• Title/Summary/Keyword: 오음산

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The Vascular plants of Mt. Myeongu, Mt. Ouem(Jukwang-myeon, Gosung-gun, Gangwon-do) in the vicinity of the DMZ (DMZ일원 명우산, 오음산(강원도 고성군 죽왕면)의 관속식물상)

  • Hwang, Hee-Suk;An, Jong-Bin;Bak, Gippeum;Park, Jinsun;Kim, Sang-Jun;Lee, Ahyoung;Song, Jin-Heon;Yun, Ho-Geun;Jung, Ji-Young;Jung, Su-Young;Kim, Il-Kwon;Shin, Hyun-Tak;Lee, Cheol-Ho
    • Proceedings of the Plant Resources Society of Korea Conference
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    • 2019.04a
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    • pp.76-76
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    • 2019
  • 본 연구에서는 강원도 고성군 죽왕면 구성리에 위치한 명우산(335.5m)과 오봉리에 위치한 오음산(281.7m) 일대를 중심으로 식물상을 조사하였다. 명우산의 관속식물은 72과 203속 236종 4아종 23변종 3품종으로 총 239분류군이 조사되었고, 오음산의 관속식물은 71과 185속 236종 2아종 31변종 3품종으로 총 257분류군이 조사되었다. 주요 식물로 명우산의 경우 특산식물은 노랑갈퀴(Vicia chosenensis), 백운산원추리(Hemerocallis hakuunensis) 등 4분류군이 조사되었고, 이는 명우산에서 조사된 식물의 1.67%로 특산식물 360분류군(정규영 등, 2017)의 1.1%에 해당된다. 오음산의 경우 특산식물은 노랑갈퀴(Vicia chosenensis), 새며느리밥풀(Melampyrum setaceum var. nakaianum) 2분류군이 조사되었고, 이는 오음산에서 조사된 식물의 0.78%, 특산식물 360분류군(정규영 등, 2017)의 0.56%에 해당된다. 희귀식물로는 명우산은 확인되지 않았고, 오음산은 위기종(EN)인 참작약(Paeonia lactiflora var. trichocarpa) 1분류군이 확인되었다. 침입외래식물로는 명우산의 경우 단풍잎돼지풀(Ambrosia trifida), 미국쑥부쟁이(Aster pilosus) 등 총 10분류군이 확인되었고, 오음산의 경우 미국실새삼(Cuscuta pentagona), 돼지풀(Ambrosia artemisiifolia) 등 총 12분류군이 확인되었다.

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Flora of the vascular plants of Oeumsan Mountain (Hongcheon-gun and Hoengseong-gun, Gangwon-do) (오음산(강원, 홍천 및 횡성)의 관속식물상)

  • KIM, Kyung-Ah;CHEON, Kyeong-Sik;YOO, Ki-Oug
    • Korean Journal of Plant Taxonomy
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    • v.48 no.1
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    • pp.48-64
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    • 2018
  • This study was carried out to investigate the flora of Oeumsan Mountain (Hongcheon-gun and Hoengseong-gun, Gangwon-do) from March of 2016 to September of 2017. The vascular plants were summarized into 509 taxa, including 98 families, 301 genera, 436 species, 4 subspecies, 57 varieties and 12 forms. Among the 509 investigated taxa, 9 Korean endemic, 1 endangered plant, 8 rare plants and 57 floristic regional indicator plants were also included. The naturalized plants encompassed 35 taxa. The percentage of naturalized plants species and the urbanization index were estimated to be 6.9% and 10.9%, respectively.

A study on landforms in Gosung, Gangwon province (강원도 고성 일대의 지형 경관에 대한 연구)

  • Kim, Jong Yeon
    • Journal of The Geomorphological Association of Korea
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    • v.18 no.3
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    • pp.65-81
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    • 2011
  • The landforms based on granite and basalt in Gosung, Gangwon province were analysed. Some part of this area experienced volcanic activities while most of the area was experiencing erosion of weathered mantle(saprolites) of mesoic granites during cenozoic period. Two different lithologies affect the mode of landscape evolution. The basalt covers the mountain tops as a 'cap rock' with flat surfaces. It shows relatively fresh rock surface with cliff or steep slops at the boundary with weathered granite. The blocks detached from the cliff accumulated at the foot of the cliff(talus) or moved and filled the valley(block streams). These debris slopes cover the deeply weathered granites. In the case of Oeum Mt. and Duibaekjae, the number of point of origin of the basalt flow is not clear. The orientation of blocks from block stream coincides with slope aspects and it can be assumed that the bolcks were moved by solifluction. The landscape change of the block streams are dominated by removal of weathered material from beneath of the valley rather than removal of bedrock blocks themselves.

