This publication is a history of the prominent earthquakes in the United States from historical times through 1970. It supersedes all previous editions with the same or similar titles (see page ii) and, in addition to updating earthquake listings through 1970, contains several additions and corrections to previous issues. It also brings together under a common cover earthquake data previously listed in two separate reports: Earthquake History of the United States, Part I, Stronger Earthquakes of the United States (Exclusive of California and Western Nevada) and Earthquake History of the United States, Part II, Stronger Earthquakes of California and Western Nevada. Another addition to this publication is the inclusion of a section describing earthquakes in the Puerto Rico region.
\nFor the purpose of listing and describing earthquakes, the United States has been divided into nine regions: (1) Northeastern Region, which includes New England and New York activity and observations of the principal earthquakes of eastern Canada; (2) Eastern Region, including the central Appalachian seismic region activity and the area near Charleston, S.C.; (3) Central Region, which consists of the area between the region just described and the Rocky Mountains; (4) Western Mountain Region, which includes all remaining states except those on the Pacific coast; (5) Washington and Oregon; (6) Alaska; (7) Hawaii; (8) Puerto Rico; and (9) California and Western Nevada. This arrangement has been made chiefly with reference to the natural seismic divisions. It also is a convenient arrangement because there are only three states where there is an important division of earthquake activity: In Tennessee, there are quite distinct areas at opposite ends of the state that fall into different regions. Only central and eastern Nevada are included in the Western Mountain Region, as the activity of the western part is closely associated with that of California. Some earthquake activity has occurred in the part of Texas located in the Western Mountain Region.
\nThe map facing page 1 shows locations of all earthquakes in the regions that follow. A small map showing the area covered by each region immediately precedes the résumé of each chapter (except for the Alaska, Puerto Rico, and Hawaii regions). The seismic risk map below was developed in January 1969 for the conterminous United States by Dr. S. T. Algermissen of NOAA's Environmental Research Laboratories. Subject to revision as continuing research warrants, it is an updated edition of a map divides the United States into four zones: Zone 0, areas with no reasonable expectancy of earthquake damage; Zone 1, expected minor damage; Zone 2, expected moderate damage; and Zone 3, major destructive earthquakes may occur.
","language":"English","publisher":"U.S. Department of Commerce, National Oceanic and Atmospheric Administration; U.S. Department of the Interior, Geological Survey","publisherLocation":"Boulder, CO","usgsCitation":"Coffman, J.L., Von Hake, C.A., and Stover, C.W., 1982, Earthquake history of the United States (Revised edition (through 1970), reprinted 1982 with supplement (1971-80)): Publication 41-1, xii, 208 p., v, 50 p.","productDescription":"xii, 208 p., v, 50 p.","numberOfPages":"277","costCenters":[],"links":[{"id":290115,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":290114,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114182/report.pdf"}],"country":"Canada;United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 173.0,16.916667 ], [ 173.0,71.833333 ], [ -63.9832,71.833333 ], [ -63.9832,16.916667 ], [ 173.0,16.916667 ] ] ] } } ] }","edition":"Revised edition (through 1970), reprinted 1982 with supplement (1971-80)","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53aa9de9e4b065055fab1662","contributors":{"editors":[{"text":"Coffman, Jerry L.","contributorId":49706,"corporation":false,"usgs":true,"family":"Coffman","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":509910,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"von Hake, Carl A.","contributorId":112151,"corporation":false,"usgs":true,"family":"von Hake","given":"Carl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":509911,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Stover, Carl W.","contributorId":28955,"corporation":false,"usgs":true,"family":"Stover","given":"Carl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":509909,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Coffman, Jerry L.","contributorId":49706,"corporation":false,"usgs":true,"family":"Coffman","given":"Jerry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":495255,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Von Hake, Carl A.","contributorId":42634,"corporation":false,"usgs":true,"family":"Von Hake","given":"Carl","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":495254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stover, Carl W.","contributorId":28955,"corporation":false,"usgs":true,"family":"Stover","given":"Carl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":495253,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70164423,"text":"70164423 - 1982 - On Lagrangian residual currents with applications in south San Francisco Bay, California","interactions":[],"lastModifiedDate":"2018-02-05T12:40:53","indexId":"70164423","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"On Lagrangian residual currents with applications in south San Francisco Bay, California","docAbstract":"The Lagrangian residual circulation has often been introduced as the sum of the Eulerian residual circulation and the Stokes' drift. Unfortunately, this definition of the Lagrangian residual circulation is conceptually incorrect because both the Eulerian residual circulation and the Stokes' drift are Eulerian variables. In this paper a classification of various residual variables are reviewed and properly defined. The Lagrangian residual circulation is then studied by means of a two-stage formulation of a computer model. The tidal circulation is first computed in a conventional Eulerian way, and then the Lagrangian residual circulation is determined by a method patterned after the method of markers and cells. To demonstrate properties of the Lagrangian residual circulation, application of this approach in South San Francisco Bay, California, is considered. With the aid of the model results, properties of the Eulerian and Lagrangian residual circulation are examined. It can be concluded that estimation of the Lagrangian residual circulation from Eulerian data may lead to unacceptable error, particularly in a tidal estuary where the tidal excursion is of the same order of magnitude as the length scale of the basin. A direction calculation of the Lagrangian residual circulation must be made and has been shown to be feasible.
By 1980 there were 1,608 reservoirs (over 202 ha each) with a surface area of 4 million ha in the United States. Construction of new reservoirs has decreased in recent years because of the lack of suitable sites and the opposition of environmental interests. Reservoirs have characteristics of both lacustrine and riverine ecosystems. Reservoirs have been segmented into riverine, transitional and lacustrine zones for simulation modelling.Fish and plankton production increases rapidly after initial impoundment and then decreases and stabilizes at lower levels. Decreases in the number of fish species and in fish biomass following impoundment are caused by reduced quantity and quality of spawning and nursery habitat and decreased detrital input. Plankton populations can be followed downstream in a series of reservoirs and increases in abundance were associated with the inundation of vegetation or the introduction of nutrients.In addition to water level management, the most effective fish management programs have included introducing new fishes, developing vegetation or building structures on the reservoir bottom. Considerable progress has been made in predicting the effects of environmental parameters on fish production.
