The position and chloride concentration of a sizable body of salt water, moving slowly landsyard from the south-shore bays of Long Island and the Atlantic Ocean were defined by recent test drilling in the Cedarhurst-Woodmere area of southwestern Nassau County, Long Island, N. Most of the salt-water body is in the lower part of a permeable artesian aquifer; the lowermost part of the salt-water body is in clay deposits underlying the permeable aquifer. The upper limit of the salt-water body in this area was found at depths increasing progressively in a landward direction. It was 318 feet below sea level at a well in Cedarhurst and 541 feet below sea level at a well in Woodmere. The lower limit of the salt-water body was determined at depths between 578 and 630 feet below sea level in the Cedarhurst-Woodmere area. The salt-water body is more than 300 feet thick at a well in Cedarhurst, and it thins out to zero in the vicinity of a pumping center about 1- miles northeast of the Cedarhurst well. Chloride concentration in the salt-water body in the Cedarhurst-Woodmere area ranged from about 40 to 16,000 ppm (parts per million). Isochlors define a zone of diffusion about a mile wide in the Cedarhurst-Woodmere area. They indicate a thickness of diffused water ranging from a few tens to more than 150 feet vertically. Electrical-log data show that the upper boundary of the salt-water body moved upward 21 feet between 1952 and 1958 at a site in Woodmere about half a mile southwest of the pumping center. ' From this information it is inferred that between 1952 and 1958 the leading edge of the saltwater front moved landward about 2,000 feet toward the pumping center.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.8.1739","usgsCitation":"Lusczynski, N., and Swarzenski, W., 1960, Position of the salt-water body in the magothy(?) formation in the Cedarhurst-Woodmere area of southwestern Nassau county, Long Island, N.Y.: Economic Geology, v. 55, no. 8, p. 1739-1750, https://doi.org/10.2113/gsecongeo.55.8.1739.","productDescription":"12 p.","startPage":"1739","endPage":"1750","costCenters":[],"links":[{"id":385667,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","county":"Nassau County","otherGeospatial":"Long Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.79241943359375,\n 40.561807971278185\n ],\n [\n -73.48892211914062,\n 40.561807971278185\n ],\n [\n -73.48892211914062,\n 40.92388970852943\n ],\n [\n -73.79241943359375,\n 40.92388970852943\n ],\n [\n -73.79241943359375,\n 40.561807971278185\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"55","issue":"8","noUsgsAuthors":false,"publicationDate":"1960-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Lusczynski, N.J.","contributorId":10779,"corporation":false,"usgs":true,"family":"Lusczynski","given":"N.J.","affiliations":[],"preferred":false,"id":815734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swarzenski, W.V.","contributorId":80243,"corporation":false,"usgs":true,"family":"Swarzenski","given":"W.V.","email":"","affiliations":[],"preferred":false,"id":815735,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5220096,"text":"5220096 - 1960 - Peromyscus ranges at high and low population densities","interactions":[],"lastModifiedDate":"2025-03-06T22:51:26.994478","indexId":"5220096","displayToPublicDate":"1960-11-04T00:00:00","publicationYear":"1960","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":"Peromyscus ranges at high and low population densities","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70170699","usgsCitation":"Cotter, R.D., and Young, L., 1960, Municipal water supplies on the Mesabi and Vermillion Iron Ranges, northeastern Minnesota, 61 p., https://doi.org/10.3133/70170699.","productDescription":"61 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":320732,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Mesabi and Vermillion Iron ranges","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57248673e4b0b13d39159654","contributors":{"authors":[{"text":"Cotter, R. D.","contributorId":89874,"corporation":false,"usgs":true,"family":"Cotter","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":628118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, L.H.","contributorId":169025,"corporation":false,"usgs":false,"family":"Young","given":"L.H.","email":"","affiliations":[],"preferred":false,"id":628119,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70171289,"text":"70171289 - 1960 - An automatic-tracking device for visual-accumulation-tube analysis","interactions":[],"lastModifiedDate":"2018-04-02T10:39:29","indexId":"70171289","displayToPublicDate":"1960-11-01T12:15:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3718,"text":"Water Resources Bulletin","printIssn":"0043-1370","active":true,"publicationSubtype":{"id":10}},"title":"An automatic-tracking device for visual-accumulation-tube analysis","docAbstract":"No abstract available.
