• Title/Summary/Keyword: Dokdo Tourism

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A Study on Maximization of Value of Dokdo as a Tourism Destination for Marine Education (해양교육 관광목적지로서의 독도의 가치 극대화 연구)

  • Lee, Woong-Kyu
    • Journal of Digital Convergence
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    • v.17 no.8
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    • pp.171-185
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    • 2019
  • The purpose of this study was to evaluate and maximize the value of Dokdo as a marine educational tourism destination. The purpose of this study was to contribute to the identification of Dokdo as a unique territory of Korea rather than a disputed territory by further activating Dokdo tourism. The revitalization of Dokdo tourism was reviewed and analyzed from the viewpoint that it is possible when Dokdo is recognized as a destination for marine educational tourism. As a result of reviewing various research papers, periodicals, and government documents published in Korea and abroad, it is necessary to emphasize on-site education such as patriotism, anti-Japanese consciousness, and historical awareness in order to maximize value as a marine educational destination of Dokdo. Points out that it is possible to differentiate from other tourist destinations. Second, it pointed out that Dokdo preserves and develops to maximize the resource value of various tourism resources it possesses. Third, it pointed out to develop specialized tourism resources that can be linked with Dokdo tourism. Fourth, it pointed out that Dokdo will maximize its development potential as a marine educational tourism destination. Fifth, it is pointed out that there is a need to improve the educational program related to Dokdo. Finally, I pointed out that I would like to develop a variety of marine educational tourism contents and tourism programs linked with Ulleungdo.

The Problems of Dokdo's Development Policy and an Alternative for Future Development (정부의 독도개발정책 문제점과 미래대안 모색)

  • Lee, Jaeha
    • Journal of the Korean association of regional geographers
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    • v.19 no.2
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    • pp.282-300
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    • 2013
  • This study regards that a cause of intensifying sovereignty disputes between Korea and Japan over the Dokdo island has resulted from the fallacy of Dokdo's development policy directly related to exertion and consolidation of Korean government's sovereignty on Dokdo, which has been under Korea's effective control since 1953. From this internal view, this study critically reviews the Korean government's development policy for Dokdo from the 1950s to the end of July 2012 and suggests an ideal alternative for future development of Dokdo on the basis of the discussion of the problems of Dokdo's development policy and its different future development directions proposed in Korean society. The Korean government implemented quite passively the development policy for the inhabited island which is required for the consolidation of sovereignty over Dokdo not to hinder the friendly diplomatic relationship between Korea and Japan. Dokdo is currently not acknowledged as the Korea's Dokdo island in international society, but mostly called Liancourt Rocks. It may be due to the fact that Korea did not positively develop Dokdo as a valuable island which a number of Koreans can inhabit. Consequently this paper proposes 'Dokdo eco-village' as an alternative development plan from the perspective of sustainable development which the UN has adopted. It is a small scale village that contains economic function of eco-friendly fishing, eco-tourism and East Sea research. The hope is that Dokdo eco-village draft plan will be a clue to the discussion and establishment of new Dokdo's development policy to strengthen the Korea's sovereignty and effective control over Dokdo in the future.

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Variation of Allochthonous Gravels in the Beach Gravel Deposit of the Island Dokdo Natural Reserve (독도천연보호구역 해빈자갈퇴적층(몽돌 해변)의 외래 역 분포 변화)

  • Lim, Hoseong;Park, Jinsu;Kim, Jung-Hoon;Woo, Hyeon-Dong;Jang, Yun-Deuk
    • The Journal of the Petrological Society of Korea
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    • v.26 no.3
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    • pp.255-269
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    • 2017
  • Five year term monitoring investigating variation of allochthonous originated gravels are has been conducted in the beach gravel deposit of the Island Dokdo natural reserve which takes purity and uniqueness with enormous attention though a number of areas. The beach gravel deposits near the dock of the Dongdo and near the accommodation facility of the Seodo comprise various types of gravels including basalt, trachyte, and tuff from the Dokdo itself, and granite, rhyolite, gneiss, quartzite, marble, and concrete from elsewhere. The types of the allochthonous gravels on the basis of the study in 2011 and in 2016 shows no difference, so is the ranking of abundance of the allochthonous gravels; granite-concrete-gneiss in turn on the Dongdo, concrete-gneiss-granite in turn on the Seodo. Nevertheless, the relative ratio of the allochthonous gravel area against the total area is decreased. While it is suspected that the disintegrated facility and the influx of material for construction are the main 2 reasons for the contamination by allochthonous gravel, diminished total contamination ratio indicate that supervising allochthonous material has been improved; at least not worse during the 5 years. On the other hand, it is inferred that gradual influence of rockfall also has been made the gravel beach changed. Therefore, consistent rockfall investigation must be inquired.

Detailed Bathymetry and Seabed Characteristics of Wangdol-cho, Hupo Bank in the East Sea (동해 후포퇴 왕돌초 주변의 정밀해저지형 및 해저면 특성 분석)

  • Kim, Chang Hwan;Park, Chan Hong
    • Economic and Environmental Geology
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    • v.47 no.5
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    • pp.533-540
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    • 2014
  • The Wangdol-cho area, in the Hupo Bank, plays a very important role in main fishing grounds, leisure tourism and marine environmental researches of the East Sea. We analyzed the detailed bathymetry and classified the seabed characteristics of the Wangdol-cho area, based on seafloor backscattering images and sediment grain size. The Hupo Bank is developed in parallel with the eastern coastal line of Korean peninsula, and the shallowest area (Wangdol-cho) of the Hupo Bank is located along the eastern part of Hupo Port. The Wangdol-cho comprises three summits; north summit, middle summit, and south summit. The middle summit area among the three summits has the most shallow water depth with minimum about 6 m. The north summit shows about 8 m minimum depth and the south summit about 9 m. The bathymetry data around three summits represent undulating seabeds with many scattered underwater reefs and shallow water depth. The area between the underwater reefs, the flat seafloor in the northeastern part of the survey site, and the western steep slope area have relatively coarse sediments such as sandy gravel and gravelly sand. The bathymetry in the western side of the Wangdol-cho shows steep slope seabed, extending to the Hupo Basin. Fine sediments including mud and silty sand occur in the Hupo Basin area of the survey site. The submarine detailed topography and the analysis of the seafloor characteristics of the survey area are expected to contribute to management for marine environmental researches and sustainable use of ecosystems in the Wangdol-cho.