","language":"English","publisher":"Informa","doi":"10.4296/cwrj0701002","usgsCitation":"Benson, N.G., 1982, Some observations on the ecology and fish management of reservoirs in the United States: Canadian Water Resources Journal, v. 7, no. 1, p. 2-25, https://doi.org/10.4296/cwrj0701002.","productDescription":"24 p.","startPage":"2","endPage":"25","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":480246,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4296/cwrj0701002","text":"Publisher Index Page"},{"id":371115,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana, Nebraska, North Dakota, South Dakota","otherGeospatial":"Missouri River reservoirs","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.072509765625,\n 47.71715357016648\n ],\n [\n -108.314208984375,\n 47.5394554474239\n ],\n [\n -108.050537109375,\n 47.234489635299184\n ],\n [\n -106.14990234375,\n 47.53203824675999\n ],\n [\n -104.490966796875,\n 47.98256841921405\n ],\n [\n -102.952880859375,\n 47.923704717745686\n ],\n [\n -102.568359375,\n 47.42808726171425\n ],\n [\n -101.513671875,\n 47.27922900257082\n ],\n [\n -100.821533203125,\n 46.05036097561633\n ],\n [\n -100.887451171875,\n 45.18978009667531\n ],\n [\n -101.304931640625,\n 44.70770622183535\n ],\n [\n -100.61279296875,\n 44.26093725039923\n ],\n [\n -98.997802734375,\n 43.0287452513488\n ],\n [\n -98.646240234375,\n 42.91620643817353\n ],\n [\n -98.316650390625,\n 43.1090040242731\n ],\n [\n -99.47021484375,\n 44.26093725039923\n ],\n [\n -100.4150390625,\n 44.66083904265621\n ],\n [\n -100.14038085937499,\n 45.034714778688624\n ],\n [\n -100.184326171875,\n 45.598665689820635\n ],\n [\n -100.38208007812499,\n 46.15700496290803\n ],\n [\n -100.294189453125,\n 46.64189395892872\n ],\n [\n -100.94238281249999,\n 47.64318610543658\n ],\n [\n -102.008056640625,\n 47.71715357016648\n ],\n [\n -102.161865234375,\n 48.03401915864286\n ],\n [\n -103.095703125,\n 48.29050321714062\n ],\n [\n -104.99633789062499,\n 48.20271028869972\n ],\n [\n -106.12792968749999,\n 48.12943437745315\n ],\n [\n -106.6552734375,\n 48.04870994288686\n ],\n [\n -106.951904296875,\n 47.87214396888731\n ],\n [\n -107.46826171874999,\n 47.79839667295524\n ],\n [\n -108.072509765625,\n 47.71715357016648\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"7","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Benson, N. G.","contributorId":9593,"corporation":false,"usgs":true,"family":"Benson","given":"N.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":779202,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70188735,"text":"70188735 - 1982 - Sensitivity of selected geomagnetic properties to truncation level of spherical harmonic expansions","interactions":[],"lastModifiedDate":"2017-12-08T12:32:45","indexId":"70188735","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"Sensitivity of selected geomagnetic properties to truncation level of spherical harmonic expansions","docAbstract":"A two day selection of MAGSAT data is fit by spherical harmonic series truncated at increasing levels NF in the range 2<NF<14 to determine the extent to which the geomagnetic Gauss coefficients depend upon truncation level of the fit. The dependence is found to be concentrated in the range n<NF≲n+4 decreasing rapidly in magnitude to a few nanotesla as n increases to about 6.
Several geomagnetic properties are then examined by evaluating them at various truncation levels N with NF fixed and N<NF. The spectrum of magnetic energy (outside the core and outside the earth) as determined by the NF=23 MAGSAT model MGST 1/81 is evaluated. It suggests that the crustal anomaly contribution to magnetic energy outside the core will not exceed 0.1%, when the expansion is truncated at N=8. The positions of certain contours of the geomagnetic elements on the core-mantle boundary and their intersections needed for magnetic determination of the core motions, are examined and found to be relatively stable when N changes from 7 to 8, but to exhibit greater sensitivity for both larger and smaller values of N.
This article contains supplementary material.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/GL009i004p00254","usgsCitation":"Benton, E., Estes, R.H., Langel, R., and Muth, L., 1982, Sensitivity of selected geomagnetic properties to truncation level of spherical harmonic expansions: Geophysical Research Letters, v. 9, no. 4, p. 254-257, https://doi.org/10.1029/GL009i004p00254.","productDescription":"4 p.","startPage":"254","endPage":"257","costCenters":[],"links":[{"id":342769,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"4","noUsgsAuthors":false,"publicationDate":"2012-12-07","publicationStatus":"PW","scienceBaseUri":"594cd745e4b062508e39520a","contributors":{"authors":[{"text":"Benton, E.R.","contributorId":100550,"corporation":false,"usgs":true,"family":"Benton","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":699483,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Estes, Ronald H.","contributorId":193258,"corporation":false,"usgs":false,"family":"Estes","given":"Ronald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":699484,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langel, R.A.","contributorId":20918,"corporation":false,"usgs":true,"family":"Langel","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":699485,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Muth, L.A.","contributorId":65224,"corporation":false,"usgs":true,"family":"Muth","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":699486,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70188756,"text":"70188756 - 1982 - Kinematic evolution of the junction of the San Andreas, Garlock, and Big Pine faults, California","interactions":[],"lastModifiedDate":"2020-10-21T15:44:58.054907","indexId":"70188756","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Kinematic evolution of the junction of the San Andreas, Garlock, and Big Pine faults, California","docAbstract":"If the San Andreas fault with about 300 km of right slip, the Carlock fault with about 60 km of left slip, and the Big Pine fault with about 15 km of left slip are considered to have been contemporaneously active, a space problem at their high-angle junctions becomes apparent. Large crustal masses converge in the area of the junctions as a result of the simultaneous large displacements on the faults. We present here a model in which an early straight north-northwest–trending San Andreas deforms to its present bent configuration in response to a westward displacement of crust north of the Garlock fault. During this deformation, the crust north of the Garlock in the vicinity of the junction undergoes north-south shortening, while the fault junction migrates along the trace of the San Andreas fault to the southeast relative to its original position. As a result of this migration, the Mojave area is displaced to the east relative to the original junction position. We suggest a similar history in mirror image for the Big Pine fault and the areas of crust adjacent to it.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1982)10<358:KEOTJO>2.0.CO;2","usgsCitation":"Bohannon, R.G., and Howell, D.G., 1982, Kinematic evolution of the junction of the San Andreas, Garlock, and Big Pine faults, California: Geology, v. 10, no. 7, p. 358-363, https://doi.org/10.1130/0091-7613(1982)10<358:KEOTJO>2.0.CO;2.","productDescription":"6 p.","startPage":"358","endPage":"363","costCenters":[],"links":[{"id":342792,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Big Pine fault, Garlock fault, San Andreas 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\"}}]}","volume":"10","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"594cd740e4b062508e3951e3","contributors":{"authors":[{"text":"Bohannon, Robert G. rbohannon@usgs.gov","contributorId":2255,"corporation":false,"usgs":true,"family":"Bohannon","given":"Robert","email":"rbohannon@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":699733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howell, David G.","contributorId":59874,"corporation":false,"usgs":true,"family":"Howell","given":"David","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":699734,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70188945,"text":"70188945 - 1982 - The Geoid: Effect of compensated topography and uncompensated oceanic trenches","interactions":[],"lastModifiedDate":"2017-06-27T16:39:53","indexId":"70188945","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1807,"text":"Geophysical Research Letters","active":true,"publicationSubtype":{"id":10}},"title":"The Geoid: Effect of compensated topography and uncompensated oceanic trenches","docAbstract":"The geoid is becoming increasingly important in interpretation of global tectonics. Most of the topography of the earth is isostatically compensated, so removal of its effect from the geoid is appropriate before tectonic modeling. The oceanic trenches, however, are dynamically depressed features and cannot be isostatically compensated in the classical way. Continental topography compensated at 35 km gives intracontinental geoidal undulations of up to 15 m over mountain ranges in a spherical harmonic expansion to order and degree 22. Oceanic topography compensated at 40 km, reasonable for the thermally supported long wavelengths, matches the +10 m difference between old continents and old oceans in a detailed NASA/GSFC geoid. Removing the assumed compensation for the oceanic trenches leaves negative anomalies of up to 9 m amplitude caused by their uncompensated mass deficit. This mass deficit acts as a partial \"regional compensation\" for the excess mass of the subducting slabs, and partly explains why geoidal (and gravity) anomalies over the cold slabs are less than thermal models predict.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/GL009i001p00029","usgsCitation":"Chase, C., and McNutt, M.K., 1982, The Geoid: Effect of compensated topography and uncompensated oceanic trenches: Geophysical Research Letters, v. 9, no. 1, p. 29-32, https://doi.org/10.1029/GL009i001p00029.","productDescription":"4 p.","startPage":"29","endPage":"32","costCenters":[],"links":[{"id":343045,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"1","noUsgsAuthors":false,"publicationDate":"2012-12-07","publicationStatus":"PW","scienceBaseUri":"59536ee0e4b062508e3c7b19","contributors":{"authors":[{"text":"Chase, C.G.","contributorId":102965,"corporation":false,"usgs":true,"family":"Chase","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":701470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McNutt, Marcia K. 0000-0003-0117-7716 mcnutt@usgs.gov","orcid":"https://orcid.org/0000-0003-0117-7716","contributorId":327,"corporation":false,"usgs":true,"family":"McNutt","given":"Marcia","email":"mcnutt@usgs.gov","middleInitial":"K.","affiliations":[{"id":5066,"text":"Office of the Director USGS","active":true,"usgs":true}],"preferred":false,"id":701471,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70188920,"text":"70188920 - 1982 - On the distribution of species occurrence","interactions":[],"lastModifiedDate":"2025-06-05T16:35:42.631441","indexId":"70188920","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3001,"text":"Paleobiology","active":true,"publicationSubtype":{"id":10}},"title":"On the distribution of species occurrence","docAbstract":"The distribution of species abundance (number of individuals per species) is well documented. The distribution of species occurrence (number of localities per species), however, has received little attention. This study investigates the distribution of species occurrence for five large data sets. For modern benthic foraminifera, species occurrence is examined from the Atlantic continental margin of North America, where 875 species were recorded 10,017 times at 542 localities, the Gulf of Mexico, where 848 species were recorded 18,007 times at 426 localities, and the Caribbean, where 1149 species were recorded 6684 times at 268 localities. For Late Cretaceous molluscs, species occurrence is examined from the Gulf Coast where 716 species were recorded 6236 times at 166 localities and a subset of this data consisting of 643 species recorded 3851 times at 86 localities.
