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Postfire Airborne LiDAR Point Cloud and Terrain Models for the Bolt Creek Fire, Washington (NSF RAPID)
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| 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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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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Content
README.txt
# Postfire Airborne Lidar Point Cloud and Terrain Models for the Bolt Creek Fire, Washington ## Overview This dataset contains post-fire airborne Lidar point clouds and derived terrain models for the Bolt Creek Fire burn area in Washington State. Data were collected using an uncrewed aerial system (UAS) and processed to support post-fire geomorphic, hydrologic, and hazard analyses, including terrain change assessment relative to a pre-event reference elevation model. The resource is organized into folders corresponding to individual Lidar acquisitions. Within each folder, users will find 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. ## Data Contents This directory contains three folders corresponding to Lidar acquisition areas, and an additional folder which contains upsampled (10m) data of the largest survey block. Each folder includes the following data products: 1. Raw Lidar Point Cloud (BoltCreek_ULS_L1_X_YYYYMMDD.laz) Unfiltered LAS/LAZ files containing all returns from the UAS Lidar survey, including ground, vegetation, structures, and noise. These files represent the closest form of the data to the original sensor output and were used as input for subsequent filtering and terrain modeling. Note that for the largest survey block, the point cloud was upsampled to 50cm by the producers to improve data manageability. 2. Filtered Lidar Point Cloud (BoltCreek_ULS_X_YYYYMMDD_filtered.laz) LAS/LAZ files derived from the raw point cloud with vegetation and noise returns removed. These filtered point clouds were used to generate surface models and reduce artifacts associated with non-ground features. 3. Lidar Boundary (BoltCreek_ULS_X_YYYYMMDD_Boundary.zip) A polygon dataset defining the spatial extent of the Lidar acquisition. This boundary was used to clip raster products and constrain comparisons to areas where Lidar data are present. 4. Digital Surface Model (DSM) (BoltCreek_ULS_X_YYYYMMDD_DSM_1m.tif) A raster DSM generated from the filtered Lidar point cloud, representing the elevation of the uppermost surfaces captured by the Lidar without vegetation and noise filtering. The DSM was produced using triangulated interpolation and is provided at high spatial resolution. 5. Digital Terrain Model (DTM) (BoltCreek_ULS_X_YYYYMMDD_DTM_1m.tif) A raster DTM derived from the filtered Lidar point cloud using ground classification and filtering. The DTM represents bare-earth elevations and was used to characterize post-fire terrain conditions. 6. USGS Reference DEM (BoltCreek_ULS_X_USGS_Reference_DEM_1m.tif) A pre-event digital elevation model obtained from the U.S. Geological Survey and reprojected and clipped to match the Lidar boundary. This reference DEM provides a baseline for terrain comparison and change analysis. 7. DEM Difference (BoltCreek_ULS_X_YYYYMMDD_DTM_1m_BoltCreek_ULS_X_USGS_Reference_DEM_1m.tif) A raster representing the elevation difference between the post-fire Lidar-derived DTM and the USGS reference DEM. Positive values indicate areas where the Lidar-derived surface is higher than the reference surface, and negative values indicate lower elevations. This product is intended to support qualitative and quantitative assessment of post-fire surface changes. All raster products are spatially aligned and clipped to the Lidar acquisition boundary to ensure consistency across datasets. ## Spatial Reference (GeoTiff/Shapefiles) Horizontal CRS: NAD83 / UTM Zone 10N EPSG code: 26910 Units: meters Vertical datum: NAVD88 Vertical units: meters ## Spatial Reference (LAS/LAZ) Horizontal CRS: NAD83(2011) / Washington