In order to investigate the effects of nearshore discharges of water quality degrading substances and bacteria in coastal environments, models capable of predicting nearshore circulation due to local wave and tide conditions are required. One of the larger challenges to nearshore coastal modeling is accurately reproducing nearshore circulation due to wave action. Local wave action not only drives circulation through processes such as longshore transport and rip currents, but also contributes significantly to the mixing of water quality constituents. In the present work, a wave model was used to calculate radiation shear stresses and dissipation due to wave action. The shear stresses and dissipation were incorporated into a hydrodynamic model to force circulation in the nearshore environment. The model was applied to a site in Santa Cruz, CA where site specific current data was available. The model reproduces the nearshore current structure observed in the region and was used to study the transport of dredge disposal plumes in the region which could have deleterious effects on local beaches. This presentation will outline the nearshore circulation model development and application.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 2008 world environmental and water resources congress","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"World Environmental and Water Resources Congress 2008","conferenceDate":"May 12-16, 2008","conferenceLocation":"Honolulu, HI","language":"English","publisher":"ASCE","doi":"10.1061/9780784409763","usgsCitation":"Jones, C., and Angster, S.J., Modeling of wave driven circulation and water quality in nearshore environments, in Proceedings of the 2008 world environmental and water resources congress, Honolulu, HI, May 12-16, 2008, 10 p., https://doi.org/10.1061/9780784409763.","productDescription":"10 p.","costCenters":[],"links":[{"id":406231,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2012-04-26","publicationStatus":"PW","contributors":{"authors":[{"text":"Jones, Craig","contributorId":208632,"corporation":false,"usgs":false,"family":"Jones","given":"Craig","affiliations":[{"id":37853,"text":"Integral Constulting Inc., Santa Cruz, California, UNITED STATES","active":true,"usgs":false}],"preferred":false,"id":850908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Angster, Stephen J. 0000-0001-9250-8415 sangster@usgs.gov","orcid":"https://orcid.org/0000-0001-9250-8415","contributorId":3885,"corporation":false,"usgs":true,"family":"Angster","given":"Stephen","email":"sangster@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":850909,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70206320,"text":"70206320 - null - Mantle xenocrysts from the Masontown, Pennsylvania (USA) kimberlite: An ordinary mantle with Si-enriched spinels ","interactions":[],"lastModifiedDate":"2019-10-31T07:44:45","indexId":"70206320","displayToPublicDate":"2008-10-30T11:19:45","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":18,"text":"Abstract or summary"},"title":"Mantle xenocrysts from the Masontown, Pennsylvania (USA) kimberlite: An ordinary mantle with Si-enriched spinels ","docAbstract":"No abstract available.
","conferenceTitle":"9th international kimberlite conference (9IKC)","conferenceDate":"August 10-15, 2008","conferenceLocation":"Frankfurt, Germany","language":"English","usgsCitation":"Schulze, D., and Hearn, B.C., Mantle xenocrysts from the Masontown, Pennsylvania (USA) kimberlite: An ordinary mantle with Si-enriched spinels , 9th international kimberlite conference (9IKC), v. 9, Frankfurt, Germany, August 10-15, 2008.","productDescription":"A-00312, 1 p.","startPage":"1","costCenters":[],"links":[{"id":368737,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schulze, D.J.","contributorId":18549,"corporation":false,"usgs":true,"family":"Schulze","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":774140,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hearn, B. Carter chearn@usgs.gov","contributorId":189844,"corporation":false,"usgs":true,"family":"Hearn","given":"B.","email":"chearn@usgs.gov","middleInitial":"Carter","affiliations":[],"preferred":true,"id":774141,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70273251,"text":"70273251 - null - Relationship between remotely-sensed vegetation indices, canopy attributes and plant physiological processes: What vegetation indices can and cannot tell us about the landscape","interactions":[],"lastModifiedDate":"2025-12-23T15:33:23.073849","indexId":"70273251","displayToPublicDate":"2008-03-28T09:13:57","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3380,"text":"Sensors","active":true,"publicationSubtype":{"id":10}},"title":"Relationship between remotely-sensed vegetation indices, canopy attributes and plant physiological processes: What vegetation indices can and cannot tell us about the landscape","docAbstract":"Vegetation indices (VIs) are among the oldest tools in remote sensing studies. Although many variations exist, most of them ratio the reflection of light in the red and NIR sections of the spectrum to separate the landscape into water, soil, and vegetation. Theoretical analyses and field studies have shown that VIs are near-linearly related to photosynthetically active radiation absorbed by a plant canopy, and therefore to light-dependent physiological processes, such as photosynthesis, occurring in the upper canopy. Practical studies have used time-series VIs to measure primary production and evapotranspiration, but these are limited in accuracy to that of the data used in ground truthing or calibrating the models used. VIs are also used to estimate a wide variety of other canopy attributes that are used in Soil-Vegetation-Atmosphere Transfer (SVAT), Surface Energy Balance (SEB), and Global Climate Models (GCM). These attributes include fractional vegetation cover, leaf area index, roughness lengths for turbulent transfer, emissivity and albedo. However, VIs often exhibit only moderate, non-linear relationships to these canopy attributes, compromising the accuracy of the models. We use case studies to illustrate the use and misuse of VIs, and argue for using VIs most simply as a measurement of canopy light absorption rather than as a surrogate for detailed features of canopy architecture. Used this way, VIs are compatible with “Big Leaf” SVAT and GCMs that assume that canopy carbon and moisture fluxes have the same relative response to the environment as any single leaf, simplifying the task of modeling complex landscapes.
","language":"English","publisher":"MDPI","doi":"10.3390/s8042136","usgsCitation":"Glenn, E.P., Huete, A.R., Nagler, P.L., and Nelson, S.G., Relationship between remotely-sensed vegetation indices, canopy attributes and plant physiological processes: What vegetation indices can and cannot tell us about the landscape: Sensors, v. 8, no. 4, p. 2136-2160, https://doi.org/10.3390/s8042136.","productDescription":"25 p.","startPage":"2136","endPage":"2160","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":498055,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3390/s8042136","text":"Publisher Index Page"},{"id":497937,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Colorado River, Havasu National Wildlife Refuge","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -114.46320466185165,\n 34.705992498069406\n ],\n [\n -114.398916590966,\n 34.73603912838132\n ],\n [\n -114.53190465917093,\n 34.97188700395952\n ],\n [\n -114.64409364561838,\n 34.905752361774034\n ],\n [\n -114.54892208969932,\n 34.76089704626571\n ],\n [\n -114.46320466185165,\n 34.705992498069406\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"8","issue":"4","noUsgsAuthors":false,"publicationDate":"2008-03-28","publicationStatus":"PW","contributors":{"authors":[{"text":"Glenn, Edward P.","contributorId":19289,"corporation":false,"usgs":true,"family":"Glenn","given":"Edward","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":952873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huete, Alfredo R","contributorId":243589,"corporation":false,"usgs":false,"family":"Huete","given":"Alfredo","email":"","middleInitial":"R","affiliations":[{"id":48742,"text":"School of Life Sciences, Faculty of Science, University of Technology Sydney, Sydney, NSW 2007, Australia","active":true,"usgs":false}],"preferred":false,"id":952874,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nagler, Pamela L. 0000-0003-0674-103X pnagler@usgs.gov","orcid":"https://orcid.org/0000-0003-0674-103X","contributorId":1398,"corporation":false,"usgs":true,"family":"Nagler","given":"Pamela","email":"pnagler@usgs.gov","middleInitial":"L.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":952875,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, Stephen G.","contributorId":174719,"corporation":false,"usgs":false,"family":"Nelson","given":"Stephen","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":952876,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70273252,"text":"70273252 - null - Reconciling environmental and flood control goals on an arid-zone river: Case study of the Limitrophe Region of the lower Colorado River in the United States and Mexico","interactions":[],"lastModifiedDate":"2025-12-23T15:47:30.467798","indexId":"70273252","displayToPublicDate":"2008-03-01T09:39:49","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1547,"text":"Environmental Management","active":true,"publicationSubtype":{"id":10}},"title":"Reconciling environmental and flood control goals on an arid-zone river: Case study of the Limitrophe Region of the lower Colorado River in the United States and Mexico","docAbstract":"Arid zone rivers have highly variable flow rates, and flood control projects are needed to protect adjacent property from flood damage. On the other hand, riparian corridors provide important wildlife habitat, especially for birds, and riparian vegetation is adapted to the natural variability in flows on these rivers. While environmental and flood control goals might appear to be at odds, we show that both goals can be accommodated in the Limitrophe Region (the shared border between the United States and Mexico) on the Lower Colorado River. In 1999, the International Boundary and Water Commission proposed a routine maintenance project to clear vegetation and create a pilot channel within the Limitrophe Region to improve flow capacity and delineate the border. In 2000, however, Minute 306 to the international water treaty was adopted, which calls for consideration of environmental effects of IBWC actions. We conducted vegetation and bird surveys within the Limitrophe and found that this river segment is unusually rich in native cottonwood and willow trees, marsh habitat, and resident and migratory birds compared to flow-regulated segments of river. A flood-frequency analysis showed that the existing levee system can easily contain a 100 year flood even if vegetation is not removed, and the existing braided channel system has greater carrying capacity than the proposed pilot channel.