Flora of Wonju-Hoengseong Area (원주.횡성 지역의 식물상)

  • Ko, Sung-Chul;Son, Dong-Chan;Kim, Hyun-Jong;Hwang, Hee-Suk;Shin, Young-Hwa
    • Korean Journal of Plant Resources
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    • v.22 no.5
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    • pp.365-380
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    • 2009
  • Flora of vascular plants in mountains located at Wonju-si and Hoengseong-gun areas such as Chiak-san(1,288m), Taegi-san(1,261.4m), Obong-san(1,126.2m), Eungbong-san(1,094.9m), Eodab-san(789.4m), Deokgo-san(521.2m), Deokga-san(700.5m) and Seongji-bong(791m) was investigated from April, 2008 to May, 2009, and results from the previous researches in which voucher specimens had been presented from Balgyo-san(998.4m), Oeum-san(930.4m), Baekun-san(1,037.1m) and Chiak-san(1,288m) were included in the list of vascular plants from these areas. This investigations resulted in 804 taxa consisted of 680 species, 1 subspecies, 111 varieties, and 12 forms of 383 genera under 97 families, and totally in 973 taxa (21.14% of all vascular plants in Korea) of 818 species, 1 subspecies, 138 varieties and 16 forms of 418 genera under 105 families on addition of voucher specimens in the previous researches. Forests of the investigated areas were generally mixed of Pinus densiflora and deciduous trees. The areas with comparatively excellent vegetation were valley from Guryong-sa (temple) to Biro-bong (summit) via Seryeom-pokpo (fall) in Mt. Chiak-san, and Keunseong-gol (valley) and eastern slope from Taegibungyo-teo to Naksu-dae (fall) in Mt. Taegi-san. 10 families with abundantly collected species were Compositae, Graminae, Rosaceae, Ranunculaceae, Leguminosae, Cyperaceae, Liliaceae, Saxifragaceae, Umbelliferae and Labiatae in order, and they occuied 49.12% of all collected taxa. Endemic plants found in these areas were 38 taxa including Hanabusaya asiatica, Megaleranthis saniculifolia, and Pyrus ussuriensis var. diamantica, and rare and endangered ones were 24 taxa including Hanabusaya asiatica, Viola websteri, Viola diamantica, and Patrina saniculaefolia. Specially designated plants by the Ministry of Environment were 88 taxa including 12 taxa of 5th degree such as Woodsia intermedia, Hanabusaya asiatica, Equisetum pratense, Iris koreana, Lilium cernum, Trillium tschonoskii, Magnolia kobus(cultivated), Gastrodia elata, Polypodium virginianum, Cimicifuga heracleifolia, Megaleranthis saniculifolia and Viola websteri. 47 taxa of alien plants were found. As to 609 taxa (13.23% of all vascular plants in Korea) of useful plants, 334 taxa for the edible, 269 taxa for the medicinal, 127 taxa for the ornamental, 332 taxa for the forage, 3 taxa for the industrial raw material, 31 taxa for the timber and 13 taxa for the fiber were classified, respectively.

The Formation of the Cenozoic Volcanic Edifice in the Goseong-Ganseong Area, Gangwondo, Korea (강원도 고성-간성일대의 신생대 화산체의 형성과정)

  • Kim, Hwa Sung;Kil, Youngwoo;Lee, Moon Won
    • Journal of the Korean earth science society
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    • v.33 no.7
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    • pp.627-636
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    • 2012
  • In the Obongri-Goseong area of Gangwondo, South Korea, there are six densely distributed volcanic edifices i.e., Duibaejae, Oeumsan, Galmibong, 249 m height, 166 m height, and 102 m height, and two other volcanic edifices including Goseongsan and Unbongsan volcanic edifice that are separately located from a distance. A previously undiscovered 249m volcanic edifice in Obongri was found in this investigation, and the six volcanic edifices distributed in Obongri will be referred to as the Obongri volcanic edifice group. Volcanic edifices in this area were interpreted by other researchers as being volcanic plug, plug dome, and cylindrical volcanic pipe type edifices. The aim of this study is to investigate the aspect of volcanic activity in the Obongri-Goseong area and the formation of volcanic edifices by examining of the shape of volcanic edifices, stratigraphy, and characterization of volcanic products. All the volcanic edifices in the area are composed of basaltic rocks on the Mesozoic granite basement, and the prevalence of the dome shape increased towards the upper part of the mountain. Three volcanic edifices (Duibaejae, 166 m height, 102 m height) include intercalated pyroclastic deposits between the basaltic rocks and the basement. The pyroclastic deposit in the Duibaejae volcanic edifice is composed of quartz, feldspar, granite fragments originated from the basement, and scoria fragments originated from the volcanic eruption. In addition to angular olivine, plagioclase, and pyroxene xenocrysts, all the basaltic rocks contained mantle xenolith, gabbroic xenolith originated from the lower crust, and granitic xenolith originated from the basement. This fact indicates that magma rapidly rose to the surface and that the volcanic activity was explosive. It is also interpreted that, as the basaltic magma became highly viscous due to the large amount of xenocrysts, the erupted magma formed a dome structure on the surface. The original dome structure was then severely eroded out leaving a plug dome formation on the basement.