• 도로교통
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• s.78
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• pp.34-47
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• 1999

• Magazine of the Korean Society of Hazard Mitigation
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• v.3 no.1 s.8
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• pp.49-59
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• 2003

• Korean Journal of Environment and Ecology
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• v.28 no.2
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• pp.161-170
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• 2014

This study classified the types of major forest vegetation and analyzed the syngeographical characteristics of the vegetation in the Mt. Deokhang with exhumed lime rocks. The forest vegetation on the ridge of Mt. Deokhang was classified into 1 community group, 3 communities, 2 groups, and 2 subgroups, 5 types in total. The syngeographical form of Deokhangsan fully exhibited the topographical peculiarity, proximity to subalpine, and limestone zone. In addition, Carex ciliato-marginata, Carex humilis var. nana, and so forth which appear as species with high consistency in the well-drained semiarid zone represent the soil environment of the lime stone area and northern plants such as Carex ussuriensis and Asplenium ruta-muraria represent the characteristics of the vegetation in alpestrine in close proximity. Moreover, the Carpinus turczaninowii in the area appears to show the characteristics of migratory vegetation due to the peculiarity of the habitat. The syngeographical characteristics of this study area show both the characteristics of the habitat and phytogeographic characteristics. Furthermore, they are expected to contribute to the diversity in community and habitat form in Korean peninsula in terms of vegetation science.

• Journal of the Speleological Society of Korea
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• v.16 no.17
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• pp.27-33
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• 1988

석회동굴의 분포는 석회암지대에 존재하기 때문에 Karst 지형의 분포와 밀접한 관계가 있다. Karst 지형은 1893년 유고슬라비아의 J.Cvijic에 의해서 Istria에서 Kotoor지역에서 최초로 보고되었다. 세계의 주요 카르스트지형의 분포지를 보면 Yugoslavia의 Karst지방 남부, France의 Causs지방, Espania의 Andalusia지방, 그 밖에 Greece와 북부 Yucatan반도, 중앙 America의 Jamaica와 Puerto Rico와 Cuba의 북부지역 그리고 북부 Great Australian Bight 부근의 해안평야, 미국의 Florida 반도의 중부와 Great Valley, Indiana 남부 Kentucky의 각지의 Tennessee 중서부, 그리고 영국의 중앙북부인 백악지방, 중국의 화남지방, Thailand, Vietnam, Burma, Celebes 남부, Java, 일본의 추길대지방과 평미대지역 등이다.(중략)

• Proceedings of the Korean Society for Rock Mechanics Conference
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• 2007.10a
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• pp.37-46
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• 2007

• Magazine of korean Tunnelling and Underground Space Association
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• v.10 no.1
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• pp.26-30
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• 2008

• Korean Journal of Agricultural Science
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• v.6 no.2
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• pp.125-133
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• 1979

The characteristics of landslides occurred in August 5, 1979 in pyeongchangkun were surveyed and indentified as follows. 1. Deep limestone regions. Distinct differences in soil texture between A1 and B horizon could be observed on soil profile, which is attributed to the clay illuviation. The clay illuvial horizon is supposed to be an important cause of large scale mudflows on middle slopes by the lubricant action of ground water flowing between top soil and subsoil. 2. Shallow limestone regions. Very shallow top soils (less than 50cm) laid on tilted bedrock stratification provide a proper condition of mass soil movement if the top soil is saturated and ground water flows between top soil and bedrock when concentrated heavy rainfalls shower. 3. Granite regions. Weathering granitic bedrock produces very coarse textured top soils which are very cohesionless and have many pores. Therefore, the soil has high infiltration ratio and is easy to be saturated by water and to be detached from the bedrock. The landslides abrase very severely both sides of gully with high potential energy when they flow down. The following methods for landslide prevention can be recommended. 1. The original parts of landslides on top of the gully must be treated by intensive planting of deep rooting species and check dams. 2. Clear-cutting and crop planting on steep slope (more than 25 degrees) should be controlled and prohibited. 3. Establishment of landslide prevention forest should be practised on proper site.

• Journal of the Speleological Society of Korea
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• v.33 no.34
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• pp.23-29
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• 1993

온달굴은 충청북도 단양군 영춘면 하리에 소재하며 남한강이 서남류하여 굽이치는 남안의 남산 기음에 위치한다. 이 남산은 서남쪽에 하리와 박자리의 경계를 이루고 있는 남한강변에 우뚝솟은 해발고도 427m 성산의 기슭에 해당하는 구릉봉으로 석회암 지대의 산지지형인 급경사의 산세를 이루고 있다. 영춘지역의 남산 산마루를 따라 성산으로 오르면 산정 부근에서 능선을 따라 그 유명한 성산고성이 축조되어 있다. 이것이 현재 온달성으로 불리우고 있는 고성이다.(중략)

• Journal of the Speleological Society of Korea
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• v.40 no.41
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• pp.11-38
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• 1995

온달굴은 천연기념물 제261호로 1979년 6월 18일에 지정받은 문화재 동굴이다. 원래 남굴로 불리운 이 동굴은 충청북도 단양군 영춘면 하리의 남한강이 서남류하여 굽이치는 남안의 남산 기슭에 위치한다. 이 남산은 서남쪽에 하리와 백자리에 경계를 이루고 있으며 남한강변에 우뚝솟은 해발 427m 성산의 기슭에 해당하는 구릉봉으로 석회암 지대의 산지지형인 급경사인 산세를 이루고 있다.(중략)

• The Korean Journal of Ecology
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• v.25 no.3 s.107
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• pp.145-152
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• 2002

Saussurea chabyoungsanica was recorded in new species by Lim Hyoung Tak in 1997. In order to understand the entity of new species, we investigated the new distribution sites, vegetation structure and soil environmental factors. Additionally discovered distribution sites of S. chabyoungsanica were Manduckbong, Mt. Sukbyoung, Mt. Duckhang, and Sukgaejae, which were located on ridge of the Taebaek Mountains. Those sites are typical limestone zones of Korea and among them Sukgaejae belongs to lower great limestone area and Manduckbong, Mt. Sukbyoung and Mt. Duckhang belong to upper great limestone area. According to the result of phytosociological study, plant communities of S. chabyoungsanica were classified by 1 Community group, 4 Communities and 2 Subcommunities; Carex humilis var. nana-Saussurea chabyoungsanica Community group in wide sense Quercus mongolica Community group, Lespedeza maximowiczii-Saussurea chabyounsanica Community, Galium kinuta-Saussurea chabyoungsanica Community, Salvia chanryonica-Saussurea chabyoungsanica Community, Zabelia coreana-Saussurea chabyoungsanica Community. Environmental factor analysis of habitat showed that the distribution site of S. chabyoungsanica was ridge of North aspect and displayed pH $7{\sim}8$ typical of limestone. Soil moisture content was high, whereas organic matter content was low. Considering its high occurrence in sites of $1{\sim}10cm$ in soil depth, and of $30{\sim}45%$ in relative light intensity, major distribution sites were outcrops and boundaries between shrubland and forest. After community division by vegetation structure in habitat of S. chabyoungsanica, we investigated characters of soil environment by community. As a result of PCA analysis of soil sample by community, it was possible to divide community by characters of soil environmental factor. The cumulative value of contribution rate represented in second dimension space was 73% and the major factors for that value were soil texture, organic matter content and field capacity.