","language":"English","publisher":"American Water Resources Association","publisherLocation":"Herndon, VA","usgsCitation":"Skinner, J.V., 1960, An automatic-tracking device for visual-accumulation-tube analysis: Water Resources Bulletin, v. November, p. 135-137.","productDescription":"3 p.","startPage":"135","endPage":"137","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321734,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"November","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57481e2ce4b07e28b664db81","contributors":{"authors":[{"text":"Skinner, J. V.","contributorId":32504,"corporation":false,"usgs":true,"family":"Skinner","given":"J.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":630447,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220495,"text":"70220495 - 1960 - The chief oxide-burgin area discoveries, East Tintic district, Utah; A case history","interactions":[],"lastModifiedDate":"2021-05-17T13:54:52.042882","indexId":"70220495","displayToPublicDate":"1960-11-01T08:47:35","publicationYear":"1960","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":"The chief oxide-burgin area discoveries, East Tintic district, Utah; A case history","docAbstract":"In 1955 exploration for base and precious metals was undertaken by Bear Creek Mining Company immediately north of the Main Tintic district, Utah. During the course of this work Bear Creek became interested in the East Tintic district, primarily as a result of the activities of the U.S. Geological Survey in that area. Data published on the East Tintic district by the Survey and others were studied and map data made available from various mining companies were compiled. Preliminary economic studies were made to determine the present day value of the type of ore body discovered previously in the district. Encouraging results from these investigations led to the selection of specific targets for exploration. Recommendations for a project program were made and approved. Negotiations were successfully concluded in mid-1956 for a unit lease agreement on lands in the East Tintic district owned by the Tintic Standard and Chief Consolidated mining companies and their subsidiaries. Of the targets selected for exploration, the Chief Oxide area seemed to be one of the most prominent. Our preliminary work in the Chief Oxide area corroborated the findings of the U.S. Geological Survey described in Part I of this paper. After careful consideration it was decided to gamble the cost of an exploration shaft in this area for the purpose of providing an underground drilling platform. We also hoped by means of underground workings to establish the existence and nature of the postulated fault. A limited amount of surface drilling was done prior to shaft sinking in order to locate a shaft site and also to obtain additional information of subvolcanic structure and alteration. Underground exploration in the Chief Oxide area was started in January, 1957. The Burgin shaft was sunk to a depth of 1,100 feet and by August, 1959, lateral development on the 1050 level totaled 4,721 feet and underground diamond drilling totaled 15,480 feet. Results of the work done to date are as follows: (a) Identification of the sedimentary rock section and an interpretation of the structure in the Burgin mine area. (b) Discovery by penetration of the previously postulated East Tintic thrust fault. (c) Discovery of large zones of manganese oxides and carbonates, which were found to be closely related to silver-lead-zinc mineralization. (d) Discovery of ore-grade lead-zinc mineralization within the footwall rocks of the East Tintic thrust. (e) Discovery of high-grade silver-lead ore within the thrust zone. Insofar as ore localization is concerned the most important structural feature in the Burgin mine area is the East Tintic thrust fault-a fact that opens up new ore potential over a large part of the East Tintic district not previously explored. Although the discoveries to date must be attributed essentially to the application of geology to exploration, the tools of geochemical prospecting and geophysics were also used, and the geochemical work, in particular, was found to be a definite aid in the selection of areas for further exploration.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.7.1507","usgsCitation":"Bush, J., Cook, D., Lovering, T.S., and Morris, H.T., 1960, The chief oxide-burgin area discoveries, East Tintic district, Utah; A case history: Economic Geology, v. 55, no. 7, p. 1507-1540, https://doi.org/10.2113/gsecongeo.55.7.1507.","productDescription":"34 p.","startPage":"1507","endPage":"1540","costCenters":[],"links":[{"id":385678,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"east Tintic Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.9287109375,\n 38.81831117374662\n ],\n [\n -110.8795166015625,\n 38.81831117374662\n ],\n [\n -110.8795166015625,\n 40.069664523297774\n ],\n [\n -111.9287109375,\n 40.069664523297774\n ],\n [\n -111.9287109375,\n 38.81831117374662\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"55","issue":"7","noUsgsAuthors":false,"publicationDate":"1960-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Bush, J.B.","contributorId":258145,"corporation":false,"usgs":false,"family":"Bush","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":815769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cook, D.R.","contributorId":20585,"corporation":false,"usgs":true,"family":"Cook","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":815770,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lovering, T. S.","contributorId":108085,"corporation":false,"usgs":true,"family":"Lovering","given":"T.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":815771,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Morris, H. T.","contributorId":15585,"corporation":false,"usgs":true,"family":"Morris","given":"H.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":815772,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70220493,"text":"70220493 - 1960 - A rapid and accurate contour interpolator","interactions":[],"lastModifiedDate":"2021-05-17T12:29:58.643014","indexId":"70220493","displayToPublicDate":"1960-11-01T07:26:11","publicationYear":"1960","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":"A rapid and accurate contour interpolator","docAbstract":"An instrument called a \"contourpolator\" is described. The device is constructed from readily available materials costing about $2.00 and consists of 4 primary parts. Detailed instructions are provided for its assembly and use.