{"pageNumber":"5736","pageRowStart":"143375","pageSize":"25","recordCount":184652,"records":[{"id":85353,"text":"85353 - 1979 - Approaches, field considerations and problems associated with radio tracking carnivores","interactions":[],"lastModifiedDate":"2012-02-02T00:03:59","indexId":"85353","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Approaches, field considerations and problems associated with radio tracking carnivores","docAbstract":"The adaptation of radio tracking to ecological studies was a major technological advance affecting field investigations of animal movements and behavior. Carnivores have been the recipients of much attention with this new technology and study approaches have varied from simple to complex. Equipment performance has much improved over the years, but users still face many difficulties. The beginning of all radio tracking studies should be a precise definition of objectives. Study objectives dictate type of gear required and field procedures. Field conditions affect equipment performance and investigator ability to gather data. Radio tracking carnivores is demanding and generally requires greater time than anticipated. Problems should be expected and planned for in study design. Radio tracking can be an asset in carnivore studies but caution is needed in its application.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"A handbook on biotelemetry and radio tracking","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Pergamon Press","publisherLocation":"Oxford and N.Y.","usgsCitation":"Sargeant, A., 1979, Approaches, field considerations and problems associated with radio tracking carnivores, chap. <i>of</i> A handbook on biotelemetry and radio tracking, p. 57-63 [804 pp.].","productDescription":"p. 57-63 [804 pp.]","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a61b6","contributors":{"editors":[{"text":"Amlaner, C. J. Jr.","contributorId":111363,"corporation":false,"usgs":true,"family":"Amlaner","given":"C. J.","suffix":"Jr.","affiliations":[],"preferred":false,"id":504434,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"MacDonald, D.W.","contributorId":112448,"corporation":false,"usgs":true,"family":"MacDonald","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":504435,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Sargeant, A.B.","contributorId":13171,"corporation":false,"usgs":true,"family":"Sargeant","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":295946,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190671,"text":"70190671 - 1979 - The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan","interactions":[{"subject":{"id":9104,"text":"ofr7793 - 1977 - The Yellow Dog peridotite and a possible buried igneous complex of Lower Keweenawan Age in the northern peninsula of Michigan","indexId":"ofr7793","publicationYear":"1977","noYear":false,"title":"The Yellow Dog peridotite and a possible buried igneous complex of Lower Keweenawan Age in the northern peninsula of Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":70190671,"text":"70190671 - 1979 - The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan","indexId":"70190671","publicationYear":"1979","noYear":false,"title":"The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan"},"id":1}],"lastModifiedDate":"2018-11-19T11:06:20","indexId":"70190671","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":282,"text":"Michigan Geological Survey Report of Investigation","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"24","title":"The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan","docAbstract":"<p>Partly serpentinized peridotite of early Keweenawan age crops out in two places along a 20-kilometer-long zone of positive aeromagnetic anomalies in northern Marquette County, Michigan. Most of the area is mantled by Pleistocene drift with few bedrock exposures.</p><p>Petrographic and electron microprobe studies show that the peridotite was originally a plagioclase lherzolite containing 40 to 50 percent<span>&nbsp;</span>olivine (Fo8<sub>0</sub>) and approximately 10 to 15 percent each of enstatite (En<sub>78</sub>Wo<sub>04</sub>Fs<sub>18</sub>) and diopsidic augite (En<sub>47</sub>Wo<sub>42</sub>Fs<sub>11</sub>). The plagioclase varies from 5 to 10 percent, and according to Morris (1977) is labradorite with a composition of An<sub>57-65</sub>. Major oxide minerals (4 to 6 percent) are ilmenite and magnetite. Sulfides comprise 1 to 2 percent of the peridotite and are chiefly pyrrhotite, pentlandite, and chalcopyrite.</p><p>Ground magnetic, gravity, and very low frequency electro-magnetic (VLF-EM)<span>&nbsp;</span>surveys have refined the location and magnitude of anomalies previously known only from aeromagnetic studies. These surveys together with soil geochemical studies suggest that peridotite, and possibly other mafic rocks forming a differentiated igneous complex, may occur throughout a belt 20 kilometers long (east-west) and 1 to 2 kilometers wide (north-south).</p><p>Differentiated igneous complexes in many parts of the world are hosts for copper, nickel, chromium, or precious-metal deposits. The peridotite in the area of this study is anomalously rich in copper and sulfur compared to world-wide averages for peridotite. Positive electro-magnetic anomalies found near the peridotite outcrops may be caused by sulfide-rich zones in the igneous rocks and should be explored further for copper-nickel&nbsp;mineralization.</p>","language":"English","publisher":"State of Michigan Department of Natural Resources","publisherLocation":"Lansing, MI","usgsCitation":"Klasner, J.S., Snider, D.W., Cannon, W., and Slack, J.F., 1979, The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan: Michigan Geological Survey Report of Investigation 24, v, 31 p.","productDescription":"v, 31 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":345637,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345636,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.michigan.gov/documents/deq/RI_24opt_309211_7.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59b8f222e4b08b1644e0af0f","contributors":{"authors":[{"text":"Klasner, John S.","contributorId":46591,"corporation":false,"usgs":true,"family":"Klasner","given":"John","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":710088,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snider, David W.","contributorId":196332,"corporation":false,"usgs":true,"family":"Snider","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":710089,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cannon, W.F. 0000-0002-2699-8118","orcid":"https://orcid.org/0000-0002-2699-8118","contributorId":70382,"corporation":false,"usgs":true,"family":"Cannon","given":"W.F.","affiliations":[],"preferred":false,"id":710090,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Slack, John F. 0000-0001-6600-3130 jfslack@usgs.gov","orcid":"https://orcid.org/0000-0001-6600-3130","contributorId":1032,"corporation":false,"usgs":true,"family":"Slack","given":"John","email":"jfslack@usgs.gov","middleInitial":"F.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":true,"id":710091,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70169247,"text":"70169247 - 1979 - Electrical measurements as stress-strain monitors","interactions":[],"lastModifiedDate":"2016-04-05T15:00:27","indexId":"70169247","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Electrical measurements as stress-strain monitors","docAbstract":"<p>Many of the measurements of phyiscal properties being made in earthquake prediction studies are based on the premise that these properties are influenced by stresses and strains, especially so near the failure point. Electrical properties of rocks are controlled by the fluid in the pores and cracks in the rocks. Because these regions are most influenced by stresses, one should expect electrical measurements to be sensitive measures of changing stresses and strains. Nevertheless, the strain changes we are dealing with are very small, and, consequently, we need very sensitive instruments to detect them. &nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Madden, T.R., 1979, Electrical measurements as stress-strain monitors: Earthquake Information Bulletin (USGS), v. 11, no. 1, p. 4-8.","productDescription":"5 p.","startPage":"4","endPage":"8","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319270,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56f3be41e4b0f59b85e02e78","contributors":{"authors":[{"text":"Madden, T. R.","contributorId":167750,"corporation":false,"usgs":false,"family":"Madden","given":"T.