There were no major earthquakes during the first 2 months of the year and there were no earthquake-related deaths reported during this same time period. In the United States a moderate earthquake on February 28 in southern California caused some minor injuries and considerable damage.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1990, Earthquakes, January-February 1990: Earthquakes & Volcanoes (USGS), v. 22, no. 4, p. 179-182.","productDescription":"4 p.","startPage":"179","endPage":"182","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318481,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56d6cb40e4b015c306f32c75","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621676,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70168945,"text":"70168945 - 1990 - Volcano hazard mitigation program in Indonesia","interactions":[],"lastModifiedDate":"2016-03-08T16:49:08","indexId":"70168945","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1437,"text":"Earthquakes & Volcanoes (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Volcano hazard mitigation program in Indonesia","docAbstract":"Volcanological investigations in Indonesia were started in the 18th century, when Valentijn in 1726 prepared a chronological report of the eruption of Banda Api volcno, Maluku. Modern and intensive volcanological studies did not begin until the catastrophic eruption of Kelut volcano, East Java, in 1919. The eruption took 5,011 lives and destroyed thousands of acres of coffee plantation. An eruption lahar generated by the crater lake water mixed with volcanic eruptions products was the cause of death for a high number of victims. An effort to mitigate the danger from volcanic eruption was first initiated in 1921 by constructing a tunnel to drain the crater lake water of Kelut volcano. At the same time a Volcanological Survey was established by the government with the responsibility of seeking every means for minimizing the hazard caused by volcanic eruption.
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The primary objective of this operation was to capture live, oiled sea otters for cleaning and rehabilitation. Between 30 March and 29 May 1989, 139 live sea otters were captured in the sound and transported to rehabilitation centers in Valdez, Alaska. Within the first 15 days of capture operations, 122 (88%) otters were captured. Most sea otters were captured near Knight, Green, and Evans islands in the western sound. The primary capture method consisted of dipnetting otters out of water and off beaches. While capture rates declined over time, survival of captured otters increased as the interval from spill date to capture date increased. The relative degree of oiling observed for each otter captured declined over time. Declining capture rates led to the use of tangle nets. The evidence suggests the greatest threat to sea otters in Prince William Sound occurred within the first 3 weeks after the spill. Thus, in the future, the authors believe rescue efforts should begin as soon as possible after an oil spill in sea otter habitat. Further, preemptive capture and relocation of sea otters in Prince William Sound may have increased the number of otters that could have survived this event.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Sea otter symposium: Proceedings of a symposium to evaluate the response effort on behalf of sea otters after the T/V Exxon Valdez oil spill into Prince William Sound (Biological Reports 90[12])","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"conferenceTitle":"Sea Otter Symposium: Symposium to evaluate the response effort on behalf of sea otters after the T/V Exxon Valdez oil spill into Prince William Sound","conferenceDate":"April 17-19, 1990","conferenceLocation":"Anchorage, AK","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Anchorage, AK","doi":"10.5962/bhl.title.45854","issn":"0895-1926","usgsCitation":"Bodkin, J.L., and Weltz, F., 1990, Evaluation of sea otter capture after the Exxon Valdez oil spill, Prince William Sound, Alaska, in Sea otter symposium: Proceedings of a symposium to evaluate the response effort on behalf of sea otters after the T/V Exxon Valdez oil spill into Prince William Sound (Biological Reports 90[12]), Anchorage, AK, April 17-19, 1990, p. 61-69, https://doi.org/10.5962/bhl.title.45854.","productDescription":"9 p.","startPage":"61","endPage":"69","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":488641,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5962/bhl.title.45854","text":"Publisher Index Page"},{"id":343082,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Prince William Sound","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5965f9c5e4b0d1f9f05cae6c","contributors":{"editors":[{"text":"Bayha, Keith","contributorId":30270,"corporation":false,"usgs":false,"family":"Bayha","given":"Keith","email":"","affiliations":[{"id":6654,"text":"USFWS","active":true,"usgs":false}],"preferred":false,"id":702307,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Kormendy, Jennifer","contributorId":190781,"corporation":false,"usgs":false,"family":"Kormendy","given":"Jennifer","email":"","affiliations":[],"preferred":false,"id":702308,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Bodkin, James L. 0000-0003-1641-4438 jbodkin@usgs.gov","orcid":"https://orcid.org/0000-0003-1641-4438","contributorId":748,"corporation":false,"usgs":true,"family":"Bodkin","given":"James","email":"jbodkin@usgs.gov","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":702305,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weltz, F.","contributorId":100704,"corporation":false,"usgs":false,"family":"Weltz","given":"F.","email":"","affiliations":[],"preferred":false,"id":702306,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70168811,"text":"70168811 - 1990 - The mass media and disasters","interactions":[],"lastModifiedDate":"2016-03-03T15:29:15","indexId":"70168811","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1437,"text":"Earthquakes & Volcanoes (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"The mass media and disasters","docAbstract":"Past investigations by myself and others on the role of the mass media in disasters indicate that news people typically find themselves in situations of uncertainty, ambiguity, and conflicting information; the communication and transportation services that these people use in covering a story become inoperative. However, the media are expected to make sense of the disaster situation almost immediately. the difficulties of doing so were reflected by the ABC Goodyear Blimp footage of the collapsed Nimitz Freeway in Oakland, California, broadcast nationally on the evening of October 17, 1989. The televised picture showed the disastrous results of the Loma Prieta earthquake, but for an hour or more the announcer could not correctly identify what was being shown. He did not seem to realize that the upper deck of the freeway had collapsed on the lower deck, crushing vechiles and people.