","language":"English","publisher":"Springer","doi":"10.1007/s00267-007-9056-4","usgsCitation":"Glenn, E.P., Hucklebridge, K., Hinojosa-Huerta, O., Nagler, P.L., and Pitt, J., Reconciling environmental and flood control goals on an arid-zone river: Case study of the Limitrophe Region of the lower Colorado River in the United States and Mexico: Environmental Management, v. 41, p. 322-335, https://doi.org/10.1007/s00267-007-9056-4.","productDescription":"14 p.","startPage":"322","endPage":"335","costCenters":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"links":[{"id":497938,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico, United States","otherGeospatial":"lower Colorado River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -113.84952634861096,\n 34.55176370207661\n ],\n [\n -115.2034771735304,\n 34.55176370207661\n ],\n [\n -115.2034771735304,\n 31.579861300988156\n ],\n [\n -113.84952634861096,\n 31.579861300988156\n ],\n [\n -113.84952634861096,\n 34.55176370207661\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"41","noUsgsAuthors":false,"publicationDate":"2008-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Glenn, Edward P.","contributorId":19289,"corporation":false,"usgs":true,"family":"Glenn","given":"Edward","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":952877,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hucklebridge, Kate","contributorId":364563,"corporation":false,"usgs":false,"family":"Hucklebridge","given":"Kate","affiliations":[],"preferred":false,"id":952878,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hinojosa-Huerta, Osvel","contributorId":195177,"corporation":false,"usgs":false,"family":"Hinojosa-Huerta","given":"Osvel","email":"","affiliations":[],"preferred":false,"id":952879,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nagler, Pamela L. 0000-0003-0674-103X pnagler@usgs.gov","orcid":"https://orcid.org/0000-0003-0674-103X","contributorId":1398,"corporation":false,"usgs":true,"family":"Nagler","given":"Pamela","email":"pnagler@usgs.gov","middleInitial":"L.","affiliations":[{"id":568,"text":"Southwest Biological Science Center","active":true,"usgs":true}],"preferred":true,"id":952880,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Pitt, Jennifer","contributorId":255277,"corporation":false,"usgs":false,"family":"Pitt","given":"Jennifer","affiliations":[{"id":51507,"text":"Audubon","active":true,"usgs":false}],"preferred":false,"id":952881,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70206199,"text":"70206199 - null - Cross-borehole flow tests and insights into hydraulic connections in fractured mudstone and sandstone","interactions":[],"lastModifiedDate":"2020-03-10T14:58:10","indexId":"70206199","displayToPublicDate":"2007-12-31T15:11:34","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Cross-borehole flow tests and insights into hydraulic connections in fractured mudstone and sandstone","docAbstract":"Cross-borehole flow tests provided insights into hydraulic connections in fractured and dipping mudstone and sandstone that were consistent with the lithostratigraphic and structural framework of a VOCcontaminated bedrock research site in west-central New Jersey. Two cross-borehole flow tests were completed. Each test involved measurement and analysis of transient flow in a newly installed deep corehole with a long open interval during short-term pumping and recovery in an adjacent shallow well with a short open interval. The cross-borehole flow test in the mudstone identified a hydraulic connection through a dipping fractured bed between the pumped interval in the well and a flow zone at an intermediate depth in the corehole. The presence of a hydraulic connection between the pumped well and the corehole was not obvious because the water-level response in the corehole was dominated by a shallow zone of high transmissivity, which was hydraulically isolated from the pumped interval. In the sandstone, the cross-borehole flow test identified a hydraulic connection along dipping fractured beds as well as a connection to a deep high-angle fracture that cuts across bedding. These results suggest that application of cross-borehole flow tests at other contaminated fractured-bedrock sites could provide insights into hydraulic connections useful the design and implementation of monitoring and remediation programs.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Symposium on the Application of Geophysics to Engineering and Environmental Problems","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Symposium on the Application of Geophysics to Engineering and Environmental Problems","conferenceDate":"April 1-5, 2007","conferenceLocation":"Denver, CO","language":"English","usgsCitation":"Williams, J., Lacombe, P., Johnson, C.D., and Paillet, F.L., Cross-borehole flow tests and insights into hydraulic connections in fractured mudstone and sandstone, in Symposium on the Application of Geophysics to Engineering and Environmental Problems, Denver, CO, April 1-5, 2007, p. 1140-1152.","productDescription":"12 p.","startPage":"1140","endPage":"1152","costCenters":[{"id":470,"text":"New Jersey Water Science Center","active":true,"usgs":true},{"id":474,"text":"New York Water Science Center","active":true,"usgs":true},{"id":493,"text":"Office of Ground 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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":773831,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Paillet, Frederick L.","contributorId":63820,"corporation":false,"usgs":true,"family":"Paillet","given":"Frederick","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":773832,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70259123,"text":"70259123 - null - Comparative analysis of GPP products estimated from an empirical model and MODIS","interactions":[],"lastModifiedDate":"2024-09-27T15:19:00.857652","indexId":"70259123","displayToPublicDate":"2006-12-01T10:12:44","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Comparative analysis of GPP products estimated from an empirical model and MODIS","docAbstract":"Carbon-cycle models have uncertainties associated with data inputs, parameters, and model algorithms. The prerequisite for an applicable model is that it should perform at an acceptable level of accuracy and uncertainties should be documented. In this study, we validated the gross primary productivity (GPP) data from a piecewise regression (PWR) model and the MODIS GPP model at five grassland flux towers in the Northern Great Plains. The results showed a good agreement of GPP values (agreement coefficient d = 0.88–0.98) among PWR, MODIS, and tower measurements at Fort Peck, Mandan, and Cheyenne sites; but MODIS GPP did not agree well (d = 0.62–0.79) with tower measurements at Miles City and Lethbridge sites. Additionally, we compared PWR GPP and MODIS GPP for grasslands in the entire study area. We found that the PWR GPP was lower than or similar to the MODIS GPP in the east and higher in the west and south. We explored possible factors that may cause the GPP difference in spatial distribution between the two models.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Global priorities in land remote sensing","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"William T. Pecora Memorial Symposium on Remote Sensing, 16th","conferenceDate":"October 23-27, 2005","conferenceLocation":"Sioux Falls, SD","language":"English","publisher":"ASPRS","usgsCitation":"Zhang, L., Wylie, B.K., Loveland, T., and Ji, L., Comparative analysis of GPP products estimated from an empirical model and MODIS, in Global priorities in land remote sensing, Sioux Falls, SD, October 23-27, 2005, 12 p.","productDescription":"12 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":462337,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.asprs.org/Conference-Proceedings.html","linkFileType":{"id":5,"text":"html"}},{"id":462338,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Zhang, Li","contributorId":222540,"corporation":false,"usgs":false,"family":"Zhang","given":"Li","email":"","affiliations":[],"preferred":false,"id":914249,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wylie, Bruce K. 0000-0002-7374-1083 wylie@usgs.gov","orcid":"https://orcid.org/0000-0002-7374-1083","contributorId":750,"corporation":false,"usgs":true,"family":"Wylie","given":"Bruce","email":"wylie@usgs.gov","middleInitial":"K.","affiliations":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":914250,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Loveland, Thomas 0000-0003-3114-6646 loveland@usgs.gov","orcid":"https://orcid.org/0000-0003-3114-6646","contributorId":140611,"corporation":false,"usgs":true,"family":"Loveland","given":"Thomas","email":"loveland@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":914251,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ji, Lei 0000-0002-6133-1036 lji@usgs.gov","orcid":"https://orcid.org/0000-0002-6133-1036","contributorId":139587,"corporation":false,"usgs":true,"family":"Ji","given":"Lei","email":"lji@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true},{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"preferred":true,"id":914252,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70205983,"text":"70205983 - null - Characterizing the two-dimensional thermal conductivity distribution in a sand and gravel aquifer","interactions":[],"lastModifiedDate":"2019-10-14T14:38:34","indexId":"70205983","displayToPublicDate":"2006-10-14T14:38:13","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3420,"text":"Soil Science Society of America Journal","active":true,"publicationSubtype":{"id":10}},"title":"Characterizing the two-dimensional thermal conductivity distribution in a sand and gravel aquifer","docAbstract":"Both hydrologic and thermal transport properties play a significant role in the movement of heat through permeable sedimentary material; however, the thermal conductivity is rarely characterized in detailed spatial resolution. As part of a study of the movement of thermal plumes through a sand and gravel aquifer, we have constructed a two-dimensional profile of thermal conductivity. This work consisted of: (i) measuring the thermal conductivity of the soil solids, λs, for the main stratigraphic units using the steady-state divided-bar apparatus and estimating conductivity from mineral composition; (ii) measuring the volumetric water content and porosity using crosshole ground-penetrating radar; (iii) evaluating four models used to predict the apparent thermal conductivity, λ, of variably saturated soils and selecting the best model using the information-theoretic approach, (iv) calculating the λ field on a 0.25-m square cell grid using measured data and the selected model, and (v) simulating thermal transport within the two-dimensional domain using a finite element numerical model. The apparent thermal conductivity in the saturated aquifer ranges from 2.14 to 2.69 W m−1 K−1 with a mean of 2.42 W m−1 K−1 Numerical simulations show that the heterogeneous thermal conductivity field results in increased thermal dispersion that is most pronounced at the plume front. Our values for λ and λs may be used for glacial soils with similar mineralogy and texture. Our methods may also be used at other sites to construct the thermal conductivity distribution.
","doi":"10.2136/sssaj2005.0293","usgsCitation":"Markle, J.M., Schincariol, R.A., Sass, J., and Molson, J.W., Characterizing the two-dimensional thermal conductivity distribution in a sand and gravel aquifer: Soil Science Society of America Journal, v. 70, no. 4, p. 1281-1294, https://doi.org/10.2136/sssaj2005.0293.","productDescription":"14 p.","startPage":"1281","endPage":"1294","costCenters":[],"links":[{"id":368310,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","state":"Ontario","otherGeospatial":"Tricks Creek Watershed ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.0458984375,\n 43.52266348752663\n ],\n [\n -81.6998291015625,\n 43.52266348752663\n ],\n [\n -81.6998291015625,\n 43.94537239244209\n ],\n [\n -82.0458984375,\n 43.94537239244209\n ],\n [\n -82.0458984375,\n 43.52266348752663\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"70","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Markle, Jeff M.","contributorId":219782,"corporation":false,"usgs":false,"family":"Markle","given":"Jeff","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":773164,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schincariol, Robert A.","contributorId":219783,"corporation":false,"usgs":false,"family":"Schincariol","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":773165,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sass, J.H.","contributorId":70749,"corporation":false,"usgs":true,"family":"Sass","given":"J.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":773166,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Molson, John W.","contributorId":219784,"corporation":false,"usgs":false,"family":"Molson","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":773167,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70248281,"text":"70248281 - null - Scouting craton’s edge in Paleo-Pacific Gondwana","interactions":[],"lastModifiedDate":"2023-09-06T20:12:30.474783","indexId":"70248281","displayToPublicDate":"2006-01-01T14:47:51","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"chapter":"4.1","title":"Scouting craton’s edge in Paleo-Pacific Gondwana","docAbstract":"The geology of the ice-covered interior of the East Antarctic shield is completely unknown; inferences about its composition and history are based on extrapolating scant outcrops from the coast inland. Although the shield is clearly composite in nature, a large part of its interior has been represented by a single Precambrian block, termed the Mawson block, that includes the Archean-Mesoproterozoic Gawler and Curnamona cratons of Australia. In Australia, the Mawson block is bounded on the east by Neoproterozoic sedimentary rocks and the superimposed early Paleozoic Delamerian Orogen, marked by curvilinear belts of arc plutons, and on the west by the unexposed Coompana block and Mesoproterozoic Albany-Fraser mobile belt. In Antarctica, these crustal elements are inferred to extend across Wilkes Land and south to the Miller Range region. Aero- and satellite magnetic data provide a means to see through the ice, helping to elucidate the broad composition of the shield. Rocks of the Mawson block in Australia produce distinctive magnetic anomalies; Paleoproterozoic granites and Meso- to Neoproterozoic mafic igneous rocks are associated with high-amplitude, broad-wavelength positive aero- and satellite-magnetic anomalies. The same types of magnetic anomalies can be traced to ice-covered Wilkes Land, Antarctica, and are interpreted to signify similar rocks. However, the diagnostic satellite magnetic high ends ∼800 km south of the Antarctic coast, suggesting that the Mawson block is smaller than first proposed and that the remaining East Antarctic shield is composed of several Precambrian crustal blocks of largely undetermined composition and age. Nonetheless, the coincident eastern borders of these magnetic highs and high seismic-velocity anomalies characteristic of the Precambrian shield, together define the edge of thick cratonic lithosphere. East of this boundary, magnetic lows are explained by magnetite-poor upper Neoproterozoic and lower Paleozoic sedimentary rocks, and their metamorphic equivalents, which crop out discontinuously along the Ross margin of Antarctica and in eastern Australia. These rocks are inferred to overlie a Neoproterozoic rift margin, which transects older basement provinces. The coincidence of this cratonic rift boundary with the western limit of Paleozoic and Jurassic magmatism suggests that, although tectonically modified by younger events, the composite Antarctic-Australian shield comprised thick lithosphere that was not penetrated by Paleozoic and younger convergent-margin magmas.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Antarctica: Contributions to global earth sciences","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","doi":"10.1007/3-540-32934-X_20","usgsCitation":"Finn, C.A., Goodge, J.W., Damaske, D., and Fanning, C.M., Scouting craton’s edge in Paleo-Pacific Gondwana, chap. 4.1 of Antarctica: Contributions to global earth sciences, p. 165-173, https://doi.org/10.1007/3-540-32934-X_20.","productDescription":"9 p.","startPage":"165","endPage":"173","costCenters":[],"links":[{"id":420584,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Antarctica, Gondwana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 106.88469524334846,\n -57.49514229065598\n ],\n [\n 106.88469524334846,\n -78.93509637484914\n ],\n [\n 164.3416785133088,\n -78.93509637484914\n ],\n [\n 164.3416785133088,\n -57.49514229065598\n ],\n [\n 106.88469524334846,\n -57.49514229065598\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Futterer, Dieter Karl","contributorId":279857,"corporation":false,"usgs":false,"family":"Futterer","given":"Dieter","email":"","middleInitial":"Karl","affiliations":[],"preferred":false,"id":882257,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Kleinschmidt, Georg","contributorId":26968,"corporation":false,"usgs":true,"family":"Kleinschmidt","given":"Georg","email":"","affiliations":[],"preferred":false,"id":882258,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Miller, Hubert","contributorId":328909,"corporation":false,"usgs":false,"family":"Miller","given":"Hubert","email":"","affiliations":[],"preferred":false,"id":882259,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Tessensohn, Franz","contributorId":27196,"corporation":false,"usgs":true,"family":"Tessensohn","given":"Franz","email":"","affiliations":[],"preferred":false,"id":882260,"contributorType":{"id":2,"text":"Editors"},"rank":4}],"authors":[{"text":"Finn, Carol A. 0000-0002-6178-0405 cfinn@usgs.gov","orcid":"https://orcid.org/0000-0002-6178-0405","contributorId":1326,"corporation":false,"usgs":true,"family":"Finn","given":"Carol","email":"cfinn@usgs.gov","middleInitial":"A.