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An Aspect of Weathering Progress Based on Physical and Chemical Properties of Tafoni in the Simgok Area of Gangneung, Korea

강릉 심곡 해안에 발달한 타포니의 물리·화학적 특성에 기초한 풍화 진행 양상

  • Kim, Yu Jung (Department of Geography Education, Seoul National University) ;
  • Kim, Jong Yeon (Department of Geography Education, Chungbuk National University) ;
  • Kim, Jong Wook (Department of Geography Education, Seoul National University) ;
  • Han, Min (Geo-Environmental Hazards & Quaternary Geology Research Center, Korea Institute of Geoscience and Mineral Resources)
  • 김유정 (서울대학교 지리교육과) ;
  • 김종연 (충북대학교 지리교육과) ;
  • 김종욱 (서울대학교 지리교육과) ;
  • 한민 (한국지질자원연구원 지질환경재해연구센터)
  • Received : 2018.09.05
  • Accepted : 2018.09.22
  • Published : 2018.09.30

Abstract

In this study, we surveyed weathering progressing aspect by major elements variation and rock hardness by using XRF analysis, schmidt hammer, and thin section analysis. This observation suggested that the weathering process is likely to develop differently according to microstructural characteristics. R-value on the inside wall are lower than those on the outside. Also, the shadier the environment was, the closer it was to inshore areas, the R-value appeared to be lower. The movement of the elements such as Ca, Na and K shows that feldspar is hydrolyzed and can form salt crystallization like a gypsum or halite when they combine with the elements such as S or Cl. It proved a high CaO, $Na_2O$ and $K_2O$ content on flaking inside wall and rock meal. The exfoliation was mainly observed along the shady backwall and ceiling of tafoni. This helped in predicting the growth of tafoni as well as the direction of its progress.

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