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","language":"English","publisher":"American Fisheries Society","usgsCitation":"Nickum, J., Bart, H., Bowser, P., Greer, I., Hubbs, C., Jenkins, J.A., MacMillan, J., Rachlin, J., Rose, J.D., Sorenson, P.W., and Tomasso, J., 2004, Guidelines for the use of fishes in research, 53 p.","productDescription":"53 p.","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":370966,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Nickum, J.G.","contributorId":58227,"corporation":false,"usgs":true,"family":"Nickum","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":778809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bart, H.L. Jr.","contributorId":42679,"corporation":false,"usgs":true,"family":"Bart","given":"H.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":778976,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowser, P.R.","contributorId":17935,"corporation":false,"usgs":true,"family":"Bowser","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":778977,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Greer, I.E.","contributorId":70182,"corporation":false,"usgs":true,"family":"Greer","given":"I.E.","email":"","affiliations":[],"preferred":false,"id":778978,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hubbs, C.","contributorId":221598,"corporation":false,"usgs":false,"family":"Hubbs","given":"C.","email":"","affiliations":[],"preferred":false,"id":778979,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jenkins, Jill A. 0000-0002-5087-0894 jenkinsj@usgs.gov","orcid":"https://orcid.org/0000-0002-5087-0894","contributorId":2710,"corporation":false,"usgs":true,"family":"Jenkins","given":"Jill","email":"jenkinsj@usgs.gov","middleInitial":"A.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true},{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":778980,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"MacMillan, J.R.","contributorId":181511,"corporation":false,"usgs":false,"family":"MacMillan","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":778981,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Rachlin, J.W.","contributorId":86725,"corporation":false,"usgs":true,"family":"Rachlin","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":778982,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Rose, J. D.","contributorId":221596,"corporation":false,"usgs":false,"family":"Rose","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":778983,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sorenson, P. W.","contributorId":221595,"corporation":false,"usgs":false,"family":"Sorenson","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":778984,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Tomasso, J.R.","contributorId":49745,"corporation":false,"usgs":true,"family":"Tomasso","given":"J.R.","affiliations":[],"preferred":false,"id":778985,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}} ,{"id":70206345,"text":"70206345 - 2004 - Combined use of borehole geophysics and packers to site potable wells in a contaminated area in Montville, Connecticut","interactions":[],"lastModifiedDate":"2020-03-10T16:49:50","indexId":"70206345","displayToPublicDate":"2004-12-31T16:48:53","publicationYear":"2004","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Combined use of borehole geophysics and packers to site potable wells in a contaminated area in Montville, Connecticut","docAbstract":"A leaking underground gasoline tank contaminated a crystalline bedrock aquifer in Montville, Connecticut, USA with MTBE and benzene. At the original residential bedrock supply wells, the median MTBE concentration was 165 micrograms per liter (mg/L), and the median benzene concentration was 320 mg/L. The maximum concentrations of MTBE and benzene were 4,300 mg/l and 1,700 mg/L, respectively. Because of the unavailability of a public water supply and the long-term expense of point-of-use (on-site) treatment systems, the Connecticut Department of Environmental Protection Leaking Underground Storage Tank Program considered drilling replacement wells for water supply, if suitable drill sites could be located. Borehole geophysical methods were used as part of the investigation to find suitable drill sites. The U.S. Geological Survey performed borehole radar logging in three of the most contaminated wells. Other geophysical logs were run in two of the wells to enhance the hydrogeological characterizations. These data, combined with straddle-packer testing provided by a drilling contractor, formed the basis of a conceptual model used in the search for discrete fractures with better water quality than provided by an open-hole sample.
At Property A, a single transmissive fracture was identified at the bottom of the well. This well, although having historically lower gasoline concentrations than the other two wells, had persistent high iron bacteria fouling of the filtration system. By 2002, concentrations of MTBE and benzene had decreased to 59 and 3 mg/L, respectively, and the water was treatable except for the iron. Because no water-bearing fractures were encountered above the well bottom, an alternate well site was selected based on a set of vertical fractures observed in a nearby outcrop, rather than on the geophysical data. The new well, sited along the strike of these fractures, yielded 9 gallons per minute (gpm) but was found to be more contaminated than the original well. MTBE and benzene were detected at 224 and 7 mg/L, respectively. At Property B, the isolated fractures associated with four radar reflections contained MTBE in concentrations ranging from 460 to 680 mg/L, with concentration increasing with depth. A new well site was selected based upon topography and physical limitations of the property. A target drilling depth was selected to avoid encountering the most contaminated fracture, as projected from the radar data in the contaminated well. A new well, drilled to the target depth, yielded 2 gpm, which was sufficient for domestic supply. No contaminants were detected during 7 years of annual sampling. Over the next 2 years, MTBE was detected twice at 2 and 8 mg/L. At Property C, the isolated fractures associated with 12 radar reflections and acoustic televiewer images yielded MTBE concentrations ranging from 47 to 1,200 mg/L and benzene concentrations from 6 to 1,000 mg/L, with concentrations generally increasing with depth. A new well site was selected based upon physical limitations of the site. A target drilling depth was chosen to avoid encountering the most contaminated fractures, as projected from the radar data in the contaminated well. A new well, drilled to the target depth, yielded 6 gpm. MTBE was detected at concentrations ranging from trace levels to 12 mg/L for 6 years. Benzene was not detected.
