The flat hexagonal crystals from the Big Horn Basin, Wyoming, Iocally called \"Indian Pennies,\" are shown to consist of dolomite pseudomorphous after crystals of aragonite.
","language":"English","publisher":"Mineralogical Society of America","usgsCitation":"Andrews, D., and Schaller, W.T., 1942, Dolomite pseudomorphs after crystals of aragonite [Wyoming]: American Mineralogist, v. 27, no. 2, p. 135-140.","productDescription":"6 p.","startPage":"135","endPage":"140","costCenters":[],"links":[{"id":369439,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":369438,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.geoscienceworld.org/msa/ammin/article/27/2/135/538188/dolomite-pseudomorphous-after-crystals-of"}],"country":"United States","state":"Wyoming","otherGeospatial":"Big Horn River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.23681640625,\n 44.01652134387754\n ],\n [\n -107.6824951171875,\n 44.01652134387754\n ],\n [\n -107.6824951171875,\n 45.00365115687186\n ],\n [\n -110.23681640625,\n 45.00365115687186\n ],\n [\n -110.23681640625,\n 44.01652134387754\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"27","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Andrews, D. A.","contributorId":83603,"corporation":false,"usgs":true,"family":"Andrews","given":"D. A.","affiliations":[],"preferred":false,"id":806129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schaller, W. T.","contributorId":19518,"corporation":false,"usgs":true,"family":"Schaller","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":806130,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70207400,"text":"70207400 - 1942 - Correlation of the outcropping cretaceous formations of the Atlantic and Gulf Coastal Plain and trans-Pecos Texas","interactions":[],"lastModifiedDate":"2019-12-19T14:13:10","indexId":"70207400","displayToPublicDate":"1942-12-31T15:13:21","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Correlation of the outcropping cretaceous formations of the Atlantic and Gulf Coastal Plain and trans-Pecos Texas","docAbstract":"This is Number 9 of a series of correlation charts prepared by the Committee on Stratigraphy of the National Research Council, which will cover the post-Proterozoic sedimentary formations of North America. For general information about the project the reader is referred to the general introduction preceding this paper.
The senior author, Lloyd W. Stephenson, is responsible for that part of the chart treating of the Upper Cretaceous series in the Atlantic and Gulf Coastal Plain (exceptions noted below) and the Lower Cretaceous series of the North Atlantic Coastal Plain; with respect to the Upper Cretaceous his presentation is based largely on his personal knowledge of the paleontology and stratigraphy of the area, gained from field and laboratory studies ranging from reconnaissance to detailed; all published information has been considered, and much of it utilized, but it is not practicable to include a complete bibliography. References are given to papers presenting views differing from those of the author, and to recent papers not yet listed in bibliographies. A complete bibliography of Texas geology through 1932 is given by Sellards (1933, p. 819-965). Watson H. Monroe has collaborated in the preparation of that part of the chart showing therelations of the Upper Cretaceous units in Alabama and Mississippi. The classification shown in the Upper Cretaceous part of the Delaware column is based on a recently published paper by Charles W. Carter (1937, p. 237-281). Philip B. King is responsible for the remainder of the chart covering the Lower Cretaceous (Comanche series) of central Texas (largely compiled from published sources) and all of the Cretaceous in trans-Pecos Texas (from personal knowledge and published sources). In March 1941 this part of the chart was checked by R. W. Imlay, and changes were made by King at his suggestion. References to the more important literature are given.
In a correlation chart of this kind, in which age equivalencies are expressed by horizontal lining, it is obviously impossible to indicate relative thicknesses by vertical spacing. Hiatuses are indicated by vertical lining. The red-line overprint is intended to indicate certain important lithologic and faunal boundaries, and to assist the eye in recognizing the age relationships of the geologic units
","language":"English","publisher":"Geographical Society of America ","doi":"10.1130/GSAB-53-435","issn":"00167606","usgsCitation":"Stephenson, L.W., King, P., Monroe, W.H., and Imlay, R.W., 1942, Correlation of the outcropping cretaceous formations of the Atlantic and Gulf Coastal Plain and trans-Pecos Texas: Geological Society of America Bulletin, v. 53, no. 3, p. 435-448, https://doi.org/10.1130/GSAB-53-435.","productDescription":"14 p. ","startPage":"435","endPage":"448","costCenters":[],"links":[{"id":370435,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"53","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stephenson, L. W.","contributorId":70349,"corporation":false,"usgs":true,"family":"Stephenson","given":"L.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":777903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, P.B.","contributorId":221242,"corporation":false,"usgs":false,"family":"King","given":"P.B.","email":"","affiliations":[],"preferred":false,"id":777904,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Monroe, W. H.","contributorId":9709,"corporation":false,"usgs":true,"family":"Monroe","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777905,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Imlay, R. W.","contributorId":23118,"corporation":false,"usgs":true,"family":"Imlay","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":777906,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70238522,"text":"70238522 - 1942 - Research notes on botulism in western marsh areas with recommendations for control","interactions":[],"lastModifiedDate":"2022-11-28T16:32:16.439679","indexId":"70238522","displayToPublicDate":"1942-12-31T10:28:50","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3637,"text":"Transactions of the North American Wildlife Conference","active":true,"publicationSubtype":{"id":10}},"title":"Research notes on botulism in western marsh areas with recommendations for control","docAbstract":"No abstract available.
