The magnitude 7.1 mainshock on April 25, 992, caused substantial changes in the elevation of the Earth's surface in the Cape Mendocino region. Precise measurements of such elevation changes aid in long-term emergency planning and are needed for engineering design and the maintenance of roads, bridges, and waterways. Such measurements also enable researchers to estimate the attitude and slip of the causative fault.
\nElevation changes, as well as horizontal displacements of the Earth's surface, are an expected consequence of dip-slip displacement on earthquake faults. the rock surrounding and overlying the fault is forced to stretch and bend to accommodate fault slip. Slip in the case of the April 25 mainshock is thought to have occurred on a gently inclined plane dipping to the northeast at a small angle (see article on preliminary seismological results in this issue).The associated fault-plane solution implies that rock overlying the fault plane (the hanging-wall block west and south of the epicenter) rose and shifted to the northeast. The map on the next page shows the location of the epicenter and approximate extent of uplift and subsidence derived from estimates of the geometry, location. and slip on the buried fault plane.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Jayko, A., Marshall, G., and Carver, G.A., 1992, Elevation changes: Earthquakes & Volcanoes (USGS), v. 23, no. 3, p. 139-143.","productDescription":"5 p.","startPage":"139","endPage":"143","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":315005,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Cape Mendocino","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.6785888671875,\n 40.62646106367355\n ],\n [\n -124.8486328125,\n 40.60561205826018\n ],\n [\n -123.9752197265625,\n 38.93377552819722\n ],\n [\n -122.9754638671875,\n 39.11727568585595\n ],\n [\n -123.629150390625,\n 40.622291783092706\n ],\n [\n -123.6785888671875,\n 40.62646106367355\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ab49c4e4b07ca61bfea52b","contributors":{"authors":[{"text":"Jayko, A. S.","contributorId":118738,"corporation":false,"usgs":true,"family":"Jayko","given":"A. S.","affiliations":[],"preferred":false,"id":590118,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marshall, G.A.","contributorId":42615,"corporation":false,"usgs":true,"family":"Marshall","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":590119,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Carver, G. A.","contributorId":80762,"corporation":false,"usgs":false,"family":"Carver","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":590120,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70162666,"text":"70162666 - 1992 - The Cape Mendocino tsunami","interactions":[],"lastModifiedDate":"2016-02-11T16:19:42","indexId":"70162666","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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 Cape Mendocino tsunami","docAbstract":"The Cape Mendocino earthquake of April 25, 1992, generated a tsunami recorded by NOAA (National Oceanic and Atmospheric Administration) sea level gauges in California, Oregon, and Hawaii. The accompanying figure shows the tsunami waveforms acquired at twelve of these stations. the table that follows identifies these stations and gives preliminary estimates of the tsunami travel time from the source region to selected West Coast stations.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Gonzalez, F., and Bernard, E.N., 1992, The Cape Mendocino tsunami: Earthquakes & Volcanoes (USGS), v. 23, no. 3, p. 135-138.","productDescription":"4 p.","startPage":"135","endPage":"138","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314992,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Cape Mendocino","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.288330078125,\n 41.95131994679697\n ],\n [\n -125.05737304687499,\n 41.795888098191426\n ],\n [\n -124.98046874999999,\n 39.78321267821705\n ],\n [\n -123.93676757812499,\n 39.740986355883564\n ],\n [\n -123.99169921875,\n 41.03793062246529\n ],\n [\n -123.85986328124999,\n 41.6154423246811\n ],\n [\n -124.112548828125,\n 41.97582726102573\n ],\n [\n -124.288330078125,\n 41.95131994679697\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ab49d5e4b07ca61bfea5f8","contributors":{"authors":[{"text":"Gonzalez, F.I.","contributorId":68100,"corporation":false,"usgs":true,"family":"Gonzalez","given":"F.I.","email":"","affiliations":[],"preferred":false,"id":590099,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bernard, E. N.","contributorId":152671,"corporation":false,"usgs":false,"family":"Bernard","given":"E.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":590100,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70168821,"text":"70168821 - 1992 - The 1992 Landers earthquake and surface faulting","interactions":[],"lastModifiedDate":"2016-09-19T14:46:50","indexId":"70168821","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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 1992 Landers earthquake and surface faulting","docAbstract":"Faulting associated with the June 28, 992, earthquake near Landers, California, broke the surface of the ground over a length of more than 70 km, the longest surface rupture in the United States since the great San Francisco quake of 1906. the strongest shaking associated with this magnitude 7.6 (MS) earthquake, the largest in the contiguous 48 states in the last 40 years, occurred in a sparsely populated sections of the Mojave Desert more than 200 km east of Los Angeles. the earthquake began with a sudden slip on the Johnson Valley fault about 10 km southwest of Landers. The initial fault movement probably occurred at a depth of less than 10 km. Surface faulting then propagated over 70 km to the north and northeast. The faulting linked preexisting faults-some previously known and mapped and others previously unknown-into a complex, coherent rupture zone.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Rymer, M.J., 1992, The 1992 Landers earthquake and surface faulting: Earthquakes & Volcanoes (USGS), v. 23, no. 5, p. 209-218.","productDescription":"10 p.","startPage":"209","endPage":"218","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318547,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Landers","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.1746826171875,\n 34.768691457552706\n ],\n [\n -116.15295410156249,\n 34.76192255039478\n ],\n [\n -115.96343994140625,\n 33.51849923765608\n ],\n [\n -117.158203125,\n 33.53681606773302\n ],\n [\n -117.1746826171875,\n 34.768691457552706\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"23","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56d96e5fe4b015c306f764ce","contributors":{"authors":[{"text":"Rymer, Michael J. mrymer@usgs.gov","contributorId":1522,"corporation":false,"usgs":true,"family":"Rymer","given":"Michael","email":"mrymer@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":621852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162674,"text":"70162674 - 1992 - Hazards of geomagnetic storms","interactions":[],"lastModifiedDate":"2016-02-16T14:15:11","indexId":"70162674","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"Hazards of geomagnetic storms","docAbstract":"Geomagnetic storms are large and sometimes rapid fluctuations in the Earth's magnetic field that are related to disturbances on the Sun's surface. Although it is not widely recognized, these transient magnetic disturbances can be a significant hazard to people and property. Many of us know that the intensity of the auroral lights increases during magnetic storms, but few people realize that these storms can also cause massive power outages, interrupt radio communications and satellite operations, increase corrosion in oil and gas pipelines, and lead to spuriously high rejection rates in the manufacture of sensitive electronic equipment.