These case histories suggest that the combined use of borehole geophysics and discrete-fracture sampling can, in some cases, be used to predict the locations of less contaminated or uncontaminated fractures, at distances of tens of feet from contaminated bedrock wells. This information may be used to improve the chances of successfully siting alternate potable water wells. Likewise, the same data and approach potentially could be used for targeting specific fractures for remediation.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings: 2004 U.S. EPA/NGWA Fractured Rock Conference","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"2004 U.S. EPA/NGWA Fractured Rock Conference","conferenceDate":"September 13-15, 2004","conferenceLocation":"Portland, ME","language":"English","publisher":"EPA/NGWA","usgsCitation":"Green, A., Lane, J., Johnson, C.D., Williams, J., Mondazzi, R.A., and Joesten, P.K., 2004, Combined use of borehole geophysics and packers to site potable wells in a contaminated area in Montville, Connecticut, in Proceedings: 2004 U.S. EPA/NGWA Fractured Rock Conference, Portland, ME, September 13-15, 2004, p. 295-307.","productDescription":"13 p.","startPage":"295","endPage":"307","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":368773,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":368772,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/ogw/bgas/publications/FracRock04_Green/"}],"country":"United States","state":"Connecticut","city":"Montville","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.22686767578125,\n 41.39689998354142\n ],\n [\n -72.0648193359375,\n 41.39689998354142\n ],\n [\n -72.0648193359375,\n 41.52785688696333\n ],\n [\n -72.22686767578125,\n 41.52785688696333\n ],\n [\n -72.22686767578125,\n 41.39689998354142\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Green, A.","contributorId":42333,"corporation":false,"usgs":true,"family":"Green","given":"A.","affiliations":[],"preferred":false,"id":774231,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lane, John W. Jr. 0000-0002-3558-243X","orcid":"https://orcid.org/0000-0002-3558-243X","contributorId":210076,"corporation":false,"usgs":true,"family":"Lane","given":"John W.","suffix":"Jr.","affiliations":[{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":true,"id":774232,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Carole D. 0000-0001-6941-1578 cjohnson@usgs.gov","orcid":"https://orcid.org/0000-0001-6941-1578","contributorId":1891,"corporation":false,"usgs":true,"family":"Johnson","given":"Carole","email":"cjohnson@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":774233,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, John 0000-0002-6054-6908 jhwillia@usgs.gov","orcid":"https://orcid.org/0000-0002-6054-6908","contributorId":1553,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"jhwillia@usgs.gov","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":774234,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mondazzi, Remo A.","contributorId":77898,"corporation":false,"usgs":true,"family":"Mondazzi","given":"Remo","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":774235,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Joesten, Peter K. pjoesten@usgs.gov","contributorId":1929,"corporation":false,"usgs":true,"family":"Joesten","given":"Peter","email":"pjoesten@usgs.gov","middleInitial":"K.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true},{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":true,"id":774236,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70206336,"text":"70206336 - 2004 - Time-series monitoring in fractured-rock aquifers","interactions":[],"lastModifiedDate":"2020-03-10T16:57:44","indexId":"70206336","displayToPublicDate":"2004-12-31T15:12:28","publicationYear":"2004","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Time-series monitoring in fractured-rock aquifers","docAbstract":"Time-lapse monitoring of subsurface processes is an emerging and promising area of hydrogeophysics. The combined use of non-invasive or minimally invasive geophysical methods with hydraulic and geochemical sampling is a cost-effective approach for aquifer characterization, long-term aquifer monitoring, and remediation monitoring. Time-lapse geophysical surveys can indirectly measure time-varying hydrologic parameters such as fluid saturation or solute concentration. Monitoring of time-varying hydrologic processes provides insight into aquifer properties and structure and aquifer responses to natural or induced stresses, such as seasonal fluctuations or fluid injection experiments for active remediation. The U.S. Geological Survey (USGS) Office of Ground Water, Branch of Geophysics, in cooperation with USGS Toxic Substances Hydrology Program, Environmental Protection Agency (USEPA), Department of Defense, the University of Connecticut, and Stanford University researchers, has applied time-lapse geophysics for site characterization and remediation monitoring in a number of studies. Recent and ongoing examples of time-lapse monitoring in fractured-rock aquifers include: 1) application of attenuation-difference, boreholeradar tomography used to monitor a series of sodium chloride tracer injection tests in fractured crystalline rock; 2) application of attenuation- and velocity-difference tomography and radar-reflection data to monitor steam injection in a fractured limestone aquifer; 3) design of an electrical resistivity tomography investigation to monitor the injection of resistive water into brackish water in a fractured limestone aquifer for aquifer storage and recovery (ASR); and 4) combined application of borehole-geophysical logging with long-term discreteinterval monitoring of hydraulic head and water-chemistry in a fractured crystalline-rock aquifer. These investigations demonstrate the application of geophysical methods to provide quantitative information about the subsurface critical for characterizing aquifer structure, flow dynamics, and hydraulic processes.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings: 2004 U.S. EPA/NGWA fractured rock conference: State of the science and measuring success in remediation","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"2004 U.S. EPA/NGWA Fractured Rock Conference: State of the Science and Measuring Success in Remediation","conferenceDate":"September 13-15, 2004","conferenceLocation":"Portland, ME","language":"English","publisher":"EPA/NGWA","usgsCitation":"Johnson, C.D., Lane, J., and Day-Lewis, F.D., 2004, Time-series monitoring in fractured-rock aquifers, in Proceedings: 2004 U.S. EPA/NGWA fractured rock conference: State of the science and measuring success in remediation, Portland, ME, September 13-15, 2004, p. 295-307.","productDescription":"13 p.","startPage":"295","endPage":"307","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":368756,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":368755,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/ogw/bgas/publications/FracRock04_Johnson-2/"}],"country":"United States","state":"New Hampshire","county":"Grafton County","otherGeospatial":"Mirror Lake, USGS Fractured-Rock Research site","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.70132637023926,\n 43.94231330042362\n ],\n [\n -71.69900894165039,\n 43.94231330042362\n ],\n [\n -71.69900894165039,\n 43.94351841607096\n ],\n [\n -71.70132637023926,\n 43.94351841607096\n ],\n [\n -71.70132637023926,\n 43.94231330042362\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Johnson, Carole D. 0000-0001-6941-1578 cjohnson@usgs.gov","orcid":"https://orcid.org/0000-0001-6941-1578","contributorId":1891,"corporation":false,"usgs":true,"family":"Johnson","given":"Carole","email":"cjohnson@usgs.gov","middleInitial":"D.