The Flattery Rocks, Quillayute Needles, and Copalis National Wildlife Refuges lie off the Pacific coast of the Olympic Peninsula between Cape Flattery and Grays Harbor. They have a total land area of 247 acres and consists of numerous small islands, sea stacks and rocks that rise above a wave-cut platform. The refuges are in a belt of intensely folded and faulted marine sedimentary and volcanic rocks of early Eocene to Pliocene age. Pleistocene glaciofluvial deposits blanket the Tertiary strata along this coastal belt. The disturbed belt borders the eastern margin of a depositional basin on the continental shelf that probably contains a thick sequence of late Tertiary rocks.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr879_1967","usgsCitation":"Weissenborn, A.E., and Snavely, P.D., 1967, Mineral appraisal of the Flattery Rocks, Quillayute Needles, and Copalis National Wildlife Refuges, Washington: U.S. Geological Survey Open-File Report 879, 30 p., https://doi.org/10.3133/ofr879_1967.","productDescription":"30 p.","costCenters":[],"links":[{"id":417115,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/879_1967/report-thumb.jpg"},{"id":417330,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8872.htm","linkFileType":{"id":5,"text":"html"}},{"id":434871,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/879_1967/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Copalis National Wildlife Refuge, Flattery Rocks National Wildlife Refuge, Quillayute Needles National Wildlife Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.77391836685513,\n 48.1815019611561\n ],\n [\n -124.77391836685513,\n 48.15030925780698\n ],\n [\n -124.73338665471016,\n 48.15030925780698\n ],\n [\n -124.73338665471016,\n 48.1815019611561\n ],\n [\n -124.77391836685513,\n 48.1815019611561\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.46562950263186,\n 47.83854729846999\n ],\n [\n -124.5104214830809,\n 47.83854729846999\n ],\n [\n -124.5104214830809,\n 47.82039144984293\n ],\n [\n -124.46562950263186,\n 47.82039144984293\n ],\n [\n -124.46562950263186,\n 47.83854729846999\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.3384552486784,\n 47.44579550453264\n ],\n [\n -124.35453823958551,\n 47.44579550453264\n ],\n [\n -124.35453823958551,\n 47.42648577612718\n ],\n [\n -124.3384552486784,\n 47.42648577612718\n ],\n [\n -124.3384552486784,\n 47.44579550453264\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Weissenborn, Albert Edward","contributorId":98698,"corporation":false,"usgs":true,"family":"Weissenborn","given":"Albert","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":510897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snavely, Parke Detweiler Jr.","contributorId":48535,"corporation":false,"usgs":true,"family":"Snavely","given":"Parke","suffix":"Jr.","email":"","middleInitial":"Detweiler","affiliations":[],"preferred":false,"id":872863,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70202796,"text":"70202796 - 1967 - Basic data for three lacustrine clay deposits in the southern part of the San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2019-03-29T13:52:02","indexId":"70202796","displayToPublicDate":"1967-01-01T14:51:45","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Basic data for three lacustrine clay deposits in the southern part of the San Joaquin Valley, California","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70202796","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Croft, M., 1967, Basic data for three lacustrine clay deposits in the southern part of the San Joaquin Valley, California: Open-File Report, Report: 44 p.; 1 Plate: 45.85 x 38.01 inches, https://doi.org/10.3133/70202796.","productDescription":"Report: 44 p.; 1 Plate: 45.85 x 38.01 inches","costCenters":[],"links":[{"id":362537,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70202796/report-thumb.jpg"},{"id":362538,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70202796/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":362539,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70202796/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","datum":"Mean sea level","country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.25,\n 34.75\n ],\n [\n -118.25,\n 34.75\n ],\n [\n -118.25,\n 36.75\n ],\n [\n -121.25,\n 36.75\n ],\n [\n -121.25,\n 34.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Croft, M.G.","contributorId":55413,"corporation":false,"usgs":true,"family":"Croft","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":760259,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70110392,"text":"wdrIN661 - 1967 - Water resources data for Indiana, 1966","interactions":[],"lastModifiedDate":"2014-06-11T09:46:03","indexId":"wdrIN661","displayToPublicDate":"1967-01-01T14:01:45","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IN-66-1","title":"Water resources data for Indiana, 1966","docAbstract":"The surface-water records for the 1966 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering states.
\nThe quality-of-water investigations of the U.S. Geological Survey are concerned with the chemical and physical characteristics of surface- and ground-water supplies of the Nation. The basic records for the 1966 water year for quality of surface waters within the State of Indiana are given in this report. For convenience and interest, there are also records for a few water quality stations in bordering states.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrIN661","collaboration":"Prepared in cooperation with Indiana Department of Natural Resources; Indiana State Board of Health; Indiana State Highway Commission; Corps of Engineers, U.S. Army","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Water resources data for Indiana, 1966: U.S. Geological Survey Water Data Report IN-66-1, viii, 252 p., https://doi.org/10.3133/wdrIN661.","productDescription":"viii, 252 p.","numberOfPages":"266","temporalStart":"1965-10-01","temporalEnd":"1966-09-30","costCenters":[],"links":[{"id":288276,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288275,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1966/in-66-1/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"538052d2e4b0826cd5016a66","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535660,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221320,"text":"70221320 - 1967 - Determining transmissibility from cyclic discharge by N. Thomas Sheahan —July, 1966","interactions":[],"lastModifiedDate":"2021-06-09T19:00:57.905181","indexId":"70221320","displayToPublicDate":"1967-01-01T13:56:47","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Determining transmissibility from cyclic discharge by N. Thomas Sheahan —July, 1966","docAbstract":"No abstract available.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1967.tb01239.x","usgsCitation":"Appel, C., 1967, Determining transmissibility from cyclic discharge by N. Thomas Sheahan —July, 1966: Groundwater, v. 5, no. 1, p. 55-56, https://doi.org/10.1111/j.1745-6584.1967.tb01239.x.","productDescription":"2 p.","startPage":"55","endPage":"56","costCenters":[],"links":[{"id":386366,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Appel, C.A.","contributorId":84786,"corporation":false,"usgs":true,"family":"Appel","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":817298,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70114650,"text":"70114650 - 1967 - Results of the second phase of the drought-disaster test-drilling program near Morristown, N.J.","interactions":[],"lastModifiedDate":"2018-01-08T18:31:02","indexId":"70114650","displayToPublicDate":"1967-01-01T13:17:37","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":149,"text":"New Jersey Division of Water Policy and Supply Water Resources Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"17","title":"Results of the second phase of the drought-disaster test-drilling program near Morristown, N.J.","docAbstract":"The continued drought in northeastern New Jersey through the summer of 1966 with its attendant water-supply problems resulted in an extension of the drought-disaster test-drilling program originally requested by the Office of Emergency Planning on August 30, 1965. Authorization to continue test drilling was fiven by the Office of Emergency Planning on September 26, 1966, with the stipulation that all field work be complete by January 31, 1977. Contractural costs were paid by the Office of Emergency Planning, whereas personnel costs were shared by the U.S. Geological Survey and the New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply.