","language":"English","publisher":"Wildlife Management Institute","usgsCitation":"Quortrup, E.R., and Sudheimer, R.L., 1942, Research notes on botulism in western marsh areas with recommendations for control: Transactions of the North American Wildlife Conference, v. 7, p. 284-293.","productDescription":"10 p.","startPage":"284","endPage":"293","costCenters":[],"links":[{"id":409706,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -104.89157196956688,\n 48.6067029701843\n ],\n [\n -126.41965728489834,\n 48.6067029701843\n ],\n [\n -126.41965728489834,\n 33.252275887849834\n ],\n [\n -104.89157196956688,\n 33.252275887849834\n ],\n [\n -104.89157196956688,\n 48.6067029701843\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Quortrup, E. R.","contributorId":81201,"corporation":false,"usgs":true,"family":"Quortrup","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":857733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sudheimer, R. L.","contributorId":299412,"corporation":false,"usgs":false,"family":"Sudheimer","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":857734,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37972,"text":"37972 - 1942 - Wildlife contributions to the Nation's war program","interactions":[],"lastModifiedDate":"2014-07-18T16:34:38","indexId":"37972","displayToPublicDate":"1942-12-01T16:34:05","publicationYear":"1942","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"227","title":"Wildlife contributions to the Nation's war program","docAbstract":"No abstract available.","language":"English","publisher":"United States Dept. of the interior","publisherLocation":"Chicago, IL","usgsCitation":"Sater, E.N., 1942, Wildlife contributions to the Nation's war program: Wildlife Leaflet 227, 13 p.","productDescription":"13 p.","numberOfPages":"13","costCenters":[],"links":[{"id":290500,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7daee4b0b2908510f854","contributors":{"authors":[{"text":"Sater, Edna N.","contributorId":45227,"corporation":false,"usgs":true,"family":"Sater","given":"Edna","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":218709,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206632,"text":"70206632 - 1942 - Reconnaissance survey of the Roberts Mountains, Nevada","interactions":[],"lastModifiedDate":"2024-09-24T18:38:09.426143","indexId":"70206632","displayToPublicDate":"1942-12-01T08:26:06","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Reconnaissance survey of the Roberts Mountains, Nevada","docAbstract":"The Roberts Mountains region, central Nevada, provides an excellent section of Paleozoic rocks ranging from Upper Cambrian to Permian. Major low-angle thrusting is indicated by deformed Ordovician strata resting on Paleozoics of varying age. Overlying a thick breccia zone, the upper thrust plate consists of sandstones, andesitic flows and tuffs, black shales, and bedded cherts (Vinini formation). Ordovician age of the Vinini is established on the basis of graptolite faunules. A belt of Lower to Middle Ordovician graptolitic facies similar to the Vinini formation crosses the Great Basin west of Roberts Mountains. Deposits of roughly the same age in the Roberts Mountains meridian and eastward are dominantly limestone, carrying distinct faunas. Axial planes of overturned folds in the thrust plate dip west, a further indication that the upper thrust plate moved from west to east. Minimum horizontal displacement is 16 miles. The date of thrusting is uncertain, but presumably was later Cretaceous or early Tertiary. Following thrusting, an alaskite stock and rhyolite porphyry plugs were intruded; lava flows and tuffs covered the area in part. Thrust plate and cover of volcanics have been broken into normal fault blocks. The post-thrusting igneous rocks, like volcanic rocks of Utah and New Mexico, are characterized by high potash content.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/GSAB-53-1675","usgsCitation":"Merriam, C., and Anderson, C., 1942, Reconnaissance survey of the Roberts Mountains, Nevada: Geological Society of America Bulletin, v. 53, no. 12, p. 1675-1727, https://doi.org/10.1130/GSAB-53-1675.","productDescription":"53 p.","startPage":"1675","endPage":"1727","costCenters":[],"links":[{"id":369196,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Roberts Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116.47304167084806,\n 39.96228576658174\n ],\n [\n -116.47304167084806,\n 39.69688865629308\n ],\n [\n -116.1191336966752,\n 39.69688865629308\n ],\n [\n -116.1191336966752,\n 39.96228576658174\n ],\n [\n -116.47304167084806,\n 39.96228576658174\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"53","issue":"12","edition":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Merriam, C.W.","contributorId":51350,"corporation":false,"usgs":true,"family":"Merriam","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":775272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, C.A.","contributorId":105277,"corporation":false,"usgs":true,"family":"Anderson","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":775273,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70206629,"text":"70206629 - 1942 - Intrusive rocks in the Blue Ridge plateau, Virginia","interactions":[],"lastModifiedDate":"2019-11-14T07:41:03","indexId":"70206629","displayToPublicDate":"1942-11-30T07:36:17","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Intrusive rocks in the Blue Ridge plateau, Virginia","title":"Intrusive rocks in the Blue Ridge plateau, Virginia","docAbstract":"An injection complex of early pre‐Cambrian age is exposed in the Elk Creek anticline in Grayson County, Virginia. There, sedimentary rocks and diorite have been intruded by the Striped Rock and the Carsonville granites. The granites have metamorphosed, injected, reacted with, and replaced the older rocks to form many mixed types. This injection complex is part of a large area of similar rocks that form the core of the Catoctin Mountain‐Blue Ridge uplift in Virginia, and is much older than the overlying volcanic series of later pre‐Cambrian age. ©1942. American Geophysical Union. All Rights Reserved.
