| snippet:
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The deep susceptibility zones were established based upon location and proximity to deep landslide deposits and head scarps, buffers along the landslide head scarps, susceptible geologic units, slope angles, and mapper judgement following protocol developed by Burns (2008) DOGAMI |
| summary:
|
The deep susceptibility zones were established based upon location and proximity to deep landslide deposits and head scarps, buffers along the landslide head scarps, susceptible geologic units, slope angles, and mapper judgement following protocol developed by Burns (2008) DOGAMI |
| extent:
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[[-123.555440044982,45.0686527455557],[-121.805044369298,46.1415923838041]] |
| accessInformation:
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|
| thumbnail:
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thumbnail/thumbnail.png |
| maxScale:
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1.7976931348623157E308 |
| typeKeywords:
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["Data","Service","Map Service","ArcGIS Server"] |
| description:
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The symbology in this map includes high and moderate susceptibility zones, with low zones exluded. The deep susceptibility zones were established based upon location and proximity to deep landslide deposits and head scarps, buffers along the landslide head scarps, susceptible geologic units, slope angles, and mapper judgement following protocol developed by Burns (2008) |
| licenseInfo:
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|
| catalogPath:
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|
| title:
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DeepSusceptibility |
| type:
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Map Service |
| url:
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|
| tags:
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["landslide"] |
| culture:
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en-US |
| name:
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DeepSusceptibility |
| guid:
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A49AFDD8-7AC0-4DC4-BFD5-6F4B9159F52C |
| minScale:
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0 |
| spatialReference:
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NAD_1983_HARN_Oregon_Statewide_Lambert_Feet_Intl |