The work undertaken in 1965 by the Geological Survey was \"...to preform the necessary drilling and testing of wells to identify the extent and nature of a reserve ground-water source in the vicinity of the Passaic River near the northern New Jersey metropolitan area.\" Results of this first phase were made available in the fall of 1966 in Water Resources Circular 16 of the New Jersey Department of Conservation and Economic Development. Three of the five areas tested (figure 1)--two in Parsippany-Troy Hills Township (areas 2 and 4) and one in East Hanover Township (area 1), Morris County--proved capable of providing an aggregate sustained yield of 7.5 million gallons daily (mgd) from wells constructed in sand and gravel deposits. Because significant supplies of ground water for emergency use were located in the first phase of the exploratory test-drilling program, it was though desirable to extend the originally planned studies so as to obtain maximum practicable information on emergency supplies.
During this second phase of the investigation, drilling was conducted in 16 sites in Chatham, Madison, and Florham Park Boroughs and in Hanover and East Hanover Townships, Morris County. (See figure 2.) The drilling in Hanover and East Hanover Townships, and part of the drilling done in Florham Park was to explore the availability of large undeveloped ground-water supplies. Drilling in Chatham, Madison, and Florham Park Boroughs was done primarily to determine the extent and continuity of buried valley-fill aquifers, so that a full evaluation of the effects of pumpage from other areas on these already heavily pumped areas could be made. In addition, it was anticipated that the drilling could help in defining the feasibility of artificial recharge of the heavily pumped areas and in the determination of the prospective method of recharge and points of emplacement.
Arrangements for easements with landowners, preparation of specifications for well drilling and seismic work, and supervision of well drilling and seismic contracts were all performed by the New Jersey District, Water Resources Division of the Geological Survey.
Prior to the test drilling, seismic exploration under contract with Alpine Geophysical Associates of Norwood, N. J. was conducted at five locations in the Chatham-Madison-Florham Park area and at one place in Parsippany-Troy Hills Township. The seismic work was done to determine the most favorable location for a test well at several potential test-well sites and to help in the interpretation of subsurface geology between test sites.
Contracts for the drilling of the test holes were awarded during November and drilling commences on November 30. Kaye Well drilling, Inc. of Jackson, N. J. was the recipient of a contract for eight of the test holes, and a second contract was awarded to Rinbrand Well Drilling Co., Inc. of Glen Rock, N. J.--also for eight test holes.
Acknowledgment is due to the many public officials of Chatham, Madison, Florham Park, Morristown, and East Hanover Township as well as officials of the Braidburn Corporation and Esso Research and Engineering Co., who cooperated by making their lands available for exploration.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Trenton, NJ","collaboration":"Prepared by the State of New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply, in cooperation with United States Department of the Interior Geological Survey","usgsCitation":"Vecchioli, J., Nichols, W., and Nemickas, B., 1967, Results of the second phase of the drought-disaster test-drilling program near Morristown, N.J.: New Jersey Division of Water Policy and Supply Water Resources Circular 17, Report: v, 23 p.; 3 Plates: 34.65 x 21.48 inches or smaller.","productDescription":"Report: v, 23 p.; 3 Plates: 34.65 x 21.48 inches or smaller","numberOfPages":"30","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":290164,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327417,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70114650/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":327415,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70114650/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":327416,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70114650/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":290163,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114650/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey","city":"Morristown","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.501444,40.780231 ], [ -74.501444,40.818361 ], [ -74.456181,40.818361 ], [ -74.456181,40.780231 ], [ -74.501444,40.780231 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ad40f9e4b0729c154181d6","contributors":{"authors":[{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":495394,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nichols, William D.","contributorId":98296,"corporation":false,"usgs":true,"family":"Nichols","given":"William D.","affiliations":[],"preferred":false,"id":495395,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nemickas, Bronius","contributorId":105733,"corporation":false,"usgs":true,"family":"Nemickas","given":"Bronius","email":"","affiliations":[],"preferred":false,"id":495396,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70039249,"text":"70039249 - 1967 - Mountains and plains Denver's geologic setting","interactions":[],"lastModifiedDate":"2012-08-03T01:02:04","indexId":"70039249","displayToPublicDate":"1967-01-01T13:01:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Mountains and plains Denver's geologic setting","docAbstract":"A slice of geologic history is exposed to view in the Denver, Colorado area. Denver is situated on the High Plains near the east front of the Rocky Mountains. As one travels westward from Denver toward the mountains, successively older rocks are crossed from the geologically young rocks of the High Plains and the South Platte River valley to the older rocks of the foothills and the ancient rocks of the mountains. Thus, within a few miles,the journey turns back the pages of time in a lifesized textbook that vividly illustrates the geologic events that shaped the landscape.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039249","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Mountains and plains Denver's geologic setting: General Information Product, 23 p., https://doi.org/10.3133/70039249.","productDescription":"23 p.","numberOfPages":"24","costCenters":[],"links":[{"id":261472,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039249/report.pdf"},{"id":261473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039249/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Denver","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.25,38.833333333333336 ], [ -106.25,40.583333333333336 ], [ -103.5,40.583333333333336 ], [ -103.5,38.833333333333336 ], [ -106.25,38.