","language":"English ","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00342","issn":"00028606","usgsCitation":"Stose, A., 1942, Intrusive rocks in the Blue Ridge plateau, Virginia: Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 342-342, https://doi.org/10.1029/TR023i002p00342.","productDescription":"1 p.","startPage":"342","endPage":"342","costCenters":[],"links":[{"id":369187,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"Virginia ","county":"Grayson County ","otherGeospatial":"Elk Creek ","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-81.047,36.807],[-80.9888,36.7402],[-80.9835,36.7339],[-80.9817,36.7317],[-80.9806,36.7299],[-80.9764,36.7254],[-80.9747,36.7232],[-80.97,36.7173],[-80.967,36.7137],[-80.9629,36.7083],[-80.9582,36.7034],[-80.9553,36.6998],[-80.9547,36.6989],[-80.9517,36.6953],[-80.9488,36.6922],[-80.9441,36.6859],[-80.9406,36.6814],[-80.9359,36.676],[-80.9341,36.6738],[-80.933,36.6724],[-80.9306,36.6697],[-80.9334,36.6685],[-80.9398,36.676],[-80.9434,36.6765],[-80.9463,36.6744],[-80.95,36.6626],[-80.9485,36.651],[-80.9399,36.6474],[-80.9382,36.647],[-80.9368,36.6474],[-80.9264,36.6412],[-80.932,36.627],[-80.9254,36.6242],[-80.9178,36.6256],[-80.9157,36.634],[-80.916,36.6398],[-80.9142,36.65],[-80.906,36.6405],[-80.8585,36.5844],[-80.8567,36.5821],[-80.838,36.5597],[-80.8632,36.5598],[-80.8992,36.5609],[-80.9072,36.5611],[-80.9123,36.561],[-81.0695,36.5653],[-81.2777,36.5709],[-81.3228,36.5721],[-81.3497,36.5729],[-81.3698,36.5735],[-81.4885,36.5807],[-81.5878,36.588],[-81.6758,36.589],[-81.6475,36.6125],[-81.6279,36.6122],[-81.6198,36.6124],[-81.6124,36.6143],[-81.6108,36.6171],[-81.6052,36.6407],[-81.5972,36.6436],[-81.5875,36.6447],[-81.5824,36.647],[-81.574,36.6544],[-81.5672,36.6577],[-81.5557,36.6579],[-81.5454,36.6586],[-81.5386,36.6614],[-81.53,36.6828],[-81.5296,36.6892],[-81.5447,36.6976],[-81.5466,36.7007],[-81.5449,36.7035],[-81.5375,36.705],[-81.5191,36.7053],[-81.5061,36.7109],[-81.4849,36.7122],[-81.4649,36.7166],[-81.4557,36.7186],[-81.4425,36.7179],[-81.4317,36.7203],[-81.4061,36.732],[-81.3851,36.7392],[-81.3656,36.7431],[-81.309,36.7508],[-81.2907,36.7551],[-81.2736,36.7622],[-81.2622,36.7651],[-81.2559,36.7652],[-81.2461,36.7635],[-81.2328,36.7632],[-81.2259,36.7615],[-81.2138,36.7599],[-81.196,36.7597],[-81.1875,36.7634],[-81.184,36.7639],[-81.1714,36.7623],[-81.1668,36.7633],[-81.1645,36.766],[-81.16,36.7688],[-81.156,36.7689],[-81.1439,36.7663],[-81.1347,36.7664],[-81.1163,36.7689],[-81.0985,36.7683],[-81.0916,36.7688],[-81.0882,36.7716],[-81.0867,36.7784],[-81.0879,36.7838],[-81.0857,36.7875],[-81.0789,36.7903],[-81.0635,36.7973],[-81.0545,36.8042],[-81.047,36.807]]]},\"properties\":{\"name\":\"Grayson\",\"state\":\"VA\"}}]}","volume":"23","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Stose, Anna","contributorId":220607,"corporation":false,"usgs":true,"family":"Stose","given":"Anna","email":"","affiliations":[],"preferred":false,"id":775263,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220499,"text":"5220499 - 1942 - Notes on the Alleghenian least weasel in Virginia","interactions":[],"lastModifiedDate":"2025-03-05T17:52:06.003301","indexId":"5220499","displayToPublicDate":"1942-11-14T00:00:00","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Notes on the Alleghenian least weasel in Virginia","docAbstract":"No abstract available.
","language":"English","publisher":"Oxford Academic","doi":"10.1093/jmammal/23.4.439-a","usgsCitation":"Llewellyn, L.M., 1942, Notes on the Alleghenian least weasel in Virginia: Journal of Mammalogy, v. 23, no. 4, p. 439-441, https://doi.org/10.1093/jmammal/23.4.439-a.","productDescription":"3 p.","startPage":"439","endPage":"441","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197032,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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\"}}]}","volume":"23","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6969c4","contributors":{"authors":[{"text":"Llewellyn, L. M.","contributorId":104998,"corporation":false,"usgs":true,"family":"Llewellyn","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":331918,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213116,"text":"70213116 - 1942 - Monthly evapo‐transpiration losses from natural drainage‐basin","interactions":[],"lastModifiedDate":"2020-09-09T19:57:53.587761","indexId":"70213116","displayToPublicDate":"1942-09-09T14:46:21","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Monthly evapo‐transpiration losses from natural drainage‐basin","docAbstract":"With limited restrictions the hydrologic cycle in a given area may be expressed essentially as follows: P = (R + E + ΔFm) in which P represents the precipitation during a given period, R that portion which has reached or will reach the stream‐channel either through surface or subsurface paths, E that part which is evaporated from land and water surfaces and transpired by vegetation during the same period, and ΔFm the change in field‐moisture content during the period. In general both E and Fm are unknown. When the period of time considered in the above expression is long, ΔFm may be neglected and then the evapo‐transpiration losses equal the difference between P (rainfall) and R (runoff) [see 1 of “References” at end of paper]; on the other hand, when the period of time considered is short and considerable rain has fallen then E may be neglected and ΔFm equals the difference between P and R represents water stored as an increment to field‐moisture to be disposed of by evapo‐transpiration during subsequent rainless periods [2].
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00604","usgsCitation":"Langbein, W., 1942, Monthly evapo‐transpiration losses from natural drainage‐basin: Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 604-614, https://doi.org/10.1029/TR023i002p00604.","productDescription":"11 p.","startPage":"604","endPage":"614","costCenters":[],"links":[{"id":378282,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Langbein, Walter B.","contributorId":98294,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter B.","affiliations":[],"preferred":false,"id":798281,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213115,"text":"70213115 - 1942 - Recharge to ground‐water from floods in a typical desert wash, Pinal County, Arizona","interactions":[],"lastModifiedDate":"2020-09-09T19:41:53.838049","indexId":"70213115","displayToPublicDate":"1942-09-09T14:37:34","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Recharge to ground‐water from floods in a typical desert wash, Pinal County, Arizona","docAbstract":"Queen Creek, considered in this paper, is a typical large desert wash. It rises in the Pinal Mountains near the mining town of Superior and enters the outwash‐plain at Black Point about three miles north of Florence Junction (see Fig. 1). Thence it passes over the desert in a southwesterly direction toward Chandler, spreads over the lowlands, and disappears. The flow of the stream consists almost entirely of storm‐water and is of the quick, flashy type common to the deserts of the Southwest. In ordinary years the stream is dry most of the time. Formerly the flood‐waters spread over the floor of the desert and did no harm. Now, however, they invade highly cultivated lands that are irrigated with water from Salt River or from wells, and cause serious damage to both crops and canals. The damage could be prevented by storing the stormwaters in a reservoir formed by a dam at or above Black Point.