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":623388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":94048,"text":"94048 - 1979 - Procedures for the detection and identification of certain fish pathogens: Revised edition","interactions":[],"lastModifiedDate":"2012-02-02T00:03:55","indexId":"94048","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Procedures for the detection and identification of certain fish pathogens: Revised edition","docAbstract":"No abstract available at this time","language":"English","publisher":"American Fisheries Society, Fish Health Section","publisherLocation":"Bethesda, MD","collaboration":"None/NFC","usgsCitation":"McDaniel, D., 1979, Procedures for the detection and identification of certain fish pathogens: Revised edition.","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":127504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66090c","contributors":{"authors":[{"text":"McDaniel, D.W.","contributorId":34072,"corporation":false,"usgs":true,"family":"McDaniel","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":298375,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70162275,"text":"70162275 - 1979 - Potentials and limits for the use of ozone as a fish disease control agent","interactions":[],"lastModifiedDate":"2016-01-19T16:39:14","indexId":"70162275","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2976,"text":"Ozone: Science and Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Potentials and limits for the use of ozone as a fish disease control agent","docAbstract":"<p><span>Ozone and chlorine inactivation curves were determined in three types of freshwater at 20 C for the destruction of the fish pathogens&nbsp;</span><i>Aeromonas salmonicida</i><span>&nbsp;the etiologic agent of furunculosis, and&nbsp;</span><i>Yersinia ruckeri</i><span>&nbsp;the enteric redmouth bacterium (ERM). Ozone and chlorine inactivation curves were also obtained in the same water types at 10 C for the fish pathogenic viruses infectious hematopoietic necrosis (IHNV), and infectious pancreatic necrosis (IPNV). Acute toxicity tests using the rainbow trout as a representative salmonid revealed that ozone was highly toxic at the dose levels used. Partial chronic (3. mo.) testing revealed that ozone exposure at 2 &mu;g/L causes only minimal physiological changes, none of which would be expected to compromise biological function.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/01919512.1979.10684566","usgsCitation":"Wedemeyer, G.A., Nelson, N.C., and Yasutake, T., 1979, Potentials and limits for the use of ozone as a fish disease control agent: Ozone: Science and Engineering, v. 1, no. 4, p. 295-318, https://doi.org/10.1080/01919512.1979.10684566.","productDescription":"24 p.","startPage":"295","endPage":"318","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":314506,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"569f6c49e4b0961cf27fd1bf","contributors":{"authors":[{"text":"Wedemeyer, Gary A.","contributorId":30668,"corporation":false,"usgs":true,"family":"Wedemeyer","given":"Gary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":589076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, Nancy C.","contributorId":152336,"corporation":false,"usgs":false,"family":"Nelson","given":"Nancy","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":589077,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yasutake, T.","contributorId":152372,"corporation":false,"usgs":false,"family":"Yasutake","given":"T.","email":"","affiliations":[],"preferred":false,"id":589078,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011709,"text":"70011709 - 1979 - Modification of a commercial micrometer hanging mercury drop electrode","interactions":[],"lastModifiedDate":"2023-03-10T17:44:20.298047","indexId":"70011709","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Modification of a commercial micrometer hanging mercury drop electrode","docAbstract":"<p>U.S. Geological Survey</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac50050a033","usgsCitation":"Bonelli, J.E., Taylor, H.E., and Skogerboe, R.K., 1979, Modification of a commercial micrometer hanging mercury drop electrode: Analytical Chemistry, v. 51, no. 14, p. 2412-2413, https://doi.org/10.1021/ac50050a033.","productDescription":"2 p.","startPage":"2412","endPage":"2413","numberOfPages":"2","costCenters":[],"links":[{"id":221385,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"51","issue":"14","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a5cafe4b0c8380cd6fe8d","contributors":{"authors":[{"text":"Bonelli, J. E.","contributorId":35064,"corporation":false,"usgs":true,"family":"Bonelli","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":361779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Taylor, H. E.","contributorId":208305,"corporation":false,"usgs":false,"family":"Taylor","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":866162,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Skogerboe, R. K","contributorId":189803,"corporation":false,"usgs":false,"family":"Skogerboe","given":"R.","email":"","middleInitial":"K","affiliations":[],"preferred":false,"id":866163,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185410,"text":"70185410 - 1979 - Nesting ecology of Arctic loons","interactions":[],"lastModifiedDate":"2018-07-15T11:03:19","indexId":"70185410","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Nesting ecology of Arctic loons","docAbstract":"<p><span>Arctic Loons were studied on the Yukon-Kuskokwim Delta, Alaska, from the time of their arrival in May to their departure in September, in 1974 and 1975. Pairs arrived on breeding ponds as soon as sufficient meltwater was available to allow their take-off and landing. Loons apparently do not initiate nests immediately after their arrival, even when nest-sites are available. Delayed egg-laying may be dependent on a period of yolk formation. Delaying yolk formation until after arrival on nest ponds is an adaptation by loons to the variable time suitable habitat becomes available for nesting. Predation of eggs by Glaucous Gulls, Long-tailed and Parasitic jaegers and foxes varied in relation to the location of the nest-site, and the availability of alternate prey. Hatching success was the lowest recorded for Arctic Loons (5%) in 1974, when eggs of both loons and Cackling Geese were taken in large numbers by predators. Hatching success increased to 32% in 1975 when an abundance of tundra voles was observed. No loon eggs hatched after the hatching of the Cackling Goose eggs when this alternate prey was no longer available. Nests destroyed by foxes were predominantly along shorelines, and those by gulls and jaegers were predominantly on islands. Nest-site selection by Arctic Loons may reflect an adaptive response to varying selective pressures by their predators.