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5ebae4b0c8380cd70c33","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221309,"text":"70221309 - 1967 - An electrical analog study of the geometry of limestone solution","interactions":[],"lastModifiedDate":"2021-06-09T17:42:25.755466","indexId":"70221309","displayToPublicDate":"1967-01-01T12:38:36","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"An electrical analog study of the geometry of limestone solution","docAbstract":"This study of the geometry of limestone solution is based on the following conditions: (1) the limestone is impermeable but contains and transmits water in joints, fractures, bedding‐plane partings, and solution channels; (2) at depth, the limestone aquifer is underlain by impermeable rock; (3) ground water in the limestone is under water‐table conditions; (4) recharge to the limestone is by infiltration of precipitation through the overlying rock to the zone of saturation; (5) discharge from the aquifer is by seeps and springs; and (6) ground water dissolves the limestone through which it flows, continuously modifying the flow pattern and the hydrologic properties of the medium. These conditions commonly are found in limestone terranes in the eastern and central United States. An electrical analog was constructed conforming to this description of the ground‐water flow system and has been used to define the pattern, velocity, and density of ground‐water flow and the relative length of time of contact of water with the aquifer. Successive models are used to illustrate progressive limestone solution and changes in ground‐water flow in the aquifer. The initial analog indicates a strongly convex water table with the greatest density of flow at shallow depths beneath the water table near the point of discharge. Successive models indicate greater concentration of flow near and on the level of ground‐water discharge, an overall lowering of the water table, and a pronounced flattening of the water table near the discharge point. Results of the analog study support the following conclusions: (1) The most active zone of solution is at shallow depths beneath the water table and near the point of ground‐water discharge. Consequently, the size of channels generally decreases with depth and increases with proximity to the point of ground‐water discharge. (2) Generally, solution channels have a greater lateral than vertical extent.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1745-6584.1967.tb01235.x","usgsCitation":"Bedinger, M.S., 1967, An electrical analog study of the geometry of limestone solution: Groundwater, v. 59, no. 12, p. 24-24, https://doi.org/10.1111/j.1745-6584.1967.tb01235.x.","productDescription":"1 p.","startPage":"24","endPage":"24","costCenters":[],"links":[{"id":386356,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"12","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":817286,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70211073,"text":"70211073 - 1967 - Basement map of North America: between latitudes 24° and 60° N","interactions":[],"lastModifiedDate":"2020-07-15T15:05:44.810973","indexId":"70211073","displayToPublicDate":"1967-01-01T12:27:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Basement map of North America: between latitudes 24° and 60° N","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70211073","usgsCitation":"American Association of Petroleum Geologists, and U.S. Geological Survey, 1967, Basement map of North America: between latitudes 24° and 60° N, HTML Document, https://doi.org/10.3133/70211073.","productDescription":"HTML Document","costCenters":[],"links":[{"id":376338,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":376336,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_55276.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","otherGeospatial":"North America","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -133.154296875,\n 24\n ],\n [\n -55.458984375,\n 24\n ],\n [\n -55.458984375,\n 60\n ],\n [\n -133.154296875,\n 60\n ],\n [\n -133.154296875,\n 24\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"American Association of Petroleum Geologists","contributorId":228978,"corporation":true,"usgs":false,"organization":"American Association of Petroleum Geologists","id":792683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"U.S. Geological Survey","contributorId":152492,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":792684,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5222035,"text":"5222035 - 1967 - New records of birds from the Phoenix and Line Islands","interactions":[],"lastModifiedDate":"2025-01-06T16:01:49.62069","indexId":"5222035","displayToPublicDate":"1967-01-01T12:17:37","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1961,"text":"Ibis","active":true,"publicationSubtype":{"id":10}},"title":"New records of birds from the Phoenix and Line Islands","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"/10.1111/j.1474-919X.1967.tb00013.x","usgsCitation":"Clapp, R.B., and Sibley, F., 1967, New records of birds from the Phoenix and Line Islands: Ibis, v. 109, no. 1, p. 122-125, https://doi.org//10.1111/j.1474-919X.1967.tb00013.x.","productDescription":"4 p.","startPage":"122","endPage":"125","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197596,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"109","issue":"1","noUsgsAuthors":false,"publicationDate":"2008-04-03","publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697589","contributors":{"authors":[{"text":"Clapp, R. B.","contributorId":9371,"corporation":false,"usgs":true,"family":"Clapp","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":335327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sibley, F.C.","contributorId":79971,"corporation":false,"usgs":true,"family":"Sibley","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":335328,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25259,"text":"25259 - 1967 - Water quality at Patuxent River Bridge, MD","interactions":[],"lastModifiedDate":"2014-08-01T11:54:03","indexId":"25259","displayToPublicDate":"1967-01-01T11:50:02","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesNumber":"C819t","title":"Water quality at Patuxent River Bridge, MD","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","doi":"10.3133/25259","issn":"0364-7064","usgsCitation":"Cory, R.L., and Nauman, J.W., 1967, Water quality at Patuxent River Bridge, MD, https://doi.org/10.3133/25259.","costCenters":[],"links":[{"id":291521,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Maryl","city":"Patuxent","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.763695,38.531239 ], [ -76.763695,38.548694 ], [ -76.731681,38.548694 ], [ -76.731681,38.531239 ], [ -76.763695,38.531239 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53dca9cfe4b07615786377ac","contributors":{"authors":[{"text":"Cory, Robert L.","contributorId":77967,"corporation":false,"usgs":true,"family":"Cory","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":193355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nauman, Jon W.","contributorId":56232,"corporation":false,"usgs":true,"family":"Nauman","given":"Jon","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":193354,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70210849,"text":"70210849 - 1967 - Scapolite in the Belt Series in the St. Joe-Clearwater Region, Idaho","interactions":[],"lastModifiedDate":"2020-06-29T16:42:29.404119","indexId":"70210849","displayToPublicDate":"1967-01-01T11:35:53","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1727,"text":"GSA Special Papers","active":true,"publicationSubtype":{"id":10}},"title":"Scapolite in the Belt Series in the St. Joe-Clearwater Region, Idaho","docAbstract":"Scapolite is a common rock-forming mineral in parts of the Belt Series of Precambrian age in southern Shoshone County and adjoining parts of Clearwater County, Idaho. It is most abundant in moderately metamorphosed calcareous shaly layers of the Wallace Formation but occurs also in their highly metamorphosed equivalents and in the lowest part of the Prichard Formation.
