• Journal of the Speleological Society of Korea
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• no.81
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• pp.55-74
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• 2007

지하전철은 고비용 구축에 의한 대량 수송의 실적에도 불구하고 현실적으로 고액의 적자행정에서 벗어나지 못하고 있다. 선진국에서는 비용과 효율성을 위하여 지하전철선호에서 지상 모노레일로 급격한 변화를 가져오고 있다. 특히 경량화에 의한 첨단기술력에서 생산되는 고급 모노레일 카의 쾌적성, 친환경적, 경제성, 저소음, 저오염, 국지적 효율성 등에 의한 유비쿼터스 사회에 기여될 수 있는 최적의 조건을 가지고 있으므로 향후 지자체 위주의 행정에 의한 재정자립도의 확보를 위한 관광지의 개발에 관련된 천연성 지형지물, 인문성 문화제, 조경성 예술분야 등에 효자 상품으로 등극할 것이다. 이에 따라 정책적인 조정에 필요한 법제도 및 지방 조례 등의 조정으로 특색 있고 미래지향적인 모노레일 카의 정책방안의 설정이 시급하다. 특히 지정학적으로 3면이 바다로 위호되어 있고 중국, 러시아, 일본 등의 열강 국들에 육교적인 지정학적인 최상의 관광 및 첨단 한류문화의 교류의 니치성 상품의 활성화로 상대적으로 작지만 큰 경제적인 효과를 가져 올 수 있는 신 수송환경에 적극적인 행정과 민의의 접점에 교두보적인 수송의 르네상스 개념이 필요하다.

• Proceedings of the Korean Society of Disaster Information Conference
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• 2015.11a
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• pp.221-223
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• 2015

해방70년을 맞이하는 차원에서 일제강점기 동안에 조선인 강재징용으로 구축된 진지갱도(신주백, 2003)에 대한 구조물의 분포와 활용에 대한 내역을 규명하고(황석규, 2006), 일제에 의하여 자행된 국토훼손의 실상 및 만행을 확인하여 분류하는데 있다. '한반도는 일제강점기 일본 제국의 군사요새였다'(이완희, 2014)고 제시하였듯이 조사탐사의 범위는 전국을 대상으로 하며, 진지갱도지역에 대한 3-D LiDAR 기법에 의한 도면작성으로 붕괴위험에 처한 진지동굴의 분포, 형상, 내용 등의 분석으로 문화재적 측면의 보전위한 기록물 구현방안에 있다.

• The Korean Journal of Quaternary Research
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• v.25 no.1
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• pp.41-49
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• 2011

Archaeological survey has been carried out to find some evidence of human occupation in 31 caves in Pyeoungchang, Danyang, Jincheon, Goesan, Munkyoung, Boeun, Sangju in central limestone area of the Korean peninsula. Among those caves, some archaeological evidences were observed in 11 caves. Various types of potteries, animal bones and stone artifacts were collected on surface of sediments in caves. Among them, the Mosan cave in Munkyoung and the Kwangcheonseongul in Pyeoungchang are very likely to yield important archaeological remains in the well preserved deposits in the caves. Further researches are expected to provide significant information for explaining human living from prehistoric time to historical periods.

• The Journal of Engineering Geology
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• v.30 no.3
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• pp.327-345
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• 2020

The effects of ground vibration on lava tubes during construction were studied to aid design of management and preservation measures for lava tubes. Ground conditions were assessed by RMR (Rock mass rating) and Q-system classifications for the Geomunoreum lava tubes, and vibration velocity was measured during in situ blasting tests in the Manjanggul and Yongcheondonggul lava tubes. Results indicate that the higher the rock quality, the greater the effect of vibration, although there is no clear linear relationship due to ground heterogeneity. A relationship derived between vibration velocity (PPV) and intensity (dB(V)) on the basis of blasting tests indicates that a vibration level of < 0.285 cm/sec meets the regulatory limit of 0.371 cm/sec and 65 dB(V) during daytime, and 0.285 cm/sec and 60 dB(V) during night. For blasting vibrations, square- and cube-root scaled distances are linearly correlated, with R² ≥ 0.76. On the basis of this correlation, explosive-charge weights meeting the 0.2 cm/sec vibration criterion for cultural heritage were estimated to be 2.88 kg at 50 m distance, and 11.52 kg at 100 m.

• 한국문화재보존과학회:학술대회논문집
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• 2002.02a
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• pp.8-11
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• 2002

• Korean Journal of Heritage: History & Science
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• v.46 no.1
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• pp.290-317
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• 2013