</span></p>","language":"English","publisher":"Wilson Ornithological Society","usgsCitation":"Petersen, M.R., 1979, Nesting ecology of Arctic loons: The Wilson Bulletin, v. 91, no. 4, p. 608-617.","productDescription":"10 p.","startPage":"608","endPage":"617","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337985,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":337984,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://wjoonline.org/?code=wors-site","text":"Journal's Homepage"}],"country":"United States","state":"Alaska","otherGeospatial":"Clarence Rhode National Wildlife Range, Yukon-Kuskokwim Delta","volume":"91","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d23b9be4b0236b68f829b7","contributors":{"authors":[{"text":"Petersen, Margaret R. 0000-0001-6082-3189 mrpetersen@usgs.gov","orcid":"https://orcid.org/0000-0001-6082-3189","contributorId":167729,"corporation":false,"usgs":true,"family":"Petersen","given":"Margaret","email":"mrpetersen@usgs.gov","middleInitial":"R.","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":685497,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012618,"text":"70012618 - 1979 - Barometric fluctuations in wells tapping deep unconfined aquifers","interactions":[],"lastModifiedDate":"2018-02-05T12:29:43","indexId":"70012618","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Barometric fluctuations in wells tapping deep unconfined aquifers","docAbstract":"<p><span>Water levels in wells screened only below the water table in unconfined aquifers fluctuate in response to atmospheric pressure changes. These fluctuations occur because the materials composing the unsaturated zone resist air movement and have capacity to store air with a change in pressure. Consequently, the translation of any pressure change at land surface is slowed as it moves through the unsaturated zone to the water table, but it reaches the water surface in the well instantaneously. Thus a pressure imbalance is created that results in a water level fluctuation. Barometric effects on water levels in unconfined aquifers can be computed by solution of the differential equation governing the flow of gas in the unsaturated zone subject to the appropriate boundary conditions. Solutions to this equation for two sets of boundary conditions were applied to compute water level response in a well tapping the Ogallala Formation near Lubbock, Texas from simultaneous microbarograph records. One set of computations, based on the step function unit response solution and convolution, resulted in a very good match between computed and measured water levels. A second set of computations, based on analysis of the amplitude ratios of simultaneous cyclic microbarograph and water level fluctuations, gave inconsistent results in terms of the unsaturated zone pneumatic properties but provided useful insights on the nature of unconfined-aquifer water level fluctuations.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/WR015i005p01167","usgsCitation":"Weeks, E.P., 1979, Barometric fluctuations in wells tapping deep unconfined aquifers: Water Resources Research, v. 15, no. 5, p. 1167-1176, https://doi.org/10.1029/WR015i005p01167.","productDescription":"10 p.","startPage":"1167","endPage":"1176","costCenters":[],"links":[{"id":222487,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","city":"Lubbock","otherGeospatial":"Ogallala Formation","volume":"15","issue":"5","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5059efbce4b0c8380cd4a40f","contributors":{"authors":[{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":364077,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70181771,"text":"70181771 - 1979 - Resistance of different stocks and transferrin genotypes of coho salmon, Oncorhynchus kisutch, and steelhead trout, Salmo gairdneri, to bacterial kidney disease and vibriosis","interactions":[],"lastModifiedDate":"2018-02-27T17:58:55","indexId":"70181771","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Resistance of different stocks and transferrin genotypes of coho salmon, Oncorhynchus kisutch, and steelhead trout, Salmo gairdneri, to bacterial kidney disease and vibriosis","docAbstract":"<p>Juvenile coho salmon and steelhead trout ofdifferentstocks and three transferrin genotypes(AA, AC, and CCl, all reared in identical or similar environments, were experimentally infected with Corynebacterium sp., the causative agent ofbacterial kidney disease, or with Vibrio anguillarum, the causative agent of vibriosis. Mortality due to the pathogens was compared among stocks within a species and among transferrin genotypes within a stock to determine whetherthere was a geneticbasis for resistance to disease. Differences in resistance to bacterial kidney disease among coho salmon stocks had a genetic basis. Stock susceptibility to vibriosis was strongly influenced by environmental factors. Coho salmon orsteelhead trout of one stock may be resistant to one disease but susceptible to another. The importance of transferrin genotype of coho salmon in resistance to bacterial kidney disease was stock specific; in stocks that showed differential resistance of genotypes, the AA was the most susceptible. No differencesin resistance to vibriosis were observed among transferrin genotypes.</p>","language":"English","publisher":"National Oceanic and Atmospheric Adminstration","usgsCitation":"Winter, G.W., Schreck, C.B., and McIntyre, J.D., 1979, Resistance of different stocks and transferrin genotypes of coho salmon, Oncorhynchus kisutch, and steelhead trout, Salmo gairdneri, to bacterial kidney disease and vibriosis: Fishery Bulletin, v. 77, no. 4, p. 795-802.","productDescription":"8 p. ","startPage":"795","endPage":"802","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335281,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://fishbull.noaa.gov/77-4/winter.pdf"},{"id":335282,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"77","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a2d3c3e4b0c82512869a3a","contributors":{"authors":[{"text":"Winter, Gary W.","contributorId":181513,"corporation":false,"usgs":false,"family":"Winter","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":668453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schreck, Carl B. 0000-0001-8347-1139 carl.schreck@usgs.gov","orcid":"https://orcid.org/0000-0001-8347-1139","contributorId":878,"corporation":false,"usgs":true,"family":"Schreck","given":"Carl","email":"carl.schreck@usgs.gov","middleInitial":"B.","affiliations":[{"id":289,"text":"Forest and Rangeland Ecosys Science Center","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":true,"id":668454,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McIntyre, John D.","contributorId":152343,"corporation":false,"usgs":false,"family":"McIntyre","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":668455,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70181034,"text":"70181034 - 1979 - Status and distribution of the California Clapper Rail (<i>Rallus longirostris obsoletus</i>)","interactions":[],"lastModifiedDate":"2018-05-20T11:36:26","indexId":"70181034","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1153,"text":"California Fish and Game","active":true,"publicationSubtype":{"id":10}},"title":"Status and distribution of the California Clapper Rail (<i>Rallus longirostris obsoletus</i>)","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"California Department of Fish and Wildlife","usgsCitation":"Gill, R., 1979, Status and distribution of the California Clapper Rail (<i>Rallus longirostris obsoletus</i>): California Fish and Game, v. 65, no. 1, p. 36-49.","startPage":"36","endPage":"49","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"links":[{"id":335161,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":335160,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.wildlife.ca.gov/Publications/Journal/Contents#1979","text":"Volume 65 on Publisher's Website"}],"volume":"65","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a030a3e4b099f50d3e04fe","contributors":{"authors":[{"text":"Gill, Robert E. Jr. 0000-0002-6385-4500 rgill@usgs.gov","orcid":"https://orcid.org/0000-0002-6385-4500","contributorId":171747,"corporation":false,"usgs":true,"family":"Gill","given":"Robert E.","suffix":"Jr.","email":"rgill@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":663390,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70181764,"text":"70181764 - 1979 - Histochemistry of leucine aminoaphthylamidase (LAN) in rainbow trout (Salmo gairdneri)","interactions":[],"lastModifiedDate":"2021-03-16T19:09:36.304717","indexId":"70181764","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"Histochemistry of leucine aminoaphthylamidase (LAN) in rainbow trout (Salmo gairdneri)","docAbstract":"<p><span>The histochemistry of leucine aminonaphthylamidase (LAN) was studied in frozen tissue sections of rainbow trout both in yearling and adult fish. Age of fish had relatively little effect upon the results. The most intense LAN color production was in epithelial cells of midgut, pyloric ceca, hindgut, and in some segments of kidney tubules. Lower levels of LAN were evident in liver cells of Kupffer, and still lower or slight levels of LAN activity were found in blood cells, muscle, nerve, connective tissue, gonad, and pancreas. The results indicate that LAN might be useful in assessing histotoxicity to LAN‐rich areas of the body.