Item talk:Q58679: Difference between revisions

From geokb
(Added abstract and other texts to publication item's discussion page for reference)
 
(Wrote fresh schema.org document to item wiki page)
Line 1: Line 1:
= Assessing landslide potential on coastal bluffs near Mukilteo, Washington—Geologic site characterization for hydrologic monitoring =
{"@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Assessing landslide potential on coastal bluffs near Mukilteo, Washington\u2014Geologic site characterization for hydrologic monitoring", "identifier": [{"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "ofr20161082", "url": "https://pubs.usgs.gov/publication/ofr20161082"}, {"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70171185}, {"@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/ofr20161082", "url": "https://doi.org/10.3133/ofr20161082"}], "inLanguage": "en", "isPartOf": [{"@type": "CreativeWorkSeries", "name": "Open-File Report"}], "datePublished": "2016", "dateModified": "2016-07-01", "abstract": "During the summer 2015, the U.S. Geological Survey collected geologic and geotechnical data for two sites on coastal bluffs along the eastern shore of Puget Sound, Washington. The U.S. Geological Survey also installed hydrologic instrumentation at the sites and collected specimens for laboratory testing. The two sites are located on City of Mukilteo open-space land and are about 0.6 kilometers apart. The bluffs at each site are approximately 42 meters high, and rise steeply from the shoreline with 32\u201335\u00b0 slopes. The more northerly of the two sites occupies an active landslide and is mostly unvegetated. The other site is forested, and although stable during the preparation of this report, shows evidence of historical and potential landslide activity. The slopes of the bluffs at both sites are mantled by a thin, nonuniform colluvium underlain by clay-rich glacial deposits and tills of the Whidbey Formation or Double Bluff Drift. Till consisting of sand, gravel, and cobbles caps the bluffs and rests on finer grained glacial deposits of sand, silt, and clay. These types of different glacial deposits are dense, vertically fractured, and generally have low permeability, but field observations indicate that locally the deposits are sufficiently permeable to allow lateral flow of water along fractures and subhorizontal boundaries between deposits of different texture. Laboratory tests indicate that many of the deposits are highly plastic, with low hydraulic conductivity, and moderate shear strength. Steep slopes combined with the strength and hydraulic characteristics of the deposits leave the bluffs prone to slope instability, particularly during the wet season when infiltrating rainfall changes moisture content, pore-water pressure, and effective stress within the hillslope. The instrumentation was designed to primarily observe rainfall variability and hydrologic changes in the subsurface that can affect stability of the bluffs, and also to compare the hydrologic response between areas where previous landslides have disturbed vegetation and areas where the bluff is apparently more stable and well vegetated.", "description": "Report: vi,  34 p. HTML Document: Data Release", "publisher": {"@type": "Organization", "name": "U.S. Geological Survey"}, "author": [{"@type": "Person", "name": "Mirus, Benjamin B.", "givenName": "Benjamin B.", "familyName": "Mirus", "affiliation": [{"@type": "Organization", "name": "University of North Carolina"}]}, {"@type": "Person", "name": "Smith, Joel B. jbsmith@usgs.gov", "givenName": "Joel B.", "familyName": "Smith", "email": "jbsmith@usgs.gov", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-7219-7875", "url": "https://orcid.org/0000-0001-7219-7875"}, "affiliation": [{"@type": "Organization", "name": "Geologic Hazards Science Center", "url": "https://www.usgs.gov/centers/geologic-hazards-science-center"}]}, {"@type": "Person", "name": "Benjamin Stark", "familyName": "Benjamin Stark", "affiliation": [{"@type": "Organization", "name": "U.S. Army Corps of Engineers"}]}, {"@type": "Person", "name": "York Lewis", "familyName": "York Lewis", "affiliation": [{"@type": "Organization", "name": "U.S. Army Corps of Engineers"}]}, {"@type": "Person", "name": "Abigail Michel", "familyName": "Abigail Michel", "affiliation": [{"@type": "Organization", "name": "U.S. Army Corps