Earthquakes and tsunamis pose significant threats to Pacific Northwest coastal port and harbor communities. Developing holistic mitigation and preparedness strategies to reduce the potential for loss of life and property damage requires community-wide vulnerability assessments that transcend traditional site-specific analyses. The ability of a geographic information system (GIS) to integrate natural, socioeconomic, and hazards information makes it an ideal assessment tool to support community hazard planning efforts. This article summarizes how GIS was used to assess the vulnerability of an Oregon port and harbor community to earthquake and tsunami hazards, as part of a larger risk-reduction planning initiative. The primary purposes of the GIS were to highlight community vulnerability issues and to identify areas that both are susceptible to hazards and contain valued port and harbor community resources. Results of the GIS analyses can help decision makers with limited mitigation resources set priorities for increasing community resiliency to natural hazards.
Western West Virginia lies downwind from numerous coal-fired power plants along the Ohio River Valley. To test whether geochemical and mineralogical impacts from these power plants are detectable on the West Virginia landscape, we obtained reservoir cores, soils, and rocks from two separate sites in West Virginia, one in Harrison County (Hinkel and Deegan Reservoirs) and the other in Roane County (Miletree Run Reservoir). Both have small drainage basins that have the effect of maximizing atmospheric inputs relative to weathering inputs. Sediments from Hinkel Reservoir were dated using the 137Cs method, and by knowledge of the age of the base of the sedimentary section. Major elements in Hinkel Reservoir sediments do not vary systematically over time, suggesting that the depositional history of these sediments has been relatively constant. In contrast, minor elements and sulfur do show dramatic shifts. Zn, Pb, As, S, Cd, Ge, and Hg all peak during the late 1960s and early 1970s. Polyaromatic hydrocarbons associated with combustion processes likewise show this same behavior. Coincident with these maxima is a peak in isothermal remnant magnetization (IRM), a parameter that is proportional to magnetite abundance. We separated the magnetic fraction of the sediments and examined this fraction petrographically. It is dominated by magnetite with a spherical morphology, which is characteristic of magnetite produced by combustion processes. Chemical analyses on local rocks showed that they were not the likely source for the trace element and magnetite enrichments. To compare soils and reservoir sediments, we normalized geochemical data to Ti; the underlying assumption is that Ti will track physical inputs of soil materials into the reservoir sediments. The normalized sediment data for the elements Zn, Pb, As, and S are all higher for sediments deposited during the late 1960s and early 1970s compared to normalized soil data, implying that soils are not the source for the element enrichments. We thus attribute the enrichment to atmospheric inputs. However, a coal-burning zinc smelter within 10 km of the reservoir site that operated until 1971 may have supplied some or all of the anomalous input: There are no nearby major atmospheric pollution sites near Miletree Run Reservoir. A core from this reservoir was dated based on knowledge of the time it was impounded. Like Hinkel Reservoir, there are no systematic shifts in major element contents over its depositional history. Like Hinkel Reservoir, there are also significant shifts in trace elements and IRM that cannot be explained by local soil sources. Magnetic separates from this reservoir are also dominated by spherical combustion-produced magnetite. Covariance over the period 1930-1980 between magnetite and sulfur with US SO2 production (which comes dominantly from coal combustion) is strongly suggestive of a significant atmospheric input into Miletree Run Reservoir sediments. The nearest upwind power plants are between 50 and 75 km distant. Thus, relatively long distance transmission of particulate matter from the power plants of the Ohio River Valley is likely in this case.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geochemical investigations in earth and space sciences","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Elsevier","doi":"10.1016/S1873-9881(04)80014-2","usgsCitation":"Goldhaber, M.B., Callender, T., and Reynolds, R.L., 2004, The geochemical and magnetic record of coal combustion products in West Virginia reservoir sediments and soils, chap. of Geochemical investigations in earth and space sciences, v. 9, p. 159-186, https://doi.org/10.1016/S1873-9881(04)80014-2.","productDescription":"28 p.","startPage":"159","endPage":"186","costCenters":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"links":[{"id":374098,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"West Virginia","county":"Harrison County","otherGeospatial":"Deegan Reservoir, Hinkel Reservoir","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -80.25744438171387,\n 39.26507167693608\n ],\n [\n -80.24669408798218,\n 39.26507167693608\n ],\n [\n -80.24669408798218,\n 39.275188319478964\n ],\n [\n -80.25744438171387,\n 39.275188319478964\n ],\n [\n -80.25744438171387,\n 39.26507167693608\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":788217,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Callender, Ted","contributorId":224410,"corporation":false,"usgs":false,"family":"Callender","given":"Ted","email":"","affiliations":[],"preferred":false,"id":788218,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":788219,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70189443,"text":"70189443 - 2004 - Environmental assessment","interactions":[],"lastModifiedDate":"2017-07-13T09:33:41","indexId":"70189443","displayToPublicDate":"2004-06-16T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"title":"Environmental assessment","docAbstract":"Final report of the Independent US Assessment Team, Section 5.
The aftershock zone of the 3 November 2002, M = 7.9 earthquake that ruptured along the right-slip Denali fault in south-central Alaska has been investigated by using gravity and magnetic, magnetotelluric, and deep-crustal, seismic reflection data as well as outcrop geology and earthquake seismology. Strong seismic reflections from within the Alaska Range orogen north of the Denali fault dip as steeply as 25°N and extend to depths as great as 20 km. These reflections outline a relict crustal architecture that in the past 20 yr has produced little seismicity. The Denali fault is nonreflective, probably because this fault dips steeply to vertical. The most intriguing finding from geophysical data is that earthquake aftershocks occurred above a rock body, with low electrical resistivity (>10 Ω·m), that is at depths below ∼10 km. Aftershocks of the Denali fault earthquake have mainly occurred shallower than 10 km. A high geothermal gradient may cause the shallow seismicity. Another possibility is that the low resistivity results from fluids, which could have played a role in locating the aftershock zone by reducing rock friction within the middle and lower crust.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/G20127.1","usgsCitation":"Fisher, M.A., Nokleberg, W.J., Ratchkovski, N.A., Pellerin, L., Glen, J.M., Brocher, T.M., and Booker, J., 2004, Geophysical investigation of the Denali fault and Alaska Range orogen within the aftershock zone of the October–November 2002, M = 7.9 Denali fault earthquake: Geology, v. 32, no. 3, p. 269-272, https://doi.org/10.1130/G20127.1.","productDescription":"4 p.","startPage":"269","endPage":"272","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":375523,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Range, Denali Fault","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -153.544921875,\n 59.987997631212224\n ],\n [\n -141.328125,\n 59.987997631212224\n ],\n [\n -141.328125,\n 63.966318784384235\n ],\n [\n -153.544921875,\n 63.966318784384235\n ],\n [\n -153.544921875,\n 59.987997631212224\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"32","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fisher, Michael A. mfisher@usgs.gov","contributorId":1991,"corporation":false,"usgs":true,"family":"Fisher","given":"Michael","email":"mfisher@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":790796,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nokleberg, Warren J. 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":2077,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","middleInitial":"J.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":790797,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ratchkovski, N. A.","contributorId":225178,"corporation":false,"usgs":false,"family":"Ratchkovski","given":"N.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":790798,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pellerin, Louise","contributorId":20824,"corporation":false,"usgs":true,"family":"Pellerin","given":"Louise","email":"","affiliations":[],"preferred":false,"id":790799,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Glen, Jonathan M.G. 0000-0002-3502-3355 jglen@usgs.gov","orcid":"https://orcid.org/0000-0002-3502-3355","contributorId":176530,"corporation":false,"usgs":true,"family":"Glen","given":"Jonathan","email":"jglen@usgs.gov","middleInitial":"M.G.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":790800,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Brocher, Thomas M. 0000-0002-9740-839X brocher@usgs.gov","orcid":"https://orcid.org/0000-0002-9740-839X","contributorId":262,"corporation":false,"usgs":true,"family":"Brocher","given":"Thomas","email":"brocher@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":790801,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Booker, J.","contributorId":20540,"corporation":false,"usgs":true,"family":"Booker","given":"J.","email":"","affiliations":[],"preferred":false,"id":790802,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":70210584,"text":"70210584 - 2004 - Geophysical data reveal the crustal structure of the Alaska range orogen within the aftershock zone of the Mw 7.9 Denali fault earthquake","interactions":[],"lastModifiedDate":"2020-06-10T19:07:12.569482","indexId":"70210584","displayToPublicDate":"2004-06-10T13:49:06","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1135,"text":"Bulletin of the Seismological Society of America","onlineIssn":"1943-3573","printIssn":"0037-1106","active":true,"publicationSubtype":{"id":10}},"title":"Geophysical data reveal the crustal structure of the Alaska range orogen within the aftershock zone of the Mw 7.9 Denali fault earthquake","docAbstract":"Geophysical information, including deep-crustal seismic reflection, magnetotelluric (mt), gravity, and magnetic data, cross the aftershock zone of the 3 November 2002 Mw 7.9 Denali fault earthquake. These data and aftershock seismicity, jointly interpreted, reveal the crustal structure of the right-lateral-slip Denali fault and the eastern Alaska Range orogen, as well as the relationship between this structure and seismicity. North of the Denali fault, strong seismic reflections from within the Alaska Range orogen show features that dip as steeply as 25° north and extend downward to depths between 20 and 25 km. These reflections reveal crustal structures, probably ductile shear zones, that most likely formed during the Late Cretaceous, but these structures appear to be inactive, having produced little seismicity during the past 20 years. Furthermore, seismic reflections mainly dip north, whereas alignments in aftershock hypocenters dip south. The Denali fault is nonreflective, but modeling of mt, gravity, and magnetic data suggests that the Denali fault dips steeply to vertically. However, in an alternative structural model, the Denali fault is defined by one of the reflection bands that dips to the north and flattens into the middle crust of the Alaska Range orogen. Modeling of mt data indicates a rock body, having low electrical resistivity (>10 Ω·m), that lies mainly at depths greater than 10 km, directly beneath aftershocks of the Denali fault earthquake. The maximum depth of aftershocks along the Denali fault is 10 km. This shallow depth may arise from a higher-than-normal geothermal gradient. Alternatively, the low electrical resistivity of deep rocks along the Denali fault may be associated with fluids that have weakened the lower crust and helped determine the depth extent of the aftershock zone.