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1979)108<57:HOLALI>2.0.CO;2","usgsCitation":"Bouck, G.R., 1979, Histochemistry of leucine aminoaphthylamidase (LAN) in rainbow trout (Salmo gairdneri): Transactions of the American Fisheries Society, v. 108, no. 1, p. 57-62, https://doi.org/10.1577/1548-8659(1979)108<57:HOLALI>2.0.CO;2.","productDescription":"6 p.","startPage":"57","endPage":"62","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335267,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"108","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a2d3c4e4b0c82512869a42","contributors":{"authors":[{"text":"Bouck, Gerald R.","contributorId":152420,"corporation":false,"usgs":false,"family":"Bouck","given":"Gerald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":668440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70181766,"text":"70181766 - 1979 - An erythroleukemic-like disease in fish","interactions":[],"lastModifiedDate":"2017-02-13T14:56:15","indexId":"70181766","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"An erythroleukemic-like disease in fish","docAbstract":"<p>No abstract available&nbsp;</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 9th international symposium on comparative Leukemia and related diseases","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":" 9th international symposium on comparative Leukemia and related diseases","language":"English","publisher":"Elsevier-North-Holland","publisherLocation":"New York, NY","usgsCitation":"MacMillan, J., Landolt, M., and Mulcahy, D., 1979, An erythroleukemic-like disease in fish, <i>in</i> Proceedings of the 9th international symposium on comparative Leukemia and related diseases, p. 219-219.","productDescription":"1 p.","startPage":"219","endPage":"219","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335273,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a2d3c3e4b0c82512869a3e","contributors":{"authors":[{"text":"MacMillan, J.R.","contributorId":181511,"corporation":false,"usgs":false,"family":"MacMillan","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":668444,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Landolt, M.","contributorId":90239,"corporation":false,"usgs":true,"family":"Landolt","given":"M.","email":"","affiliations":[],"preferred":false,"id":668445,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mulcahy, D.","contributorId":82642,"corporation":false,"usgs":true,"family":"Mulcahy","given":"D.","email":"","affiliations":[],"preferred":false,"id":668446,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40429,"text":"ofr791399 - 1979 - Coal resource occurrence and coal development potential maps of the SW quarter of the Citadel Plateau 15-minute quadrangle, Moffat County, Colorado","interactions":[],"lastModifiedDate":"2023-08-24T20:44:25.653021","indexId":"ofr791399","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","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":"79-1399","title":"Coal resource occurrence and coal development potential maps of the SW quarter of the Citadel Plateau 15-minute quadrangle, Moffat County, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791399","usgsCitation":"Dames & Moore, 1979, Coal resource occurrence and coal development potential maps of the SW quarter of the Citadel Plateau 15-minute quadrangle, Moffat County, Colorado: U.S. Geological Survey Open-File Report 79-1399, Report: iii, 19 p.; 29.57 x 23.38 inches or smaller, https://doi.org/10.3133/ofr791399.","productDescription":"Report: iii, 19 p.; 29.57 x 23.38 inches or smaller","costCenters":[],"links":[{"id":420137,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75104.htm","linkFileType":{"id":5,"text":"html"}},{"id":74579,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1399/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74578,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1399/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74577,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1399/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74576,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1399/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74575,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1399/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74581,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1399/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74580,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1399/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74573,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1399/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74574,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1979/1399/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":74582,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1399/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172181,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1399/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"SW quarter of the Citadel Plateau 15-minute quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.25,\n              40.375\n            ],\n            [\n              -108.25,\n              40.25\n            ],\n            [\n              -108.125,\n              40.25\n            ],\n            [\n              -108.125,\n              40.375\n            ],\n            [\n              -108.25,\n              40.375\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6b000e","contributors":{"authors":[{"text":"Dames & Moore","contributorId":127975,"corporation":true,"usgs":false,"organization":"Dames & Moore","id":530217,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012411,"text":"70012411 - 1979 - Surface faults in the gulf coastal plain between Victoria and Beaumont, Texas","interactions":[],"lastModifiedDate":"2017-06-14T15:14:48","indexId":"70012411","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Surface faults in the gulf coastal plain between Victoria and Beaumont, Texas","docAbstract":"<p>Displacement of the land surface by faulting is widespread in the Houston-Galveston region, an area which has undergone moderate to severe land subsidence associated with fluid withdrawal (principally water, and to a lesser extent, oil and gas). A causative link between subsidence and fluid extraction has been convincingly reported in the published literature. However, the degree to which fluid withdrawal affects fault movement in the Texas Gulf Coast, and the mechanism(s) by which this occurs are as yet unclear. </p><p>Faults that offset the ground surface are not confined to the large (&gt;6000-km<sup>2</sup>) subsidence “bowl” centered on Houston, but rather are common and characteristic features of Gulf Coast geology. Current observations and conclusions concerning surface faults mapped in a 35,000-km<sup>2</sup> area between Victoria and Beaumont, Texas (which area includes the Houston subsidence bowl) may be summarized as follows:</p><p> (1) Hundreds of faults cutting the Pleistocene&nbsp;and Holocene sediments exposed in the coastal plain have been mapped. Many faults lie well outside the Houston-Galveston region; of these, more than 10% are active, as shown by such features as displaced, fractured, and patched road surfaces, structural failure of buildings astride faults, and deformed railroad tracks.&nbsp;</p><p>(2) Complex patterns of surface faults are common above salt domes. Both radial patterns (for example, in High Island, Blue Ridge, Clam Lake, and Clinton domes) and crestal grabens (for example, in the South Houston and Friendswood-Webster domes) have been recognized. Elongate grabens connecting several known and suspected salt domes, such as the fault zone connecting Mykawa, Friendswood-Webster, and Clear Lake domes, suggest fault development above rising salt ridges. </p><p>(3) Surface faults associated with salt domes tend to be short (&lt;5 km in length), numerous, curved in map view, and of diverse trend. Intersecting faults are common. In contrast, surface faults in areas unaffected by salt diapirism are frequently mappable for appreciable distances (&gt;10 km), occur  singly or in simple grabens, have gently sinuous traces, and tend to lie roughly parallel to the ENE-NE “coastwise” trend common to regional growth faults identified in subsurface Tertiary sediments.