Water resources data for the 1981 water year for Missouri consist of records of stage, discharge, and water quality of lakes and reservoirs; contains records for water discharge at 124 gaging stations; stage and contents at 7 lakes and reservoirs; water quality at 33 gaging stations (including 1 lake); 11 sites measured bi-monthly, 2 USGS water quality monitors, and 1 temperature (continuous recording) site. Also included are data for 30 crest-stage, 11 water-quality partial-record stations, and 20 low-flow partial-record stations.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMO811","collaboration":"Prepared in cooperation with the Missouri Department of Natural Resources, Division of Geology and Land Survey and Division of Environmental Quality; Missouri State Highway Commission; and with other State and Federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data for Missouri, water year 1981: U.S. Geological Survey Water Data Report MO-81-1, viii, 394 p., https://doi.org/10.3133/wdrMO811.","productDescription":"viii, 394 p.","costCenters":[],"links":[{"id":135835,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/mo-81-1/report-thumb.jpg"},{"id":496980,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/mo-81-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3109","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531757,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57341,"text":"wdrHI812 - 1982 - Water Resources Data Hawaii, other Pacific Areas, water year 1981: Volume 2. Guam, Northern Mariana Islands, Federated States of Micronesia, Palau Islands and American Samoa","interactions":[],"lastModifiedDate":"2025-12-05T16:53:42.732638","indexId":"wdrHI812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"HI-81-2","title":"Water Resources Data Hawaii, other Pacific Areas, water year 1981: Volume 2. Guam, Northern Mariana Islands, Federated States of Micronesia, Palau Islands and American Samoa","docAbstract":"Volume 2 of water resources data for the 1981 water year for other Pacific areas consist of records of stage, discharge, and water quality of streams; stage of a reservoir; and water levels in wells and springs. This report contains discharge records for 41 gaging stations; stage only record for 2 gaging stations; water quality for 3 gaging stations, 39 partial-record stations; water temperature for 60 gaging stations; and water levels for 10 observation wells. Also included are 47 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Governments and Federal agencies in other Pacific areas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrHI812","collaboration":"Prepared in cooperation with the Governments of Guam, Northern Mariana Islands, Federated States of Micronesia, Palau Islands, American Samoa, and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water Resources Data Hawaii, other Pacific Areas, water year 1981: Volume 2. Guam, Northern Mariana Islands, Federated States of Micronesia, Palau Islands and American Samoa: U.S. Geological Survey Water Data Report HI-81-2, ix, 148 p., https://doi.org/10.3133/wdrHI812.","productDescription":"ix, 148 p.","costCenters":[],"links":[{"id":497149,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/hi-81-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185250,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1981/hi-81-2/report-thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"American Samoa, Federated States of Micronesia, Guam, Northern Mariana Islands, Palau 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd2b2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8398,"text":"ofr82237 - 1982 - New papers related to remote sensing of the earth","interactions":[],"lastModifiedDate":"2025-09-23T16:21:49.447892","indexId":"ofr82237","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-237","title":"New papers related to remote sensing of the earth","docAbstract":"Worldwide experience of many individuals and organizations with remote sensing data acquired from space, primarily Landsat-1, -2, and -3, has demonstrated its utility for land use classification, agricultural assessment, energy and resource exploration, and many other applications. There has been some reluctance to adopt these systems in operational programmes because of a lack of assured continuity of data collection, continuing changes in the systems, and some dissatisfaction with the types of data made available to users. Nevertheless, there is sufficient conviction of the value of satellite remote sensing so that new systems will be developed by several countries in the decade of the 1980's. The status changes continuously as studies are completed, and budgets are adjusted. This review presents the situation at the beginning of 1982.