{"pageNumber":"80","pageRowStart":"1975","pageSize":"25","recordCount":3813,"records":[{"id":74223,"text":"fs20053129 - 2005 - Inventory of Anchialine Pools in Hawaii's National Parks","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"fs20053129","displayToPublicDate":"2006-02-14T00:00:00","publicationYear":"2005","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":"2005-3129","title":"Inventory of Anchialine Pools in Hawaii's National Parks","docAbstract":"BACKGROUND\r\n\r\nAnchialine (?near the sea?) pools are rare and localized brackish waters along coastal lava flows that exhibit tidal fluctuations without a surface connection with the ocean (Fig. 1). In Hawai`i, these pools were frequently excavated or otherwise modified by Hawaiians to serve as sources of drinking water, baths and fish ponds. National Parks in Hawai`i possess the full spectrum of pool types, from walled fish ponds to undisturbed pools in collapsed lava tubes, cracks and caves. Pools contain relatively rare and unique fauna threatened primarily by invasive species and habitat loss. In collaboration with the National Park Service?s Inventory and Monitoring Program, the U.S. Geological Survey?s Pacific Island Ecosystems Research Center undertook inventories of these unique ecosystems in two National Parks on the island of Hawai`i: Hawai`i Volcanoes National Park and Kaloko-Honokohau National Historical Park.","language":"ENGLISH","doi":"10.3133/fs20053129","usgsCitation":"Foote, D., 2005, Inventory of Anchialine Pools in Hawaii's National Parks: U.S. Geological Survey Fact Sheet 2005-3129, 2 p., https://doi.org/10.3133/fs20053129.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":121000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3129.jpg"},{"id":10713,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://biology.usgs.gov/pierc/Plants,_Insects_&_Ecosystems/Anchialine_pools.pdf","size":"957","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c5e4b07f02db53f91f","contributors":{"authors":[{"text":"Foote, David dfoote@usgs.gov","contributorId":375,"corporation":false,"usgs":true,"family":"Foote","given":"David","email":"dfoote@usgs.gov","affiliations":[{"id":5049,"text":"Pacific Islands Ecosys Research Center","active":true,"usgs":true}],"preferred":true,"id":286576,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":74163,"text":"fs20053154 - 2005 - Aquatic invasive species research capabilities at the Upper Midwest Environmental Sciences Center","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"fs20053154","displayToPublicDate":"2006-02-14T00:00:00","publicationYear":"2005","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":"2005-3154","title":"Aquatic invasive species research capabilities at the Upper Midwest Environmental Sciences Center","language":"ENGLISH","doi":"10.3133/fs20053154","usgsCitation":"Rach, J., 2005, Aquatic invasive species research capabilities at the Upper Midwest Environmental Sciences Center: U.S. Geological Survey Fact Sheet 2005-3154, 2 p., https://doi.org/10.3133/fs20053154.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":123027,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3154.jpg"},{"id":7369,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.umesc.usgs.gov/reports_publications/fact_sheets/invasives_capabilities.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db67a041","contributors":{"authors":[{"text":"Rach, Jeffery","contributorId":73291,"corporation":false,"usgs":true,"family":"Rach","given":"Jeffery","affiliations":[],"preferred":false,"id":286567,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":74113,"text":"fs20053113 - 2005 - Great Lakes basin water availability and use: a study of the National Assessment of Water Availability and Use Program","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"fs20053113","displayToPublicDate":"2006-02-14T00:00:00","publicationYear":"2005","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":"2005-3113","title":"Great Lakes basin water availability and use: a study of the National Assessment of Water Availability and Use Program","language":"ENGLISH","doi":"10.3133/fs20053113","usgsCitation":"Grannemann, N.G., and Reeves, H.W., 2005, Great Lakes basin water availability and use: a study of the National Assessment of Water Availability and Use Program: U.S. Geological Survey Fact Sheet 2005-3113, 4 p., https://doi.org/10.3133/fs20053113.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":122459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3113.bmp"},{"id":7314,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3113/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671f46","contributors":{"authors":[{"text":"Grannemann, Norman G. nggranne@usgs.gov","contributorId":4823,"corporation":false,"usgs":true,"family":"Grannemann","given":"Norman","email":"nggranne@usgs.gov","middleInitial":"G.","affiliations":[{"id":5068,"text":"Midwest Regional Director's Office","active":true,"usgs":true}],"preferred":true,"id":286558,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeves, Howard W. 0000-0001-8057-2081 hwreeves@usgs.gov","orcid":"https://orcid.org/0000-0001-8057-2081","contributorId":2307,"corporation":false,"usgs":true,"family":"Reeves","given":"Howard","email":"hwreeves@usgs.gov","middleInitial":"W.","affiliations":[{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":286557,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":74193,"text":"fs20053150 - 2005 - Geomorphic Assessment of Bank Instability, Missouri National Recreational River","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"fs20053150","displayToPublicDate":"2006-02-14T00:00:00","publicationYear":"2005","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":"2005-3150","title":"Geomorphic Assessment of Bank Instability, Missouri National Recreational River","language":"ENGLISH","doi":"10.3133/fs20053150","usgsCitation":"Elliott, C.M., 2005, Geomorphic Assessment of Bank Instability, Missouri National Recreational River: U.S. Geological Survey Fact Sheet 2005-3150, 2 p., https://doi.org/10.3133/fs20053150.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":7371,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://infolink.cr.usgs.gov/RSB/MNRR-L.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122448,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3150.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c570","contributors":{"authors":[{"text":"Elliott, Caroline M. 0000-0002-9190-7462 celliott@usgs.gov","orcid":"https://orcid.org/0000-0002-9190-7462","contributorId":2380,"corporation":false,"usgs":true,"family":"Elliott","given":"Caroline","email":"celliott@usgs.gov","middleInitial":"M.