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":882253,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goodge, John W.","contributorId":20414,"corporation":false,"usgs":true,"family":"Goodge","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":882254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Damaske, Detlef","contributorId":77384,"corporation":false,"usgs":true,"family":"Damaske","given":"Detlef","email":"","affiliations":[],"preferred":false,"id":882255,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fanning, C. Mark","contributorId":193462,"corporation":false,"usgs":false,"family":"Fanning","given":"C.","email":"","middleInitial":"Mark","affiliations":[],"preferred":false,"id":882256,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70242598,"text":"70242598 - null - Remnant damage from the 1906 San Francisco earthquake","interactions":[],"lastModifiedDate":"2023-04-10T17:02:43.389339","indexId":"70242598","displayToPublicDate":"2006-01-01T11:48:36","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Remnant damage from the 1906 San Francisco earthquake","docAbstract":"This field trip consists of two stops at locations where it is possible to see damage from the 1906 earthquake and to gauge the intensity of the ground shaking that caused the damage. The first stop is at a cemetery in Colma, where the damage to monuments and headstones was photographed and roughly quantified in the Report of the State Earthquake Investigation Commission, Lawson (1908), commonly referred to as the “Lawson Report.” The Lawson Report represents the formal study of the earthquake and consists of a compilation of the reports of many investigators who gathered information about faulting, ground failure, and damage due to the 1906 earthquake. The second stop is at a brick office building at the southern limit of San Francisco that was damaged by the earthquake but repaired in such a fashion that the damage is still clearly evident.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"1906 San Francisco earthquake centennial field guides: Field trips associated with the 100th Anniversary Conference, 18–23 April 2006, San Francisco, California","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"100th Anniversary Conference","conferenceDate":"April 18-23, 2006","conferenceLocation":"San Francisco, CA","language":"English","publisher":"Geological Society of America","doi":"10.1130/2006.1906SF(02)","usgsCitation":"Boatwright, J., Remnant damage from the 1906 San Francisco earthquake, chap. of 1906 San Francisco earthquake centennial field guides: Field trips associated with the 100th Anniversary Conference, 18–23 April 2006, San Francisco, California, p. 25-29, https://doi.org/10.1130/2006.1906SF(02).","productDescription":"5 p.","startPage":"25","endPage":"29","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":415500,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Colma, San Francisco","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.44458882597738,\n 37.665931425168225\n ],\n [\n -122.4366965123254,\n 37.67202373256798\n ],\n [\n -122.44393656865076,\n 37.6805417983678\n ],\n [\n -122.44582811489799,\n 37.68141936169974\n ],\n [\n -122.4513723021741,\n 37.68028368953031\n ],\n [\n -122.45685126371754,\n 37.676308700024876\n ],\n [\n -122.44889372433289,\n 37.66856460244338\n ],\n [\n -122.44458882597738,\n 37.6658281614107\n ],\n [\n -122.44458882597738,\n 37.665931425168225\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.44777106677859,\n 37.72084882908082\n ],\n [\n -122.44777106677859,\n 37.71895408813427\n ],\n [\n -122.44573210611418,\n 37.71895408813427\n ],\n [\n -122.44573210611418,\n 37.72084882908082\n ],\n [\n -122.44777106677859,\n 37.72084882908082\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Prentice, Carol S. 0000-0003-3732-3551 cprentice@usgs.gov","orcid":"https://orcid.org/0000-0003-3732-3551","contributorId":2676,"corporation":false,"usgs":true,"family":"Prentice","given":"Carol","email":"cprentice@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":869068,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Scotchmoor, Judith G.","contributorId":304052,"corporation":false,"usgs":false,"family":"Scotchmoor","given":"Judith","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":869069,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Moores, Eldridge M.","contributorId":304053,"corporation":false,"usgs":false,"family":"Moores","given":"Eldridge","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":869070,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Kiland, Jon P.","contributorId":304054,"corporation":false,"usgs":false,"family":"Kiland","given":"Jon","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":869071,"contributorType":{"id":2,"text":"Editors"},"rank":4}],"authors":[{"text":"Boatwright, John 0000-0002-6931-5241 boat@usgs.gov","orcid":"https://orcid.org/0000-0002-6931-5241","contributorId":1938,"corporation":false,"usgs":true,"family":"Boatwright","given":"John","email":"boat@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":869067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70208299,"text":"70208299 - null - Old-growth bottomland hardwood forests as bird habitat: Implications for contemporary management","interactions":[],"lastModifiedDate":"2020-02-03T12:33:56","indexId":"70208299","displayToPublicDate":"2005-12-31T12:31:20","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Old-growth bottomland hardwood forests as bird habitat: Implications for contemporary management","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Ecology and management of bottomland hardwood systems: The state of our understanding: A symposium","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Ecology and Management of Bottomland Hardwood Systems: The State of Our Understanding : A Symposium","conferenceDate":"Mar 11-13, 1999","conferenceLocation":"Memphis, TN","language":"English","publisher":"University of Missouri-Columbia","publisherLocation":"2005","usgsCitation":"Hamilton, R., Barrow, W., and Ouchley, K., Old-growth bottomland hardwood forests as bird habitat: Implications for contemporary management, in Ecology and management of bottomland hardwood systems: The state of our understanding: A symposium, Memphis, TN, Mar 11-13, 1999, p. 373-388.","productDescription":"16 p.","startPage":"373","endPage":"388","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":371942,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hamilton, Robert","contributorId":222134,"corporation":false,"usgs":false,"family":"Hamilton","given":"Robert","affiliations":[],"preferred":false,"id":781317,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barrow, Wylie C. Jr. 0000-0003-4671-2823 barroww@usgs.gov","orcid":"https://orcid.org/0000-0003-4671-2823","contributorId":168953,"corporation":false,"usgs":true,"family":"Barrow","given":"Wylie C.","suffix":"Jr.","email":"barroww@usgs.gov","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":781318,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ouchley, Keith","contributorId":216315,"corporation":false,"usgs":false,"family":"Ouchley","given":"Keith","email":"","affiliations":[],"preferred":false,"id":781319,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70263458,"text":"70263458 - null - Development of stochastic modeling systems using deterministic models and GIS: Principles and a case study in the Atlantic Zone of Costa Rica","interactions":[],"lastModifiedDate":"2025-02-11T16:55:21.741843","indexId":"70263458","displayToPublicDate":"2003-12-01T10:49:02","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Development of stochastic modeling systems using deterministic models and GIS: Principles and a case study in the Atlantic Zone of Costa Rica","docAbstract":"The most important requirements for large-area environmental modeling are a tight integration between models and data, and a close match of the spatial scale at which the model is developed with the scale at which the model is to be applied. To better match the scale of data with that of the model, we propose a set of principles for the development of stochastic modeling systems based on linkage of deterministic models with GIS data. For modeling purposes, a region is usually rasterized into cells and the environmental conditions of those cells are specified by ranges or classes using GIS data layers. It is not necessary to simulate each and every GIS cell in the study area because many cells may have similar environmental conditions and can be grouped together to form cohorts. We define a cohort as the assembly of the cells sharing a unique combination of environmental conditions within the study region. Multiple model simulations can be performed for any given cohort. For each simulation, some of the parameter values can be randomly generated within the specified environmental conditions of the cohort according to a certain statistical distribution which, in turn, can be specified by GIS data layers. By this method the variance and covariance of environmental variables in space and time are integrated into the simulation processes with these modeling systems to make full use of the available data and to assess the uncertainties of the simulated results. An integrated simulation system between CENTURY model and GIS was developed to demonstrate the value of the concepts imbedded in stochastic simulation systems for large area studies.