Logseries and lognormal distributions were fitted to these data sets. In most instances the logseries best predicts the distribution of species occurrence. The lognormal, however, also fits the data fairly well, and, in one instance, better. The use of these distributions allows the prediction of the number of species occurring once, twice, …, n times.
Species abundance data are also available for the molluscan data sets. They indicate that the most abundant species (greatest number of individuals) usually occur most frequently. In all data sets approximately half the species occur four or less times. The probability of noting the presence of rarely occurring species is small, and, consequently, such species must be used with extreme caution in studies requiring knowledge of the distribution of species in space and time.
","language":"English","publisher":"Cambridge University Press","doi":"10.1017/S0094837300004486","usgsCitation":"Buzas, M.A., Koch, C.F., Culver, S., and Sohl, N.F., 1982, On the distribution of species occurrence: Paleobiology, v. 8, no. 2, p. 143-150, https://doi.org/10.1017/S0094837300004486.","productDescription":"8 p.","startPage":"143","endPage":"150","costCenters":[],"links":[{"id":343007,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"2","noUsgsAuthors":false,"publicationDate":"2015-07-14","publicationStatus":"PW","scienceBaseUri":"59536ee1e4b062508e3c7b25","contributors":{"authors":[{"text":"Buzas, Martin A.","contributorId":85098,"corporation":false,"usgs":true,"family":"Buzas","given":"Martin","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":701233,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koch, Carl F.","contributorId":8331,"corporation":false,"usgs":true,"family":"Koch","given":"Carl","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":701234,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Culver, Stephen J.","contributorId":79331,"corporation":false,"usgs":true,"family":"Culver","given":"Stephen J.","affiliations":[],"preferred":false,"id":701235,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sohl, Norman F.","contributorId":27906,"corporation":false,"usgs":true,"family":"Sohl","given":"Norman","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":701236,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70188838,"text":"70188838 - 1982 - The Yellowstone-Snake River Plain seismic profiling experiment: Crustal structure of the Eastern Snake River Plain","interactions":[],"lastModifiedDate":"2017-06-26T11:13:55","indexId":"70188838","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"The Yellowstone-Snake River Plain seismic profiling experiment: Crustal structure of the Eastern Snake River Plain","docAbstract":"Seismic refraction profiles recorded along the eastern Snake River Plain (ESRP) in southeastern Idaho during the 1978 Yellowstone-Snake River Plain cooperative seismic profiling experiment are interpreted to infer the crustal velocity and attenuation (Q-1) structure of the ESRP. Travel-time and synthetic seismogram modeling of a 250 km reversed refraction profile as well as a 100 km detailed profile indicate that the crust of the ESRP is highly anomalous. Approximately 3 to 6 km of volcanic rocks (with some interbedded sediments) overlie an upper-crustal layer (compressional velocity ≅6.1 km/s) which thins southwestward along the ESRP from a thickness of 10 km near Island Park Caldera to 2 to 3 km beneath the central and southwestern portions of the ESRP. An intermediate-velocity (≅6.5 km/s) layer extends from ≅10 to ≅20 km depth. A thick (≅22 km) lower crust of compressional velocity 6.8 km/s, a total crustal thickness of ≅42 km, and a Pnvelocity of ≅7.9 km/s is observed in the ESRP, similar to the western Snake River Plain and the Rocky Mountains Provinces. High attenuation is evident on the amplitude corrected seismic data due to low-Q values in the volcanic rocks (Qp = 20 to 200) and throughout the crust (Qp = 160 to 300). Based on these characteristics of the crustal structure and volcanic-age progression data, it is suggested that the ESRP has resulted from an intensive period of intrusion of mantle-derived basaltic magma into the upper crust generating explosive silicic volcanism and associated regional uplift and caldera collapse. This activity began about 15 m.y. ago in southwestern Idaho and has migrated northeast to its present position at Yellowstone. Subsequent cooling of the intruded upper crust results in the 6.5 km/s velocity intermediate layer. Crustal subsidence and periodic basaltic volcanism as represented by the ESRP complete the sequence of crustal evolution.