","language":"English","publisher":"SSA","doi":"10.1785/0120040613","usgsCitation":"Fisher, M.A., Ratchkovski, N., Nokleberg, W., Pellerin, L., and Glen, J.M., 2004, Geophysical data reveal the crustal structure of the Alaska range orogen within the aftershock zone of the Mw 7.9 Denali fault earthquake: Bulletin of the Seismological Society of America, v. 94, no. 6B, p. S107-S131, https://doi.org/10.1785/0120040613.","productDescription":"25 p.","startPage":"S107","endPage":"S131","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":375501,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -148.798828125,\n 62.14497603754045\n ],\n [\n -142.734375,\n 62.14497603754045\n ],\n [\n -142.734375,\n 64.54844014422517\n ],\n [\n -148.798828125,\n 64.54844014422517\n ],\n [\n -148.798828125,\n 62.14497603754045\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"94","issue":"6B","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fisher, M. A.","contributorId":69972,"corporation":false,"usgs":true,"family":"Fisher","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":790683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ratchkovski, N.","contributorId":89316,"corporation":false,"usgs":true,"family":"Ratchkovski","given":"N.","affiliations":[],"preferred":false,"id":790684,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nokleberg, Warren 0000-0002-1574-8869 wnokleberg@usgs.gov","orcid":"https://orcid.org/0000-0002-1574-8869","contributorId":204786,"corporation":false,"usgs":true,"family":"Nokleberg","given":"Warren","email":"wnokleberg@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":790685,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pellerin, Louise","contributorId":20824,"corporation":false,"usgs":true,"family":"Pellerin","given":"Louise","email":"","affiliations":[],"preferred":false,"id":790686,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Glen, Jonathan M.G. 0000-0002-3502-3355 jglen@usgs.gov","orcid":"https://orcid.org/0000-0002-3502-3355","contributorId":176530,"corporation":false,"usgs":true,"family":"Glen","given":"Jonathan","email":"jglen@usgs.gov","middleInitial":"M.G.","affiliations":[{"id":309,"text":"Geology and Geophysics Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":790687,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70170065,"text":"70170065 - 2004 - Responses of male fathead minnows to wastewater effluent--Indications of causative factors","interactions":[],"lastModifiedDate":"2016-04-04T12:29:06","indexId":"70170065","displayToPublicDate":"2004-06-01T13:30:00","publicationYear":"2004","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":18,"text":"Abstract or summary"},"title":"Responses of male fathead minnows to wastewater effluent--Indications of causative factors","docAbstract":"No abstract available.
","conferenceTitle":"Minnesota Water 2004--Policy and planning to ensure Minnesota's water supplies","conferenceDate":"March 23-24, 2004","conferenceLocation":"Minneapolis, MN","language":"English","usgsCitation":"Lee, K.E., Barber, L.B., and Schoenfuss, H., 2004, Responses of male fathead minnows to wastewater effluent--Indications of causative factors, Minnesota Water 2004--Policy and planning to ensure Minnesota's water supplies, Minneapolis, MN, March 23-24, 2004.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":319773,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"570390f2e4b0328dcb81c6c0","contributors":{"authors":[{"text":"Lee, K. E.","contributorId":100014,"corporation":false,"usgs":true,"family":"Lee","given":"K.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":625978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barber, L. B.","contributorId":64602,"corporation":false,"usgs":true,"family":"Barber","given":"L.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":625979,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schoenfuss, H.L.","contributorId":103877,"corporation":false,"usgs":true,"family":"Schoenfuss","given":"H.L.","affiliations":[],"preferred":false,"id":625980,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70170061,"text":"70170061 - 2004 - Ground-water evapotranspiration estimates near wet meadows using well hydrographs","interactions":[],"lastModifiedDate":"2016-04-04T12:02:17","indexId":"70170061","displayToPublicDate":"2004-06-01T13:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":18,"text":"Abstract or summary"},"title":"Ground-water evapotranspiration estimates near wet meadows using well hydrographs","docAbstract":"No abstract available.
","conferenceTitle":"Minnesota Water 2004--Policy and planning to ensure Minnesota's water supplies","conferenceDate":"March 23-24, 2004","conferenceLocation":"Minneapolis, MN","language":"English","usgsCitation":"Cowdery, T., 2004, Ground-water evapotranspiration estimates near wet meadows using well hydrographs, Minnesota Water 2004--Policy and planning to ensure Minnesota's water supplies, Minneapolis, MN, March 23-24, 2004.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":319766,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57039097e4b0328dcb81c60c","contributors":{"authors":[{"text":"Cowdery, T.K.","contributorId":92658,"corporation":false,"usgs":true,"family":"Cowdery","given":"T.K.","affiliations":[],"preferred":false,"id":625972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70170063,"text":"70170063 - 2004 - Unsaturated zone tracer test at a crude oil spill site","interactions":[],"lastModifiedDate":"2016-04-04T12:06:01","indexId":"70170063","displayToPublicDate":"2004-06-01T13:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":18,"text":"Abstract or summary"},"title":"Unsaturated zone tracer test at a crude oil spill site","docAbstract":"No abstract available.
","conferenceTitle":"Minnesota Water 2004--Policy and planning to ensure Minnesota's water supplies","conferenceDate":"March 23-24, 2004","conferenceLocation":"Minneapolis, MN","language":"English","usgsCitation":"Delin, G., and Herkelrath, W., 2004, Unsaturated zone tracer test at a crude oil spill site, Minnesota Water 2004--Policy and planning to ensure Minnesota's water supplies, Minneapolis, MN, March 23-24, 2004.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":319767,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57039130e4b0328dcb81c731","contributors":{"authors":[{"text":"Delin, G. N.","contributorId":12834,"corporation":false,"usgs":true,"family":"Delin","given":"G. N.","affiliations":[],"preferred":false,"id":625973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herkelrath, W.N.","contributorId":77981,"corporation":false,"usgs":true,"family":"Herkelrath","given":"W.N.","affiliations":[],"preferred":false,"id":625974,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70239861,"text":"70239861 - 2004 - Linking metal bioaccumulation of aquatic insects to their distribution patterns in a mining-impacted river","interactions":[],"lastModifiedDate":"2023-01-23T18:32:10.367122","indexId":"70239861","displayToPublicDate":"2004-06-01T12:14:47","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1571,"text":"Environmental Toxicology and Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Linking metal bioaccumulation of aquatic insects to their distribution patterns in a mining-impacted river","docAbstract":"Although the differential responses of stream taxa to metal exposure have been exploited for bioassessment and monitoring, the mechanisms affecting these responses are not well understood. In this study, the subcellular partitioning of metals in operationally defined metal-sensitive and detoxified fractions were analyzed in five insect taxa. Samples were collected in two separate years along an extensive metal contamination gradient in the Clark Fork River (MT, USA) to determine if interspecific differences in the metal concentrations of metal-sensitive fractions and detoxified fractions were linked to the differences in distributions of taxa relative to the gradient. Most of the Cd, Cu, and Zn body burdens were internalized and potentially biologically active in all taxa, although all taxa appeared to detoxify metals (e.g., metal bound to cytosolic metal-binding proteins). Metal concentrations associated with metal-sensitive fractions were highest in the mayflies Epeorus albertae and Serratella tibialis, which were rare or absent from the most contaminated sites but occurred at less contaminated sites. Relatively low concentrations of Cu were common to the tolerant taxa Hydropsyche spp. and Baetis spp., which were widely distributed and dominant in the most contaminated sections of the river. This suggested that distributions of taxa along the contamination gradient were more closely related to the bioaccumulation of Cu than of other metals. Metal bioaccumulation did not appear to explain the spatial distribution of the caddisfly Arctopsyche grandis, considered to be a bioindicator of metal effects in the river. Thus, in this system the presence/absence of most of these taxa from sites where metal exposure was elevated could be differentiated on the basis of differences in metal bioaccumulation.