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Rogers, E.M., 1990, The mass media and disasters: Earthquakes & Volcanoes (USGS), v. 22, no. 4, p. 176-178.","productDescription":"3 p.","startPage":"176","endPage":"178","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318542,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56d96e5fe4b015c306f764d6","contributors":{"authors":[{"text":"Rogers, E. M.","contributorId":167337,"corporation":false,"usgs":false,"family":"Rogers","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":621841,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1003211,"text":"1003211 - 1990 - Egg size and laying order of snowy egrets, great egrets, and black-crowned night-herons","interactions":[],"lastModifiedDate":"2023-11-29T12:24:24.890881","indexId":"1003211","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1318,"text":"Condor","active":true,"publicationSubtype":{"id":10}},"title":"Egg size and laying order of snowy egrets, great egrets, and black-crowned night-herons","docAbstract":"The authors' objective was to describe egg size in relation to laying order for Great Egrets (Casmerodius albus ), Snowy Egrets (Egretta thula ), and Black-crowned Night-Herons (Nycticorax nycticorax ) in a southern Texas colony and Great Egrets in a southern Florida colony. Based on egg-size patterns in other colonial waterbirds and the occurrence of brood reduction in egrets and herons, they predicted that the final egg laid in a clutch would be smaller than those laid earlier.","language":"English","publisher":"Oxford Academic","doi":"10.2307/1368698","usgsCitation":"Custer, T., and Frederick, P.C., 1990, Egg size and laying order of snowy egrets, great egrets, and black-crowned night-herons: Condor, v. 92, no. 3, p. 772-775, https://doi.org/10.2307/1368698.","productDescription":"4 p.","startPage":"772","endPage":"775","numberOfPages":"4","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":133871,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"92","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60f2a1","contributors":{"authors":[{"text":"Custer, T. W. 0000-0003-3170-6519","orcid":"https://orcid.org/0000-0003-3170-6519","contributorId":91802,"corporation":false,"usgs":true,"family":"Custer","given":"T. W.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":312964,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frederick, P. C.","contributorId":66645,"corporation":false,"usgs":true,"family":"Frederick","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":312963,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70016431,"text":"70016431 - 1990 - Geophysical constraints on Washington convergent margin structure","interactions":[],"lastModifiedDate":"2024-05-24T15:28:32.02146","indexId":"70016431","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Geophysical constraints on Washington convergent margin structure","docAbstract":"Gravity and magnetic maps of western Washington reveal the lateral structure and fabric of the Washington Coast Range, Puget Basin, and southern Washington Cascade Range. The magnetic and gravity maps show large amplitude positive anomalies associated with the shallow but largely buried section of Washington Coast Range mafic rocks which are separated by negative anomalies over deep sedimentary basins. The positive anomalies indicate that the Coast Range mafic basement extends farther east than previously thought, at least as far east as the longitude of Seattle. Linear and steep gravity and magnetic gradients indicate many unmapped, often buried faults in the Washington Coast Range Province. Magnetic highs are also associated with mapped batholiths in the Cascade arc. Several magnetic highs observed east of the Coast Range rocks and west of these batholiths may be associated with buried Tertiary plutons or ophiolites. Two-dimensional gravity and magnetic modeling constrained with geological and other geophysical data indicate that the Coast Range Province rocks are about 1 km thick at the coast, thickening to as much as 30 km near their postulated eastern edge. A maximum boundary on the average density of the upper 15–20 km of the rocks that compose the Coast Range Province of 2920 kg/m3 was established by the modeling, suggesting a composition largely of basalt and gabbro with little interbedded sediments. Under these rocks may be mantle or a subduction complex composed of dense mafic, ultramafic, and sedimentary rocks like that proposed to underlie Vancouver Island. Previous gravity models of the Washington margin include lower densities for the proposed subduction complex than for Vancouver Island, suggesting a lower component of mafic and ultramafic rocks than the rocks underlying Vancouver Island. However, my Washington model requires that the proposed subduction complex be more dense than the trench sediments and, therefore, that material denser than sediments be incorporated within it. The absence of continental mantle and the modeled wedge shape of the Coast Range Province upper crust suggest that erosion of the bottom of the overriding plate by subduction processes may have occurred.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB095iB12p19533","issn":"01480227","usgsCitation":"Finn, C.A., 1990, Geophysical constraints on Washington convergent margin structure: Journal of Geophysical Research Solid Earth, v. 95, no. B12, p. 19533-19546, https://doi.org/10.1029/JB095iB12p19533.","productDescription":"14 p.","startPage":"19533","endPage":"19546","costCenters":[],"links":[{"id":222972,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.99289441326454,\n 48.94625600979734\n ],\n [\n -129.5979382121656,\n 48.94625600979734\n ],\n [\n -129.5979382121656,\n 45.56775656606118\n ],\n [\n -120.99289441326454,\n 45.56775656606118\n ],\n [\n -120.99289441326454,\n 48.94625600979734\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"95","issue":"B12","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a2814e4b0c8380cd59deb","contributors":{"authors":[{"text":"Finn, Carol A. 0000-0002-6178-0405 cfinn@usgs.gov","orcid":"https://orcid.org/0000-0002-6178-0405","contributorId":1326,"corporation":false,"usgs":true,"family":"Finn","given":"Carol","email":"cfinn@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":373492,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70016269,"text":"70016269 - 1990 - Influence of climate and eolian dust on the major-element chemistry and clay mineralogy of soils in the northern Bighorn basin, U.S.A.","interactions":[],"lastModifiedDate":"2023-09-06T18:12:02.223595","indexId":"70016269","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1198,"text":"Catena","active":true,"publicationSubtype":{"id":10}},"title":"Influence of climate and eolian dust on the major-element chemistry and clay mineralogy of soils in the northern Bighorn basin, U.S.A.","docAbstract":"Soil chronosequences in the northern Bighorn basin permit the study of chronologic changes in the major-element chemistry and clay mineralogy of soils formed in different climates. Two chronosequences along Rock Creek in south-central Montana formed on granitic alluvium in humid and semiarid climates over the past two million years. A chronosequence at the Kane fans in north-central Wyoming formed on calcareous alluvium in an arid climate over the past 600,000 years. Detailed analyses of elemental chemistry indicate that the soils in all three areas gradually incorporated eolian dust that contained less zirconium, considered to be chemically immobile during weathering, than did the alluvium. B and C horizons of soils in the wettest of the chronosequences developed mainly at logarithmic rates, suggesting that leaching, initially rapid but decelerating, dominated the dust additions. In contrast, soils in the most arid of the chronosequences developed at linear rates that reflect progressive dust additions that were little affected by leaching. Both weathering and erosion may cause changes with time to appear logarithmic in A horizons of soils under the moist and semiarid climatic regimes. Clay minerals form with time in the basal B and C horizons and reflect climatic differences in the three areas. Vermiculite, mixed-layer illite-smectite, and smectite form in the soils of the moist-climate chronosequence; smectite forms in the semiarid-climate chronosequence; and smectite and palygorskite form in the arid-climate chronosequence. ?? 1990.","language":"English","publisher":"Elsevier","doi":"10.1016/0341-8162(90)90018-9","usgsCitation":"Reheis, M.C., 1990, Influence of climate and eolian dust on the major-element chemistry and clay mineralogy of soils in the northern Bighorn basin, U.S.A.: Catena, v. 17, no. 3, p. 219-248, https://doi.org/10.1016/0341-8162(90)90018-9.","productDescription":"30 p.","startPage":"219","endPage":"248","numberOfPages":"30","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":223460,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3b18e4b0c8380cd62219","contributors":{"authors":[{"text":"Reheis, Marith C. 0000-0002-8359-323X mreheis@usgs.gov","orcid":"https://orcid.org/0000-0002-8359-323X","contributorId":138571,"corporation":false,"usgs":true,"family":"Reheis","given":"Marith","email":"mreheis@usgs.gov","middleInitial":"C.