","language":"English","publisher":"Wiley","doi":"10.1029/JB087iB04p02597","usgsCitation":"Braile, L., Smith, R.B., Ansorge, J., Baker, M., Sparlin, M., Prodehl, C., Schilly, M., Healy, J.H., , M., and Olsen, K., 1982, The Yellowstone-Snake River Plain seismic profiling experiment: Crustal structure of the Eastern Snake River Plain: Journal of Geophysical Research B: Solid Earth, v. 87, no. B4, p. 2597-2609, https://doi.org/10.1029/JB087iB04p02597.","productDescription":"13 p.","startPage":"2597","endPage":"2609","costCenters":[],"links":[{"id":342866,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B4","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"59521d2ae4b062508e3c36f1","contributors":{"authors":[{"text":"Braile, L.W.","contributorId":85332,"corporation":false,"usgs":true,"family":"Braile","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":700633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R. B.","contributorId":64589,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":700634,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ansorge, J.","contributorId":38318,"corporation":false,"usgs":true,"family":"Ansorge","given":"J.","email":"","affiliations":[],"preferred":false,"id":700635,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baker, M.R.","contributorId":193474,"corporation":false,"usgs":false,"family":"Baker","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":700636,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sparlin, M.A.","contributorId":193497,"corporation":false,"usgs":false,"family":"Sparlin","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":700637,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Prodehl, C.","contributorId":100376,"corporation":false,"usgs":true,"family":"Prodehl","given":"C.","affiliations":[],"preferred":false,"id":700638,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schilly, M.M.","contributorId":193496,"corporation":false,"usgs":false,"family":"Schilly","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":700639,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":700640,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":" Mueller","contributorId":19328,"corporation":false,"usgs":true,"given":"Mueller","email":"","affiliations":[],"preferred":false,"id":700641,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Olsen, K.H.","contributorId":95201,"corporation":false,"usgs":true,"family":"Olsen","given":"K.H.","email":"","affiliations":[],"preferred":false,"id":700642,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":70195419,"text":"70195419 - 1982 - Paleo-oceanography of the Norwegian Sea during the past 130,000 years: Coccolithophorid and foraminferal data","interactions":[],"lastModifiedDate":"2018-02-14T08:28:36","indexId":"70195419","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1068,"text":"Boreas","active":true,"publicationSubtype":{"id":10}},"title":"Paleo-oceanography of the Norwegian Sea during the past 130,000 years: Coccolithophorid and foraminferal data","docAbstract":"Faunal, floral and sedimentological properties of Norwegian Sea core V27-86 were examined in order to reconstruct the paleo-oceanographic history of this region. Downcore variations in the relative abundance of three microfossil groups and several sediment properties exhibit three different climate response patterns (CRP). Each pattern is judged to represent the response of a different part of the climate system. The covariance patterns among coccoliths, henthic foraminifera, and other properties suggest that the Norwegian Sea has been ice-free and productive during the present interhlacial. the penultimate interglacial (isotopic-stage se) and at least partially ice-free during an intermediate climatic regime (stages sa-d). A maximum change in these measures occurs at the boundary between isotopic stage 5a (an intermediate climatic regime)and isotopic stage 4 (a glacial climatic regime). In contrast, planktic foraminiferal assemblages and oxygen isotope measurements on planktic foraminifera show a major change at the end of stage 5e (the penultimate interglacial). The contrasting behavior of these two sets of observations is explained by a model which postulates a low-salinity surface layer 115,000 to 75,000 years ago (stages 5a-d).
","language":"English","publisher":"Wiley","doi":"10.1111/j.1502-3885.1982.tb00516.x","usgsCitation":"Belanger, P., 1982, Paleo-oceanography of the Norwegian Sea during the past 130,000 years: Coccolithophorid and foraminferal data: Boreas, v. 11, no. 1, p. 29-36, https://doi.org/10.1111/j.1502-3885.1982.tb00516.x.","productDescription":"8 p.","startPage":"29","endPage":"36","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":351584,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Norwegian Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -30.937499999999996,\n 52.802761415419674\n ],\n [\n 43.9453125,\n 52.802761415419674\n ],\n [\n 43.9453125,\n 77.8418477505252\n ],\n [\n -30.937499999999996,\n 77.8418477505252\n ],\n [\n -30.937499999999996,\n 52.802761415419674\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"11","issue":"1","noUsgsAuthors":false,"publicationDate":"2008-01-16","publicationStatus":"PW","scienceBaseUri":"5aff4241e4b0da30c1bfdac3","contributors":{"authors":[{"text":"Belanger, P.E.","contributorId":51074,"corporation":false,"usgs":true,"family":"Belanger","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":728519,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207172,"text":"70207172 - 1982 - Triggering of large earthquakes by magma-chamber inflation, Izu Peninsula (Japan)","interactions":[],"lastModifiedDate":"2020-06-01T12:31:49.611074","indexId":"70207172","displayToPublicDate":"1982-12-11T11:34:14","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Triggering of large earthquakes by magma-chamber inflation, Izu Peninsula (Japan)","docAbstract":"A close spatial and temporal association between three aseismic uplift episodes and subsequent large (M ≈ 7) earthquakes on the Izu Peninsula, Japan, suggests a causal relation. Quaternary geology, as well as studies by other workers, indicates a volcanic origin for the observed uplift, and we use a simple inflation model constrained by leveling data to compute the expected increments in normal and shear stress across faults that ruptured in the earthquakes. Using a Mohr-Coulomb criterion, we find that in two cases out of three, stress changes induced by inflation are in the correct sense to trigger failure. Although changes are no more than a few bars, they represent the equivalent of several decades to a century of secular stress buildup.
","language":"English","publisher":"GSA","doi":"10.1130/0091-7613(1982)10<637:TOLEBM>2.0.CO;2","usgsCitation":"Thatcher, W.R., and Savage, J.C., 1982, Triggering of large earthquakes by magma-chamber inflation, Izu Peninsula (Japan): Geology, v. 10, no. 12, p. 637-640, https://doi.org/10.1130/0091-7613(1982)10<637:TOLEBM>2.0.CO;2.","productDescription":"4 p.","startPage":"637","endPage":"640","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":370154,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","otherGeospatial":"Izu Peninsula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 138.22723388671875,\n 34.53597500508991\n ],\n [\n 139.735107421875,\n 34.53597500508991\n ],\n [\n 139.735107421875,\n 35.55457449014312\n ],\n [\n 138.22723388671875,\n 35.55457449014312\n ],\n [\n 138.22723388671875,\n 34.53597500508991\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"10","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Thatcher, Wayne R. 0000-0001-6324-545X thatcher@usgs.gov","orcid":"https://orcid.org/0000-0001-6324-545X","contributorId":2599,"corporation":false,"usgs":true,"family":"Thatcher","given":"Wayne","email":"thatcher@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":777147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Savage, James C. 0000-0002-5114-7673 jasavage@usgs.gov","orcid":"https://orcid.org/0000-0002-5114-7673","contributorId":2412,"corporation":false,"usgs":true,"family":"Savage","given":"James","email":"jasavage@usgs.gov","middleInitial":"C.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":777148,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011673,"text":"70011673 - 1982 - Uranium in spring water and bryophytes at basin creek in central idaho","interactions":[],"lastModifiedDate":"2025-04-08T16:52:38.282389","indexId":"70011673","displayToPublicDate":"1982-12-03T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Uranium in spring water and bryophytes at basin creek in central idaho","docAbstract":"Arkosic sandstones and conglomerates of Tertiary age beneath the Challis Volcanics of Eocene age at Basin Creek, 10 km northeast of Stanley, Idaho, contain uranium-bearing vitrainized carbon fragments. The economic potential of these sandstones and conglomerates is currently being assessed. Springs abound at the contacts of rock units, and water from these springs supports abundant growths of bryophytes (mosses and liverworts). Water from 22 springs and associated bryophytes were sampled; two springs were found to contain apparently anomalous concentrations (normalized) of uranium — as much as 6.5 μg/L (ppb) in water and 1800 μg/g (ppm) in ash of mosses. Moss samples from both springs also contained anomalous concentrations of arsenic, and one contained highly anomalous amounts of beryllium. Water from a third spring contained slightly anomalous amounts of uranium, and two species of mosses at the spring contained anomalous uranium (400 and 700 μg/g) and high levels of both cadmium and lead. Water from a fourth spring was normal for uranium (0.18 μg/L), but the moss from the water contained a moderate uranium level and highly anomalous concentrations of lead, germanium, and thallium.
These results suggest that, in the Basin Creek area, moss sampling at springs may give a more reliable indication of uranium occurrence than would water sampling. The reason for this may be the ability of mosses to concentrate uranium and its associated pathfinder elements and to integrate uranium fluctuations that occur in the spring water over any period of time.