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82237","usgsCitation":"Colvocoresses, A., and Doyle, F., 1982, New papers related to remote sensing of the earth: U.S. Geological Survey Open-File Report 82-237, 34 p., https://doi.org/10.3133/ofr82237.","productDescription":"34 p.","costCenters":[],"links":[{"id":495909,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0237/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142146,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0237/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6975cc","contributors":{"authors":[{"text":"Colvocoresses, A. P.","contributorId":82703,"corporation":false,"usgs":true,"family":"Colvocoresses","given":"A. P.","affiliations":[],"preferred":false,"id":157655,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doyle, F.J.","contributorId":29426,"corporation":false,"usgs":true,"family":"Doyle","given":"F.J.","email":"","affiliations":[],"preferred":false,"id":157654,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70114182,"text":"70114182 - 1982 - Earthquake history of the United States","interactions":[],"lastModifiedDate":"2014-07-15T10:39:29","indexId":"70114182","displayToPublicDate":"1985-01-01T08:28:54","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":63,"text":"Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"41-1","title":"Earthquake history of the United States","docAbstract":"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":70207318,"text":"70207318 - 1982 - Massive sulfide deposits of the Southern Appalachians central Virginia volcanic-plutonic belt as a host for massive sulfide deposits","interactions":[],"lastModifiedDate":"2019-12-17T07:17:01","indexId":"70207318","displayToPublicDate":"1984-01-04T07:11:36","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Massive sulfide deposits of the Southern Appalachians central Virginia volcanic-plutonic belt as a host for massive sulfide deposits","docAbstract":"Strata-bound massive sulfide deposits of the central Virginia Piedmont occur in a volcanic- plutonic belt composed of Lower Cambrian(?) metamorphosed volcanic rocks and locally of pre-Upper Ordovician, low potassium granitoid rocks. The belt, interpreted as an ancient island arc, begins about 50 km south of Washington, D. C, and extends some 175 km south- westward. The volcanic rocks within the belt are located along the flanks of the Quantico- Columbia synclinorium and the Arvonia syncline. The Chopawamsic Formation, a western facies of the belt, consists of volcanic rocks that have the geochemical features (rare earth and immobile elements) of a tholeiitic island-arc suite; it also contains calc-alkaline components. Tholeiitic amphibolites of the Ta River Metamorphic Suite on the eastern side of the belt form an oceanward facies of the island arc, coeval with the Chopawamsic. This distribution suggests an underlying westward-dipping Cambrian(?) subduction zone. Contrasts in stratigraphy, geochemistry, and magnetic and gravity features indicate that the central Virginia volcanic- plutonic belt is not related to the Carolina slate belt as has been proposed in the past. Known sulfide bodies in the Chopawamsic and its coeval units total about 13.5 million tons. The Mineral district on the northwest flank of the Quantico-Columbia synclinorium has the largest deposits and contains about 10 million tons. Sulfide bodies in the belt consist largely of pyrite with minor sphalerite and chalcopyrite; Zn and Pb are important in a few of the smaller deposits. There are local concentrations of sphalerite and other base metal minerals within the major pyritic deposits (Zn = 1-12.5%; Cu - 1-2%; Pb as much as 5%). The dom- inantly sphaleritic deposits are found in and northward for about 15 km from the Mineral district. Sulfide mineralization is found in all types of volcanic rock, but the large sulfide bodies on the northwest flank of the Quantico-Columbia synclinorium are in felsite. Am- phibolite, containing local beds of iron-formation, is abundant on the southeast flank of the Arvonia syncline; however, most sulfide mineralization there took place in felsitic to intermediate layers. Mineralization, attributed to submarine volcanic exhalation, took place during formation of the island arc.
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.
No abstract available.
