4.7 Article

FIRE AND FOREST HISTORY AT MOUNT RUSHMORE

Journal

ECOLOGICAL APPLICATIONS
Volume 18, Issue 8, Pages 1984-1999

Publisher

WILEY
DOI: 10.1890/07-1337.1

Keywords

dendroecology; fire behavior; fire frequency; fire history; fire severity; forest structure; ponderosa pine; reference dynamics; restoration ecology

Funding

  1. Joint Fire Science Program
  2. National Park Service
  3. Rocky Mountain Tree-Ring Research

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Mount Rushmore National Memorial in the Black Hills of South Dakota is known worldwide for its massive sculpture of four of the United States' most respected presidents. The Memorial landscape also is covered by extensive ponderosa pine (Pinus ponderosa) forest that has not burned in over a century. We compiled dendroecological and forest structural data from 29 plots across the 517-ha Memorial and used fire behavior modeling to reconstruct the historical. re regime and forest structure and compare them to current conditions. The historical. re regime is best characterized as one of low-severity surface fires with occasional (> 100 years) patches (< 100 ha) of passive crown fire. We estimate that only similar to 3.3% of the landscape burned as crown fire during 22 landscape fire years ( recorded at >= 25% of plots) between 1529 and 1893. The last landscape. re was in 1893. Mean. re intervals before 1893 varied depending on spatial scale, from 34 years based on scar-to-scar intervals on individual trees to 16 years between landscape. re years. Modal. re intervals were 11 - 15 years and did not vary with scale. Fire rotation ( the time to burn an area the size of the study area) was estimated to be 30 years for surface fire and 800+ years for crown. re. The current forest is denser and contains more small trees, fewer large trees, lower canopy base heights, and greater canopy bulk density than a reconstructed historical (1870) forest. Fire behavior modeling using the NEXUS program suggests that surface fires would have dominated. re behavior in the 1870 forest during both moderate and severe weather conditions, while crown fire would dominate in the current forest especially under severe weather. Changes in the fire regime and forest structure at Mount Rushmore parallel those seen in ponderosa pine forests from the southwestern United States. Shifts from historical to current forest structure and the increased likelihood of crown fire justify the need for forest restoration before a catastrophic wild fire occurs and adversely impacts the ecological and aesthetic setting of the Mount Rushmore sculpture.

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