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":774195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lane, John W. Jr. 0000-0002-3558-243X","orcid":"https://orcid.org/0000-0002-3558-243X","contributorId":210076,"corporation":false,"usgs":true,"family":"Lane","given":"John W.","suffix":"Jr.","affiliations":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":774196,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Day-Lewis, Frederick D. 0000-0003-3526-886X daylewis@usgs.gov","orcid":"https://orcid.org/0000-0003-3526-886X","contributorId":1672,"corporation":false,"usgs":true,"family":"Day-Lewis","given":"Frederick","email":"daylewis@usgs.gov","middleInitial":"D.","affiliations":[{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":774197,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70204066,"text":"70204066 - 2004 - Global climate change and wildlife in North America","interactions":[],"lastModifiedDate":"2019-07-01T15:13:44","indexId":"70204066","displayToPublicDate":"2004-12-31T14:49:50","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":223,"text":"Technical Review","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"04-2","title":"Global climate change and wildlife in North America","docAbstract":"It is widely accepted by the scientific community that the earth, which has always experienced climate variation, is now undergoing a period of rapid climate change that is enhanced by anthropogenic atmospheric carbon enrichment during the past 100 years. These climatic changes are accelerating and projections for the next 100 years indicate extensive warming in most (but not all) areas, changing patterns of precipitation, and a significant acceleration of sea level rise. Other likely components of ongoing climate change include changes in season lengths, decreasing range of nighttime versus daytime temperatures, declining snowpack, and increasing frequency and intensity of severe weather events. The many components of climate change, and especially the unprecedented rapid rate of change, are just as important as increasing temperatures. Wildlife species are closely adapted to their environments and readily respond to climate variation. However, as discussed in this technical review, the climate change now underway has extensive potential to affect wildlife throughout North America, either directly or indirectly through responses to changing habitat conditions. When
considered in combination with other factors (e.g., pollution, ozone depletion, urbanization, etc.), the potential effect is even greater. The effects of climate change on populations and range distributions of wildlife are expected to be species specific and highly variable, with some effects considered negative and others considered positive. In North America the ranges of habitats and wildlife are predicted to generally move northward as temperatures increase. Variations in this overall pattern will be dependent upon specific local conditions, changing precipitation patterns, and the response of different species to different components of climate change. It follows that the structure of plant–animal communities will also change. Ignoring climate change is likely to increasingly result in failure to reach wildlife management objectives. Wildlife managers need to become knowledgeable about climate change, ways to cope with it, and ways to take advantage of it. Management options currently available include protecting coastal wetlands to allow for sea level rise, reducing the risks to wildlife from potential catastrophic events, adjusting yield and harvest models, accounting for known climatic variations, and taking climate change into consideration when selecting the location and other characteristics of conservation areas. Wildlife managers also need to expect the unexpected and reduce nonclimate stressors on ecosystems. Overall, wildlife managers can minimize negative impacts to wildlife and take advantage of positive aspects by planning ahead and employing adaptive management.
To best respond to natural and human-induced stresses, resource managers and researchers require remote sensing techniques that can map the biophysical characteristics of natural resources on regional and local scales. The implementation of advanced measurement techniques would provide significant improvements in the quantity, quality, and timeliness of biophysical data useful in understanding the sensitivity of vegetation communities to external influences. In turn, this biophysical data would provide resource planners with a rational decision-making system for resource allocation and response action development planning.
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","language":"English","publisher":"Louisiana Ornithological Society","usgsCitation":"Michot, T., and Jeske, C.W., 2004, Gulf coast states wood stork tracking project: LOS news, p. 3-3.","productDescription":"1 p.","startPage":"3","endPage":"3","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":366407,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":366406,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://losbird.org/los_news.htm"}],"country":"United States","state":"Alabama, Florida, Georgia, Louisiana, Mississippi, South Carolina","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.5302734375,\n 33.8521697014074\n ],\n [\n -81.474609375,\n 35.137879119634185\n ],\n [\n -83.25439453125,\n 34.994003757575776\n ],\n [\n -87.890625,\n 35.0120020431607\n ],\n [\n -90.5712890625,\n 35.04798673426734\n ],\n [\n -91.20849609375,\n 33.100745405144245\n ],\n [\n -93.93310546875,\n 33.063924198120645\n ],\n [\n -93.779296875,\n 29.878755346037977\n ],\n [\n -90.439453125,\n 29.11377539511439\n ],\n [\n -88.0224609375,\n 29.36302703778376\n ],\n [\n -87.16552734375,\n 30.41078179084589\n ],\n [\n -86.06689453125,\n 30.278044377800153\n ],\n [\n -85.23193359375,\n 29.668962525992505\n ],\n [\n -84.24316406249999,\n 29.935895213372444\n ],\n [\n -82.77099609375,\n 28.9600886880068\n ],\n [\n -82.72705078125,\n 28.34306490482549\n ],\n [\n -82.85888671875,\n 27.839076094777816\n ],\n [\n -82.50732421875,\n 27.15692045688088\n ],\n [\n -81.80419921875,\n 26.15543796871355\n ],\n [\n -81.18896484375,\n 25.20494115356912\n ],\n [\n -80.31005859375,\n 25.085598897064752\n ],\n [\n -80.09033203125,\n 25.819671943904044\n ],\n [\n -80.13427734374999,\n 27.11781284232125\n ],\n [\n -80.48583984375,\n 28.401064827220896\n ],\n [\n -80.947265625,\n 29.248063243796576\n ],\n [\n -81.36474609375,\n 30.581179257386985\n ],\n [\n -80.96923828125,\n 31.952162238024975\n ],\n [\n -78.5302734375,\n 33.8521697014074\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Michot, Tommy 0000-0002-7044-987X","orcid":"https://orcid.org/0000-0002-7044-987X","contributorId":107585,"corporation":false,"usgs":true,"family":"Michot","given":"Tommy","affiliations":[],"preferred":false,"id":768062,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jeske, Clinton W. jeskec@usgs.gov","contributorId":2982,"corporation":false,"usgs":true,"family":"Jeske","given":"Clinton","email":"jeskec@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":768063,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70209815,"text":"70209815 - 2004 - U-Series isotopes as indicators of water/rock interaction in the unsaturated zone at Yucca Mountain, Nevada, USA","interactions":[],"lastModifiedDate":"2020-04-29T18:50:31.518541","indexId":"70209815","displayToPublicDate":"2004-12-31T13:46:39","publicationYear":"2004","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"U-Series isotopes as indicators of water/rock interaction in the unsaturated zone at Yucca Mountain, Nevada, USA","docAbstract":"No abstract available.