","conferenceTitle":"4th International Conference on Integrating GIS and Environmental Modeling (GIS/EM4)","conferenceDate":"September 2-8, 2000","conferenceLocation":"Banff, Alberta, Canada","language":"English","publisher":"University of Colorado, Cooperative Institute for Research in Environmental Sciences","usgsCitation":"Liu, S., Reiners, W.A., Gerow, K.G., Schimel, D.S., and Keller, M., Development of stochastic modeling systems using deterministic models and GIS: Principles and a case study in the Atlantic Zone of Costa Rica, 4th International Conference on Integrating GIS and Environmental Modeling (GIS/EM4), Banff, Alberta, Canada, September 2-8, 2000, 9 p.","productDescription":"9 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":481935,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Costa Rica","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -82.6133520275848,\n 9.499325548625436\n ],\n [\n -82.44230009071387,\n 9.73121764978167\n ],\n [\n -83.54701051633626,\n 11.16801392273345\n ],\n [\n -83.68242663302513,\n 10.951175271798036\n ],\n [\n -83.66104514091643,\n 10.78319089811086\n ],\n [\n -84.16707378749192,\n 10.566072375621317\n ],\n [\n -83.7038081251345,\n 9.604750752776496\n ],\n [\n -82.88418426096321,\n 9.506354909569495\n ],\n [\n -82.6133520275848,\n 9.499325548625436\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Liu, Shuguang 0000-0002-6027-3479 sliu@usgs.gov","orcid":"https://orcid.org/0000-0002-6027-3479","contributorId":147403,"corporation":false,"usgs":true,"family":"Liu","given":"Shuguang","email":"sliu@usgs.gov","affiliations":[{"id":223,"text":"Earth Resources Observation and Science (EROS) Center (Geography)","active":false,"usgs":true}],"preferred":true,"id":927046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reiners, William A.","contributorId":147117,"corporation":false,"usgs":false,"family":"Reiners","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":927047,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gerow, Kenneth G.","contributorId":49672,"corporation":false,"usgs":true,"family":"Gerow","given":"Kenneth","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":927048,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schimel, David S","contributorId":267312,"corporation":false,"usgs":false,"family":"Schimel","given":"David","email":"","middleInitial":"S","affiliations":[{"id":55473,"text":"Jep Propulsion Laboratory","active":true,"usgs":false}],"preferred":false,"id":927049,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Keller, Michael","contributorId":42681,"corporation":false,"usgs":true,"family":"Keller","given":"Michael","email":"","affiliations":[],"preferred":false,"id":927050,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70267836,"text":"ofr2000130 - null - Alaska resource data file: Chignak quadrangle","interactions":[],"lastModifiedDate":"2025-06-10T14:35:52.992213","indexId":"ofr2000130","displayToPublicDate":"2003-01-08T08:34:51","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":"2000-130","title":"Alaska resource data file: Chignak quadrangle","doi":"10.3133/ofr2000130","issn":"0094-9140","onlineOnly":"N","costCenters":[],"links":[{"id":489512,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/2000/0130/coverthb.jpg"},{"id":489513,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2000/0130/ofr00130.pdf"}],"publishedDate":"2003-01-08","noUsgsAuthors":false,"publicationDate":"2003-01-08","publicationStatus":"PW"} ,{"id":70206346,"text":"70206346 - null - Integrated geophysical characterization of the Winthrop Landfill Southern Flow Path, Winthrop, Maine","interactions":[],"lastModifiedDate":"2019-10-31T07:46:54","indexId":"70206346","displayToPublicDate":"2002-12-31T17:03:47","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Integrated geophysical characterization of the Winthrop Landfill Southern Flow Path, Winthrop, Maine","docAbstract":"The U.S. Geological Survey (USGS), in cooperation with United Technologies Corporation, used an integrated suite of borehole, surface, and water-borne geophysical methods near the site of the former Winthrop Landfill, Winthrop, Maine, to investigate the hydrogeology controlling the transport of leachate from the landfill to nearby Annabessacook Lake. During the fall of 2000 and summer of 2001, the USGS conducted borehole electromagnetic (EM) induction and gamma logging, and inductive terrain-conductivity, two-dimensional (2D) resistivity, continuous seismic reflection, and magnetic surveys.
The objectives of this integrated geophysical study were to provide constraints on the location and extent of the southern flow path(s) of contamination from the landfill to the lake; identify shoreline seep geophysical signatures; identify potentially hidden seeps in the lake; and determine depth to bedrock below Annabessacook Lake in the study area.