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","language":"English","publisher":"Inter-Research","usgsCitation":"Cloern, J.E., 1982, Does the benthos control phytoplankton biomass in South San Francisco Bay?: Marine Ecology Progress Series, v. 9, p. 191-202.","productDescription":"12 p.","startPage":"191","endPage":"202","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1980-01-01","temporalEnd":"1980-12-31","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":307045,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307044,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.int-res.com/abstracts/meps/v9/"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.25997924804688,\n 37.76420119453823\n ],\n [\n -122.40829467773436,\n 37.74682893940135\n ],\n [\n -122.39593505859376,\n 37.58703054044867\n ],\n [\n -122.244873046875,\n 37.54784381205082\n ],\n [\n -122.09930419921876,\n 37.43670283999782\n ],\n [\n -121.97158813476561,\n 37.41270958119496\n ],\n [\n -121.90155029296875,\n 37.44106442458555\n ],\n [\n -121.98806762695311,\n 37.50972584293751\n ],\n [\n -122.05123901367186,\n 37.5151724596446\n ],\n [\n -122.11441040039061,\n 37.61423141542417\n ],\n [\n -122.25997924804688,\n 37.76420119453823\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"9","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa30e4b0518e3546bc30","contributors":{"authors":[{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":568982,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70156948,"text":"70156948 - 1982 - The impact of waste-water discharge on biological communities in San Francisco Bay","interactions":[],"lastModifiedDate":"2016-07-27T12:13:58","indexId":"70156948","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"The impact of waste-water discharge on biological communities in San Francisco Bay","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"San Francisco Bay: use and protection","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Association for the Advancement of Science Pacific Division","isbn":"0-934394-04-0","usgsCitation":"Luoma, S., and Cloern, J., 1982, The impact of waste-water discharge on biological communities in San Francisco Bay, chap. of San Francisco Bay: use and protection, p. 137-160.","productDescription":"24 p.","startPage":"137","endPage":"160","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":307864,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307863,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://associations.sou.edu/aaaspd/WebPubs.html"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"560bb70ae4b058f706e53f0c","contributors":{"editors":[{"text":"Kockelman, W. J.","contributorId":55427,"corporation":false,"usgs":true,"family":"Kockelman","given":"W. J.","affiliations":[],"preferred":false,"id":571227,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Luoma, S. N.","contributorId":86353,"corporation":false,"usgs":true,"family":"Luoma","given":"S. N.","affiliations":[],"preferred":false,"id":571225,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cloern, J. E.","contributorId":59453,"corporation":false,"usgs":true,"family":"Cloern","given":"J. E.","affiliations":[],"preferred":false,"id":571226,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70157375,"text":"70157375 - 1982 - Annual report of the USGS Mission, Kingdom of Saudi Arabia, for the first year of the sixth extension of the USGS-MPMR work agreement : fiscal year 1401/02, 1 Rajab 1401-30 Jumad Thani 1402 (5 May 1981-23 April 1982)","interactions":[],"lastModifiedDate":"2015-09-22T11:58:36","indexId":"70157375","displayToPublicDate":"1982-12-31T19:45:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesNumber":"USGS-TR-02-3","title":"Annual report of the USGS Mission, Kingdom of Saudi Arabia, for the first year of the sixth extension of the USGS-MPMR work agreement : fiscal year 1401/02, 1 Rajab 1401-30 Jumad Thani 1402 (5 May 1981-23 April 1982)","docAbstract":"An interagency report prepared by the U.S. Geological Survey Saudi Arabian Mission for the Ministry of Petroleum and Mineral Resources, Kingdom of Saudi Arabia. The work on which this report was based was performed in accordance with a cooperative agreement between the U.S. Geological Survey and the Ministry of Petroleum and Mineral Resources.
","language":"English","publisher":"Ministry of Petroleum and Mineral Resources, Deputy Ministry for Mineral Resources","publisherLocation":"Jiddah, Saudi Arabia","usgsCitation":"U.S. Geological Survey Saudi Arabia Mission, and Saudi Arabia. Deputy Ministry for Mineral Resources, 1982, Annual report of the USGS Mission, Kingdom of Saudi Arabia, for the first year of the sixth extension of the USGS-MPMR work agreement : fiscal year 1401/02, 1 Rajab 1401-30 Jumad Thani 1402 (5 May 1981-23 April 1982), vi, 56 p.","productDescription":"vi, 56 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308360,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Saudi Arabia","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56027bb1e4b03bc34f5447ee","contributors":{"authors":[{"text":"U.S. Geological Survey Saudi Arabia Mission","contributorId":147326,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey Saudi Arabia Mission","id":572911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saudi Arabia. Deputy Ministry for Mineral Resources","contributorId":147327,"corporation":true,"usgs":false,"organization":"Saudi Arabia. Deputy Ministry for Mineral Resources","id":572912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70157272,"text":"70157272 - 1982 - Paleomagnetic investigations of Upper Proterozoic rocks in the eastern Arabian Shield, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-16T16:27:10","indexId":"70157272","displayToPublicDate":"1982-12-31T19:45:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Paleomagnetic investigations of Upper Proterozoic rocks in the eastern Arabian Shield, Kingdom of Saudi Arabia","language":"English","publisher":"Ministry of Petroleum and Mineral Resources, Deputy Ministry for Mineral Resources","publisherLocation":"Jiddah, Saudi Arabia","usgsCitation":"Kellogg, K., Beckmann, G.E., and Saudi Arabia. Deputy Ministry for Mineral Resources, 1982, Paleomagnetic investigations of Upper Proterozoic rocks in the eastern Arabian Shield, Kingdom of Saudi Arabia, Report: iv, 33 p.","productDescription":"Report: iv, 33 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308230,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Saudi Arabia","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55fa92c6e4b05d6c4e501ab2","contributors":{"authors":[{"text":"Kellogg, Karl S.","contributorId":89896,"corporation":false,"usgs":true,"family":"Kellogg","given":"Karl S.","affiliations":[],"preferred":false,"id":572529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beckmann, George E. J.","contributorId":147751,"corporation":false,"usgs":false,"family":"Beckmann","given":"George","email":"","middleInitial":"E. J.","affiliations":[],"preferred":false,"id":572530,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Saudi Arabia. Deputy Ministry for Mineral Resources","contributorId":147344,"corporation":true,"usgs":false,"organization":"Saudi Arabia. Deputy Ministry for Mineral Resources","id":572531,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70207667,"text":"70207667 - 1982 - Managing coastal ecosystems: Progress towards a systems approach","interactions":[],"lastModifiedDate":"2020-01-02T18:06:47","indexId":"70207667","displayToPublicDate":"1982-12-31T18:00:57","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Managing coastal ecosystems: Progress towards a systems approach","docAbstract":"No abstract available.