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Herzog, D., 1992, Hazards of geomagnetic storms: Earthquakes & Volcanoes (USGS), v. 23, no. 4, p. 152-159.","productDescription":"8 p.","startPage":"152","endPage":"159","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318081,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ab49c6e4b07ca61bfea553","contributors":{"authors":[{"text":"Herzog, D.C.","contributorId":46696,"corporation":false,"usgs":true,"family":"Herzog","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":590111,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70162672,"text":"70162672 - 1992 - Natural hazards research and response; international decade for reducing loss from natural disasters","interactions":[],"lastModifiedDate":"2016-02-11T16:48:39","indexId":"70162672","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"Natural hazards research and response; international decade for reducing loss from natural disasters","docAbstract":"Worldwide losses from natural disasters are increasing rapidly due to population growth, urban sprawl, and increasing concentration of new construction in high-risk areas. to deal with these problems, the United Nations has designated the 1990's as the International Decade for Natural Disaster Reduction (IDNDR). The United States and more than 150 other nations signed the IDNDR resolution at the 44th General Assembly of the United Nations. The resolution calls on all nations to develop programs to reduce loss of life, economic impact, and human suffering caused by natural disasters.
\nIDNDR offers an unprecedented opportunity to apply new knowledge and technology to minimize losses in regions at high risks. The program is very challenging because full implementation requires a multidisciplinary effort on a global scale, an undertaking never before attempted. In concert with the other signatory nations, the Untied States is carrying out a balanced and comprehensive program of research and applications as a contribution to the IDNDR. The U.S program is designed to reduce both loss of life and property damage from natural disasters.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Hays, W.W., 1992, Natural hazards research and response; international decade for reducing loss from natural disasters: Earthquakes & Volcanoes (USGS), v. 23, no. 6, p. 268-273.","productDescription":"6 p.","startPage":"268","endPage":"273","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":314998,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56ab49cde4b07ca61bfea598","contributors":{"authors":[{"text":"Hays, W. W.","contributorId":66693,"corporation":false,"usgs":true,"family":"Hays","given":"W.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":590107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70168760,"text":"70168760 - 1992 - Earthquakes, May-June 1991","interactions":[],"lastModifiedDate":"2016-03-01T14:52:44","indexId":"70168760","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","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":"Earthquakes, May-June 1991","docAbstract":"One major earthquake occurred during this reporting period. This was a magntidue 7.1 in Indonesia (Minahassa Peninsula) on June 20. Earthquake-related deaths were reported in the Western Caucasus (Georgia, USSR) on May 3 and June 15. One earthquake-related death was also reported El Salvador on June 21.
\nIn the United States, a magnitude 5.8 earthquake in southern California on June 28 killed two people and caused considerable damage. Strong earthquakes hit Alaska on May 1 and May 30; the May 1 earthquake caused some minor damage.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1992, Earthquakes, May-June 1991: Earthquakes & Volcanoes (USGS), v. 23, no. 2, p. 77-81.","productDescription":"5 p.","startPage":"77","endPage":"81","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318465,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56d6cb55e4b015c306f32cc5","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621653,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70186621,"text":"70186621 - 1992 - Site investigations: a review of studies of contaminated groundwater conducted by the U.S. geological survey organics project, Menlo Park, California, 1961-1990","interactions":[],"lastModifiedDate":"2017-04-06T11:21:06","indexId":"70186621","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Site investigations: a review of studies of contaminated groundwater conducted by the U.S. geological survey organics project, Menlo Park, California, 1961-1990","docAbstract":"No abstract available
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Groundwater contamination and analysis at hazardous waste sites","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","usgsCitation":"Goerlitz, D., 1992, Site investigations: a review of studies of contaminated groundwater conducted by the U.S. geological survey organics project, Menlo Park, California, 1961-1990, chap. of Groundwater contamination and analysis at hazardous waste sites, p. 295-355.","productDescription":"61 p. ","startPage":"295","endPage":"355","costCenters":[],"links":[{"id":339307,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58e7540be4b09da6799c0caa","contributors":{"authors":[{"text":"Goerlitz, D.F.","contributorId":8445,"corporation":false,"usgs":true,"family":"Goerlitz","given":"D.F.","affiliations":[],"preferred":false,"id":690072,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70185784,"text":"70185784 - 1992 - Synthetic organic agrochemicals in the lower Mississippi River and its major tributaries--Distribution, transport and fate","interactions":[],"lastModifiedDate":"2019-03-19T09:30:50","indexId":"70185784","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2233,"text":"Journal of Contaminant Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Synthetic organic agrochemicals in the lower Mississippi River and its major tributaries--Distribution, transport and fate","docAbstract":"The Mississippi River and its major tributaries transport herbicides and their degradation products from agricultural areas in the mid-western U.S.A. These compounds include atrazine and its degradation products (desethyl- and desisopropylatrazine), simazine, cyanazine, metolachlor, and alachlor and its degradation products (2-chloro-2′,6′-diethylacetanilide 2-hydroxy-2′,6′-diethylacetanilide and 2,6-diethylaniline). These compounds were identified and confirmed by gas chromatography-ion trap mass spectrometry. Loads of these compounds were determined during five sampling trips in 1987–1989. Stream loads of these compounds indicated that atrazine and metolachlor were relatively conservative in downstream transport. Alachlor and its degradation products were generated from point and non-point sources. Seasonal variations and hydrologic conditions controlled the loads of these compounds in the Mississippi River. Cross-channel mixing was slow downstream from major river confluences, possibly requiring several hundred kilometers of downriver transit for completion. The annual transport of these compounds into the Gulf of Mexico was estimated to be < 2% of the annual application of each herbicide in the Midwest.