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.7.1555","usgsCitation":"Marsh, O., 1960, A rapid and accurate contour interpolator: Economic Geology, v. 55, no. 7, p. 1555-1560, https://doi.org/10.2113/gsecongeo.55.7.1555.","productDescription":"6 p.","startPage":"1555","endPage":"1560","costCenters":[],"links":[{"id":385674,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"7","noUsgsAuthors":false,"publicationDate":"1960-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Marsh, O.T.","contributorId":64672,"corporation":false,"usgs":true,"family":"Marsh","given":"O.T.","email":"","affiliations":[],"preferred":false,"id":815763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220489,"text":"70220489 - 1960 - Metallization and post-mineral hypogene argillization, Lost River tin mine, Alaska","interactions":[],"lastModifiedDate":"2021-05-17T12:09:18.380166","indexId":"70220489","displayToPublicDate":"1960-11-01T07:04:22","publicationYear":"1960","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":"Metallization and post-mineral hypogene argillization, Lost River tin mine, Alaska","docAbstract":"The Lost River tin and tungsten deposit occurs in a buried granite pluton and in associated rhyolite dikes that intrude Paleozoic limestone. The dikes and parts of the granite were greisenized and then argillized irregularly. Metallization accompanied greisenization rather than argilli-zation, although both processes probably were closely related in time. Iron-zinc ratios in sphalerite indicate that the ore minerals were deposited at a temperature between 425°C and 740°C. This temperature is within the range of the temperatures at which topaz, a comman associate of the ore minerals, has been synthesized in the laboratory. The temperature of deposition of the ore minerals is above the temperature interval in which clay minerals are stable. Thus, clay minerals could not have formed while ore was being deposited. As temperatures fell and entered the stability range of the clay minerals, argillic alteration encroached upon greisen ores and wall rocks. Reaction rims between quartz and topaz indicate that kaolinite could have formed according to the following reaction: topaz + quartz + water + limestone -* kaolinite + fluorite + Cajj\"C (Al,F)2Si04 + Si02 +3H2O+ CaCOa - Al2Si20B(OH)41 + CaF2 + H2CO3 The clay minerals, which formed from diverse rock types, consist of kaolinite, dickite, mixed-layered chlorite-montmorillonite, and minor montmorillonite, accompanied by variable amounts of muscovite and zinnwaldite. The dickite is most common in and near late veins that cut the earlier-formed greisen. Temperature is believed to be the principal agent governing the relations between ore deposition and argillization. Similar relations are to be expected in other high-temperature deposits where abundant veining and fracturing indicate that wall rocks reached an isothermal condition above a maximum temperature of 480°C during ore deposition.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.7.1478","usgsCitation":"Sainsbury, C., 1960, Metallization and post-mineral hypogene argillization, Lost River tin mine, Alaska: Economic Geology, v. 55, no. 7, p. 1478-1506, https://doi.org/10.2113/gsecongeo.55.7.1478.","productDescription":"29 p.","startPage":"1478","endPage":"1506","costCenters":[],"links":[{"id":385669,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Bering land bridge","volume":"55","issue":"7","noUsgsAuthors":false,"publicationDate":"1960-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Sainsbury, C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":815737,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220488,"text":"70220488 - 1960 - Scheelite in the precambrian gneisses of Colorado","interactions":[],"lastModifiedDate":"2021-05-17T11:59:53.430829","indexId":"70220488","displayToPublicDate":"1960-11-01T06:56:15","publicationYear":"1960","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":"Scheelite in the precambrian gneisses of Colorado","docAbstract":"Scheelite of Precambrian age has been found at several localities in Colorado and Wyoming in recent years. Most of it is disseminated in regionally metamorphosed rocks, principally in calc-silicate gneiss, but also in amphibolite. Small amounts are found in pegmatites and in gold-or copper-quartz veins of Precambrian age. The scheelite in most of the deposits contains molybdenum, and much of it is accompanied by discrete powellite (CaMoCX). The scheelite deposits vary in age with the rocks that contain them and show no consistent genetic associations. Many of the deposits are products of some phase of the major plutonic stage that included regional metamorphism, migmatization, and emplacement of syntectonic granites, A few deposits may be related to younger Precambrian granites, and some are related to late diorite and pegmatite. Tungsten originally present in minor concentration in the sedimentary rocks that gave rise to the gneisses was evidently redistributed and r eery stall ized through successive Precambrian plutonic episodes. Reworked Precambrian deposits may have been a source of the tungsten in the economically important Tertiary deposits, and possibly also of molybdenum. The Precambrian scheelite deposits found thus far have proved to be of minor economic importance, but others are still being found, and many more can be presumed to exist; among these may be some of importance.