A drive trap, used to capture dusky grouse (Dendragapus obscurus obscurus) females and their broods for transplantation, is described. The trap consists of two 75-foot wings, leading to a netting-covered enclosure with a smaller wooden catch box at the rear. A four-man crew finds a brood in open cover and, while one or two men keep the brood under observation, the others rig the trap along the birds' anticipated route to cover. It takes about 10-20 minutes to set up the trap, depending on roughness of terrain, and another 5-60 minutes to make the catch. The trap was tried on seven broods, of which five were caught entire and all but one bird from each of the other two broods were captured. Two additional broods were accidentally flushed before the trap could be used.
","language":"English","publisher":"Wiley","doi":"10.2307/3798466","usgsCitation":"Tomlinson, R.E., 1963, A method for drive-trapping dusky grouse: Journal of Wildlife Management, v. 27, no. 4, p. 563-566, https://doi.org/10.2307/3798466.","productDescription":"4 p.","startPage":"563","endPage":"566","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":486902,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3798466","text":"Publisher Index Page"},{"id":198286,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae0c8","contributors":{"authors":[{"text":"Tomlinson, R. E.","contributorId":78830,"corporation":false,"usgs":true,"family":"Tomlinson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":332165,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5220603,"text":"5220603 - 1963 - Disease and infection in the Tetraonidae","interactions":[],"lastModifiedDate":"2025-02-05T16:09:43.720999","indexId":"5220603","displayToPublicDate":"1963-10-04T00:00:00","publicationYear":"1963","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":"Disease and infection in the Tetraonidae","docAbstract":"Disease is one of many factors advanced to explain the fluctuations of grouse populations, but no profound study of natural disease losses in Tetraonidae exists. The literature contains frequent references to THE grouse disease, although many potential pathogens are listed in numerous surveys and limited investigations, and the relevant data indicate that no single etiologic agent is universally responsible for disease in grouse. Few experimental infections or related studies on parasite biology have been attempted. Well-trained personnel and specialized facilities are required for research and analysis (1) to develop new methods of interpretation to be used with existing census techniques, (2) to conduct intensive studies of ecological factors of host and habitat, and (3) to establish base lines for recognition of deviations from the norm. Disease in wildlife can be controlled only through management procedures based on information concerning the biology of pathogens, hosts, and environments. It cannot be studied as a separate entity if its impact on survival or population fluctuations of grouse is to be correctly assessed.","language":"English","publisher":"Wiley","doi":"10.2307/3798499","usgsCitation":"Herman, C.M., 1963, Disease and infection in the Tetraonidae: Journal of Wildlife Management, v. 27, no. 4, p. 850-855, https://doi.org/10.2307/3798499.","productDescription":"6 p.","startPage":"850","endPage":"855","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196345,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a59e","contributors":{"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":332092,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221091,"text":"70221091 - 1963 - Water-level trends in key observation well May-July 1963 (Abstracted from U. S. Geological Survey “Water Resources Review”)","interactions":[],"lastModifiedDate":"2021-06-01T19:30:58.880533","indexId":"70221091","displayToPublicDate":"1963-10-01T14:28:07","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Water-level trends in key observation well May-July 1963 (Abstracted from U. S. Geological Survey “Water Resources Review”)","docAbstract":"No abstract available.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1963.tb01934.x","usgsCitation":"West, S.W., 1963, Water-level trends in key observation well May-July 1963 (Abstracted from U. S. Geological Survey “Water Resources Review”): Groundwater, v. 1, no. 4, p. 50-50, https://doi.org/10.1111/j.1745-6584.1963.tb01934.x.","productDescription":"1 p.","startPage":"50","endPage":"50","costCenters":[],"links":[{"id":386070,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"West, S. W.","contributorId":104029,"corporation":false,"usgs":true,"family":"West","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":816726,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221090,"text":"70221090 - 1963 - Television — A new tool for the ground‐water geologist","interactions":[],"lastModifiedDate":"2021-06-01T19:26:42.462439","indexId":"70221090","displayToPublicDate":"1963-10-01T14:22:28","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Television — A new tool for the ground‐water geologist","docAbstract":"The television camera has become a tool of the ground‐water geologist, enabling him to examine visually the inside of a well deep below the land surface. Using the camera, the rocks can be viewed in place. Of great importance to the ground‐water studies in coastal Georgia, the camera enables the geologist to see the important water‐bearing zones in a limestone aquifer, and to recognize cracks and solution cavities, the changes in geologic formations, and the irregularities in the well bore that indicate the relative hardness of the rocks. The engineer, well driller, and water developer can examine a well when “trouble shooting” to see whether the casing is broken, whether screens are eroded, or whether the well contains obstructions.