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00049","usgsCitation":"Babcock, H.M., and Cushing, E.M., 1942, Recharge to ground‐water from floods in a typical desert wash, Pinal County, Arizona: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 49-56, https://doi.org/10.1029/TR023i001p00049.","productDescription":"8 p.","startPage":"49","endPage":"56","costCenters":[],"links":[{"id":378281,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","city":"Pinal","otherGeospatial":"Queens Creek Area","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-110.4491,33.1944],[-110.4484,32.5144],[-110.5485,32.5139],[-110.685,32.5147],[-110.6942,32.5143],[-110.7045,32.5145],[-110.7562,32.5146],[-110.8405,32.5136],[-110.8405,32.5114],[-110.8546,32.512],[-110.9509,32.5124],[-111.0634,32.5121],[-111.0982,32.5119],[-111.1547,32.5114],[-111.1548,32.5028],[-111.2054,32.5027],[-111.2228,32.5028],[-111.2625,32.5031],[-111.4468,32.5023],[-111.4642,32.5019],[-111.4712,32.5019],[-111.5674,32.5019],[-111.5674,32.5069],[-111.5875,32.507],[-111.655,32.5067],[-111.6723,32.5063],[-111.7218,32.5065],[-111.7397,32.507],[-111.7566,32.5065],[-111.7898,32.5066],[-111.7936,32.5066],[-112.0996,32.5077],[-112.2029,32.5071],[-112.2021,32.5955],[-112.2022,32.6405],[-112.2023,32.682],[-112.2023,32.6952],[-112.2024,32.7221],[-112.2025,32.7553],[-112.2025,32.7699],[-112.2025,32.7817],[-112.2026,32.7922],[-112.202,32.799],[-112.2021,32.8241],[-112.2016,32.8568],[-112.2023,32.8869],[-112.2018,32.9324],[-112.2013,32.9434],[-112.2019,32.9443],[-112.2014,32.9884],[-112.2014,33.0034],[-112.2015,33.0317],[-112.1999,33.0317],[-112.2,33.0772],[-112.2,33.0913],[-112.1995,33.1068],[-112.2001,33.119],[-112.2002,33.165],[-112.1998,33.2064],[-112.2004,33.2483],[-112.1999,33.2633],[-112.2,33.2915],[-112.2017,33.2915],[-112.2011,33.3079],[-112.1989,33.3061],[-112.1973,33.302],[-112.1962,33.2965],[-112.1951,33.2902],[-112.1912,33.2806],[-112.189,33.2774],[-112.184,33.2743],[-112.1807,33.2715],[-112.1785,33.2683],[-112.1785,33.2643],[-112.1752,33.2597],[-112.1719,33.2588],[-112.1692,33.257],[-112.1653,33.2584],[-112.1609,33.2579],[-112.1554,33.2543],[-112.1533,33.2547],[-112.1505,33.2561],[-112.1445,33.2552],[-112.1428,33.2552],[-112.1395,33.2538],[-112.1384,33.252],[-112.1373,33.2498],[-112.1395,33.2452],[-112.1379,33.2425],[-112.1346,33.2397],[-112.1324,33.2393],[-112.1307,33.2379],[-112.1285,33.2384],[-112.1247,33.2384],[-112.1214,33.2375],[-112.1176,33.2343],[-112.1148,33.2352],[-112.1093,33.2343],[-112.1055,33.2352],[-112.1038,33.2334],[-112.0984,33.2284],[-112.0956,33.2275],[-112.0945,33.2275],[-112.0912,33.2275],[-112.0896,33.2243],[-112.089,33.2211],[-112.0874,33.2184],[-112.0874,33.2143],[-112.0857,33.2107],[-112.083,33.2098],[-112.0813,33.2084],[-112.0764,33.2052],[-111.8905,33.2038],[-111.6832,33.2048],[-111.58,33.2054],[-111.5819,33.3801],[-111.5786,33.3806],[-111.5792,33.4661],[-111.5099,33.4658],[-111.4741,33.4661],[-111.4576,33.466],[-111.4405,33.4664],[-111.0647,33.4649],[-111.0344,33.4651],[-111.0262,33.4518],[-111.0032,33.4043],[-110.993,33.3846],[-110.986,33.3722],[-110.9759,33.344],[-110.9616,33.3033],[-110.9537,33.281],[-110.9431,33.2527],[-110.8814,33.1506],[-110.8723,33.1359],[-110.8632,33.1208],[-110.8547,33.1062],[-110.852,33.1016],[-110.8456,33.0924],[-110.8365,33.0782],[-110.807,33.0337],[-110.8006,33.0228],[-110.7807,32.9862],[-110.7643,32.9873],[-110.763,33.0047],[-110.7563,33.0054],[-110.7459,33.0101],[-110.7277,33.0271],[-110.7268,33.0281],[-110.7265,33.0292],[-110.7274,33.0359],[-110.7217,33.0425],[-110.715,33.0426],[-110.7146,33.0508],[-110.7245,33.0702],[-110.7197,33.0764],[-110.7102,33.0814],[-110.7054,33.0837],[-110.6913,33.077],[-110.6889,33.0783],[-110.6868,33.0814],[-110.6866,33.084],[-110.6866,33.0861],[-110.6842,33.0882],[-110.6822,33.0894],[-110.6831,33.099],[-110.678,33.1118],[-110.664,33.119],[-110.6615,33.1193],[-110.6605,33.1118],[-110.6552,33.1138],[-110.6375,33.1344],[-110.6329,33.142],[-110.6084,33.1432],[-110.5984,33.1385],[-110.5847,33.1381],[-110.5668,33.1447],[-110.5504,33.1529],[-110.5488,33.157],[-110.5446,33.1678],[-110.543,33.1687],[-110.535,33.1608],[-110.5308,33.1596],[-110.5284,33.1589],[-110.5278,33.1589],[-110.5266,33.1595],[-110.5244,33.161],[-110.525,33.1633],[-110.5262,33.164],[-110.5285,33.1639],[-110.5297,33.1639],[-110.5319,33.1646],[-110.5325,33.1657],[-110.5322,33.1679],[-110.5269,33.1711],[-110.5251,33.178],[-110.5216,33.1783],[-110.5192,33.1786],[-110.5149,33.1804],[-110.509,33.1839],[-110.5039,33.1857],[-110.4762,33.1829],[-110.4644,33.1834],[-110.4608,33.1852],[-110.463,33.1925],[-110.4531,33.1984],[-110.4491,33.1944]]]},\"properties\":{\"name\":\"Pinal\",\"state\":\"AZ\"}}]}","volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Babcock, H. M.","contributorId":90698,"corporation":false,"usgs":true,"family":"Babcock","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":798279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cushing, E. M.","contributorId":94273,"corporation":false,"usgs":true,"family":"Cushing","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":798280,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70213114,"text":"70213114 - 1942 - Recharge and discharge of the ground‐water reservoirs on the High Plains in Texas","interactions":[],"lastModifiedDate":"2020-09-09T19:35:59.486953","indexId":"70213114","displayToPublicDate":"1942-09-09T14:32:01","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Recharge and discharge of the ground‐water reservoirs on the High Plains in Texas","docAbstract":"The High Plains in Texas occupy an area of about 35,000 square miles extending from the northern boundary of the Panhandle southward about 300 miles, and from the New Mexico line eastward an average distance of about 120 miles to a boundary which in most places is sharply defined by a bold escarpment several hundred feet in height.