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.7.1406","usgsCitation":"Tweto, O., 1960, Scheelite in the precambrian gneisses of Colorado: Economic Geology, v. 55, no. 7, p. 1406-1428, https://doi.org/10.2113/gsecongeo.55.7.1406.","productDescription":"13 p.","startPage":"1406","endPage":"1428","costCenters":[],"links":[{"id":385668,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.072265625,\n 37.020098201368114\n ],\n [\n -102.0849609375,\n 37.020098201368114\n ],\n [\n -102.0849609375,\n 40.94671366508002\n ],\n [\n -109.072265625,\n 40.94671366508002\n ],\n [\n -109.072265625,\n 37.020098201368114\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"55","issue":"7","noUsgsAuthors":false,"publicationDate":"1960-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Tweto, O.L.","contributorId":102873,"corporation":false,"usgs":true,"family":"Tweto","given":"O.L.","affiliations":[],"preferred":false,"id":815736,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220752,"text":"5220752 - 1960 - A colored leg strip for marking birds","interactions":[],"lastModifiedDate":"2025-02-03T17:34:08.850404","indexId":"5220752","displayToPublicDate":"1960-10-03T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"A colored leg strip for marking birds","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3796529","usgsCitation":"Campbell, D.L., 1960, A colored leg strip for marking birds: Journal of Wildlife Management, v. 24, no. 4, p. 431-431, https://doi.org/10.2307/3796529.","productDescription":"1 p.","startPage":"431","endPage":"431","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197417,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b10c0","contributors":{"authors":[{"text":"Campbell, D. L.","contributorId":90726,"corporation":false,"usgs":true,"family":"Campbell","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":332383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220751,"text":"5220751 - 1960 - Mallard age and sex determination from wings","interactions":[],"lastModifiedDate":"2025-02-05T15:08:23.791745","indexId":"5220751","displayToPublicDate":"1960-10-03T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Mallard age and sex determination from wings","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3796514","usgsCitation":"Carney, S., and Geis, A.D., 1960, Mallard age and sex determination from wings: Journal of Wildlife Management, v. 24, no. 4, p. 372-381, https://doi.org/10.2307/3796514.","productDescription":"10 p.","startPage":"372","endPage":"381","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":487090,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3796514","text":"Publisher Index Page"},{"id":197416,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Louisiana, Minnesota, 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\"}}]}","volume":"24","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649fb2","contributors":{"authors":[{"text":"Carney, S.M.","contributorId":43869,"corporation":false,"usgs":true,"family":"Carney","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":332381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Geis, A. D.","contributorId":72885,"corporation":false,"usgs":true,"family":"Geis","given":"A.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":332382,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220494,"text":"70220494 - 1960 - Geological age of the Claypool site, northeastern Colorado","interactions":[],"lastModifiedDate":"2021-05-17T12:40:17.718636","indexId":"70220494","displayToPublicDate":"1960-10-01T07:35:55","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":700,"text":"American Antiquity","active":true,"publicationSubtype":{"id":10}},"title":"Geological age of the Claypool site, northeastern Colorado","docAbstract":"Artifacts related to the Cody complex occur in medium-grained sand that is spread as a blanket eolian deposit a few feet thick in the Claypool site area, Washington County, Colorado. The artifact-bearing sand lacks noticeable dunal topography and lies unconformably on marl of Yarmouth age and on waterlaid coarse sand and fine gravel of Kansan age that underlie the marl. The deposits underlying the artifact-bearing sand are much too old to date the artifacts precisely, but the physical characteristics of the artifact-bearing sand suggest that it was deposited under conditions cool and dry, rather than warm and dry, possibly during retreat of Valders ice that began about 10,000 years ago. A moderately mature Brown Soil about 5 feet thick developed on the sand, possibly about 7000 to 5000 years ago during a moist phase of the Thermal Maximum. Thus, the artifacts are possibly 10,000 to 7000 years old. Deposits which overlie the artifact-bearing sand reflect several episodes of erosion and sedimentation that are inferred to represent climatic changes.
","language":"English","publisher":"Society for American Archaeology","doi":"10.2307/276202","usgsCitation":"Malde, H., 1960, Geological age of the Claypool site, northeastern Colorado: American Antiquity, v. 26, no. 2, p. 215-222, https://doi.org/10.2307/276202.","productDescription":"8 p.","startPage":"215","endPage":"222","costCenters":[],"links":[{"id":385675,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"northeastern Colorado","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.083984375,\n 38.85682013474361\n ],\n [\n -102.0849609375,\n 38.85682013474361\n ],\n [\n -102.0849609375,\n 41.0130657870063\n ],\n [\n -106.083984375,\n 41.0130657870063\n ],\n [\n -106.083984375,\n 38.85682013474361\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"26","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Malde, H.E.","contributorId":65863,"corporation":false,"usgs":true,"family":"Malde","given":"H.E.","affiliations":[],"preferred":false,"id":815764,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220536,"text":"70220536 - 1960 - Variation in surface elevation of the nisqually glacier