","language":"English","publisher":"Society of Environmental Toxicology and Chemistry","doi":"10.1897/03-291","usgsCitation":"Cain, D.J., Luoma, S.N., and Wallace, W., 2004, Linking metal bioaccumulation of aquatic insects to their distribution patterns in a mining-impacted river: Environmental Toxicology and Chemistry, v. 23, no. 6, p. 1463-1473, https://doi.org/10.1897/03-291.","productDescription":"11 p.","startPage":"1463","endPage":"1473","costCenters":[],"links":[{"id":478036,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1897/03-291","text":"Publisher Index Page"},{"id":412222,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","city":"Anaconda, Butte","otherGeospatial":"Blackfoot River, Clark Fork, Rock Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -112.79158715513537,\n 45.78524179725878\n ],\n [\n -112.40157250669786,\n 45.64743865418836\n ],\n [\n -111.88521508482286,\n 45.72418829749364\n ],\n [\n -111.31941918638513,\n 45.96526146652312\n ],\n [\n -111.20955590513518,\n 46.045387054928625\n ],\n [\n -111.23152856138545,\n 46.2394946511632\n ],\n [\n -111.21504906919776,\n 46.44048927034987\n ],\n [\n -111.35237817076018,\n 46.54637685784397\n ],\n [\n -111.53365258482278,\n 46.68221513911473\n ],\n [\n -111.71492699888539,\n 46.73118412240726\n ],\n [\n -111.8797219207603,\n 46.89284201266702\n ],\n [\n -112.29720238951015,\n 47.05401407816328\n ],\n [\n -112.8080666473229,\n 47.10426076306271\n ],\n [\n -112.97835473326037,\n 47.11921471082056\n ],\n [\n -113.24751977232266,\n 47.2312354017738\n ],\n [\n -113.48372582701023,\n 47.46199618684685\n ],\n [\n -113.65950707701028,\n 47.7176249403291\n ],\n [\n -113.70345238951045,\n 47.90576572460023\n ],\n [\n -113.87374047544792,\n 48.09322512238063\n ],\n [\n -114.08248070982268,\n 48.261722078648745\n ],\n [\n -114.0934670379478,\n 48.14456542957663\n ],\n [\n -113.96712426451018,\n 47.909447946855465\n ],\n [\n -113.84627465513562,\n 47.44898603829617\n ],\n [\n -113.68697289732292,\n 47.25919342227073\n ],\n [\n -113.79683617857287,\n 46.93010244114254\n ],\n [\n -113.52217797544802,\n 46.715855622687684\n ],\n [\n -113.39034203794782,\n 46.61784540934639\n ],\n [\n -113.53865746763537,\n 46.51965747208172\n ],\n [\n -113.50569848326032,\n 46.29998223919168\n ],\n [\n -113.68697289732292,\n 46.23542698831048\n ],\n [\n -113.50569848326032,\n 46.1327417878056\n ],\n [\n -113.28597192076045,\n 46.193615429712025\n ],\n [\n -113.25850610044795,\n 46.39098964320587\n ],\n [\n -113.03877953794807,\n 46.512097191513675\n ],\n [\n -112.917929928573,\n 46.3947783305276\n ],\n [\n -112.95088891294806,\n 46.121320481217424\n ],\n [\n -113.08821801451049,\n 46.041305025927045\n ],\n [\n -112.76412133482289,\n 45.94207748513807\n ],\n [\n -112.79158715513537,\n 45.78524179725878\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"23","issue":"6","noUsgsAuthors":false,"publicationDate":"2004-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Cain, Daniel J. 0000-0002-3443-0493 djcain@usgs.gov","orcid":"https://orcid.org/0000-0002-3443-0493","contributorId":1784,"corporation":false,"usgs":true,"family":"Cain","given":"Daniel","email":"djcain@usgs.gov","middleInitial":"J.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":862190,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luoma, Samuel N. 0000-0001-5443-5091 snluoma@usgs.gov","orcid":"https://orcid.org/0000-0001-5443-5091","contributorId":2287,"corporation":false,"usgs":true,"family":"Luoma","given":"Samuel","email":"snluoma@usgs.gov","middleInitial":"N.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":862191,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wallace, W.G.","contributorId":55588,"corporation":false,"usgs":true,"family":"Wallace","given":"W.G.","email":"","affiliations":[],"preferred":false,"id":862192,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70239860,"text":"70239860 - 2004 - Interdisciplinary discussion of volcanic processes beneath the Long Valley Caldera-Mono Craters Area","interactions":[],"lastModifiedDate":"2023-01-23T18:10:15.595967","indexId":"70239860","displayToPublicDate":"2004-06-01T12:02:39","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":7458,"text":"Eos Science News","active":true,"publicationSubtype":{"id":10}},"title":"Interdisciplinary discussion of volcanic processes beneath the Long Valley Caldera-Mono Craters Area","docAbstract":"Volcanism in the Long Valley Caldera-Mono Craters (LVCMC) volcanic field in eastern California over the past 4 Ma is dominated by the 0.76 Ma caldera-forming eruption of 600 km3 of rhyolite to form the Bishop Tuff. Over the last 150 k.y., volcanism has concentrated along the Mono-Inyo chain, which extends 45 km north from Mammoth Mountain to Mono Lake (Figure 1, below). Recent eruptions along this chain have occurred from multiple vents 650±50 yr B.P. and from a vent in the middle of Mono Lake ∼300 yr B.P. An earthquake swarm in May 1980, including four M6 earthquakes accompanied by uplift of the resurgent dome in the center of the caldera, called attention to the restless nature of Long Valley caldera. Subsequent activity has included recurring swarms of earthquakes (M≤5.8), episodic uplift of the resurgent dome, diffuse outgassing of magmatic CO2, and mid-crustal (10- to 25- km deep), long period (LP) volcanic earthquakes.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/2004EO230005","usgsCitation":"Hill, D.P., and Segall, P., 2004, Interdisciplinary discussion of volcanic processes beneath the Long Valley Caldera-Mono Craters Area: Eos Science News, v. 85, no. 23, p. 228-230, https://doi.org/10.1029/2004EO230005.","productDescription":"3 p.","startPage":"228","endPage":"230","costCenters":[],"links":[{"id":478037,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1029/2004eo230005","text":"Publisher Index Page"},{"id":412221,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Long Valley, Mono Craters","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.23649758839697,\n 38.32502830627854\n ],\n [\n -119.30525387805034,\n 38.27322770865979\n ],\n [\n -119.36025890977305,\n 38.176001936454924\n ],\n [\n -119.39326192880674,\n 38.1392383908923\n ],\n [\n -119.30525387805034,\n 38.134912049426646\n ],\n [\n -119.23924783998297,\n 38.056994053386205\n ],\n [\n -119.17599205350191,\n 38.00500258290651\n ],\n [\n -119.12923777653756,\n 37.942130335658476\n ],\n [\n -119.15123978922657,\n 37.855321661186466\n ],\n [\n -119.09898500909021,\n 37.766236556452895\n ],\n [\n -119.0632317384702,\n 37.76188819257996\n ],\n [\n -119.0467302289535,\n 37.68575045091809\n ],\n [\n -118.98622469405848,\n 37.626962161637465\n ],\n [\n -118.8487121147517,\n 37.585564728113255\n ],\n [\n -118.74695280606466,\n 37.53542122654635\n ],\n [\n -118.6836970195836,\n 37.50488257532501\n ],\n [\n -118.67819651641148,\n 37.40445332163641\n ],\n [\n -118.63694274261945,\n 37.36730404405546\n ],\n [\n -118.61769098151643,\n 37.23166254409088\n ],\n [\n -118.50218041489869,\n 37.323575451103295\n ],\n [\n -118.44442513158965,\n 37.26669021811128\n ],\n [\n -118.24915726897419,\n 37.29951387167142\n ],\n [\n -118.20515324359584,\n 37.33450998669913\n ],\n [\n -118.20790349518217,\n 37.52887828209252\n ],\n [\n -118.28491053959388,\n 37.69880819318749\n ],\n [\n -118.36741808717792,\n 37.848806883868306\n ],\n [\n -119.1732418019156,\n 38.41865106846589\n ],\n [\n -119.23649758839697,\n 38.32502830627854\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"85","issue":"23","noUsgsAuthors":false,"publicationDate":"2011-06-03","publicationStatus":"PW","contributors":{"authors":[{"text":"Hill, David P. 0000-0002-1619-2006 dhill@usgs.gov","orcid":"https://orcid.org/0000-0002-1619-2006","contributorId":206752,"corporation":false,"usgs":true,"family":"Hill","given":"David","email":"dhill@usgs.gov","middleInitial":"P.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":862188,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Segall, Paul","contributorId":241093,"corporation":false,"usgs":false,"family":"Segall","given":"Paul","affiliations":[{"id":6986,"text":"Stanford University","active":true,"usgs":false}],"preferred":false,"id":862189,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70170144,"text":"70170144 - 2004 - A national fish-tissue mercury model--Implications for monitoring program design","interactions":[],"lastModifiedDate":"2016-04-08T10:46:43","indexId":"70170144","displayToPublicDate":"2004-06-01T11:45:00","publicationYear":"2004","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":18,"text":"Abstract or summary"},"title":"A national fish-tissue mercury model--Implications for monitoring program design","docAbstract":"No abstract available.
