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독도 서도 및 동도 남부 해안의 파식대 지형 발달

Geomorphological Development of Shore Platforms at Dongdo and Seodo in the Southern Coast of Dok-do Island

  • 황상일 (경북대학교 지리학과.경북대학교 울릉도.독도연구소) ;
  • 권용휘 (경북대학교 지리학과.경북대학교 울릉도.독도연구소) ;
  • 윤순옥 (경희대학교 지리학과)
  • Hwang, Sangill (Department of Geography, Kyungpook National University.Institute for Dok-do and Ulleung-do Island) ;
  • Kwon, Yong-whuy (Department of Geography, Kyungpook National University.Institute for Dok-do and Ulleung-do Island) ;
  • Yoon, Soon-Ock (Department of Geography, Kyung Hee University)
  • 투고 : 2019.12.12
  • 심사 : 2019.12.20
  • 발행 : 2019.12.30

초록

The shore platforms at Dok-do could be an important and clear indicator showing dimensional reduction of Dok-do. Especially flat type shore platforms are distributed in the southern coast of Dok-do island, composed of weak rocks against erosional resistance like interbedded lapilli tuff and massive tuff breccia. The distribution of shore platform is partially related to the wind direction at Dok-do island. The primary SW- and secondary SE winds are representative among wind directions at Dok-do, maintaining from spring to the autumn. Therefore, wide shore platforms could be developed by waves approaching from SW and SE directions in the southern coast of Dok-do. The sea stacks like Gunham-rock, Neopdeok-rock, Keungaje-rock and Jakeungaje-rock on the western coast are also considered to be formed by wave erosion from the SE direction. The shore platforms in the southern coast of Dok-do island were developed since ca. 7,000 yr. BP, when sea level raised almost to the present level. The average extension speed of shore platform was calculated to 4.0mm/y, because the broadest shore platform with the width ca. 28m was extended for ca. 7,000 years. The width's dimension of shore platform at Dok-do reflects a slow extension rate in the present, although erosional process will be faster with the sea level rise in the future.

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과제정보

이 논문은 2016년도 정부(교육부)의 재원으로 한국연구재단의 지원을 받아 수행된 기초연구사업임(No. 2016R1A6A1A05011910).