&nbsp;</p><p>(4) Evidence to support the thesis that surface scarps are the shallow expression of faults extending downward into the Tertiary section is mostly indirect, but nonetheless reasonably convincing. Certainly the patterns of crestal grabens and radiating faults mapped on the surface above salt domes are more than happenstance; analogous fault patterns have been documented around these structures at depth. Similarly, some of the long surface faults not associated with salt domes seem to have subsurface counterparts among known regional growth faults documented through well logs and seismic data. Correlations between surface scarps and faults offsetting subsurface data are not conclusive because of the large vertical distances (1900- 3800 m) involved in making the most of the inferred connections. Nevertheless, the large number of successful correlations - in trend, movement sense, and position - suggests that many surface scarps represent merely the most recent displacements on faults formed during the Tertiary. </p><p>(5) Upstream-facing fault scarps in this region of low relief can be significant impediments to streams. Locally, both abandoned, mud-filled Pleistocene distributary channels and, more commonly, Holocene drainage lines still occupied by perennial streams reflect the influence of faulting on their development. Some bend sharply near faults and have tended to flow along or pond against the base of scarps; others meander within topographically expressed grabens. Such evidence for Quaternary displacement of the ground surface is widespread in the Texas Gulf coast. In the general, however, streams in areas now offset by faulting show no disruption of their courses where they cross fault scarps. Such scarps are probably very young, and where they can be demonstrated to partly or wholly predate fluid withdrawal, very recent natural fault activity is indicated.&nbsp;<br></p><p>(6) Early aerial photographs (1930) of the entire region and topographic maps (1915-16 surveys) of Harris County (Houston and vicinity) show that many faults had already displaced the land surface at a time when appreciable pressure declines in subjacent strata were localized to relatively few areas of large-scale pumping. Prehistoric faulting of the land surface, as noted above, appears to have affected much of the Texas Gulf Coast. </p><p>(7) A relation between groundwater extraction and current motion on active faults is suspected because of the increased incidence of ground failure in the Houston-Galveston subsidence bowl. This argument is weakened somewhat by recognition of numerous surface faults, some of them active today, far beyond the periphery of the strongly subsiding area. Moreover, tilt beam records from two monitored faults in northwest Houston and accounts of fault damage from local residents demonstrate a complex, episodic nature of fault creep which can only partially be correlated with groundwater production. Nevertheless, although specific mechanisms are in doubt, the extraction of groundwater from shallow (&lt;800-m) sands is probably a major factor in contributing to current displacement of the ground surface in the Houston-Galveston region. Within this large area, the number of faults recognizable from aerial photographs has increased at least tenfold between 1930 and 1970. Elsewhere in the Texas Gulf Coast only a moderate increase has been noted, some of which is possibly attributable to oil and gas production. Surface fault density in the Houston-Galveston region is far greater than in any other area of the Texas Gulf Coast investigated to date. A plausible explanation for these differences is that large overdrafts of groundwater over an extended period of time in the Houston-Galveston region have stimulated fault activity there. Throughout the Texas Gulf Coast, however, a natural contribution to fault motion remains a distinct possibility. </p>","language":"English","publisher":"Elsevier ","doi":"10.1016/0040-1951(79)90248-8","issn":"00401951","usgsCitation":"Verbeek, E.R., 1979, Surface faults in the gulf coastal plain between Victoria and Beaumont, Texas: Tectonophysics, v. 52, no. 1-4, p. 373-375, https://doi.org/10.1016/0040-1951(79)90248-8.","productDescription":"3 p.","startPage":"373","endPage":"375","costCenters":[],"links":[{"id":221821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.30639648437499,\n              32.045332838858506\n            ],\n            [\n              -98.646240234375,\n              30.90222470517144\n            ],\n            [\n              -96.56982421875,\n              28.168875180063345\n            ],\n            [\n              -93.61450195312499,\n              29.6880527498568\n            ],\n            [\n              -95.30639648437499,\n              32.045332838858506\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"52","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9face4b08c986b31e785","contributors":{"authors":[{"text":"Verbeek, Earl R.","contributorId":64222,"corporation":false,"usgs":true,"family":"Verbeek","given":"Earl","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363474,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185089,"text":"70185089 - 1979 - A preliminary assessment of the timing and migration of shorebirds along the northcentral Alaska Peninsula","interactions":[],"lastModifiedDate":"2018-05-20T11:36:15","indexId":"70185089","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesTitle":{"id":5103,"text":"Studies in Avian Biology","printIssn":"0197-9922","active":true,"publicationSubtype":{"id":24}},"title":"A preliminary assessment of the timing and migration of shorebirds along the northcentral Alaska Peninsula","docAbstract":"<p><span>An intensive study of post-breeding and migrating shorebirds was conducted in 1976 on a major estuary of the Alaska Peninsula at Nelson Lagoon. Twenty species were recorded, eight of them breeding on the study area. Temporal patterns of relative abundance were obtained from aerial and ground censuses. Prominent events in the seasonal southward movements were (a) congregation of non- and post-breeding birds after mid-June, (b) an early migratory peak before early August dominated by Western Sandpipers, Short-billed Dowitchers, Least Sandpipers, and Whimbrels, and (c) a later, much larger peak in late Setember and early October dominated by Dunlins, Rock Sandpipers, Bar-tailed Godwits, and Long-billed Dowitchers. In the five-month period July- November, several hundred thousand shorebirds used the study area as a stopover and/or staging area. The most abundant species was the Dunlin. The area is also critical for such species as the Bar-tailed Godwit, apparently serving as a unique concentration site for this species prior to fall migration.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Shorebirds in Marine Environments (Studies in Avian Biology no. 2)","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Cooper Ornithological Society","usgsCitation":"Gill, R., and Jorgensen, P.D., 1979, A preliminary assessment of the timing and migration of shorebirds along the northcentral Alaska Peninsula, chap. <i>of</i> Shorebirds in Marine Environments (Studies in Avian Biology no. 2): Studies in Avian Biology, v. 2, p. 113-123.","productDescription":"9 p.","startPage":"113","endPage":"123","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337543,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":337542,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.americanornithology.org/content/studies-avian-biology","text":"<I>Studies in Avian Biology</i> Homepage"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Peninsula, Nelson Lagoon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -161.69952392578125,\n              55.658996099428364\n            ],\n            [\n              -160.0762939453125,\n              55.658996099428364\n            ],\n            [\n              -160.0762939453125,\n              56.160847254089816\n            ],\n            [\n              -161.69952392578125,\n              56.160847254089816\n            ],\n            [\n              -161.69952392578125,\n              