Mt. Rainier, Washington","interactions":[],"lastModifiedDate":"2021-05-18T17:49:49.422099","indexId":"70220536","displayToPublicDate":"1960-09-30T12:44:53","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Variation in surface elevation of the nisqually glacier Mt. Rainier, Washington","docAbstract":"Variation in surface elevations of the Nisqually Glacier has been recorded since 1942 by the annual measurement of three profiles across the glacier, designated as nos. 1, 2, and 3, located 0.5, 1.0, and 1.7 miles respectively from the terminus, at approximate mean elevations of 5,250,6,000, and 6,800 feet. A fourth profile, 2-A, located 1.4 miles from the terminus at an approximate mean elevation of 6,450 was measured from 1948 to 1954. These profiles cross the glacier approximately normal to the direction of flow. Additional data are available from measurements made at profiles no. 1 and no. 2 in 1931, 1932 and 1941. The results of these measurements show that a wave or surge has been moving down the glacier.The mean elevation at profile no. 3 began to increase in 1945 and continued through 1951 when it was 83 feet higher than in 1944. The general trend from 1952 to 1959 has been a decrease in elevation with a net change of 30 feet since 1951. The surface elevation at profile no. 2 continued to decrease through 1948, but began to increase in 1949 and continued to do so through 1957 in which year the mean elevation was 102 feet higher than in 1948. The wave became apparent at profile no. 1 in 1954 or 9 years after it first became evident at profile no. 3. The mean elevation has continued to increase and in 1959 was 70 feet higher than in 1954. The increase in surface elevation has been accompanied by a pronounced increase in rate of movement of the glacier.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666009493180","usgsCitation":"Johnson, A., 1960, Variation in surface elevation of the nisqually glacier Mt. Rainier, Washington: International Association of Scientific Hydrology - Bulletin , v. 5, no. 3, p. 54-60, https://doi.org/10.1080/02626666009493180.","productDescription":"7 p.","startPage":"54","endPage":"60","costCenters":[],"links":[{"id":385723,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Mt. Rainier","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.27783203125,\n 46.483264729155586\n ],\n [\n -120.70678710937499,\n 46.483264729155586\n ],\n [\n -120.70678710937499,\n 47.17477833929903\n ],\n [\n -122.27783203125,\n 47.17477833929903\n ],\n [\n -122.27783203125,\n 46.483264729155586\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"5","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Johnson, A.","contributorId":258183,"corporation":false,"usgs":false,"family":"Johnson","given":"A.","affiliations":[],"preferred":false,"id":815914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220535,"text":"70220535 - 1960 - Montana earthquakes noted in pennsylvania mine‐water pools","interactions":[],"lastModifiedDate":"2021-05-18T17:43:32.530024","indexId":"70220535","displayToPublicDate":"1960-09-30T12:40:32","publicationYear":"1960","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":"Montana earthquakes noted in pennsylvania mine‐water pools","docAbstract":"A recent paper by daCosta [1959] reported water‐level fluctuations caused by the Montana earthquake of August 18, 1959, and mentioned the fluctuations registered in three mine‐water pools of the Northern anthracite field in northeastern Pennsylvania, ten miles north of Wilkes‐Barre. This paper will discuss the water‐level phenomena of these pools in more detail. Most of the coal mines near Wilkes‐Barre are idle, and ground water is forming extensive mine‐water pools in the underground mine openings. Some of the pools are interconnected by boreholes, tunnels, and other openings through the barrier pillars between adjacent mines.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR041i003p00435","usgsCitation":"Hopkins, W., and Simpson, T., 1960, Montana earthquakes noted in pennsylvania mine‐water pools: Eos, Transactions, American Geophysical Union, v. 41, no. 3, p. 435-436, https://doi.org/10.1029/TR041i003p00435.","productDescription":"2 p.","startPage":"435","endPage":"436","costCenters":[],"links":[{"id":385722,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.27929687499999,\n 44.276671273775186\n ],\n [\n -103.271484375,\n 44.276671273775186\n ],\n [\n -103.271484375,\n 49.095452162534826\n ],\n [\n -116.27929687499999,\n 49.095452162534826\n ],\n [\n -116.27929687499999,\n 44.276671273775186\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"41","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Hopkins, W.B.","contributorId":10072,"corporation":false,"usgs":true,"family":"Hopkins","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":815912,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simpson, T.A.","contributorId":97553,"corporation":false,"usgs":true,"family":"Simpson","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":815913,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220529,"text":"70220529 - 1960 - Chemical equilibrium diagrams for ground-water systems/les graphiques de l'équilibre chimique pour les systèmes des eaux souterrainnes","interactions":[],"lastModifiedDate":"2021-05-18T17:08:40.335274","indexId":"70220529","displayToPublicDate":"1960-09-30T12:06:26","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Chemical equilibrium diagrams for ground-water systems/les graphiques de l'équilibre chimique pour les systèmes des eaux souterrainnes","docAbstract":"Chemical equilibrium in water in contact with calcite is expressed by means of a pH grid overlay on a log-log plot of activities of bicarbonate vs. calcium ions. Solubility of ferrous iron and the solid-phase minerals that would be stable in a solution containing activities of 10 ppm of sulfate and 100 ppm of bicarbonate or related species is expressed by means of a stability-field diagram with pH as abscissa and redox potential as ordinate.The diagrams can be used to tell whether water injected in recharge wells may form precipitates that may plug the aquifer and have other uses in studies of natural water chemistry.