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":286570,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":73583,"text":"fs20053111 - 2005 - Naturally Occurring Arsenic in Ground Water, Norman, Oklahoma, 2004, and Remediation Options for Produced Water","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"fs20053111","displayToPublicDate":"2006-02-10T00:00:00","publicationYear":"2005","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":"2005-3111","title":"Naturally Occurring Arsenic in Ground Water, Norman, Oklahoma, 2004, and Remediation Options for Produced Water","docAbstract":"In 2000, the U.S. Environmental Protection Agency (EPA) reviewed the arsenic drinking water standard for public water supplies. Considering the available research and statistics on the health effects of arsenic ingestion, the EPA reduced the Maximum Contaminant Level (MCL) for public drinking water from 50 micrograms per liter (?g/L) to 10 ?g/L (U.S. Environmental Protection Agency, 2001a). As a result of the more stringent standard, the EPA estimates that about 3,000 public water providers across the United States must take action to meet the new standard before it becomes effective on January 23, 2006 (U.S. Environmental Protection Agency, 2001b).\r\n\r\nThe City of Norman (City) is one of several Oklahoma municipalities affected by the new arsenic standard. About 20 percent of Norman?s water is supplied by wells completed in the Central Oklahoma (Garber-Wellington) aquifer; the rest is supplied by Lake Thunderbird (fig. 1) or purchased from Oklahoma City. The Norman well field is composed of 24 active wells, and water produced from about half of the wells will not be in compliance with the new MCL (figs. 2 and 3). Chemical treatment of water with elevated arsenic is possible, but it is generally cost prohibitive. Another costly solution is simply to abandon the high-arsenic wells and replace them with new wells in low-arsenic areas. In the next phase of well construction beginning in 2005, the City plans to construct as many as 30 new wells in northeast Norman (Bryan Mitchell, City of Norman, oral commun., 2005). The new wells will replace production lost to the new arsenic standard and add new production to keep pace with rapidly growing consumer demand. Well modification to exclude arsenic-bearing water from existing wells is a more cost-effective solution, but it requires a great deal of knowledge about local aquifer properties and individual well dynamics to decide which wells are good candidates for modification. With the goal of determining if well modification can be used to bring some of Norman?s high-arsenic wells into compliance with the new arsenic standard, the EPA Office of Research and Development (ORD) initiated a three-year research project in 2003 with participation from the U.S. Geological Survey (USGS), Oklahoma State University, and the City of Norman. The primary objectives of the project are to: (1) determine where naturally occurring arsenic is entering wells by collecting water samples at different depths, (2) investigate the utility of new methods for collecting water-quality data in a pumping well, (3) better understand the stratigraphy and composition of aquifer rocks, (4) assess 10 wells for the possibility of arsenic remediation by well modification, and (5) evaluate the effectiveness of well modification in bringing marginal wells into compliance with the new arsenic MCL. The purpose of this report is to describe the occurrence of arsenic in ground water near Norman, Oklahoma, and available options for reducing arsenic concentrations in produced ground water.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/fs20053111","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency and the City of Norman","usgsCitation":"Smith, S.J., and Christenson, S., 2005, Naturally Occurring Arsenic in Ground Water, Norman, Oklahoma, 2004, and Remediation Options for Produced Water: U.S. Geological Survey Fact Sheet 2005-3111, 6 p., https://doi.org/10.3133/fs20053111.","productDescription":"6 p.","numberOfPages":"6","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":125326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2005/3111/report-thumb.jpg"},{"id":91186,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2005/3111/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6672f5","contributors":{"authors":[{"text":"Smith, S. Jerrod 0000-0002-9379-8167 sjsmith@usgs.gov","orcid":"https://orcid.org/0000-0002-9379-8167","contributorId":981,"corporation":false,"usgs":true,"family":"Smith","given":"S.","email":"sjsmith@usgs.gov","middleInitial":"Jerrod","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":286436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christenson, Scott","contributorId":59128,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","affiliations":[],"preferred":false,"id":286437,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":73833,"text":"fs20053156 - 2005 - Landslide hazards: A national threat","interactions":[],"lastModifiedDate":"2023-05-03T21:23:23.453705","indexId":"fs20053156","displayToPublicDate":"2006-02-10T00:00:00","publicationYear":"2005","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":"2005-3156","title":"Landslide hazards: A national threat","docAbstract":"Landslides occur and can cause damage in all 50 States. Severe storms, earthquakes, volcanic activity, coastal wave attack, and wildfires can cause widespread slope instability. Landslide danger may be high even as emergency personnel are providing rescue and recovery services.\r\n\r\nTo address landslide hazards, several questions must be considered: Where and when will landslides occur? How big will the landslides be? How fast and how far will they move? What areas will the landslides affect or damage? How frequently do landslides occur in a given area?\r\n\r\nAnswers to these questions are needed to make accurate landslide hazard maps and forecasts of landslide occurrence, and to provide information on how to avoid or mitigate landslide impacts.\r\n\r\nThe U.S. Geological Survey develops methods to answer these questions to help protect U.S. communities from the dangers of landslides.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"USGS Science Helps Build Safer Communities","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20053156","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, Landslide hazards: A national threat: U.S. Geological Survey Fact Sheet 2005-3156, 2 p., https://doi.org/10.3133/fs20053156.","productDescription":"2 p.","numberOfPages":"2","costCenters":[{"id":595,"text":"U.S. Geological 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2004","interactions":[],"lastModifiedDate":"2015-09-25T13:51:12","indexId":"fs20053134","displayToPublicDate":"2006-02-10T00:00:00","publicationYear":"2005","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":"2005-3134","title":"Methods for monitoring the effects of grazing management on bank erosion and channel morphology, Fever River, Pioneer Farm, Wisconsin, 2004","docAbstract":"

