{"pageNumber":"1526","pageRowStart":"38125","pageSize":"25","recordCount":41032,"records":[{"id":70010304,"text":"70010304 - 1983 - Stability of streams and lakes on Mars","interactions":[],"lastModifiedDate":"2024-02-16T12:20:34.967206","indexId":"70010304","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Stability of streams and lakes on Mars","docAbstract":"<div id=\"preview-section-abstract\"><div id=\"abstracts\" class=\"Abstracts u-font-serif text-s\"><div id=\"aep-abstract-id3\" class=\"abstract author\"><div id=\"aep-abstract-sec-id4\"><p>Under present climatic conditions streams and lakes on Mars will freeze. Freezing is slow and would have a negligible effect in impeding flow of the large floods that are believed to have eroded the outflow channels. Valley networks are more difficult to form under current climatic conditions since they appear to have formed by slow erosion by streams of modest discharges. Freezing of small Martian streams was modeled for a variety of climatic conditions on the supposition that the Martian atmosphere may have been considerably thicker in the past when the valley networks formed. The modeling involves examination of the energy balance at the upper and lower surfaces of ice on streams to determine the rate at which the ice thickens with time. The results indicate that freezing rates are not strongly dependent on atmospheric pressure. With no wind, increasing the pressure by a factor of 10 cuts the time taken to freeze solid only by about a factor of about 2. Under windy conditions dependence on atmospheric pressure is even weaker. The distance that water could travel in a stream before flow is arrested by freezing is also calculated. The distances depend on the initial temperature of the stream and when icings develop, but in general, if a stream deeper than 2 m can be initiated and sustained, the water within it can survive long enough to cut most of the valley networks observed. The main problem with forming the valley is initiating the flow. Groundwater seepage alone appears inadequate because of the difficulty of recharging the groundwater system. Melting of ice precipitated onto the surface following injection of water into the atmosphere by large impacts is a possible source of water, but the climatic conditions under which the ice could melt and the water be collected into streams that can survive long enough to cut the valley is uncertain.</p></div></div></div></div><div id=\"preview-section-introduction\"><br></div><div id=\"preview-section-snippets\"><br></div><div id=\"preview-section-references\"><br></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(83)90168-9","issn":"00191035","usgsCitation":"Carr, M.H., 1983, Stability of streams and lakes on Mars: Icarus, v. 56, no. 3, p. 476-495, https://doi.org/10.1016/0019-1035(83)90168-9.","productDescription":"20 p.","startPage":"476","endPage":"495","numberOfPages":"20","costCenters":[],"links":[{"id":219443,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"56","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b965ce4b08c986b31b46d","contributors":{"authors":[{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":358584,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011389,"text":"70011389 - 1983 - Relationship of two lacustrine ostracode species to solute composition and salinity: Implications for paleohydrochemistry ( Limnocythere sappaensis/staplini)","interactions":[],"lastModifiedDate":"2024-01-31T01:31:48.095816","indexId":"70011389","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Relationship of two lacustrine ostracode species to solute composition and salinity: Implications for paleohydrochemistry ( Limnocythere sappaensis/staplini)","docAbstract":"<div id=\"15567849\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Nonmarine ostracode species are indicative of the physical and chemical nature of lacustrine environments. Although salinity has traditionally been regarded as one of the more important parameters that affect the occurrence patterns of lacustrine ostracodes, examination of the solute composition and salinities of the lakes where<span>&nbsp;</span><i>Limnocythere sappaensis</i><span>&nbsp;</span>and<span>&nbsp;</span><i>L. staplini</i><span>&nbsp;</span>live reveals that solute composition and not salinity is the most critical factor that controls their occurrence. The occurrence of these taxa in the modern world is mutually exclusive.<span>&nbsp;</span><i>L. sappaensis</i><span>&nbsp;</span>lives in water that is enriched in Na<sup>+</sup>-HCO<sub>3</sub><sup>−</sup>-<img class=\"content-image\" src=\"https://pubs.geoscienceworld.org/gsa/geology/article/11/8/435/203527/[XSLTMediumImagePath]\" alt=\"graphic\" data-mce-src=\"https://pubs.geoscienceworld.org/gsa/geology/article/11/8/435/203527/[XSLTMediumImagePath]\"><span>&nbsp;</span>and depleted in Ca<sup>2+</sup>.<span>&nbsp;</span><i>L. staplini</i><span>&nbsp;</span>lives in water that is enriched in various combinations of Na<sup>+</sup>-Mg<sup>2+</sup>-Ca<sup>2+</sup>-<img class=\"content-image\" src=\"https://pubs.geoscienceworld.org/gsa/geology/article/11/8/435/203527/[XSLTMediumImagePath]\" alt=\"graphic\" data-mce-src=\"https://pubs.geoscienceworld.org/gsa/geology/article/11/8/435/203527/[XSLTMediumImagePath]\">-Cl<sup>−</sup><span>&nbsp;</span>and is depleted in HCO<sub>3</sub>. These solute compositions are the product of the mineral fractionation processes described by Eugster and Hardie. The positive correlation between these two species occurrences and the mineralogic fractionation processes suggests that these taxa may be used as reliable paleohydrochemical indicators. Studies in progress dealing with other ostracode taxa suggest that saline lacustrine ostracodes can provide a precise method for reconstructing paleohydrochemistry.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1983)11<435:ROTLOS>2.0.CO;2","issn":"00917613","usgsCitation":"Forester, R.M., 1983, Relationship of two lacustrine ostracode species to solute composition and salinity: Implications for paleohydrochemistry ( Limnocythere sappaensis/staplini): Geology, v. 11, no. 8, p. 435-438, https://doi.org/10.1130/0091-7613(1983)11<435:ROTLOS>2.0.CO;2.","productDescription":"4 p.","startPage":"435","endPage":"438","numberOfPages":"4","costCenters":[],"links":[{"id":221585,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50e4a77ee4b0e8fec6cdc4a8","contributors":{"authors":[{"text":"Forester, R. M.","contributorId":76332,"corporation":false,"usgs":true,"family":"Forester","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":360984,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70164341,"text":"70164341 - 1983 - Research in seismology and earthquake engineering in Venezuela","interactions":[],"lastModifiedDate":"2016-03-21T15:03:55","indexId":"70164341","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Research in seismology and earthquake engineering in Venezuela","docAbstract":"<p>Venezuela has been affected by destructive earthquakes for the past four centuries. According to entries in the national seismic catalog, there have been about 180 earthquakes which have caused some type of damage to the country. The most catastrophic earthquake occurred on March 26, 1812, on the Bocono fault system and caused widespread destruction in the cities of Merida and Caracas and claimed an estimated 30,000 lives.</p>\n<p>After the July 29, 1967, damaging earthquake (with a moderate magnitude of 6.3) caused widespread damage to the northern coastal area of Venezuela and to the Caracas Valley, the Venezuelan Government decided to establish a Presidential Earthquake Commission. This commission undertook the task of coordinating the efforts to study the after-effects of the earthquake. The July 1967 earthquake claimed numerous lives and caused extensive damage to the capital of Venezuela. In 1968, the U.S Geological Survey conducted a seismological field study in the northern coastal area and in the Caracas Valley of Venezuela. the objective was to study the area that sustained severe, moderate, and no damage to structures. A reported entitled&nbsp;<i>Ground Amplification Studies in Earthquake Damage Areas: The Caracas Earthquake of 1967&nbsp;</i>documented, for the first time, short-period seismic wave ground-motion amplifications in the Caracas Valley. Figure 1 shows the area of severe damage in the Los Palos Grantes suburb and the correlation with depth of alluvium and the arabic numbers denote the ground amplification factor at each site in the area. the Venezuelan Government initiated many programs to study in detail the damage sustained and to investigate the ongoing construction practices. These actions motivated professionals in the academic, private, and Government sectors to develops further capabilities and self-sufficiency in the fields of engineering and seismology. Allocation of funds was made to assist in training professionals and technicians and in developing new seismological stations and new programs at the national level in earthquake engineering and seismology. A brief description of the ongoing programs in Venezuela is listed below. these programs are being performed by FUNVISIS and by other national organizations listed at the end of this article. &nbsp;&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Urbina, L., and Grases, J., 1983, Research in seismology and earthquake engineering in Venezuela: Earthquake Information Bulletin (USGS), v. 15, no. 1, p. 32-38.","productDescription":"7 p.","startPage":"32","endPage":"38","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316415,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Venezuela","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.4111328125,\n       