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Postfire Airborne LiDAR Point Cloud and Terrain Models for the Bolt Creek Fire, Washington (NSF RAPID)
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| Type: | Resource | |
| Storage: | The size of this resource is 1.6 GB | |
| Created: | Feb 27, 2026 at 2:12 a.m. (UTC) | |
| Last updated: | Feb 27, 2026 at 7:59 a.m. (UTC) | |
| Citation: | See how to cite this resource | |
| Content types: | Single File Content Geographic Raster Content |
| Sharing Status: | Public |
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| Views: | 525 |
| Downloads: | 57 |
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Abstract
The Bolt Creek Fire started on September 10, 2022 and has burned ~14,600 acres of steep forested land within the North Cascade Range in northwestern Washington State (confluence of the Beckler and South Fork Skykomish rivers). Nearly 90% of the burned area has local slopes greater than 15 degrees, which is an approximate lower limit for saturated landslide initiation in cohesion-less soils. Most of the steep upland slopes (generally >30 degrees) and moderately steep mid-slopes (15 - 30 degrees) bear high and moderate soil burn severity levels. Several landslides were reported in the region in the winter of 2025. This resource publishes raw airborne LiDAR point clouds from surveys conducted in 2022, 2024, and 2025, and digital surface models (DSM) and bare earth DTMs obtained from airborne LiDAR. The resource are organized in folders that contain the original (raw) point cloud, filtered point cloud products, spatial boundaries, and multiple raster surfaces derived from the Lidar, including digital surface models (DSM), digital terrain models (DTM), a USGS reference DEM used for coregistration, and a DEM difference product for each LiDAR survey block. These include a composite data for a large downstream portion of Eagle Creek, two post landslide surveys, and a clearcut region where fire first started. The data provide evidence for post-fire geomorphic response in the cool and wet western slopes of the Cascades.
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Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
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| U.S. National Science Foundation | RAPID: Monitoring postfire geomorphic response on humid slopes | NSF 2303870 |
Contributors
People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.
| Name | Organization | Address | Phone | Author Identifiers |
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| NSF RAPID Facility | University of Washington | 3760 E Stevens Way NE, Seattle, WA 98195 |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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