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666009493179","usgsCitation":"Hem, J., 1960, Chemical equilibrium diagrams for ground-water systems/les graphiques de l'équilibre chimique pour les systèmes des eaux souterrainnes: International Association of Scientific Hydrology - Bulletin , v. 5, no. 3, p. 45-53, https://doi.org/10.1080/02626666009493179.","productDescription":"9 p.","startPage":"45","endPage":"53","costCenters":[],"links":[{"id":488823,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666009493179","text":"Publisher Index Page"},{"id":385716,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":815906,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220581,"text":"70220581 - 1960 - Mapping mean areal precipitation","interactions":[],"lastModifiedDate":"2021-05-19T15:19:52.742332","indexId":"70220581","displayToPublicDate":"1960-09-30T10:16:05","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Mapping mean areal precipitation","docAbstract":"A method is presented for using point mean precipitation data to estimate areal values in regions of high relief. Variation of precipitation with altitude is determined. Local anomalies from this relationship are mapped, and lines of equal anomaly are drawn. By use of the mean relation corrected for the local anomaly, the mean precipitation at any point can be determined and an isohyetal map drawn. A similar approach can be used to determine mean temperature for studies of snowmelt or of potential evapotranspiration.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666009493176","usgsCitation":"Dawdy, D., and Langbein, W.B., 1960, Mapping mean areal precipitation: International Association of Scientific Hydrology - Bulletin , v. 5, no. 3, p. 16-23, https://doi.org/10.1080/02626666009493176.","productDescription":"8 p.","startPage":"16","endPage":"23","costCenters":[],"links":[{"id":480388,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666009493176","text":"Publisher Index Page"},{"id":385773,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dawdy, D.R.","contributorId":99956,"corporation":false,"usgs":true,"family":"Dawdy","given":"D.R.","affiliations":[],"preferred":false,"id":816070,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":816071,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220576,"text":"70220576 - 1960 - Areal flood-frequency analysis in a humid region","interactions":[],"lastModifiedDate":"2021-05-19T14:47:50.036486","indexId":"70220576","displayToPublicDate":"1960-09-30T09:45:10","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Areal flood-frequency analysis in a humid region","docAbstract":"This study was made to define the relation between floods in a humid region and the causative factors that account for their variability. The study covered the basic relationships between peak discharges and hydrologic factors as well as the practical working methods for generalizing the results on a regional basis. Statistical multiple-correlation techniques were applied to hydrologic data in New England. A field and library investigation of historical flood data extended the period of flood knowledge to as much as 300 years. The relation of many topographic and climatic factors to flood peaks was tested. Flood peaks with recurrence intervals at 9 levels, from 1.2 to 300 years, were related to 6 independent variables, 3 of which are topographic, 2 climatic, and 1 orographic.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666009493175","usgsCitation":"Benson, M.A., 1960, Areal flood-frequency analysis in a humid region: International Association of Scientific Hydrology - Bulletin , v. 5, no. 3, p. 5-15, https://doi.org/10.1080/02626666009493175.","productDescription":"11 p.","startPage":"5","endPage":"15","costCenters":[],"links":[{"id":480389,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666009493175","text":"Publisher Index Page"},{"id":385768,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Benson, M. A.","contributorId":32510,"corporation":false,"usgs":true,"family":"Benson","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":816065,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010772,"text":"70010772 - 1960 - Botanical prospecting for ore deposits","interactions":[],"lastModifiedDate":"2026-02-26T16:19:48.836982","indexId":"70010772","displayToPublicDate":"1960-09-02T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Botanical prospecting for ore deposits","docAbstract":"How plant chemistry is being used to aid the geologist in his search for metals at home and abroad.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.132.3427.591","issn":"00368075","usgsCitation":"Cannon, H., 1960, Botanical prospecting for ore deposits: Science, p. 591-598.","productDescription":"8 p.","startPage":"591","endPage":"598","costCenters":[],"links":[{"id":218660,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"132","issue":"3427","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f223e4b0c8380cd4b021","contributors":{"authors":[{"text":"Cannon, H.L.","contributorId":43416,"corporation":false,"usgs":true,"family":"Cannon","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":359616,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37760,"text":"37760 - 1960 - Big game inventory for 1959","interactions":[],"lastModifiedDate":"2014-07-23T11:23:24","indexId":"37760","displayToPublicDate":"1960-09-01T11:22:27","publicationYear":"1960","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":"425","title":"Big game inventory for 1959","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled in Bird and Mammal Laboratories, Branch of Wildlife Research.","usgsCitation":"U.S. Fish and Wildlife Service, 1960, Big game inventory for 1959 (Updates Wildlife Leaflet 346 (1953).): Wildlife Leaflet 425, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290784,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Updates Wildlife Leaflet 346 (1953).