","conferenceTitle":"Minnesota Water 2004--Policy and planning to ensure Minnesota's water supplies","conferenceDate":"March 22-23, 2004","conferenceLocation":"Minneapolis, MN","language":"English","usgsCitation":"Wente, S.P., 2004, A national fish-tissue mercury model--Implications for monitoring program design, Minnesota Water 2004--Policy and planning to ensure Minnesota's water supplies, Minneapolis, MN, March 22-23, 2004, 22 p.","productDescription":"22 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":319906,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"572485afe4b0b13d391592d9","contributors":{"authors":[{"text":"Wente, Stephen P.","contributorId":75226,"corporation":false,"usgs":true,"family":"Wente","given":"Stephen","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":626274,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70200852,"text":"70200852 - 2004 - The emplacement of pahoehoe toes: Field observations and comparison to laboratory simulations","interactions":[],"lastModifiedDate":"2019-12-22T14:21:01","indexId":"70200852","displayToPublicDate":"2004-06-01T08:04:58","publicationYear":"2004","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1109,"text":"Bulletin of Volcanology","active":true,"publicationSubtype":{"id":10}},"title":"The emplacement of pahoehoe toes: Field observations and comparison to laboratory simulations","docAbstract":"We observed active pahoehoe lobes erupted on Kilauea during May-June 1996, and found a range of emplacement styles associated with variations in local effusion rate, flow velocity, and strain rate. These emplacement styles were documented and quantified for comparison with earlier laboratory experiments.
At the lowest effusion rates, velocities, and strain rates, smooth-surfaced lobes were emplaced via swelling, where new crust formed along an incandescent lip at the front of the lobe and the rest of the lobe was covered with a dark crust. At higher effusion rates, strain rates and velocities, lobes were emplaced through tearing or cracking. Tearing was characterized by ripping of the ductile crust near the initial breakout point, and most of the lobe surface was incandescent during its emplacement. This mechanism was observed to generate both smooth-surfaced lobes, and, when the lava encountered an obstacle, folded lobes. Cracking lobes were similar to those emplaced via tearing, but involved breaking of a thicker, brittle crust at the initial breakout of the lobe and therefore required somewhat higher flow rates than did tearing. Cracking lobes typically formed ropy folds in the center of the lobe, and smooth margins. At the highest effusion rates, strain rates, and flow velocities, the lava formed open channels with distinct levees.
The final lobe morphologies were compared to results from laboratory simulations, which were designed to infer effusion rate from final flow morphology, to quantitatively test the laboratory results on the scale of individual natural pahoehoe lobes. There is general agreement between results from laboratory simulations and natural lavas on the scale of individual pahoehoe lobes, but there are disparities between laboratory flows and lava flows on the scale of an entire pahoehoe lava flow field.
","language":"English","publisher":"Springer","doi":"10.1007/s00445-003-0319-5","issn":"1432-0819","usgsCitation":"Gregg, T., and Keszthelyi, L., 2004, The emplacement of pahoehoe toes: Field observations and comparison to laboratory simulations: Bulletin of Volcanology, v. 66, no. 5, p. 381-391, https://doi.org/10.1007/s00445-003-0319-5.","productDescription":"11 p.","startPage":"381","endPage":"391","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":359264,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea volcano","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -155.5938720703125,\n 18.895892559415024\n ],\n [\n -155.225830078125,\n 19.145168196205297\n ],\n [\n -154.8193359375,\n 19.342244996771804\n ],\n [\n -154.8797607421875,\n 19.48730751856426\n ],\n [\n -155.23681640625,\n 19.585668899245324\n ],\n [\n -155.4840087890625,\n 19.46141299683288\n ],\n [\n -155.74768066406247,\n 19.16592425362802\n ],\n [\n -155.5938720703125,\n 18.895892559415024\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"66","issue":"5","noUsgsAuthors":false,"publicationDate":"2004-04-23","publicationStatus":"PW","scienceBaseUri":"5be40826e4b0b3fc5cf7cc1e","contributors":{"authors":[{"text":"Gregg, Tracy K. P.","contributorId":57937,"corporation":false,"usgs":true,"family":"Gregg","given":"Tracy K. P.","affiliations":[],"preferred":false,"id":750873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keszthelyi, Laszlo P. 0000-0003-1879-4331 laz@usgs.gov","orcid":"https://orcid.org/0000-0003-1879-4331","contributorId":52802,"corporation":false,"usgs":true,"family":"Keszthelyi","given":"Laszlo P.","email":"laz@usgs.gov","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":750874,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":54101,"text":"cir1226 - 2004 - Water quality in the New England coastal basins, Maine, New Hampshire, Massachusetts, and Rhode Island, 1999-2001","interactions":[],"lastModifiedDate":"2022-08-03T19:31:09.397064","indexId":"cir1226","displayToPublicDate":"2004-06-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1226","title":"Water quality in the New England coastal basins, Maine, New Hampshire, Massachusetts, and Rhode Island, 1999-2001","docAbstract":"This report contains the major findings of a 1999-2001 assessment of water quality in the New England Coastal Basins. It is one of a series of reports by the National Water-Quality Assessment (NAWQA) Program that present major findings in 51 major river basins and aquifer systems across the Nation. In these reports, water quality is discussed in terms of local, State, and regional issues. Conditions in a particular basin or aquifer system are compared to conditions found elsewhere and to selected national benchmarks, such as those for drinking-water quality and the protection of aquatic organisms. This report is intended for individuals working with water-resource issues in Federal, State, or local agencies, universities, public interest groups, or in the private sector. The information will be useful in addressing a number of current issues, such as the effects of agricultural and urban land use on water quality, human health, drinking water, source-water protection, hypoxia and excessive growth of algae and plants, pesticide registration, and monitoring and sampling strategies. This report is also for individuals who wish to know more about the quality of streams and ground water in areas near where they live and how that water quality compares to the quality of water in other areas across the Nation. The water-quality conditions in the New England Coastal Basins summarized in this report are discussed in detail in other reports that can be accessed from http://nh.water.usgs.gov/CurrentProjects/nawqa/nawqaweb.htm. Detailed technical information, data and analyses, collection and analytical methodology, models, graphs, and maps that support the findings presented in this report in addition to reports in this series from other basins can be accessed from the national NAWQA Web site (http://water.usgs.gov/nawqa).