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]\n}","volume":"15","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b08fe6e4b010e2af2a5e05","contributors":{"authors":[{"text":"Urbina, L.","contributorId":156258,"corporation":false,"usgs":false,"family":"Urbina","given":"L.","email":"","affiliations":[],"preferred":false,"id":597079,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grases, J.","contributorId":156259,"corporation":false,"usgs":false,"family":"Grases","given":"J.","email":"","affiliations":[],"preferred":false,"id":597080,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185619,"text":"70185619 - 1983 - Complexation of copper by aquatic humic substances from different environments","interactions":[],"lastModifiedDate":"2020-01-20T19:52:46","indexId":"70185619","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3352,"text":"Science of the Total Environment","active":true,"publicationSubtype":{"id":10}},"title":"Complexation of copper by aquatic humic substances from different environments","docAbstract":"<p>The copper-complexing properties of aquatic humic substances isolated from eighteen different environments were characterized by potentiometric titration, using a cupric ion selective electrode. Potentiometric data were analyzed using FITEQL, a computer program for the determination of chemical equilibrium constants from experimental data. All the aquatic humic substances could be modelled as having two types of Cu(II)-binding sites: one with K equal to about 10<sup>6</sup> and a concentration of 1.0 ± 0.4 × 10<sup>−6</sup> M(mg C)<sup>−1</sup> and another with K equal to about 10<sup>8</sup> and a concentration of 2.6 ± 1.6 × 10<sup>−7</sup> M(mg C)<sup>−1</sup>.</p><p>A method is described for estimating the Cu(II)-binding sites associated with dissolved humic substances in natural water based on a measurement of dissolved organic carbon, which may be helpful in evaluating chemical processes controlling speciation of Cu and bioavailability of Cu to aquatic organisms.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0048-9697(83)80008-4","usgsCitation":"McKnight, D.M., Feder, G., Thurman, E.M., and Wershaw, R.L., 1983, Complexation of copper by aquatic humic substances from different environments: Science of the Total Environment, v. 28, no. 1-3, p. 65-76, https://doi.org/10.1016/S0048-9697(83)80008-4.","productDescription":"12 p. ","startPage":"65","endPage":"76","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":338320,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"1-3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63040e4b05ec799131119","contributors":{"authors":[{"text":"McKnight, Diane M.","contributorId":59773,"corporation":false,"usgs":false,"family":"McKnight","given":"Diane","email":"","middleInitial":"M.","affiliations":[{"id":16833,"text":"INSTAAR, University of Colorado","active":true,"usgs":false}],"preferred":false,"id":686132,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feder, Gerald L.","contributorId":60192,"corporation":false,"usgs":true,"family":"Feder","given":"Gerald L.","affiliations":[],"preferred":false,"id":686133,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thurman, E. Michael","contributorId":9636,"corporation":false,"usgs":true,"family":"Thurman","given":"E.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":686134,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wershaw, Robert L. rwershaw@usgs.gov","contributorId":4856,"corporation":false,"usgs":true,"family":"Wershaw","given":"Robert","email":"rwershaw@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":686135,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70168856,"text":"70168856 - 1983 - Earthquakes; September-October 1982","interactions":[],"lastModifiedDate":"2016-03-24T16:01:57","indexId":"70168856","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquakes; September-October 1982","docAbstract":"<p>Seismically speaking the months of September and October were very quiet. There were no major (magnitude 7.0-7.9) earthquakes. Guatemala was struck by a moderate earthquake on September 29 causing fatalities and considerable damage.&nbsp;</p>\n<p>In the United States, a number of earthquakes occurred, but only slight damage was reported.&nbsp;</p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Person, W., 1983, Earthquakes; September-October 1982: Earthquake Information Bulletin (USGS), v. 15, no. 2, p. 73-76.","productDescription":"4 p.","startPage":"73","endPage":"76","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318605,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"15","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56dabfd7e4b015c306f84c70","contributors":{"authors":[{"text":"Person, W. J.","contributorId":91472,"corporation":false,"usgs":true,"family":"Person","given":"W. J.","affiliations":[],"preferred":false,"id":621991,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011331,"text":"70011331 - 1983 - HIGH-TEMPERATURE GEOTHERMAL RESOURCES IN HYDROTHERMAL CONVECTION SYSTEMS IN THE UNITED STATES.","interactions":[],"lastModifiedDate":"2012-03-12T17:18:28","indexId":"70011331","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"HIGH-TEMPERATURE GEOTHERMAL RESOURCES IN HYDROTHERMAL CONVECTION SYSTEMS IN THE UNITED STATES.","docAbstract":"The calculation of high-temperature geothermal resources ( greater than 150 degree C) in the United States has been done by estimating the temperature, area, and thickness of each identified system. These data, along with a general model for recoverability of geothermal energy and a calculation that takes account of the conversion of thermal energy to electricity, yielded an estimate of 23,000 MW//e for 30 years. The undiscovered component was estimated based on multipliers of the identified resource as either 72,000 or 127,000 MW//e for 30 years depending on the model chosen for the distribution of undiscovered energy as a function of temperature.","largerWorkTitle":"Electric Power Research Institute, Advanced Power Systems Division, (Report) EPRI AP","conferenceTitle":"Proceedings - Seventh Annual Geothermal Conference and Workshop.","conferenceLocation":"San Diego, CA, USA","language":"English","publisher":"EPRI","publisherLocation":"Palo Alto, CA, USA","usgsCitation":"Nathenson, M., 1983, HIGH-TEMPERATURE GEOTHERMAL RESOURCES IN HYDROTHERMAL CONVECTION SYSTEMS IN THE UNITED STATES., <i>in</i> Electric Power Research Institute, Advanced Power Systems Division, (Report) EPRI AP, San Diego, CA, USA.","costCenters":[],"links":[{"id":220699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2e7ee4b0c8380cd5c5c6","contributors":{"authors":[{"text":"Nathenson, Manuel 0000-0002-5216-984X mnathnsn@usgs.gov","orcid":"https://orcid.org/0000-0002-5216-984X","contributorId":1358,"corporation":false,"usgs":true,"family":"Nathenson","given":"Manuel","email":"mnathnsn@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":360855,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011265,"text":"70011265 - 1983 - Noble gas systematics for coexisting glass and olivine crystals in basalts and dunite xenoliths from Loihi Seamount","interactions":[],"lastModifiedDate":"2023-12-10T22:04:49.183163","indexId":"70011265","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Noble gas systematics for coexisting glass and olivine crystals in basalts and dunite xenoliths from Loihi Seamount","docAbstract":"<p>Noble gas isotopes including<span>&nbsp;</span><sup>3</sup>He/<sup>4</sup>He,<span>&nbsp;</span><sup>40</sup>Ar/<sup>36</sup>Ar and Xe isotope ratios were determined for coexisting glass and olivine crystals in tholeiitic and alkalic basalts and dunite xenoliths from Loihi Seamount.</p><p>Glass and coexisting olivine crystals have similar<span>&nbsp;</span><sup>3</sup>He/<sup>4</sup>He ratios (2.8–3.4) × 10<sup>−5</sup>, 20 to 24 times the atmospheric ratio (<i>R</i><sub>A</sub>), but different<span>&nbsp;</span><sup>40</sup>Ar/<sup>36</sup>Ar ratios (400–1000). Based on the results of noble gas isotope ratios and microscopic observation, some olivine crystals are xenocrysts. We conclude that He is equilibrated between glass and olivine xenocrysts, but Ar is not.</p><p>The apparent high<span>&nbsp;</span><sup>3</sup>He/<sup>4</sup>He ratio (3 × 10<sup>−5</sup>; = 21<span>&nbsp;</span><i>R</i><sub>A</sub>) coupled with a relatively high<span>&nbsp;</span><sup>40</sup>Ar/<sup>36</sup>Ar ratio (4200) for dunite xenoliths (KK 17-5) may be explained by equilibration of He between MORB-type cumulates and the host magma.</p><p>Except for the dunite xenoliths, noble gas data for these Loihi samples are compatible with a model in which samples from hot spot areas may be explained by mixing between P (plume)-type and M (MORB)-type components with the addition of A (atmosphere)-type component.</p><p>Excess<span>&nbsp;</span><sup>129</sup>Xe has not been observed due to apparent large mass fractionation among Xe isotopes.