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","language":"English","publisher":"Slovenian Academy of Sciences and Arts","doi":"10.3986/ac.v33i2.300","usgsCitation":"Waery, D.J., Harrison, R., Jacobson, R.B., Javich, M.P., Mahan, S.A., and Wronkiewicz, D., 2004, Constraints on the geological history of the karst system in Southern Missouri, U.S.A. provided by radiogenic, cosmogenic and physical/chemical characteristics of doline fill: Acta Carsologica, v. 33, no. 2, p. 207-217, https://doi.org/10.3986/ac.v33i2.300.","productDescription":"11 p.","startPage":"207","endPage":"217","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":478003,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3986/ac.v33i2.300","text":"Publisher Index Page"},{"id":374235,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Missouri","otherGeospatial":"Ozark Plateau","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.59228515625,\n 36.04465753921525\n ],\n [\n -89.5166015625,\n 36.04465753921525\n ],\n [\n -89.5166015625,\n 38.57823196583313\n ],\n [\n -94.59228515625,\n 38.57823196583313\n ],\n [\n -94.59228515625,\n 36.04465753921525\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"33","issue":"2","noUsgsAuthors":false,"publicationDate":"2016-05-23","publicationStatus":"PW","contributors":{"authors":[{"text":"Waery, David J.","contributorId":224338,"corporation":false,"usgs":false,"family":"Waery","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":787826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrison, Richard W. rharriso@usgs.gov","contributorId":544,"corporation":false,"usgs":true,"family":"Harrison","given":"Richard W.","email":"rharriso@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":787827,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jacobson, Robert B. 0000-0002-8368-2064 rjacobson@usgs.gov","orcid":"https://orcid.org/0000-0002-8368-2064","contributorId":1289,"corporation":false,"usgs":true,"family":"Jacobson","given":"Robert","email":"rjacobson@usgs.gov","middleInitial":"B.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":787828,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Javich, Milan P.","contributorId":224339,"corporation":false,"usgs":false,"family":"Javich","given":"Milan","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":787829,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mahan, Shannon A. 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":147159,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","middleInitial":"A.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":787830,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wronkiewicz, David","contributorId":172154,"corporation":false,"usgs":false,"family":"Wronkiewicz","given":"David","email":"","affiliations":[{"id":26996,"text":"Missouri University of Science & Technology","active":true,"usgs":false}],"preferred":false,"id":787831,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70206231,"text":"70206231 - 2004 - Application of borehole radar for monitoring steam-enhanced remediation of a contaminated site in fractured limestone, Maine, USA","interactions":[],"lastModifiedDate":"2019-10-25T10:49:36","indexId":"70206231","displayToPublicDate":"2004-12-31T10:38:15","publicationYear":"2004","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Application of borehole radar for monitoring steam-enhanced remediation of a contaminated site in fractured limestone, Maine, USA","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Engineering geology for infrastructure planning in europe -- A European perspective","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","usgsCitation":"Gregoire, C., Lane, J., and Joesten, P.K., 2004, Application of borehole radar for monitoring steam-enhanced remediation of a contaminated site in fractured limestone, Maine, USA, chap. of Engineering geology for infrastructure planning in europe -- A European perspective, p. 385-392.","productDescription":"8 p.","startPage":"385","endPage":"392","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":368606,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":368605,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.springer.com/gp/book/9783540210757"}],"country":"United States","state":"Maine","otherGeospatial":"former Loring Air Force Base","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -67.93087005615234,\n 46.91486166357001\n ],\n [\n -67.85018920898438,\n 46.91486166357001\n ],\n [\n -67.85018920898438,\n 46.960573239955984\n ],\n [\n -67.93087005615234,\n 46.960573239955984\n ],\n [\n -67.93087005615234,\n 46.91486166357001\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gregoire, Colette","contributorId":24864,"corporation":false,"usgs":true,"family":"Gregoire","given":"Colette","email":"","affiliations":[],"preferred":false,"id":773887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lane, John W. Jr. 0000-0002-3558-243X","orcid":"https://orcid.org/0000-0002-3558-243X","contributorId":210076,"corporation":false,"usgs":true,"family":"Lane","given":"John W.","suffix":"Jr.","affiliations":[{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true},{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"preferred":true,"id":773888,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Joesten, Peter K. pjoesten@usgs.gov","contributorId":1929,"corporation":false,"usgs":true,"family":"Joesten","given":"Peter","email":"pjoesten@usgs.gov","middleInitial":"K.