The mode of occurrence varies with distance from the Idaho batholith, with bulk composition, and with grade of metamorphism. In the northern part of the area where rocks were metamorphosed to the epidote-amphibolite facies, the highest concentration of scapolite is in layers rich in calcite, biotite, or hornblende and diopside. In biotite-rich layers interbedded with quartzite, scapolite is in round holoblasts; in carbonate granofels, crystals are euhedral to subhedral; and in hornblende- and diopside-bearing layers, small anhedral grains are common. In rocks metamorphosed to the amphibolite facies, such as diopside gneiss and calcium-magnesium-aluminum silicate rocks (here named “camalsite”), scapolite occurs in small anhedral grains. In diopside gneiss, scapolite is in thin layers that extend long distances parallel to the bedding. In camalsite, small masses exceptionally rich in scapolite are common.
The mode of occurrence and the distribution parallel to the bedding suggest that scapolite crystallized from a sedimentary rock that contained saline minerals. The scapolite contains much Cl but only a little SO3, suggesting that halite was the chief source mineral. The local high concentrations of scapolite occur in a zone where elements have been redistributed, either because of metamorphism of dispersed or layered saline minerals with accompanying migration of chlorine or because of metamorphism of primary local masses of such minerals.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/SPE86-p1","usgsCitation":"Hietanen, A., 1967, Scapolite in the Belt Series in the St. Joe-Clearwater Region, Idaho: GSA Special Papers, v. 86, p. 1-54, https://doi.org/10.1130/SPE86-p1.","productDescription":"54 p.","startPage":"1","endPage":"54","costCenters":[],"links":[{"id":375984,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"St. Joe-Clearwater region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.83959960937499,\n 46.210249600187225\n ],\n [\n -114.334716796875,\n 46.210249600187225\n ],\n [\n -114.334716796875,\n 47.502358951968574\n ],\n [\n -116.83959960937499,\n 47.502358951968574\n ],\n [\n -116.83959960937499,\n 46.210249600187225\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"86","noUsgsAuthors":false,"publicationDate":"1967-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hietanen, Anna","contributorId":43841,"corporation":false,"usgs":true,"family":"Hietanen","given":"Anna","affiliations":[],"preferred":false,"id":791704,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70201217,"text":"70201217 - 1967 - Mineral appraisal of the Poker Jim Ridge and Fort Warner areas of the Hart Mountain National Antelope Refuge, Lake County, Oregon","interactions":[],"lastModifiedDate":"2018-12-11T10:22:12","indexId":"70201217","displayToPublicDate":"1967-01-01T11:21:39","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Mineral appraisal of the Poker Jim Ridge and Fort Warner areas of the Hart Mountain National Antelope Refuge, Lake County, Oregon","docAbstract":"The Poker Jim Ridge and Fort Warner areas, which are candidate areas for inclusion in the National Wilderness Preservation System, are in the Hart Mountain National Antelope Refuge in east-central Lake County, south-central Oregon. The two areas form part of an upraised and tilted fault block--a structural element that is typical of the northern part of the Great Basin province. Rocks in the two areas are principally volcanic in origin. They have been faulted, uplifted, and tilted eastward, the older rocks having been more strongly deformed than the younger ones.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70201217","usgsCitation":"Walker, G.W., and Swanson, D., 1967, Mineral appraisal of the Poker Jim Ridge and Fort Warner areas of the Hart Mountain National Antelope Refuge, Lake County, Oregon: Open-File Report, iii, 28 p., https://doi.org/10.3133/70201217.","productDescription":"iii, 28 p.","costCenters":[],"links":[{"id":360142,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70201217/report-thumb.jpg"},{"id":360143,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70201217/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","county":"Lake County","otherGeospatial":"Hart Mountain National Antelope Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.81964111328124,\n 42.33418438593939\n ],\n [\n -119.34173583984375,\n 42.33418438593939\n ],\n [\n -119.34173583984375,\n 42.742978093466434\n ],\n [\n -119.81964111328124,\n 42.742978093466434\n ],\n [\n -119.81964111328124,\n 42.33418438593939\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5c10dadfe4b034bf6a7fcc63","contributors":{"authors":[{"text":"Walker, George W.","contributorId":101308,"corporation":false,"usgs":true,"family":"Walker","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":753762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swanson, Donald A. 0000-0002-1680-3591 donswan@usgs.gov","orcid":"https://orcid.org/0000-0002-1680-3591","contributorId":3137,"corporation":false,"usgs":true,"family":"Swanson","given":"Donald A.","email":"donswan@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":753763,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70170953,"text":"70170953 - 1967 - Geochemistry and ground-water movement in northwestern Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T10:00:51","indexId":"70170953","displayToPublicDate":"1967-01-01T11:15:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Geochemistry and ground-water movement in northwestern Minnesota","docAbstract":"The relation between water quality and water movement within the ground-water reservoir may be better understood if studies of flow systems are used in conjunction with hydrochemical methods. Within small watersheds, local, intermediate, and regional flow systems may develop, depending upon the shape, the relief, and the thickness of the ground-water reservoir. Lateral and vertical variations of water quality in the ground-water reservoir reflect the difference in length of flow paths within a system. The relative ion concentration of the major ions in solution in ground waters change as water moves from recharge areas to discharge areas. These changes are used to interpret the direction and rate of ground-water movement.
\nGround-water types mapped in the Two Rivers watershed of northwestern Minnesota indicate that calcium bicarbonate type water occurs near the source of recharge and progressively changes to the sulfate type as water moves downgradient toward the discharge area. Local recharge areas are indicated by the greater penetration of calcium bicarbonate waters into the ground-water reservoir. The calcrum bicarbonate type water of surface streams during low flow indicates that water moves into the stream from the upper part of the ground-water reservoir. Chloride type water moves from the Paleozoic rocks and mixes with water in the glacial drift probably at places where permeable zones in the Paleozoic rocks are in contact with the overlying drift.