55.658996099428364\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c90130e4b0849ce97abd73","contributors":{"editors":[{"text":"Pitelka, Frank A.","contributorId":58508,"corporation":false,"usgs":true,"family":"Pitelka","given":"Frank","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":684307,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Gill, Robert E. Jr. 0000-0002-6385-4500 rgill@usgs.gov","orcid":"https://orcid.org/0000-0002-6385-4500","contributorId":171747,"corporation":false,"usgs":true,"family":"Gill","given":"Robert E.","suffix":"Jr.","email":"rgill@usgs.gov","affiliations":[{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true}],"preferred":true,"id":684312,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jorgensen, Paul D.","contributorId":43871,"corporation":false,"usgs":false,"family":"Jorgensen","given":"Paul","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":684313,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012457,"text":"70012457 - 1979 - A large submarine sand-rubble flow on kilauea volcano, hawaii","interactions":[],"lastModifiedDate":"2012-03-12T17:19:02","indexId":"70012457","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"A large submarine sand-rubble flow on kilauea volcano, hawaii","docAbstract":"Papa'u seamount on the south submarine slope of Kilauea volcano is a large landslide about 19 km long, 6 km wide, and up to 1 km thick with a volume of about 39 km3. Dredge hauls, remote camera photographs, and submersible observations indicate that it is composed primarily of unconsolidated angular glassy basalt sand with scattered basalt blocks up to 1 m in size; no lava flows were seen. Sulfur contents of basalt glass from several places on the sand-rubble flow and nearby areas are low (< 240 ppm), indicating that the clastic basaltic material was all erupted on land. The Papa'u sandrubble flow was emplaced during a single flow event fed from a large near-shore bank of clastic basaltic material which in turn was formed as lava flows from the summit area of Kilauea volcano disintegrated when they entered the sea. The current eruptive output of the volcano suggests that the material in the submarine sand-rubble flow represents about 6000 years of accumulation, and that the flow event occurred several thousand years ago. ?? 1979.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Fornari, D., Moore, J., and Calk, L., 1979, A large submarine sand-rubble flow on kilauea volcano, hawaii: Journal of Volcanology and Geothermal Research, v. 5, no. 3-4, p. 239-256.","startPage":"239","endPage":"256","numberOfPages":"18","costCenters":[],"links":[{"id":222594,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e432e4b0c8380cd464bb","contributors":{"authors":[{"text":"Fornari, D.J.","contributorId":49520,"corporation":false,"usgs":true,"family":"Fornari","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":363620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":363621,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Calk, L.","contributorId":106264,"corporation":false,"usgs":true,"family":"Calk","given":"L.","affiliations":[],"preferred":false,"id":363622,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012439,"text":"70012439 - 1979 - Solubility of some alkali and alkaline earth chlorides in water at moderate temperatures","interactions":[],"lastModifiedDate":"2025-01-07T16:47:47.170023","indexId":"70012439","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2209,"text":"Journal of Chemical and Engineering Data","active":true,"publicationSubtype":{"id":10}},"title":"Solubility of some alkali and alkaline earth chlorides in water at moderate temperatures","docAbstract":"Solubilities for the binary systems, salt-H2O, of the chlorides of lithium, rubidium, cesium, magnesium, calcium, strontium, and barium from near 0??C to the saturated boiling point are reported. The experimental data and coefficients of an equation for a smoothed curve describing each system are listed in the tables. The data are improvements on those previously reported in the literature, having a precision on the average of ??0.09%.","language":"English","publisher":"ACS Publications","doi":"10.1021/je60083a019","issn":"00219568","usgsCitation":"Clynne, M., and Potter, R., 1979, Solubility of some alkali and alkaline earth chlorides in water at moderate temperatures: Journal of Chemical and Engineering Data, v. 24, no. 4, p. 338-340, https://doi.org/10.1021/je60083a019.","productDescription":"3 p.","startPage":"338","endPage":"340","numberOfPages":"3","costCenters":[],"links":[{"id":222306,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505b9247e4b08c986b319de5","contributors":{"authors":[{"text":"Clynne, M.A.","contributorId":90722,"corporation":false,"usgs":true,"family":"Clynne","given":"M.A.","affiliations":[],"preferred":false,"id":363586,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Potter, R.W. II","contributorId":16857,"corporation":false,"usgs":true,"family":"Potter","given":"R.W.","suffix":"II","email":"","affiliations":[],"preferred":false,"id":363585,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012533,"text":"70012533 - 1979 - Arsenic and fluoride in the upper madison river system: Firehole and gibbon rivers and their tributaries, yellowstone national park, wyoming, and southeast montana","interactions":[],"lastModifiedDate":"2012-03-12T17:19:10","indexId":"70012533","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"Arsenic and fluoride in the upper madison river system: Firehole and gibbon rivers and their tributaries, yellowstone national park, wyoming, and southeast montana","docAbstract":"Chemical analyses of 21 water samples from the Firehole and Gibbon Rivers, which combine to form the Madison River, gave arsenic and fluoride values above the Environmental Protection Agency Interim Primary Drinking Water maximum contaminant levels (0.05 mg/l arsenic and 2.0 mg/l fluoride). On 18 October, 1975, during a period of moderate flow (16,600 l/s), the Madison River at West Yellowstone contained 0.23 mg/l arsenic and 6.2 mg/l fluoride. Below Hebgen Lake the Madison River during periods of high flow (56,000 liter/s at West Yellowstone and 708,000 liter/s below Hebgen Lake) would contain 0.05 mg/l arsenic at both stations and 1.5 and 4.0 mg/l fluoride at West Yellowstone and below Hebgen Lake, respectively. The strong correlations of arsenic and fluoride with other chemical constituents of the river water at the sampling sites demonstrate the conservative nature of each element after it reaches the Madison River system. Calculations indicate that water from three sampling sites is above saturation with respect to fluorite. ?? 1979 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF02423274","issn":"09430105","usgsCitation":"Thompson, J., 1979, Arsenic and fluoride in the upper madison river system: Firehole and gibbon rivers and their tributaries, yellowstone national park, wyoming, and southeast montana: Environmental Geology, v. 3, no. 1, p. 13-21, https://doi.org/10.1007/BF02423274.","startPage":"13","endPage":"21","numberOfPages":"9","costCenters":[],"links":[{"id":221831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205147,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02423274"}],"volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ed87e4b0c8380cd49870","contributors":{"authors":[{"text":"Thompson, J. M.","contributorId":77142,"corporation":false,"usgs":true,"family":"Thompson","given":"J. M.","affiliations":[],"preferred":false,"id":363838,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012534,"text":"70012534 - 1979 - Beach-cusp formation","interactions":[],"lastModifiedDate":"2014-10-16T15:05:27","indexId":"70012534","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Beach-cusp formation","docAbstract":"<p>Field experiments on beach-cusp formation were undertaken to document how the cuspate form develops and to test the edge-wave hypothesis on the uniform spacing of cusps. These involved observations of cusps forming from an initially plane foreshore.