Frost-weathering control on the rate of late Quaternary landscape evolution, western flank of the Taebaek Mountain Range, Korea: a case of passive margin landscape evolution. Issue 4 (2nd October 2022)

• Record Type: Journal Article
• Authors: Kim, Dong-Eun; Seong, Yeong Bae; Weber, John; Yu, Byung Yong
• Is Part Of: Geografiska annaler. Volume 104:Issue 4(2022)
• Page Start: 245
• Page End: 267
• Publication Date: 2022-10-02
• Subjects: Geomorphic equilibrium -- cosmogenic 10Be -- catchment-wide denudation rate -- topographic parameter -- divide migration -- frost cracking; Physical geography -- Periodicals; 551.4
• DOI: 10.1080/04353676.2022.2121998
• Languages: English
• ISSNs: 0435-3676

Abstract

ABSTRACT: Passive continental margins can show anomalously high topography and exhibit a discrete steep escarpment, divide, and gentle slope from the exterior to the interior of the margin. Compared with active (i.e. convergent and strike-slip) tectonic regions, the processes and rates of change of high-altitude landscapes driven by tectonics and/or climate in tectonically inactive (passive) continental margins are poorly understood. We used 10 Be catchment-wide denudation rates of fluvial sands (n = 29) collected in 17 catchments and 12 sub-catchments, as well as topographic analysis, to quantify the rate of landscape change along the western flank of the Taebaek Mountain Range (TMR). The denudation rates range from ∼20 to ∼70 mm/ka. These rates show no significant difference between upstream and downstream areas, implying that denudation is not (or is only negligibly) affected by deep-seated mass wasting processes and human impact. 10 Be denudation rates in the northern TMR are 1.6 times higher than in the south. In addition, the relationship between denudation rates and geomorphic parameter values also differs from north to south. These observed spatial differences in the rate of denudation and geomorphic response can be explained by intense frost weathering rather than lithological control. Our quantitative analysis of denudation rates and topography suggests that southwest-directed migration of the range's main divide occurs and that the range's western flank (low relief) is likely to be in a geomorphic state of quasi-equilibrium whereas the eastern flank (steep) still remains transient.