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","language":"English","publisher":"Gulf Coast Association of Geological Societies","usgsCitation":"Bybell, L.M., 1982, Late Eocene to early Oligocene calcareous nannofossils in Alabama and Mississippi: Gulf Coast Association of Geological Societies Transactions, v. 32, p. 295-302.","productDescription":"8 p.","startPage":"295","endPage":"302","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"links":[{"id":386900,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama, Mississippi","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.47314453125,\n 30.32547125932808\n ],\n [\n -87.374267578125,\n 30.675715404167743\n ],\n [\n -87.57202148437499,\n 31.015278981711266\n ],\n [\n -85.02319335937499,\n 31.015278981711266\n ],\n [\n -85.089111328125,\n 31.700129553985924\n ],\n [\n -84.8583984375,\n 32.37996146435729\n ],\n [\n -85.60546875,\n 34.985003130171066\n ],\n [\n -90.252685546875,\n 35.003003395276714\n ],\n [\n -90.867919921875,\n 34.20725938207231\n ],\n [\n -91.153564453125,\n 33.58716733904656\n ],\n [\n -91.12060546875,\n 32.8149783969858\n ],\n [\n -90.999755859375,\n 32.37996146435729\n ],\n [\n -91.58203125,\n 31.25037814985571\n ],\n [\n -91.593017578125,\n 31.034108344903512\n ],\n [\n -89.71435546875,\n 31.034108344903512\n ],\n [\n -89.82421875,\n 30.65681556429287\n ],\n [\n -89.62646484375,\n 30.230594564932193\n ],\n [\n -89.483642578125,\n 30.059585699708215\n ],\n [\n -87.4951171875,\n 30.07860131571654\n ],\n [\n -87.47314453125,\n 30.32547125932808\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"32","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":818599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221739,"text":"70221739 - 1982 - Biostratigraphy and paleoecology of lower Paleozoic, upper Cretaceous, and lower Tertiary rocks in U.S. Geological Survey New Madrid test wells, Southeastern Missouri","interactions":[],"lastModifiedDate":"2021-06-30T15:40:45.034309","indexId":"70221739","displayToPublicDate":"1982-12-31T10:29:07","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":8946,"text":"Tulane Studies in Geology and Paleontology","active":false,"publicationSubtype":{"id":10}},"title":"Biostratigraphy and paleoecology of lower Paleozoic, upper Cretaceous, and lower Tertiary rocks in U.S. Geological Survey New Madrid test wells, Southeastern Missouri","docAbstract":"The paleontology and biostratigraphy of Tertiary, Cretaceous, and Paleozoic rocks in the upper Mississippi embayment are incompletely known because marine fossils are only locally present in these rocks. This study concerns material from two U.S. Geological Survey test wells drilled in New Madrid County, southeastern Missouri, as part of earthquake hazard studies in the northern Mississippi Embayment. Test well1 sampled lower Tertiary strata to a depth of 146ft; these strata were found to be late Eocene in age on the basis of sporomorphs. Test well1-X, 29ft northwest of well1, provided cuttings and cores from lower Tertiary, Upper Cretaceous, and lower Paleozoic rocks to a total depth of 2,316 ft below the Kelly bushing (at an altitude of 288 ft). Lithologic evidence suggests that the base of the Jackson Formation may be at 270 ft, but sporomorphs indicate that the base of the Jacksonian Stage (upper Eocene) is possibly at a depth of about 350ft in test well1-X. Lithologic units of the Claibornian Stage (middle Eocene) here consist of the Cockfield(?) and Cook Mountain(?) Formations and Memphis Sand, in descending order. The Claibornian could not be subdivided using sporomorphs from cuttings, but sporomorphs show that the top of the Sabinian Stage (top of the lower Eocene) is at about 1,055 ft; lithologically, the top of the Wilcox Group (top of the Flour Island Formation) is at 1,048 ft. Sporomorphs suggest that the top of the lower Sabinian (top of the Paleocene) is within the Flour Island Formation at about 1,105 ft. The next major lithologic break, the top of the Fort Pillow Sand at 1,186 ft, does not coincide with any detectable biostratigraphic boundary. Lithologically, the interval from 1,339 to 1,377 ft may belong to the Old Breastworks Formation; dinoflagellates from cuttings indicate that this interval is likely to be late Midwayan in age and, therefore, correlative with the Naheola Formation of the eastern