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dc.contributor.authorMol, Lisa
dc.contributor.authorGrenfell, Michael
dc.date.accessioned2023-06-05T09:23:38Z
dc.date.available2023-06-05T09:23:38Z
dc.date.issued2022
dc.identifier.citationMol, L., & Grenfell, M. (2022). Influence of landscape moisture sources and topography on rock weathering patterns associated with wildfire. Earth Surface Processes and Landforms, 47(7),1761–1777. https://doi.org/10.1002/esp.5345en_US
dc.identifier.issn1096-9837
dc.identifier.urihttps://doi.org/10.1002/esp.5345
dc.identifier.urihttp://hdl.handle.net/10566/9009
dc.description.abstractFrom 9 March 2015, a wildfire burned an area of 25.7 km2, or approximately half of the Jonkershoek catchment (Western Cape, South Africa), over the course of 3 days. During this period, large areas of fynbos and commercial forest plantations were razed, and rocks, including boulders and smaller rocks, were exposed to high temperatures. While a substantial body of work has been carried out to investigate the effects of wildfire on landscape development, less is known about the effect of wildfire on rock weathering within a landscape. Previous studies have reported the overall effect of wildfire on rock deterioration, but the effect of intra-fire temperature differences associated with heat behaviour on a slope has not been sufficiently addressed. In this study we investigate the effects of topography and proximity to moisture on rock deterioration processes.en_US
dc.language.isoenen_US
dc.publisherWileyen_US
dc.subjectClimate changeen_US
dc.subjectTopographyen_US
dc.subjectWildfireen_US
dc.subjectGeographyen_US
dc.subjectGeoscienceen_US
dc.titleInfluence of landscape moisture sources and topography on rock weathering patterns associated with wildfireen_US
dc.typeArticleen_US


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