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":373029,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70015821,"text":"70015821 - 1990 - Precambrian terrane of north-central Wisconsin: an aeromagnetic perspective","interactions":[],"lastModifiedDate":"2023-09-21T17:33:00.578995","indexId":"70015821","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1168,"text":"Canadian Journal of Earth Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Precambrian terrane of north-central Wisconsin: an aeromagnetic perspective","docAbstract":"A shaded relief magnetic map covering most of the region of exposed Precambrian rocks of north-central Wisconsin shows the structural grain and many lithologic units with clarity and comprehensive detail. The area includes part of the volcanic sequence of the Keweenawan Supergroup south of Lake Superior, the southern margin of the Archean Superior Province, the accreted island-arc terranes of the Penokean Orogen, and the Wolf River batholith. Numerous dikes are evident in the shaded relief, some being more than 200 km in length. Many of the longer dikes are reversely magnetized Keweenawan diabase associated with early extension of the Midcontinent Rift; some apparently were intruded along preexisting faults. A northwest system of dikes and faults indicated by the shaded relief map may be related to later stages of Keweenawan rifting. The Wolf River batholith is characterized by low magnetic relief associated with the predominant granitoids but includes circular plutons of highly magnetic anorthosite and a large area of magnetic rock having a signature different from the mapped anorthosite bodies. A fault bounding the western side of the batholith is paralleled by an apparent system of faults or dikes in the older terrane to the west. The magnetic map covering the Wisconsin magmatic terranes and the Archean Superior Province margin to the north is dominated by east-northeast-trending Penokean rocks. Large units of magnetic mafic rocks and less magnetic granitoid rocks are cut by a system of well-defined northeast shear zones and a more easterly trending, possibly younger set of faults, some of which contain dikes along parts of their lengths. Although the sutures bounding the magmatic terranes generally follow the magnetic trends, they do not have distinctive magnetic signatures.
","language":"English","publisher":"Canadian Science Publishing","doi":"10.1139/e90-156","issn":"00084077","usgsCitation":"King, E.R., 1990, Precambrian terrane of north-central Wisconsin: an aeromagnetic perspective: Canadian Journal of Earth Sciences, v. 27, no. 11, p. 1472-1477, https://doi.org/10.1139/e90-156.","productDescription":"6 p.","startPage":"1472","endPage":"1477","costCenters":[],"links":[{"id":223434,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Lake Superior","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -87.66671060976584,\n 44.3610017587431\n ],\n [\n -87.66671060976584,\n 46.373762217927776\n ],\n [\n -92.90108864423792,\n 46.373762217927776\n ],\n [\n -92.90108864423792,\n 44.3610017587431\n ],\n [\n -87.66671060976584,\n 44.3610017587431\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"27","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8107e4b0c8380cd7b321","contributors":{"authors":[{"text":"King, E. R.","contributorId":93482,"corporation":false,"usgs":true,"family":"King","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":371848,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2000055,"text":"2000055 - 1990 - International position statement and evaluation guidelines for artificial reefs in the Great Lakes","interactions":[],"lastModifiedDate":"2012-02-02T00:14:56","indexId":"2000055","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":217,"text":"Special Publication","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"90-2","title":"International position statement and evaluation guidelines for artificial reefs in the Great Lakes","docAbstract":"The purpose of this position statement is to guide the evaluation of artificial reef proposals in the Great Lakes so that any reefs built will enhance the fisheries and recreational uses of the lakes without adversely affecting natural resources or impeding other beneficial uses. This position statement sets minimum recommended standards for evaluating artifical reef proposals and lists the factors that should be considered in planning artificial reefs. Other relevant lists are summarized. The Great Lakes jurisdictions are encouraged to incorporate the elements of this position statement, as a minimum, into their own policy. In lieu of official policy development the jurisdictions and agencies are encouraged to use the position statement and accompanying guidelines when reviewing artificial reef proposals.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"Gannon, J., 1990, International position statement and evaluation guidelines for artificial reefs in the Great Lakes: Special Publication 90-2.","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198858,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adee1","contributors":{"authors":[{"text":"Gannon, John E.","contributorId":74706,"corporation":false,"usgs":true,"family":"Gannon","given":"John E.","affiliations":[],"preferred":false,"id":325003,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2002257,"text":"2002257 - 1990 - The hydrologic role of the unsaturated zone of a forested colluvium-mantled hollow","interactions":[],"lastModifiedDate":"2012-02-02T00:15:00","indexId":"2002257","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":91,"text":"Technical Report","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"26","title":"The hydrologic role of the unsaturated zone of a forested colluvium-mantled hollow","docAbstract":"No abstract available at this time","language":"English","publisher":"National Park Service, Redwood National Park","publisherLocation":"Arcata, CA","usgsCitation":"Amen, B., 1990, The hydrologic role of the unsaturated zone of a forested colluvium-mantled hollow: Technical Report 26.","costCenters":[],"links":[{"id":112256,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.waterboards.ca.gov/water_issues/programs/tmdl/records/region_1/2003/ref1954.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":199225,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a85e4b07f02db64d821","contributors":{"authors":[{"text":"Amen, B.B.","contributorId":95984,"corporation":false,"usgs":true,"family":"Amen","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":326301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2002235,"text":"2002235 - 1990 - Plant communities of Santa Rosa Island, Channel Islands National Park","interactions":[],"lastModifiedDate":"2016-08-11T14:31:40","indexId":"2002235","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":91,"text":"Technical Report","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"42","title":"Plant communities of Santa Rosa Island, Channel Islands National Park","docAbstract":"A survey of the plant communities on Santa Rosa Island, Channel Islands National Park, was conducted from January through July 1988. Vegetation data were collected at 296 sites using a releve technique. The plant communities described include: grassland, coastal marsh, caliche scrub, coastal sage scrub, lupine scrub, baccharis scrub, coastal bluff scrub, coastal dune scrub, mixed chaparral, mixed woodland, torrey pine woodland, closed-cone pine woodland, island oak woodland, riparian woodland, and riparian herbaceous vegetation. The areal extent of each community was mapper on USGS 7.5' topographic maps, and digitized for GIS manipulation.