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0012-821X(83)90156-5","issn":"0012821X","usgsCitation":"Kaneoka, I., Takaoka, N., and Clague, D., 1983, Noble gas systematics for coexisting glass and olivine crystals in basalts and dunite xenoliths from Loihi Seamount: Earth and Planetary Science Letters, v. 66, no. C, p. 427-437, https://doi.org/10.1016/0012-821X(83)90156-5.","productDescription":"11 p.","startPage":"427","endPage":"437","numberOfPages":"11","costCenters":[],"links":[{"id":220825,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"66","issue":"C","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6722e4b0c8380cd731cc","contributors":{"authors":[{"text":"Kaneoka, I.","contributorId":77298,"corporation":false,"usgs":true,"family":"Kaneoka","given":"I.","email":"","affiliations":[],"preferred":false,"id":360701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Takaoka, N.","contributorId":51017,"corporation":false,"usgs":true,"family":"Takaoka","given":"N.","email":"","affiliations":[],"preferred":false,"id":360700,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clague, D.A.","contributorId":36129,"corporation":false,"usgs":true,"family":"Clague","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":360699,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70142182,"text":"70142182 - 1983 - The role of remotely sensed and other special data for predictive modeling: the Umatilla, Oregon example","interactions":[],"lastModifiedDate":"2017-01-18T14:44:47","indexId":"70142182","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"The role of remotely sensed and other special data for predictive modeling: the Umatilla, Oregon example","docAbstract":"<p>Landsat data and 1:24 000-scale aerial photographs were initially used to map the expansion of irrigation from 1973 to 1979 and to identify crops under irrigation in 1979. The crop data were then used with historical water requirement figures and digital topographic and hydrographic data to estimate water and power use for the 1979 irrigation season. The final project task involved production of a composite map of land suitability for irrigation development based on land cover (from Landsat), landownership, soil irrigability, slope gradient, and potential energy costs.</p>","language":"English","publisher":"American Society for Photogrammetry and Remote Sensing","usgsCitation":"Loveland, T., and Johnson, G., 1983, The role of remotely sensed and other special data for predictive modeling: the Umatilla, Oregon example: Photogrammetric Engineering and Remote Sensing, v. 49, no. 8, p. 1183-1192.","productDescription":"10 p.","startPage":"1183","endPage":"1192","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":298225,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","city":"Umatilla","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.42413330078125,\n              45.87471224890479\n            ],\n            [\n              -119.42413330078125,\n              45.954968795113395\n            ],\n            [\n              -119.26071166992186,\n              45.954968795113395\n            ],\n            [\n              -119.26071166992186,\n              45.87471224890479\n            ],\n            [\n              -119.42413330078125,\n              45.87471224890479\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"49","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54f597cee4b02419550d2f55","contributors":{"authors":[{"text":"Loveland, Thomas R. 0000-0003-3114-6646 loveland@usgs.gov","orcid":"https://orcid.org/0000-0003-3114-6646","contributorId":3005,"corporation":false,"usgs":true,"family":"Loveland","given":"Thomas R.","email":"loveland@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":541700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Gary E.","contributorId":65007,"corporation":false,"usgs":true,"family":"Johnson","given":"Gary E.","affiliations":[],"preferred":false,"id":541701,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011310,"text":"70011310 - 1983 - Land-use planning: One geologist's viewpoint","interactions":[],"lastModifiedDate":"2023-10-20T16:39:42.048953","indexId":"70011310","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1531,"text":"Environmental Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Land-use planning: One geologist's viewpoint","docAbstract":"<div class=\"abstract-content\"><div class=\"abstract\" data-abstract-type=\"text-abstract\"><p>Planning for the best use of land and its resources should take fully into consideration the long-term consequences of each type of use in order to stretch out most beneficially the well-being of society in the future, and to protect the integrity of the land and its biota. Three kinds of land-use can be distinguished for planning purposes.<span>&nbsp;</span><span class=\"italic\">Reversible</span><span>&nbsp;</span>land-use leaves the land, after use, essentially as it was before; little or no man-induced modification remains. An example of reversible use in the United States is the designation of certain public lands as Wilderness.<span>&nbsp;</span><span class=\"italic\">Terminal</span><span>&nbsp;</span>land-use commits the land to a chosen particular use, and any attempt at reversal requires either time-scales that are long compared with the expected lifespan of the social and political institution, or a commitment of resources that is too high for society to consider worth bearing. Examples of terminal land-use are location of metropolises and sites of toxic and/or radioactive waste disposals; by its nature the list grows monotonically. A current source of some social tension arises from the fact that Wilderness designation appears to assign a terminal-use status by legislative fiat, whereas in fact the land is being used reversibly.</p></div></div>","language":"English","publisher":"Cambridge University Press","doi":"10.1017/S0376892900012182","usgsCitation":"Zen, E., 1983, Land-use planning: One geologist's viewpoint: Environmental Conservation, v. 10, no. 2, p. 97-104, https://doi.org/10.1017/S0376892900012182.","productDescription":"8 p.","startPage":"97","endPage":"104","numberOfPages":"8","costCenters":[],"links":[{"id":221439,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"2","noUsgsAuthors":false,"publicationDate":"2009-08-24","publicationStatus":"PW","scienceBaseUri":"505a43c0e4b0c8380cd665b7","contributors":{"authors":[{"text":"Zen, E-An","contributorId":47064,"corporation":false,"usgs":true,"family":"Zen","given":"E-An","email":"","affiliations":[],"preferred":false,"id":360796,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70140556,"text":"70140556 - 1983 - Synthesis of geophysical data with space-acquired imagery: a review","interactions":[],"lastModifiedDate":"2017-12-14T16:41:05","indexId":"70140556","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":661,"text":"Advances in Space Research","active":true,"publicationSubtype":{"id":10}},"title":"Synthesis of geophysical data with space-acquired imagery: a review","docAbstract":"<p>Geophysical data obtained from ground and airborne platforms have been used in the development of regional geologic models for many years. Space-acquired data and imagery have a shorter but similar history of applications. All these data may be synthesized either manually or digitally. Manual synthesis methods consist of overlaying and comparing maps, whereas digital synthesis methods consist of computer storage and analysis of registered digital data sets.</p>\n<p>A data base may include topographic, geologic, soils, aeromagnetic, gravity, radiometric, electromagnetic and geochemical data, and Landsat, Seasat, and Heat Capacity Mapping Mission (HCMM) images, all of which can be evaluated individually or compared in multiple layers (overlays).</p>\n<p>Stereographic models, useful in the correlation and interpretation of geophysical data, have been created from Landsat images by using aeromagnetic, gravity, geochemical, or topographic values to offset Landsat pixels, thus introducing parallax and permitting stereoscopic viewing.</p>\n<p>Statistical correlation has been used to determine the applicability of specific data sets to the development of geologic or exploration models. Various arithmetic functions have proven useful in developing models from such data sets.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0273-1177(83)90116-3","usgsCitation":"Hastings, D.A., 1983, Synthesis of geophysical data with space-acquired imagery: a review: Advances in Space Research, v. 3, no. 2, p. 157-168, https://doi.org/10.1016/0273-1177(83)90116-3.","productDescription":"12 p.","startPage":"157","endPage":"168","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":297837,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"54dd2c67e4b08de9379b379a","contributors":{"authors":[{"text":"Hastings, David A.","contributorId":138985,"corporation":false,"usgs":true,"family":"Hastings","given":"David","email":"","middleInitial":"A.","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":false,"id":540071,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17967,"text":"ofr83504 - 1983 - Cenozoic structural history of selected areas in the eastern Great Basin, Nevada-Utah","interactions":[],"lastModifiedDate":"2023-03-03T22:37:00.831466","indexId":"ofr83504","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"83-504","title":"Cenozoic structural history of selected areas in the eastern Great Basin, Nevada-Utah","docAbstract":"The Confusion Range structural trough (CRST) of west-central Utah predates the Oligocene rocks that are exposed along it. The northern part of the axial region of the CRST is complicated by structures that include reverse faults and associated folds, a large-amplitude mushroom fold, and belts of sharply flexed to overturned strata some of which are fault bounded. These structures, which also predate the Oligocene rocks, formed in a compressional regime that has been interpreted as resulting from thin-skinned gravitational gliding toward the axis of the CRST. \r\n\r\nStudy of the sparse Tertiary rocks that are scattered along the axial region of the CRST reveals abundant evidence of Oligocene and younger deformation. The chief evidence includes (1) widespread