","language":"English","publisher":"Elsevier","doi":"10.1016/0169-7722(92)90057-L","usgsCitation":"Pereira, W.E., Rostad, C., and Leiker, T., 1992, Synthetic organic agrochemicals in the lower Mississippi River and its major tributaries--Distribution, transport and fate: Journal of Contaminant Hydrology, v. 9, no. 1-2, p. 175-188, https://doi.org/10.1016/0169-7722(92)90057-L.","productDescription":"14 p.","startPage":"175","endPage":"188","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338525,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58dcc81ee4b02ff32c685726","contributors":{"authors":[{"text":"Pereira, W. E.","contributorId":46981,"corporation":false,"usgs":true,"family":"Pereira","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":686731,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rostad, C.E.","contributorId":50939,"corporation":false,"usgs":true,"family":"Rostad","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":686732,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leiker, T.J.","contributorId":96719,"corporation":false,"usgs":true,"family":"Leiker","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":686733,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70186915,"text":"70186915 - 1992 - Saltwater intrusion into fresh ground-water supplies, southern Cape May County, New Jersey, 1890-1991","interactions":[],"lastModifiedDate":"2017-04-13T19:24:45","indexId":"70186915","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Saltwater intrusion into fresh ground-water supplies, southern Cape May County, New Jersey, 1890-1991","docAbstract":"No abstract available
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the national symposium on the future availability of ground water resources","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","usgsCitation":"Lacombe, P., and Carleton, G., 1992, Saltwater intrusion into fresh ground-water supplies, southern Cape May County, New Jersey, 1890-1991, in Proceedings of the national symposium on the future availability of ground water resources, p. 287-297.","productDescription":"11 p.","startPage":"287","endPage":"297","costCenters":[],"links":[{"id":339718,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58f08e65e4b06911a29fa87e","contributors":{"authors":[{"text":"Lacombe, P.J.","contributorId":67915,"corporation":false,"usgs":true,"family":"Lacombe","given":"P.J.","email":"","affiliations":[],"preferred":false,"id":690986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carleton, G.B.","contributorId":107729,"corporation":false,"usgs":true,"family":"Carleton","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":690987,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70186631,"text":"70186631 - 1992 - Volcanoes of Alaska: Kupreanof (Stepovak Bay)","interactions":[],"lastModifiedDate":"2017-04-06T12:15:59","indexId":"70186631","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Volcanoes of Alaska: Kupreanof (Stepovak Bay)","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Volcanoes of North America: United States and Canada","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Cambridge University Press","isbn":"9780521438117","usgsCitation":"Wilson, F.H., 1992, Volcanoes of Alaska: Kupreanof (Stepovak Bay), chap. of Volcanoes of North America: United States and Canada, p. 55-56.","productDescription":"2 p.","startPage":"55","endPage":"56","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":339321,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":339320,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.cambridge.org/us/academic/subjects/earth-and-environmental-science/mineralogy-petrology-and-volcanology/volcanoes-north-america-united-states-and-canada?format=PB"}],"country":"United States","state":"Alaska","otherGeospatial":"Kupreanof, Stepovak Bay","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58e7540ae4b09da6799c0ca8","contributors":{"editors":[{"text":"Wood, Charles A.","contributorId":27599,"corporation":false,"usgs":true,"family":"Wood","given":"Charles","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":690099,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Kienle, Juergen","contributorId":45343,"corporation":false,"usgs":true,"family":"Kienle","given":"Juergen","email":"","affiliations":[],"preferred":false,"id":690100,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":690098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70187312,"text":"70187312 - 1992 - Lower Cretaceous smarl turbidites of the Argo Abyssal Plain, Indian Ocean","interactions":[],"lastModifiedDate":"2018-05-07T21:18:03","indexId":"70187312","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":5640,"text":"Proceedings of the Ocean Drilling Program: Scientific Results","onlineIssn":"1096-7451","printIssn":"0884-5891","active":true,"publicationSubtype":{"id":3}},"seriesNumber":"123","chapter":"5","title":"Lower Cretaceous smarl turbidites of the Argo Abyssal Plain, Indian Ocean","docAbstract":"Sediments recovered during Ocean Drilling Program (ODP) Leg 123 from the Argo Abyssal Plain (AAP) consist largely of turbidites derived from the adjacent Australian continental margin. The oldest abundant turbidites are Valanginian-Aptian in age and have a mixed (smarl) composition; they contain subequal amounts of calcareous and siliceous biogenic components, as well as clay and lesser quartz. Most are thin-bedded, fine sand to mud-sized, and best described by Stow and Piper's model (1984) for fine-grained biogenic turbidites. Thicker (to 3 m), coarser-grained (medium-to-coarse sand-sized) turbidites fit Bouma's model (1962) for sandy turbidites; these generally are base-cut-out (BCDE, BDE) sequences, with B-division parallel lamination as the dominant structure. Parallel laminae most commonly concentrate quartz and/or calcispheres vs. lithic clasts or clay, but distinctive millimeter to centimeter-thick, radiolarian-rich laminae occur in both fine and coarse-grained Valanginian-Hauterivian turbidites.