","language":"English","publisher":"University of California, NPS Cooperative Park Studies Unit","usgsCitation":"Clark, R.A., Halvorson, W., Sawdo, A.A., and Danielsen, K.C., 1990, Plant communities of Santa Rosa Island, Channel Islands National Park: Technical Report 42, v, 93 p.","productDescription":"v, 93 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":198262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":326406,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.nps.gov/parkhistory/online_books/chis/plant_communities.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6850f6","contributors":{"authors":[{"text":"Clark, Ronilee A.","contributorId":54931,"corporation":false,"usgs":true,"family":"Clark","given":"Ronilee","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":326241,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Halvorson, William L.","contributorId":97194,"corporation":false,"usgs":true,"family":"Halvorson","given":"William L.","affiliations":[],"preferred":false,"id":326242,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sawdo, Andell A.","contributorId":173613,"corporation":false,"usgs":false,"family":"Sawdo","given":"Andell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":326243,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Danielsen, Karen C.","contributorId":173614,"corporation":false,"usgs":false,"family":"Danielsen","given":"Karen","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":326244,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70137851,"text":"70137851 - 1990 - Accumulation of bank-top sediment on the western slope of Great Bahama Bank: rapid progradation of a carbonate megabank","interactions":[],"lastModifiedDate":"2017-08-16T08:54:23","indexId":"70137851","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Accumulation of bank-top sediment on the western slope of Great Bahama Bank: rapid progradation of a carbonate megabank","docAbstract":"High-resolution seismic profiles and submersible observations along the leeward slope of western Great Bahama Bank show large-scale export of bank-top sediment and rapid progradation of the slope during the Holocene. A wedge-shaped sequence, up to 90 m thick, is present along most of the slope and consists of predominantly aragonite mud derived from the bank since flooding of the platform 6-8 ka. Total sediment volume of the slope sequence is 40%-80% that of Holocene sediment currently retained on the bank. Maximum rates of vertical accumulation and lateral progradation are 11-15 m/ka and 80-110 m/ka, respectively: 10 to 100 times greater than previously known for periplatform muds. Slope deposition of exported mud during sea-level highs appears to have been a major mechanism for the westward progradation of Great Bahama Bank throughout the Quaternary; this may provide a critical modern analogue for ancient progradational margins.
","language":"English","publisher":"Geological Society of America","usgsCitation":"Wilber, R.J., Milliman, J., and Halley, R., 1990, Accumulation of bank-top sediment on the western slope of Great Bahama Bank: rapid progradation of a carbonate megabank: Geology, v. 18, no. 10, p. 970-974.","productDescription":"5 p.","startPage":"970","endPage":"974","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":297184,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":297183,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://geology.gsapubs.org/content/18/10/970.abstract"}],"otherGeospatial":"Great Bahama Bank","volume":"18","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2b28e4b08de9379b3279","contributors":{"authors":[{"text":"Wilber, R. Jude","contributorId":138640,"corporation":false,"usgs":false,"family":"Wilber","given":"R.","email":"","middleInitial":"Jude","affiliations":[],"preferred":false,"id":538181,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Milliman, John D.","contributorId":76735,"corporation":false,"usgs":false,"family":"Milliman","given":"John D.","affiliations":[{"id":6706,"text":"Woods Hole Oceanographic Institution,","active":true,"usgs":false}],"preferred":false,"id":538182,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Halley, Robert B.","contributorId":45692,"corporation":false,"usgs":true,"family":"Halley","given":"Robert B.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":538183,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27508,"text":"wri904050 - 1990 - Ground-water resources of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada","interactions":[],"lastModifiedDate":"2022-05-10T17:23:56.874406","indexId":"wri904050","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"90-4050","title":"Ground-water resources of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada","docAbstract":"Honey Lake Valley is a 2,200 sq-mi, topographically closed basin about 35 miles northwest of Reno, Nevada. Unconsolidated basin-fill deposits on the valley floor and fractured volcanic rocks in northern and eastern uplands are the principal aquifers. In the study area, about 130,000 acre- ft of water recharges the aquifer system annually, about 40% by direct infiltration of precipitation and about 60% by infiltration of streamflow and irrigation water. Balancing this is an equal amount of groundwater discharge, of which about 65% evaporates from the water table or is transpired by phreatophytes, about 30 % is withdrawn from wells, and about 5% leaves the basin as subsurface outflow to the east. Results of a groundwater flow model of the eastern part of the basin, where withdrawals for public supply have been proposed, indicate that if 15,000 acre-ft of water were withdrawn annually, a new equilibrium would eventually be established by a reduction of about 60% in both evapotranspiration and subsurface outflow to the east. Hydrologic effects would be minimal at the western boundary of the flow-model area. Within the modeled area, the increased withdrawals cause an increase in the simulated net flow of groundwater eastward across the California-Nevada State line from about 670 acre-ft/yr to about 2,300 acre-ft/yr. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri904050","collaboration":"Prepared in cooperation with the California Department of Water Resources and the Nevada Division of Water Resources","usgsCitation":"Handman, E.H., Londquist, C.J., and Maurer, D.K., 1990, Ground-water resources of Honey Lake Valley, Lassen County, California, and Washoe County, Nevada: U.S. Geological Survey Water-Resources Investigations Report 90-4050, Report: vii, 112 p.; 4 Plates: 16.03 x 21.94 inches, https://doi.org/10.3133/wri904050.","productDescription":"Report: vii, 112 p.; 4 Plates: 16.03 x 21.94 inches","costCenters":[],"links":[{"id":400440,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4050/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":400439,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4050/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":400438,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4050/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":400441,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4050/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56354,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4050/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119863,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4050/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","county":"Lassen County, Washoe County","otherGeospatial":"Honey Lake Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.22314453124999,\n 39.592990390285024\n ],\n [\n -119.1302490234375,\n 39.592990390285024\n ],\n [\n -119.1302490234375,\n 40.67438908251788\n ],\n [\n -121.22314453124999,\n 40.67438908251788\n ],\n [\n -121.22314453124999,\n 39.592990390285024\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae167","contributors":{"authors":[{"text":"Handman, Elinor H.","contributorId":31748,"corporation":false,"usgs":true,"family":"Handman","given":"Elinor","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":198231,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Londquist, Clark J.","contributorId":44149,"corporation":false,"usgs":true,"family":"Londquist","given":"Clark","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198232,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Maurer, Douglas K. dkmaurer@usgs.gov","contributorId":2308,"corporation":false,"usgs":true,"family":"Maurer","given":"Douglas","email":"dkmaurer@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":198230,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70137865,"text":"70137865 - 1990 - Major off-axis hydrothermal activity on the northern Gorda Ridge","interactions":[],"lastModifiedDate":"2019-12-10T13:39:05","indexId":"70137865","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Major off-axis hydrothermal activity on the northern Gorda Ridge","docAbstract":"The first hydrothermal field on the northern Gorda Ridge, the Sea Cliff hydrothermal field, was discovered and geologic controls of hydrothermal activity in the rift valley were investigated on a dive series using the DSV Sea Cliff. The Sea Cliff hydrothermal field was discovered where predicted at the intersection of axis-oblique and axis-parallel faults at the south end of a linear ridge at mid-depth (2700 m) on the east wall. Preliminary mapping and sampling of the field reveal: a setting nested on nearly sediment-free fault blocks 300 m above the rift valley floor 2.6 km from the axis; a spectrum of venting types from seeps to black smokers; high conductive heat flow estimated to be equivalent to the convective flux of multiple black smokers through areas of the sea floor sealed by a caprock of elastic breccia primarily derived from basalt with siliceous cement and barite pore fillings; and a vent biota with Juan de Fuca Ridge affinites. These findings demonstrate the importance of off-axis hydrothermal activity and the role of the intersection of tectonic lineations in controlling hydrothermal sites at sea-floor spreading centers.