Oligocene and Miocene coarse clastic rocks, many of which are conglomerates, that attest to local and distant tectonism, (2) faults that range from high-angle structures generally with less than 100 m of normal displacement to low-angle attenuation faults some of which may have large displacements, and (3) open asymmetric folds. Together with the distribution of sheet-form bodies of ash-flow tuffs, the Oligocene stratigraphic record allows for paleogeographic reconstruction of a lacustrine basin across what is now the northern Confusion Range and one or more basins in the southern part of the CRST. The basins are inferred to have been fault controlled by reactivation of previously formed faults or steep fold flanks. They may have been localized by differential vertical movements similar to those that produced the older systems of folds and faults. Parts of early formed basins were cannibalized as local syndepositional deformation took place in the axial region of the CRST. \r\n\r\nBoth limbs of the CRST have been modified by folds that involve Oligocene rocks. Some of these folds appear to be genetically related to displacements on faults that bound them. They may record thin-skinned Neogene tectonic displacements toward the axis of the CRST. \r\n\r\nThe most intensely faulted and tilted rocks along the axis of the CRST are located in the Tunnel Spring Mountains where Miocene(?) extension on closely spaced listric faults produced as much as 70 percent extension locally. Three episodes of Oligocene-Miocene deformation, all interpreted to have formed in an extensional environment, are recognized in the Tunnel Spring Mountains. The nearby Burbank Hills area may have been involved in the same deformational episodes, though there the relationships are not as clear-cut nor does evidence occur of extreme extension. Tight asymmetric folds in the Burbank Hills are interpreted as drape structures formed over buried normal faults. Other structures along the southern CRST have fold-like forms, but they result from cross-strike alternations in fault-related tilt directions, and they formed in an extensional stress regime. Least-principal stress directions inferred from orientations of extensional structures vary from ENE-WSW in the southern Tunnel Spring Mountains to approximately E-W in the Disappointment Hills and NW-SE in selected areas east of the axis of the CRST. The size, geographic distribution, and new data on the age of areas of major extensional faulting preclude previously published interpretations that the extension is related to major east-directed overthrusting of the Sevier orogeny in areas east of the hinterland of west-central Utah.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83504","usgsCitation":"Anderson, R.E., 1983, Cenozoic structural history of selected areas in the eastern Great Basin, Nevada-Utah: U.S. Geological Survey Open-File Report 83-504, Report: i, 47 p.; 2 Plates: 19.14 x 10.65 inches and 18.40 x 15.48 inches, https://doi.org/10.3133/ofr83504.","productDescription":"Report: i, 47 p.; 2 Plates: 19.14 x 10.65 inches and 18.40 x 15.48 inches","costCenters":[],"links":[{"id":108459,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14070.htm","linkFileType":{"id":5,"text":"html"},"description":"14070"},{"id":47206,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0504/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47205,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0504/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":47204,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0504/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151228,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0504/report-thumb.jpg"}],"country":"United States","state":"Nevada, Utah","otherGeospatial":"eastern Great Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114.708,\n              39.833\n            ],\n            [\n              -114.708,\n              38.75\n            ],\n            [\n              -113.647,\n              38.75\n            ],\n            [\n              -113.647,\n              39.833\n            ],\n            [\n              -114.708,\n              39.833\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6ef3","contributors":{"authors":[{"text":"Anderson, R. Ernest","contributorId":104484,"corporation":false,"usgs":true,"family":"Anderson","given":"R.","email":"","middleInitial":"Ernest","affiliations":[],"preferred":false,"id":178298,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70135757,"text":"70135757 - 1983 - Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling","interactions":[],"lastModifiedDate":"2017-08-24T12:56:52","indexId":"70135757","displayToPublicDate":"1982-12-27T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling","docAbstract":"<p><span>Gravity models computed for a profile across the long-wavelength paired negative-positive Bouguer anomalies of the southern Appalachian Mountains show that the large negative anomaly can be explained by a crustal root zone, whereas the steep gradient and positive anomaly east of the root may be explained equally well by three different geometries: a suture zone, a mantle upwarp, or a shallow body. Seismic data support the existence of a mountain root but are inadequate to resolve differences among the three possible geometries for the positive anomaly. The presence of outcropping mafic and ultramafic rocks in the southern Appalachians and the inferred tectonic history of the Appalachian orogen are most consistent with the suture-zone model. Crust similar to continental crust probably exists beneath the Coastal Plain and inner continental shelf where the gravity anomalies return to near-zero values.</span></p>","language":"English","publisher":"Geological Society of  America","doi":"10.1130/0091-7613(1983)11<611:CSBTSA>2.0.CO;2","usgsCitation":"Hutchinson, D.R., Grow, J., and Klitgord, K.D., 1983, Crustal structure beneath the southern Appalachians: Nonuniqueness of gravity modeling: Geology, v. 11, no. 10, p. 611-615, https://doi.org/10.1130/0091-7613(1983)11<611:CSBTSA>2.0.CO;2.","productDescription":"5 p.","startPage":"611","endPage":"615","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":296724,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Appalachian Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -69.01611328125,\n              47.502358951968596\n            ],\n            [\n              -66.6650390625,\n              45.336701909968106\n            ],\n            [\n              -86.484375,\n              31.82156451492074\n            ],\n            [\n              -88.2861328125,\n              33.65120829920497\n            ],\n            [\n              -69.01611328125,\n              47.502358951968596\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"11","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"549165bfe4b0d0759afaad80","contributors":{"authors":[{"text":"Hutchinson, Deborah R. 0000-0002-2544-5466 dhutchinson@usgs.gov","orcid":"https://orcid.org/0000-0002-2544-5466","contributorId":521,"corporation":false,"usgs":true,"family":"Hutchinson","given":"Deborah","email":"dhutchinson@usgs.gov","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":536831,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grow, John A.","contributorId":51739,"corporation":false,"usgs":true,"family":"Grow","given":"John A.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":536832,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klitgord, Kim D.","contributorId":82307,"corporation":false,"usgs":true,"family":"Klitgord","given":"Kim","email":"","middleInitial":"D.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":536833,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70180225,"text":"70180225 - 1982 - Aeromagnetic survey of the Chignik and Sutwik Island quadrangles: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1980</i>","interactions":[{"subject":{"id":70180225,"text":"70180225 - 1982 - Aeromagnetic survey of the Chignik and Sutwik Island quadrangles: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1980</i>","indexId":"70180225","publicationYear":"1982","noYear":false,"title":"Aeromagnetic survey of the Chignik and Sutwik Island quadrangles: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1980</i>"},"predicate":"IS_PART_OF","object":{"id":4434,"text":"cir844 - 1982 - The United States Geological Survey in Alaska: Accomplishments during 1980","indexId":"cir844","publicationYear":"1982","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1980"},"id":1}],"isPartOf":{"id":4434,"text":"cir844 - 1982 - The United States Geological Survey in Alaska: Accomplishments during 1980","indexId":"cir844","publicationYear":"1982","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1980"},"lastModifiedDate":"2017-01-27T11:11:59","indexId":"70180225","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"844","title":"Aeromagnetic survey of the Chignik and Sutwik Island quadrangles: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1980</i>","docAbstract":"<p>The recently completed aeromagnetic survey of the Chignik and Sutwik Island quadrangles, on the Alaska Peninsula, is one of the most detailed systematic surveys ever made across a modern \"volcanic arc\" setting where both Holocene volcanic edifices and older volcanic centers occur (fig. 54). </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The United States Geological Survey in Alaska: Accomplishments during 1980 (Circular 844)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Alexandria, VA","doi":"10.3133/70180225","usgsCitation":"Case, J.E., Cox, D.P., Detra, D.E., Detterman, R.L., and