The region is noted for its abundant supply of ground‐water, most of which is found in the Ogallala formation, a sandy deposit lying at or near the surface throughout most of the region, and reaching a depth of between 200 and 300 feet. The Ogallala formerly extended over a much greater area, but it has been removed by erosion from much of the territory it once occupied. The areas in which it remains are the High Plains, which are bounded by prominent escarpments both on the east and on the west, and are traversed in Texas by the Canadian River, which is deeply entrenched in the older rocks. The water‐bearing sands of the Ogallala in both segments are cut off in all directions from any underground connection, except through the underlying older rocks which contain highly mineralized water unlike the fresh water in the Ogallala. The source of the fresh water, therefore, is within the High Plains themselves, and is from the rain and snow that falls on the surface of the Plains.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00009","usgsCitation":"Broadhurst, W., 1942, Recharge and discharge of the ground‐water reservoirs on the High Plains in Texas: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 9-15, https://doi.org/10.1029/TR023i001p00009.","productDescription":"7 p.","startPage":"9","endPage":"15","costCenters":[],"links":[{"id":378280,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Broadhurst, W. L.","contributorId":55414,"corporation":false,"usgs":true,"family":"Broadhurst","given":"W. L.","affiliations":[],"preferred":false,"id":798278,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213113,"text":"70213113 - 1942 - Recharge, movement, and discharge in the Edwards Limestone Reservoir, Texas","interactions":[],"lastModifiedDate":"2020-09-09T18:18:37.876063","indexId":"70213113","displayToPublicDate":"1942-09-09T13:03:32","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Recharge, movement, and discharge in the Edwards Limestone Reservoir, Texas","docAbstract":"The Edwards limestone of Lower Cretaceous age is the principal water‐bearing formation in a belt 5 to 25 miles wide that extends from Austin southwest to San Antonio and thence west through Uvalde and Del Rio to Comstock, a distance of about 250 miles (see Fig. 1). Throughout this belt it supplies water to wells for stock, industrial, irrigation, and municipal use and to a series of fault‐springs, some of which are among the largest in the United States. These springs have played an important part in the economic and cultural development of Texas. In 1718 the Spaniards stationed a department of light infantry near the springs at San Antonio and soon after established missions and constructed elaborate systems of canals for irrigating considerable areas. After the winning of Texas' independence large numbers of settlers moved into the area. This influx was greatly accelerated following the admission of Texas to the Federal Union and towns were soon established near all of the major springs. However, it was not until about 1880 that the rapid development of the Edwards limestone aquifer by wells was begun.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00019","usgsCitation":"Sayre, A., and Bennett, R., 1942, Recharge, movement, and discharge in the Edwards Limestone Reservoir, Texas: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 19-27, https://doi.org/10.1029/TR023i001p00019.","productDescription":"9 p.","startPage":"19","endPage":"27","costCenters":[],"links":[{"id":378279,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Edwards Limestone Reservoir","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -101.3818359375,\n 29.554345125748267\n ],\n [\n -100.01953125,\n 27.430289738862594\n ],\n [\n -98.9208984375,\n 25.819671943904044\n ],\n [\n -97.470703125,\n 27.01998400798257\n ],\n [\n -97.646484375,\n 30.031055426540206\n ],\n [\n -100.0634765625,\n 30.694611546632277\n ],\n [\n -102.12890625,\n 30.35391637229704\n ],\n [\n -101.3818359375,\n 29.554345125748267\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Sayre, A.N.","contributorId":84339,"corporation":false,"usgs":true,"family":"Sayre","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":798276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bennett, R.R.","contributorId":104880,"corporation":false,"usgs":true,"family":"Bennett","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":798277,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70213112,"text":"70213112 - 1942 - Solution‐phenomena in the Pecos basin in New Mexico","interactions":[],"lastModifiedDate":"2020-09-10T13:22:15.857176","indexId":"70213112","displayToPublicDate":"1942-09-09T12:35:17","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Solution‐phenomena in the Pecos basin in New Mexico","docAbstract":"The drainage‐basin of the Pecos River in New Mexico is a broad asymmetric trough extending from the Sangre de Cristo Mountains southward into Texas (see Fig. 1). It is bounded on the east by the westward facing escarpment of the High Plains and on the west by the crests of the Guadalupe, Sacramento and Sierra Blanca mountains, and a poorly defined divide extending northward through Gallinas Mountain and Pedernal Mountain to Glorieta Mesa. Most of the basin is formed by extensive upland erosion‐surfaces that slope gently toward the river. The valley proper, through much of its length, is relatively narrow and is bounded by steep marginal bluffs, but in some sections, notably between Acme and Lakewood (the Roswell artesian basin) and between Carlsbad and Black River, it is considerably expanded and the lowlands adjoining the river extend from 3 to 16 miles back from the river.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00027","usgsCitation":"Morgan, A., 1942, Solution‐phenomena in the Pecos basin in New Mexico: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 27-25, https://doi.org/10.1029/TR023i001p00027.","productDescription":"9 p.","startPage":"27","endPage":"25","costCenters":[],"links":[{"id":378278,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Pecos River Drainage Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.1396484375,\n 35.94243575255426\n ],\n [\n -106.45751953125,\n 36.03133177633187\n ],\n [\n -107.99560546875,\n 35.67514743608467\n ],\n [\n -107.4462890625,\n 33.211116472416855\n ],\n [\n -107.20458984375,\n 32.008075959291055\n ],\n [\n -103.24951171875,\n 32.045332838858506\n ],\n [\n -103.1396484375,\n 35.94243575255426\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"1","edition":"18","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Morgan, Arthur M.","contributorId":59051,"corporation":false,"usgs":true,"family":"Morgan","given":"Arthur M.","affiliations":[],"preferred":false,"id":798436,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213111,"text":"70213111 - 1942 - Quality of stored water available for use in the lower basin of the Pecos River, Texas","interactions":[],"lastModifiedDate":"2020-09-09T17:34:29.239201","indexId":"70213111","displayToPublicDate":"1942-09-09T12:24:41","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Quality of stored water available for use in the lower basin of the Pecos River, Texas","docAbstract":"Storage of water in reservoir s may be for (1) irrigation, (2) power‐generation sometimes in connection with releases for irrigation, (3) flood‐control, (4) recreation, or combinations of these four uses. The control of releases of the stored water may involve conflicts of interests as to the best use of the available supply.