Bank erosion is a natural process that occurs in meandering streams (Leopold and others, 1964); however, in the Midwestern United States, historical and present agricultural activities in uplands, riparian areas, and channels have increased erosion (Waters, 1995; Lyons and others, 2000; Simon and Rinaldi, 2000; and Knox, 2001). Reducing streambank erosion is important because sediment carried by streams has adverse environmental effects; for example, sediment carried by streams is a major source of phosphorus (Waters, 1995). Continuous cattle grazing in riparian areas may increase local erosion processes in a meandering stream by removal or trampling of bank vegetation, which in turn affects channel morphology, water chemistry, and fish and aquatic-insect habitat (Kauffman and Krueger, 1984; Fitch and Adams, 1998). However, studies of livestock exclusion from riparian corridors have shown mixed results in reducing bank erosion (Trimble, 1994; Sarr, 2002). Some studies have shown reduced bank erosion after row-cropped or continuously grazed riparian areas are converted to managed grazing (see inset box) (Lyons and others, 2000; Sovell and others, 2000; and Zaimes and others, 2004).

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These studies are hampered by imperfect detection of these species, which can result in some sites appearing to be unoccupied that are actually occupied. Occupancy models solve this problem and produce unbiased estimates of occupancy and related parameters. Required data (detection/non-detection information) are relatively simple and inexpensive to collect. 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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs20053123","usgsCitation":"Kolker, A., Mose, D.G., Spitzer, S., and East, J.A., 2005, Expanding the mercury deposition network in Virginia and the U.S. mid-Atlantic region: U.S. Geological Survey Fact Sheet 2005-3123, 4 p., https://doi.org/10.3133/fs20053123.","productDescription":"4 p.","costCenters":[],"links":[{"id":120830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3123.jpg"},{"id":7307,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3123/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f935f","contributors":{"authors":[{"text":"Kolker, Allan 0000-0002-5768-4533 akolker@usgs.gov","orcid":"https://orcid.org/0000-0002-5768-4533","contributorId":643,"corporation":false,"usgs":true,"family":"Kolker","given":"Allan","email":"akolker@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":286466,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mose, Douglas G.","contributorId":56518,"corporation":false,"usgs":true,"family":"Mose","given":"Douglas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":286468,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spitzer, Shane","contributorId":63421,"corporation":false,"usgs":true,"family":"Spitzer","given":"Shane","email":"","affiliations":[],"preferred":false,"id":286469,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"East, Joseph A. 0000-0003-4226-9174 jeast@usgs.gov","orcid":"https://orcid.org/0000-0003-4226-9174","contributorId":2747,"corporation":false,"usgs":true,"family":"East","given":"Joseph","email":"jeast@usgs.gov","middleInitial":"A.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":286467,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":73133,"text":"fs20053147 - 2005 - Parking lot sealcoat: a major source of polycyclic aromatic hydrocarbons (PAHs) in urban and suburban environments","interactions":[],"lastModifiedDate":"2016-08-23T13:32:39","indexId":"fs20053147","displayToPublicDate":"2006-01-19T00:00:00","publicationYear":"2005","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":"2005-3147","title":"Parking lot sealcoat: a major source of polycyclic aromatic hydrocarbons (PAHs) in urban and suburban environments","docAbstract":"