Wilson, F.H., 1982, Aeromagnetic survey of the Chignik and Sutwik Island quadrangles: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1980</i>: U.S. Geological Survey Circular 844, 2 p., https://doi.org/10.3133/70180225.","productDescription":"2 p.","startPage":"88","endPage":"89","numberOfPages":"2","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":333981,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333980,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1982/0844/report.pdf#page=96","text":"Start page in larger work"}],"country":"United States","state":"Alaska","otherGeospatial":"Chignik, Sutwik Island","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7c7e4b0ba3b075e065e","contributors":{"authors":[{"text":"Case, James E.","contributorId":68702,"corporation":false,"usgs":true,"family":"Case","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":660809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cox, Dennis P. dcox@usgs.gov","contributorId":2766,"corporation":false,"usgs":true,"family":"Cox","given":"Dennis","email":"dcox@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":660810,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Detra, David E.","contributorId":17342,"corporation":false,"usgs":true,"family":"Detra","given":"David","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":660811,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":660812,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":660813,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70043184,"text":"70043184 - 1982 - A topology of mineralization and its meaning for prospecting","interactions":[{"subject":{"id":10514,"text":"ofr80298 - 1980 - A topology of mineralization and its meaning for prospecting","indexId":"ofr80298","publicationYear":"1980","noYear":false,"title":"A topology of mineralization and its meaning for prospecting"},"predicate":"SUPERSEDED_BY","object":{"id":70043184,"text":"70043184 - 1982 - A topology of mineralization and its meaning for prospecting","indexId":"70043184","publicationYear":"1982","noYear":false,"title":"A topology of mineralization and its meaning for prospecting"},"id":1}],"lastModifiedDate":"2013-02-20T08:55:41","indexId":"70043184","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"A topology of mineralization and its meaning for prospecting","docAbstract":"Epigenetic mineral deposits are universal members of an orderly spatial and temporal arrangement of igneous rocks, endomorphic rocks, and hydrothermally altered rocks. The association and sequence of these rocks is invariant whereas the metric relations and configurations of the properties of these rocks are unlimited in variety. This characterization satisfies the doctrines of topology. Metric relations are statistical, and their modes are among the better guides to optimal areas for exploration. Metric configurations are graphically irregular and unpredictable mathematical surfaces like mountain topography. Each mineral edifice must be mapped to locate its mineral deposits. All measurements and observations are only positive or neutral for the occurrence of a mineral deposit. Effective prospecting is based on an increasing density of positive data with proximity to the mineral deposit. This means sampling for maximal numbers of positive data, pragmatically the highest ore-element assays at each site, by selecting rock showing maximal development of lode attributes.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Ore Genesis: Special Publication of the Society for Geology Applied to Mineral Deposits","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Springer","publisherLocation":"Amsterdam, Netherlands","doi":"10.1007/978-3-642-68344-2_62","usgsCitation":"Neuerburg, G.J., 1982, A topology of mineralization and its meaning for prospecting, chap. <i>of</i> Ore Genesis: Special Publication of the Society for Geology Applied to Mineral Deposits, v. 2, p. 657-666, https://doi.org/10.1007/978-3-642-68344-2_62.","productDescription":"10 p.","startPage":"657","endPage":"666","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":267099,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267098,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/978-3-642-68344-2_62"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5114daf2e4b0ca7af0743aef","contributors":{"authors":[{"text":"Neuerburg, G. J.","contributorId":29395,"corporation":false,"usgs":true,"family":"Neuerburg","given":"G.","middleInitial":"J.","affiliations":[],"preferred":false,"id":473122,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70038344,"text":"70038344 - 1982 - Water resources inventory of Connecticut Part 10: Lower Connecticut River basin","interactions":[],"lastModifiedDate":"2014-06-27T11:19:00","indexId":"70038344","displayToPublicDate":"2012-05-01T11:47:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"31","title":"Water resources inventory of Connecticut Part 10: Lower Connecticut River basin","docAbstract":"</p>The lower Connecticut River basin study area in south-central Connecticut includes 639 square miles and is drained principally by the Connecticut River and by seven smaller streams that flow directly to Long Island Sound between the West River on the west and the Connecticut River on the east. The population in 1979 was estimated to be 210,380. Much of the industrial development and population centers are in the Mattabesset River basin in the northwestern part, and the largest water use is also in the Mattabesset River basin.</p>\n<br>\n<p>Precipitation averages 47 inches per year and provides an abundant supply of water. About 20 inches returns to the atmosphere as evapotranspiration, and the remainder either flows directly to streams or percolates to the water table, eventually discharging to Long Island Sound. Small quantities of water are exported from the basin by the New Haven and Meridan Water Departments, and small quantities are imported by the New Britain Water Department and Metropolitan Direct Commission. Precipitation during 1931-60 resulted in an average annual runoff of 302 billion gallons. In inflow from the Connecticut River is added to the average annual runoff, the 4,370 billion gallon s per year is potentially available for water ue.</p>\n<br>\n<p>The domestic, institutional, commercial, and industrial (other than cooling water) water use for 1970 was 7 billion gallons, which is only 3 percent of the total water used, whereas 97 percent of the total is cooling water for power plants. Approximately 60 percent of the 7 billion gallons is treated before being discharged back to the streams.</p>\n<br>\n<p>The total amount of fresh water used during 1970 was estimated to be 256,000 million gallons (Mgal), of which 247,000 Mgal was used for cooling water at stream electric-generating plants. The quantity for domestic, commercial, industrial, and agricultural used was 9,000 Mgal, which was approximately 120 gallons a day per person. Public water systems providing 70 percent of these requirement and all the systems supplying water met the drinking water standards of the Connecticut General Assembly (1975).</p>\n<br>\n<p>Till is widespread and generally provides only small amounts of water. Wells in till normally yield only a few hundred gallons of water daily and may be inadequate during dry periods. The thickness of of till ranges from 0 to 15 feet; a median thickness of 26 feet is estimated from information provided in drillers' logs of 467 wells penetrating underlying bedrock. The till is generally used only as an emergency or secondary source of water.</p>\n<br>\n<p>Bedrock aquifers underlie the entire area and include sedimentary and crystalline (igneous and metamorphic) rock types. These aquifers supply small and usually reliable quantities of water to wells and are the chief source of water for many rural homes and farms., About 90 percent of the wells tapping bedrock yield at least 2 gal/min. The median yields from wells tapping aquifers in sedimentary, igneous, and metamorphic rocks are 11, 8, and 6.5 gal/min, respectively.</p>\n<br>\n<p>The quantity of water potentially available from stratified drift was estimated on the basis of hydraulic characteristics of the aquifers, mathematical modeling of the aquifer system, and evaluation of natural and induced recharge. Long-term yields estimated or ten areas underlain by significant thickness of stratified drift range from 0.4 to 4.4 million gallons per day (Mgal/d). A change in well spacing or numbering could increase the long-term yields, but detailed modeling verification studies are needed to confirm optimal well locations.</p>\n<br>\n<p>The chemical and physical (turbidity, color, taste, and sediment load) quality of water is good. The water if generally low in dissolved solids and is classified as soft to hard. Surface water is less mineralized than ground water, especially during high flow, when it is primarily derived from surface runoff rather than groundwater runoff. A median dissolved-solids concentration of 42 milligrams per liter (mg/L) and median hardness of 18 mg/L were determined from water samples collected from 26 streams during the high-flow period. During the low-flow period, median dissolved-solids concentration of 61 mg/L and median hardness of 27 mg/L were determined from sample from the same streams.</p>\n<br>\n<p>The quality of water in stratified-drift and crystalline-rock aquifers is generally better than that in the sedimentary-rock aquifers. Water from 32 wells tapping stratified drift had median dissolved-solids concentrations of 116 mg/L; and 33 wells tapping stratified drift and 42 tapping crystalline rock had median hardness of 73 mg/L and 68 mg/L, respectively. Water from 32 wells tapping sedimentary rock had median dissolved concentrations of 231 and 156 mg/L, respectively. Sedimentary rock generally yields the hardest water.