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1963.tb01926.x","usgsCitation":"Callahan, J., Wait, R.L., and McCollum, M., 1963, Television — A new tool for the ground‐water geologist: Groundwater, v. 1, no. 4, p. 4-6, https://doi.org/10.1111/j.1745-6584.1963.tb01926.x.","productDescription":"3 p.","startPage":"4","endPage":"6","costCenters":[],"links":[{"id":386069,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia","otherGeospatial":"coastal Georgia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.32080078125,\n 32.519026027827515\n ],\n [\n -81.859130859375,\n 30.873940237887624\n ],\n [\n -81.968994140625,\n 30.477082932837682\n ],\n [\n -81.221923828125,\n 30.391830328088137\n ],\n [\n -80.66162109375,\n 32.045332838858506\n ],\n [\n -81.32080078125,\n 32.519026027827515\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Callahan, J.T.","contributorId":100920,"corporation":false,"usgs":true,"family":"Callahan","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":816723,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wait, R. L.","contributorId":15988,"corporation":false,"usgs":true,"family":"Wait","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":816724,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCollum, M.J.","contributorId":40576,"corporation":false,"usgs":true,"family":"McCollum","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":816725,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":37471,"text":"37471 - 1963 - Waterfowl status report, 1963","interactions":[],"lastModifiedDate":"2014-07-15T13:28:46","indexId":"37471","displayToPublicDate":"1963-10-01T13:27:21","publicationYear":"1963","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":"75","title":"Waterfowl status report, 1963","docAbstract":"No abstract available.","language":"English","publisher":"U.s. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Glover, F., and Smith, J.D., 1963, Waterfowl status report, 1963: Special Scientific Report - Wildlife 75, iv, 178 p.","productDescription":"iv, 178 p.","numberOfPages":"182","costCenters":[],"links":[{"id":290140,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64debe4b0001bd51477d8","contributors":{"authors":[{"text":"Glover, F.A.","contributorId":71485,"corporation":false,"usgs":true,"family":"Glover","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":218134,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, J. Donald","contributorId":12380,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"","middleInitial":"Donald","affiliations":[],"preferred":false,"id":218133,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25147,"text":"25147 - 1963 - Chemical analyses of surface waters in Colorado, October 1959 to September 1962","interactions":[],"lastModifiedDate":"2025-07-21T20:15:08.184674","indexId":"25147","displayToPublicDate":"1963-10-01T11:59:21","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Chemical analyses of surface waters in Colorado, October 1959 to September 1962","docAbstract":"Data presented herein are records of water quality for the period October 1959 to September 1962 for the sampling sites shown below and on the enclosed map. The data are preliminary and subject to revision. Final records are published in the annual series of Geological Survey Water-Supply Papers entitled \"Quality of Surface Waters of the United States, \" which can be obtained from the Superintendent of Documents, U. S. Government Printing Office, Washington, D. C. 20242.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/25147","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Chemical analyses of surface waters in Colorado, October 1959 to September 1962, 56 p., https://doi.org/10.3133/25147.","productDescription":"56 p.","temporalStart":"1959-10-01","temporalEnd":"1962-09-30","costCenters":[],"links":[{"id":492699,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/25147/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":290129,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/25147/report-thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0603,36.9924 ], [ -109.0603,41.0034 ], [ -102.0409,41.0034 ], [ -102.0409,36.9924 ], [ -109.0603,36.9924 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64d78e4b0001bd5147745","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":529183,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221113,"text":"70221113 - 1963 - Recharge rates of principal aquifers in Lake County, Indiana","interactions":[],"lastModifiedDate":"2021-06-02T13:56:06.824623","indexId":"70221113","displayToPublicDate":"1963-10-01T08:50:34","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Recharge rates of principal aquifers in Lake County, Indiana","docAbstract":"The upper 350 to 400 feet of rocks underlying Lake County, Indiana, form a single but complex hydrologic system. The rock units composing this system consist (in ascending order) of dolomite, clay till (unit 4), glaciofluvial sand (unit 3), clay till (unit 2), and lacustrine sand, silt, and clay (unit 1). The dolomite and unit 3 form the principal aquifers and the clay tills, units 4 and 2, the confining layers. The geohydrology of the confining layers controls to a large extent the rate at which the aquifers are recharged from local precipitation and, thereby, their potential yield. Unit 4, the dolomite's confining layer, has an estimated average vertical permeability of about 0.003 gpd (gallon per day) per square foot. Under present conditions of head difference, the rate of recharge to the dolomite through unit 4 is estimated to average 20,000 gpd per square mile. Unit 2, the confining layer for unit 3, has an average estimated vertical permeability of about 0.007 gpd per square foot. Under present conditions of head difference the recharge through unit 3's confining layer is estimated to average about 100,000 gpd per square mile. However, these rates of recharge can be expected to increase as the head difference across each confining layer increases with extensive development of the aquifer.