785206,44.792303],[-92.78043,44.812589],[-92.766102,44.834966],[-92.76909,44.861997],[-92.764133,44.875905],[-92.773946,44.889997],[-92.774571,44.898084],[-92.758701,44.908979],[-92.750645,44.937299],[-92.754603,44.955767],[-92.769445,44.97215],[-92.771231,45.001378],[-92.76206,45.02432],[-92.770362,45.033803],[-92.793282,45.047178],[-92.803079,45.060978],[-92.800851,45.069477],[-92.791528,45.079647],[-92.746749,45.107051],[-92.739528,45.116515],[-92.745694,45.123112],[-92.757707,45.155466],[-92.752542,45.171772],[-92.764872,45.182812],[-92.767408,45.190166],[-92.763908,45.204866],[-92.751708,45.218666],[-92.760249,45.2496],[-92.751659,45.26591],[-92.760615,45.278827],[-92.761013,45.289028],[-92.737122,45.300459],[-92.709968,45.321302],[-92.698967,45.336374],[-92.703705,45.35633],[-92.679193,45.37271],[-92.669505,45.389111],[-92.650422,45.398507],[-92.646602,45.441635],[-92.652698,45.454527],[-92.680234,45.464344],[-92.702224,45.493046],[-92.726677,45.514462],[-92.726082,45.541112],[-92.770223,45.566939],[-92.785741,45.567888],[-92.823309,45.560934],[-92.871082,45.567581],[-92.883749,45.575483],[-92.886442,45.598679],[-92.882529,45.610216],[-92.888035,45.624959],[-92.887929,45.639006],[-92.875488,45.689014],[-92.870145,45.696757],[-92.869193,45.717568],[-92.809837,45.744172],[-92.784621,45.764196],[-92.776496,45.790014],[-92.757815,45.806574],[-92.765146,45.830183],[-92.739991,45.846283],[-92.734039,45.868108],[-92.712503,45.891705],[-92.676607,45.90637],[-92.676807,45.91093],[-92.659549,45.922937],[-92.639116,45.924555],[-92.640115,45.932478],[-92.636316,45.934634],[-92.614314,45.934529],[-92.60246,45.940815],[-92.551933,45.951651],[-92.549806,45.967986],[-92.527052,45.983245],[-92.469354,45.973811],[-92.46126,45.979427],[-92.464512,45.985038],[-92.453373,45.992913],[-92.442259,46.016177],[-92.428555,46.024241],[-92.410649,46.027259],[-92.372717,46.014198],[-92.35176,46.015685],[-92.344244,46.02743],[-92.343604,46.040917],[-92.332912,46.062697],[-92.294033,46.074377],[-92.292192,46.666042],[-92.287392,46.667342],[-92.286192,46.660342],[-92.274392,46.657441],[-92.270592,46.650741],[-92.256592,46.658741],[-92.242493,46.649241],[-92.228492,46.652941],[-92.216392,46.649841],[-92.207092,46.651941],[-92.202292,46.655041],[-92.204092,46.666941],[-92.176091,46.686341],[-92.183091,46.695241],[-92.198491,46.696141],[-92.205192,46.698341],[-92.205692,46.702541],[-92.189091,46.717541],[-92.167291,46.719941],[-92.146291,46.71594],[-92.141291,46.72524],[-92.14329,46.73464],[-92.13789,46.73954],[-92.108777,46.749105],[-92.08949,46.74924],[-92.03399,46.708939],[-92.020289,46.704039],[-92.007989,46.705039],[-91.961889,46.682539],[-91.942988,46.679939],[-91.886963,46.690211],[-91.820027,46.690176],[-91.790473,46.694624],[-91.74965,46.709129],[-91.646146,46.734575],[-91.590684,46.754331],[-91.511077,46.757453],[-91.489125,46.766997],[-91.44957,46.773252],[-91.411799,46.78964],[-91.369387,46.793745],[-91.33825,46.817704],[-91.315061,46.826729],[-91.256873,46.836833],[-91.226796,46.86361],[-91.207524,46.865835],[-91.200107,46.854017],[-91.178292,46.844259],[-91.168297,46.844727],[-91.140301,46.873105],[-91.133337,46.870341],[-91.134977,46.859023],[-91.107323,46.857469],[-91.096565,46.86153],[-91.090916,46.88267],[-91.080951,46.883609],[-91.069331,46.878772],[-91.052991,46.881325],[-91.03989,46.88923],[-91.034518,46.903053],[-91.019141,46.911502],[-90.995149,46.917577],[-90.968419,46.94391],[-90.92204,46.931372],[-90.914044,46.933346],[-90.908654,46.941221],[-90.880358,46.957661],[-90.855874,46.962232],[-90.838814,46.957728],[-90.786595,46.927019],[-90.75563,46.899247],[-90.751151,46.887863],[-90.77017,46.876296],[-90.798545,46.823922],[-90.825696,46.803858],[-90.835008,46.790366],[-90.854916,46.788952],[-90.863542,46.780565],[-90.859724,46.774433],[-90.862333,46.768135],[-90.885021,46.756341],[-90.870396,46.723293],[-90.853225,46.70028],[-90.853644,46.694464],[-90.870079,46.679449],[-90.914619,46.659054],[-90.924487,46.625417],[-90.93831,46.608768],[-90.951418,46.600774