Landslide

20140416 11211600 FALSE 20230522 10125100 20230522 10125100 Published LANDSLIDE 002 5828753.879015 6037113.261225 2119115.096583 2319837.329602 1 Projected GCS_North_American_1983_HARN Linear Unit: Foot_US (0.304801) NAD_1983_HARN_StatePlane_California_III_FIPS_0403_Feet <ProjectedCoordinateSystem xsi:type='typens:ProjectedCoordinateSystem' xmlns:xsi='http://www.w3.org/2001/XMLSchema-instance' xmlns:xs='http://www.w3.org/2001/XMLSchema' xmlns:typens='http://www.esri.com/schemas/ArcGIS/10.8'><WKT>PROJCS["NAD_1983_HARN_StatePlane_California_III_FIPS_0403_Feet",GEOGCS["GCS_North_American_1983_HARN",DATUM["D_North_American_1983_HARN",SPHEROID["GRS_1980",6378137.0,298.257222101]],PRIMEM["Greenwich",0.0],UNIT["Degree",0.0174532925199433]],PROJECTION["Lambert_Conformal_Conic"],PARAMETER["False_Easting",6561666.666666666],PARAMETER["False_Northing",1640416.666666667],PARAMETER["Central_Meridian",-120.5],PARAMETER["Standard_Parallel_1",37.06666666666667],PARAMETER["Standard_Parallel_2",38.43333333333333],PARAMETER["Latitude_Of_Origin",36.5],UNIT["Foot_US",0.3048006096012192],AUTHORITY["EPSG",2872]]</WKT><XOrigin>-115860599.99969342</XOrigin><YOrigin>-93269499.999998093</YOrigin><XYScale>7812.4999927240433</XYScale><ZOrigin>0</ZOrigin><ZScale>1</ZScale><MOrigin>0</MOrigin><MScale>1</MScale><XYTolerance>0.0010240000009536742</XYTolerance><ZTolerance>0.001</ZTolerance><MTolerance>2</MTolerance><HighPrecision>true</HighPrecision><WKID>2872</WKID><LatestWKID>2872</LatestWKID></ProjectedCoordinateSystem> 1.0 FGDC U.S. GEOLOGICAL SURVEY 1997 Landslide LANDSLIDE vector digital data withheld Summary Distribution of Slides and Earth Flows in the San Francisco Bay Menlo Park, CA U.S. GEOLOGICAL SURVEY ESRI ArcCatalog 9.3.1.1850 en Slides and earth flows are landslides that can pose serious hazard to property in the hillside terrain of the San Francisco Bay region. They tend to move slowly and thus rarely threaten life directly. When they move -- in response to such changes as increased water content, earthquake shaking, addition of load, or removal of downslope support -- they deform and tilt the ground surface. The result can be destruction of foundations, offset of roads, and breaking of underground pipes within and along the margins of the landslide, as well as overriding of property and structures downslope. The best available predictor of where movement of slides and earth flows might occur is the distribution of past movements (Nilsen and Turner, 1975). These landslides can be recognized from their distinctive topographic shapes, which can persist in the landscape for thousands of years. Most of the landslides recognizable in this fashion range in size from a few acres to several square miles. Most show no evidence of recent movement and are not currently active. Some small proportion of them may become active in any one year, with movements concentrated within all or part of the landslide masses or around their edges. These maps and databases provide a summary of the distribution of landslides evident in the landscape of the San Francisco Bay region. Original identification and map delineation of these landslides required detailed analysis of the topography by skilled geologists, a task generally accomplished through the study of aerial photographs. Such original landslide maps are now available for most of the region at scales of 1:24,000 - 1:62,500 (Pike, 1997). The summary map presented here makes selected use of these original maps and the 9-county compilation by Nilsen, Wright, and others (1979) to provide a basis for initial evaluation of areas vulnerable to slumps, translational slides, and earth flows in the region. The summary map modifies and improves the compilation by Nilsen and Wright, which was prepared from sources available in the mid-1970's. The generalized landslide distribution shown on that map has here been improved in areas where the 1970's sources were notably deficient (Figure 1), has been extended to include Santa Cruz County, and includes the distribution of surficial deposits that define landscape not generally vulnerable to these kinds of landslides. The method of compilation and resolution of 1:125,000 (1 inch = 2 miles) limits use of the map to regional considerations. For more detailed information, see the maps listed by Pike (1997) or consult local officials or private consultants. To provide Landslide data to the Marin Countywide Plan Update. publication date 1997 Complete As needed -123.055543 -122.315672 38.351839 37.787427 5828753.879015 6037113.261225 2119115.096583 2319837.329602 REQUIRED: Reference to a formally registered thesaurus or a similar authoritative source of theme keywords. Landslides geoscientificInformation None. REQUIRED: Restrictions and legal prerequisites for using the data set after access is granted. Feature Class U.S. GEOLOGICAL SURVEY withheld 002 4.147 Feature Class Feature Class Dataset copied. 