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1963.tb01928.x","usgsCitation":"Rosenshein, J., 1963, Recharge rates of principal aquifers in Lake County, Indiana: Groundwater, v. 1, no. 4, p. 13-20, https://doi.org/10.1111/j.1745-6584.1963.tb01928.x.","productDescription":"8 p.","startPage":"13","endPage":"20","costCenters":[],"links":[{"id":386122,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Indiana","county":"Lake County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.528076171875,\n 41.017210578228436\n ],\n [\n -86.9073486328125,\n 41.017210578228436\n ],\n [\n -86.9073486328125,\n 41.701627343789205\n ],\n [\n -87.528076171875,\n 41.701627343789205\n ],\n [\n -87.528076171875,\n 41.017210578228436\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"1","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Rosenshein, J.S.","contributorId":95082,"corporation":false,"usgs":true,"family":"Rosenshein","given":"J.S.","affiliations":[],"preferred":false,"id":816791,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014049,"text":"1014049 - 1963 - The embronic and larval development of the rainbow trout","interactions":[],"lastModifiedDate":"2026-04-15T16:07:10.989268","indexId":"1014049","displayToPublicDate":"1963-10-01T00:00:00","publicationYear":"1963","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":"The embronic and larval development of the rainbow trout","docAbstract":"Photographs of the developing rainbow trout, Salmo gairdneri Richardson, are presented in sequence from the initial cleavage through hatching. Approximately 3,000 eggs were incubated in standard hatchery troughs supplied with spring water at a constant temperature of 54° F. Accepted fish cultural methods were followed to insure normal developmental patterns. Samples of these eggs were taken for study at 1‐hour intervals from the 5th to the 24th hour after fertilization; then once every 6 hours until they were 72 hours old; then at 1‐day intervals through the peak of hatching on the 23rd day. The embryos were fixed in 5 percent neutral formalin containing 0.95 percent sodium chloride, stained in Harrisˈ hematoxylin, and photographed with a vertically mounted camera.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1963)92[344:TEALDO]2.0.CO;2","usgsCitation":"Knight, A., 1963, The embronic and larval development of the rainbow trout: Transactions of the American Fisheries Society, v. 92, no. 4, p. 344-355, https://doi.org/10.1577/1548-8659(1963)92[344:TEALDO]2.0.CO;2.","productDescription":"12 p.","startPage":"344","endPage":"355","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131454,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"92","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dd4c","contributors":{"authors":[{"text":"Knight, A.E.","contributorId":15566,"corporation":false,"usgs":true,"family":"Knight","given":"A.E.","email":"","affiliations":[],"preferred":false,"id":319686,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1007573,"text":"1007573 - 1963 - Residual premolar roots in pocket mice","interactions":[],"lastModifiedDate":"2026-03-12T16:12:28.985606","indexId":"1007573","displayToPublicDate":"1963-10-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3634,"text":"Transactions of the Kansas Academy of Science","active":true,"publicationSubtype":{"id":10}},"title":"Residual premolar roots in pocket mice","docAbstract":"No abstract available.
","language":"English","publisher":"Kansas Academy of Science","doi":"10.2307/3626550","usgsCitation":"Douglas, C.L., 1963, Residual premolar roots in pocket mice: Transactions of the Kansas Academy of Science, v. 66, no. 3, p. 513-515, https://doi.org/10.2307/3626550.","productDescription":"3 p.","startPage":"513","endPage":"515","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130193,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"66","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629eb0","contributors":{"authors":[{"text":"Douglas, C. L.","contributorId":64586,"corporation":false,"usgs":true,"family":"Douglas","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":315649,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014134,"text":"1014134 - 1963 - An aid in the preparation of blood samples from fish","interactions":[],"lastModifiedDate":"2025-08-01T16:10:06.350634","indexId":"1014134","displayToPublicDate":"1963-10-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"An aid in the preparation of blood samples from fish","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1963)25[174:AAITPO]2.0.CO;2","usgsCitation":"Snieszko, S.F., 1963, An aid in the preparation of blood samples from fish: Progressive Fish-Culturist, v. 25, no. 4, p. 174-174, https://doi.org/10.1577/1548-8659(1963)25[174:AAITPO]2.0.CO;2.","productDescription":"1 p.","startPage":"174","endPage":"174","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130491,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685b98","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319848,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171210,"text":"70171210 - 1963 - Reductive dechlorination of DDT to DDD by yeast","interactions":[],"lastModifiedDate":"2016-05-25T15:33:13","indexId":"70171210","displayToPublicDate":"1963-09-13T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Reductive dechlorination of DDT to DDD by yeast","docAbstract":"Labeled DDD [ 1,1-dichlor-o-2,2-bis(p-chlorophenyl)-ethane] was formed from C14-labeled DDT in the presence of yeast. The formation of DDD from DDE [1,1-dichloro-2,2-bis (p-chlorophenyl)-ethylene] was not observed, indicating that a reductive dechlorination of DDT occurs.