AAP turbidites were derived from relatively deep parts of the continental margin (outer shelf, slope, or rise) that lay below the photic zone, but above the calcite compensation depth (CCD). Biogenic components are largely pelagic (calcispheres, foraminifers, radiolarians, nannofossils); lesser benthic foraminifers are characteristic of deep-water (abyssal to bathyal) environments. Abundant nonbiogenic components are mostly clay and clay clasts; smectite is the dominant clay species, and indicates a volcanogenic provenance, most likely the Triassic-Jurassic volcanic suite exposed along the northern Exmouth Plateau.
Lower Cretaceous smarl turbidites were generated during eustatic lowstands and may have reached the abyssal plain via Swan Canyon, a submarine canyon thought to have formed during the Late Jurassic. In contrast to younger AAP turbidites, however, Lower Cretaceous turbidites are relatively fine-grained and do not contain notably older reworked fossils. Early in its history, the northwest Australian margin provided mainly contemporaneous slope sediment to the AAP; marginal basins adjacent to the continent trapped most terrigenous detritus, and pronounced canyon incisement did not occur until Late Cretaceous and, especially, Cenozoic time.
","language":"English","publisher":"Ocean Drilling Program, Texas A&M University","publisherLocation":"College Station, TX","doi":"10.2973/odp.proc.sr.123.154.1992","usgsCitation":"Dumoulin, J.A., 1992, Lower Cretaceous smarl turbidites of the Argo Abyssal Plain, Indian Ocean: Proceedings of the Ocean Drilling Program: Scientific Results 123, v. 123, 25 p., https://doi.org/10.2973/odp.proc.sr.123.154.1992.","productDescription":"25 p.","startPage":"111","endPage":"135","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":488639,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/odp.proc.sr.123.154.1992","text":"Publisher Index Page"},{"id":340546,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Argo Abyssal Plain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 123,\n -21\n ],\n [\n 112,\n -21\n ],\n [\n 112,\n -10\n ],\n [\n 123,\n -10\n ],\n [\n 123,\n -21\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"123","publicComments":"Volume topic: Argo Abyssal Plain/Exmouth Plateau, covering Leg 123 of the cruises of the Drilling Vessel JOIDES Resolution, Singapore, Republic of Sing., to Singapore, Republic of Sing., Sites 765-766, 28 August 1988 - 1 November 1988","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59030339e4b0e862d230f7f8","contributors":{"editors":[{"text":"Stewart, Sondra K.","contributorId":117324,"corporation":false,"usgs":false,"family":"Stewart","given":"Sondra","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":730033,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Kennett, Diana","contributorId":27521,"corporation":false,"usgs":false,"family":"Kennett","given":"Diana","email":"","affiliations":[],"preferred":false,"id":730050,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Mazzullo, Elsa K.","contributorId":60618,"corporation":false,"usgs":false,"family":"Mazzullo","given":"Elsa","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":730051,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Dumoulin, Julie A. 0000-0003-1754-1287 dumoulin@usgs.gov","orcid":"https://orcid.org/0000-0003-1754-1287","contributorId":203209,"corporation":false,"usgs":true,"family":"Dumoulin","given":"Julie","email":"dumoulin@usgs.gov","middleInitial":"A.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":693303,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70185460,"text":"70185460 - 1992 - Reply to comment by G. de Marsily, P. Combes, and P. Goblet on \"Ground-water models cannot be validated\"","interactions":[],"lastModifiedDate":"2019-03-14T06:09:28","indexId":"70185460","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":664,"text":"Advances in Water Resources","active":true,"publicationSubtype":{"id":10}},"title":"Reply to comment by G. de Marsily, P. Combes, and P. Goblet on \"Ground-water models cannot be validated\"","docAbstract":"No abstract available.