Gulf Coast. The Porters Creek Clay extends from a probable top at 1,377 ft to 1,691 ft, and the base of the underlying Clayton Formation (Tertiary-Cretaceous contact) is at 1, 703 ft. Calcareous nannofossils, dinoflagellates, foraminifers, mollusks, ostracodes, and sporomorphs from continuous cores of the Porters Creek Clay and Clayton Formation indicate that the upper half of the Porters Creek correlates with the upper part of the same formation or perhaps partly with slightly younger rocks in the eastern Gulf Coast, the lowermost Porters Creek appears to correlate with the upper part of the Clayton Formation of the eastern Gulf Coast and with the Kincaid Formation of Texas, and the thin Clayton of the test well probably correlates with only the lower part of the thicker Clayton of the eastern Gulf Coast. Sporomorphs from McNairy Sand (Upper Cretaceous) cores indicate Maestrichtian and perhaps latest Campanian Age. Lower Paleozoic dolostone from 2,023 ft to total depth at 2,316 ft is barren of identifiable fossils except for a probable fragment of the fish Anatolepis; the dolostone is probably Late Cambrian in age. The McNairy Sand of New Madrid well 1-X seems to have been deposited in nonmarine to nearshore marine environments; the Clayton Formation and lower part of the Porters Creek Clay were deposited under marine conditions during an early Paleocene marine transgression. A major regression followed that continued through the end of Porters Creek time and perhaps into Naheola (late Midwayan) time; the Sabinian, Claibornian, and Jacksonian strata in southeastern Missouri were deposited primarily or entirely in nonmarine environments.
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\"}}]}","volume":"32","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gibson, T. G.","contributorId":190324,"corporation":false,"usgs":false,"family":"Gibson","given":"T. G.","affiliations":[],"preferred":false,"id":818581,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mancini, E. A.","contributorId":18114,"corporation":false,"usgs":true,"family":"Mancini","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":818582,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":818583,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70188938,"text":"70188938 - 1982 - Geologic factors that control mineral matter in coal","interactions":[],"lastModifiedDate":"2017-06-27T16:07:34","indexId":"70188938","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Geologic factors that control mineral matter in coal","docAbstract":"Elements other than organically derived and bound C, H, N, O, and S constitute mineral matter in coal. Mineral matter may consist of discrete minerals such as calcite, quartz, clays, and pyrite, and/or organic compounds that contain organically bonded elements such as Ca and CI. Processes that may affect the association and content of mineral matter are operable from the initial peat-forming stage to the time of utilization of the coal. However, the objective of this paper is to discuss some of the various geologic processes that may influence content and associations in unmined coal.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Atomic and Nuclear Methods in Fossil Energy Research","language":"English","publisher":"Springer","doi":"10.1007/978-1-4684-4133-8_23","usgsCitation":"Cecil, C.B., Stanton, R., Dulong, F., and Renton, J., 1982, Geologic factors that control mineral matter in coal, chap. of Atomic and Nuclear Methods in Fossil Energy Research, p. 323-335, https://doi.org/10.1007/978-1-4684-4133-8_23.","productDescription":"13 p.","startPage":"323","endPage":"335","costCenters":[],"links":[{"id":343038,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59536ee1e4b062508e3c7b1d","contributors":{"editors":[{"text":"Filby, R.H.","contributorId":26071,"corporation":false,"usgs":true,"family":"Filby","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":701408,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Carpenter, Brett","contributorId":193685,"corporation":false,"usgs":false,"family":"Carpenter","given":"Brett","affiliations":[],"preferred":false,"id":701409,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Ragaini, Richard C.","contributorId":147012,"corporation":false,"usgs":false,"family":"Ragaini","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":701410,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Cecil, C. B. 