Interpretation of surface 2D resistivity, magnetic, and inductive terrain-conductivity data and borehole EM logs delineates an electrically conductive anomaly consistent with a leachate plume moving from the current landfill boundary southward through the overburden to the shores of Annabessacook Lake. Surface and borehole geophysical data collected south and southeast of the landfill indicate the presence of discrete, shallow conductive anomalies at the southeastern edge of the landfill and near the lakeshore. The conductive anomalies appear at increasing depths closer to the lake. Magnetic anomalies offshore confirm the presence of iron-rich landfill leachate discharging into the lake south of the landfill. High-resolution swept-frequency seismic data used to map sediment and grain size distribution in the lake sub-bottom along the shoreline identified sediment-infilled bedrock lows that may act as conduits for contaminant migration.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings: Symposium on the application of geophysics to engineering and environmental problems","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Symposium on the application of geophysics to engineering and environmental problems","conferenceDate":"February 10-14, 2002","conferenceLocation":"Las Vegas, NV","language":"English","publisher":"Environmental and Engineering Geophysical Society","usgsCitation":"Dawson, C.B., Lane, J., White, E.A., and Belaval, M., Integrated geophysical characterization of the Winthrop Landfill Southern Flow Path, Winthrop, Maine, in Proceedings: Symposium on the application of geophysics to engineering and environmental problems, Las Vegas, NV, February 10-14, 2002, 22 p.","productDescription":"22 p.","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"links":[{"id":368775,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":368774,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://water.usgs.gov/ogw/bgas/publications/SAGEEP02_13ESC6/"}],"country":"United States","state":"Maine","city":"Winthrop","otherGeospatial":"Winthrop Landfill","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -69.9964714050293,\n 44.269419395641016\n ],\n [\n -69.9580192565918,\n 44.269419395641016\n ],\n [\n -69.9580192565918,\n 44.31561943401762\n ],\n [\n -69.9964714050293,\n 44.31561943401762\n ],\n [\n -69.9964714050293,\n 44.269419395641016\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dawson, Cian B. cbdawson@usgs.gov","contributorId":1890,"corporation":false,"usgs":true,"family":"Dawson","given":"Cian","email":"cbdawson@usgs.gov","middleInitial":"B.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":774237,"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":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},{"id":486,"text":"OGW Branch of Geophysics","active":true,"usgs":true}],"preferred":true,"id":774238,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, Eric A. 0000-0002-7782-146X eawhite@usgs.gov","orcid":"https://orcid.org/0000-0002-7782-146X","contributorId":1737,"corporation":false,"usgs":false,"family":"White","given":"Eric","email":"eawhite@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":774239,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Belaval, Marcel 0000-0002-4049-6798","orcid":"https://orcid.org/0000-0002-4049-6798","contributorId":207205,"corporation":false,"usgs":false,"family":"Belaval","given":"Marcel","email":"","affiliations":[{"id":37476,"text":"U.S. EPA, Region 1","active":true,"usgs":false}],"preferred":false,"id":774240,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70208984,"text":"70208984 - null - Perspectives on the diagnosis, epizootiology, and control of the 1973 duck plague epizootic in wild waterfowl at Lake Andes, South Dakota","interactions":[],"lastModifiedDate":"2020-03-10T08:36:59","indexId":"70208984","displayToPublicDate":"1997-10-31T08:29:49","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Perspectives on the diagnosis, epizootiology, and control of the 1973 duck plague epizootic in wild waterfowl at Lake Andes, South Dakota","docAbstract":"An epizootic of duck plague occurred in early 1973 in a population of 163,500 wild waterfowl, primarily mallards (Anas platyrhynchos), wintering on Lake Andes and the nearby Missouri River in southeastern South Dakota (USA). The diagnosis was based on pathologic lesions and confirmed by virus isolation. Control measures included quarantine, attempts to reduce virus contamination of the area, dispersal of waterfowl, and monitoring of wild waterfowl populations for mortality. The epizootic resulted in documented mortality of 18% and estimated mortality of 26% of the waterfowl at risk. Prompt implementation of control measures might have limited mortality to approximately 8%. Losses during the epizootic were equivalent to 0.12% of the annual mortality in the North American 1996 fall population of 80,000,000 wild ducks. The most likely sources of the infection were free-flying wild mallard or American black duck (Anas rubripes) carriers from the upper midwestern or northeastern United States. Duck plague serum neutralization antibodies were demonstrated in 31% of 395 apparently healthy mallards sampled prior to dispersal of the flock at Lake Andes, suggesting that tens of thousands of potential duck plague carriers entered the wild waterfowl populations of all four major flyways. Consequently, the absence of major epizootics of duck plague in wild waterfowl in the subsequent two decades is evidence that substantial numbers of duck plague carriers can occur in wild waterfowl populations without resulting in epizootic mortalities. The failure to isolate duck plague virus from apparently healthy mallards sampled during the epizootic raises questions concerning the validity of conclusions regarding the status of duck plague in wild waterfowl based upon negative results of random surveys conducted in the absence of epizootics. © Wildlife Disease Association 1997.
","language":"English","doi":"10.7589/0090-3558-33.4.681","issn":"00903558","usgsCitation":"Pearson, G.L., and Cassidy, D.R., Perspectives on the diagnosis, epizootiology, and control of the 1973 duck plague epizootic in wild waterfowl at Lake Andes, South Dakota: Journal of Wildlife Diseases, v. 33 , no. 4, p. 681-705, https://doi.org/10.7589/0090-3558-33.4.681.","productDescription":"25 p. ","startPage":"681","endPage":"705","costCenters":[],"links":[{"id":373039,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"South Dakota ","county":"Charles Mix County ","city":"Lake Andes ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -100.1678466796875,\n 43.032760685832\n ],\n [\n -98.54736328125,\n 43.032760685832\n ],\n [\n -98.54736328125,\n 44.02442151965934\n ],\n [\n -100.1678466796875,\n 44.02442151965934\n ],\n [\n -100.1678466796875,\n 43.032760685832\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"33 ","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pearson, Gary L.","contributorId":76676,"corporation":false,"usgs":true,"family":"Pearson","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":784413,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cassidy, Delmar R.","contributorId":223166,"corporation":false,"usgs":false,"family":"Cassidy","given":"Delmar","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":784414,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70205042,"text":"70205042 - null - Detecting hurricane impact and recovery from tree rings","interactions":[],"lastModifiedDate":"2019-08-28T15:26:57","indexId":"70205042","displayToPublicDate":"1996-12-31T15:21:17","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"title":"Detecting hurricane impact and recovery from tree rings","docAbstract":"No abstract available
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Tree Rings, Environment, and Humanity","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Proceedings of the International Conference","conferenceDate":"May 17-21, 1994","conferenceLocation":"Tuscon, AZ","language":"English","usgsCitation":"Doyle, T.W., Detecting hurricane impact and recovery from tree rings, in Tree Rings, Environment, and Humanity, Tuscon, AZ, May 17-21, 1994, p. 405-412.","productDescription":"8 p.","startPage":"405","endPage":"412","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":367027,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana, Mississippi","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.845947265625,\n 29.219302076779456\n ],\n [\n -87.451171875,\n 29.219302076779456\n ],\n [\n -87.451171875,\n 31.400535326863935\n ],\n [\n -90.845947265625,\n 31.400535326863935\n ],\n [\n -90.845947265625,\n 29.219302076779456\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Doyle, Thomas W. 0000-0001-5754-0671 doylet@usgs.gov","orcid":"https://orcid.org/0000-0001-5754-0671","contributorId":703,"corporation":false,"usgs":true,"family":"Doyle","given":"Thomas","email":"doylet@usgs.gov","middleInitial":"W.","affiliations":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"preferred":true,"id":769727,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70246753,"text":"70246753 - null - Exsolved magmatic fluid and its role in the formation of comb-layered quartz at the Cretaceous Logtung W-Mo deposit, Yukon Territory, Canada","interactions":[],"lastModifiedDate":"2023-07-18T16:21:51.724071","indexId":"70246753","displayToPublicDate":"1996-01-01T11:13:58","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Exsolved magmatic fluid and its role in the formation of comb-layered quartz at the Cretaceous Logtung W-Mo deposit, Yukon Territory, Canada","docAbstract":"Comb-layered quartz is a type of unidirectional solidification texture found at the roofs of shallow silicic intrusions that are often associated spatially with Mo and W mineralisation. The texture consists of multiple layers of euhedral, prismatic quartz crystals (Type I) that have grown on subplanar aplite substrates. The layers are separated by porphyritic aplite containing equant phenocrysts of quartz (Type II), which resemble quartz typical of volcanic rocks and porphyry intrusions. At Logtung, Type I quartz within comb layers is zoned with respect to a number of trace elements, including Al and K. Concentrations of these elements as well as Mn, Ti, Ge, Rb and H are anomalous and much higher than found in Type II quartz from Logtung or in igneous quartz reported elsewhere. The two populations appear to have formed under different conditions. The Type II quartz phenocrysts almost certainly grew from a high-silica melt between 600 and 800°C (as β-quartz); in contrast, the morphology of Type I quartz is consistent with precipitation from a hydrothermal solution, possibly as α-quartz grown below 600°C. The bulk compositions of comb-layered rocks, as well as the aplite interlayers, are consistent with the hypothesis that these textures did not precipitate solely from a crystallising silicate melt. Instead, Type I quartz may have grown from pockets of exsolved magmatic fluid located between the magma and its crystallised border. The Type II quartz represents pre-existing phenocrysts in the underlying magma; this magma was quenched to aplite during fracturing/degassing events. Renewed and repeated formation and disruption of the pockets of exsolved aqueous fluid accounts for the rhythmic banding of the rocks.