of Engineers"}]}, {"@type": "Person", "name": "Baum, Rex L. baum@usgs.gov", "givenName": "Rex L.", "familyName": "Baum", "email": "baum@usgs.gov", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-5337-1970", "url": "https://orcid.org/0000-0001-5337-1970"}, "affiliation": [{"@type": "Organization", "name": "Geologic Hazards Science Center", "url": "https://www.usgs.gov/centers/geologic-hazards-science-center"}]}], "funder": [{"@type": "Organization", "name": "Geologic Hazards Science Center", "url": "https://www.usgs.gov/centers/geologic-hazards-science-center"}], "spatialCoverage": [{"@type": "Place", "additionalType": "country", "name": "United States", "url": "https://geonames.org/6252001"}, {"@type": "Place", "additionalType": "state", "name": "Washington", "url": "https://geonames.org/5815135"}, {"@type": "Place", "additionalType": "unknown", "name": "Puget Sound", "url": "https://geonames.org/5807517"}, {"@type": "Place", "geo": [{"@type": "GeoShape", "additionalProperty": {"@type": "PropertyValue", "name": "GeoJSON", "value": {"type": "FeatureCollection", "features": [{"type": "Feature", "properties": {}, "geometry": {"type": "Polygon", "coordinates": [[[-122.66098022460939, 48.448333001219005], [-122.68157958984375, 48.448333001219005], [-122.68844604492186, 48.43193420325806], [-122.67608642578126, 48.4164415885222], [-122.67333984374999, 48.37632112598019], [-122.77084350585938, 48.26034139584532], [-122.80517578125, 48.17158081783164], [-122.91778564453125, 48.09275716032736], [-122.90679931640624, 47.7476346002088], [-122.90267944335938, 47.6441113460123], [-122.80517578125, 47.646886969413], [-122.75024414062499, 47.666312203609145], [-122.67745971679688, 47.585789182379905], [-122.56759643554689, 47.304378285521565], [-122.46734619140625, 47.280160670764744], [-122.39730834960938, 47.26711582310954], [-122.29980468749999, 47.352780247239586], [-122.3272705078125, 47.525547335516556], [-122.30804443359375, 47.78363463526376], [-122.20642089843749, 47.989002568678686], [-122.1844482421875, 48.060643120324514], [-122.38632202148438, 48.31882083063846], [-122.66098022460939, 48.448333001219005]]]}}]}}}, {"@type": "GeoCoordinates", "latitude": 47.88152695646555, "longitude": -122.55458917111018}]}]}
During the summer 2015, the U.S. Geological Survey collected geologic and geotechnical data for two sites on coastal bluffs along the eastern shore of Puget Sound, Washington. The U.S. Geological Survey also installed hydrologic instrumentation at the sites and collected specimens for laboratory testing. The two sites are located on City of Mukilteo open-space land and are about 0.6 kilometers apart. The bluffs at each site are approximately 42 meters high, and rise steeply from the shoreline with 32–35° slopes. The more northerly of the two sites occupies an active landslide and is mostly unvegetated. The other site is forested, and although stable during the preparation of this report, shows evidence of historical and potential landslide activity. The slopes of the bluffs at both sites are mantled by a thin, nonuniform colluvium underlain by clay-rich glacial deposits and tills of the Whidbey Formation or Double Bluff Drift. Till consisting of sand, gravel, and cobbles caps the bluffs and rests on finer grained glacial deposits of sand, silt, and clay. These types of different glacial deposits are dense, vertically fractured, and generally have low permeability, but field observations indicate that locally the deposits are sufficiently permeable to allow lateral flow of water along fractures and subhorizontal boundaries between deposits of different texture. Laboratory tests indicate that many of the deposits are highly plastic, with low hydraulic conductivity, and moderate shear strength. Steep slopes combined with the strength and hydraulic characteristics of the deposits leave the bluffs prone to slope instability, particularly during the wet season when infiltrating rainfall changes moisture content, pore-water pressure, and effective stress within the hillslope. The instrumentation was designed to primarily observe rainfall variability and hydrologic changes in the subsurface that can affect stability of the bluffs, and also to compare the hydrologic response between areas where previous landslides have disturbed vegetation and areas where the bluff is apparently more stable and well vegetated.
 