North EPSG Code: 6596 Units: meters Vertical datum: NAVD88 EPSG Code: 5703 Units: meters Geoid: GEOID18 EPSG Code: 6319 (EPOCH 2010) ## LAS/LAZ Coordinate Reference System (CRS) Definition (WKT) COMPOUNDCRS["Compound CRS NAD83(2011) / Washington North + North American Vertical Datum 1988 + PROJ us_noaa_g2018u0.tif",PROJCRS["NAD83(2011) / Washington North",BASEGEOGCRS["NAD83(2011)",DATUM["NAD83 (National Spatial Reference System 2011)",ELLIPSOID["GRS 1980",6378137,298.257222101,LENGTHUNIT["metre",1]]],PRIMEM["Greenwich",0,ANGLEUNIT["degree",0.0174532925199433]],ID["EPSG",6318]],CONVERSION["unnamed",METHOD["Lambert Conic Conformal (2SP)",ID["EPSG",9802]],PARAMETER["Latitude of false origin",47,ANGLEUNIT["degree",0.0174532925199433],ID["EPSG",8821]],PARAMETER["Longitude of false origin",-120.833333333333,ANGLEUNIT["degree",0.0174532925199433],ID["EPSG",8822]],PARAMETER["Latitude of 1st standard parallel",48.7333333333333,ANGLEUNIT["degree",0.0174532925199433],ID["EPSG",8823]],PARAMETER["Latitude of 2nd standard parallel",47.5,ANGLEUNIT["degree",0.0174532925199433],ID["EPSG",8824]],PARAMETER["Easting at false origin",500000,LENGTHUNIT["metre",1],ID["EPSG",8826]],PARAMETER["Northing at false origin",0,LENGTHUNIT["metre",1],ID["EPSG",8827]]],CS[Cartesian,2],AXIS["easting",east,ORDER[1],LENGTHUNIT["metre",1,ID["EPSG",9001]]],AXIS["northing",north,ORDER[2],LENGTHUNIT["metre",1,ID["EPSG",9001]]]],VERTCRS["North American Vertical Datum 1988 + PROJ us_noaa_g2018u0.tif",VDATUM["North American Vertical Datum 1988",ID["EPSG",5103]],CS[vertical,1],AXIS["gravity-related height",up,LENGTHUNIT["metre",1]]]] ## Temporal Information BoltCreek_ULS_All_20240624_28 acquisition date(s): 2024-06-24 to 2024-06-28 BoltCreek_ULS_A_20250904 acquisition date(s): 2025-09-04 BoltCreek_ULS_B_20250904 acquisition date(s): 2025-09-04 ## Processing Workflow Point cloud processing included the following steps: 1. Noise and outlier removal 2. Ground point classification 3. Classification refinement and quality control 4. Rasterization Final DEM products derived from this point cloud were generated using TIN-based interpolation following reprojection to a common CRS. ## Point Cloud Characteristics BoltCreek_ULS_All_20240624_28 Platform: Airborne Lidar Survey Area: 6.08 km2 Points (Raw): 45,082,512 Points (Filtered): 4,009,878 BoltCreek_ULS_A_20250904 Platform: Airborne Lidar Survey Area: 0.22 km2 Points (Raw): 61,035,548 Points (Filtered): 165,266 BoltCreek_ULS_B_20250904 Platform: Airborne Lidar Survey Area: 0.17 km2 Points (Raw): 72,377,247 Points (Filtered): 215,900 ## Data Quality & Limitations - Dense canopy and steep terrain may result in localized ground gaps. - Some slope-adjacent triangulation artifacts may occur in derived surfaces. - Data are intended for research and analysis purposes and are not survey-grade. ## Usage Notes Users should ensure that vertical datums and projections are consistent before differencing this dataset with other elevation products. ## Software Primary processing software: - PDAL - CloudCompare - QGIS ## Software Citations CloudCompare (version 2.13.1) [GPL software]. (2026). Retrieved from http://www.cloudcompare.org/ PDAL Contributors, 2022. PDAL Point Data Abstraction Library. https://doi.org/10.5281/zenodo.2616780 Shean, D. E., O. Alexandrov, Z. Moratto, B. E. Smith, I. R. Joughin, C. C. Porter, Morin, P. J., An automated, open-source pipeline for mass production of digital elevation models (DEMs) from very high-resolution commercial stereo satellite imagery, ISPRS J. Photogramm. Remote Sens, 116, 101-117, doi: 10.1016/j.isprsjprs.2016.03.012, 2016. Zhang W, Qi J, Wan P, Wang H, Xie D, Wang X, Yan G. An Easy-to-Use Airborne LiDAR Data Filtering Method Based on Cloth Simulation. Remote Sensing. 2016; 8(6):501.
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Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
|---|---|---|
| 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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