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00593","usgsCitation":"Howard, C.S., 1942, Quality of stored water available for use in the lower basin of the Pecos River, Texas: Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 593-598, https://doi.org/10.1029/TR023i002p00593.","productDescription":"6 p.","startPage":"593","endPage":"598","costCenters":[],"links":[{"id":378277,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas, New Mexico","otherGeospatial":"Pecos River Drainage Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102.83203125,\n 36.13787471840729\n ],\n [\n -106.69921875,\n 36.13787471840729\n ],\n [\n -106.5234375,\n 34.813803317113155\n ],\n [\n -106.171875,\n 33.100745405144245\n ],\n [\n -105.4248046875,\n 31.5504526754715\n ],\n [\n -103.4912109375,\n 30.486550842588485\n ],\n [\n -101.6455078125,\n 30.637912028341123\n ],\n [\n -100.94238281249999,\n 33.50475906922609\n ],\n [\n -101.29394531249999,\n 36.06686213257888\n ],\n [\n -102.83203125,\n 36.13787471840729\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":798275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213109,"text":"70213109 - 1942 - Hydraulic criteria for sand‐waves ","interactions":[],"lastModifiedDate":"2020-09-09T17:24:00.712348","indexId":"70213109","displayToPublicDate":"1942-09-09T12:10:10","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Hydraulic criteria for sand‐waves ","docAbstract":"Sand‐waves on rivers are rhythmic successions of waves which occur at flood‐stages of streams heavily loaded with sediments. They take their name from the fact that sand and associated silts and gravels form a large part of the load transported by a river at such times. They seem to be peculiar to the Southwest and many vivid descriptions of them can be found in the literature of that region. R. C. PIERCE [see 1 of “References” at end of paper[, who observed many sand‐waves on the San Juan River in Utah, has described them as resembling in appearance “the waves thrown up by a stern‐wheel river steamboat.” He further describes their appearances as follows: “The sand‐waves are not continuous, but follow a rhythmic movement. At one moment the stream is running smoothly for a distance of perhaps several hundred yards. Then suddenly a number of waves, usually from six to ten, appear. They reach their full size in a few seconds, flow for perhaps two or three minutes, then suddenly disappear. Often, for perhaps half a minute before disappearing, the crests of the waves go through a combing movement, accompanied by a roaring sound. On first appearance it seems that the wave‐forms occupy fixed positions, but by watching them closely it is seen that they move slowly upstream. In the narrow parts of the stream the waves may reach nearly the width of the river, but in the wider parts they occupy smaller proportional widths. Usually they are at right‐angles to the axis of the stream, but at some places, particularly in the wider parts of the river, they may suddenly assume a diagonal position, moving rather rapidly across the stream in the direction toward which the upstream side of the wave has turned.” Many such descriptions may be found which in the main bear out PIERCE'S account, varying, however, as to size of wave, rate, and sometimes as to direction of movement.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00615","usgsCitation":"Langbein, W., 1942, Hydraulic criteria for sand‐waves : Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 615-619, https://doi.org/10.1029/TR023i002p00615.","productDescription":"4 p.","startPage":"615","endPage":"619","costCenters":[],"links":[{"id":378276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Langbein, Walter B.","contributorId":98294,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter B.","affiliations":[],"preferred":false,"id":798274,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213108,"text":"70213108 - 1942 - Report of Committee on Underground Waters, 1941–42","interactions":[],"lastModifiedDate":"2020-09-09T17:02:34.270957","indexId":"70213108","displayToPublicDate":"1942-09-09T11:51:57","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of Committee on Underground Waters, 1941–42","docAbstract":"So many ground‐water hydrologists are engaged on problems relating directly to the war that the usual annual inquiry for information as to projects that deserve review in the annual report of the Committee on Underground Waters brought relatively little response. It is in part for this reason, but also in part because the Chairman of the Committee is busy on war problems, that this report is shorter than usual.
The Boise River Project in southwestern Idaho comprises an area of about 333,000 acres of highly developed agricultural land. Precipitation in the irrigated valley averages about ten inches a year which is too low to support any but desert vegetation. Water for irrigation during the growing season is obtained from Arrowrock Reservoir located on the Boise River four miles above Moore Creek, and from Deer Flat Reservoir near Nampa. The deposition of sediment in the river‐channel, in irrigation‐canals, and in farm‐laterals has interfered with the normal operation of the irrigation‐system and has occasionally required the expenditure of considerable time and money for removal of the deposited material.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00652","usgsCitation":"Love, S.K., and Benedict, P.C., 1942, Sediment loads in the Moore Creek drainage‐basin, Idaho 1939–40: Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 652-657, https://doi.org/10.1029/TR023i002p00652.","productDescription":"6 p.","startPage":"652","endPage":"657","costCenters":[],"links":[{"id":378272,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Moore Creek Drainage","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.3232421875,\n 43.49676775343911\n ],\n [\n -115.27954101562499,\n 43.49676775343911\n ],\n [\n -115.27954101562499,\n 44.46123053905879\n ],\n [\n -116.3232421875,\n 44.46123053905879\n ],\n [\n -116.3232421875,\n 43.49676775343911\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":798266,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benedict, Paul Charles","contributorId":32135,"corporation":false,"usgs":true,"family":"Benedict","given":"Paul","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":798267,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70213071,"text":"70213071 - 1942 - Runoff in the Santa Ynez River Basin, California, following the excessive rainfall of 1940–41","interactions":[],"lastModifiedDate":"2020-09-08T20:29:41.286539","indexId":"70213071","displayToPublicDate":"1942-09-08T15:24:21","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Runoff in the Santa Ynez River Basin, California, following the excessive rainfall of 1940–41","docAbstract":"This paper reports briefly on the runoff‐characteristics of the Santa Ynez River in Santa Barbara County, California, following the excessive rainfall in the winter of 1940–41; also, it contrasts these conditions of 1940–41 with earlier years of less rainfall. The data for this report were compiled in connection with an investigation of the water‐resources of Santa Barbara County which is being conducted by the United States Geological Survey in cooperation with the County of Santa Barbara.