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This report is also for individuals who wish to know more about the quality of streams and ground water in areas near where they live, and how that water quality compares to the quality of water in other areas across the Nation.\r\n\r\n \r\n\r\nThe water-quality conditions in the Cook Inlet Basin summarized in this report are discussed in detail in other reports that can be accessed at http://ak.water.usgs.gov. Detailed technical information, data and analyses, collection and analytical methodology, models, graphs, and maps that support the findings presented in this report, in addition to reports in this series from other basins, can be accessed from the national NAWQA Web site (http://water.usgs.gov/nawqa).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir1240","usgsCitation":"Glass, R.L., Brabets, T.P., Frenzel, S.A., Whitman, M.S., and Ourso, R.T., 2004, Water quality in the Cook Inlet Basin Alaska, 1998-2001: U.S. Geological Survey Circular 1240, vi, 32 p., https://doi.org/10.3133/cir1240.","productDescription":"vi, 32 p.","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":5488,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/circ1240/","linkFileType":{"id":5,"text":"html"}},{"id":174890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":407982,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_68279.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Cook Inlet Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -155.390625,\n 58.56252272853734\n ],\n [\n -147.48046875,\n 58.56252272853734\n ],\n [\n -147.48046875,\n 62.61356210229029\n ],\n [\n -155.390625,\n 62.61356210229029\n ],\n [\n -155.390625,\n 58.56252272853734\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb6e5","contributors":{"authors":[{"text":"Glass, Roy L.","contributorId":86813,"corporation":false,"usgs":true,"family":"Glass","given":"Roy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":249040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brabets, Timothy P. tbrabets@usgs.gov","contributorId":2087,"corporation":false,"usgs":true,"family":"Brabets","given":"Timothy","email":"tbrabets@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":249037,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frenzel, Steven A. sfrenzel@usgs.gov","contributorId":688,"corporation":false,"usgs":true,"family":"Frenzel","given":"Steven","email":"sfrenzel@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":249036,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whitman, Matthew S.","contributorId":67961,"corporation":false,"usgs":false,"family":"Whitman","given":"Matthew","email":"","middleInitial":"S.","affiliations":[{"id":7217,"text":"Bureau of Land Management","active":true,"usgs":false}],"preferred":false,"id":249039,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Ourso, Robert T. 0000-0002-5952-8681 rtourso@usgs.gov","orcid":"https://orcid.org/0000-0002-5952-8681","contributorId":203207,"corporation":false,"usgs":true,"family":"Ourso","given":"Robert","email":"rtourso@usgs.gov","middleInitial":"T.","affiliations":[{"id":120,"text":"Alaska Science Center Water","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":249038,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":73663,"text":"cir1196K - 2004 - Tin recycling in the United States in 1998","interactions":[],"lastModifiedDate":"2012-02-02T00:13:58","indexId":"cir1196K","displayToPublicDate":"2004-06-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1196","chapter":"K","title":"Tin recycling in the United States in 1998","language":"ENGLISH","doi":"10.3133/cir1196K","usgsCitation":"Carlin, J.F., 2004, Tin recycling in the United States in 1998: U.S. Geological Survey Circular 1196, v, K1-K8, https://doi.org/10.3133/cir1196K.","productDescription":"v, K1-K8","costCenters":[],"links":[{"id":191397,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7430,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/circ/2004/1196am/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b485","contributors":{"authors":[{"text":"Carlin, James F. Jr. jcarlin@usgs.gov","contributorId":2685,"corporation":false,"usgs":true,"family":"Carlin","given":"James","suffix":"Jr.","email":"jcarlin@usgs.gov","middleInitial":"F.","affiliations":[{"id":432,"text":"National Minerals Information Center","active":true,"usgs":true}],"preferred":false,"id":286444,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":54134,"text":"fs20043026 - 2004 - Water-level changes in the High Plains aquifer, predevelopment to 2002, 1980 to 2002, and 2001 to 2002","interactions":[],"lastModifiedDate":"2012-02-02T00:11:39","indexId":"fs20043026","displayToPublicDate":"2004-06-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-3026","title":"Water-level changes in the High Plains aquifer, predevelopment to 2002, 1980 to 2002, and 2001 to 2002","language":"ENGLISH","doi":"10.3133/fs20043026","usgsCitation":"McGuire, V.L., 2004, Water-level changes in the High Plains aquifer, predevelopment to 2002, 1980 to 2002, and 2001 to 2002: U.S. Geological Survey Fact Sheet 2004-3026, 6 p., https://doi.org/10.3133/fs20043026.","productDescription":"6 p.","costCenters":[],"links":[{"id":5581,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs2004-3026/","linkFileType":{"id":5,"text":"html"}},{"id":120602,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2004_3026.bmp"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7784","contributors":{"authors":[{"text":"McGuire, Virginia L. 0000-0002-3962-4158 vlmcguir@usgs.gov","orcid":"https://orcid.org/0000-0002-3962-4158","contributorId":404,"corporation":false,"usgs":true,"family":"McGuire","given":"Virginia","email":"vlmcguir@usgs.gov","middleInitial":"L.","affiliations":[{"id":464,"text":"Nebraska Water Science Center","active":true,"usgs":true}],"preferred":true,"id":249297,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":54133,"text":"sir20045014 - 2004 - Simulated interaction between freshwater and saltwater and effects of ground-water pumping and sea-level change, lower Cape Cod aquifer system, Massachusetts","interactions":[],"lastModifiedDate":"2018-05-17T14:16:48","indexId":"sir20045014","displayToPublicDate":"2004-06-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5014","title":"Simulated interaction between freshwater and saltwater and effects of ground-water pumping and sea-level change, lower Cape Cod aquifer system, Massachusetts","docAbstract":"The U.S. Geological Survey, in cooperation with the National Park Service, Massachusetts Executive Office of Environmental Affairs, Cape Cod Commission, and the Towns of Eastham, Provincetown, Truro, and Wellfleet, began an investigation in 2000 to improve the understanding of the hydrogeology of the four freshwater lenses of the Lower Cape Cod aquifer system and to assess the effects of changing ground-water pumping, recharge conditions, and sea level on ground-water flow in Lower Cape Cod, Massachusetts.\r\n\r\nA numerical flow model was developed with the computer code SEAWAT to assist in the analysis of freshwater and saltwater flow. Model simulations were used to determine water budgets, flow directions, and the position and movement of the freshwater/saltwater interface.\r\n\r\nModel-calculated water budgets indicate that approximately 68 million gallons per day of freshwater recharge the Lower Cape Cod aquifer system with about 68 percent of this water moving through the aquifer and discharging directly to the coast, 31 percent flowing through the aquifer, discharging to streams, and then reaching the coast as surface-water discharge, and the remaining 1 percent discharging to public-supply wells. The distribution of streamflow varies greatly among flow lenses and streams; in addition, the subsurface geology greatly affects the position and movement of the underlying freshwater/saltwater interface. \r\n\r\nThe depth to the freshwater/saltwater interface varies throughout the study area and is directly proportional to the height of the water table above sea level. Simulated increases in sea level appear to increase water levels and streamflows throughout the Lower Cape Cod aquifer system, and yet decrease the depth to the freshwater/saltwater interface. The resulting change in water levels and in the depth to the freshwater/saltwater interface from sea-level rise varies throughout the aquifer system and is controlled largely by non-tidal freshwater streams.\r\n\r\nPumping from large-capacity municipal-supply wells increases the potential for effects on surface-water bodies, which are affected by pumping and wastewater-disposal locations and rates. Pumping wells that are upgradient of surface-water bodies potentially capture water that would otherwise discharge to these surface-water bodies, thereby reducing streamflow and pond levels. Kettle-hole ponds, such as Duck Pond in Wellfleet, that are near the top of a freshwater flow lens, appear to be more susceptible to changing pumping and recharge conditions than kettle-hole ponds closer to the coast or near discharge boundaries, such as the Herring River.","language":"ENGLISH","doi":"10.3133/sir20045014","usgsCitation":"Masterson, J., 2004, Simulated interaction between freshwater and saltwater and effects of ground-water pumping and sea-level change, lower Cape Cod aquifer system, Massachusetts: U.S. Geological Survey Scientific Investigations Report 2004-5014, 78 p., https://doi.org/10.3133/sir20045014.","productDescription":"78 p.","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":124741,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir_2004_5014.jpg"},{"id":5580,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5014/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f31c8","contributors":{"authors":[{"text":"Masterson, John P. 0000-0003-3202-4413 jpmaster@usgs.gov","orcid":"https://orcid.org/0000-0003-3202-4413","contributorId":1865,"corporation":false,"usgs":true,"family":"Masterson","given":"John P.","email":"jpmaster@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":249296,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":54148,"text":"b2209H - 2004 - Stratiform barite deposits in the Roberts Mountains allochthon, Nevada: A review of potential