","language":"English","publisher":"National Groundwater Association","publisherLocation":"Herndon, VA","doi":"10.1111/j.1745-6584.1967.tb01233.x","usgsCitation":"Maclay, R., and Winter, T.C., 1967, Geochemistry and ground-water movement in northwestern Minnesota: Groundwater, v. 5, no. 1, p. 11-19, https://doi.org/10.1111/j.1745-6584.1967.tb01233.x.","productDescription":"9 p.","startPage":"11","endPage":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321174,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","volume":"5","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","scienceBaseUri":"5735a938e4b0dae0d5df5115","contributors":{"authors":[{"text":"Maclay, R.W.","contributorId":72804,"corporation":false,"usgs":true,"family":"Maclay","given":"R.W.","affiliations":[],"preferred":false,"id":629203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winter, T. C.","contributorId":23485,"corporation":false,"usgs":true,"family":"Winter","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":629204,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70252069,"text":"70252069 - 1967 - Pre-Olympia Pleistocene stratigraphy and chronology in the central Puget Lowland, Washington","interactions":[],"lastModifiedDate":"2024-03-12T16:07:12.955763","indexId":"70252069","displayToPublicDate":"1967-01-01T10:50:36","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Pre-Olympia Pleistocene stratigraphy and chronology in the central Puget Lowland, Washington","docAbstract":"Drifts of two pre-Olympia glaciations separated by nonglacial sediments are widespread in the central Puget Lowland of western Washington. The Double Bluff Drift (older) and Possession Drift represent advances of the Puget lobe of the Cordilleran ice sheet more than 40,000 years ago. The nonglacial Whidbey Formation between the drifts was formed in streams and lakes. During its deposition, climate was initially cool and moist, as inferred from pollen in peat beds, but subsequently it became much like that of the present in the lowland. The Possession Drift is tentatively correlated with glacial deposits of Salmon Springs age in the southern part of the lowland. The Whidbey Formation may correlate with nonglacial deposits between two Salmon Springs Drifts or with the Puyallup Formation.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1967)78[13:PPSACI]2.0.CO;2","usgsCitation":"Easterbrook, D.J., Crandell, D., and Leopold, E.B., 1967, Pre-Olympia Pleistocene stratigraphy and chronology in the central Puget Lowland, Washington: GSA Bulletin, v. 78, no. 1, p. 13-20, https://doi.org/10.1130/0016-7606(1967)78[13:PPSACI]2.0.CO;2.","productDescription":"8 p.","startPage":"13","endPage":"20","costCenters":[],"links":[{"id":426558,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Central Puget Lowland","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.13981196181514,\n 48.3375501570402\n ],\n [\n -122.85544279427498,\n 48.35045469190817\n ],\n [\n -122.85544279427498,\n 47.76461892070904\n ],\n [\n -122.13981196181516,\n 47.75902516658033\n ],\n [\n -122.13981196181514,\n 48.3375501570402\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"78","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Easterbrook, D. J.","contributorId":55089,"corporation":false,"usgs":true,"family":"Easterbrook","given":"D.","middleInitial":"J.","affiliations":[],"preferred":false,"id":896491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crandell, Dwight R.","contributorId":75946,"corporation":false,"usgs":true,"family":"Crandell","given":"Dwight R.","affiliations":[],"preferred":false,"id":896492,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leopold, Estella B.","contributorId":30979,"corporation":false,"usgs":true,"family":"Leopold","given":"Estella","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":896493,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70270905,"text":"70270905 - 1967 - Water resources of the Guanica area, Puerto Rico: A preliminary appraisal, 1963","interactions":[],"lastModifiedDate":"2025-08-29T14:38:32.636793","indexId":"70270905","displayToPublicDate":"1967-01-01T10:37:37","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources of the Guanica area, Puerto Rico: A preliminary appraisal, 1963","docAbstract":"Guánica and the lower Rio Loco valley lie between the extensive agricultural development in Lajas Valley to the west and the industrial development at Guayanilla to the east. Having a protected deep-water port, the Guánica area is particularly well suited to further development. The economic growth of the area depends, in important degree, on the amount of water available-water in the immediate area or water to be brought in from other areas.
The purpose of the study of the Guánica area was to evaluate the water supply in the immediate area. How much water is there? How much water moves through the area and what are the factors that control the movement? What is the composition of the water? And how much more water can be used?
The study itself took one year. Active data collection included measurements of streamflow, measurements of water levels in wells, measurements of well discharge, chemical analyses of surface and ground water, geologic reconnaissance, and considerable interviewing. Information for more than one year was obtained for rainfall and other weather data, well pumpage, water leaving Lago loco, and water used by the Southwestern Puerto Rico project.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70270905","collaboration":"In cooperation with the Commonwealth of Puerto Rico","usgsCitation":"McClymonds, N.E., 1967, Water resources of the Guanica area, Puerto Rico: A preliminary appraisal, 1963, Report: 43 p.; 2 Figures: 13.90 x 22.82 inches and 13.89 x 8.24 inches, https://doi.org/10.3133/70270905.","productDescription":"Report: 43 p.; 2 Figures: 13.90 x 22.82 inches and 13.89 x 8.24 inches","costCenters":[],"links":[{"id":495081,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70270905/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":495080,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70270905/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":495082,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70270905/figure-7.pdf","text":"Figure 7","linkFileType":{"id":1,"text":"pdf"}},{"id":495079,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70270905/report-thumb.jpg"}],"country":"Puerto Rico","city":"Guanica","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -67.41782863900221,\n 18.61812040597721\n ],\n [\n -67.41782863900221,\n 17.80333089063508\n ],\n [\n -65.56416750050371,\n 17.80333089063508\n ],\n [\n -65.56416750050371,\n 18.61812040597721\n ],\n [\n -67.41782863900221,\n 18.61812040597721\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McClymonds, Neal E.","contributorId":360640,"corporation":false,"usgs":false,"family":"McClymonds","given":"Neal","middleInitial":"E.","affiliations":[],"preferred":false,"id":947337,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221354,"text":"70221354 - 1967 - Critique of the principle of uniformity","interactions":[],"lastModifiedDate":"2021-06-14T11:44:50.216612","indexId":"70221354","displayToPublicDate":"1967-01-01T07:57:11","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3459,"text":"Special Paper of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Critique of the principle of uniformity","docAbstract":"No abstract available.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/SPE89-p3","usgsCitation":"Hubbert, M.K., 1967, Critique of the principle of uniformity: Special Paper of the Geological Society of America, v. 89, p. 3-33, https://doi.org/10.1130/SPE89-p3.","productDescription":"31 p.","startPage":"3","endPage":"33","costCenters":[],"links":[{"id":386446,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"89","noUsgsAuthors":false,"publicationDate":"1967-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hubbert, M. King","contributorId":50197,"corporation":false,"usgs":true,"family":"Hubbert","given":"M.","email":"","middleInitial":"King","affiliations":[],"preferred":false,"id":817472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70156255,"text":"70156255 - 1967 - Devonian of the Southwestern United States","interactions":[],"lastModifiedDate":"2015-08-17T13:17:10","indexId":"70156255","displayToPublicDate":"1967-01-01T01:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Devonian of the Southwestern United States","docAbstract":"The structural framework that controlled Devonian deposition consisted of, from west to east: (1) a eugeosynclinal area in northern California and western Nevada; (2) a miogeosynclinal area in southeastern California, eastern Nevada, and western Utah; and (3) a cratonic area in Arizona, eastern Utah, Colorado, New Mexico, and western Texas, east of a northeast-trending hinge line (Wasatch line).