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true},{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":true,"id":773889,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70209311,"text":"70209311 - 2004 - Deciphering multiple Mesoproterozoic and Paleozoic events recorded in zircon and titanite from the Baltimore Gneiss, Maryland: SEM imaging, SHRIMP U-Pb geochronology, and EMP analysis","interactions":[],"lastModifiedDate":"2020-05-01T18:38:26.530197","indexId":"70209311","displayToPublicDate":"2004-12-31T10:18:15","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2711,"text":"Memoir of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"subseriesTitle":"","title":"Deciphering multiple Mesoproterozoic and Paleozoic events recorded in zircon and titanite from the Baltimore Gneiss, Maryland: SEM imaging, SHRIMP U-Pb geochronology, and EMP analysis","docAbstract":"The Baltimore Gneiss, exposed in antiforms in the eastern Maryland Piedmont, consists of a suite of felsic and mafic gneisses of Mesoproterozoic age. Zircons from the felsic gneisses are complexly zoned, as shown in cathodoluminescence imaging; most zircon grains have multiple overgrowth zones, some of which are adjacent and parallel to elongate cores. Sensitive high-resolution ion microprobe (SHRIMP) analyses of oscillatory-zoned cores indicate that the volcanic protoliths of the felsic gneisses crystallized at ca. 1.25 Ga. These rocks were subsequently affected by at least three Mesoproterozoic growth events, at ca. 1.22, 1.16, and 1.02 Ga. Foliated biotite granite intruded the Baltimore Gneiss metavolcanic sequence at ca. 1075 Ma. The Slaughterhouse Granite (renamed herein) also is Mesoproterozoic, but extremely discordant U-Pb data from high-U, metamict zircons preclude calculating a precise age. The 1.25 Ga rocks of the Baltimore Gneiss are coeval with rocks emplaced in the Grenville Province during the Elzevirian orogeny, and the 1.22 Ga zircon overgrowths are coincident with a later stage of this event. Younger zircon overgrowths formed during the Ottawan phase of the Grenville orogeny. Backscattered electron imaging of titanites from felsic gneisses and foliated biotite granite reveals that many of the grains contain cores, intermediate mantles, and rims. Electron microprobe traverses across zoned grains show regular variations in composition. SHRIMP ages for titanite from the foliated biotite granite are 374 ± 8, 336 ± 8, and 301 ± 12 Ma. The ca. 374 Ma age suggests growth of titanite during a thermal event following the Acadian orogeny, whereas the late Paleozoic titanite growth ages may be due to greenschist-facies replacement reactions associated with Alleghanian metamorphism and deformation.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-1197-5.411","issn":"","usgsCitation":"Aleinikoff, J.N., Horton,, J., Drake, A.A., Wintsch, R., Fanning, C., and Yi, K., 2004, Deciphering multiple Mesoproterozoic and Paleozoic events recorded in zircon and titanite from the Baltimore Gneiss, Maryland: SEM imaging, SHRIMP U-Pb geochronology, and EMP analysis: Memoir of the Geological Society of America, v. 197, p. 411-434, https://doi.org/10.1130/0-8137-1197-5.411.","productDescription":"24 p. 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Downward trends in sulfate concentrations likely are attributable to reductions in sulfur dioxide emissions mandated by the Clean Air Act of 1970 and amendments made in 1990. Upward trends in chloride concentrations illustrate some effects of increasing urbanization and nonpoint-source pollution. Current (2003) and future water quality challenges for the Connecticut River include reducing nitrogen loads from point and nonpoint sources, reducing bacteria and other contaminant concentrations in urban stormwater runoff, and separating stormwater and sanitary sewers at some locations to prevent combined-sewer overflows.
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This is important because expanding resource extraction in Alaska's Arctic regions may threaten the welfare of polar bears and their habitat. In recent years, exploration and development activities have expanded east and west of the original oil fields of Prudhoe Bay. Hydrocarbon extraction is now occurring or planned along much of the central Beaufort Sea coast. As development continues into the National Petroleum Reserve, the scope of expansion could include 213 of the northern coastal region of Alaska. Industrial activities are a potential threat to polar bears, especially as they might disturb bears in maternal dens (Lentfer and Hensel 1980, Stirling 1990, Stirling and Andriashek 1992, Amstrup 1993, Amstrup and Gardner 1994). As the number of humans and their activities have increased in recent years, there has been a concurrent increase in the number of female polar bears deming on land (Amstrup and Gardner 1994). Therefore, the probability of disrupting maternal deming can be expected to increase in the future. Using FLIR surveys to detect bears in dens could reduce or eliminate that probability. The purpose of this manual is to provide agency and private sector land managers with the information necessary to perform effective FLIR surveys to detect maternal dens. A list of personnel who can provide additional information is provided in Appendix 2.