analogs in modern sea-floor environments","interactions":[{"subject":{"id":54148,"text":"b2209H - 2004 - Stratiform barite deposits in the Roberts Mountains allochthon, Nevada: A review of potential analogs in modern sea-floor environments","indexId":"b2209H","publicationYear":"2004","noYear":false,"chapter":"H","title":"Stratiform barite deposits in the Roberts Mountains allochthon, Nevada: A review of potential analogs in modern sea-floor environments"},"predicate":"IS_PART_OF","object":{"id":44273,"text":"b2209 - 2003 - Contributions to Industrial-Minerals Research","indexId":"b2209","publicationYear":"2003","noYear":false,"title":"Contributions to Industrial-Minerals Research"},"id":1}],"isPartOf":{"id":44273,"text":"b2209 - 2003 - Contributions to Industrial-Minerals Research","indexId":"b2209","publicationYear":"2003","noYear":false,"title":"Contributions to Industrial-Minerals Research"},"lastModifiedDate":"2022-06-13T19:55:27.103051","indexId":"b2209H","displayToPublicDate":"2004-06-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2209","chapter":"H","title":"Stratiform barite deposits in the Roberts Mountains allochthon, Nevada: A review of potential analogs in modern sea-floor environments","docAbstract":"The United States is a net importer of barite, a critical mineral for the oil and gas industry; more than 80 percent of current domestic consumption of barite is imported from China. Nearly all of the domestic production of barite comes from stratiform deposits in Nevada. The 'modern analogs' approach adopted in this review can contribute to improving deposit models and the long-term resource picture in the United States.\r\n\r\nMassive barite deposits in Nevada are interlayered with deep-water siliceous sedimentary strata of Paleozoic age within the Roberts Mountains Allochthon. Although the barite deposits formed along the long-lived, tectonically active margin of western North America before the Antler orogeny, uncertainty still exists regarding key aspects of their genesis, especially with respect to tectonic setting and depositional processes. Proposed tectonic settings include a continental slope adjacent to an ocean basin, and a rifted basin formed on continental crust. A margin dominated by other stress configurations\r\nand strike-slip faulting may also have been present during the Paleozoic. Hypotheses for the genesis of sediment-hosted, stratiform barite deposits in Nevada can be grouped into two categories: (1) a synsedimentary hydrothermal model and (2) an ocean-circulation/productivity-zone model. Both models include a stage involving bacterial reduction of seawater sulfate.\r\n\r\nDisseminated, diagenetic, and hydrothermal barite deposits are widespread features of the modern ocean. In the Pacific Ocean, disseminated barite deposits (max 9 weight percent BaSO4) are forming below high-productivity zones (for example, in equatorial belts) and on the flanks of ocean ridges (as fallout of 'black smoker' particles). Massive barite deposits of diagenetic (in the subsea floor and at cold seeps) and hydrothermal origins are present in several sediment-covered tectonic settings, including ocean ridges (Escanaba Trough and Guaymas Basin), oceanic transform faults (Blanco Fracture Zone), marginal basins (Sea of Okhotsk), convergent margins (Peru, Oregon, Alaska), and transform margins (California Continental Borderland). Both hydrothermal and diagenetic barite deposits may be present in some environments (for example, the California California Borderland).\r\n\r\nOn the basis of a consideration of tectonic settings and a comparison of deposit attributes (associated rock types, size, structure), mineralogy (BaSO4 content, SiO2 content), and geochemistry (S- and Sr-isotopic ratios) for modern and ancient massive barite deposits, cold seeps along transform margins (or, possibly, marginal basins) represent the most promising present-day metallogenetic analogs for stratiform barite. Hydrothermal systems can also produce high-grade barite, but the ubiquity of associated sulfide mineralization on the modern sea floor (and the paucity of sulfides in Nevada deposits) is problematic. On the basis of data from modern barite deposits, the presence of vent-specific faunas (tubeworms) and the variation in d34S values for barite (related to bacterial reduction of seawater sulfate) may not permit discrimination between a diagenetic or hydrothermal origin for ancient barite deposits.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to Industrial-Minerals Research (Bulletin 2209)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2209H","usgsCitation":"Koski, R.A., and Hein, J.R., 2004, Stratiform barite deposits in the Roberts Mountains allochthon, Nevada: A review of potential analogs in modern sea-floor environments (Version 1.0): U.S. Geological Survey Bulletin 2209, iii, 17 p., https://doi.org/10.3133/b2209H.","productDescription":"iii, 17 p.","onlineOnly":"Y","costCenters":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true},{"id":658,"text":"Western Mineral Resources","active":false,"usgs":true}],"links":[{"id":184951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5594,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/b2209-h/","linkFileType":{"id":5,"text":"html"}},{"id":402121,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_66121.htm"}],"country":"United States","state":"Nevada","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.30078125,\n 36.86204269508728\n ],\n [\n -114.169921875,\n 36.86204269508728\n ],\n [\n -114.169921875,\n 41.83682786072714\n ],\n [\n -118.30078125,\n 41.83682786072714\n ],\n [\n -118.30078125,\n 36.86204269508728\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e565f","contributors":{"authors":[{"text":"Koski, Randolph A. rkoski@usgs.gov","contributorId":2949,"corporation":false,"usgs":true,"family":"Koski","given":"Randolph","email":"rkoski@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":249334,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hein, James R. 0000-0002-5321-899X jhein@usgs.gov","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":2828,"corporation":false,"usgs":true,"family":"Hein","given":"James","email":"jhein@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":249333,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":54158,"text":"wri034336 - 2004 - Results of a Two-Dimensional Hydrodynamic and Sediment-Transport Model to Predict the Effects of the Phased Construction and Operation of the Olmsted Locks and Dam on the Ohio River near Olmsted, Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:12:11","indexId":"wri034336","displayToPublicDate":"2004-06-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2003-4336","title":"Results of a Two-Dimensional Hydrodynamic and Sediment-Transport Model to Predict the Effects of the Phased Construction and Operation of the Olmsted Locks and Dam on the Ohio River near Olmsted, Illinois","docAbstract":"The Olmsted two-dimensional hydrodynamic and sediment-transport model was developed in cooperation with the U.S. Army Corps of Engineers, Louisville District. The model was used to estimate the effects that the phased-construction sequence and operation of the Olmsted Locks and Dam had on sediment-transport patterns in the 11.9-mile study reach (Ohio River miles 962.6 to 974.5), particularly over an area of endangered orange-footed pearly mussel (Plethobasus cooperianus) beds beginning approximately 2 miles downstream of the dam construction. A Resource Management Associates?2 (RMA-2) two-dimensional hydrodynamic model for the reach was calibrated to a middle-flow hydraulic survey (350,000 cubic feet per second) and verified with data collected during low- and high-flow hydraulic surveys (72,500 and 770,000 cubic feet per second, respectively). The calibration and validation process included matching water-surface elevations at the construction site and velocity profiles at 15 cross sections throughout the study reach.\r\n\r\nThe sediment-transport aspect of the project was simulated with the Waterways Experiment Station's Sed2D model for a 6-year planned-construction period (construction-phase modeling) and a subsequent 3-year operational period (operational-phase modeling). The sediment-transport results from the construction and operational models both were compared to results of concurrent baseline simulations to determine the changes in erosional and depositional patterns induced by the dam construction and operation throughout the study reach and more importantly over the area of the endangered mussel beds. \r\n\r\nSimulation of the phased-in-the-wet Olmsted Locks and Dam construction and subsequent operation period resulted in a maximum additional deposition of approximately 2 feet over a localized region of the mussel beds when compared to the bed change simulated with baseline conditions (river conditions that included only the completed locks section). Most areas on the mussel beds experienced less than 0.5 feet of cumulative bed change between the baseline and construction phases during the nine annual hydrographs. The bed change over the 9 year Olmsted Locks and Dam simulation reveals a continuous downstream progression and deepening of the main channel and deposition along the right bank with limited lateral migration toward the more densely populated mussel-bed areas. The sensitivity of the mussels to sediment deposition is difficult to quantify; therefore, the effect of simulated deposition on the welfare of the mussels is uncertain. The model also will provide the U.S. Army Corps of Engineers a tool to predict the locations of high deposition in navigable sections, which can save engineers time and resources when monitoring the need for dredging operations.","language":"ENGLISH","doi":"10.3133/wri034336","usgsCitation":"Wagner, C., 2004, Results of a Two-Dimensional Hydrodynamic and Sediment-Transport Model to Predict the Effects of the Phased Construction and Operation of the Olmsted Locks and Dam on the Ohio River near Olmsted, Illinois (Online only): U.S. Geological Survey Water-Resources Investigations Report 2003-4336, 68 p., https://doi.org/10.3133/wri034336.","productDescription":"68 