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd1e5e4b0824b2d17696d","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529705,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220521,"text":"70220521 - 1960 - Reflectivity measurements with a hallimond visual microphotometer","interactions":[],"lastModifiedDate":"2021-05-18T13:29:12.895159","indexId":"70220521","displayToPublicDate":"1960-09-01T08:25:33","publicationYear":"1960","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":"Reflectivity measurements with a hallimond visual microphotometer","docAbstract":"No abstract available.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.6.1306","usgsCitation":"Leonard, B.F., 1960, Reflectivity measurements with a hallimond visual microphotometer: Economic Geology, v. 55, no. 6, p. 1306-1312, https://doi.org/10.2113/gsecongeo.55.6.1306.","productDescription":"7 p.","startPage":"1306","endPage":"1312","costCenters":[],"links":[{"id":385705,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"55","issue":"6","noUsgsAuthors":false,"publicationDate":"1960-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Leonard, Benjamin F. III","contributorId":59817,"corporation":false,"usgs":true,"family":"Leonard","given":"Benjamin","suffix":"III","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":815885,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37517,"text":"37517 - 1960 - Waterfowl status report, 1960","interactions":[],"lastModifiedDate":"2014-07-15T13:49:59","indexId":"37517","displayToPublicDate":"1960-08-01T13:49:03","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"51","title":"Waterfowl status report, 1960","docAbstract":"No abstract available.","language":"English","publisher":"U.S Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Crissey, W., 1960, Waterfowl status report, 1960: Special Scientific Report - Wildlife 51, 192 p.","productDescription":"192 p.","numberOfPages":"192","costCenters":[],"links":[{"id":290151,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64deae4b0001bd51477d4","contributors":{"authors":[{"text":"Crissey, W.F.","contributorId":21656,"corporation":false,"usgs":true,"family":"Crissey","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":218205,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37759,"text":"37759 - 1960 - Fur catch in the United States, 1959","interactions":[],"lastModifiedDate":"2014-07-23T11:20:09","indexId":"37759","displayToPublicDate":"1960-08-01T11:19:02","publicationYear":"1960","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":"424","title":"Fur catch in the United States, 1959","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled in the Bird and Mammal Laboratories, Branch of Wildlife Research, Bureau of Sport Fisheries and Wildlife.","usgsCitation":"U.S. Branch of Wildlife Research, 1960, Fur catch in the United States, 1959 (Revises Wildlife Leaflet BS-140 (1939).): Wildlife Leaflet 424, 3 p.","productDescription":"3 p.","numberOfPages":"3","costCenters":[],"links":[{"id":290782,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises Wildlife Leaflet BS-140 (1939).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd1e5e4b0824b2d17696f","contributors":{"authors":[{"text":"U.S. Branch of Wildlife Research","contributorId":127903,"corporation":true,"usgs":false,"organization":"U.S. Branch of Wildlife Research","id":529704,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220522,"text":"70220522 - 1960 - Extract ability of humic acid from coalified logs as a guide to temperatures in colorado plateau sediments","interactions":[],"lastModifiedDate":"2021-05-18T14:09:06.935516","indexId":"70220522","displayToPublicDate":"1960-08-01T09:04:39","publicationYear":"1960","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":"Extract ability of humic acid from coalified logs as a guide to temperatures in colorado plateau sediments","docAbstract":"Coalified logs in Triassic and Jurassic sediments of the Colorado Plateau have been exposed to alkaline ground water. Extraction of humic acids under such conditions is temperature dependent. Study of residual humic acids in a suite of coalified logs has indicated that temperatures up to but not over 120° C prevailed in the sediments. This maximum temperature corresponds with that to be expected from geothermal gradient and estimated from mineralogic evidence.