GIS Data Catalog
Landslide Hazards along River Corridors - Rock fall potential
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Summary
Suitable for general reference and analyses.
Identifies only rock fall potential along the river corridor within the study limits in King County.
Description
Rock fall is a type of landslide that occurs in bedrock where single or multiple rocks are dislodged and fall from steep cliff faces.
In a typical alpine setting, cliffs are located on the upper slopes of a mountain with a talus below, extending to the base of the mountain.
The talus is composed of rocks that have fallen from the cliff face and accumulate below the cliff.
The talus marks the limit of most rock fall from the cliff, but a few boulders that fall from the cliff travel beyond the toe of the talus.
It is these outliers that can pose a hazard to adjacent development (see figure "b" below).
Rock fall can be triggered by earthquakes, freeze-thaw cycles, or severe weather.
Tumbling boulders falling from a cliff face are fast moving and can level virtually anything in their path.
Layer information
| Layer Name | lsr_rf_rockfallpotential_area |
| Subject Category | Environment |
| Title | Landslide Hazards along River Corridors - Rock fall potential |
| Feature Count | 150 |
| Feature Type | Polygon |
| Next Update | None planned |
| Spatial reference | EPSG:2926 |
| Control ID | 2564 |
| Place Keywords | Pacific NW, King County, WA, Washington State |
| Theme Keywords | Enviro, Pacific NW, King County WA, Washington State, Landslide, Slide, Mass Movement, Landslide Hazard Mapping, Debris Slides, Shallow Landslides, Shallow Landsliding, Debris Sliding |
| Supplemental Information |
The CONEFALL software program was used to implements this approach in a GIS environment to map areas where rock fall could propagate downslope from a source. As a starting point for the CONEFALL program, cliff-faces were identified to delineate the line representing the base-of-cliff/top-of-talus. Within the study limits, these lines were mapped based on professional judgement using a variety of tools in a GIS environment including vertical orthophotography, oblique photography, and slope mapping. Slopes inclined at more than 200 percent were especially identified. |
Table Preview
Attribute information
|
OBJECTID
From Esri |
Description
Internal feature number. DomainSequential unique whole numbers that are automatically generated. |
|
LiDAR_Sour
From King County |
Description
Source LiDAR imagery and date imagery data sent to Author DomainKC GIS 2015 |
|
MapDate
From King County |
Description
Date Author completed mapping Domain2015 |
|
MapMethod
From King County |
Description
Method to map rock fall potential DomainCONEFALL method |
|
MapBy
From King County |
Description
Author of mapped shapes DomainKC_DNRP |
|
Shape
From Esri |
Description
Feature geometry. DomainCoordinates defining the features. |
|
Shape.STArea()
From SQL Server |
Description
Returns the area of a geometry instance in square units, based on the spatial reference identifier (SRID) of the geometry. DomainDouble |
|
Shape.STLength()
From SQL Server |
Description
Returns the total length of the elements in a geometry instance. DomainDouble |
Contact information
| Maintained by | DNRP - Water and Land Resources |
| Primary |
Harkeerat Kang
Harkeerat.Kang@kingcounty.gov |
Terms of Use
| License | Terms of use and copyright |
Use this Data
|
Links
How to use in ArcGIS Pro |
|
| Sharing Status | Public |
Summary
Suitable for general reference and analyses.
Identifies only rock fall potential along the river corridor within the study limits in King County.
Description
Rock fall is a type of landslide that occurs in bedrock where single or multiple rocks are dislodged and fall from steep cliff faces.
In a typical alpine setting, cliffs are located on the upper slopes of a mountain with a talus below, extending to the base of the mountain.
The talus is composed of rocks that have fallen from the cliff face and accumulate below the cliff.
The talus marks the limit of most rock fall from the cliff, but a few boulders that fall from the cliff travel beyond the toe of the talus.
It is these outliers that can pose a hazard to adjacent development (see figure "b" below).
Rock fall can be triggered by earthquakes, freeze-thaw cycles, or severe weather.
Tumbling boulders falling from a cliff face are fast moving and can level virtually anything in their path.
Contact information
| Maintained by | DNRP - Water and Land Resources |
| Primary |
Harkeerat Kang
Harkeerat.Kang@kingcounty.gov |
Terms of use and copyright
| License | Terms of use and copyright |