\nThe eugeosyncline contains a fragmentary record of Middle Devonian rocks at least 4,000 feet thick characterized by thin-bedded chert, siliceous mudstone, and some limestone and volcanic rocks. The original thickness, however, probably exceeded 6,000 feet and probably included Lower and Upper Devonian rocks. The miogeosyncline contains Lower, Middle, and Upper Devonian rocks as much as 6,000 feet thick characterized by thick units of dolomite and limestone and some local interbeds of sandstone. A transitional zone perhaps 50 miles wide separates the eugeosynclinal and miogeosynclinal facies. The craton contains mostly Upper Devonian rocks, generally less than 1,000 feet thick, characterized by dolomite and limestone and local interbeds of sandstone and mudstone.
\nWidespread crustal movements occurred during Late Devonian time. The Antler orogeny in Nevada initiated a culm facies in the geosyncline. Eugeosynclinal and transitional rocks including those of Devonian age were uplifted to form the Antler orogenic belt, and then were thrust eastward over autochthonous miogeosynclinal rocks in latest Devonian or earliest Mississippian time. Folding and faulting, and subsequent erosion on local uplifts, produced clastic deposits of Late Devonian age in Utah and southwestern Colorado.
\nDevonian rocks in many parts of the geosynclinal area have been moved since Devonian time by large-scale, generally eastward thrusting, oroflexural bending and strike-slip faulting.
\nFour major subdivisions of the Devonian System and related rocks are treated separately:
\n1) Lower Devonian (Gedinnian, Siegenian, Emsian) and related Upper Silurian (Ludlovian) rocks.
\n2) Middle Devonian (Eifelian and Givetian) rocks.
\n3) Lower Upper Devonian (Frasnian, to I) rocks.
\n4) Upper Upper Devonian (Famennian, to II-VI) and related lowermost Mississippian (Tournaisian, cu I) rocks.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"International symposium on the Devonian system","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"International symposium on the Devonian system","conferenceDate":"1967","conferenceLocation":"Calgary, Alberta, Canada","language":"English","publisher":"Alberta Society of Petroleum Geologists","publisherLocation":"Calgary, Alberta","usgsCitation":"Poole, F.G., Baars, D., Drewes, H., Hayes, P.T., Ketner, K.B., McKee, E., Teichert, C., and Williams, J.S., 1967, Devonian of the Southwestern United States, in International symposium on the Devonian system, v. I, Calgary, Alberta, Canada, 1967, p. 879-912.","productDescription":"34 p.","startPage":"879","endPage":"912","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":306806,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"state":"Arizona, California, Colorado, Nevada, New Mexico, 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D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":568265,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Teichert, C.","contributorId":17755,"corporation":false,"usgs":false,"family":"Teichert","given":"C.","email":"","affiliations":[{"id":6773,"text":"University of Kansas","active":true,"usgs":false}],"preferred":false,"id":568266,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Williams, J. S.","contributorId":65819,"corporation":false,"usgs":false,"family":"Williams","given":"J.","email":"","middleInitial":"S.","affiliations":[{"id":12682,"text":"Utah State University, Logan, UT","active":true,"usgs":false}],"preferred":false,"id":568267,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":70156254,"text":"70156254 - 1967 - Devonian of the Northern Rocky Mountains and plains","interactions":[],"lastModifiedDate":"2015-08-17T12:47:04","indexId":"70156254","displayToPublicDate":"1967-01-01T01:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Devonian of the Northern Rocky Mountains and plains","docAbstract":"The Devonian System, represented predominantly by shallow-water marine carbonate, is widespread in Montana, Wyoming, eastern Idaho, North Dakota, South Dakota, and northwestern Nebraska. It comprises cratonic rocks in the east and miogeosynclinal rocks in the west.
\nThe cratonic rocks thicken generally northward from their southern limit in Wyoming across a broad shelf that occupies most of Wyoming and Montana. In northern Montana, they are as much as 1,250 feet thick. Cratonic rocks also thicken eastward from areas of Early Mississippian erosional thinning in central and eastern Montana to as much as 2,000 feet in the intracratonic Williston basin centered in northwestern North Dakota.
\nThe miogeosynclinal rocks, which moved eastward on low-angle thrust faults, abut against cratonic rocks along a north-trending disturbed belt in western Wyoming, western Montana and eastern Idaho. The miogeosynclinal rocks thicken abruptly westward from 1,000 feet near this belt to about 3,000 feet near the east edge of the Idaho batholith. Farther west they have been buried beneath younger rocks, altered by the batholith, or eroded.
\nFive subdivisions of the Devonian System are treated separately:
\n1. Upper Lower Devonian (Coblenzian) marginal and nearshore marine carbonate rocks and related continental and estuarine discontinuous sinkhole and channel-fill deposits.
\n2. Upper Middle Devonian (Givetian) carbonate rocks that contain a 525-foot-thick evaporitic sequence in the Williston basin.
\n3. Lower Upper Devonian (Frasnian, toI) cyclically deposited carbonate rocks that include thick beds of dolarenite and dolomitized calcarenite on the west.
\n4. Upper Upper Devonian (Famennian, toII-IV) evaporitic rocks overlain by fossilferous open-marine shale and limestone.