],[-90.942101,46.588573],[-90.906058,46.58343],[-90.873154,46.601223],[-90.794775,46.624941],[-90.770192,46.636127],[-90.755381,46.646225],[-90.756495,46.664591],[-90.74809,46.669817],[-90.73726,46.692267],[-90.627885,46.623839],[-90.558141,46.586384],[-90.538346,46.581182],[-90.505909,46.589614],[-90.437596,46.561492],[-90.418136,46.566094],[-90.39332,46.532615],[-90.369964,46.540549],[-90.350121,46.537337],[-90.344338,46.552087],[-90.331887,46.553278],[-90.326686,46.54615],[-90.320428,46.546287],[-90.310859,46.539365],[-90.316983,46.517319],[-90.285707,46.518846],[-90.277131,46.524487],[-90.272599,46.521127],[-90.274721,46.515416],[-90.270684,46.508237],[-90.263018,46.502777],[-90.231587,46.509842],[-90.230324,46.501732],[-90.216594,46.501759],[-90.204009,46.478175],[-90.188996,46.469015],[-90.193294,46.463143],[-90.180336,46.456746],[-90.17786,46.440548],[-90.166919,46.439851],[-90.158603,46.422656],[-90.157851,46.409291],[-90.144359,46.390255],[-90.13225,46.381249],[-90.133871,46.371828],[-90.116844,46.355153],[-90.12138,46.338131],[-89.09163,46.138505],[-88.85027,46.040274],[-88.837991,46.030176],[-88.811948,46.021609],[-88.79646,46.023605],[-88.80067,46.030036],[-88.796182,46.033712],[-88.779221,46.031869],[-88.783891,46.020934],[-88.779915,46.015436],[-88.765208,46.022086],[-88.756295,46.020173],[-88.746422,46.025798],[-88.730675,46.026535],[-88.721125,46.022013],[-88.718397,46.013284],[-88.704687,46.018154],[-88.679132,46.013538],[-88.661312,45.988819],[-88.6375,45.98496],[-88.616405,45.9877],[-88.611466,46.003332],[-88.60144,46.017599],[-88.59386,46.015132],[-88.589755,46.005602],[-88.565485,46.015708],[-88.550756,46.012896],[-88.541078,46.013763],[-88.533825,46.020915],[-88.514601,46.019926],[-88.507188,46.0183],[-88.498108,45.99636],[-88.492495,45.992157],[-88.476002,45.992826],[-88.470855,46.001004],[-88.458658,45.999391],[-88.450325,45.990181],[-88.439733,45.990456],[-88.416914,45.975323],[-88.388847,45.982675],[-88.380183,45.991654],[-88.330137,45.965951],[-88.330296,45.956625],[-88.326953,45.955071],[-88.316894,45.960969],[-88.292381,45.951115],[-88.250133,45.963147],[-88.246307,45.962983],[-88.242518,45.950363],[-88.23314,45.947405],[-88.201852,45.945173],[-88.202116,45.949836],[-88.191991,45.95274],[-88.170096,45.93947],[-88.146352,45.935314],[-88.121864,45.92075],[-88.104686,45.922121],[-88.096496,45.917273],[-88.095354,45.913895],[-88.105677,45.904387],[-88.101814,45.883504],[-88.095841,45.880042],[-88.083965,45.881186],[-88.073944,45.875593],[-88.075146,45.864832],[-88.081641,45.865087],[-88.13611,45.819029],[-88.129461,45.809288],[-88.105355,45.800104],[-88.103247,45.791361],[-88.072091,45.780261],[-88.050634,45.780972],[-88.040221,45.789236],[-87.991447,45.795393],[-87.98087,45.776977],[-87.989829,45.772945],[-87.96697,45.764021],[-87.963452,45.75822],[-87.905873,45.759364],[-87.896032,45.752285],[-87.875813,45.753888],[-87.864141,45.745697],[-87.86432,45.737139],[-87.85548,45.726943],[-87.805867,45.706841],[-87.809181,45.700337],[-87.782226,45.683053],[-87.780737,45.675458],[-87.823164,45.662732],[-87.824102,45.647138],[-87.810194,45.638732],[-87.79588,45.618846],[-87.780845,45.614599],[-87.777199,45.588499],[-87.787534,45.581376],[-87.790874,45.564096],[-87.806104,45.562863],[-87.829346,45.568776],[-87.833591,45.562529],[-87.80339,45.538272],[-87.802267,45.514233],[-87.792769,45.499967],[-87.812971,45.4661],[-87.861697,45.434473],[-87.860432,45.423504],[-87.849322,45.403872],[-87.859131,45.398967],[-87.859418,45.388227],[-87.875424,45.379373],[-87.871789,45.373557],[-87.884855,45.362792],[-87.888052,45.354697],[-87.881114,45.351278],[-87.86856,45.360537],[-87.860871,45.351192],[-87.850418,45.347492],[-87.848368,45.340676],[-87.832612,45.352249],[-87.790324,45.353444],[-87.783076,45.349725],[-87.754104,45.349442],[-87.751626,45.354169],[-87.738352,45.358243],[-87.718891,45.377462],[-87.693956,45.389893],[-87.675017,45.382454],[-87.674403,45.378065],[-87.657349,45.368752],[-87.656632,45.358617],[-87.648476,45.352243],[-87.648126