High-resolution seismic-reflection profiles of the Quicksands, located along a broad ridge on the platform shelf west of Key West, Florida, indicate a significant deposit of non-oolitic carbonate sand occurs in a belt 47 km long by 28 km wide. The surface of the belt is ornamented by large (5 m), migrating tidal bars, oriented in a north-south direction, on which sand waves, oriented in an east-west direction, are superimposed. Some of the sand waves are awash at low tide. The sand waves are formed by strong reversing tidal currents flowing between the Gulf of Mexico and the Straits of Florida. The waves migrate directly over Pleistocene bedrock to the east, but the deposit thickens to the west and sand waves there overlie non-oolitic Holocene accumulations as thick as 12 m. Westward-dipping accretionary bedding indicates that net migration of the sands is to the west, despite north-south movement of tidal currents. The westward edge of the accumulation has accreted over deeper, muddier deposits. Although tidal currents and resultant bedforms appear identical to those of active ooid deposits in the Bahamas and elsewhere, no oolitically coated grains were found in this study. Thin-section analyses show the principal component (average 48%) of the sands is fragmented plates of species of the green alga Halimeda , followed by particulate coral (average 17%), which increases off the flanks of the main sand body. Short vibracores confirm the presence of cross-bedding.
","language":"English","publisher":"American Geological Institute","doi":"10.1306/D4267654-2B26-11D7-8648000102C1865D","usgsCitation":"Shinn, E., Lidz, B.H., and Holmes, C.W., 1990, High-energy carbonate-sand accumulation, the Quicksands, southwest Florida Keys: Journal of Sedimentary Research, v. 60, no. 6, p. 952-967, https://doi.org/10.1306/D4267654-2B26-11D7-8648000102C1865D.","productDescription":"16 p.","startPage":"952","endPage":"967","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":297189,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Florida Keys","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.375244140625,\n 25.334096684794456\n ],\n [\n -79.969482421875,\n 25.334096684794456\n ],\n [\n -80.04638671875,\n 24.427145340082046\n ],\n [\n -83.21044921875,\n 24.387127324604496\n ],\n [\n -83.375244140625,\n 25.334096684794456\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"60","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2bc1e4b08de9379b34ae","contributors":{"authors":[{"text":"Shinn, Eugene A.","contributorId":86708,"corporation":false,"usgs":true,"family":"Shinn","given":"Eugene A.","affiliations":[],"preferred":false,"id":538194,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lidz, Barbara H. blidz@usgs.gov","contributorId":2475,"corporation":false,"usgs":true,"family":"Lidz","given":"Barbara","email":"blidz@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":538195,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holmes, Charles W.","contributorId":31071,"corporation":false,"usgs":true,"family":"Holmes","given":"Charles","email":"","middleInitial":"W.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":538196,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5222335,"text":"5222335 - 1990 - Summer-fall survival of American woodcock in Maine","interactions":[],"lastModifiedDate":"2024-11-27T16:59:38.349548","indexId":"5222335","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","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":"Summer-fall survival of American woodcock in Maine","docAbstract":"We estimated summer-fall (15 Jun-20 Oct) survival for 32 adult and 96 fledged young American woodcock (Scolopax minor) radiotagged in eastern Maine during 1982-84 using single-interval, multiple-interval, and nonparametric (product-limit) methods. Single-interval survival estimates were 0.90, 0.88, 0.57, and 0.73 for adult males, adult females, young males, and young females, respectively. Multiple-interval survival estimates (0.93, 0.88, 0.63, and 0.71) and product-limit estimates were similar (0.92, 0.90, 0.60, and 0.69). Within each age class, male and female period survival was not significantly different for any method. However, point estimates of survival for young females exceeded those of young males by 0.08-0.16. Regardless of sex, adults exhibited higher summer-fall survival (range = 0.89-0.92) than young woodcock (range = 0.64-0.68). Age-specific variation in survival was caused by different predation rates that may be related to age-specific differences in mobility. The survival rates sustained by young woodcock during our study were similar to 4-month rates derived from annual survival estimates that assume constant mortality throughout the year. The high summer-fall survival estimates exhibited by adult woodcock suggest that most of their annual mortality occurs during another season.