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","language":"English","publisher":"Nevada Bureau of Mines and Geology","publisherLocation":"Reno, NV","usgsCitation":"House, K., Howard, K.A., Pearthree, P.A., and Bell, J.W., 2004, Preliminary geologic map of the Nevada and Arizona parts of the Mount Manchester quadrangle: Nevada Bureau Mines & Geology Report 2004-04, 26.5 x 25.5 inches.","productDescription":"26.5 x 25.5 inches","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355920,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":355919,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.nbmg.unr.edu/Geol-map-Mt-Manchester-quad-p/of2004-04.htm"}],"country":"United States","state":"Arizona, New Mexico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.22412109375,\n 37.142803443716836\n ],\n [\n -117.158203125,\n 37.142803443716836\n ],\n [\n -117.158203125,\n 37.16031654673677\n ],\n [\n -117.22412109375,\n 37.16031654673677\n ],\n [\n -117.22412109375,\n 37.142803443716836\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.3232421875,\n 34.361576287484176\n ],\n [\n -114.2138671875,\n 34.361576287484176\n ],\n [\n -114.2138671875,\n 36.24427318493909\n ],\n [\n -116.3232421875,\n 36.24427318493909\n ],\n [\n -116.3232421875,\n 34.361576287484176\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b98c9d3e4b0702d0e84672f","contributors":{"authors":[{"text":"House, Kyle 0000-0002-0019-8075 khouse@usgs.gov","orcid":"https://orcid.org/0000-0002-0019-8075","contributorId":2293,"corporation":false,"usgs":true,"family":"House","given":"Kyle","email":"khouse@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":740762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":740763,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pearthree, Philip A.","contributorId":17363,"corporation":false,"usgs":true,"family":"Pearthree","given":"Philip","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":740764,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bell, John W.","contributorId":61411,"corporation":false,"usgs":true,"family":"Bell","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":740765,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70188077,"text":"70188077 - 2004 - Testing archival tag technology in coho salmon","interactions":[],"lastModifiedDate":"2018-08-21T16:30:50","indexId":"70188077","displayToPublicDate":"2004-12-31T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Testing archival tag technology in coho salmon","docAbstract":"Archive tags with temperature and light-geolocation sensors will be monitored for post-smolt coho salmon in Cook Inlet. Light/location relationships specific to the Gulf of Alaska developed under Project 00478 will be applied in this study of movement and migration paths for coho salmon during maturation in ocean environments in Cook Inlet. Salmon for this study will be reared in captivity (at the Alaska Department of Fish and Game hatchery at Fort Richardson) to 1+ year of age (200-250mm) and released in Cook Inlet as part of the department's Ship Creek sport-fishing hatchery release. FY 01 includes pilot studies of tag retention, behavior, and growth for coho in captivity. Ship Creek coho will be tagged mid-May. A spring release experiment in the first year will be contingent on the successful implementation and retention of these tags. Surveys for early jack recoveries will be done at the Ship Creek weir and among sport fishers. Monitoring for adult tag recoveries will be done in the coho commercial fishery in Cook Inlet and the derby sport fishery on Ship Creek. Archive tagged fish will be used to document coho salmon use of marine habitats, migration routes, contribution to the sport fishery, and hatchery/wild interactions for salmon in Cook Inlet.
","language":"English","publisher":"Exxon Valdez Oil Spill Trustee Council","publisherLocation":"Anchorage, AK","usgsCitation":"Nielsen, J.L., Richards, P., Tingey, T., Wilson, D., and Zimmerman, C.E., 2004, Testing archival tag technology in coho salmon, 18 p.","productDescription":"18 p.","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":341893,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":342532,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.evostc.state.ak.us/index.cfm?FA=searchresults.projectInfo&Project_ID=344"}],"country":"United States","state":"Alaska","otherGeospatial":"Cook Inlet","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -149.150390625,\n 59.72594656451894\n ],\n [\n -146.7279052734375,\n 59.72594656451894\n ],\n [\n -146.7279052734375,\n 60.98376689595989\n ],\n [\n -149.150390625,\n 60.98376689595989\n ],\n [\n -149.150390625,\n 59.72594656451894\n ]\n ]\n ]\n }\n }\n ]\n}","publicComments":"Final Report: Exxon Valdez Oil Spill Restoration Project 02404","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"592e84cae4b092b266f10de8","contributors":{"authors":[{"text":"Nielsen, Jennifer L.","contributorId":43722,"corporation":false,"usgs":true,"family":"Nielsen","given":"Jennifer","email":"","middleInitial":"L.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":696575,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richards, Philip","contributorId":55090,"corporation":false,"usgs":false,"family":"Richards","given":"Philip","email":"","affiliations":[],"preferred":false,"id":698296,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tingey, Thor","contributorId":38654,"corporation":false,"usgs":false,"family":"Tingey","given":"Thor","email":"","affiliations":[],"preferred":false,"id":698297,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, Derek","contributorId":178950,"corporation":false,"usgs":true,"family":"Wilson","given":"Derek","email":"","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":false,"id":698298,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zimmerman, Christian E. 0000-0002-3646-0688 czimmerman@usgs.gov","orcid":"https://orcid.org/0000-0002-3646-0688","contributorId":410,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Christian","email":"czimmerman@usgs.gov","middleInitial":"E.","affiliations":[{"id":120,"text":"Alaska Science Center Water","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":698299,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70185123,"text":"70185123 - 2004 - The depositional history of three freshwater lakes in north central Florida: Brooklyn Lake, Levy's Prairie, and Cowpen Lake","interactions":[],"lastModifiedDate":"2023-03-14T13:16:45.969345","indexId":"70185123","displayToPublicDate":"2004-12-31T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":21,"text":"Thesis"},"publicationSubtype":{"id":28,"text":"Thesis"},"title":"The depositional history of three freshwater lakes in north central Florida: Brooklyn Lake, Levy's Prairie, and Cowpen Lake","docAbstract":"Florida has approximately 7800 lakes that are heavily concentrated in the north-central part of the state—a mantled karst terrain. Although much research has been conducted in Florida’s lakes, there is not much information on the sedimentary infill. The focus of this research is to define the sedimentary infill of three closely spaced lakes (Brooklyn Lake, Levys Prairie, and Cowpen Lake) in north-central Florida and determine the relative importance of the various
sedimentary inputs and their associated processes. Interlake lithostratigraphy comparison helped determine if they experienced a similar depositional infilling history or a unique one.
Twenty-three vibracores were taken (12 in Brooklyn Lake; 8 in Levys Prairie; 3 in Cowpen Lake) from which 331 sub-samples were analyzed for grain size, carbonate content, LOI index for total organic content, pollen content, mineralogy, and internal structures. Five sedimentary facies were defined in Brooklyn Lake, four in Levys Prairie, and three in Cowpen Lake. Using lithologic cross sections a depositional scenario was developed for each lake. Subaqueous and subaerial environments in conjunction with groundwater fluctuation and subsidence activity are key factors in lake development. The comparison of sediment infill of these three lakes reveals that Brooklyn Lake and Cowpen Lake are most similar in sediment facies content, basin morphology and the extent of subsidence depicted in the developmental scenarios, whereas, Levys Prairie is much different in sediment facies and basin morphology.