20031024 10335800 Dataset copied. withheld 20040323 09543300 Dataset copied. withheld 20040324 11271700 125000 The digital compilation was performed in ARC/INFO, a commercial Geographic Information System (Environmental Research Institute [ESRI], Redlands, California). The three 1:125,000 map sheets of the region (Aitken, 1997) were compiled separately and then combined. County databases were clipped from the composite polygon coverage for the region. The generalized landslide zones of Nilsen and Wright (1979, category 5 of plates 1-3) were captured in digital form by scanning publication negatives. Vector perimeters of the resulting category 5 areas in the raster scans were determined automatically (GRIDPOLY) and processed to smooth the boundaries and eliminate polygons with areas less than 4000-5000 square meters (noise in the data). Registration proved to be a problem. Initial registration using geographic locations of various marks on the negatives (determined by comparison with a base map) was improved by rubbersheeting to better fit quadrangle corners evident in the data. Most misfits in the result are probably less than 50 meters on the ground. The revision lines in the northern part of the region were traced, scanned, hand-edited on-screen, registered with latitude/longitude intersections and intersections in the township/range network, and converted to closed polygons. The information for Santa Cruz County was prepared in the same fashion, using the original 1:24,000 quadrangles as a source. As an initial step, a coherent original for tracing was prepared by scanning, projecting, and plotting the 7.5 minute quadrangles together at 1:62,500. Ellen's terrain map in northwestern Marin county (Ellen and others, 1988) was scanned and projected and then interpreted on-screen together with the slope data to produce vector polygons. The areas of surficial deposits were extracted from Wentworth (1997) by selecting appropriate polygons, putting them into a separate data layer, and then dissolving internal lines. The result was a vector polygon layer in which the polygons were categorized as unmapped (within outer sheet boundaries), water, surficial deposits, or bedrock. Combining of the several polygon datasets was performed in bulk for each sheet, using the INTERSECT and UNION commands in ARC. Because the polygons from the different sources overlapped, this process resulted in many sliver polygons of various sizes. These were largely eliminated in two steps: 1. Assigning unit identities in a priority sequence -- water, surficial deposits, mostly landslide, many landslides, and finally the remaining few landslides category, 2. Dissolving the boundaries between adjacent polygons with the same resultant identities. This was a complex process that yielded a usable result, although numerous slivers remain. The hand editing required to produce a more elegant result was not feasible. Version 6.2 (Build 9200) ; Esri ArcGIS 10.9.1.28388 LANDSLIDE 5828753.879015 6037113.261225 2319837.329602 2119115.096583 1 -123.055543 -122.315672 38.351839 37.787427 1 1 -123.055543 -122.315672 38.351839 37.787427 The published representation of Landslide data used in the Marin Countywide Plan Update. <div style='text-align:Left;'><div><p><span>Slides and earth flows are landslides that can pose serious hazard to property in the hillside terrain of the San Francisco Bay region. They tend to move slowly and thus rarely threaten life directly. When they move -- in response to such changes as increased water content, earthquake shaking, addition of load, or removal of downslope support -- they deform and tilt the ground surface. The result can be destruction of foundations, offset of roads, and breaking of underground pipes within and along the margins of the landslide, as well as overriding of property and structures downslope. The best available predictor of where movement of slides and earth flows might occur is the distribution of past movements (Nilsen and Turner, 1975). These landslides can be recognized from their distinctive topographic shapes, which can persist in the landscape for thousands of years. Most of the landslides recognizable in this fashion range in size from a few acres to several square miles. Most show no evidence of recent movement and are not currently active. Some small proportion of them may become active in any one year, with movements concentrated within all or part of the landslide masses or around their edges. These maps and databases provide a summary of the distribution of landslides evident in the landscape of the San Francisco Bay region. Original identification and map delineation of these landslides required detailed analysis of the topography by skilled geologists, a task generally accomplished through the study of aerial photographs. Such original landslide maps are now available for most of the region at scales of 1:24,000 - 1:62,500 (Pike, 1997). The summary map presented here makes selected use of these original maps and the 9-county compilation by Nilsen, Wright, and others (1979) to provide a basis for initial evaluation of areas vulnerable to slumps, translational slides, and earth flows in the region. The summary map modifies and improves the compilation by Nilsen and Wright, which was prepared from sources available in the mid-1970's. The generalized landslide distribution shown on that map has here been improved in areas where the 1970's sources were notably deficient (Figure 1), has been extended to include Santa Cruz County, and includes the distribution of surficial deposits that define landscape not generally vulnerable to these kinds of landslides. The method of compilation and resolution of 1:125,000 (1 inch = 2 miles) limits use of the map to regional considerations. For more detailed information, see the maps listed by Pike (1997) or consult local officials or private consultants.