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00124","usgsCitation":"LaRocque, G., 1942, Runoff in the Santa Ynez River Basin, California, following the excessive rainfall of 1940–41: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 124-129, https://doi.org/10.1029/TR023i001p00124.","productDescription":"6 p.","startPage":"124","endPage":"129","costCenters":[],"links":[{"id":378227,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Santa Ynez River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.673828125,\n 34.35704160076073\n ],\n [\n -119.5751953125,\n 34.35704160076073\n ],\n [\n -119.5751953125,\n 34.88593094075317\n ],\n [\n -120.673828125,\n 34.88593094075317\n ],\n [\n -120.673828125,\n 34.35704160076073\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"LaRocque, G.A. Jr.","contributorId":22837,"corporation":false,"usgs":true,"family":"LaRocque","given":"G.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":798101,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213070,"text":"70213070 - 1942 - Ground‐water studies in the Southwest ","interactions":[],"lastModifiedDate":"2020-09-08T20:23:59.148789","indexId":"70213070","displayToPublicDate":"1942-09-08T15:19:02","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Ground‐water studies in the Southwest ","docAbstract":"Geologists are concerned with the rock‐systems that form the crust of the Earth. The groundwater geologists are concerned with the rock‐systems specifically because the open spaces which the rocks contain serve as reservoirs and conduits for water—water which performs a large part of the geologic work that is in progress today and has been in progress during past ages; water which affects profoundly the whole hydrologic cycle and is still the principal source of water‐supply for mankind, as it has been for primitive man and the other land animals before the time of artificial waterworks.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00006","usgsCitation":"Meinzer, O.E., 1942, Ground‐water studies in the Southwest : Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 6-9, https://doi.org/10.1029/TR023i001p00006.","productDescription":"4 p.","startPage":"6","endPage":"9","costCenters":[],"links":[{"id":378226,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":798100,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213069,"text":"70213069 - 1942 - Report of committee on the chemistry of natural waters, 1941–42","interactions":[],"lastModifiedDate":"2020-09-09T13:53:38.452258","indexId":"70213069","displayToPublicDate":"1942-09-08T15:14:10","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of committee on the chemistry of natural waters, 1941–42","docAbstract":"The membership of the Committee during the past year was as follows: I. A. Dennison, National Bureau of Standards; C S. Howard (Chairman), Geological Survey; C. S. Scofield, Department of Agriculture; D. G. Thompson, Geological Survey; and T. G. Thompson, University of Washington, Seattle, Washington.
SCOFIELD has continued his studies in connection with the salt balance in irrigated areas and has made progress‐reports to interested parties concerning the salt balance on the El Paso Project, Wapato Project, and the Yuma Project. These studies are of great interest to those responsible for the operation of the projects and should be of considerable value to other projects in indicating the volumes of water that may be necessary under certain conditions to insure proper drainage of the project.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00466","usgsCitation":"Howard, C.S., 1942, Report of committee on the chemistry of natural waters, 1941–42: Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 466-467, https://doi.org/10.1029/TR023i002p00466.","productDescription":"2 p.","startPage":"466","endPage":"467","costCenters":[],"links":[{"id":378225,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":798099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213067,"text":"70213067 - 1942 - Origin of the Ayer granodiorite in the Lowell area, Massachusetts","interactions":[],"lastModifiedDate":"2020-09-09T13:55:31.765838","indexId":"70213067","displayToPublicDate":"1942-09-08T15:10:47","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Origin of the Ayer granodiorite in the Lowell area, Massachusetts","docAbstract":"The elongate stock of Ayer granodiorite exposed north and west of Lowell, Massachusetts, is reasonably typical of the many bodies of granitic rocks in the central and north‐central parts of the State. It lies within a terrane composed predominantly of steeply tilted, thinly inter bedded quartzite and biotite schist, and many of its structural relations superficially suggest for it a metasomatic origin, involving the quiet replacement of preexisting bedded and foliated rocks by invading fluids of magmatic derivation. The elongation of the stock and a distinct foliation characteristic of the granodiorite itself are both essentially conformable with country‐rock structure, and the contacts, wherever seen, also appear to be concordant. This general parallelism is further emphasized by a consistent orientation of numerous tabular inclusions, the edges of most of which have been obscured by reaction with the igneous material. Moreover, apparent transitions from country‐rock into granodiorite in a direction parallel to their structural trends occur at several places. Dikes and lenses of pegmatite are abundant within and adjacent to the granodiorite body.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i002p00341-2","usgsCitation":"Jahns, R., 1942, Origin of the Ayer granodiorite in the Lowell area, Massachusetts: Eos, Transactions, American Geophysical Union, v. 23, no. 2, p. 341-342, https://doi.org/10.1029/TR023i002p00341-2.","productDescription":"2 p.","startPage":"341","endPage":"342","costCenters":[],"links":[{"id":378224,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","city":"Lowell","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.378173828125,\n 42.593532625649935\n ],\n [\n -71.26007080078125,\n 42.593532625649935\n ],\n [\n -71.26007080078125,\n 42.65012181368022\n ],\n [\n -71.378173828125,\n 42.65012181368022\n ],\n [\n -71.378173828125,\n 42.593532625649935\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jahns, Richard H.","contributorId":107757,"corporation":false,"usgs":true,"family":"Jahns","given":"Richard H.","affiliations":[],"preferred":false,"id":798098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213066,"text":"70213066 - 1942 - Results of pumping tests of the Carrizo sand in the Lufkin area, Texas","interactions":[],"lastModifiedDate":"2020-09-08T20:08:28.039461","indexId":"70213066","displayToPublicDate":"1942-09-08T15:02:23","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Results of pumping tests of the Carrizo sand in the Lufkin area, Texas","docAbstract":"The Lufkin Area, as the term is used in this paper, is comprised of Angelina and Nacogdoches counties, Texas, and parts of adjoining counties. Its surface is gently rolling, with a maximum relief of about 150 feet and a maximum altitude of less than 400 feet. The average annual rainfall is about 45 inches. Practically all of the water‐supplies in the area come from ground‐water and it has been found that the Carrizo sand contains water of better quality and is more productive than any other water‐bearing formation in the area [see 1 of “References” at end of paper]. Figure 1 is a map of the area, showing the positions of the cities of Lufkin and Nacogdoches, the wells of the Southland Paper Mill, and other wells mentioned in this paper.