","language":"English","publisher":"Elsevier","doi":"10.1016/0309-1708(92)90004-L","usgsCitation":"Bredehoeft, J., and Konikow, L.F., 1992, Reply to comment by G. de Marsily, P. Combes, and P. Goblet on \"Ground-water models cannot be validated\": Advances in Water Resources, v. 15, no. 6, p. 371-372, https://doi.org/10.1016/0309-1708(92)90004-L.","productDescription":"2 p. ","startPage":"371","endPage":"372","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338050,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d38d60e4b0236b68f98f74","contributors":{"authors":[{"text":"Bredehoeft, J.D.","contributorId":12836,"corporation":false,"usgs":true,"family":"Bredehoeft","given":"J.D.","affiliations":[],"preferred":false,"id":685634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Konikow, Leonard F. 0000-0002-0940-3856 lkonikow@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-3856","contributorId":158,"corporation":false,"usgs":true,"family":"Konikow","given":"Leonard","email":"lkonikow@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":759261,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185761,"text":"70185761 - 1992 - Associations of free-living bacteria and dissolved organic compounds in a plume of contaminated groundwater","interactions":[],"lastModifiedDate":"2019-03-19T08:20:40","indexId":"70185761","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2233,"text":"Journal of Contaminant Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Associations of free-living bacteria and dissolved organic compounds in a plume of contaminated groundwater","docAbstract":"Associations of free-living bacteria (FLB) and dissolved organic contaminants in a 4-km-long plume of sewage-contaminated groundwater were investigated. Abundance of FLB in the core of the plume (as delineated by maximum specific conductance) steadily decreased in the direction of flow from a point 0.25 km downgradient from the source to the toe of the plume. At 0.25 km downgradient, FLB comprised up to 31% of the total bacterial population, but constituted <7% of the population at 2 km downgradient. Abundance of FLB correlated strongly (r = 0.80, n = 23) with total dissolved organic carbon (DOC) in contaminated groundwater between 0.64 and 2.1 km downgradient, although distributions of individual contaminants such as di-, tri- and tetrachloroethene were highly variable, and their association with FLB less clear. Numbers of FLB in the downgradient portion of the plume which is contaminated with branched-chain alkylbenzenesulfonate (ABS) surfactants were low (<5 · 108/L) in spite of relatively high levels of DOC (up to 4 mg/L). However, abundance of FLB correlated strongly with non-surfactant DOC along vertical transects through the plume. The ratio of FLB to DOC and the ratio of FLB to attached bacteria generally decreased in the direction of flow and, consequently, with the age of the organic contaminants.
","language":"English","publisher":"Elsevier","doi":"10.1016/0169-7722(92)90052-G","usgsCitation":"Harvey, R.W., and Barber, L.B., 1992, Associations of free-living bacteria and dissolved organic compounds in a plume of contaminated groundwater: Journal of Contaminant Hydrology, v. 9, no. 1-2, p. 91-103, https://doi.org/10.1016/0169-7722(92)90052-G.","productDescription":"23 p. ","startPage":"91","endPage":"103","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338508,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58db7639e4b0ee37af29e4ee","contributors":{"authors":[{"text":"Harvey, Ronald W. 0000-0002-2791-8503 rwharvey@usgs.gov","orcid":"https://orcid.org/0000-0002-2791-8503","contributorId":564,"corporation":false,"usgs":true,"family":"Harvey","given":"Ronald","email":"rwharvey@usgs.gov","middleInitial":"W.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":686693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barber, Larry B. II","contributorId":189675,"corporation":false,"usgs":false,"family":"Barber","given":"Larry","suffix":"II","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":686694,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70186441,"text":"70186441 - 1992 - Change-in-ratio methods for estimating population size","interactions":[],"lastModifiedDate":"2018-08-01T11:04:55","indexId":"70186441","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Change-in-ratio methods for estimating population size","docAbstract":"Change-in-ratio (CIR) methods can provide an effective, low cost approach for estimating the size of wildlife populations. They rely on being able to observe changes in proportions of population subclasses that result from the removal of a known number of individuals from the population. These methods were first introduced in the 1940’s to estimate the size of populations with 2 subclasses under the assumption of equal subclass encounter probabilities. Over the next 40 years, closed population CIR models were developed to consider additional subclasses and use additional sampling periods. Models with assumptions about how encounter probabilities vary over time, rather than between subclasses, also received some attention. Recently, all of these CIR models have been shown to be special cases of a more general model. Under the general model, information from additional samples can be used to test assumptions about the encounter probabilities and to provide estimates of subclass sizes under relaxations of these assumptions. These developments have greatly extended the applicability of the methods. CIR methods are attractive because they do not require the marking of individuals, and subclass proportions often can be estimated with relatively simple sampling procedures. However, CIR methods require a carefully monitored removal of individuals from the population, and the estimates will be of poor quality unless the removals induce substantial changes in subclass proportions. In this paper, we review the state of the art for closed population estimation with CIR methods. Our emphasis is on the assumptions of CIR methods and on identifying situations where these methods are likely to be effective. We also identify some important areas for future CIR research.