A doubling in pine pollen from Brooklyn Lake and Levys Prairie indicate a change from drier to a wetter environment. This change is present in Sheelar Lake and Mud Lake and carbon14 dated at 7200 yrs BP and 5070+/-150 yrs BP (Watts and Stuiver, 1980, Watts, 1969 respectively). This suggests that Brooklyn Lake and Levys Prairie are older than 7200 yrs BP.
Sediment infill from Brooklyn Lake, Levys Prairie and Cowpen Lake is conducive to understanding the depositional processes and environments that contributed to their development. Based on results and evidence presented in this study, it can be expected that lake development in a karst terrain will include subaqueous and subaerial intervals, and times of subsidence that can be recorded in the lake sediment.
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Paleolimnology","active":true,"publicationSubtype":{"id":10}},"title":"The history of recent limnological changes and human impact on Upper Klamath Lake, Oregon","docAbstract":"Hypereutrophic Upper Klamath Lake has been studied for almost 50 years to evaluate the nature, cause, and effects of its very productive waters. Mitigation of undesirable effects of massive cyanobacterial blooms requires understanding their modern causes as well as their history. Knowledge of the pre-settlement natural limnology of this system can provide guidelines for lake restoration and management of land and water use strategies to maximize the benefits of this aquatic resource. This investigation uses a paleolimnological approach to document the nature and chronology of limnological and biological changes in Upper Klamath Lake for the past 200 years, covering the time when the lake was first described until today. A 45-cm gravity core, dated by 210Pb and diatom correlations, was analyzed for diatoms, pollen, akinetes (resting spores) of the cyanobacterium Aphanizomenon flos-aquae, reworked tephra shards, and sediment magnetic characteristics. Pollen profiles show little vegetation change during this time. In contrast, diatoms indicative of increased nutrient fluxes (P and Si) increase moderately, coinciding with the settlement of the region by Euro-Americans. Numerous settlement activities, including draining of lake-margin marshes, upstream agriculture and timber harvest, road construction, and boat traffic, may have affected the lake. Magnetic properties and reworked tephra suggest riparian changes throughout the basin and increased lithogenic sediment delivery to the lake, especially after 1920 when the marshes near the mouth of the Williamson River were drained and converted to agricultural and pasture land. Drainage and channelization also decreased the ability of the marshes to function as traps and filters for upstream water and sediments. Akinetes of Aphanizomenon flos-aquae record progressive eutrophication of Upper Klamath Lake beginning in the 20th century and particularly after 1920 when lake-margin marsh reclamation more than doubled. The coincidence of limnological changes and human activities following European settlement suggests a major impact on the Upper Klamath Lake ecosystem, although ascribing specific limnological changes to specific human activities is difficult.
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Platt","contributorId":91106,"corporation":false,"usgs":true,"family":"Bradbury","given":"J.","email":"","middleInitial":"Platt","affiliations":[],"preferred":false,"id":725704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colman, Steve M.","contributorId":49807,"corporation":false,"usgs":true,"family":"Colman","given":"Steve","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":725705,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":147880,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":271,"text":"Federal Center","active":false,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":725706,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70189375,"text":"70189375 - 2004 - Acidity and alkalinity in mine drainage: Theoretical considerations","interactions":[],"lastModifiedDate":"2017-07-11T18:19:43","indexId":"70189375","displayToPublicDate":"2004-12-31T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Acidity and alkalinity in mine drainage: Theoretical considerations","docAbstract":"Acidity, net acidity, and net alkalinity are widely used parameters for the characterization of mine drainage, but these terms are not well defined and are often misunderstood. Incorrect interpretation of acidity, alkalinity, and derivative terms can lead to inadequate treatment design or poor regulatory decisions. We briefly explain derivations of theoretical expressions of three types of alkalinities (caustic, phenolphthalein, and total) and acidities (mineral, CO2, and total). Theoretically defined total alkalinity is closely analogous to measured alkalinity and presents few practical interpretation problems. Theoretically defined “CO2- acidity” is closely related to most standard titration methods used for mine drainage with an endpoint pH of 8.3, but it presents numerous interpretation problems, and it is unfortunately named because CO2 is intentionally driven off during titration of mine-drainage samples. Using the proton condition/massaction approach and employing graphs for visualization, we explore the concept of principal components and how to assign acidity contributions to solution species, including aqueous complexes, commonly found in mine drainage. We define a comprehensive theoretical definition of acidity in mine drainage on the basis of aqueous speciation at the sample pH and the capacity of these species to undergo hydrolysis to pH 8.3. This definition indicates the computed acidity in milligrams per liter (mg L-1 ) as CaCO3 (based on pH and analytical concentrations of dissolved FeIII , FeII , Mn, and Al in mg L-1 ): Aciditycomputed = 50. (10(3-pH) + 3.CFeIII/55.8 + 2.CFeII/55.8 + 2.CMn/54.9 + 3.CAl/27.0) underestimates contributions from HSO4 - and H+ , but overestimates the acidity due to Fe3+. These errors tend to approximately cancel each other.