</p>\n<br>\n<p>Iron and manganese occur objectionable concentrations in places, particularly in water from streams draining swamps and in water from aquifers either rich in iron and manganese-nearing minerals or where the reducing environment for solution of these minerals is favorable. Concentrations of iron in excess of 0.3 mg/L were found in 35 percent of the high streamflow samples, and in 45 percent of the ground-water samples. Most of the high iron and manganese concentration in streams and aquifers are found east of the Connecticut River.</p>\n<br>\nHuman activities and tidal influence along the coast have modified the quality of water in much f the study area. The greatest influence from human activities has been in the northwestern part, in the Mattabesset River basin. There, the quality of water has been affected by domestic and animal wastes, which cause high dissolved-solids concentrations, high nitrate and phosphate loads and high bacterial counts. In the entire area, high nitrate in groundwater occur only locally, and its presence in an individual water supply is chiefly a function of its proximity to sources of contamination, of well construction, and of thickness of overburden. Thirty public-supply wells did have water that had high sodium concentrations or objectionable iron and manganese concentrations, but these are not considered health hazards in the concentrations found in the water samples. Streams, wetlands, and some aquifers along the sough boundary of the basin contain salty water because of tidal movement or extensive ground-water withdrawals. High sediment concentrations also occur as a result of tidal influence in this area.</p>","language":"English","publisher":"Connecticut Department of Environmental Protection","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Weiss, L.A., Bingham, J.W., and Thomas, M.P., 1982, Water resources inventory of Connecticut Part 10: Lower Connecticut River basin: Connecticut Water Resources Bulletin 31, Report: viii, 85 p.; 5 Plates: 42.00 x 30.34 inches and smaller.","productDescription":"Report: viii, 85 p.; 5 Plates: 42.00 x 30.34 inches and smaller","numberOfPages":"94","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":258824,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0031/report.pdf","size":"27252","linkFileType":{"id":1,"text":"pdf"}},{"id":258825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0031/report-thumb.jpg"},{"id":286232,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038344/plate-c.pdf"},{"id":286233,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038344/plate-d.pdf"},{"id":286234,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038344/plate-e.pdf"},{"id":286230,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038344/plate-a.pdf"},{"id":286231,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038344/plate-b.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Lower Connecticut River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.833333,41.233333 ], [ -72.833333,41.8 ], [ -72.2,41.8 ], [ -72.2,41.233333 ], [ -72.833333,41.233333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb76e4b08c986b32d675","contributors":{"authors":[{"text":"Weiss, Lawrence A.","contributorId":102528,"corporation":false,"usgs":true,"family":"Weiss","given":"Lawrence","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bingham, James W.","contributorId":36939,"corporation":false,"usgs":true,"family":"Bingham","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":463917,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463919,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70000678,"text":"70000678 - 1982 - Sonographs of submarine sediment failure caused by the 1980 earthquake off northern California","interactions":[],"lastModifiedDate":"2012-03-08T17:16:36","indexId":"70000678","displayToPublicDate":"2010-09-28T23:09:28","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Sonographs of submarine sediment failure caused by the 1980 earthquake off northern California","docAbstract":"In 1980, a large earthquake caused extensive sediment failure on the shallow continental shelf off the Klamath River in northern California. Side-scan sonography was used to complement detailed geophysical profiling in identifying specific features and resolving modes of failure. The features include a nearly flat failure terrace mantled with sand boils, collapse craters and sediment flows, and bounded on the seaward side by a meandering continuous toe ridge. Seaward of the terrace lies a compression zone delineated by small pressure ridges. Our findings indicate a temporal progression of failure from lique-faction of shallow subsurface sand to lateral spread of intact blocks to sediment collapse and flow. ?? 1982 A. M. Dowden, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462754","issn":"02760460","usgsCitation":"Field, M., and Hall, R.K., 1982, Sonographs of submarine sediment failure caused by the 1980 earthquake off northern California: Geo-Marine Letters, v. 2, no. 3-4, p. 135-141, https://doi.org/10.1007/BF02462754.","startPage":"135","endPage":"141","costCenters":[],"links":[{"id":203636,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18997,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462754"}],"volume":"2","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e77db","contributors":{"authors":[{"text":"Field, M.E.","contributorId":27052,"corporation":false,"usgs":true,"family":"Field","given":"M.E.","affiliations":[],"preferred":false,"id":346462,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hall, R. K.","contributorId":11233,"corporation":false,"usgs":true,"family":"Hall","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":346461,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70000682,"text":"70000682 - 1982 - Channel systems and lobe construction in the Mississippi Fan","interactions":[],"lastModifiedDate":"2012-03-08T17:16:34","indexId":"70000682","displayToPublicDate":"2010-09-28T23:09:26","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1742,"text":"Geo-Marine Letters","active":true,"publicationSubtype":{"id":10}},"title":"Channel systems and lobe construction in the Mississippi Fan","docAbstract":"Morphological features on the Mississippi Fan in the eastern Gulf of Mexico were mapped using GLORIA II, a long-range side-scan sonar system. Prominent is a sinuous channel flanked by well-developed levees and occasional crevasse splays. The channel follows the axis and thickest part of the youngest fan lobe; seismic-reflection profiles offer evidence that its course has remained essentially constant throughout lobe development. Local modification and possible erosion of levees by currents indicates a present state of inactivity. Superficial sliding has affected part of the fan lobe, but does not appear to have been a factor in lobe construction. ?? 1982 A. M. Dowden, Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Geo-Marine Letters","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF02462797","issn":"02760460","usgsCitation":"Garrison, L.E., Kenyon, N.H., and Bouma, A., 1982, Channel systems and lobe construction in the Mississippi Fan: Geo-Marine Letters, v. 2, no. 1-2, p. 31-39, https://doi.org/10.1007/BF02462797.","startPage":"31","endPage":"39","costCenters":[],"links":[{"id":203652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":19001,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02462797"}],"volume":"2","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e607b","contributors":{"authors":[{"text":"Garrison, L. E.","contributorId":66676,"corporation":false,"usgs":true,"family":"Garrison","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":346471,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kenyon, Neil H.","contributorId":89535,"corporation":false,"usgs":false,"family":"Kenyon","given":"Neil","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":346472,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bouma, A.H.","contributorId":107281,"corporation":false,"usgs":true,"family":"Bouma","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":346473,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221796,"text":"5221796 - 1982 - Medical and husbandry aspects of captive Andean condors: A model for the California condor","interactions":[],"lastModifiedDate":"2012-02-02T00:14:47","indexId":"5221796","displayToPublicDate":"2010-06-16T12:19:29","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":704,"text":"American Association of Zoo Veterinarians, Annual Proceedings","active":true,"publicationSubtype":{"id":10}},"title":"Medical and husbandry aspects of captive Andean condors: A model for the California condor","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"American Association of Zoo Veterinarians, Annual Proceedings","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Carpenter, J.W., 1982, Medical and husbandry aspects of captive Andean condors: A model for the California condor: American Association of Zoo Veterinarians, Annual Proceedings, v. 1982, p. 13-19.","productDescription":"13-19","startPage":"13","endPage":"19","numberOfPages":"7","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1982","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db6100d1","contributors":{"authors":[{"text":"Carpenter, J. W.","contributorId":81854,"corporation":false,"usgs":true,"family":"Carpenter","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":334703,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221729,"text":"5221729 - 1982 - Optimal stochastic control in natural resource management: Framework and examples","interactions":[],"lastModifiedDate":"2012-02-02T00:14:39","indexId":"5221729","displayToPublicDate":"2010-06-16T12:19:29","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1458,"text":"Ecological Modelling","active":true,"publicationSubtype":{"id":10}},"title":"Optimal stochastic control in natural resource management: Framework and examples","docAbstract":"A framework is presented for the application of optimal control methods to natural resource problems.  