Collaborative studies by the City of Austin and the U. S. Geological Survey (USGS) have identified coal-tar based sealcoat—the black, shiny emulsion painted or sprayed on asphalt pavement such as parking lots—as a major and previously unrecognized source of polycyclic aromatic hydrocarbon (PAH) contamination. Several PAHs are suspected human carcinogens and are toxic to aquatic life. Studies in Austin, Texas, showed that particles in runoff from coal-tar based sealcoated parking lots had concentrations of PAHs that were about 65 times higher than concentrations in particles washed off parking lots that had not been sealcoated. Biological studies, conducted by the City of Austin in the field and in the laboratory, indicated that PAH levels in sediment contaminated with abraded sealcoat were toxic to aquatic life and were degrading aquatic communities, as indicated by loss of species and decreased numbers of organisms. Identification of this source of PAHs may help to improve future strategies for controlling these compounds in urban water bodies across the Nation where parking lot sealcoat is used.

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No abstract available.

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Wildland fires are inevitable in the western United States. Expansion of man-made developments into fire-prone wildlands has created situations where wildfires can destroy lives and property, as can the flooding and debris flows that are common in the aftermath of the fires. Fast-moving, highly destructive debris flows triggered by intense rainfall are one of the most dangerous post-fire hazards. Such debris flows are particularly dangerous because they tend to occur with little warning. Their mass and speed make them particularly destructive: debris flows can strip vegetation, block drainages, damage structures, and endanger human life.

The U.S. Geological Survey’s Landslide Hazards Program is participating in a multi-agency cooperative effort to investigate debris flows in burned areas of southern California and other parts of the western United States. Participating agencies are the USDA Forest Service, the Natural Resources Conservation Service, and the California, Colorado, and Montana Geological Surveys. The objective of this project is to develop methods needed to estimate the locations, probability of occurrence, and size of potentially destructive debris flows. Public officials can use this information to plan and execute emergency response and post-fire rehabilitation.

Analysis of data collected from studies of debris flows following wildfires can answer many of the questions fundamental to post-fire hazard assessments— what and why, where, when, how big, and how often?

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