0000-0002-9032-1689","orcid":"https://orcid.org/0000-0002-9032-1689","contributorId":62204,"corporation":false,"usgs":true,"family":"Cecil","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":701404,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanton, R.W.","contributorId":19164,"corporation":false,"usgs":true,"family":"Stanton","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":701405,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dulong, F.T.","contributorId":81490,"corporation":false,"usgs":true,"family":"Dulong","given":"F.T.","affiliations":[],"preferred":false,"id":701406,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Renton, J.J.","contributorId":38716,"corporation":false,"usgs":true,"family":"Renton","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":701407,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70187882,"text":"70187882 - 1982 - Net-mortality of Common Murres and Atlantic Puffins in Newfoundland, 1951-81","interactions":[],"lastModifiedDate":"2017-05-24T17:48:01","indexId":"70187882","displayToPublicDate":"1982-12-31T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Net-mortality of Common Murres and Atlantic Puffins in Newfoundland, 1951-81","docAbstract":"Band recoveries (N = 315) over 26 years (1951-77) and three surveys of seabird bycatch in inshore fishing nets (1972, 1980-81) indicate that there has been a substantial net-mortality of Atlantic Puffins (Fratercula arctica) and Common Murres (Uria aalge) in Newfoundland coastal waters for the past 2 decades. Offshore (e.g. Grand Banks) gill-netting is limited, but some data suggest that murre net-mortality also occurs offshore at murre wintering areas. The vast majority of inshore net-mortality incidents occur over a 2-week period during the annual inshore spawning migration of capelin (Mallotus villosus), the major prey item for alcids in eastern Canada. Most murres (83%) were drowned in bottom-set (30-185 m) cod (Gadus morhua) gill nets, whereas more puffins were drowned in surface-set salmon (Salmo salar) gill nets or cod traps (55%) than in cod gillnets (45%). Murre band recoveries, colony censuses, and fishing-effort data suggest that at the second largest Common Murre colony in Newfoundland (Witless Bay Seabird Sanctuary, 77,000 breeding pairs) net-mortality was relatively low in the 1950s and early 1960s, but increased during the 1960s as the murre population grew in size and gill-net fishing effort increased in the colony area. By 1971, net-mortality accounted for 70% of murre band recoveries and calculations show that almost 30,000 breeding adults, or about 20% of the local breeding population, were drowned in that year. More reliable estimates of alcid bycatch in the Witless Bay area have been made on the basis of actual bycatch surveys. In 1972 about 20,000 adult murres, or 13% of the breeding stock, were killed in gill-nets. Net-mortality of murres apparently diminished through the 1970s as capelin stocks declined and fewer birds foraged in heavily netted inshore areas. Bycatch surveys in the Witless Bay area in 1980-81 revealed that, relative to previous years, murre net-mortality was greatly reduced and resulted in the loss of only 3-4% of the breeding stock. Even these low mortality rates, however, are cause for concern as adult murre mortality from all sources (including hunting, oil, and natural mortality) should not exceed 6-12% per annum to maintain a stable breeding population. Little is known about the magnitude of net-mortality at other major Newfoundland murre colonies though it is known to be a problem in all colony areas. The bycatch of adult Atlantic Puffins in the Witless Bay area was low compared to murre bycatch and in 3 years of study never exceeded 1.6% of the breeding population. During the 1970s, fishing effort increased five-fold in colony areas and we predict that if capelin spawning stocks return to early 1970s size, then net-mortality of puffins and murres in Newfoundland coastal regions will increase dramatically. Indeed, preliminary examination of 1982 capelin spawning and seabird bycatch data suggests that capelin were much more abundant inshore and murre bycatch increased two- to three-fold over 1981.
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