An expression of the optimal control problem appropriate for renewable natural resources is given and its application to Markovian systems is presented in some detail.  Three general approaches are outlined for determining optimal control of infinite time horizon systems and three examples from the natural resource literature are used for illustration.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Ecological Modelling","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0304-3800(82)90012-6","collaboration":"2798_Williams.pdf","usgsCitation":"Williams, B.K., 1982, Optimal stochastic control in natural resource management: Framework and examples: Ecological Modelling, v. 16, no. 2-4, p. 275-297, https://doi.org/10.1016/0304-3800(82)90012-6.","productDescription":"275-297","startPage":"275","endPage":"297","numberOfPages":"23","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18421,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://dx.doi.org/10.1016/0304-3800(82)90012-6","linkFileType":{"id":5,"text":"html"}}],"volume":"16","issue":"2-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db6913a2","contributors":{"authors":[{"text":"Williams, B. Kenneth","contributorId":107798,"corporation":false,"usgs":true,"family":"Williams","given":"B.","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":334543,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221771,"text":"5221771 - 1982 - Capturing birds with mist nets: A review","interactions":[],"lastModifiedDate":"2012-02-02T00:14:45","indexId":"5221771","displayToPublicDate":"2010-06-16T12:19:26","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2881,"text":"North American Bird Bander","active":true,"publicationSubtype":{"id":10}},"title":"Capturing birds with mist nets: A review","docAbstract":"Herein we have tried to provide a comprehensive review of mist-netting techniques suitable for both novice and experienced netters. General mist-netting procedures and modifications developed by netters for particular bird species and habitats are included. Factors which influence capture success, including site selection, net specifications and placement, weather, and time of day, are discussed. Guidelines are presented for the care of netted birds and the use of mist-net data in the study of bird communities. The advantages of the use of mist nets over other methods of capturing birds are also discussed.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"North American Bird Bander","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Keyes, B., and Grue, C., 1982, Capturing birds with mist nets: A review: North American Bird Bander, v. 7, no. 1, p. 2-14.","productDescription":"2-14","startPage":"2","endPage":"14","numberOfPages":"13","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":18356,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://elibrary.unm.edu/sora/NABB/v007n01/p0002-p0014.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":197062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5cf6","contributors":{"authors":[{"text":"Keyes, B.E.","contributorId":22878,"corporation":false,"usgs":true,"family":"Keyes","given":"B.E.","email":"","affiliations":[],"preferred":false,"id":334643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grue, C.E.","contributorId":86446,"corporation":false,"usgs":true,"family":"Grue","given":"C.E.","affiliations":[],"preferred":false,"id":334644,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221784,"text":"5221784 - 1982 - Techniques for trapping, aging, and banding wintering canvasbacks","interactions":[],"lastModifiedDate":"2012-02-02T00:14:40","indexId":"5221784","displayToPublicDate":"2010-06-16T12:19:23","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2284,"text":"Journal of Field Ornithology","active":true,"publicationSubtype":{"id":10}},"title":"Techniques for trapping, aging, and banding wintering canvasbacks","docAbstract":"Techniques used to trap, band, and determine age of Canvasbacks during winter on Chesapeake Bay  are presented. Canvasbacks were captured with welded-wire traps baited with corn. Two trap designs were used and traps and trapping techniques are described. Ducks were dipnetted from traps and held in modified poultry crates that provided seclusion and ventilation and allowed birds to dry unsoiled. Carney's (1964) wing plumage methodology was found most  efficient in determining age of Canvasbacks during large-scale bandings.  This technique was rapid and was easily taught to inexperienced personnel. In contrast, the cloacal technique could be performed efficiently only by experienced and skillful banders. Band wear was observed to vary widely on individual birds and rounding of bands was  recognized as an important technique in extending band life. Bands were placed upside down on the tarsus so that wear along the upper edge would be less likely to destroy band numbers. In 5 winter seasons, over 17,000 Canvasbacks  were captured.  Mortality rate for the program was .3%.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Field Ornithology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Haramis, G., Derleth, E., and McAuley, D., 1982, Techniques for trapping, aging, and banding wintering canvasbacks: Journal of Field Ornithology, v. 53, no. 4, p. 342-351.","productDescription":"342-351","startPage":"342","endPage":"351","numberOfPages":"10","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18297,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://elibrary.unm.edu/sora/JFO/v053n04/p0342-p0351.pdf","linkFileType":{"id":1,"text":"pdf"}}],"volume":"53","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685a1f","contributors":{"authors":[{"text":"Haramis, G.M.","contributorId":101212,"corporation":false,"usgs":true,"family":"Haramis","given":"G.M.","email":"","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":334677,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Derleth, E.L.","contributorId":31483,"corporation":false,"usgs":true,"family":"Derleth","given":"E.L.","affiliations":[],"preferred":false,"id":334676,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McAuley, D.G. 0000-0003-3674-6392","orcid":"https://orcid.org/0000-0003-3674-6392","contributorId":15296,"corporation":false,"usgs":true,"family":"McAuley","given":"D.G.","affiliations":[],"preferred":false,"id":334675,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5221786,"text":"5221786 - 1982 - Care of nestlings by wild female starlings exposed to an organophosphate pesticide","interactions":[],"lastModifiedDate":"2024-03-01T17:10:53.806856","indexId":"5221786","displayToPublicDate":"2010-06-16T12:18:37","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2163,"text":"Journal of Applied Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Care of nestlings by wild female starlings exposed to an organophosphate pesticide","docAbstract":"<p>(1) Our objective was to determine the effect of exposure to an organophosphate pesticide (OP), dicrotophos (3-hydroxy-<i>N,N</i>-dimethyl-<i>cis</i>-scrotonamide dimethyl phosphate), on care of nestlings by wild female starlings (<i>Sturnus vulgaris</i>).</p><p>(2) We selected twelve pairs of active nests based on synchrony in the reproductive cycle. When nestlings were 10 days old (day 10), adult males were captured and killed and brood size was adjusted to four. The frequency and temporal distribution of sorties made by each pair of females to feed their young were recorded for 2 h at 18.00 hours on day 11 and 06.00 hours on day 12. One female from each pair was given a single oral dose of dicrotophos (2.5 mg/kg of body weight) dissolved in corn oil; the second female received an equivalent exposure of pure corn oil. Birds were released and their nestlings weighed. Parental care was again monitored between 18.00 and 20.00 hours on day 12 and 06.00 and 08.00 hours on day 13. Females were then captured and they with their young were weighed and killed. Changes in parental care in OP-dosed and control females were compared using paired t-tests.</p><p>(3) The OP-dosed females made significantly (<i>P</i> &lt; 0.5) fewer sorties to feed their young and remained away from their boxes for longer periods of time than controls. Nestlings of OP-treated females lost significantly more weight (<i><span>X̄</span></i> = 9.3%) than nestlings of controls (<i><span>X̄</span></i> = 3.2%). Brain ChE activity in OP-treated females was inhibited an average of 50.7% compared with controls. Weight changes in OP-dosed (<i><span>X̄</span></i> = -8.9%) and control females (<i><span>X̄</span></i> = -8.3%) were similar.</p><p>(4) Results indicate that parental care may be significantly reduced in songbirds receiving severe but sublethal exposure to organophosphate pesticides. The potential for a reduction or modification in parental care to alter reproductive success in passerines is discussed.</p><p>(5) Techniques utilized, or modifications thereof, may be useful in collecting the additional data needed to adequately assess the impact of OPs on songbird reproduction.