,45.339396],[-87.662029,45.326434],[-87.663666,45.318257],[-87.687498,45.298055],[-87.698248,45.281512],[-87.69878,45.26942],[-87.709137,45.260341],[-87.711339,45.239965],[-87.724156,45.233236],[-87.721935,45.228444],[-87.726952,45.218949],[-87.726198,45.209391],[-87.741732,45.198201],[-87.736509,45.173389],[-87.683902,45.144135],[-87.675816,45.135059],[-87.678511,45.131204],[-87.672447,45.121294],[-87.661296,45.112566],[-87.661211,45.108279],[-87.631535,45.106224],[-87.59188,45.094689],[-87.587147,45.089495],[-87.587992,45.085271],[-87.601849,45.082297],[-87.610395,45.075617],[-87.625748,45.045157],[-87.624693,45.014176],[-87.630298,44.976865],[-87.661964,44.973035],[-87.696492,44.974233],[-87.766115,44.965351],[-87.817551,44.951986],[-87.837647,44.933091],[-87.844299,44.918524],[-87.827751,44.891229],[-87.832764,44.880939],[-87.852789,44.86486],[-87.865898,44.840988],[-87.878218,44.839016],[-87.899787,44.828051],[-87.941453,44.75608],[-87.964714,44.74357],[-87.983065,44.72073],[-87.990081,44.669791],[-88.002085,44.664035],[-88.009766,44.637081],[-87.998836,44.609523],[-88.001943,44.603909],[-88.012395,44.602438],[-88.027103,44.578992],[-88.039092,44.574324],[-88.042261,44.567344],[-88.005518,44.539216],[-87.970702,44.530292],[-87.943801,44.529693],[-87.929001,44.535993],[-87.901206,44.568887],[-87.899368,44.573043],[-87.903689,44.581317],[-87.901179,44.584545],[-87.867941,44.607606],[-87.809076,44.636189],[-87.77516,44.639281],[-87.756048,44.649117],[-87.748409,44.667122],[-87.71978,44.693246],[-87.720312,44.725073],[-87.610063,44.838384],[-87.581635,44.851638],[-87.550288,44.85129],[-87.530999,44.857437],[-87.515142,44.869596],[-87.502431,44.864619],[-87.478489,44.863572],[-87.437084,44.892718],[-87.421007,44.887869],[-87.419951,44.87594],[-87.405658,44.860098]]],[[[-86.880572,45.331467],[-86.895055,45.329035],[-86.899488,45.322588],[-86.896667,45.307275],[-86.899891,45.295185],[-86.925681,45.3242],[-86.95499,45.34128],[-86.956192,45.351179],[-86.946297,45.35869],[-86.95497,45.383194],[-86.943041,45.41525],[-86.934724,45.421123],[-86.928045,45.411273],[-86.917686,45.40789],[-86.892893,45.40898],[-86.877502,45.413981],[-86.862174,45.412151],[-86.853145,45.405547],[-86.830353,45.410852],[-86.828731,45.428461],[-86.810055,45.422619],[-86.805415,45.407324],[-86.824383,45.406135],[-86.841432,45.389601],[-86.853103,45.370861],[-86.863367,45.365],[-86.869031,45.333244],[-86.880572,45.331467]]]]},\"properties\":{\"name\":\"Wisconsin\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e09e6","contributors":{"authors":[{"text":"Ericson, D.W.","contributorId":80295,"corporation":false,"usgs":true,"family":"Ericson","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":244892,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52165,"text":"ofr6150 - 1961 - Data on wells at Ladd Air Force Base, Alaska","interactions":[],"lastModifiedDate":"2023-07-24T21:05:38.643088","indexId":"ofr6150","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":"61-50","title":"Data on wells at Ladd Air Force Base, Alaska","docAbstract":"Ladd Air Force Base, in central Alaska, obtains its water supply from wells. A tabulation of 104 wells gives available data on depth, diameter, yield, and depth of permafrost encountered. Also given are 23 well logs and 21 chemical analyses of well waters and treated waters from Ladd Air Force Base.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6150","usgsCitation":"Feulner, A., 1961, Data on wells at Ladd Air Force Base, Alaska: U.S. Geological Survey Open-File Report 61-50, 41 p., https://doi.org/10.3133/ofr6150.","productDescription":"41 p.","costCenters":[],"links":[{"id":419271,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1961/0050/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":178854,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0050/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Ladd Air Force Base","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -147.67058155896018,\n 64.85214806667582\n ],\n [\n -147.67058155896018,\n 64.81946132923088\n ],\n [\n -147.48595313270116,\n 64.81946132923088\n ],\n [\n -147.48595313270116,\n 64.85214806667582\n ],\n [\n -147.67058155896018,\n 64.85214806667582\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c5db","contributors":{"authors":[{"text":"Feulner, Alvin J.","contributorId":15694,"corporation":false,"usgs":true,"family":"Feulner","given":"Alvin J.","affiliations":[],"preferred":false,"id":244897,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4016,"text":"cir445 - 1961 - Occurrence of minor elements in water","interactions":[],"lastModifiedDate":"2018-01-02T20:01:22","indexId":"cir445","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"445","title":"Occurrence of minor elements in water","docAbstract":"Three basic studies, using spectrographic methods, have been used to establish the occurrence of minor elements in natural waters. One study, of oceanborne chemicals in principal rivers, has established a method for the quantitative analysis of many minor elements. Strontium, barium, lithium, rubidium, chromium, nickel, copper, lead, boron, titanium, molybdenum, manganese, and vanadium occur most frequently in measurable quantities. \r\n\r\nReconnaissance of the strontium in surface waters of the United States, shows that surface waters in parts of northern and western Texas and southern New Mexico and Arizona are comparatively high in strontium. A study of minor elements in selected waters of California is continuing. Assessment of preliminary data on uranium and radium in waters is facilitated by grouping data for 10 geotectonic regions of the United States.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir445","usgsCitation":"Durum, W.H., and Haffty, J., 1961, Occurrence of minor elements in water: U.S. Geological Survey Circular 445, iii, 11 p. :maps, diagrs., tables. ;27cm., https://doi.org/10.3133/cir445.","productDescription":"iii, 11 p. :maps, diagrs., tables. ;27cm.","costCenters":[],"links":[{"id":31108,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0445/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0445/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db69235d","contributors":{"authors":[{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":147987,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haffty, Joseph","contributorId":79450,"corporation":false,"usgs":true,"family":"Haffty","given":"Joseph","email":"","affiliations":[],"preferred":false,"id":147988,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":38969,"text":"pp424A - 1961 - Synopsis of geologic and hydrologic results: Chapter A in Geological Survey research 1961","interactions":[],"lastModifiedDate":"2017-09-07T10:37:44","indexId":"pp424A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"424","chapter":"A","title":"Synopsis of geologic and hydrologic results: Chapter A in Geological Survey research 1961","docAbstract":"The Geological Survey is engaged in many different kinds of investigations in the fields of geology and hydrology. These investigations may be grouped into several broad, inter-related categories as follows:
(a) Economic geology, including engineering geology
(b) Regional geologic mapping, including detailed mapping and stratigraphic studies
(c) Resource and topical studies
(d) Ground-water studies
(e) Surface-water studies
(f) Quality-of-water studies
(g) Field and laboratory research on geologic and hydrologic processes and principles.
The Geological Survey also carries on investigations in its fields of competence for other Federal agencies that do not have the required specialized staffs or scientific facilities.
Nearly all the Geological Survey's activities yield new data and principles of value in the development or application of the geologic and hydrologic sciences. The purpose of this report, which consists of 4 chapters, is to present as promptly as possible findings that have come to the fore during the fiscal year 1961 the 12 months ending June 30, 1961.