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Wildlife 2001: Populations","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","isbn":"978-94-011-2868-1","usgsCitation":"Udevitz, M.S., and Pollock, K.H., 1992, Change-in-ratio methods for estimating population size, chap. of Wildlife 2001: Populations, p. 90-101.","productDescription":"12 p.","startPage":"90","endPage":"101","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":339154,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":356080,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://link.springer.com/chapter/10.1007/978-94-011-2868-1_9"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58e4b0b3e4b09da6799977a1","contributors":{"editors":[{"text":"McCullough, Dale R.","contributorId":113841,"corporation":false,"usgs":true,"family":"McCullough","given":"Dale","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":688473,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Barrett, Reginald H.","contributorId":48261,"corporation":false,"usgs":true,"family":"Barrett","given":"Reginald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":688474,"contributorType":{"id":2,"text":"Editors"},"rank":2}],"authors":[{"text":"Udevitz, Mark S. 0000-0003-4659-138X mudevitz@usgs.gov","orcid":"https://orcid.org/0000-0003-4659-138X","contributorId":3189,"corporation":false,"usgs":true,"family":"Udevitz","given":"Mark","email":"mudevitz@usgs.gov","middleInitial":"S.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":688471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pollock, Kenneth H.","contributorId":8590,"corporation":false,"usgs":false,"family":"Pollock","given":"Kenneth","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":688472,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1014567,"text":"1014567 - 1992 - Hormonal control of sulfate uptake by bronchial cartilage of coho salmon: Role of IGF-I","interactions":[],"lastModifiedDate":"2024-04-30T15:15:55.156093","indexId":"1014567","displayToPublicDate":"1992-01-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2278,"text":"Journal of Experimental Zoology","active":true,"publicationSubtype":{"id":10}},"title":"Hormonal control of sulfate uptake by bronchial cartilage of coho salmon: Role of IGF-I","docAbstract":"The direct hormonal control of sulfate uptake by cartilage matrix of coho salmon was examined by exposing branchial cartilage to 1 μCi · ml−1 35SO4 for 48 hours at 15°C in a defined medium. Sulfate uptake occurred primarily in cartilage (rather than bone) and the amount of specific uptake was similar in epibranchial and ceratobranchial cartilages. Intact and hypophysectomized coho salmon starved for 22 days had equivalent in vitro sulfate uptake, which in both cases were 30% of the uptake seen in branchial cartilage of fed, intact controls. In branchial cartilage from starved coho salmon, in vitro exposure to recombinant bovine insulin-like growth factor I (rbIGF-I) at 1, 10, 100, and 1,000 ng · ml−1 caused a dose-dependent increase in sulfate uptake, with a maximum 3-fold increase over control at 1,000 ng · ml−1 rbIGF-I. Coho salmon insulin (1, 10, 100, and 1,000 ng · ml−1) resulted in a maximum 30% increase in sulfate uptake at the highest dose. Growth hormone and triiodo-L-thyronine had no direct effect on in vitro sulfate uptake. The results indicate that IGF-I has direct effects on coho salmon cartilage and may be an important regulator of growth in salmon and other teleosts.
","language":"English","publisher":"Wiley","doi":"10.1002/jez.1402620206","usgsCitation":"McCormick, S., Tsai, P., Kelley, K., Nishioka, R.S., and Bern, H.A., 1992, Hormonal control of sulfate uptake by bronchial cartilage of coho salmon: Role of IGF-I: Journal of Experimental Zoology, v. 262, no. 2, p. 166-171, https://doi.org/10.1002/jez.1402620206.","productDescription":"6 p.","startPage":"166","endPage":"171","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132322,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"262","issue":"2","noUsgsAuthors":false,"publicationDate":"2005-04-26","publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62be3c","contributors":{"authors":[{"text":"McCormick, S. D. 0000-0003-0621-6200","orcid":"https://orcid.org/0000-0003-0621-6200","contributorId":20278,"corporation":false,"usgs":true,"family":"McCormick","given":"S. D.","affiliations":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"preferred":false,"id":320626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tsai, P.I.","contributorId":100775,"corporation":false,"usgs":true,"family":"Tsai","given":"P.I.","email":"","affiliations":[],"preferred":false,"id":320630,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kelley, K.M.","contributorId":62952,"corporation":false,"usgs":true,"family":"Kelley","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":320628,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nishioka, R. S.","contributorId":69915,"corporation":false,"usgs":false,"family":"Nishioka","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":320629,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Bern, H. A.","contributorId":61771,"corporation":false,"usgs":false,"family":"Bern","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":320627,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70201439,"text":"wdrOK911 - 1992 - Water Resources Data, Oklahoma, Water Year 1991","interactions":[],"lastModifiedDate":"2021-01-26T20:47:36.870839","indexId":"wdrOK911","displayToPublicDate":"1991-01-01T10:50:08","publicationYear":"1992","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OK-91-1","title":"Water Resources Data, Oklahoma, Water Year 1991","docAbstract":"Water resources data for the 1991 water year for Oklahoma consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes or reservoirs; and water levels of ground-water wells. This report contains discharge records for 131 gaging stations; stage and contents for 30 lakes or reservoirs; water quality for 46 gaging stations and 2 lakes. Also included are 11 partial-record stations and 27 ground-water sites. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Oklahoma.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrOK911","collaboration":"Prepared in cooperation with the State of Oklahoma and with other agencies","usgsCitation":"Blazs, R., Walters, D., Coffey, T., White, D., Boyle, D., and Kerestes, J., 1992, Water Resources Data, Oklahoma, Water Year 1991: U.S. Geological Survey Water Data Report OK-91-1, xiv, 449 p., https://doi.org/10.3133/wdrOK911.","productDescription":"xiv, 449 p.","numberOfPages":"470","costCenters":[],"links":[{"id":382004,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1991/ok-91-1/report-thumb.jpg"},{"id":382627,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1991/ok-91-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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D.L.","contributorId":55505,"corporation":false,"usgs":true,"family":"Boyle","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":807786,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kerestes, J.F.","contributorId":19219,"corporation":false,"usgs":true,"family":"Kerestes","given":"J.F.","affiliations":[],"preferred":false,"id":807787,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70185420,"text":"70185420 - 1992 - Breeding distribution of the Black Turnstone","interactions":[],"lastModifiedDate":"2018-05-20T11:33:55","indexId":"70185420","displayToPublicDate":"1991-01-01T00:00:00","publicationYear":"1992","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":"Breeding distribution of the Black Turnstone","docAbstract":"No abstract available