","language":"English","publisher":"Wiley","doi":"10.2307/3808908","usgsCitation":"Derleth, E.L., and Sepik, G.F., 1990, Summer-fall survival of American woodcock in Maine: Journal of Wildlife Management, v. 54, no. 1, p. 97-106, https://doi.org/10.2307/3808908.","productDescription":"10 p.","startPage":"97","endPage":"106","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196805,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maine","otherGeospatial":"Moosehorn National Wildlife Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -67.3421839957323,\n 45.12198312819828\n ],\n [\n -67.3421839957323,\n 45.043085523510314\n ],\n [\n -67.22936983686924,\n 45.043085523510314\n ],\n [\n -67.22936983686924,\n 45.12198312819828\n ],\n [\n -67.3421839957323,\n 45.12198312819828\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"54","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6986b8","contributors":{"authors":[{"text":"Derleth, Eric L.","contributorId":220145,"corporation":false,"usgs":false,"family":"Derleth","given":"Eric","email":"","middleInitial":"L.","affiliations":[{"id":6661,"text":"US Fish and Wildlife Service","active":true,"usgs":false}],"preferred":false,"id":336103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sepik, Greg F.","contributorId":100055,"corporation":false,"usgs":false,"family":"Sepik","given":"Greg","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":336104,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70195676,"text":"70195676 - 1990 - 1986 Great Lakes Seismic refraction survey (GLIMPCE): Line A - refraction mode","interactions":[],"lastModifiedDate":"2023-03-21T13:24:05.406215","indexId":"70195676","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":5636,"text":"Geological Survey of Canada Open File","active":true,"publicationSubtype":{"id":4}},"seriesNumber":"2283","title":"1986 Great Lakes Seismic refraction survey (GLIMPCE): Line A - refraction mode","docAbstract":"In the fall of 1986, the Geological Survey of Canada (GSC), the United States Geological Survey (USGS), two Canadian universities -- University of Western Ontario and University of Saskatchewan, and four American universities -- Northern Illinois University, Southern Illinois University, University of Wisconsin-Madison and University of Wisconsin-Oshkosh participated in a major deep seismic experiment in Lake Superior under the GLIMPCE (Great Lakes International Multidisciplinary Program on Crustal Evolution) umbrella. This Open-File Report presents the seismic sections for line A, which was shot specifically for refraction recording. The main target for study by this line was the Mid-Continent Rift System. All recording stations, 31 in total (26 land stations and 5 OBSs), recorded energy from shots fired every two minutes (333 m spacing) by a tuned airgun array towed by a contracted ship along line A in Lake Superior. These data are the densest such data ever recorded in the continental North America over such distances. It is also unique since coincident seismic reflection and refraction are available.
","language":"English","publisher":"Geological Survey of Canada","doi":"10.4095/128170","usgsCitation":"Morel-a-l’Huissier, P., Karl, J.H., Trehu, A.M., Hajnal, Z., Mereu, R.F., Meyer, R.P., Sexton, J.L., Ervin, C.P., Green, A.G., and Hutchinson, D., 1990, 1986 Great Lakes Seismic refraction survey (GLIMPCE): Line A - refraction mode: Geological Survey of Canada Open File 2283, 31 p., https://doi.org/10.4095/128170.","productDescription":"31 p.","numberOfPages":"61","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":479824,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4095/128170","text":"Publisher Index Page"},{"id":352051,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","otherGeospatial":"Lake Superior","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": 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Patrick","contributorId":8552,"corporation":false,"usgs":false,"family":"Ervin","given":"C.","email":"","middleInitial":"Patrick","affiliations":[{"id":13666,"text":"Northern Illinois University","active":true,"usgs":false}],"preferred":false,"id":729658,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Green, Alan G.","contributorId":83314,"corporation":false,"usgs":false,"family":"Green","given":"Alan","email":"","middleInitial":"G.","affiliations":[{"id":13092,"text":"Geological Survey of Canada","active":true,"usgs":false}],"preferred":false,"id":729659,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Hutchinson, Deborah 0000-0002-2544-5466 dhutchinson@usgs.gov","orcid":"https://orcid.org/0000-0002-2544-5466","contributorId":174836,"corporation":false,"usgs":true,"family":"Hutchinson","given":"Deborah","email":"dhutchinson@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":729660,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":1014643,"text":"1014643 - 1990 - Research establishes proper feeding level for young Atlantic salmon in reuse system","interactions":[],"lastModifiedDate":"2012-02-02T00:04:27","indexId":"1014643","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3330,"text":"Salmonid","active":true,"publicationSubtype":{"id":10}},"title":"Research establishes proper feeding level for young Atlantic salmon in reuse system","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Salmonid","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"90-078/TL","usgsCitation":"Poston, H.A., and Williams, R., 1990, Research establishes proper feeding level for young Atlantic salmon in reuse system: Salmonid, v. 14, no. 1, p. 12-13.","productDescription":"p. 12-13","startPage":"12","endPage":"13","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a3e1","contributors":{"authors":[{"text":"Poston, H. A.","contributorId":21893,"corporation":false,"usgs":true,"family":"Poston","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":320802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, R.C.","contributorId":103621,"corporation":false,"usgs":true,"family":"Williams","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":320803,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1014606,"text":"1014606 - 1990 - Vertical distribution of adult American shad in the Connecticut River","interactions":[],"lastModifiedDate":"2017-07-19T14:34:59","indexId":"1014606","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","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":"Vertical distribution of adult American shad in the Connecticut River","docAbstract":"Adult American shad Alosa sapidissima were sampled with vertical gill nets during the 1986 and 1987 spawning and postspawning migrations in the Connecticut River. Most (83%) were caught in the lower half of the water column, but not on the river bottom. The vertical distributions of gravid and spent fish were similar for both males and females. American shad showed no diel, seasonal, or yearly changes in depth distributions. Larger gravid fish swam deeper in the water column than did smaller gravid fish.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1990)119<0151:NVDOAA>2.3.CO;2","usgsCitation":"Witherell, D.B., and Kynard, B., 1990, Vertical distribution of adult American shad in the Connecticut River: Transactions of the American Fisheries Society, v. 119, no. 1, p. 151-155, https://doi.org/10.1577/1548-8659(1990)119<0151:NVDOAA>2.3.CO;2.","productDescription":"5 p.","startPage":"151","endPage":"155","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"119","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6020a2","contributors":{"authors":[{"text":"Witherell, David B.","contributorId":98169,"corporation":false,"usgs":false,"family":"Witherell","given":"David","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":320718,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kynard, Boyd","contributorId":84234,"corporation":false,"usgs":true,"family":"Kynard","given":"Boyd","affiliations":[],"preferred":false,"id":320717,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70186696,"text":"70186696 - 1990 - Interpreting Yosemite geology: the role of the United States Geological Survey","interactions":[],"lastModifiedDate":"2017-04-07T11:00:26","indexId":"70186696","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Interpreting Yosemite geology: the role of the United States Geological Survey","docAbstract":"No abstract available
","largerWorkTitle":"Yosemite centennial symposium proceedings: natural areas and Yosemite: prospects for the future","conferenceTitle":"17th Annual Natural Areas Conference","conferenceDate":"13-20 October 1990","language":"English","usgsCitation":"Huber, N., 1990, Interpreting Yosemite geology: the role of the United States Geological Survey, in Yosemite centennial symposium proceedings: natural areas and Yosemite: prospects for the future, 13-20 October 1990, p. 523-524.","productDescription":"2 p. ","startPage":"523","endPage":"524","costCenters":[],"links":[{"id":339411,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58e8a554e4b09da6799d6422","contributors":{"authors":[{"text":"Huber, N.K.","contributorId":73610,"corporation":false,"usgs":true,"family":"Huber","given":"N.K.","affiliations":[],"preferred":false,"id":690304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014611,"text":"1014611 - 1990 - Gas transfer within a multi-stage packed column oxygen absorber: Model development and application","interactions":[],"lastModifiedDate":"2023-08-09T15:39:11.113728","indexId":"1014611","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":852,"text":"Aquacultural Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Gas transfer within a multi-stage packed column oxygen absorber: Model development and application","docAbstract":"A packed column oxygen obsorber was developed in which oxygen flow is directed, in serial reuse, through parallel packed column stages receiving equal portions of the liquid being treated. The relative performance of the absorber was established using a computer simulation program employing finite difference-mass transfer calculations. The program was calibrated using packing specific mass transfer coefficients derived from pilot scale test data. A separate series of tests served to verify model assumptions and performance predictions. Simulation data indicated multi-stage operation can substantially reduce the column height required to achieve a selected oxygen absorption efficiency (AE); for example, the column height required to achieve an AE of 76·5% with an inlet volumetric oxygenwater ratio of 0·008 (column packing, 3·81 cm plastic ACTIFIL®; water temperature, 20°C; influent dissolved oxygen, 9·08 mg/litre; operating pressure (absolute), 760 mm Hg) was 0·27 m using a 10-stage system versus 1·39 m using a single-stage absorber. Reductions in column height achieved were related to oxygen and water feed rates, number of stages employed, mass transfer characteristics of the column packing used, and concentrations of dissolved gases in the liquid being treated.