== Table of Contents ==
* Preface
* Acknowledgments
* Abstract
* Introduction
* Geologic Site Conditions
* Field Instrumentation
* Laboratory Analyses of Colluvium and Glacial Sediments
* Discussion
* Summary
* References

Revision as of 20:24, 15 July 2024

{"@context": "https://schema.org", "@type": "CreativeWork", "additionalType": "USGS Numbered Series", "name": "Assessing landslide potential on coastal bluffs near Mukilteo, Washington\u2014Geologic site characterization for hydrologic monitoring", "identifier": [{"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "ofr20161082", "url": "https://pubs.usgs.gov/publication/ofr20161082"}, {"@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70171185}, {"@type": "PropertyValue", "propertyID": "DOI", "value": "10.3133/ofr20161082", "url": "https://doi.org/10.3133/ofr20161082"}], "inLanguage": "en", "isPartOf": [{"@type": "CreativeWorkSeries", "name": "Open-File Report"}], "datePublished": "2016", "dateModified": "2016-07-01", "abstract": "During the summer 2015, the U.S. Geological Survey collected geologic and geotechnical data for two sites on coastal bluffs along the eastern shore of Puget Sound, Washington. The U.S. Geological Survey also installed hydrologic instrumentation at the sites and collected specimens for laboratory testing. The two sites are located on City of Mukilteo open-space land and are about 0.6 kilometers apart. The bluffs at each site are approximately 42 meters high, and rise steeply from the shoreline with 32\u201335\u00b0 slopes. The more northerly of the two sites occupies an active landslide and is mostly unvegetated. The other site is forested, and although stable during the preparation of this report, shows evidence of historical and potential landslide activity. The slopes of the bluffs at both sites are mantled by a thin, nonuniform colluvium underlain by clay-rich glacial deposits and tills of the Whidbey Formation or Double Bluff Drift. Till consisting of sand, gravel, and cobbles caps the bluffs and rests on finer grained glacial deposits of sand, silt, and clay. These types of different glacial deposits are dense, vertically fractured, and generally have low permeability, but field observations indicate that locally the deposits are sufficiently permeable to allow lateral flow of water along fractures and subhorizontal boundaries between deposits of different texture. Laboratory tests indicate that many of the deposits are highly plastic, with low hydraulic conductivity, and moderate shear strength. Steep slopes combined with the strength and hydraulic characteristics of the deposits leave the bluffs prone to slope instability, particularly during the wet season when infiltrating rainfall changes moisture content, pore-water pressure, and effective stress within the hillslope. The instrumentation was designed to primarily observe rainfall variability and hydrologic changes in the subsurface that can affect stability of the bluffs, and also to compare the hydrologic response between areas where previous landslides have disturbed vegetation and areas where the bluff is apparently more stable and well vegetated.", "description": "Report: vi, 34 p. HTML Document: Data Release", "publisher": {"@type": "Organization", "name": "U.S. Geological Survey"}, "author": [{"@type": "Person", "name": "Mirus, Benjamin B.", "givenName": "Benjamin B.", "familyName": "Mirus", "affiliation": [{"@type": "Organization", "name": "University of North Carolina"}]}, {"@type": "Person", "name": "Smith, Joel B. jbsmith@usgs.gov", "givenName": "Joel B.", "familyName": "Smith", "email": "jbsmith@usgs.gov", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-7219-7875", "url": "https://orcid.org/0000-0001-7219-7875"}, "affiliation": [{"@type": "Organization", "name": "Geologic Hazards Science Center", "url": "https://www.usgs.gov/centers/geologic-hazards-science-center"}]}, {"@type": "Person", "name": "Benjamin Stark", "familyName": "Benjamin Stark", "affiliation": [{"@type": "Organization", "name": "U.S. Army Corps of Engineers"}]}, {"@type": "Person", "name": "York Lewis", "familyName": "York Lewis", "affiliation": [{"@type": "Organization", "name": "U.S. Army Corps of Engineers"}]}, {"@type": "Person", "name": "Abigail Michel", "familyName": "Abigail Michel", "affiliation": [{"@type": "Organization", "name": "U.S. Army Corps of Engineers"}]}, {"@type": "Person", "name": "Baum, Rex L. baum@usgs.gov", "givenName": "Rex L.", "familyName": "Baum", "email": "baum@usgs.gov", "identifier": {"@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0001-5337-1970", "url": "https://orcid.org/0000-0001-5337-1970"}, "affiliation": [{"@type": "Organization", "name": "Geologic Hazards Science Center", "url": "https://www.usgs.gov/centers/geologic-hazards-science-center"}]}], "funder": [{"@type": "Organization", "name": "Geologic Hazards Science Center", "url": "https://www.usgs.gov/centers/geologic-hazards-science-center"}], "spatialCoverage": [{"@type": "Place", "additionalType": "country", "name": "United States", "url": "https://geonames.org/6252001"}, {"@type": "Place", "additionalType": "state", "name": "Washington", "url": "https://geonames.org/5815135"}, {"@type": "Place", "additionalType": "unknown", "name": "Puget Sound", "url": "https://geonames.org/5807517"}, {"@type": "Place", "geo": [{"@type": "GeoShape", "additionalProperty": {"@type": "PropertyValue", "name": "GeoJSON", "value": {"type": "FeatureCollection", "features": [{"type": "Feature", "properties": {}, "geometry": {"type": "Polygon", "coordinates": [[[-122.66098022460939, 48.448333001219005], [-122.68157958984375, 48.448333001219005], [-122.68844604492186, 48.43193420325806], [-122.67608642578126, 48.4164415885222], [-122.67333984374999, 48.37632112598019], [-122.77084350585938, 48.26034139584532], [-122.80517578125, 48.17158081783164], [-122.91778564453125, 48.09275716032736], [-122.90679931640624, 47.7476346002088], [-122.90267944335938, 47.6441113460123], [-122.80517578125, 47.646886969413], [-122.75024414062499, 47.666312203609145], [-122.67745971679688, 47.585789182379905], [-122.56759643554689, 47.304378285521565], [-122.46734619140625, 47.280160670764744], [-122.39730834960938, 47.26711582310954], [-122.29980468749999, 47.352780247239586], [-122.3272705078125, 47.525547335516556], [-122.30804443359375, 47.78363463526376], [-122.20642089843749, 47.989002568678686], [-122.1844482421875, 48.060643120324514], [-122.38632202148438, 48.31882083063846], [-122.66098022460939, 48.448333001219005]]]}}]}}}, {"@type": "GeoCoordinates", "latitude": 47.88152695646555, "longitude": -122.55458917111018}]}]}