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.141.3585.1050","usgsCitation":"Kallman, B.J., and Andrews, A.K., 1963, Reductive dechlorination of DDT to DDD by yeast: Science, v. 141, no. 3585, p. 1050-1051, https://doi.org/10.1126/science.141.3585.1050.","productDescription":"2 p.","startPage":"1050","endPage":"1051","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":321673,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"141","issue":"3585","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccc0e4b07e28b662dd14","contributors":{"authors":[{"text":"Kallman, Burton J.","contributorId":169580,"corporation":false,"usgs":false,"family":"Kallman","given":"Burton","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630274,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andrews, Austin K.","contributorId":85516,"corporation":false,"usgs":true,"family":"Andrews","given":"Austin","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":630275,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221081,"text":"70221081 - 1963 - Sinuosity of alluvial rivers on the great plains","interactions":[],"lastModifiedDate":"2021-06-01T18:35:40.027724","indexId":"70221081","displayToPublicDate":"1963-09-01T13:32:06","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Sinuosity of alluvial rivers on the great plains","docAbstract":"Data on the morphologic and sediment characteristics of stable alluvial rivers of the Great Plains were collected at 50 cross sections. The channel patterns of these rivers were classified into five types: tortuous, irregular, regular, transitional, and straight. Because no clear demarcation existed between each of the types, the pattern of the rivers was described by sinuosity, a ratio of channel length to valley length. The sinuosity ((P)) of these rivers is related to the shape of the channels expressed as a width-depth ratio (F) and to the percentage of silt and clay in the perimeter of the channel (M) as follows: Sinuous streams are characterized by a low width-depth ratio (F), a high percentage of silt-clay in the perimeter of the channel (M), a high percentage of silt-clay in the banks (although the banks of straight channels may also contain large amounts of silt-clay), and a lower gradient than straight channels having the same mean discharge. Discharge itself does not appear to affect the sinuosity of streams. Another possible distinction between straight and sinuous streams is in the proportions of the components of total sediment load. In a wide, shallow channel much of the sediment transported is bed-material load. In a narrow, deep channel most of the sediment transported is wash load. On the Great Plains both straight and sinuous streams may flow on the surface of alluvial valley fills at about the same valley slope. The departure of a stream from a straight course down the alluvial valley results from changes in both the caliber of the sediment load and in the relative proportions of bed-material load and wash load during the post-Pleistocene alluviation of these valleys. When during this alluviation the proportion of wash load increased, most probably by a decrease in bed-material load, the stream adjusted itself by decreasing its gradient through the development of a sinuous course. Recent changes in stream sinuosity in response to changes in the proportions of bed load and suspended load support this hypothesis.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1089:SOAROT]2.0.CO;2","usgsCitation":"Schumm, S.A., 1963, Sinuosity of alluvial rivers on the great plains: Geological Society of America Bulletin, v. 74, no. 9, p. 1089-1100, https://doi.org/10.1130/0016-7606(1963)74[1089:SOAROT]2.0.CO;2.","productDescription":"12 p.","startPage":"1089","endPage":"1100","costCenters":[],"links":[{"id":386056,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"74","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schumm, S. A.","contributorId":71957,"corporation":false,"usgs":true,"family":"Schumm","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":816711,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221074,"text":"70221074 - 1963 - Origin of some intermittent ponds on quartzite ridges in western North Carolina","interactions":[],"lastModifiedDate":"2021-06-01T17:36:55.332649","indexId":"70221074","displayToPublicDate":"1963-09-01T12:31:41","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Origin of some intermittent ponds on quartzite ridges in western North Carolina","docAbstract":"Several intermittent ponds and closed depressions as much as 200 feet wide occur on the crests of ridges in gently dipping Cambrian(?) quartzites in the southeastern foothills of the Blue Ridge Mountains near Morganton, North Carolina. The unconsolidated fill and debris in the ponds consists of clayey sand and saprolite with accessory minerals that could have been derived entirely from the quartzite. The pond water contains appreciable quantities of dissolved silica and with the aid of organic substances could have formed the depressions by solution since the beginning of the Pleistocene.