\n5. Undivided uppermost Devonian (Famennian, to V-VI) and lowermost Mississippian (Tournaisian, cuI-lower cuIIα) carbonaceous and clastic rocks deposited in six shallow basins interspersed among areas uplifted during the penecontemporaneous Antler orogeny.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"International symposium on the Devonian system","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"International symposium on the Devonian system","conferenceLocation":"Calgary, Alberta, Canada","language":"English","publisher":"Alberta Society of Petroleum Geologists","publisherLocation":"Calgary, Alberta","usgsCitation":"Sandberg, C.A., and Mapel, W., 1967, Devonian of the Northern Rocky Mountains and plains, in International symposium on the Devonian system, v. I, Calgary, Alberta, Canada, p. 843-877.","productDescription":"35 p.","startPage":"843","endPage":"877","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":306804,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho, Montana, Nebraska, North Dakota, South Dakota, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.83984375,\n 41.83682786072714\n ],\n [\n -115.83984375,\n 49.210420445650286\n ],\n [\n -96.240234375,\n 49.210420445650286\n ],\n [\n -96.240234375,\n 41.83682786072714\n ],\n [\n -115.83984375,\n 41.83682786072714\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"I","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d305b1e4b0518e35468ceb","contributors":{"authors":[{"text":"Sandberg, Charles A. sandberg@usgs.gov","contributorId":2362,"corporation":false,"usgs":true,"family":"Sandberg","given":"Charles","email":"sandberg@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":568253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mapel, William J.","contributorId":89796,"corporation":false,"usgs":true,"family":"Mapel","given":"William J.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":568254,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2000010,"text":"2000010 - 1967 - Physical limnology of Saginaw Bay, Lake Huron","interactions":[],"lastModifiedDate":"2012-02-02T00:15:00","indexId":"2000010","displayToPublicDate":"1967-01-01T01:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"12","title":"Physical limnology of Saginaw Bay, Lake Huron","docAbstract":"Water temperature and the distribution of various chemicals measured during surveys from June 7 to October 30, 1956, reflect a highly variable and rapidly changing circulation in Saginaw Bay, Lake Huron. The circulation is influenced strongly by local winds and by the stronger circulation of Lake Huron which frequently causes injections of lake water to the inner extremity of the bay. The circulation patterns determined at six times during 1956 reflect the general characteristics of a marine estuary of the northern hemisphere. The prevailing circulation was counterclockwise; the higher concentrations of solutes from the Saginaw River tended to flow and enter Lake Huron along the south shore; water from Lake Huron entered the northeast section of the bay and had a dominant influence on the water along the north shore of the bay.\nThe concentrations of major ions varied little with depth, but a decrease from the inner bay toward Lake Huron reflected the dilution of Saginaw River water as it moved out of the bay. Concentrations in the outer bay were not much greater than in Lake Huron proper. The proportions of various cations and anions were similar to the average proportions for the freshwaters of the world.\nThe average flushing time was 186 days, but was 113 days during the period of peak river discharge. The lakeward transport of Saginaw River water ranged from 619 to 2,294 feet per day in the inner bay to 1,410 to 3,000 feet per day in the outer bay on June 7 and October 30, respectively.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"Beeton, A.M., Smith, S.H., and Hooper, F.F., 1967, Physical limnology of Saginaw Bay, Lake Huron: Technical Report 12, 56 p.","productDescription":"56 p.","startPage":"0","endPage":"56","numberOfPages":"56","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92062,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr12.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685b43","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":324922,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":324921,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hooper, Frank F.","contributorId":97847,"corporation":false,"usgs":true,"family":"Hooper","given":"Frank","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":324923,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2000033,"text":"2000033 - 1967 - Lamprey control and research","interactions":[],"lastModifiedDate":"2023-04-07T15:16:10.327683","indexId":"2000033","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":156,"text":"Annual Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"1965","title":"Lamprey control and research","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Annual report of the Great Lakes Fishery Commission 1965","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"Great Lakes Fishery Commission","usgsCitation":"Smith, B.R., 1967, Lamprey control and research: Annual Report 1965.","startPage":"27","endPage":"45","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198945,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":415419,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.glfc.org/annual-reports.php","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b425c","contributors":{"authors":[{"text":"Smith, Bernard R.","contributorId":38924,"corporation":false,"usgs":true,"family":"Smith","given":"Bernard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":324959,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000252,"text":"1000252 - 1967 - Diatoms as food of larval sea lampreys in a small tributary of northern Lake Michigan","interactions":[],"lastModifiedDate":"2016-02-22T09:22:41","indexId":"1000252","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Diatoms as food of larval sea lampreys in a small tributary of northern Lake Michigan","docAbstract":"The food and food preferences of sea lamprey ammocoetes have not been investigated. The food of the larval American brook lamprey, Lampetra lamottei, in the Great Lakes region consisted mainly of diatoms and desmids according to Creaser and Hann. Schroll discussed the biology of feeding of ammocoetes of Lampetra planeri and Eudontomyzon danfordi in Europe. This report presents data on the availability and use of diatoms by sea lamprey, Petromyzon marinus Linnaeus, ammocoetes in a small tributary of northern Lake Michigan.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1967)96[224:DAFOLS]2.0.CO;2","usgsCitation":"Manion, P.J., 1967, Diatoms as food of larval sea lampreys in a small tributary of northern Lake Michigan: Transactions of the American Fisheries Society, v. 96, no. 2, p. 224-226, https://doi.org/10.1577/1548-8659(1967)96[224:DAFOLS]2.0.CO;2.","productDescription":"3 p.","startPage":"224","endPage":"226","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65da87","contributors":{"authors":[{"text":"Manion, Patrick J.","contributorId":99080,"corporation":false,"usgs":true,"family":"Manion","given":"Patrick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308295,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000253,"text":"1000253 - 1967 - Morphological abnormalities among lampreys","interactions":[],"lastModifiedDate":"2023-12-06T22:24:33.709457","indexId":"1000253","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"Morphological abnormalities among lampreys","docAbstract":"The experimental control of the sea lamprey (Petromyzon marinus) in the Great Lakes has required the collection of thousands of lampreys. Representatives of each life stage of the four species of the Lake Superior basin were examined for structural abnormalities. The most common aberration was the presence of additional tails. The accessory tails were always postanal and smaller than the normal