GIS Data Catalog

Landslide Hazards along River Corridors - Rock fall potential

View in GIS Open Data

Learn how to use GIS Open Data 🗺

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.


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.

Domain

Sequential unique whole numbers that are automatically generated.

LiDAR_Sour

From King County

Description

Source LiDAR imagery and date imagery data sent to Author

Domain

KC GIS 2015

MapDate

From King County

Description

Date Author completed mapping

Domain

2015

MapMethod

From King County

Description

Method to map rock fall potential

Domain

CONEFALL method

MapBy

From King County

Description

Author of mapped shapes

Domain

KC_DNRP

Shape

From Esri

Description

Feature geometry.

Domain

Coordinates 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.

Domain

Double

Shape.STLength()

From SQL Server

Description

Returns the total length of the elements in a geometry instance.

Domain

Double


Contact information

Maintained by DNRP - Water and Land Resources
Primary Harkeerat Kang

Harkeerat.Kang@kingcounty.gov


Terms of Use

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