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1183:OOSIPO]2.0.CO;2","usgsCitation":"Reed, J.C., Bryant, B.H., and Hack, J., 1963, Origin of some intermittent ponds on quartzite ridges in western North Carolina: Geological Society of America Bulletin, v. 74, no. 9, p. 1183-1188, https://doi.org/10.1130/0016-7606(1963)74[1183:OOSIPO]2.0.CO;2.","productDescription":"6 p.","startPage":"1183","endPage":"1188","costCenters":[],"links":[{"id":386047,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.87158203125,\n 36.56260003738545\n ],\n [\n -82.28759765625,\n 36.66841891894786\n ],\n [\n -82.5732421875,\n 35.99578538642032\n ],\n [\n -83.91357421875,\n 35.53222622770337\n ],\n [\n -84.1552734375,\n 35.24561909420681\n ],\n [\n -84.26513671875,\n 34.97600151317588\n ],\n [\n -82.7490234375,\n 35.08395557927643\n ],\n [\n -82.177734375,\n 35.24561909420681\n ],\n [\n -80.83740234375,\n 35.191766965947394\n ],\n [\n -80.74951171875,\n 34.77771580360469\n ],\n [\n -79.60693359375,\n 34.77771580360469\n ],\n [\n -78.46435546875,\n 33.76088200086917\n ],\n [\n -77.95898437499999,\n 33.8339199536547\n ],\n [\n -76.3330078125,\n 34.88593094075317\n ],\n [\n -75.6298828125,\n 35.8356283888737\n ],\n [\n -75.87158203125,\n 36.56260003738545\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Reed, John C. Jr.","contributorId":223980,"corporation":false,"usgs":false,"family":"Reed","given":"John","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":816700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bryant, Bruce H. bbryant@usgs.gov","contributorId":26713,"corporation":false,"usgs":true,"family":"Bryant","given":"Bruce","email":"bbryant@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":false,"id":816701,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hack, John T.","contributorId":45168,"corporation":false,"usgs":true,"family":"Hack","given":"John T.","affiliations":[],"preferred":false,"id":816702,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221069,"text":"70221069 - 1963 - Composition of fluid inclusions, cave-in-rock fluorite district, Illinois, and upper Mississippi valley zinc-lead district","interactions":[],"lastModifiedDate":"2021-06-01T17:09:48.318378","indexId":"70221069","displayToPublicDate":"1963-09-01T12:05:43","publicationYear":"1963","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":"Composition of fluid inclusions, cave-in-rock fluorite district, Illinois, and upper Mississippi valley zinc-lead district","docAbstract":"No abstract available.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.58.6.886","usgsCitation":"Hall, W., and Friedman, I., 1963, Composition of fluid inclusions, cave-in-rock fluorite district, Illinois, and upper Mississippi valley zinc-lead district: Economic Geology, v. 58, no. 6, p. 886-911, https://doi.org/10.2113/gsecongeo.58.6.886.","productDescription":"26 p.","startPage":"886","endPage":"911","costCenters":[],"links":[{"id":386042,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"6","noUsgsAuthors":false,"publicationDate":"1963-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hall, W. E.","contributorId":6431,"corporation":false,"usgs":true,"family":"Hall","given":"W. E.","affiliations":[],"preferred":false,"id":816691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":816692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221068,"text":"70221068 - 1963 - Distribution of fluorine in unaltered silicic volcanic rocks of the western conterminous United States","interactions":[],"lastModifiedDate":"2021-06-01T17:04:12.010628","indexId":"70221068","displayToPublicDate":"1963-09-01T11:59:53","publicationYear":"1963","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":"Distribution of fluorine in unaltered silicic volcanic rocks of the western conterminous United States","docAbstract":"An investigation of more than 170 samples of glass-rich volcanic rocks of rhyolitic or rhyodacitic composition shows marked regional variations in the fluorine content. The uniformity of the class of rocks was controlled by index of refraction determinations on fused beads and by chemical analyses of about one-seventh of the total number. The fluorine content ranges from 20 to 4,900 ppm. The frequency distribution closely approaches a log-normal one; the median value is 520 ppm, the 90 percentile 1,820 ppm. The mean for 167 samples is 820 ppm. These correspond fairly well with earlier averages for similar types of rocks. The highest values are predominantly from a belt in central Colorado and west-central New Mexico, from the Big Bend region of Texas, and from southeastern Idaho and western Utah and northeastern Nevada. The distribution of the fluorine in these rocks correlates well with the distribution of significant fluorspar deposits and somewhat less well with areas where volcanic rocks are prevalent and ground waters carry large amounts of fluorine.