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The geology of Antarctica","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English ","publisher":"Cambridge University Press","doi":"10.1017/S0954102093270298","usgsCitation":"Ford, A.B., and Himmelberg, G.R., 1992, Geology and crystallization of the Dufek Intrusion, chap. of The geology of Antarctica, p. 175-214, https://doi.org/10.1017/S0954102093270298.","productDescription":"40 p. ","startPage":"175","endPage":"214","costCenters":[],"links":[{"id":339250,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2004-05-13","publicationStatus":"PW","scienceBaseUri":"58e60285e4b09da6799ac6e9","contributors":{"authors":[{"text":"Ford, A. B.","contributorId":44924,"corporation":false,"usgs":false,"family":"Ford","given":"A.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":689646,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Himmelberg, G. R.","contributorId":27106,"corporation":false,"usgs":true,"family":"Himmelberg","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":689647,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185788,"text":"70185788 - 1992 - Discussion of \"Aeration at Ohio River basin navigation dams\"","interactions":[],"lastModifiedDate":"2019-03-19T07:51:45","indexId":"70185788","displayToPublicDate":"1990-03-01T00:00:00","publicationYear":"1992","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2255,"text":"Journal of Environmental Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Discussion of \"Aeration at Ohio River basin navigation dams\"","docAbstract":"No abstract available.
","language":"English","publisher":"American Society of Civil Engineers","doi":"10.1061/(ASCE)0733-9372(1992)118:3(444)","usgsCitation":"Gulliver, J.S., and Wilhelms, S.C., 1992, Discussion of \"Aeration at Ohio River basin navigation dams\": Journal of Environmental Engineering, v. 118, no. 3, p. 446-447, https://doi.org/10.1061/(ASCE)0733-9372(1992)118:3(444).","productDescription":"2 p. ","startPage":"446","endPage":"447","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338529,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"118","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58dcc81fe4b02ff32c685728","contributors":{"authors":[{"text":"Gulliver, John S.","contributorId":190002,"corporation":false,"usgs":false,"family":"Gulliver","given":"John","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":686746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilhelms, Steven C.","contributorId":190003,"corporation":false,"usgs":false,"family":"Wilhelms","given":"Steven","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":686747,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70206822,"text":"70206822 - 1992 - Acute toxicity testing of sediments","interactions":[],"lastModifiedDate":"2019-11-22T16:56:29","indexId":"70206822","displayToPublicDate":"1988-12-31T16:49:51","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"chapter":"9.2.1","title":"Acute toxicity testing of sediments","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Results of the third Joint US-USSR Bering & Chukchi Seas Expedition (BERPAC) : Summer 1988","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Roscigno, P.F., Stiffey, A.V., Burke, W., and Arwood, D.K., 1992, Acute toxicity testing of sediments, in Results of the third Joint US-USSR Bering & Chukchi Seas Expedition (BERPAC) : Summer 1988.","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":369505,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Bering Sea, Chukchi Sea","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Roscigno, Pasquale F.","contributorId":214752,"corporation":false,"usgs":false,"family":"Roscigno","given":"Pasquale","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":775936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stiffey, Arthur V.","contributorId":220845,"corporation":false,"usgs":false,"family":"Stiffey","given":"Arthur","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":775937,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burke, W. David","contributorId":214753,"corporation":false,"usgs":false,"family":"Burke","given":"W. David","affiliations":[],"preferred":false,"id":775938,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Arwood, Diane K.","contributorId":220846,"corporation":false,"usgs":false,"family":"Arwood","given":"Diane","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":775939,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70209355,"text":"70209355 - 1992 - Mesozoic and Cenozoic intrusions and batholiths of the Circum-Pacific region as analogues of pre-Phanerozoic batholiths: A summary","interactions":[],"lastModifiedDate":"2020-04-30T14:23:04.819782","indexId":"70209355","displayToPublicDate":"1988-04-01T14:26:58","publicationYear":"1992","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Mesozoic and Cenozoic intrusions and batholiths of the Circum-Pacific region as analogues of pre-Phanerozoic batholiths: A summary","docAbstract":"No abstract available.