</p>\n<br/>\n<p>The cuspate form was observed to be a product of swash modification of an intertidal beach ridge as follows. A ridge, cut by a series of channels quasi-equally spaced along its length, was deposited onto the lower foreshore. The ridge migrated shoreward with flood tide, while the longshore positions of the channels remained fixed. On ebb tide, changes in swash circulation over the ridge allowed the upwash to flow shoreward through the channels and the channel mouths were eroded progressively wider until adjacent mouths met, effecting a cuspate shape.</p>\n<br/>\n<p>Measured spacings of cusps, ranging in size from less than 1 m to more than 12 m, agree well with computed spacings due to either zero-mode subharmonic or zero-mode synchronous edge waves. Edge-wave-induced longshore variations in run up will cause water ponded behind a ridge to converge at points of low swash and flow seaward as relatively narrow currents eroding channels spaced at one edge-wave wavelength for synchronous edge waves or one half wavelength for subharmonic edge waves. The channels are subsequently modified into cusp troughs as described above.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Marine Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(79)90100-2","issn":"00253227","usgsCitation":"Sallenger, A.H., 1979, Beach-cusp formation: Marine Geology, v. 29, no. 1-4, p. 23-37, https://doi.org/10.1016/0025-3227(79)90100-2.","productDescription":"15 p.","startPage":"23","endPage":"37","numberOfPages":"15","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":221896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":295430,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0025-3227(79)90100-2"}],"volume":"29","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f032e4b0c8380cd4a643","contributors":{"authors":[{"text":"Sallenger, A. H. Jr.","contributorId":8818,"corporation":false,"usgs":true,"family":"Sallenger","given":"A.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":363839,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012501,"text":"70012501 - 1979 - Origin of reverse-graded bedding in air-fall pumice, Coso Range, California","interactions":[],"lastModifiedDate":"2018-10-25T14:11:33","indexId":"70012501","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Origin of reverse-graded bedding in air-fall pumice, Coso Range, California","docAbstract":"<p>The origin of reverse grading in air-fall pyroclastic deposits has been ascribed to: (1) changing conditions at an erupting vent; (2) deposition in water; or (3) rolling of large clasts over smaller clasts on the surface of a steep slope. Structural features in a deposit of air-fall pumice lapilli in the Coso Range, California, indicate that reverse grading there formed by a fourth mechanism during flow of pumice. Reverse-graded beds in this deposit occur where pumice lapilli fell on slopes at or near the angle of repose and formed as parts of the blanket of accumulating pumice became unstable and flowed downslope. The process of size sorting during such flow is probably analogous to that which sorts sand grains in a reverse fashion during avalanching on the slip faces of sand dunes, attributed by Bagnold (1954a) to a grain-dispersive pressure acting on particles subjected to a shear stress. In view of the several ways in which air-fall pyroclastic debris may become reverse graded, caution is advised in interpretation of the origin of this structure both in modern and in ancient deposits.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0377-0273(79)90031-3","issn":"03770273","usgsCitation":"Duffield, W.A., Bacon, C., and Roquemore, G., 1979, Origin of reverse-graded bedding in air-fall pumice, Coso Range, California: Journal of Volcanology and Geothermal Research, v. 5, no. 1-2, p. 35-48, https://doi.org/10.1016/0377-0273(79)90031-3.","productDescription":"14 p.","startPage":"35","endPage":"48","numberOfPages":"14","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":222357,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Coso Range","volume":"5","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a70f1e4b0c8380cd7635c","contributors":{"authors":[{"text":"Duffield, W. A.","contributorId":71935,"corporation":false,"usgs":true,"family":"Duffield","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":363766,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bacon, C. R. 0000-0002-2165-5618","orcid":"https://orcid.org/0000-0002-2165-5618","contributorId":21522,"corporation":false,"usgs":true,"family":"Bacon","given":"C. R.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":363764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roquemore, G.R.","contributorId":33453,"corporation":false,"usgs":true,"family":"Roquemore","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":363765,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012453,"text":"70012453 - 1979 - Rare earth abundances and Rb-Sr systematics of basalts, gabbro, anorthosite and minor granitic rocks from the Indian Ocean Ridge System, Western Indian Ocean","interactions":[],"lastModifiedDate":"2012-03-12T17:19:06","indexId":"70012453","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Rare earth abundances and Rb-Sr systematics of basalts, gabbro, anorthosite and minor granitic rocks from the Indian Ocean Ridge System, Western Indian Ocean","docAbstract":"Basalts dredged from the Mid-Indian Ocean Ridge System have rare earth, Rb, and Sr concentrations like those from other mid-ocean ridges, but have slightly higher Sr87/Sr86 ratios. Underlying gabbroic complexes are similar to the basalts in Sr87/Sr86, but are poorer K, Rb, and in rare earths. The chemical and isotopic data, as well as the geologic relations suggest a cumulate origin for the bulk of the gabbroic complexes. ?? 1979 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF01164522","issn":"00107990","usgsCitation":"Hedge, C., Futa, K., Engel, C., and Fisher, R., 1979, Rare earth abundances and Rb-Sr systematics of basalts, gabbro, anorthosite and minor granitic rocks from the Indian Ocean Ridge System, Western Indian Ocean: Contributions to Mineralogy and Petrology, v. 68, no. 4, p. 373-376, https://doi.org/10.1007/BF01164522.","startPage":"373","endPage":"376","numberOfPages":"4","costCenters":[],"links":[{"id":222480,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":205244,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01164522"}],"volume":"68","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9517e4b0c8380cd817d0","contributors":{"authors":[{"text":"Hedge, C. E.","contributorId":73611,"corporation":false,"usgs":true,"family":"Hedge","given":"C. E.","affiliations":[],"preferred":false,"id":363612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Futa, K.","contributorId":26435,"corporation":false,"usgs":true,"family":"Futa","given":"K.","affiliations":[],"preferred":false,"id":363610,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Engel, C.G.","contributorId":18489,"corporation":false,"usgs":true,"family":"Engel","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":363609,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fisher, R.L.","contributorId":68028,"corporation":false,"usgs":true,"family":"Fisher","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":363611,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012537,"text":"70012537 - 1979 - Amino acid racemization dating of fossil bones, I. inter-laboratory comparison of racemization measurements","interactions":[],"lastModifiedDate":"2023-12-15T00:35:41.823643","indexId":"70012537","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Amino acid racemization dating of fossil bones, I. inter-laboratory comparison of racemization measurements","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"ab1\" class=\"abstract author\" lang=\"en\"><div id=\"aep-abstract-sec-id11\"><p>Enantiomeric measurements for aspartic acid, glutamic acid, and alanine in twenty-one different fossil bone samples have been carried out by three different laboratories using different analytical methods. These inter-laboratory comparisons demonstrate that<span>&nbsp;</span><i>D/L</i><span>&nbsp;</span>aspartic acid measurements are highly reproducible, whereas the enantiomeric measurements for the other amino acids show a wide variation between the three laboratories. At present, aspartic acid measurements are the most suitable for racemization dating of bone because of their superior analytical precision.