","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(82)90004-8","usgsCitation":"Shacklette, H., and Erdman, J.A., 1982, Uranium in spring water and bryophytes at basin creek in central idaho: Journal of Geochemical Exploration, v. 17, no. 3, p. 221-236, https://doi.org/10.1016/0375-6742(82)90004-8.","productDescription":"16 p.","startPage":"221","endPage":"236","costCenters":[],"links":[{"id":220717,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"central Idaho","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.11898816098233,\n 46.88064351215584\n ],\n [\n -117.11898816098233,\n 43.52384377775087\n ],\n [\n -112.3634806336367,\n 43.52384377775087\n ],\n [\n -112.3634806336367,\n 46.88064351215584\n ],\n [\n -117.11898816098233,\n 46.88064351215584\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"17","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbdb8e4b08c986b3291af","contributors":{"authors":[{"text":"Shacklette, H.T.","contributorId":61813,"corporation":false,"usgs":true,"family":"Shacklette","given":"H.T.","affiliations":[],"preferred":false,"id":361679,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erdman, J. A.","contributorId":59786,"corporation":false,"usgs":true,"family":"Erdman","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":361678,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70120255,"text":"70120255 - 1982 - Susitna Hydroelectric Project: terrestrial environmental workshop and preliminary simulation model","interactions":[],"lastModifiedDate":"2014-08-13T13:41:01","indexId":"70120255","displayToPublicDate":"1982-10-22T13:39:28","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Susitna Hydroelectric Project: terrestrial environmental workshop and preliminary simulation model","docAbstract":"The technical feasibility, economic viability, and environmental impacts of a hydroelectric development project in the Susitna River Basin are being studied by Acres American, Inc. on behalf of the Alaska Power Authority. As part of these studies, Acres American recently contracted LGL Alaska Research Associates, Inc. to coordinate the terrestrial environmental studies being performed by the Alaska Department of Fish and Game and, as subcontractors to LGL, several University of Alaska research groups. LGL is responsible for further quantifying the potential impacts of the project on terrestrial wildlife and vegetation, and for developing a plan to mitigate adverse impacts on the terrestrial environment. The impact assessment and mitigation plan will be included as part of a license application to the Federal Energy Regulatory Commission (FERC) scheduled for the first quarter of 1983.
\nThe quantification of impacts, mitigation planning, and design of future research is being organized using a computer simulation modelling approach. Through a series of workshops attended by researchers, resource managers, and policy-makers, a computer model is being developed and refined for use in the quantification of impacts on terrestrial wildlife and vegetation, and for evaluating different mitigation measures such as habitat enhancement and the designation of replacement lands to be managed by wildlife habitat. This report describes the preliminary model developed at the first workshop held August 23 -27, 1982 in Anchorage.
","language":"English","publisher":"Enviromental and Social Systems Analysts","publisherLocation":"Vancouver, British Columbia, Canada","usgsCitation":"Everitt, R.R., Sonntag, N.C., Auble, G.T., Roelle, J.E., and Gazey, W., 1982, Susitna Hydroelectric Project: terrestrial environmental workshop and preliminary simulation model, 123 p.","productDescription":"123 p.","numberOfPages":"123","costCenters":[],"links":[{"id":292100,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ec7bd3e4b02bf5a76740b6","contributors":{"authors":[{"text":"Everitt, Robert R.","contributorId":34837,"corporation":false,"usgs":true,"family":"Everitt","given":"Robert","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":498063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sonntag, Nicholas C.","contributorId":85894,"corporation":false,"usgs":true,"family":"Sonntag","given":"Nicholas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":498065,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Auble, Gregory T.","contributorId":23456,"corporation":false,"usgs":true,"family":"Auble","given":"Gregory","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":498062,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Roelle, James E. roelleb@usgs.gov","contributorId":2330,"corporation":false,"usgs":true,"family":"Roelle","given":"James","email":"roelleb@usgs.gov","middleInitial":"E.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":498061,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gazey, William","contributorId":78653,"corporation":false,"usgs":true,"family":"Gazey","given":"William","email":"","affiliations":[],"preferred":false,"id":498064,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70011552,"text":"70011552 - 1982 - Modern sedimentary environments on the Rhode Island inner shelf, off the eastern United States","interactions":[],"lastModifiedDate":"2024-10-16T15:41:34.328013","indexId":"70011552","displayToPublicDate":"1982-10-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Modern sedimentary environments on the Rhode Island inner shelf, off the eastern United States","docAbstract":"Analyses of side-scan sonar records along with previously published bathymetric, textural and subbottom data reveal the sedimentary environments on the inner Continental Shelf south of Narragansett Bay, Rhode Island. The bottom topography in this area is characterized by a broad central depression bordered by shallow, irregular sea floor on the north and east and by a discontinuous, curvilinear ridge on the south and west.
Four distinct environments were identified:
(1) Pre-Mesozoic coastal rocks are exposed on the sea floor at isolated locations near the shore (waterdepths < 32 m). These exposures have pronounced, irregular topographic relief and produce blotchy patterns op side-scan sonographs.
(2) Glacial moraine deposits form the discontinuous offshore ridge. These deposits have hummocky sea-floor relief, are covered by lag gravel and boulders, and appear as predominantly black (strongly reflective) patterns on the side-scan records.
(3) Over most of the shallow, irregular bottom in the northeast, on the flanks of the morainal ridge, and atop bathymetric highs, the sea floor is characterized as a mosaic of light and dark patches and lineations. The dark (more reflective) zones are areas of coarse sands and megaripples (wavelengths = 0.8--1.2 m) that either have no detectable relief or are slightly depressed relative to surrounding (fight) areas of finer-grained sands.
(4) Smooth beds that produce nearly featureless patterns on the sonographs occupy the broad central bathymetric depression as well as smaller depressions north and east of Block Island. Within the broad depression, sonographs having practically no shading indicate a central zone of modern sandy silt, whereas records having moderate tonality define a peripheral belt of silty sand.
The sedimentary environments that are outlined range from erosional or nondepositional (bedrock, glacial moraine) to depositional (featureless beds), and include areas that may reflect a combination of erosional and depositional processes (textural patchiness). The distribution and characteristics of the environments reveal the general post-glacial sedimentary history of this area and provide a guide to future utilization of the shelf surface.
This is an annotated bibliography of the publications authored or co-authored by the staff of the National Fisheries Center - Leetown (NFC-L) from 1972 through 1980. It includes publications from NFC-L staff at the Fish Farming Experimental Station, Stuttgart, AR; the Fish Genetics Laboratory, Beulah, WY; the Hagerman Field Station of the Tunison Laboratory of Fish Nutrition, Hagerman, ID; the National Fisheries Research and Development Laboratory, Marison, AL; and, the Tunison Laboratory of Fish Nutrition, Cortland, NY. It also includes publications from NFC-L staff at the Aquaculture Production/Demonstration Station, Fisheries Academy, Fish Genetics Station, National Fish Health Research Laboratory, and Technical Information Services, each located in Kearneysville, WV. Prior to 1977, each functioned as a separate entity within the U.S. Fish and Wildlife Service. In 1977, the administrative and program activities of these components were merged into the Natkonal Fisheries Center. This bibliography lists the publications issued by each of these entities both before and after becoming joined into the Center. Publications from these components prior to 1972 are documents in U.S. Bureau of Sport Fisheries and Wildlife, Resource Publication 120, Bibliography of Research Publications of the U.S. Bureau of Sport Fisheries and Wildlife, 1928-72.