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":5604,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri034336/","linkFileType":{"id":5,"text":"html"}},{"id":184138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625495","contributors":{"authors":[{"text":"Wagner, Chad R. 0000-0002-9602-7413 cwagner@usgs.gov","orcid":"https://orcid.org/0000-0002-9602-7413","contributorId":1530,"corporation":false,"usgs":true,"family":"Wagner","given":"Chad R.","email":"cwagner@usgs.gov","affiliations":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true},{"id":38131,"text":"WMA - Office of Planning and Programming","active":true,"usgs":true}],"preferred":false,"id":249353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":53852,"text":"sir20045026 - 2004 - Estimating Monthly, Annual, and Low 7-Day, 10-Year Streamflows for Ungaged Rivers in Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:11:43","indexId":"sir20045026","displayToPublicDate":"2004-06-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2004-5026","title":"Estimating Monthly, Annual, and Low 7-Day, 10-Year Streamflows for Ungaged Rivers in Maine","docAbstract":"Regression equations to estimate monthly, annual, and low 7-day, 10-year (7Q10) streamflows were derived for rivers in Maine. The derived regression equations for estimating mean monthly, mean annual, median monthly, median annual, and low 7Q10 streamflows for ungaged rivers in Maine presented in this report supersede those derived in previous studies. \r\n\r\nTwenty-six U.S. Geological Survey streamflow-gaging stations on unregulated, rural rivers in Maine with 10 years or more of recorded streamflow were used to develop the regression equations. Ordinary least squares (OLS) regression techniques were used to select the explanatory variables (basin and climatic characteristics) that would appear in the final regression equations. OLS regression of all possible subsets was done with 62 explanatory variables for each of 27 response variables. Five explanatory variables were chosen for the final regression equations: drainage basin area, areal fraction of the drainage basin underlain by sand and gravel aquifers, distance from the coast to the drainage basin centroid, mean drainage basin annual precipitation, and mean drainage basin winter precipitation (the sum of mean monthly precipitation for December, January, and February). Generalized least-squares regression techniques were used to derive the final coefficients and measures of uncertainty for the regression equations.\r\n\r\nThe forms of many of the derived regression equations indicate some physical, mechanistic processes. Drainage basin area is the most statistically important explanatory variable and appears in all derived regression equations. Monthly streamflows are related inversely to the distance from the coast to the drainage basin centroid during December, January, February, and March; that is, the closer a river basin is to the coast, the higher monthly streamflows are per unit drainage basin area during the winter. The relation reverses in May when higher streamflows are attributed to basins farther from the coast. These relations are consistent with colder, inland drainage basins storing more water in snowpack during the winter and releasing it in the spring. The monthly streamflows (and low 7Q10) during July, August, September, and October are related positively to areal fraction of the drainage basin underlain by sand and gravel aquifers. In general, sand and gravel aquifers underlying Maine river basins have excellent water-yielding characteristics and can provide water to streams during low-flow conditions in the summer and early fall.","language":"ENGLISH","doi":"10.3133/sir20045026","usgsCitation":"Dudley, R.W., 2004, Estimating Monthly, Annual, and Low 7-Day, 10-Year Streamflows for Ungaged Rivers in Maine: U.S. Geological Survey Scientific Investigations Report 2004-5026, 30 p., https://doi.org/10.3133/sir20045026.","productDescription":"30 p.","costCenters":[],"links":[{"id":4686,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5026/","linkFileType":{"id":5,"text":"html"}},{"id":177665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc9d4","contributors":{"authors":[{"text":"Dudley, Robert W. 0000-0002-0934-0568 rwdudley@usgs.gov","orcid":"https://orcid.org/0000-0002-0934-0568","contributorId":2223,"corporation":false,"usgs":true,"family":"Dudley","given":"Robert","email":"rwdudley@usgs.gov","middleInitial":"W.","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true},{"id":371,"text":"Maine Water Science Center","active":true,"usgs":true}],"preferred":true,"id":248497,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":54033,"text":"cir1230 - 2004 - Water quality in the upper Illinois River basin: Illinois, Indiana, and Wisconsin, 1999-2001","interactions":[],"lastModifiedDate":"2022-09-06T21:55:19.051975","indexId":"cir1230","displayToPublicDate":"2004-06-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1230","title":"Water quality in the upper Illinois River basin: Illinois, Indiana, and Wisconsin, 1999-2001","docAbstract":"This report contains the major findings of a 1999?2001 assessment of water quality in the upper Illinois River Basin. It is one of a series of reports by the National Water-Quality Assessment (NAWQA) Program that present major findings in 51 major river basins and aquifer systems across the Nation.\r\n\r\n \r\n\r\nIn these reports, water quality is discussed in terms of local, State, and regional issues. Conditions in a particular basin or aquifer system are compared to conditions found elsewhere and to selected national benchmarks, such as those for drinking-water quality and the protection of aquatic organisms.\r\n\r\n \r\n\r\nThis report is intended for individuals working with water-resource issues in Federal, State, or local agencies, universities, public-interest groups, or in the private sector. The information will be useful in addressing a number of current issues, such as the effects of agricultural and urban land use on water quality, human health, drinking water, source-water protection, hypoxia and excessive growth of algae and plants, pesticide registration, and monitoring and sampling strategies. This report also is for individuals who wish to know more about the quality of streams and ground water in areas near where they live, and how that water quality compares to the quality of water in other areas across the Nation.\r\n\r\n \r\n\r\nThe water-quality conditions in the upper Illinois River Basin summarized in this report are discussed in detail in other reports that can be accessed from (http://il.water.usgs.gov/nawqa/uirb). Detailed technical information, data and analyses, collection and analytical methodology, models, graphs, and maps that support the findings presented in this report in addition to reports in this series from other basins can be accessed from the national NAWQA Web site at\r\n(http://water.usgs.gov/nawqa).","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir1230","usgsCitation":"Groschen, G.E., Arnold, T., Harris, M.A., Dupre, D.H., Fitzpatrick, F.A., Scudder, B.C., Morrow, W.S., Terrio, P.J., Warner, K., and Murphy, E., 2004, Water quality in the upper Illinois River basin: Illinois, Indiana, and Wisconsin, 1999-2001: U.S. Geological Survey Circular 1230, vi, 32 p., https://doi.org/10.3133/cir1230.","productDescription":"vi, 32 p.","costCenters":[],"links":[{"id":174496,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":5475,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/circ1230","linkFileType":{"id":5,"text":"html"}},{"id":406281,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_68274.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Illinois, Indiana, and Wisconsin","otherGeospatial":"upper Illinois River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89,\n 40.4222\n ],\n [\n -86,\n 40.4222\n ],\n [\n -86,\n 43.1667\n ],\n [\n -89,\n 43.1667\n ],\n [\n -89,\n 40.4222\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd3c9","contributors":{"authors":[{"text":"Groschen, George 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maharris@usgs.gov","contributorId":1382,"corporation":false,"usgs":true,"family":"Harris","given":"Mitchell","email":"maharris@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":248978,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dupre, David H. dhdupre@usgs.gov","contributorId":2782,"corporation":false,"usgs":true,"family":"Dupre","given":"David","email":"dhdupre@usgs.gov","middleInitial":"H.","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":248981,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fitzpatrick, Faith A. fafitzpa@usgs.gov","contributorId":1182,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Faith","email":"fafitzpa@usgs.gov","middleInitial":"A.","affiliations":[{"id":476,"text":"North Carolina Water Science 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pjterrio@usgs.gov","orcid":"https://orcid.org/0000-0002-1515-9570","contributorId":3313,"corporation":false,"usgs":true,"family":"Terrio","given":"Paul","email":"pjterrio@usgs.gov","middleInitial":"J.","affiliations":[{"id":36532,"text":"Central Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":248982,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Warner, Kelly L. klwarner@usgs.gov","contributorId":655,"corporation":false,"usgs":true,"family":"Warner","given":"Kelly L.","email":"klwarner@usgs.gov","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":248976,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Murphy, Elizabeth A.","contributorId":69660,"corporation":false,"usgs":true,"family":"Murphy","given":"Elizabeth A.","affiliations":[],"preferred":false,"id":248983,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":54132,"text":"cir1232 - 2004 - Water quality in the Acadian-Pontchartrain drainages: Louisiana and Mississippi, 1999–2001","interactions":[],"lastModifiedDate":"2022-07-15T20:36:44.943796","indexId":"cir1232","displayToPublicDate":"2004-06-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1232","title":"Water quality in the Acadian-Pontchartrain drainages: Louisiana and Mississippi, 1999–2001","docAbstract":"This report contains the major findings of a 1999-2001 assessment of water quality in the