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00040","usgsCitation":"Guyton, W., 1942, Results of pumping tests of the Carrizo sand in the Lufkin area, Texas: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 40-48, https://doi.org/10.1029/TR023i001p00040.","productDescription":"9 p.","startPage":"40","endPage":"48","costCenters":[],"links":[{"id":378223,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Lufkin Area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.086669921875,\n 31.287939892641734\n ],\n [\n -94.48791503906249,\n 31.287939892641734\n ],\n [\n -94.48791503906249,\n 31.695455797778713\n ],\n [\n -95.086669921875,\n 31.695455797778713\n ],\n [\n -95.086669921875,\n 31.287939892641734\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Guyton, W.F.","contributorId":11688,"corporation":false,"usgs":true,"family":"Guyton","given":"W.F.","affiliations":[],"preferred":false,"id":798097,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213064,"text":"70213064 - 1942 - Manganese-bearing veins in southwestern Virginia","interactions":[],"lastModifiedDate":"2020-09-08T19:28:14.089444","indexId":"70213064","displayToPublicDate":"1942-09-08T14:24:19","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Manganese-bearing veins in southwestern Virginia","docAbstract":"Veins carrying manganese silicates largely in the form of the manganese garnet, spessartite, occur in the crystalline schists and gneisses of Carroll and Grayson Counties, Virginia, in the southern parts of the Galax and Independence quadrangles just north of the North Carolina State line. This brief paper includes a discussion of these manganese-bearing veins which are described in a report on the Geology and Mineral resources of the Great Gossan Lead district prepared by G. W. Stose and the writer for publication by the Virginia Geological Survey
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.37.5.408","usgsCitation":"Jonas, A., 1942, Manganese-bearing veins in southwestern Virginia: Economic Geology, v. 37, no. 5, p. 408-423, https://doi.org/10.2113/gsecongeo.37.5.408.","productDescription":"16 p.","startPage":"408","endPage":"423","costCenters":[],"links":[{"id":378220,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Virginia","otherGeospatial":"Blue Ridge Plateau","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.57623291015625,\n 36.55598153635691\n ],\n [\n -80.81817626953125,\n 36.55598153635691\n ],\n [\n -80.81817626953125,\n 36.767492156196745\n ],\n [\n -81.57623291015625,\n 36.767492156196745\n ],\n [\n -81.57623291015625,\n 36.55598153635691\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"37","issue":"5","noUsgsAuthors":false,"publicationDate":"1942-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Jonas, Anna I.","contributorId":73466,"corporation":false,"usgs":true,"family":"Jonas","given":"Anna I.","affiliations":[],"preferred":false,"id":798095,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213063,"text":"70213063 - 1942 - Differential density of ground water in ore deposition","interactions":[],"lastModifiedDate":"2020-09-08T19:22:52.636571","indexId":"70213063","displayToPublicDate":"1942-09-08T14:14:09","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Differential density of ground water in ore deposition","docAbstract":"No abstract available.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.37.5.424","usgsCitation":"McKnight, E., 1942, Differential density of ground water in ore deposition: Economic Geology, v. 37, no. 5, p. 424-426, https://doi.org/10.2113/gsecongeo.37.5.424.","productDescription":"3 p.","startPage":"424","endPage":"426","costCenters":[],"links":[{"id":378219,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"5","noUsgsAuthors":false,"publicationDate":"1942-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"McKnight, Edwin T.","contributorId":85039,"corporation":false,"usgs":true,"family":"McKnight","given":"Edwin T.","affiliations":[],"preferred":false,"id":798094,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213062,"text":"70213062 - 1942 - Differential density of ground water in ore deposition","interactions":[],"lastModifiedDate":"2020-09-08T19:05:53.227005","indexId":"70213062","displayToPublicDate":"1942-09-08T14:03:17","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Differential density of ground water in ore deposition","docAbstract":"No abstract available.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.37.6.524","usgsCitation":"Cedarstrom, D., 1942, Differential density of ground water in ore deposition: Economic Geology, v. 37, p. 524-524, https://doi.org/10.2113/gsecongeo.37.6.524.","productDescription":"1 p.","startPage":"524","endPage":"524","costCenters":[],"links":[{"id":378218,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cedarstrom, D.J.","contributorId":102127,"corporation":false,"usgs":true,"family":"Cedarstrom","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":798093,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207285,"text":"70207285 - 1942 - Deep‐seated solution in the Meade basin and vicinity, Kansas and Oklahoma","interactions":[],"lastModifiedDate":"2019-12-16T06:30:25","indexId":"70207285","displayToPublicDate":"1942-08-31T06:24:19","publicationYear":"1942","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Deep‐seated solution in the Meade basin and vicinity, Kansas and Oklahoma","docAbstract":"During the closing years of the 19th century, Haworth [see 1 and 2 of “References” at end of paper] and Johnson [3] noted the abundant depressions resembling sink‐holes in the Southern High Plains, especially in Meade and Clark counties, Kansas, and Beaver County, Oklahoma. Johnson was of the opinion that all the depressions and basins in this region were due to solution, whereas Haworth [1] believed the Meade artesian basin to be structural, although he held to a solutional origin for the Ashland and Englewood basins, which are a few miles to the east. ©1942. American Geophysical Union. All Rights Reserved.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR023i001p00035","issn":"00028606","usgsCitation":"Frye, K., and Schoff, S., 1942, Deep‐seated solution in the Meade basin and vicinity, Kansas and Oklahoma: Eos, Transactions, American Geophysical Union, v. 23, no. 1, p. 35-39, https://doi.org/10.1029/TR023i001p00035.","productDescription":"5 p. ","startPage":"35","endPage":"39","costCenters":[],"links":[{"id":370292,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"Kansas, Oklahoma ","county":"Meade, Clark, Beaver","otherGeospatial":"Meade basin ","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-99.5557,37.4689],[-99.5551,37.3832],[-99.5435,37.3828],[-99.5399,36.9998],[-100.0009,36.9985],[-100.0024,36.9985],[-100.004,36.8538],[-100.0044,36.76],[-100.0045,36.5917],[-100.0044,36.5849],[-100.0038,36.4998],[-100.1458,36.4998],[-100.3204,36.4999],[-100.5459,36.4994],[-100.7022,36.5],[-100.8939,36.4998],[-100.9524,36.4998],[-100.9534,36.8476],[-100.9448,36.8478],[-100.9441,36.9988],[-100.6337,36.9986],[-100.635,37.3881],[-100.6518,37.3878],[-100.652,37.4757],[-100.217,37.4758],[-100.1068,37.4751],[-99.5557,37.4689]]]},\"properties\":{\"name\":\"Clark\",\"state\":\"KS\"}}]}","volume":"23","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Frye, K.C.","contributorId":221248,"corporation":false,"usgs":false,"family":"Frye","given":"K.C.","email":"","affiliations":[],"preferred":false,"id":777540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoff, S.L.","contributorId":107365,"corporation":false,"usgs":true,"family":"Schoff","given":"S.L.","email":"","affiliations":[],"preferred":false,"id":777541,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}