","language":"English","publisher":"Elsevier","doi":"10.1016/0144-8609(90)90010-W","usgsCitation":"Watten, B.J., and Boyd, C.E., 1990, Gas transfer within a multi-stage packed column oxygen absorber: Model development and application: Aquacultural Engineering, v. 9, no. 1, p. 33-59, https://doi.org/10.1016/0144-8609(90)90010-W.","productDescription":"27 p.","startPage":"33","endPage":"59","numberOfPages":"27","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131831,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b12f9","contributors":{"authors":[{"text":"Watten, Barnaby J. 0000-0002-2227-8623 bwatten@usgs.gov","orcid":"https://orcid.org/0000-0002-2227-8623","contributorId":2002,"corporation":false,"usgs":true,"family":"Watten","given":"Barnaby","email":"bwatten@usgs.gov","middleInitial":"J.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":320730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boyd, Claude E.","contributorId":192710,"corporation":false,"usgs":false,"family":"Boyd","given":"Claude","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":320731,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1013299,"text":"1013299 - 1990 - Computer-aided procedure for counting waterfowl on aerial photographs","interactions":[],"lastModifiedDate":"2017-11-18T09:36:09","indexId":"1013299","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3779,"text":"Wildlife Society Bulletin","onlineIssn":"1938-5463","printIssn":"0091-7648","active":true,"publicationSubtype":{"id":10}},"title":"Computer-aided procedure for counting waterfowl on aerial photographs","docAbstract":"Examination of 46 Canada goose goslings yielded 14 species of parasites, including five Protozoa, four Nematoda, two Cestoda, and three Trematoda. Evidence indicates that goslings acquired most of these infections during their first week of life. Some parasites, Prosthogonimus sp., occurred only in younger birds. Others, Leucocytozoon simondi, were evident only during the initial course of infection, while still others remained evident in older geese. Parasites with a direct life cycle appeared to be more prevalent than those requiring intermediate hosts. Among 29 birds from a refuge in Michigan, 14 species of parasites were found; while in 17 goslings from a Utah refuge, only five species occurred.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wildlife Society Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Bajzak, D., and Piatt, J.F., 1990, Computer-aided procedure for counting waterfowl on aerial photographs: Wildlife Society Bulletin, v. 18, no. 2, p. 125-129.","productDescription":"pp. 125-129","startPage":"125","endPage":"129","numberOfPages":"5","costCenters":[{"id":106,"text":"Alaska Biological Science Center","active":false,"usgs":true}],"links":[{"id":131861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a637b","contributors":{"authors":[{"text":"Bajzak, D.","contributorId":45262,"corporation":false,"usgs":true,"family":"Bajzak","given":"D.","email":"","affiliations":[],"preferred":false,"id":318575,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Piatt, John F. 0000-0002-4417-5748 jpiatt@usgs.gov","orcid":"https://orcid.org/0000-0002-4417-5748","contributorId":3025,"corporation":false,"usgs":true,"family":"Piatt","given":"John","email":"jpiatt@usgs.gov","middleInitial":"F.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":117,"text":"Alaska Science Center Biology WTEB","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":318576,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1014642,"text":"1014642 - 1990 - Effects of ozonated-water reuse on salinity tolerance of Atlantic salmon","interactions":[],"lastModifiedDate":"2025-07-24T15:44:03.533462","indexId":"1014642","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","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":"Effects of ozonated-water reuse on salinity tolerance of Atlantic salmon","docAbstract":"We conducted several seasonal aquarium experiments to determine survival and body chemistry changes of Atlantic salmon (Salmo salar) after 24‐h exposures to salinities of 0, 16.5, 33, and 40‰ at 10°C. Fish transferred directly to test aquaria from an ozonated, 100‰ closed water‐reuse system at 18°C were compared with fish acclimated to single‐use water at 10°C for 1–3 weeks before salinity challenges in solutions of sea salt. In the initial (December and January) challenges, all Atlantic salmon from the closed system with a fork length of at least 200 mm survived exposure to 16.5 and 33‰ salinity, but not 40‰; fish 135 mm long or shorter did not survive exposure to 33‰ salinity. In later experiments, prior acclimation of fish to single‐use water at 10°C helped protect them against exposure to high salinity (i.e., 33 and 40‰) at 10°C. Few fish that were moved directly from the water‐reuse system into test aquaria lived for 24 h in 33 or 40‰ salinity. Atlantic salmon contained less water at 33‰ than at 16.5‰ or in fresh water, but carcass water content did not differ within salinity treatments between fish previously held at 18°C and those acclimated to 10°C and single‐use water. At each salinity, serum sodium concentration tended to rise less in those fish acclimated to the singleuse system than in those transferred directly from the reuse system to the aquaria. The exposure of Atlantic salmon to an elevated acclimation temperature (18°C) in the water‐reuse system exacerbated the disruption of their ionic exchange at exposures to 33 and 40‰ sea salt. A trace of copper (27 μg/L) in the reused water also may have reduced the salinity tolerance of these fish.