Acadian-Pontchartrain Drainages Study Unit. It is one of a series of reports by the National Water-Quality Assessment (NAWQA) Program that present major findings in 51 major river basins and aquifer systems across the Nation. In these reports, water quality is discussed in terms of local, State, and regional issues. Conditions in a particular basin or aquifer system are compared to conditions found elsewhere and to selected national benchmarks, such as those for drinking-water quality and the protection of aquatic organisms. This report is intended for individuals working with water-resource issues in Federal, State, or local agencies, universities, public interest groups, or in the private sector. The information will be useful in addressing a number of current issues, such as the effects of agricultural and urban land use on water quality, human health, drinking water, source-water protection, hypoxia and excessive growth of algae and plants, pesticide registration, and monitoring and sampling strategies. This report also is for individuals who wish to know more about the quality of streams and ground water in areas near where they live, and how that water quality compares to other areas across the Nation. The water-quality conditions in the Acadian-Pontchartrain Drainages Study Unit summarized in this report are discussed in detail in other reports that can be accessed from (http://la.water.usgs.gov/nawqa/default.htm). Detailed technical information, data and analyses, collection and analytical methodology, models, graphs, and maps that support the findings presented in this report in addition to other reports in this series from other basins can be accessed from the national NAWQA Web site (http://water.usgs.gov/nawqa).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir1232","usgsCitation":"Demcheck, D.K., Tollett, R.W., Mize, S.V., Skrobialowski, S.C., Fendick, R., Swarzenski, C.M., and Porter, S., 2004, Water quality in the Acadian-Pontchartrain drainages: Louisiana and Mississippi, 1999–2001: U.S. Geological Survey Circular 1232, vi, 41 p., https://doi.org/10.3133/cir1232.","productDescription":"vi, 41 p.","costCenters":[],"links":[{"id":124376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_1232.jpg"},{"id":403868,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70813.htm","linkFileType":{"id":5,"text":"html"}},{"id":5579,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/circ1232","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Louisiana, Mississippi","otherGeospatial":"Acadian-Ponchartrain drainages","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.5833,\n 29\n ],\n [\n -88.8092,\n 29\n ],\n [\n -88.8092,\n 31.5\n ],\n [\n -93.5833,\n 31.5\n ],\n [\n -93.5833,\n 29\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697c11","contributors":{"authors":[{"text":"Demcheck, Dennis K. 0000-0003-2981-078X ddemchec@usgs.gov","orcid":"https://orcid.org/0000-0003-2981-078X","contributorId":3273,"corporation":false,"usgs":true,"family":"Demcheck","given":"Dennis","email":"ddemchec@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":249294,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tollett, Roland W. 0000-0002-4726-5845 rtollett@usgs.gov","orcid":"https://orcid.org/0000-0002-4726-5845","contributorId":1896,"corporation":false,"usgs":true,"family":"Tollett","given":"Roland","email":"rtollett@usgs.gov","middleInitial":"W.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"preferred":true,"id":249292,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mize, Scott V. 0000-0001-6751-5568 svmize@usgs.gov","orcid":"https://orcid.org/0000-0001-6751-5568","contributorId":2997,"corporation":false,"usgs":true,"family":"Mize","given":"Scott","email":"svmize@usgs.gov","middleInitial":"V.","affiliations":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":249293,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Skrobialowski, Stanley C. 0000-0001-8627-0279 sski@usgs.gov","orcid":"https://orcid.org/0000-0001-8627-0279","contributorId":1402,"corporation":false,"usgs":true,"family":"Skrobialowski","given":"Stanley","email":"sski@usgs.gov","middleInitial":"C.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":249291,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fendick, Robert B. Jr. rfendick@usgs.gov","contributorId":1313,"corporation":false,"usgs":true,"family":"Fendick","given":"Robert B.","suffix":"Jr.","email":"rfendick@usgs.gov","affiliations":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"preferred":false,"id":249290,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Swarzenski, Christopher M. 0000-0001-9843-1471 cswarzen@usgs.gov","orcid":"https://orcid.org/0000-0001-9843-1471","contributorId":656,"corporation":false,"usgs":true,"family":"Swarzenski","given":"Christopher","email":"cswarzen@usgs.gov","middleInitial":"M.","affiliations":[{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true},{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":249289,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Porter, Stephen","contributorId":107767,"corporation":false,"usgs":true,"family":"Porter","given":"Stephen","affiliations":[],"preferred":false,"id":249295,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":54047,"text":"cir1236 - 2004 - Water Quality in the Great Salt Lake Basins, Utah, Idaho, and Wyoming, 1998-2001","interactions":[],"lastModifiedDate":"2012-02-02T00:11:55","indexId":"cir1236","displayToPublicDate":"2004-06-01T00:00:00","publicationYear":"2004","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1236","title":"Water Quality in the Great Salt Lake Basins, Utah, Idaho, and Wyoming, 1998-2001","docAbstract":"This report contains the major findings of a 1998-2001 assessment of water quality in the Great Salt Lake Basins. It is one of a series of reports by the National Water-Quality Assessment (NAWQA) Program that present major findings in 51 major river basins and aquifer systems across the Nation.\r\n\r\n \r\n\r\nIn these reports, water quality is discussed in terms of local, State, and regional issues. Conditions in a particular basin or aquifer system are compared to conditions found elsewhere and to selected national benchmarks, such as those for drinking-water quality and the protection of aquatic organisms.\r\n\r\n \r\n\r\nThis report is intended for individuals working with water-resource issues in Federal, State, or local agencies, universities, public interest groups, or in the private sector. The information will be useful in addressing a number of current issues, such as the effects of agricultural and urban land use on water quality, human health, drinking water, source-water protection, hypoxia and excessive growth of algae and plants, pesticide registration, and monitoring and sampling strategies. This report is also for individuals who wish to know more about the quality of streams and ground water in areas near where they live, and how that water quality compares to water quality in other areas across the Nation.\r\n\r\n \r\n\r\nThe water-quality conditions in the Great Salt Lake Basins summarized in this report are discussed in detail in other reports that can be accessed at http://ut.water.usgs.gov. Detailed technical information, data and analyses, collection and analytical methodology, models, graphs, and maps that support the findings presented in this report in addition to reports in this series from other basins can be accessed at the national NAWQA Web site http://water.usgs.gov/nawqa.","language":"ENGLISH","doi":"10.3133/cir1236","usgsCitation":"Waddell, K.M., Gerner, S.J., Thiros, S.A., Giddings, E.M., Baskin, R.L., Cederberg, J.R., and Albano, C., 2004, Water Quality in the Great Salt Lake Basins, Utah, Idaho, and Wyoming, 1998-2001: U.S. Geological Survey Circular 1236, 46 p., https://doi.org/10.3133/cir1236.","productDescription":"46 p.","costCenters":[],"links":[{"id":5489,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/circ1236/","linkFileType":{"id":5,"text":"html"}},{"id":125144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/cir_1236.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd3a0","contributors":{"authors":[{"text":"Waddell, Kidd M.","contributorId":20720,"corporation":false,"usgs":true,"family":"Waddell","given":"Kidd","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":249046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gerner, Steven J. 0000-0002-5701-1304 sjgerner@usgs.gov","orcid":"https://orcid.org/0000-0002-5701-1304","contributorId":972,"corporation":false,"usgs":true,"family":"Gerner","given":"Steven","email":"sjgerner@usgs.gov","middleInitial":"J.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":249044,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thiros, Susan A. 0000-0002-8544-553X sthiros@usgs.gov","orcid":"https://orcid.org/0000-0002-8544-553X","contributorId":965,"corporation":false,"usgs":true,"family":"Thiros","given":"Susan","email":"sthiros@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":249043,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Giddings, Elise M.","contributorId":79164,"corporation":false,"usgs":true,"family":"Giddings","given":"Elise","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":249047,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Baskin, Robert L. 0000-0002-2175-8502 rbaskin@usgs.gov","orcid":"https://orcid.org/0000-0002-2175-8502","contributorId":360,"corporation":false,"usgs":true,"family":"Baskin","given":"Robert","email":"rbaskin@usgs.gov","middleInitial":"L.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":249041,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cederberg, Jay R. 0000-0001-6649-7353 cederber@usgs.gov","orcid":"https://orcid.org/0000-0001-6649-7353","contributorId":964,"corporation":false,"usgs":true,"family":"Cederberg","given":"Jay","email":"cederber@usgs.gov","middleInitial":"R.","affiliations":[{"id":128,"text":"Arizona Water Science Center","active":true,"usgs":true}],"preferred":true,"id":249042,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Albano, Christine M.","contributorId":17681,"corporation":false,"usgs":true,"family":"Albano","given":"Christine M.","affiliations":[],"preferred":false,"id":249045,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ]}