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.58.6.941","usgsCitation":"Coats, R., Gross, W., and Rader, L.F., 1963, Distribution of fluorine in unaltered silicic volcanic rocks of the western conterminous United States: Economic Geology, v. 58, no. 6, p. 941-951, https://doi.org/10.2113/gsecongeo.58.6.941.","productDescription":"11 p.","startPage":"941","endPage":"951","costCenters":[],"links":[{"id":386041,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"58","issue":"6","noUsgsAuthors":false,"publicationDate":"1963-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Coats, R.R.","contributorId":78339,"corporation":false,"usgs":true,"family":"Coats","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":816688,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gross, W.D.","contributorId":259165,"corporation":false,"usgs":false,"family":"Gross","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":816689,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rader, L. F. Jr.","contributorId":100909,"corporation":false,"usgs":true,"family":"Rader","given":"L.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":816690,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":37748,"text":"37748 - 1963 - Migratory game birds special permits: for salvage of sick, injured, or oil-soaked migratory game birds for rehabilitation and propagation: for acquisition and propagation of rare and endangered species","interactions":[],"lastModifiedDate":"2014-07-23T10:39:21","indexId":"37748","displayToPublicDate":"1963-09-01T10:38:49","publicationYear":"1963","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":"456","title":"Migratory game birds special permits: for salvage of sick, injured, or oil-soaked migratory game birds for rehabilitation and propagation: for acquisition and propagation of rare and endangered species","docAbstract":"No abstract available.","language":"English","publisher":"U.S Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Bureau of Sport Fisheries and Wildlife, 1963, Migratory game birds special permits: for salvage of sick, injured, or oil-soaked migratory game birds for rehabilitation and propagation: for acquisition and propagation of rare and endangered species: Wildlife Leaflet 456, 7 p.","productDescription":"7 p.","numberOfPages":"7","costCenters":[],"links":[{"id":290772,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcfdae4b0824b2d17612a","contributors":{"authors":[{"text":"U.S. Bureau of Sport Fisheries and Wildlife","contributorId":128149,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Sport Fisheries and Wildlife","id":529698,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37746,"text":"37746 - 1963 - Big game inventory for 1962","interactions":[],"lastModifiedDate":"2014-07-23T10:36:41","indexId":"37746","displayToPublicDate":"1963-09-01T10:35:53","publicationYear":"1963","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":"454","title":"Big game inventory for 1962","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.","usgsCitation":"U.S. Bureau of Sport Fisheries and Wildlife, 1963, Big game inventory for 1962 (Revises Wildlife Leaflet 342 (1952).): Wildlife Leaflet 454, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290771,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises Wildlife Leaflet 342 (1952).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcfdae4b0824b2d17612c","contributors":{"authors":[{"text":"U.S. Bureau of Sport Fisheries and Wildlife","contributorId":128149,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Sport Fisheries and Wildlife","id":529696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221115,"text":"70221115 - 1963 - Factors influencing the pore volume of fine-grained sediments under low-to-moderate overburden loads","interactions":[],"lastModifiedDate":"2021-06-02T15:40:56.925074","indexId":"70221115","displayToPublicDate":"1963-09-01T10:34:45","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3369,"text":"Sedimentology","active":true,"publicationSubtype":{"id":10}},"title":"Factors influencing the pore volume of fine-grained sediments under low-to-moderate overburden loads","docAbstract":"An anomalous increase of pore volume with increasing depth in the range 0—1,900 ft. occurs in fine‐grained sediments along the east side of the San Joaquin Valley of Cali‐ fornia. Several possible causes for the anomaly were inferred from a literature search and from study of the core samples. Statistical analyses of the core sample data suggest the principle causes to be variations in particle size, the diatom‐skeleton content, and the type of exchangeable cation adsorbed by the clay‐mineral constituents of the sediments.
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1365-3091.1963.tb01217.x","usgsCitation":"Meade, R., 1963, Factors influencing the pore volume of fine-grained sediments under low-to-moderate overburden loads: Sedimentology, v. 2, no. 3, p. 235-242, https://doi.org/10.1111/j.1365-3091.1963.tb01217.x.","productDescription":"8 p.","startPage":"235","endPage":"242","costCenters":[],"links":[{"id":386129,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"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 -121.6241455078125,\n 36.721273880045004\n ],\n [\n -119.7344970703125,\n 36.721273880045004\n ],\n [\n -119.7344970703125,\n 38.26406296833961\n ],\n [\n -121.6241455078125,\n 38.26406296833961\n ],\n [\n -121.6241455078125,\n 36.721273880045004\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"2","issue":"3","noUsgsAuthors":false,"publicationDate":"2006-06-14","publicationStatus":"PW","contributors":{"authors":[{"text":"Meade, R.H.","contributorId":27449,"corporation":false,"usgs":true,"family":"Meade","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":816793,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70226769,"text":"70226769 - 1963 - Hypervelocity impact of steel into Coconino Sandstone","interactions":[],"lastModifiedDate":"2021-12-10T15:42:17.031821","indexId":"70226769","displayToPublicDate":"1963-09-01T09:27:18","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":732,"text":"American