We demonstrate that “net alkalinity” is a valid mathematical construction based on theoretical definitions of alkalinity and acidity. We demonstrate that, for most mine-drainage solutions, a useful net alkalinity value can be derived from: 1) alkalinity and acidity values based on aqueous speciation, 2) measured alkalinity - computed acidity, or 3) taking the negative of the value obtained in a standard method “hot peroxide” acidity titration, provided that labs report negative values. We recommend the third approach; i.e., Net alkalinity = - Hot Acidity.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings America Society of Mining and Reclamation, 2004","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"2004 National Meeting of the American Society of Mining and Reclamation and the 25th West Virginia Surface Mine Drainage Task Force","conferenceDate":" April 18 – 24, 2004","conferenceLocation":"Morgantown, WV","publisher":"America Society of Mining and Reclamation","doi":"10.21000/JASMR04011076","usgsCitation":"Kirby, C.S., and Cravotta, C.A., 2004, Acidity and alkalinity in mine drainage: Theoretical considerations, in Proceedings America Society of Mining and Reclamation, 2004, Morgantown, WV, April 18 – 24, 2004, p. 1076-1093, https://doi.org/10.21000/JASMR04011076.","productDescription":"18 p.","startPage":"1076","endPage":"1093","costCenters":[],"links":[{"id":343631,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2004-06-30","publicationStatus":"PW","scienceBaseUri":"5965cf4ce4b0d1f9f05b5e97","contributors":{"authors":[{"text":"Kirby, Carl S.","contributorId":23618,"corporation":false,"usgs":true,"family":"Kirby","given":"Carl","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":704419,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cravotta, Charles A. III, 0000-0003-3116-4684 cravotta@usgs.gov","orcid":"https://orcid.org/0000-0003-3116-4684","contributorId":2193,"corporation":false,"usgs":true,"family":"Cravotta","given":"Charles","suffix":"III,","email":"cravotta@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":704420,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70197332,"text":"70197332 - 2004 - Origin of the Bering Sea salient","interactions":[],"lastModifiedDate":"2018-05-29T16:14:49","indexId":"70197332","displayToPublicDate":"2004-12-31T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1727,"text":"GSA Special Papers","active":true,"publicationSubtype":{"id":10}},"title":"Origin of the Bering Sea salient","docAbstract":"Our investigations in Alaska and Russia show that the curved orogen of the Bering Strait region is a composite feature that formed as a result of multiple superimposed events and cannot be related to latest Cretaceous–early Tertiary east-west shortening. Relations interpreted to record east-west shortening include the Chukchi syntaxis, deformation on Seward and Chukotka Peninsulas, the map pattern of Triassic-Jurassic mafic rocks, and plate reconstructions. These relations are reviewed in light of new data and show that the curved orogen cannot have been formed by east-west shortening. For example, the Chukchi syntaxis, the northeastern limb of the orogen, is a primary structural loop that originated during the Brookian orogeny in the Early Cretaceous and therefore predates postulated oroclinal bending. East-west shortening on Seward Peninsula and Chukotka is manifest by low-amplitude, long-wavelength folds that require only small strains. The Seward Peninsula/Yukon-Koyukuk province boundary was previously interpreted as a thrust fault, but it instead may be a left-lateral strike-slip fault. Triassic-Jurassic mafic rocks similar to the Angayucham terrane are found on the northern Chukotka Peninsula, but a better correlation is with rocks farther south in the South Anyui suture zone, resulting in a less-arcuate pattern. Mid-Cretaceous north-south extension in the Bering Strait region has enhanced the curvature of the margin. Recent plate reconstructions indicate that shortening between Eurasia and North America was previously overestimated and that significant east-west convergence probably did not occur in the region during the Tertiary. We conclude that the curved orogen in the Bering Strait region is not a true orocline and instead is a composite structural feature that is best described as a salient.
","largerWorkTitle":"Orogenic curvature: Integrating paleomagnetic and structural analyses","language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-2383-3(2004)383[131:OOTBSS]2.0.CO;2","usgsCitation":"Amato, J., Toro, J., and Moore, T.E., 2004, Origin of the Bering Sea salient: GSA Special Papers, v. 383, p. 131-144, https://doi.org/10.1130/0-8137-2383-3(2004)383[131:OOTBSS]2.0.CO;2.","productDescription":"14 p.","startPage":"131","endPage":"144","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":354554,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"383","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b1580e3e4b092d9651e2083","contributors":{"authors":[{"text":"Amato, J.M.","contributorId":63214,"corporation":false,"usgs":true,"family":"Amato","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":736710,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Toro, J.","contributorId":88502,"corporation":false,"usgs":true,"family":"Toro","given":"J.","email":"","affiliations":[],"preferred":false,"id":736711,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, Thomas E. 0000-0002-0878-0457 tmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-0878-0457","contributorId":1033,"corporation":false,"usgs":true,"family":"Moore","given":"Thomas","email":"tmoore@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":736712,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70198255,"text":"70198255 - 2004 - Geologic map of the Verdi Peak Quadrangle, Elko County, Nevada","interactions":[],"lastModifiedDate":"2018-07-24T10:05:18","indexId":"70198255","displayToPublicDate":"2004-12-31T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5655,"text":"Nevada Bureau of Mines and Geology Map","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"147","title":"Geologic map of the Verdi Peak Quadrangle, Elko County, Nevada","docAbstract":"A 1:24,000-scale, full-color geologic map of the Verdi Peak 7.5-minute quadrangle in Elko County, Nevada, with one cross section and descriptions of 19 rock units. Accompanying text describes the geology of the quadrangle.
","language":"English","publisher":"Nevada Bureau of Mines and Geology","publisherLocation":"Reno, NV","usgsCitation":"Howard, K.A., and MacCready, T., 2004, Geologic map of the Verdi Peak Quadrangle, Elko County, Nevada: Nevada Bureau of Mines and Geology Map 147, Map: 27 x 29.5 inches; Report: 4 p.","productDescription":"Map: 27 x 29.5 inches; Report: 4 p.","costCenters":[],"links":[{"id":355916,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.nbmg.unr.edu/Geologic-Verdi-Peak-quad-p/m147.htm"},{"id":355917,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Elko County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5b98c9d3e4b0702d0e846731","contributors":{"authors":[{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":740760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacCready, T.","contributorId":69418,"corporation":false,"usgs":true,"family":"MacCready","given":"T.","email":"","affiliations":[],"preferred":false,"id":740761,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}