\nEntries in this bibliography are arranged under broad subject categories, similar to those used in U.S. Fish and Wildlife Service, Sport Fishery Abstracts. Within these categories, the publications are then arranged alphabetically by author and sequentially by date of publication. They cover a wide range of scientific and technical disciplines applicable to the field of aquaculture. The annotations were submitted by each NFC-L component, and were modified to some extent for uniformity. An author index is included at the end of the bibliography.
","language":"English","publisher":"U.S. Fish and Wildlife Service, National Fisheries Center","publisherLocation":"Kearneysville, WV","usgsCitation":"Mann, J.A., Catrow, V.J., McKenzie, L.C., and Engle, F.V., 1982, Fish culture: an annotated bibliography of publications of the National Fisheries Center, Leetown, 1972-1980, 124 p.","productDescription":"124 p.","numberOfPages":"126","temporalStart":"1972-01-01","temporalEnd":"1980-12-31","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":289163,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53b286eae4b07b8813a5549c","contributors":{"authors":[{"text":"Mann, Joyce A.","contributorId":93112,"corporation":false,"usgs":true,"family":"Mann","given":"Joyce","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":355271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Catrow, Violet J.","contributorId":81411,"corporation":false,"usgs":true,"family":"Catrow","given":"Violet","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":355270,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKenzie, Lora C.","contributorId":52894,"corporation":false,"usgs":true,"family":"McKenzie","given":"Lora","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":355268,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Engle, Faye V.","contributorId":54888,"corporation":false,"usgs":true,"family":"Engle","given":"Faye","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":355269,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70120390,"text":"70120390 - 1982 - Capture-recapture and removal methods for sampling closed populations","interactions":[],"lastModifiedDate":"2014-08-14T09:08:52","indexId":"70120390","displayToPublicDate":"1982-08-01T09:07:04","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Capture-recapture and removal methods for sampling closed populations","docAbstract":"The problem of estimating animal abundance is common in wildlife management and environmental impact asessment. Capture-recapture and removal methods are often used to estimate population size. Statistical Inference From Capture Data On Closed Animal Populations, a monograph by Otis et al. (1978), provides a comprehensive synthesis of much of the wildlife and statistical literature on the methods, as well as some extensions of the general theory. In our primer, we focus on capture-recapture and removal methods for trapping studies in which a population is assumed to be closed and do not treat open-population models, such as the Jolly-Seber model, or catch-effort methods in any detail. The primer, written for students interested in population estimation, is intended for use with the more theoretical monograph.","language":"English","publisher":"Los Alamos National Laboratory","publisherLocation":"Los Alamos, NM","usgsCitation":"White, G.C., Anderson, D.R., Burnham, K.P., and Otis, D.L., 1982, Capture-recapture and removal methods for sampling closed populations, 13 p.","productDescription":"13 p.","numberOfPages":"14","costCenters":[],"links":[{"id":292143,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53edcd44e4b0f61b386d23ac","contributors":{"authors":[{"text":"White, Gary C.","contributorId":66831,"corporation":false,"usgs":false,"family":"White","given":"Gary","email":"","middleInitial":"C.","affiliations":[{"id":6621,"text":"Colorado State University","active":true,"usgs":false}],"preferred":false,"id":498121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, David R.","contributorId":92722,"corporation":false,"usgs":true,"family":"Anderson","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":498123,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burnham, Kenneth P.","contributorId":95025,"corporation":false,"usgs":true,"family":"Burnham","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[{"id":189,"text":"Colorado Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":498124,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Otis, David L.","contributorId":78455,"corporation":false,"usgs":true,"family":"Otis","given":"David","email":"","middleInitial":"L.","affiliations":[{"id":350,"text":"Iowa Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":498122,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70011860,"text":"70011860 - 1982 - Hydrogeochemical prospecting for porphyry copper deposits in the tropical-marine climate of Puerto Rico","interactions":[],"lastModifiedDate":"2025-04-09T15:02:15.596022","indexId":"70011860","displayToPublicDate":"1982-06-04T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Hydrogeochemical prospecting for porphyry copper deposits in the tropical-marine climate of Puerto Rico","docAbstract":"A hydrogeochemical survey utilizing waters from streams and springs was conducted in the area of two known porphyry copper deposits in the tropical-marine climate of westcentral Puerto Rico. The most important pathfinder for regional hydrogeochemical surveys is sulfate which reflects the associated pyrite mineralization. Because of increased mobility due to intense chemical weathering and the low pH environment, dissolved copper can also be used as a pathfinder for regional surveys and has the advantage of distinguishing barren pyrite from pyrite associated with copper mineralization. For follow-up surveys, the most important pathfinders are copper, sulfate, pH, zinc, and fluoride. High concentrations of dissolved copper and moderate concentrations of sulfate is a diagnostic indication of nearby sources of copper minerals.
An understanding of the geochemical processes taking place in the streambeds and the weathering environment, such as the precipitation of secondary copper minerals, contributes to the interpretation of the geochemical data and the selection of the most favorable areas for further exploration.
","largerWorkType":{"id":2,"text":"Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(82)90011-5","usgsCitation":"Miller, W.R., Ficklin, W.H., and Learned, R.E., 1982, Hydrogeochemical prospecting for porphyry copper deposits in the tropical-marine climate of Puerto Rico: Journal of Geochemical Exploration, v. 16, no. 3, p. 217-233, https://doi.org/10.1016/0375-6742(82)90011-5.","productDescription":"17 p.","startPage":"217","endPage":"233","costCenters":[],"links":[{"id":220796,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Puerto 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R.","contributorId":92239,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":362141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ficklin, W. H.","contributorId":89517,"corporation":false,"usgs":true,"family":"Ficklin","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":362140,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Learned, R. E.","contributorId":9638,"corporation":false,"usgs":true,"family":"Learned","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":362139,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011708,"text":"70011708 - 1982 - Uraniferous opal, Virgin Valley, Nevada: Conditions of formation and implications for uranium exploration","interactions":[],"lastModifiedDate":"2025-04-08T17:10:15.793994","indexId":"70011708","displayToPublicDate":"1982-06-04T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Uraniferous opal, Virgin Valley, Nevada: Conditions of formation and implications for uranium exploration","docAbstract":"Uraniferous, fluorescent opal, which occurs in tuffaceous sedimentary rocks at Virgin Valley, Nevada, records the temperature and composition of uranium-rich solutions as well as the time of uranium-silica coprecipitation. Results are integrated with previous geologic and geochronologic data for the area to produce a model for uranium mobility that may be used to explore for uranium deposits in similar geologic settings.
Uraniferous opal occurs as replacements of diatomite, or silicic air-fall ash layers in tuffaceous lakebeds of the Virgin Valley Formation (Miocene) of Merriam (1907). Fission-track radiography shows uranium to be homogeneously dispersed throughout the opal structure, suggesting coprecipitation of dissolved uranium and silica gel. Fluid inclusions preserved within opal replacements of diatomite have homogenization temperatures in the epithermal range and are of low salinity. Four samples of opal from one locality all have U-Pb apparent ages which suggest uraniferous opal precipitation in late Pliocene time. These ages correspond to a period of local, normal faulting, and highangle faults may have served as vertical conduits for transport of deep, thermalized ground water to shallower levels. Lateral migration of rising solutions occurred at intersections of faults with permeable strata. Silica and some uranium were dissolved from silica-rich host strata of 5–20 ppm original uranium content and reprecipitated as the solutions cooled. The model predicts that in similar geologic settings, ore-grade concentrations of uranium will occur in permeable strata that intersect high-angle faults and that contain uranium source rocks as well as efficient reductant traps for uranium. In the absence of sufficient quantities of reductant materials, uranium will be flushed from the system or will accumulate in low-grade disseminated hosts such as uraniferous opal.