</p>","language":"English","publisher":"British Ecological Society","doi":"10.2307/2403470","usgsCitation":"Grue, C., Powell, G., and McChesney, M., 1982, Care of nestlings by wild female starlings exposed to an organophosphate pesticide: Journal of Applied Ecology, v. 19, no. 2, p. 327-335, https://doi.org/10.2307/2403470.","productDescription":"9 p.","startPage":"327","endPage":"335","numberOfPages":"9","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193594,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5effa3","contributors":{"authors":[{"text":"Grue, C.E.","contributorId":86446,"corporation":false,"usgs":true,"family":"Grue","given":"C.E.","affiliations":[],"preferred":false,"id":334682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, G.V.N.","contributorId":23894,"corporation":false,"usgs":true,"family":"Powell","given":"G.V.N.","email":"","affiliations":[],"preferred":false,"id":334680,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McChesney, M.J.","contributorId":31484,"corporation":false,"usgs":true,"family":"McChesney","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":334681,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5210369,"text":"5210369 - 1982 - Regional population inferences for the American woodcock","interactions":[],"lastModifiedDate":"2012-02-02T00:15:16","indexId":"5210369","displayToPublicDate":"2009-06-09T09:23:17","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"14","title":"Regional population inferences for the American woodcock","docAbstract":"Woodcock (Philohela minor) bandings and recoveries from 1967 to 1977 were analyzed from two large banding reference areas corresponding to existing Eastern and Central harvest units.  We examined temporal, age-specific, sex-specific, and geographic variation in both survival and recovery rates, using recently developed stochastic models.  Survival rate estimates for females were higher than those for males, and higher for adults than for young.  There was no significant difference in recovery rates between young and adults.  Recovery rates of Eastern unit birds were higher, and overall survival rates were lower than those of Central unit birds.  Survival rate estimates were used with crude production rate estimates in a simple modeling effort, and resulting rates of population increase were 1.2 to 1.3 times higher in the Central reference area.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Woodcock Ecology and Management","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","usgsCitation":"Dwyer, T., and Nichols, J., 1982, Regional population inferences for the American woodcock, chap. <i>of</i> Woodcock Ecology and Management, p. 12-21.","productDescription":"v, 191","startPage":"12","endPage":"21","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c499","contributors":{"authors":[{"text":"Dwyer, T.J.","contributorId":56177,"corporation":false,"usgs":true,"family":"Dwyer","given":"T.J.","email":"","affiliations":[],"preferred":false,"id":328276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nichols, J.D. 0000-0002-7631-2890","orcid":"https://orcid.org/0000-0002-7631-2890","contributorId":14332,"corporation":false,"usgs":true,"family":"Nichols","given":"J.D.","affiliations":[],"preferred":false,"id":328275,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5210288,"text":"5210288 - 1982 - Modern pesticides and bobwhite populations","interactions":[],"lastModifiedDate":"2020-03-12T11:56:11","indexId":"5210288","displayToPublicDate":"2009-06-09T09:23:17","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Modern pesticides and bobwhite populations","docAbstract":"<p>Bobwhite (<i>Colinus virginianus</i>) are frequently used as test animals for wildlife tests of pesticides. The organophosphate and carbamate pesticides that have replaced the organochlorines have many desirable properties, but they span a wide range of acute toxicities and some of them affe,ct survival, reproduction, food consumption, behavior, and nervous system enzymes in laboratory tests. Applying these laboratory findings to the field requires assumptions about the severity of exposure in the field. Direct field measurements show that birds may be exposed to significant amounts of these pesticides or even more toxic degradation products under some conditions. Adverse population effects may also result from depression of insect populations during the seasons when bobwhites rely on insects for food.</p>","language":"English","publisher":"Oklahoma State University","publisherLocation":"Stillwater, Oklahoma","usgsCitation":"Stromborg, K., 1982, Modern pesticides and bobwhite populations, p. 69-73.","productDescription":"5 p.","startPage":"69","endPage":"73","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699518","contributors":{"editors":[{"text":"Schitoskey, Frank= Jr.","contributorId":111424,"corporation":false,"usgs":true,"family":"Schitoskey","given":"Frank=","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":506234,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Schitoskey, Elizabeth C.","contributorId":111471,"corporation":false,"usgs":true,"family":"Schitoskey","given":"Elizabeth","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":506235,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Talent, Larry G.","contributorId":112219,"corporation":false,"usgs":true,"family":"Talent","given":"Larry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":506236,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Stromborg, K. L.","contributorId":34466,"corporation":false,"usgs":true,"family":"Stromborg","given":"K. L.","affiliations":[],"preferred":false,"id":328140,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011845,"text":"70011845 - 1982 - Amino acid geochemistry of fossil bones from the Rancho La Brea asphalt deposit, California","interactions":[],"lastModifiedDate":"2025-07-10T15:42:57.8938","indexId":"70011845","displayToPublicDate":"2004-11-19T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Amino acid geochemistry of fossil bones from the Rancho La Brea asphalt deposit, California","docAbstract":"<p><span>Low aspartic acid&nbsp;</span><span class=\"small-caps\">d:l</span><span>&nbsp;ratios and modern collagenlike concentration values indicate that amino acids in bones from the Rancho La Brea asphalt deposit, Los Angeles, California are better preserved than amino acids in bones of equivalent age that have not been preserved in asphalt. Amino acids were recovered from 10 Rancho La Brea bone samples which range in age from less than 200 to greater than 36,000 yr. The calibrated rates of aspartic acid racemization range from 2.1 to 5.0 × 10</span><sup>−6</sup><span>yr</span><sup>−1</sup><span>. Although this wide range of rate constants decreases the level of confidence for age estimates, use of the larger rate constant of 5.0 × 10</span><sup>−6</sup><span>yr</span><sup>−1</sup><span>&nbsp;provides minimum age estimates which fit the known stratigraphic and chronologic records of the Rancho La Brea deposits.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0033-5894(82)90068-0","issn":"00335894","usgsCitation":"McMenamin, M., Blunt, D., Kvenvolden, K., Miller, S., Marcus, L., and Pardi, R., 1982, Amino acid geochemistry of fossil bones from the Rancho La Brea asphalt deposit, California: Quaternary Research, v. 18, no. 2, p. 174-183, https://doi.org/10.1016/0033-5894(82)90068-0.","productDescription":"10 p.","startPage":"174","endPage":"183","costCenters":[],"links":[{"id":221617,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Los Angeles","otherGeospatial":"Rancho La Brea","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.36504919269949,\n              34.084800941611704\n            ],\n            [\n              -118.36504919269949,\n              34.052190274637866\n            ],\n            [\n              -118.28768748317239,\n              34.052190274637866\n            ],\n            [\n              -118.28768748317239,\n              34.084800941611704\n            ],\n            [\n              -118.36504919269949,\n              34.084800941611704\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"18","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059e9b9e4b0c8380cd483f1","contributors":{"authors":[{"text":"McMenamin, M.A.S.","contributorId":92311,"corporation":false,"usgs":true,"family":"McMenamin","given":"M.A.S.","email":"","affiliations":[],"preferred":false,"id":362099,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blunt, D.J.","contributorId":93189,"corporation":false,"usgs":true,"family":"Blunt","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":362100,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kvenvolden, K.A.","contributorId":80674,"corporation":false,"usgs":true,"family":"Kvenvolden","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":362098,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, Scott","contributorId":58387,"corporation":false,"usgs":true,"family":"Miller","given":"Scott","affiliations":[],"preferred":false,"id":362095,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Marcus, L.F.","contributorId":71837,"corporation":false,"usgs":true,"family":"Marcus","given":"L.F.","email":"","affiliations":[],"preferred":false,"id":362097,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pardi, R.R.","contributorId":68602,"corporation":false,"usgs":true,"family":"Pardi","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":362096,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
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