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International Journal of Wildland Fire International Journal of Wildland Fire Society
Journal of the International Association of Wildland Fire
RESEARCH ARTICLE

Accelerated weathering of carbonate rocks following the 2010 wildfire on Mount Carmel, Israel

N. Shtober-Zisu A E , N. Tessler B , A. Tsatskin C and N. Greenbaum D
+ Author Affiliations
- Author Affiliations

A Department of Israel Studies, University of Haifa, Mount Carmel, Haifa, 3498838, Israel.

B Department of Biology and Environment, University of Haifa, Mount Carmel, Haifa, 3498838, Israel.

C Department of Archaeology, University of Haifa, Mount Carmel, Haifa, 3498838, Israel.

D Department of Geography and Environmental Studies, University of Haifa, Mount Carmel, Haifa, 3498838, Israel.

E Corresponding author. Email: nshtober@research.haifa.ac.il

International Journal of Wildland Fire 24(8) 1154-1167 https://doi.org/10.1071/WF14221
Submitted: 15 December 2014  Accepted: 12 July 2015   Published: 12 November 2015

Abstract

Massive destruction of carbonate rocks occurred on the slopes of Mount Carmel during the severe wildfire in 2010. The bedrock surfaces exhibited extensive exfoliation into flakes and spalls covering up to 80–100% of the exposed rocks; detached boulders were totally fractured or disintegrated. The fire affected six carbonate units – various types of chalk, limestone and dolomite. The burned flakes show a consistent tendency towards flatness, in all lithologies. The extent of the physical disruption depends on rock composition: the most severe response was found in the chalk formations covered by calcrete (Nari crusts). These rocks reacted by extreme exfoliation, at an average depth of 7.7 to 9.6 cm and a maximum depth of 20 cm. Scorched and blackened faces under the upper layer of spalls provide strong evidence that chalk breakdown took place at an early stage of the fire. It is possible to explain the extreme response of the chalks by the laminar structure of the Nari, which served as planes of weakness for the rock destruction. Three years after the fire, the rocks continue to exfoliate and break down internally. As the harder surface of the Nari deteriorates, the more brittle underlying chalk is exposed to erosion.

Additional keywords: calcrete, exfoliation, Nari, post-fire weathering, shattering, spalls.


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