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.55.5.1039","usgsCitation":"Breger, I., and Chandler, J., 1960, Extract ability of humic acid from coalified logs as a guide to temperatures in colorado plateau sediments: Economic Geology, v. 55, no. 5, p. 1039-1047, https://doi.org/10.2113/gsecongeo.55.5.1039.","productDescription":"9 p.","startPage":"1039","endPage":"1047","costCenters":[],"links":[{"id":385706,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.9404296875,\n 36.98500309285596\n ],\n [\n -101.953125,\n 36.98500309285596\n ],\n [\n -101.953125,\n 41.04621681452063\n ],\n [\n -108.9404296875,\n 41.04621681452063\n ],\n [\n -108.9404296875,\n 36.98500309285596\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"55","issue":"5","noUsgsAuthors":false,"publicationDate":"1960-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Breger, Irving A.","contributorId":41901,"corporation":false,"usgs":true,"family":"Breger","given":"Irving A.","affiliations":[],"preferred":false,"id":815886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chandler, J.C.","contributorId":225572,"corporation":false,"usgs":false,"family":"Chandler","given":"J.C.","affiliations":[],"preferred":false,"id":815887,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010846,"text":"70010846 - 1960 - First natural occurrence of coesite","interactions":[],"lastModifiedDate":"2026-02-26T15:54:35.890019","indexId":"70010846","displayToPublicDate":"1960-07-22T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"First natural occurrence of coesite","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.2307/3797530","usgsCitation":"Locke, L.N., Herman, C.M., and King, E., 1960, The need for differentiation of trichomoniasis and pox infection in doves: Journal of Wildlife Management, v. 24, no. 3, p. 348-348, https://doi.org/10.2307/3797530.","productDescription":"1 p.","startPage":"348","endPage":"348","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193945,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4723","contributors":{"authors":[{"text":"Locke, L. N.","contributorId":73539,"corporation":false,"usgs":true,"family":"Locke","given":"L.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":331889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":331890,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"King, E.S. Jr.","contributorId":65941,"corporation":false,"usgs":true,"family":"King","given":"E.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":331888,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221796,"text":"70221796 - 1960 - The chief oxide-burgin area discoveries, East Tintic district, Utah; A case history","interactions":[],"lastModifiedDate":"2021-07-07T12:28:44.400442","indexId":"70221796","displayToPublicDate":"1960-07-07T07:25:53","publicationYear":"1960","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":"The chief oxide-burgin area discoveries, East Tintic district, Utah; A case history","docAbstract":"The Burgin shaft is in the Chief Oxide area of the E. Tintic district, Utah, and is about a mile E. of any previously known ore bodies; workings from it are currently developing a substantial amount of commercial Pb-Zn ore in several blind ore bodies that lie in folded Paleozoic carbonate rock concealed beneath a blanket of Eocene lava. This area was mapped by Tower and Smith of the U.S. Geological Survey in 1897 and again by Lindgren and Loughlin in 1911, but no detailed work was done until after 1943 when a field party headed by T.S. Lovering began a study of the entire E. Tintic district. The history of the development of exploration concepts is summarized under Historical Summary. The E. Tintic mining district is in the E.-central part of a N.-trending fault-block mountain range near the eastern margin of the Great Basin; dominant structures of the range are a N.-trending syncline on the W. and a less well exposed anticline on the E. Both folds are cut by an intersecting system of transcurrent strike-slip faults and by minor thrust faults and normal faults of moderate displacement. A strong W.-dipping thrust fault cuts the anticline a short distance E. of the fold axis, but is hidden by Eocene lava throughout the E. Tintic district. The pre-Tertiary rocks range from Lower Cambrian to Upper Mississippian and exceed 7,000 ft. in total thickness; they are dominantly marine limestone and dolomite except for a thick basal Cambrian quartzite. The Tertiary rocks are chiefly dacitic lavas and pyroclastic deposits that are intruded by moderately persistent dikes and irregular bodies of monzonite and quartz porphyry. Nearly all the faulting and folding took place before the extrusion of the lavas on a rugged Eocene erosion surface. At about the time of the intrusion of monzonitic magma, many of the faults in the Paleozoic rock were re-opened and in the overlying lava some fracturing took place which was later accented by hydrothermal alteration. Most of the ore mined in the E. Tintic district has come from Pb-Zn-Ag replacement bodies in shattered Jasperoidized hydrothermal dolomite at the intersection of low angle faults and steep mineralized NE.-trending cross fractures. The U.S. Geological Survey studies of 1943 to 1957 concentrated on detailed mapping of geology and alteration in the E. Tintic district, together with field and laboratory studies of the relation of alteration to stages of mineralization and ore deposition. Trenching and core drilling were carried on after World War II to aid in interpreting the subrhyolite geology, and the Chief Oxide area was 1 of 4 localities tested by drilling. Study of the fossils, lithology, and alteration shown here in a deep drill core, together with the knowledge of the regional geology, led to an essentially correct interpretation of subrhyolite structure in the strongly discordant underlying Paleozoic rocks in which a mineralized tear fault cuts a strong thrust fault, and to the conclusion that ore stage mineralization was present in substantial amounts in the Paleozoic rocks below the Chief Oxide alteration patch in the quartz latite lava. Subsequent geothermal and geochemical work strengthened this conclusion, and the recent development work of the Bear Creek Mining Company, which sank the Burgin shaft, has shown the presence of Pb-Zn-Ag ore of commercial grade in substantial amount in blind ore bodies below the lava blanket in the Chief Oxide area.