The present volume, chapter A, is a synopsis of the highlights of recent findings of scientific and economic interest. Some of these findings have been published or placed on open file during the year; some are presented in chapters B, C, and D; still others have not been published previously. Only part of the scientific and economic results developed during the year can be presented in this synopsis. Readers who wish more complete or more detailed information should consult the bibliography of reports beginning on page A-156 of this volume, and the collection of short articles presented in the companion chapters as follows:
Prof. Paper 424-B Articles 1 to 146
Prof. Paper 424-C Articles 147 to 292
Prof. Paper 424-D Articles 293 to 435
A list of investigations in progress in the Geologic and Water Resources Divisions with the names and addresses of the project leaders is given on pages A-110 to A-155 for those interested in work in progress in various areas or on special topics.
During the fiscal year 1961, the services of the Geologic and Water Resources Divisions were utilized, or supported financially in part, by the many Federal and State agencies listed on pages A-106 to A-109. The Geological Survey has also cooperated from time to time with other agencies, and some of the work described in these chapters stems from work of previous years in cooperation with agencies not shown on the list. All cooperating agencies are identified where appropriate in the individual short articles in chapters B, C, and D, and they are mentioned in connection with some of the larger programs summarized in chapter A; because of space limitations, however, their contributions are mentioned in many of the short summary paragraphs contained in chapter A.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1961 (Professional Paper 424)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp424A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Synopsis of geologic and hydrologic results: Chapter A in Geological Survey research 1961: U.S. Geological Survey Professional Paper 424, xii, 194 p., https://doi.org/10.3133/pp424A.","productDescription":"xii, 194 p.","numberOfPages":"209","costCenters":[],"links":[{"id":336127,"rank":5,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp424D","text":"Chapter D","linkHelpText":"Articles 293-435"},{"id":336125,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp424B","text":"Chapter B","linkHelpText":"Articles 1-146"},{"id":336126,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/pp424C","text":"Chapter C","linkHelpText":"Articles 147-292"},{"id":120394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0424a/report-thumb.jpg"},{"id":66036,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0424a/report.pdf","text":"Report","size":"6.08 MB","linkFileType":{"id":1,"text":"pdf"}}],"publicComments":"A summary of recent scientific and economic results, accompanied by a list of reports released in fiscal 1961 and a list of investigations in progress.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db6876de","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":529897,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6084,"text":"pp412 - 1961 - Salinity and hydrology of closed lakes","interactions":[],"lastModifiedDate":"2017-02-22T14:30:23","indexId":"pp412","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"412","title":"Salinity and hydrology of closed lakes","docAbstract":"Lakes without outlets, called closed lakes, are exclusively features of the arid and semiarid zones where annual evaporation exceeds rainfall. The number of closed lakes increases with aridity, so there are relatively few perennial closed lakes, but \"dry\" lakes that rarely contain water are numerous.
Closed lakes fluctuate in level to a much greater degree than the open lakes of the humid zone, because variations in inflow can be compensated only by changes in surface area. Since the variability of inflow increases with aridity, it is possible to derive an approximate relationship for the coefficient of variation of lake area in terms of data on rates of evaporation, lake area, lake depth, and drainage area.
The salinity of closed lakes is highly variable, ranging from less than 1 percent to over 25 percent by weight of salts. Some evidence suggests that the tonnage of salts in a lake solution is substantially less than the total input of salts into the lake over the period of existence of the closed lake. This evidence suggests further that the salts in a lake solution represent a kind of long-term balance between factors of gain and loss of salts from the solution.
Possible mechanisms for the loss of salts dissolved in the lake include deposition in marginal bays, entrapment in sediments, and removal by wind. Transport of salt from the lake surface in wind spray is also a contributing, but seemingly not major, factor.
The hypothesis of a long-term balance between input to and losses from the lake solution is checked by deriving a formula for the equilibrium concentration and comparing the results with the salinity data. The results indicate that the reported salinities seemingly can be explained in terms of their geometric properties and hydrologic environment.
The time for accumulation of salts in the lake solution the ratio between mass of salts in the solution and the annual input may also be estimated from the geometric and hydrologic factors, in the absence of data on the salt content of the lake or of the inflow.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp412","usgsCitation":"Langbein, W.B., 1961, Salinity and hydrology of closed lakes: U.S. Geological Survey Professional Paper 412, iii, 20 p., https://doi.org/10.3133/pp412.","productDescription":"iii, 20 p.","numberOfPages":"25","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":33126,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0412/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118191,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0412/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdfa9","contributors":{"authors":[{"text":"Langbein, Walter Basil","contributorId":40581,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter","email":"","middleInitial":"Basil","affiliations":[],"preferred":false,"id":152078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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}]}} ]}