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Third Hutton symposium on the origin of granites and related rocks","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisherLocation":"1996","doi":"10.1130/0-8137-2315-9.291","usgsCitation":"Lowenstern, J.B., and Sinclair, W.D., Exsolved magmatic fluid and its role in the formation of comb-layered quartz at the Cretaceous Logtung W-Mo deposit, Yukon Territory, Canada, chap. of The Third Hutton symposium on the origin of granites and related rocks, v. 315, p. 291-303, https://doi.org/10.1130/0-8137-2315-9.291.","productDescription":"13 p.","startPage":"291","endPage":"303","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":419057,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","state":"Yukon Territory","otherGeospatial":"Logtung","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -131.918034408077,\n 60.00963320120135\n ],\n [\n -131.9420601623024,\n 60.00963320120135\n ],\n [\n -131.9420601623024,\n 60.000111867680914\n ],\n [\n -131.918034408077,\n 60.000111867680914\n ],\n [\n -131.918034408077,\n 60.00963320120135\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"315","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lowenstern, Jacob B. 0000-0003-0464-7779 jlwnstrn@usgs.gov","orcid":"https://orcid.org/0000-0003-0464-7779","contributorId":2755,"corporation":false,"usgs":true,"family":"Lowenstern","given":"Jacob","email":"jlwnstrn@usgs.gov","middleInitial":"B.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":878174,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sinclair, W. David","contributorId":69123,"corporation":false,"usgs":true,"family":"Sinclair","given":"W.","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":878175,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70207050,"text":"70207050 - null - Geodetic monitoring of the southern San Andreas Fault, California, 1980-1991","interactions":[],"lastModifiedDate":"2020-05-28T12:49:02.247298","indexId":"70207050","displayToPublicDate":"1995-12-04T14:40:08","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2312,"text":"Journal of Geophysical Research","active":true,"publicationSubtype":{"id":10}},"title":"Geodetic monitoring of the southern San Andreas Fault, California, 1980-1991","docAbstract":"Five geodetic arrays (10 to 40 km aperture) located along the San Andreas fault have been surveyed frequently (several times in most years) over the 1980–1991 interval to detect possible fluctuations in the deformation rate. In each survey of an array the distances between the same four to seven pairs of geodetic monuments were measured. The distances measured (with corresponding standard deviation) range from 8.4 km (3.4 mm) to 38 km (8.2 mm). The data are displayed as plots of measured distance as a function of time. Linear fits in such plots furnish a satisfactory representation of the data. That is, the scatter of the data about the linear fits is within the range expected for the estimated standard deviations in measurement. However, there are coherent low‐amplitude (within the observational error) fluctuations apparent in some of the measured distances. Those fluctuations need not be tectonic effects but rather may be either random patterns or artifacts introduced by systematic drift in instrument calibration or wander of the geodetic monuments. We conclude that the measurements are consistent with steady deformation of the arrays over the 1980–1991 interval, and we find no convincing evidence in the data for fluctuations in the rate of deformation.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/95JB00611","usgsCitation":"Savage, J.C., and Lisowski, M., Geodetic monitoring of the southern San Andreas Fault, California, 1980-1991: Journal of Geophysical Research, v. 100, no. B5, p. 8185-8192, https://doi.org/10.1029/95JB00611.","productDescription":"8 p.","startPage":"8185","endPage":"8192","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":369910,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.06933593749999,\n 33.7243396617476\n ],\n [\n -115.57617187499999,\n 33.7243396617476\n ],\n [\n -115.57617187499999,\n 35.88905007936091\n ],\n [\n -121.06933593749999,\n 35.88905007936091\n ],\n [\n -121.06933593749999,\n 33.7243396617476\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"100","issue":"B5","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Savage, James C. 0000-0002-5114-7673 jasavage@usgs.gov","orcid":"https://orcid.org/0000-0002-5114-7673","contributorId":2412,"corporation":false,"usgs":true,"family":"Savage","given":"James","email":"jasavage@usgs.gov","middleInitial":"C.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":776635,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lisowski, Michael 0000-0003-4818-2504 mlisowski@usgs.gov","orcid":"https://orcid.org/0000-0003-4818-2504","contributorId":637,"corporation":false,"usgs":true,"family":"Lisowski","given":"Michael","email":"mlisowski@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"preferred":true,"id":776636,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70206252,"text":"70206252 - null - Use of surface-geophysical and borehole-radar methods to detect fractures in crystalline rocks, Mirror Lake area, Grafton County, New Hampshire","interactions":[],"lastModifiedDate":"2019-10-28T06:47:00","indexId":"70206252","displayToPublicDate":"1993-12-31T14:38:22","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Use of surface-geophysical and borehole-radar methods to detect fractures in crystalline rocks, Mirror Lake area, Grafton County, New Hampshire","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hydrogeology of hard rocks: Memoires of the XXIVth Congress","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"24th Congress, Hydrogeology of Hard Rocks","conferenceDate":"June 28-July 2, 1993","conferenceLocation":"Oslo, Norway","language":"English","publisher":"Geological Survey of Norway","usgsCitation":"Haeni, F., Lane, J., and Lieblich, D., Use of surface-geophysical and borehole-radar methods to detect fractures in crystalline rocks, Mirror Lake area, Grafton County, New Hampshire, in Hydrogeology of hard rocks: Memoires of the XXIVth Congress, Oslo, Norway, June 28-July 2, 1993, p. 577-587.","productDescription":"11 p.","startPage":"577","endPage":"587","costCenters":[{"id":493,"text":"Office of Ground Water","active":true,"usgs":true}],"links":[{"id":368628,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Hampshire","county":"Grafton County","otherGeospatial":"Mirror Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.71866416931152,\n 43.92590275678158\n ],\n [\n -71.67343139648438,\n 43.92590275678158\n ],\n [\n -71.67343139648438,\n 43.96149954712646\n ],\n [\n -71.71866416931152,\n 43.96149954712646\n ],\n [\n -71.71866416931152,\n 43.92590275678158\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":773934,"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":493,"text":"Office of Ground Water","active":true,"usgs":true},{"id":486,"text":"OGW Branch of Geophysics","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":773935,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lieblich, D.A.","contributorId":73645,"corporation":false,"usgs":true,"family":"Lieblich","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":773936,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70208982,"text":"70208982 - null - The ecology of Humboldt Bay, California, an estuarine profile","interactions":[],"lastModifiedDate":"2020-03-09T20:11:54","indexId":"70208982","displayToPublicDate":"1992-12-31T19:55:13","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":93,"text":"U.S. Fish and Wildlife Service Biological Report","active":false,"publicationSubtype":{"id":1}},"title":" The ecology of Humboldt Bay, California, an estuarine profile","docAbstract":"Synthesizes data on the ecological relationships and functions of the estuary, including information on physical aspects of the bay environment; describes the biotic communities and their relationships; provides management considerations in terms including environmental concerns; and identifies research and management information gaps. Portions of the bay are managed as a national wildlife refuge. Management issues for this ecosystem include loss of habitat and degradation of the environment by additional industrial development and nonpoint source pollution. -from Authors