Journal of Science","active":true,"publicationSubtype":{"id":10}},"title":"Hypervelocity impact of steel into Coconino Sandstone","docAbstract":"Impact of a 0.4019-g steel sphere at 4.27 km/sec into Coconino Sandstone [Permian] from Meteor Crater, Arizona, produced a crater 11-12 cm across and 2.45 cm deep. The ejecta consist of sandstone fragments, disaggregated sand, splinters of sand grains, strongly shocked aggregates of crushed sandstone grains, and chips, splinters, small amounts of silica glass, and minute spheres of steel. Part of the shocked steel was melted, and some of the melted and unmelted steel occurs as impregnations in the strongly shocked sandstone. Small amounts of glass, which were produced by shock from the sandstone, were found. The fusion of the steel cannot be due to compressive heating alone but can be partly accounted for by conduction of heat from the shocked sandstone and by production of heat by viscous drag and friction along the sandstone-projectile interface and along shear planes in the projectile.
An analogy with entropy production in steady-state systems leads to a statement that the geometry of natural waterways is governed by two opposing influences: a) equal work per unit of area of bed, and b) minimum work done in the system as a whole. The resulting calculations applied to shallow, estuaries are verified by field measurements.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666309493340","usgsCitation":"Langbein, W.B., 1963, The hydraulic geometry of a shallow estuary: International Association of Scientific Hydrology - Bulletin , v. 8, no. 3, p. 84-94, https://doi.org/10.1080/02626666309493340.","productDescription":"11 p.","startPage":"84","endPage":"94","costCenters":[],"links":[{"id":386123,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":816792,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221111,"text":"70221111 - 1963 - Preliminary results of a study of calcium carbonate saturation of ground water in central Florida","interactions":[],"lastModifiedDate":"2021-06-02T12:59:17.848563","indexId":"70221111","displayToPublicDate":"1963-09-01T07:55:41","publicationYear":"1963","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":"Preliminary results of a study of calcium carbonate saturation of ground water in central Florida","docAbstract":"The departure of ground water from equilibrium with calcite is being studied in central Florida. Measurements of pH, temperature, and concentration of bicarbonate made in the field are used with standard laboratory analyses of water samples to calculate an ion activity product (K) for calcium carbonate. The calculated Kiap is compared with the equilibrium constant (Keq) for calcite to determine the departure from equilibrium. The calcium concentration is lowest in the area of the highest piezometric surface. Some of the highest concentrations of bicarbonate are in the area of low calcium. In about half of the area of study, the water is undersaturated with respect to calcite. This indicates that solution of limestone can occur several hundred feet below the water table.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666309493336","usgsCitation":"Back, W., 1963, Preliminary results of a study of calcium carbonate saturation of ground water in central Florida: International Association of Scientific Hydrology - Bulletin , v. 8, no. 3, p. 43-51, https://doi.org/10.1080/02626666309493336.","productDescription":"9 p.","startPage":"43","endPage":"51","costCenters":[],"links":[{"id":480368,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666309493336","text":"Publisher Index Page"},{"id":386120,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"central Florida","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.265380859375,\n 27.21555620902969\n ],\n [\n -79.541015625,\n 27.21555620902969\n ],\n [\n -79.541015625,\n 29.516110386062277\n ],\n [\n -83.265380859375,\n 29.516110386062277\n ],\n [\n -83.265380859375,\n 27.21555620902969\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Back, William","contributorId":59007,"corporation":false,"usgs":true,"family":"Back","given":"William","email":"","affiliations":[],"preferred":false,"id":816789,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010629,"text":"70010629 - 1963 - Radiocarbon activity of shells from living clams and snails","interactions":[],"lastModifiedDate":"2026-02-19T16:23:18.908572","indexId":"70010629","displayToPublicDate":"1963-08-16T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Radiocarbon activity of shells from living clams and snails","docAbstract":"No abstract available.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.141.3581.637.a","issn":"00368075","usgsCitation":"Rubin, M., and Taylor, D., 1963, Radiocarbon activity of shells from living clams and snails: Science, v. 141, no. 3581, p. 637-637, https://doi.org/10.1126/science.141.3581.637.a.","productDescription":"1 p.","startPage":"637","endPage":"637","costCenters":[],"links":[{"id":219176,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"141","issue":"3581","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a93cfe4b0c8380cd8103b","contributors":{"authors":[{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":359296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, D.W.","contributorId":92323,"corporation":false,"usgs":true,"family":"Taylor","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":359297,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70213469,"text":"70213469 - 1963 - Elastic constants of calcite","interactions":[],"lastModifiedDate":"2020-09-18T20:25:27.36075","indexId":"70213469","displayToPublicDate":"1963-08-01T14:52:56","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2171,"text":"Journal of Applied Physics","active":true,"publicationSubtype":{"id":10}},"title":"Elastic constants of calcite","docAbstract":"No abstract available.