tail. The point of origin varied; the extra tails occurred on dorsal, ventral, or lateral surfaces. Some of the extra tails were misshaped and curled, but others were normal in shape and pigment pattern. Other abnormalities in larval sea lampreys were malformed or twisted tails and bodies. The cause of the structural abnormalities is unknown. The presence of extra caudal fins could be genetically controlled, or be due to partial amputation or injury followed by abnormal regeneration. Few if any lampreys with structural abnormalities live to sexual maturity.","language":"English","publisher":"American Society of Ichthyologists and Herpetologists (ASIH)","doi":"10.2307/1442255","usgsCitation":"Manion, P.J., 1967, Morphological abnormalities among lampreys: Copeia, v. 1967, no. 3, p. 680-681, https://doi.org/10.2307/1442255.","productDescription":"2 p.","startPage":"680","endPage":"681","numberOfPages":"2","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132838,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1967","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698cb9","contributors":{"authors":[{"text":"Manion, Patrick J.","contributorId":99080,"corporation":false,"usgs":true,"family":"Manion","given":"Patrick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308296,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000345,"text":"1000345 - 1967 - Returns of hatchery-reared lake trout in southern Lake Superior, 1955-62","interactions":[],"lastModifiedDate":"2016-02-22T09:30:22","indexId":"1000345","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Returns of hatchery-reared lake trout in southern Lake Superior, 1955-62","docAbstract":"Experimental plantings of fin-clipped lake trout (Salvelinus namaycush) of various ages have been made in southern Lake Superior since 1952. The catch of planted lake trout by the commercial fishery was used to measure the success of stocking. Estimates of total returns were based on samples of 8.2 to 21.2% of the Wisconsin catches in 1955-62 and 36.4 to 46.8% of the Michigan catches in 1959-62. Marked lake trout were assigned to various plantings according to the fin mark, length of fish, readings of age from scales, and locations of capture. Estimated returns from Wisconsin plantings of 9-month-old lake trout varied from 2.1 to 6.4%. Wisconsin releases of 16-month-old fish yielded returns of 5.7 to 37.3%. Returns from plantings in Michigan were 0.3% for 9-month-old fish and 1.5 to 3.8% for 16-month-old fish. The ratios of the returns from plantings of 16-month-old fish to those of 9-month-old fish were 3.9:1 for Wisconsin releases and 6.7:1 for Michigan releases. Lake trout planted in Wisconsin generally survived better than those released in Michigan. Returns from fish planted at ages of 17 to 40 months in Michigan in 1958-59 were far greater than those from 16-month-old fish released in Michigan, but were not as high as from the most successful plantings of 16-month-old fish in Wisconsin. Lake trout released in 1960 from shore and from boats survived equally well. Average size of lake trout at release was more closely related to survival than any other factor. All except 1 of 10 highly successful releases were of fish larger than 22 per lb, and all 6 poor releases were of fish smaller than 34 per lb. Fish that ran 22 to 33 per lb survived only moderately well. A size of 17 to 20 fish per lb appears to be close to optimum. Abundance of native lake trout, American smelt (Osmerus mordax), and sea lampreys (Petromyzon marinus) all appeared to be unrelated to stocking success. The only apparent method of rapidly improving the success of stocking is to rear all lake trout to an average size of 17 to 20 per lb.
","language":"English","publisher":"NRC Research Press","doi":"10.1139/f67-028","usgsCitation":"Pycha, R.L., and King, G.R., 1967, Returns of hatchery-reared lake trout in southern Lake Superior, 1955-62: Journal of the Fisheries Research Board of Canada, v. 24, no. 2, p. 281-298, https://doi.org/10.1139/f67-028.","productDescription":"18 p.","startPage":"281","endPage":"298","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133265,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47f4e4b07f02db4c47bb","contributors":{"authors":[{"text":"Pycha, Richard L.","contributorId":17175,"corporation":false,"usgs":true,"family":"Pycha","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308430,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, George R.","contributorId":74721,"corporation":false,"usgs":true,"family":"King","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308431,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42164,"text":"ofr67251 - 1967 - Aeromagnetic map of the San Antonio Ranch, Baxter Spring, Lone Mountain, and Tonopah quadrangles and part of the Antelope Spring quadrangle, Nevada","interactions":[],"lastModifiedDate":"2023-03-21T19:58:28.028531","indexId":"ofr67251","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"67-251","title":"Aeromagnetic map of the San Antonio Ranch, Baxter Spring, Lone Mountain, and Tonopah quadrangles and part of the Antelope Spring quadrangle, Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67251","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the San Antonio Ranch, Baxter Spring, Lone Mountain, and Tonopah quadrangles and part of the Antelope Spring quadrangle, Nevada: U.S. Geological Survey Open-File Report 67-251, 1 Plate: 45.00 x 42.00 inches, https://doi.org/10.3133/ofr67251.","productDescription":"1 Plate: 45.00 x 42.00 inches","costCenters":[],"links":[{"id":172631,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414492,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8206.htm","linkFileType":{"id":5,"text":"html"}},{"id":98809,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0251/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","otherGeospatial":"San Antonio Ranch, Baxter Spring, Lone Mountain, Tonopah, and Antelope Spring quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.5,\n 38.5\n ],\n [\n -117.5,\n 38\n ],\n [\n -116.911,\n 38\n ],\n [\n -116.911,\n 38.5\n ],\n [\n -117.5,\n 38.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db69145b","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530881,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":33719,"text":"b1242E - 1967 - Coal resources of the Cape Lisburne-Colville River region, Alaska","interactions":[],"lastModifiedDate":"2023-03-03T22:56:57.772461","indexId":"b1242E","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1242","chapter":"E","title":"Coal resources of the Cape Lisburne-Colville River region, Alaska","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1242E","usgsCitation":"Barnes, F.F., 1967, Coal resources of the Cape Lisburne-Colville River region, Alaska: U.S. Geological Survey Bulletin 1242, Report: iii, 37 p.; 1 Plate: 30.14 x 19.48 inches, https://doi.org/10.3133/b1242E.","productDescription":"Report: iii, 37 p.; 1 Plate: 30.14 x 19.48 inches","costCenters":[],"links":[{"id":163762,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1242e/report-thumb.jpg"},{"id":96075,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1242e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":96074,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1242e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109668,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21324.htm","linkFileType":{"id":5,"text":"html"},"description":"21324"}],"country":"United States","state":"Alaska","otherGeospatial":"Cape Lisburne-Colville River region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -150,\n 71\n ],\n [\n -166.417,\n 71\n ],\n [\n -166.417,\n 68\n ],\n [\n -150,\n 68\n ],\n [\n -150,\n 71\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aee1d","contributors":{"authors":[{"text":"Barnes, Farrell F.","contributorId":58624,"corporation":false,"usgs":true,"family":"Barnes","given":"Farrell","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":211828,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}