","language":"English","publisher":"Elsevier ","usgsCitation":"Barnhart, R., Boyd, M., and Pequegnat, J., The ecology of Humboldt Bay, California, an estuarine profile: U.S. Fish and Wildlife Service Biological Report, v. 1, 121 p. .","productDescription":"121 p. ","numberOfPages":"121","costCenters":[{"id":150,"text":"California Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"links":[{"id":373032,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"California ","county":"Humboldt","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.134521484375,\n 41.0565730874647\n ],\n [\n -123.72802734375,\n 41.0565730874647\n ],\n [\n -123.72802734375,\n 41.599013054830216\n ],\n [\n -124.134521484375,\n 41.599013054830216\n ],\n [\n -124.134521484375,\n 41.0565730874647\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Barnhart, R.A.","contributorId":223148,"corporation":false,"usgs":false,"family":"Barnhart","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":784286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boyd, M.J.","contributorId":223149,"corporation":false,"usgs":false,"family":"Boyd","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":784287,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pequegnat, J.E.","contributorId":223150,"corporation":false,"usgs":false,"family":"Pequegnat","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":784288,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70206821,"text":"70206821 - null - Using GIS to determine the effects of contaminated sediments on natural resources in an estuary","interactions":[],"lastModifiedDate":"2019-11-22T16:47:23","indexId":"70206821","displayToPublicDate":"1992-12-31T16:33:58","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Using GIS to determine the effects of contaminated sediments on natural resources in an estuary","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the second international US Fish and Wildlife Service geographic information systems workshop","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Second International U. S. Fish and Wildlife Service Geographic Information Systems Workshop","conferenceDate":"June 10-13, 1991","conferenceLocation":"Fort Collins, CO","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Roscigno, P., Martin, G.M., Johnston, J.B., and Watzin, M.C., Using GIS to determine the effects of contaminated sediments on natural resources in an estuary, in Proceedings of the second international US Fish and Wildlife Service geographic information systems workshop, Fort Collins, CO, June 10-13, 1991, p. 41-50.","productDescription":"10 p.","startPage":"41","endPage":"50","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":369504,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alabama","otherGeospatial":"Mobile Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.13232421875,\n 30.548069799103555\n ],\n [\n -88.385009765625,\n 30.479449996609706\n ],\n [\n -88.36029052734375,\n 30.268556249047727\n ],\n [\n -87.62695312499999,\n 30.29701788337205\n ],\n [\n -87.62420654296875,\n 30.510216587229984\n ],\n [\n -87.8302001953125,\n 30.493651170505892\n ],\n [\n -87.791748046875,\n 30.873940237887624\n ],\n [\n -88.10211181640624,\n 30.878654895778272\n ],\n [\n -88.12408447265625,\n 30.786677249436945\n ],\n [\n -88.13232421875,\n 30.548069799103555\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Roscigno, P.F.","contributorId":67628,"corporation":false,"usgs":true,"family":"Roscigno","given":"P.F.","affiliations":[],"preferred":false,"id":775932,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, G. M.","contributorId":220843,"corporation":false,"usgs":false,"family":"Martin","given":"G.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":775933,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnston, J. B.","contributorId":220844,"corporation":false,"usgs":false,"family":"Johnston","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":775934,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Watzin, Mary C.","contributorId":214534,"corporation":false,"usgs":false,"family":"Watzin","given":"Mary","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":775935,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70236906,"text":"70236906 - null - Radiation exposure near Chernobyl based on analysis of conifer injury using Thematic Mapper satellite images","interactions":[],"lastModifiedDate":"2022-09-21T14:57:59.249544","indexId":"70236906","displayToPublicDate":"1988-12-31T09:51:28","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Radiation exposure near Chernobyl based on analysis of conifer injury using Thematic Mapper satellite images","docAbstract":"No abstract available.
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","doi":"10.1029/JC092iC02p01817","usgsCitation":"Cacchione, D., Grant, W., Drake, D., and Glenn, S., Storm‐dominated bottom boundary layer dynamics on the Northern California Continental Shelf: Measurements and predictions: Journal of Geophysical Research C: Oceans, v. 92, no. C2, p. 1817-1827, https://doi.org/10.1029/JC092iC02p01817.","productDescription":"11 p.","startPage":"1817","endPage":"1827","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":373529,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Northern California Continental Shelf","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.2718505859375,\n 37.99183365313853\n ],\n [\n -122.7008056640625,\n 37.99183365313853\n ],\n [\n -122.7008056640625,\n 39.00211029922515\n ],\n [\n -124.2718505859375,\n 39.00211029922515\n ],\n [\n -124.2718505859375,\n 37.99183365313853\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"92","issue":"C2","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"Cacchione, D.A.","contributorId":65448,"corporation":false,"usgs":true,"family":"Cacchione","given":"D.A.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":785618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grant, W.D.","contributorId":11764,"corporation":false,"usgs":true,"family":"Grant","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":785619,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Drake, D.E.","contributorId":48150,"corporation":false,"usgs":true,"family":"Drake","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":785620,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Glenn, S.M.","contributorId":223608,"corporation":false,"usgs":false,"family":"Glenn","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":785621,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70204780,"text":"70204780 - null - Summary of the conference and information needs for mitigation in wetlands","interactions":[],"lastModifiedDate":"2019-08-15T12:46:53","indexId":"70204780","displayToPublicDate":"1986-12-31T12:45:27","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"seriesNumber":"86-14","chapter":"8","title":"Summary of the conference and information needs for mitigation in wetlands","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Wetland Functions, Rehabilitation, and Creation in the Pacific Northwest: The State of our Understanding ","largerWorkSubtype":{"id":2,"text":"State or Local Government Series"},"conferenceDate":"Apr 30-May 2, 1986","conferenceLocation":"Port Townsend, WA","usgsCitation":"Quammen, M.L., Summary of the conference and information needs for mitigation in wetlands, chap. 8 of Wetland Functions, Rehabilitation, and Creation in the Pacific Northwest: The State of our Understanding , p. 151-158.","productDescription":"8 p.","startPage":"151","endPage":"158","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":366573,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":366572,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://fortress.wa.gov/ecy/publications/SummaryPages/8614.html"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Quammen, Millicent L.","contributorId":218143,"corporation":false,"usgs":false,"family":"Quammen","given":"Millicent","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":768462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70204765,"text":"70204765 - null - Vegetation pattern on channel features in the Passage Creek Gorge, Virginia","interactions":[],"lastModifiedDate":"2019-08-14T10:53:25","indexId":"70204765","displayToPublicDate":"1983-08-14T10:46:13","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1195,"text":"Castanea","active":true,"publicationSubtype":{"id":10}},"title":"Vegetation pattern on channel features in the Passage Creek Gorge, Virginia","docAbstract":"Persistent distribution patterns of woody vegetation within the bottomland forest of Passage Creek, Virginia, were related to fluvial landforms, channel geometry, streamflow characteristics, and sediment-size characteristics. Vegetation patterns were determined from species presence as observed in transects and traverses on landforms developed along the stream. Distinct species distributional patterns were found on four common fluvial geomorphic landforms: depositional bar, active-channel shelf, floodplain, and terrace. Independent hydrologic characteristics (flow duration and flood frequency) were determined for each of the landforms. Vegetation data were analyzed by binary discriminant analysis, principal components analysis, and detrended correspondence analysis. Results and related field observations suggest that certain species are significantly associated with specific fluvial landforms. Vegetation patterns appear to develop more as a result of hydrologic processes associated with each fluvial landform rather than from sediment-size characteristics. Flood disturbance may be an important factor in maintaining the vegetation patterns, which may therefore be used as indicators for particular hydrogeomorphic site conditions.
No abstract available.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Milankovitch and Climate: Understanding the Response to Astronomical Forcing","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"Advanced Research Workshop on Milankovitch and Climate","conferenceDate":"November 30- December 4, 1982","conferenceLocation":"Palisades, New York","language":"English","publisher":"Springer","usgsCitation":"Arthur, M., Dean, W.E., Bottjer, D., and Scholle, P.A., Rhythmic bedding in Mesozoic- Cenozoic pelagic carbonate sequences: The primary and diagenetic origin of Milankovitch-like cycles, in Milankovitch and Climate: Understanding the Response to Astronomical Forcing, v. 1, Palisades, New York, November 30- December 4, 1982, p. 191-222.","productDescription":"32","startPage":"191","endPage":"222","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374584,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Arthur, M.A.","contributorId":24791,"corporation":false,"usgs":true,"family":"Arthur","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":788812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dean, Walter E. dean@usgs.gov","contributorId":1801,"corporation":false,"usgs":true,"family":"Dean","given":"Walter","email":"dean@usgs.gov","middleInitial":"E.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":788813,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bottjer, D.J.","contributorId":73370,"corporation":false,"usgs":true,"family":"Bottjer","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":788814,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scholle, Peter A.","contributorId":48954,"corporation":false,"usgs":true,"family":"Scholle","given":"Peter","email":"","middleInitial":"A.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"preferred":false,"id":788815,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}