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Basement tectonics 8: Characterization and comparison of ancient and mesozoic continental margins","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"The 8th International Conference on Basement Tectonics","conferenceDate":"August 8-12, 1988","conferenceLocation":"Butte, Montana","language":"English","publisher":"Kluwer","usgsCitation":"Brew, D.A., 1992, Mesozoic and Cenozoic intrusions and batholiths of the Circum-Pacific region as analogues of pre-Phanerozoic batholiths: A summary, in Basement tectonics 8: Characterization and comparison of ancient and mesozoic continental margins, v. 8, Butte, Montana, August 8-12, 1988, p. 169-177.","productDescription":"9 p.","startPage":"169","endPage":"177","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":373722,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Brew, David A. dbrew@usgs.gov","contributorId":3244,"corporation":false,"usgs":true,"family":"Brew","given":"David","email":"dbrew@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":786273,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27105,"text":"wri904108 - 1991 - Hydrogeology of the surficial aquifer system, Dade County, Florida","interactions":[],"lastModifiedDate":"2021-10-14T12:09:26.947959","indexId":"wri904108","displayToPublicDate":"2021-10-13T11:05:00","publicationYear":"1991","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":"90-4108","title":"Hydrogeology of the surficial aquifer system, Dade County, Florida","docAbstract":"An investigation of the surficial aquifer system in Dade County, begun in 1983, is part of a regional study of the aquifer system in southeastern Florida. Test drilling for lithologic samples, flow measurements during drilling, aquifer testing, and analyses of earlier data permitted delineation of the hydraulic conductivity distribution (on hydrogeologic sections), the aquifers in the system, the generalized transmissivity distribution, and interpretation of the ground-water flow system. \r\n\r\nThe surficial aquifer system, in which an unconfined ground-water flow system exists, is composed of the sediments from land surface downward to the top of a regionally extensive zone of sediments of low permeability called the intermediate confining unit. The aquifer system units, which vary in composition from clay-size sediments to cavernous limestone, are hydro stratigraphically divided into the Biscayne aquifer at the top; an intervening semiconfining unit that consists principally of clayey sand; a predominantly gray limestone aquifer in the Tamiami Formation in western and west-central Dade County; and sand or clayey sand near the base of the surficial aquifer system. The base of the surficial aquifer system ranges from a depth of about 175 to 210 feet below land surface in westernmost Dade County to greater than 270 feet in northeastern Dade County. Test drilling and aquifer-test data indicate a complex hydraulic conductivity distribution. Hydraulic conductivities of the very highly permeable zone of the Biscayne aquifer commonly exceed 10,000 feet per day; in the gray limestone aquifer, they range from 210 to 780 feet per day. \r\n\r\nTransmissivities of the surficial aquifer system vary locally but have a recognizable areal trend. Estimated values generally are about 300,000 feet squared per day or greater in nearly all of central and eastern Dade County. Transmissivity is lower to the west, decreasing to less than 75,000 feet squared per day in western Dade County. High transmissivity usually is associated with thick sections of the Fort Thompson Formation within the Biscayne aquifer. The gray limestone aquifer of the Tamiami Formation has transmissivities that range from 5,800 to 39,000 feet squared per day in western Dade County. The transition from high transmissivity to relatively low transmissivity is often only a few miles wide and coincides with the decrease in thickness of the very highly permeable Fort Thompson Formation, which marks the western boundary of the Biscayne aquifer. \r\n\r\nMore effective drainage as a result of extensive canal systems and large-scale pumping from municipal well fields has greatly altered the predevelopment flow system in eastern Dade County by: (1) eliminating or greatly reducing a seasonal and coastal ground-water ridge; (2) reducing deep circulation; (3) reducing or eliminating seasonal westward movement of ground water; (4) causing accelerated stormwater runoff and short ground-water flow paths; and (5) generally lowering the water table and inducing saltwater intrusion. Under predevelopment conditions in western Dade County, water entered the gray limestone aquifer by lateral movement from Broward and Collier Counties, and by downward seepage from The Everglades and the Biscayne aquifer, and moved southward and southeastward into Dade County to coastal discharge areas. Circulation in the Biscayne aquifer inland also was primarily to the south and southeast. In eastern Dade County, the seasonal ground-water ridge that formed under predevelopment conditions supported both easterly and westerly ground-water flow away from the ridge axis. This seasonal flow created a zone of lower dissolved solids.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri904108","usgsCitation":"Fish, J., and Stewart, M., 1991, Hydrogeology of the surficial aquifer system, Dade County, Florida: U.S. Geological Survey Water-Resources Investigations Report 90-4108, v, 50 p., https://doi.org/10.3133/wri904108.","productDescription":"v, 50 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":2216,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4108/wri904108.pdf","text":"Report","size":"3.01 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 90-4108"},{"id":389208,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4108/wri904108_plates.pdf","text":"Plates 1-11","size":"11.5 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":159040,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4108/coverthb.jpg"}],"country":"United States","state":"Florida","county":"Dade County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.79345703124999,\n 25.28443774698303\n ],\n [\n -79.73876953124997,\n 25.28443774698303\n ],\n [\n -79.72778320312499,\n 26.401710528707707\n ],\n [\n -80.2001953125,\n 26.362342068998764\n ],\n [\n -80.74951171874999,\n 26.43122806450644\n ],\n [\n -80.79345703124999,\n 25.28443774698303\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE912","usgsCitation":"James, R., and Smigaj, M., 1991, Water resources data Maryland and Delaware, water year 1991, Volume 2: Ground-water data: U.S. Geological Survey Water Data Report MD-DE-91-2, 566 p., https://doi.org/10.3133/wdrMDDE912.","productDescription":"566 p.","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia Water Science Center","active":true,"usgs":true}],"links":[{"id":381964,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1991/md-de-91-2/wdrMDDE912.pdf","text":"Report","size":"122 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Water Data Report MD-DE-91-2"},{"id":181616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1991/md-de-91-2/wdrMDDE912_coverthb.jpg"}],"country":"United States","state":"Delaware, 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