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(79)90210-3","issn":"0012821X","usgsCitation":"Bada, J., Hoopes, E., Darling, D., Dungworth, G., Kessels, H., Kvenvolden, K., and Blunt, D., 1979, Amino acid racemization dating of fossil bones, I. inter-laboratory comparison of racemization measurements: Earth and Planetary Science Letters, v. 43, no. 2, p. 265-268, https://doi.org/10.1016/0012-821X(79)90210-3.","productDescription":"4 p.","startPage":"265","endPage":"268","numberOfPages":"4","costCenters":[],"links":[{"id":221899,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e9bae4b0c8380cd483f6","contributors":{"authors":[{"text":"Bada, J.L.","contributorId":96826,"corporation":false,"usgs":true,"family":"Bada","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":363850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoopes, E.","contributorId":8995,"corporation":false,"usgs":true,"family":"Hoopes","given":"E.","email":"","affiliations":[],"preferred":false,"id":363844,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Darling, D.","contributorId":61565,"corporation":false,"usgs":true,"family":"Darling","given":"D.","email":"","affiliations":[],"preferred":false,"id":363846,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dungworth, G.","contributorId":35465,"corporation":false,"usgs":true,"family":"Dungworth","given":"G.","email":"","affiliations":[],"preferred":false,"id":363845,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kessels, H.J.","contributorId":83667,"corporation":false,"usgs":true,"family":"Kessels","given":"H.J.","email":"","affiliations":[],"preferred":false,"id":363848,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kvenvolden, K.A.","contributorId":80674,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":363847,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Blunt, D.J.","contributorId":93189,"corporation":false,"usgs":true,"family":"Blunt","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":363849,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70012498,"text":"70012498 - 1979 - Changes in vegetation diversity caused by artificial recharge","interactions":[],"lastModifiedDate":"2012-03-12T17:19:10","indexId":"70012498","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3676,"text":"Vegetatio","active":true,"publicationSubtype":{"id":10}},"title":"Changes in vegetation diversity caused by artificial recharge","docAbstract":"Efforst to increase the rate of artificial recharge through basins often necessitates scrapping and ditching before and during operations. Such operations can result in more or less drastic changes in vegetation (depending on what was there before), characterized by diminisched numbers of species and lowered diversity. Two examples, one from Texas and one from the Netherlands are presented showing how similar treatments cause similar changes in two completely difference plant communities. ?? 1979 Dr. W. Junk b.v. - Publishers.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Vegetatio","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00055328","issn":"00423106","usgsCitation":"Van Hylckama, T.E., 1979, Changes in vegetation diversity caused by artificial recharge: Vegetatio, v. 39, no. 1, p. 53-57, https://doi.org/10.1007/BF00055328.","startPage":"53","endPage":"57","numberOfPages":"5","costCenters":[],"links":[{"id":205223,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00055328"},{"id":222309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f439e4b0c8380cd4bbf7","contributors":{"authors":[{"text":"Van Hylckama, T. E. A.","contributorId":73568,"corporation":false,"usgs":true,"family":"Van Hylckama","given":"T.","email":"","middleInitial":"E. A.","affiliations":[],"preferred":false,"id":363756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012547,"text":"70012547 - 1979 - A new instrument system to investigate sediment dynamics on continental shelves","interactions":[],"lastModifiedDate":"2025-04-18T15:12:41.304915","indexId":"70012547","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"A new instrument system to investigate sediment dynamics on continental shelves","docAbstract":"<p>A new instrumented tripod, the GEOPROBE system, has been constructed and used to collect time-series data on physical and geological parameters that are important in bottom sediment dynamics on continental shelves. Simultaneous in situ digital recording of pressure, temperature, light scattering, and light transmission, in combination with current velocity profiles measured with a near-bottom vertical array of electromagnetic current meters, is used to correlate bottom shear generated by a variety of oceanic processes (waves, tides, mean flow, etc.) with incipient movement and resuspension of bottom sediment. A bottom camera system that is activated when current speeds exceed preset threshold values provides a unique method to identify initial sediment motion and bed form development. </p><p>Data from a twenty day deployment of the GEOPROBE system in Norton Sound, Alaska, during the period September 24 - October 14, 1976 show that threshold conditions for sediment movement are commonly exceeded, even in calm weather periods, due to the additive effects of tidal currents, mean circulation, and surface waves.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(79)90021-5","issn":"00253227","usgsCitation":"Cacchione, D., and Drake, D., 1979, A new instrument system to investigate sediment dynamics on continental shelves: Marine Geology, v. 30, no. 3-4, p. 299-312, https://doi.org/10.1016/0025-3227(79)90021-5.","productDescription":"14 p.","startPage":"299","endPage":"312","costCenters":[],"links":[{"id":222083,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4a4e4b0c8380cd467c8","contributors":{"authors":[{"text":"Cacchione, D.A.","contributorId":65448,"corporation":false,"usgs":true,"family":"Cacchione","given":"D.A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":363868,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Drake, D.E.","contributorId":48150,"corporation":false,"usgs":true,"family":"Drake","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":363867,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70012514,"text":"70012514 - 1979 - A review of numerical simulation of hydrothermal systems","interactions":[],"lastModifiedDate":"2025-01-03T16:59:39.801197","indexId":"70012514","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1926,"text":"Hydrological Sciences Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"A review of numerical simulation of hydrothermal systems","docAbstract":"<p><span>Many advances in simulating single and two-phase fluid flow and heat transport in porous media have recently been made in conjunction with geothermal energy research. These numerical models reproduce system thermal and pressure behaviour and can be used for heat-transport problems other than those associated with geothermal energy development, such as high-level radioactive waste disposal and heat-storage projects. Although these models are general, additional research is necessary before they can be applied to certain site-specific problems that are concerned with additional processes, such as mass transport and flow in fractured media.</span></p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626667909491871","issn":"03036936","usgsCitation":"Mercer, J., and Faust, C., 1979, A review of numerical simulation of hydrothermal systems: Hydrological Sciences Bulletin, v. 24, no. 3, p. 335-344, https://doi.org/10.1080/02626667909491871.","productDescription":"10 p.","startPage":"335","endPage":"344","numberOfPages":"10","costCenters":[],"links":[{"id":488798,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626667909491871","text":"Publisher Index Page"},{"id":222541,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e554e4b0c8380cd46cba","contributors":{"authors":[{"text":"Mercer, J.W.","contributorId":90741,"corporation":false,"usgs":true,"family":"Mercer","given":"J.W.","affiliations":[],"preferred":false,"id":363795,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Faust, C.R.","contributorId":9922,"corporation":false,"usgs":true,"family":"Faust","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":363794,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}