The objectives of this study are to investigate the natural heritage and scientific value of various geosites on Udo Island, and to evaluate the sites as natural monuments and as world natural heritage properties. Udo Island includes a variety of geoheritage sites. Various land forms formed during the formation of the Someori Oreum formed by phreatomagmatic eruptions. The essential elements for the formation of Udo Island are the tuff cone, overflowing lava and overlying redeposited tuff sediments. Various coastal land forms are also present. About 6,000 years B.C., when sea-level rose close to its present level due to deglaciation since the Last Glacial Maximum, carbonate sediments have been formed and deposited in shallow marine environment surrounding Udo Island. In particular, the very shallow broad shelf between Udo Island and Jeju Island, less than 20 m in water depth, has provided perfect conditions for the formation of rhodoids. Significant amounts of rhodoids are now forming in this area. Occasional transport of these rhodoids by typhoons has produced unique beach deposits which are entirely composed of rhodoids. Additional features are the Hagosudong Beach with its white carbonate sands, the Geommeole Beach with its black tuffaceous sands and Tolkani Beach with its basalt cobbles and boulders. Near Hagosudong Beach, wind-blown sands in the past produced carbonate sand dunes. On the northern part of the island, special carbonate sediments are present, due to their formation by composite processes such as beach-forming process and transportation by typhoons. The development of several sea caves is another feature of Udo Island, formed by waves and typhoon erosion within tuffaceous sedimentary rocks. In particular, one sea cave found at a depth of 10 m is very special because it indicates past sea-level fluctuations. Shell mounds in Udo Island may well represent the mixed heritage feature on this island. The most valuable geoheritage sites investigated around Udo Isalnd are rhodoid depostis on beaches and in shallow seas, and Someori Oreum composed of volcanoclastic deposits and basalt lava. Beach and shallow marine sediments, composed only of rhodoids, appear to be very rare in the world. Also, the natural heritage value of the Someori Oreum is outstanding, together with other phreatomagmatic tuff cones such as Suwolbong, Songaksan and Yongmeori. Consequently, the rhodoid deposits and the Someori Oreum are worth being nominated for UNESCO World Natural Heritage status. The designation of Someori Oreum as a Natural Monument should be a prerequisite for this procedure.

• Journal of the Speleological Society of Korea
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• no.64
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• pp.61-80
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• 2004

This book deals with a .gesture of photography as a Political phenomena. In the gesture of photography, the conceptions that influences the cause and the policy of solutions that conflict the cultures, are developed. The contents of this book contains lots of items, and efforts to find the root of the digital revolution of nowadays.

• Proceedings of the Speleological Society Conference
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• 1995.08a
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• pp.86-86
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• 1995

I. 동해시의 개요 II동해시 연혁 1. 1632년 $\longrightarrow$북평땅에 박곡리부락 발생 2. 1948년 $\longrightarrow$묵호땅에 망상리 발달 3. 1941년 $\longrightarrow$묵호항(동해항구)개항 4. 1975년 $\longrightarrow$산업기지개발구역지정(500만평) 5. 1979년 2월 $\longrightarrow$북평항구개항 6. 1980년 4월 $\longrightarrow$묵호읍과 부평읍을 통합하여 동해시 승격 7. 1981년 4월 $\longrightarrow$일본국 쯔루가 항구도시와 자매결연 8. 1986년 12월 $\longrightarrow$북평항을 국제항구도시 동해항 개칭 9. 1993년 $\longrightarrow$중국 도문시와 자매결연 10. 1995년 $\longrightarrow$동해항은 동해안(남한)제1가는 국제항구(중략)

• Proceedings of the Speleological Society Conference
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• 1995.08a
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• pp.83-83
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• 1995

1. 동해시는 동해 바다에 면하고 있는 항구도시. 2. 한반도의 중부 동해안에 위치하고 있는 해항도시. 3. 동해 바다를 통하여 세계 각지로 자유왕래 할 수 있는 편리한 위치에 있는 항구도시. 4. 남북 경제 문화 교류때에는 육해산물, 산업물자의 수송에 편한 해항도시. 5. 일본지역에서 중국, 러시아 지역에의 해로는 한반도의 동해시 항구를 경유하여야하는 교통 입지에 있는 해항. \circled1 일본에서 중국, 러시아에의 직항해로는 가능하나 여객 운송의 경우 30시간 이상의 장시간 소요가 불가피하므로 동해시 해항이 중간 거점이 될 수 있다. \circled2 일본의 서남 지방에 있는 후꾸오카의 하까다항 그리고 중부지방 북안에 있는 쯔루가항으로 부터 중국 대륙과 러시아 연해주에의 해로인 경우는 반드시 동해시항에 기항하여야 한다. 6. 남한의 내륙 지방에서 동북아시아 권역에 직접 연결이 가능한 위치에 있는 해항. 7. 인접지에 다양한 발전적 배경을 지니고 있는 해항 도시.

• Korean Journal of Heritage: History & Science
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• v.42 no.1
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• pp.20-39
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• 2009

Abstract This research is a comparative study on the geological natural monuments of South and North Koreas. The classification system on natural monuments between South Korea and North Korea is similar, but North Korea's designations are relatively well-balanced. The geology field of South Korea was composed of rocks, caves, fossils and general geology, whereas that of North Korea was subdivided into rocks, fossils, strata, mineral springs, hot springs, geography, waterfalls, lakes, caves and pools. Unlike South Korea, North Korea designates and preserves geological structures such as fold and fault, and representative outcrops of mine. It is suggested that South Korea has to establish natural monument management policies for preserving geological structures and outstanding outcrops of mine. The 47-year period of preserving natural monuments in South Korea was divided into the stages I (1962~1980), II (1981~1995) and III (1996~2008). The designated numbers of geological natural monuments in the stage I, II and III average 1.1, 0.1 and 2.6, respectively. The number of geological natural monuments in South Korea is highest in Jeju province, whereas that in North Korea is highest in Gangwon province. This implies that natural monuments have been well protected especially in the locality of slow urbanization.