","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(82)90010-3","usgsCitation":"Zielinski, R.A., 1982, Uraniferous opal, Virgin Valley, Nevada: Conditions of formation and implications for uranium exploration: Journal of Geochemical Exploration, v. 16, no. 3, p. 197-216, https://doi.org/10.1016/0375-6742(82)90010-3.","productDescription":"20 p.","startPage":"197","endPage":"216","costCenters":[],"links":[{"id":221384,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Humboldt County","otherGeospatial":"Virgin 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R. A. 0000-0002-4047-5129","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":106930,"corporation":false,"usgs":true,"family":"Zielinski","given":"R.","email":"","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":361778,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011809,"text":"70011809 - 1982 - Submarine valleys in the northeastern Gulf of Alaska: Characteristics and probable origin","interactions":[],"lastModifiedDate":"2024-10-16T16:01:50.866852","indexId":"70011809","displayToPublicDate":"1982-06-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2667,"text":"Marine Geology","active":true,"publicationSubtype":{"id":10}},"title":"Submarine valleys in the northeastern Gulf of Alaska: Characteristics and probable origin","docAbstract":"The continental shelf of the northeastern Gulf of Alaska Between Prince William Sound and Cross Sound is cut by at least eight major valleys. From west to east, these are Hinchinbrook Seavalley, Egg Island Trough, Kayak Trough, Bering Trough, Pamplona Troughs, Yakutat Valley, Alsek Valley and Yakobi Valley. Evidence common to most of these troughs or valleys indicating that the present morphology is due to glacial processes includes: (1) a pre-Holocene subbottom erosional surface incised into the underlying lithified strata of the shelf; (2) U-shaped cross sections, both at the sea floor and at the pre-Holocene erosional surface; (3) concave longitudinal sections, commonly shoaling at the seaward end; (4) till-like sediments collected from the walls or outer shelf adjacent to the troughs; and (5) seismic stratigraphy that can be correlated with bottom samples indicative of glacially derived strata.
Depressions with tens of meters of relief are present on the pre-Holocene subbottom erosional surface beneath most of these valleys. These depressions have been partially filled by a seaward-thinning wedge of Holocene glacial flour (clayey silt) that is filling the valleys and blanketing the inner shelf at rates as high as 15 mm/yr (based on 210Pb measurements). Although glaciation played a dominant role in the modern morphology of these sea valleys, structural features, including structurally controlled topographic highs on the shelf (e.g. Tarr Bank, Kayak Island, Pamplona Spur and Fairweather Ground) influenced the flow directions of the glacial lobes.
","language":"English","publisher":"Elsevier","doi":"10.1016/0025-3227(82)90070-6","usgsCitation":"Carlson, P.R., Bruns, T.R., Molnia, B.F., and Schwab, W., 1982, Submarine valleys in the northeastern Gulf of Alaska: Characteristics and probable origin: Marine Geology, v. 47, no. 3-4, p. 217-242, https://doi.org/10.1016/0025-3227(82)90070-6.","productDescription":"26 p.","startPage":"217","endPage":"242","costCenters":[{"id":36171,"text":"National Civil Applications Center","active":true,"usgs":true}],"links":[{"id":221064,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"northeastern Gulf of Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -146.67638035410144,\n 60.976930988760245\n ],\n [\n -146.67638035410144,\n 52.62253667132154\n ],\n [\n -130.93473329233763,\n 52.62253667132154\n ],\n [\n -130.93473329233763,\n 60.976930988760245\n ],\n [\n -146.67638035410144,\n 60.976930988760245\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"47","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9d3ae4b08c986b31d6ff","contributors":{"authors":[{"text":"Carlson, Paul R.","contributorId":81469,"corporation":false,"usgs":true,"family":"Carlson","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":362008,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bruns, Terry R.","contributorId":29420,"corporation":false,"usgs":true,"family":"Bruns","given":"Terry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":362007,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Molnia, Bruce F. 0000-0001-8102-6269","orcid":"https://orcid.org/0000-0001-8102-6269","contributorId":301013,"corporation":false,"usgs":true,"family":"Molnia","given":"Bruce","email":"","middleInitial":"F.","affiliations":[{"id":36171,"text":"National Civil Applications Center","active":true,"usgs":true}],"preferred":true,"id":362005,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schwab, W.C.","contributorId":69989,"corporation":false,"usgs":true,"family":"Schwab","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":362006,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70210003,"text":"70210003 - 1982 - Continuous subaqueous deposition of the Permian Castile evaporites, Delaware Basin, Texas and New Mexico","interactions":[],"lastModifiedDate":"2020-05-11T12:29:45.405279","indexId":"70210003","displayToPublicDate":"1982-05-08T12:10:13","publicationYear":"1982","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Continuous subaqueous deposition of the Permian Castile evaporites, Delaware Basin, Texas and New Mexico","docAbstract":"Structures that are common in the Castile Formation (Ochoan) of the Delaware Basin, Texas and New Mexico (Fig. 1) include fine planar laminations, breccias, microfolded laminae, and nodular anhydrite. These structures, particularly the laminae, have been used to demonstrate the subaqueous depositional history of the Castile (Anderson and Kirkland, 1966; Anderson et al., 1972; Dean et al., 1975; Dean and Anderson, 1978). Kirkland and Anderson (1970) showed that the microfolds in the Castile are related to larger folds generated by tectonic compression. Breccia beds and chimneys and their relations to vertical and lateral salt dissolution in the Delaware Basin were discussed by Anderson et al. (1972), Anderson (1978), Anderson et al. (1978), and Anderson and Kirkland (1980). In this workshop we will describe and illustrate these structures and summarize how they have been used to understand the depositional and postdepositional history of a major evaporite deposit for which there is no modern analog.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Depositional and diagenetic spectra of evaporites","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":" SEPM Core Workshop","conferenceDate":"June 26-27, 1982","conferenceLocation":"Calgary, Canada","language":"English","publisher":" Society of Economic Paleontologists and Mineralogists","doi":"10.2110/cor.82.01.0324","usgsCitation":"Dean, W.E., and Anderson, R., 1982, Continuous subaqueous deposition of the Permian Castile evaporites, Delaware Basin, Texas and New Mexico, in Depositional and diagenetic spectra of evaporites, v. 3, Calgary, Canada, June 26-27, 1982, p. 324-353, https://doi.org/10.2110/cor.82.01.0324.","productDescription":"30 p.","startPage":"324","endPage":"353","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374580,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico, Texas","otherGeospatial":"Delaware Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.91943359374999,\n 31.409912194070973\n ],\n [\n -103.271484375,\n 31.409912194070973\n ],\n [\n -103.271484375,\n 32.21280106801518\n ],\n [\n -104.91943359374999,\n 32.21280106801518\n ],\n [\n -104.91943359374999,\n 31.409912194070973\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":788767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, Roger","contributorId":82188,"corporation":false,"usgs":true,"family":"Anderson","given":"Roger","affiliations":[],"preferred":false,"id":788768,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70209997,"text":"70209997 - 1982 - Application of wave field continuation to the inversion of refraction data","interactions":[],"lastModifiedDate":"2020-05-08T14:10:32.738175","indexId":"70209997","displayToPublicDate":"1982-05-08T09:04:36","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Application of wave field continuation to the inversion of refraction data","docAbstract":"Three examples of the inversion of refraction data by downward continuation illustrate the applicability of the method to field data. The first example is a refraction profile from the Mojave Desert, California. These data are spatially aliased and contain clear evidence of lateral inhomogeneity. The inversion in this case produces a broken image in the slowness‐depth domain due to the lateral inhomogeneity, but a useful average velocity model is still obtained. The second example is a shallow marine reflection profile. Here, the truncation effects due to the finite horizontal aperture of the recording cable produce artifacts in the slowness‐depth domain. The velocity model is, however, distinct from these artifacts, and the presence of strong precritical reflections aids in the inversion. The third example is another shallow marine reflection profile. The inversion of these data illustrate the utilization of constraints provided by multiples as well as primary arrivals.
