Landform recognition in granite mountains in East Asia (Seoraksan, Republic of Korea, and Huangshan and Sanqingshan, China) – a contribution of geomorphology to the UNESCO World Heritage
Vol. 37 No. 1 (2018), Articles
Vol. 37 No. 1 (2018)

Landform recognition in granite mountains in East Asia (Seoraksan, Republic of Korea, and Huangshan and Sanqingshan, China) – a contribution of geomorphology to the UNESCO World Heritage

Articles
https://doi.org/10.2478/quageo-2018-0008
Published 09.01.2019
Piotr Migoń
Department of Geomorphology, Institute of Geography and regional Development, University of Wrocław, Poland
Kyung-Sik Woo
Department of Geology and Geophysics, Kangwon National University, Chuncheon, South Korea
Marek Kasprzak
Department of Geomorphology, Institute of Geography and regional Development, University of Wrocław, Poland
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Keywords

granite geomorphology
rock control
mass movements
bedrock channels
World Heritage

How to Cite

Migoń, P., Woo, K.-S., & Kasprzak, M. (2019). Landform recognition in granite mountains in East Asia (Seoraksan, Republic of Korea, and Huangshan and Sanqingshan, China) – a contribution of geomorphology to the UNESCO World Heritage. Quaestiones Geographicae, 37(1), 103–115. https://doi.org/10.2478/quageo-2018-0008
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Abstract

Applied research in geomorphology includes landform analysis and evaluation from a specific perspective of scientific significance and global relevance. In this paper, landform diversity of Seoraksan, Republic of Korea, a UNESCO World Heritage candidate, is compared with geomorphic characteristics of two World Heritage properties in China, Huangshan and Sanqingshan. Seoraksan represents an almost complete mountain geomorphic system of considerable contemporary dynamics, with outstanding scenery and spectacular landforms such as domes, fins, bedrock channels, waterfalls, and inherited block fields. It is argued that Seoraksan contains outstanding scientific and aesthetic values, not present at the Chinese properties, offering scope for successful nomination.
https://doi.org/10.2478/quageo-2018-0008
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