</span></p></div></div> Landslides geoscientificInformation Landslide Mudslide Environment Disaster Polygon Env Hazard Marin County, CA Disclaimer: Marin County has attempted to verify the accuracy of the information contained in the GIS data at the time of publication. Marin County reserves the right to make changes and improvements at any time and without notice. Marin County assumes no liability for any errors, omissions, or inaccuracies in the information provided regardless of how caused. Marin County also assumes no liability for any decisions made or actions taken or not taken by the user in reliance upon any information or data furnished hereunder. THE DATA AND MAPS PROVIDED BY MARIN COUNTY ARE PROVIDED ON AN “AS IS” AND AS AVAILABLE BASIS, WITHOUT WARRANTY OF ANY KIND, EXPRESS OR IMPLIED, INCLUDING, WITHOUT LIMITATION, ANY WARRANTIES OF MERCHANTABILITY, FITNESS FOR A PARTICULAR PURPOSE, NON-INFRINGEMENT OR OTHER WARRANTIES, CONDITIONS, GUARANTEES OR REPRESENTATIONS, WHETHER EXPRESS OR IMPLIED. THE DATA ARE COMPLEX AND MAY CONTAIN NONCONFORMITIES, DEFECTS OR ERRORS. MARIN COUNTY HEREBY DISCLAIMS ANY REPRESENTATION OR WARRANTY THAT THE MARIN COUNTY GIS DATA WILL MEET YOUR NEEDS, EXPECTATIONS OR INTENDED USE, THAT THE MARIN COUNTY GIS DATA WILL BE ERROR FREE OR UNINTERRUPTED, OR THAT NONCONFORMITIES CAN OR WILL BE CORRECTED. THE GIS DATA ARE NOT SURVEY PRECISE. Use of the Marin County GIS data is at your own risk. To assist in the maintenance of the data, users are requested to provide information concerning any errors or discrepancies found when using the data to: County of Marin - GIS; email: <a href='mailto:GISProjects@marincounty.gov'>GISProjects@marincounty.gov</a> en FGDC Content Standards for Digital Geospatial Metadata FGDC-STD-001-1998 local time REQUIRED: The person responsible for the metadata information. REQUIRED: The organization responsible for the metadata information. REQUIRED: The mailing and/or physical address for the organization or individual. REQUIRED: The city of the address. REQUIRED: The state or province of the address. REQUIRED: The ZIP or other postal code of the address. REQUIRED: The telephone number by which individuals can speak to the organization or individual. 20090813 ISO 19115 Geographic Information - Metadata DIS_ESRI1.0 dataset Downloadable Data from http://pubs.usgs.gov/of/1997/of97-745/ 4.147 4.147 Vector Simple FALSE 1967 TRUE FALSE GCS_North_American_1983_HARN NAD_1983_HARN_StatePlane_California_III_FIPS_0403 coordinate pair survey feet 0.000128 0.000128 D_North_American_1983_HARN Geodetic Reference System 80 6378137.000000 298.257222 Explicit elevation coordinate included with horizontal coordinates 1.000000 NAD_1983_HARN_StatePlane_California_III_FIPS_0403 EPSG 6.3(9.0.0) 1967 PTYPE PType String 35 0 0 few landslides Author contains few, if any, large mapped landslides, but locally contains scattered small landslides and questionably identified larger landslides; defined in most of the region by excluding groups of mapped landslides but defined directly in areas containing the 'Many Landslides' unit by drawing envelopes around areas free of mapped landslides. many landslides Author consists of mapped landslides and more extensive intervening areas than in 'Mostly Landslide'; defined by excluding areas free of mapped landslides; outer boundaries are quadrangle and county limits to the areas in which this unit was defined. mostly landslide Author consists of mapped landslides, intervening areas typically narrower than 1500 feet, and narrow borders around landslides; defined by drawing envelopes around groups of mapped landslides. surficial deposits Author areas of gentle slope at low elevation that have little or no potential for the formation of slumps, translational slides, or earth flow except along stream banks and terrace margins; defined by the distribution of surficial deposits (Wentworth, 1997). water Author Polygon attribute type Author LANDSLIDE Feature Class 1967 OBJECTID OBJECTID OID 4 10 0 Internal feature number. ESRI Sequential unique whole numbers that are automatically generated. SHAPE Shape Geometry 4 0 0 Feature geometry. ESRI Coordinates defining the features. SHAPE.STLength() SHAPE.STArea() Double 0 0 0 Feature geometry. Esri Coordinates defining the features. Shape SHAPE.STLength() Double 0 0 0 Feature geometry. 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