Uranium-lead isotope systematics of roll-front ores in Miocene sandstone at the Felder and McLean uranium deposits (south Texas coastal plain) give a well-defined 207 Pb/ 204 Pb- 235 U/ 204 Pb isochron age of 5.07 + or - 0.15 m.y. The relatively slight degree of scatter of the points defining the isochron is probably due to initial Pb isotope inhomogeneity, and the resulting inferred persistence of closed system behavior for U and Pb is probably the result of the long-term presence of U- and Pb-immobilizing H 2 S. 206 Pb/ 238 U systematics are badly scattered owing to long-term migration of radioactive daughters of 238 U. Beta- and gamma-activity systematics of the ores consistently identify those with grossly anomalous Pb isotope systematics, however, and proved highly useful in identifying ores that have gained gross amounts of uranium daughters.FeS 2 minerals in the altered tongue of the host sandstone are characterized by abundant postore pyrite and heavy delta 34 S values, whereas FeS 2 minerals in mineralized and unaltered, barren rock are characterized by abundant ore-stage marcasite and by light delta 34 S values. The delta 34 S values of FeS 2 minerals in the altered tongue are similar to those defined for sour gas from the underlying Edwards Limestone of Cretaceous age, indicating the probable source for the sulfur of an inferred resulfidization event. The 5.07-m.y. isochron age probably reflects the end of roll-front development; we believe that the end was due to the resulfidization and does not preclude significant earlier periods of mineralization. Modern ground water in the area is also sulfide bearing (thus helping preserve the deposit), but with delta 34 S values distinct from those of sulfides in the resulfidized zone of the host rock.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.77.3.557","usgsCitation":"Ludwig, K., Goldhaber, M.B., Reynolds, R.L., and Simmons, K., 1982, Uranium-lead isochron age and preliminary sulfur isotope systematics of the Felder uranium deposit, south Texas: Economic Geology, v. 77, no. 3, p. 557-563, https://doi.org/10.2113/gsecongeo.77.3.557.","productDescription":"8 p.","startPage":"557","endPage":"563","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374165,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","county":"Live Oak County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.0037,28.6896],[-98.0894,28.6599],[-98.0167,28.5323],[-97.8084,28.1788],[-97.8136,28.1757],[-97.8896,28.1253],[-97.8991,28.1185],[-97.9007,28.1167],[-97.9018,28.1135],[-97.9008,28.1108],[-97.9009,28.1071],[-97.902,28.1048],[-97.9047,28.0998],[-97.9059,28.0934],[-97.9041,28.0846],[-97.9021,28.079],[-97.9013,28.0726],[-97.8988,28.0684],[-97.8963,28.0646],[-97.8943,28.0609],[-97.8923,28.0595],[-98.2338,28.0607],[-98.3343,28.06],[-98.3358,28.4775],[-98.336,28.4982],[-98.3363,28.6117],[-98.099,28.7882],[-98.0037,28.6896]]]},\"properties\":{\"name\":\"Live Oak\",\"state\":\"TX\"}}]}","volume":"77","issue":"3","noUsgsAuthors":false,"publicationDate":"1982-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Ludwig, K.R.","contributorId":97112,"corporation":false,"usgs":true,"family":"Ludwig","given":"K.R.","email":"","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":787598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":787599,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787600,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Simmons, Kathleen R. ksimmons@usgs.gov","contributorId":140955,"corporation":false,"usgs":true,"family":"Simmons","given":"Kathleen R.","email":"ksimmons@usgs.gov","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":false,"id":787601,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70120400,"text":"70120400 - 1982 - Preliminary evaluation of a habitat suitability model for pronghorn","interactions":[],"lastModifiedDate":"2014-08-14T10:17:13","indexId":"70120400","displayToPublicDate":"1982-04-05T10:16:05","publicationYear":"1982","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":12,"text":"Conference publication"},"title":"Preliminary evaluation of a habitat suitability model for pronghorn","largerWorkTitle":"Proceedings 10th biennial pronghorn antelope workshop","usgsCitation":"Allen, A.W., and Armbruster, M., 1982, Preliminary evaluation of a habitat suitability model for pronghorn.","costCenters":[],"links":[{"id":292171,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53edcd4ee4b0f61b386d2440","contributors":{"authors":[{"text":"Allen, Arthur W.","contributorId":40648,"corporation":false,"usgs":true,"family":"Allen","given":"Arthur","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":498147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armbruster, M.J.","contributorId":21127,"corporation":false,"usgs":true,"family":"Armbruster","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":498146,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70185630,"text":"70185630 - 1982 - Volatilization of ketones from water","interactions":[],"lastModifiedDate":"2020-01-26T09:56:15","indexId":"70185630","displayToPublicDate":"1982-04-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3728,"text":"Water, Air, & Soil Pollution","onlineIssn":"1573-2932","printIssn":"0049-6979","active":true,"publicationSubtype":{"id":10}},"title":"Volatilization of ketones from water","docAbstract":"The overall mass-transfer coefficients for the volatilization from water of acetone, 2-butanone, 2-pentanone, 3-pentanone, 4-methyl-2-pentanone, 2-heptanone, and 2-octanone were measured simultaneously with the oxygen-absorption coefficient in a laboratory stirred water bath. The liquid-film and gas-film coefficients of the two-film model were determined for the ketones from the overall coefficients, and both film resistances were important for volatilization of the ketones.
The liquid-film coefficients for the ketones varied with the 0.719 power of the molecular-diffusion coefficient, in agreement with the literature. The liquid-film coefficients showed a variable dependence on molecular weight, with the dependence ranging from the −0.263 power for acetone to the −0.378 power for 2-octanone. This is in contrast with the literature where a constant −0.500 power dependence on the molecular weight is assumed.
The gas-film coefficients for the ketones showed no dependence on molecular weight, in contrast with the literature where a −0.500 power is assumed.
","language":"English","publisher":"D. Reidel Publishing Co","doi":"10.1007/BF00283158","usgsCitation":"Rathbun, R.E., and Tai, D.Y., 1982, Volatilization of ketones from water: Water, Air, & Soil Pollution, v. 17, no. 3, p. 281-293, https://doi.org/10.1007/BF00283158.","productDescription":"13 p.","startPage":"281","endPage":"293","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338331,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63041e4b05ec799131123","contributors":{"authors":[{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":686162,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tai, D. Y.","contributorId":59778,"corporation":false,"usgs":true,"family":"Tai","given":"D.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":686163,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}