","language":"English","publisher":"American Institute of Physics","doi":"10.1063/1.1702777","usgsCitation":"Peselnick, L., and Robie, R.A., 1963, Elastic constants of calcite: Journal of Applied Physics, v. 34, p. 2494-2495, https://doi.org/10.1063/1.1702777.","productDescription":"2 p.","startPage":"2494","endPage":"2495","costCenters":[],"links":[{"id":378564,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Peselnick, L.","contributorId":66825,"corporation":false,"usgs":true,"family":"Peselnick","given":"L.","affiliations":[],"preferred":false,"id":799230,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robie, Richard A.","contributorId":92235,"corporation":false,"usgs":true,"family":"Robie","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":799231,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37747,"text":"37747 - 1963 - Birds protected by Federal law","interactions":[],"lastModifiedDate":"2014-07-24T13:44:05","indexId":"37747","displayToPublicDate":"1963-08-01T13:43:29","publicationYear":"1963","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":"455","title":"Birds protected by Federal law","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled by the Branch of Management and Enforcement.","usgsCitation":"U.S. Bureau of Sport Fisheries and Wildlife, 1963, Birds protected by Federal law (Supersedes WL 432, May 1961): Wildlife Leaflet 455, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290933,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Supersedes WL 432, May 1961","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcfdae4b0824b2d17612e","contributors":{"authors":[{"text":"U.S. Bureau of Sport Fisheries and Wildlife","contributorId":128149,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Sport Fisheries and Wildlife","id":529697,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221079,"text":"70221079 - 1963 - Correlations and problems in belt series stratigraphy, Northern idaho and western Montana","interactions":[],"lastModifiedDate":"2021-06-02T12:06:12.985609","indexId":"70221079","displayToPublicDate":"1963-08-01T13:08:36","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Correlations and problems in belt series stratigraphy, Northern idaho and western Montana","docAbstract":"A continuous strip of geologic maps has recently been completed along the Idaho-Montana state line between Clark Fork, Idaho, and Superior, Montana. New stratigraphic and petrographic information provides the basis for stratigraphic correlations and for the interpretation of facies changes in this part of the basin of deposition of the Precambrian Belt Series. Identification of facies changes is aided by the recognition of siltite (low-grade metamorphosed siltstone) as a valid rock type, in addition to quartzite and argillite, to classify most of these rocks and to establish mappable units. The older Belt rocks (Prichard through Wallace Formations) were deposited in a trough whose axis trended northwestward, perhaps approximately through Libby, Montana. Subtle facies changes suggest an ancient shore line southwest of the Coeur d'Alene district, Idaho, perhaps near the present exposed edge of the Idaho batholith. The younger Belt formations of the Missoula Group, however, thicken markedly southeastward toward Superior. Thus, the younger Belt rocks were deposited in a trough whose main axis was about at right angles to that of the older trough and perhaps was near Missoula, Montana. Deposition in the Clark Fork area was scant and often interrupted in Missoula time. The young major cross-warp in the old Belt geosyncline undoubtedly has contributed complexities to Belt correlation farther north. Detailed petrographic studies indicate that the Belt rocks from the Pend Oreille area, Idaho, are remarkably uniform in the mineralogic composition of similar rock types throughout 40,000 feet of strata. Further mineralogic studies are required to determine whether this uniformity is local or widespread.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1413:CAPIBS]2.0.CO;2","usgsCitation":"Harrison, J.E., and Campbell, A., 1963, Correlations and problems in belt series stratigraphy, Northern idaho and western Montana: Geological Society of America Bulletin, v. 74, no. 12, p. 1413-1427, https://doi.org/10.1130/0016-7606(1963)74[1413:CAPIBS]2.0.CO;2.","productDescription":"15 p.","startPage":"1413","endPage":"1427","costCenters":[],"links":[{"id":386109,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho, Montana","otherGeospatial":"northern Idaho, western Montana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.98242187499999,\n 46.40756396630067\n ],\n [\n -110.12695312499999,\n 46.40756396630067\n ],\n [\n -110.12695312499999,\n 49.009050809382046\n ],\n [\n -116.98242187499999,\n 49.009050809382046\n ],\n [\n -116.98242187499999,\n 46.40756396630067\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Harrison, J. E.","contributorId":54532,"corporation":false,"usgs":true,"family":"Harrison","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":816784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, A.B.","contributorId":22764,"corporation":false,"usgs":true,"family":"Campbell","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":816785,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}