","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8640(1990)052%3C0036:EOOWRO%3E2.3.CO;2","usgsCitation":"Poston, H.A., and Williams, R., 1990, Effects of ozonated-water reuse on salinity tolerance of Atlantic salmon: Progressive Fish-Culturist, v. 52, no. 1, p. 36-40, https://doi.org/10.1577/1548-8640(1990)052%3C0036:EOOWRO%3E2.3.CO;2.","productDescription":"5 p.","startPage":"36","endPage":"40","numberOfPages":"5","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132034,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aeb26","contributors":{"authors":[{"text":"Poston, H. A.","contributorId":21893,"corporation":false,"usgs":true,"family":"Poston","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":320800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, R.C.","contributorId":103621,"corporation":false,"usgs":true,"family":"Williams","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":320801,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1014613,"text":"1014613 - 1990 - Modeling the effects of serial off-gas reuse on the performance of a hooded surface oxygen obsorption system","interactions":[],"lastModifiedDate":"2023-08-09T15:44:56.110048","indexId":"1014613","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":852,"text":"Aquacultural Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Modeling the effects of serial off-gas reuse on the performance of a hooded surface oxygen obsorption system","docAbstract":"A numerical model was used to evaluate the performance of a surface agitation system designed to contact commercial oxygen with water. The modeled system was unique in that oxygen-rich off-gas, normally discharged to the atmosphere, was directed in serial reuse through additional contact stages receiving untreated water. A correlation between the agitator mass-transfer coefficient and power demand, needed to calibrate the model, was established using a single-stage (37 W) contactor of 1·18 m3 capacity. Additional tests, conducted with both single and three-stage equipment, verified model assumptions and performance predictions. Simulation runs indicated oxygen flow or power input required to meet a given effluent dissolved gas criterion can be substantially reduced by the off-gas reuse step; for example, to achieve an effluent dissolved oxygen of 24·1 mg/litre with a single stage agitator the oxygen feed rate needed was 61·5% greater than that required by a six-stage system receiving the same total power input (standard aeration efficiency, 0·5 kg/kW h; water flow rate, 100 litre/min; influent dissolved oxygen, 9·08 mg/litre at 15°C). The savings achieved increased with (1) greater target effluent dissolved oxygen concentrations, (2) lower oxygen feed rates, (3) higher input power levels, and (4) number of contact stages.
","language":"English","publisher":"Elsevier","doi":"10.1016/0144-8609(90)90014-Q","usgsCitation":"Watten, B.J., Meade, J.W., and Boyd, C.E., 1990, Modeling the effects of serial off-gas reuse on the performance of a hooded surface oxygen obsorption system: Aquacultural Engineering, v. 9, no. 2, p. 97-120, https://doi.org/10.1016/0144-8609(90)90014-Q.","productDescription":"24 p.","startPage":"97","endPage":"120","numberOfPages":"24","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131832,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699794","contributors":{"authors":[{"text":"Watten, Barnaby J. 0000-0002-2227-8623 bwatten@usgs.gov","orcid":"https://orcid.org/0000-0002-2227-8623","contributorId":2002,"corporation":false,"usgs":true,"family":"Watten","given":"Barnaby","email":"bwatten@usgs.gov","middleInitial":"J.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":true,"id":320732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meade, J. W.","contributorId":38082,"corporation":false,"usgs":true,"family":"Meade","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":320733,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Boyd, Claude E.","contributorId":192710,"corporation":false,"usgs":false,"family":"Boyd","given":"Claude","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":320734,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70180759,"text":"70180759 - 1990 - Management implications of a model of predation by a resident fish on juvenile salmonids migrating through a Columbia River reservoir","interactions":[],"lastModifiedDate":"2017-02-02T12:20:13","indexId":"70180759","displayToPublicDate":"1990-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2886,"text":"North American Journal of Fisheries Management","active":true,"publicationSubtype":{"id":10}},"title":"Management implications of a model of predation by a resident fish on juvenile salmonids migrating through a Columbia River reservoir","docAbstract":"We constructed a model ofpredation by northern squawfish Ptychocheilus oregonensis on juvenile salmonids migrating through John Day Reservoir. The model predicts salmonid survival as a function of number and distribution of northern squawfish, number and timing of juvenile salmonids entering the reservoir, salmonid residence time, water temperature, and flow. The model predicted survival similar to independent estimates for 1983–1986 and also approximated differences among areas and months. Uncertainty analyses showed that the number of salmonids surviving predation may vary ±5% with normal annual variation in predator number, temperature, and flow. Survival in 1983–1986 was near the average predicted from 30 years of historic environmental data. Sensitivity analyses implied that the best avenues ofreducing predation are to reduce the number of northern squawfish, pass salmonids earlier in the year, and maintain sizes of runs of juvenile salmonids at or above present levels. Survival of salmonids, as simulated by the model, is weakly affected by changes in predator distribution, changes in predator consumption rate near the upstream dam, residence time, or flow.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8675(1990)010<0290:MIOAMO>2.3.CO;2","usgsCitation":"Beamesderfer, R.C., Rieman, B.E., Bledsoe, L.J., and Vigg, S., 1990, Management implications of a model of predation by a resident fish on juvenile salmonids migrating through a Columbia River reservoir: North American Journal of Fisheries Management, v. 10, no. 3, p. 290-304, https://doi.org/10.1577/1548-8675(1990)010<0290:MIOAMO>2.3.CO;2.","productDescription":"15 p. ","startPage":"290","endPage":"304","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":334607,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58945339e4b0fa1e59b86835","contributors":{"authors":[{"text":"Beamesderfer, Raymond C.","contributorId":179031,"corporation":false,"usgs":false,"family":"Beamesderfer","given":"Raymond","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":662338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rieman, Bruce E.","contributorId":107420,"corporation":false,"usgs":true,"family":"Rieman","given":"Bruce","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":662339,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bledsoe, Lewis J.","contributorId":179044,"corporation":false,"usgs":false,"family":"Bledsoe","given":"Lewis","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":662340,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Vigg, Steven","contributorId":179032,"corporation":false,"usgs":false,"family":"Vigg","given":"Steven","email":"","affiliations":[],"preferred":false,"id":662341,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}