• Plant Resources
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• v.6 no.1
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• pp.57-75
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• 2003

This study was performed to investigate the flora and plant resources of Mt. Woosanbong (537.8 m) from April to October 2002. The collected vascular plants were composed of all 389 taxa including cultivated species, and classified into 329 species, 2 subspecies, 53 varieties, and 5 forms of 248 genera under 81 families. Six taxa of the Korean endemic plants and 4 taxa of the rare and endangered plants were also distributed in this mount. Resource plants were categorized into edible 181, pasturing 160, medicinal 136, stainable 94, ornamental 77, timber 22, fiber 5 and industrial 4 taxa, respectively. Floristic geography of the investigated area was regarded as the boundary between middle and southern parts in floristic pattern of the Korean Peninsula.

• Economic and Environmental Geology
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• v.14 no.3
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• pp.123-142
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• 1981

Granitic complex in the Woosanbong area is composed of schistose granite, two-mica granite, biotite granite, porphyritic granite and pink feldspar granite in order of intrusion. In their boundary aspects, the gradational change between porphyritic granite and pink feldspar granite is observed in field relations. All the granites of the complex are classified to quartz monzonite by the modal compositions following Bateman's classification (1961) with the exception of pink feldspar granite which belongs to granite according to the petrographical classification. The first three granites are characterized by highly development of vein and/or lens-like pegmatites in their bodies, and two others contain green hornblende uniquely. These leucocratic two-mica granite shows an unusual character in ratio of muscovite to biotite 1: 0.7 to 1:13, and contains dominantly microcline. The content of muscovite varies in places in the field. Under the polarizing microscope it is revealed that the muscovite flakes occur as the products altered from biotite partly or completely, and it usually associates with chlorite flakes nearby. These features, therefore, suggests that biotite probably has been altered to muscovite and chlorite by hydration during deuteric processes. At the same stage, sericitization of plagioclase by the hydrolytic decomposition, and transformation of orthoclase to microcline may be taken place. Accordingly, it is obviously permissible to consider the two-mica granite as a kind of 'apo-granite' by deuteric alterations during the consolidation of magma.

• The Korean Journal of Ecology
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• v.25 no.5
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• pp.297-303
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• 2002

This study was carried out to analyze forest vegetation of Gabhasan and Woosanbong in Daejeon, Employing the releve method of TWINSPAN, 62 plots were sampled from June 2001 to September 2001. Field survey carried out to examine importance value, to do diameter of breast height(DBH) measurement, and to analyze the Ordination. The Forest vegetation was classified into four communities: Quercus mongolica community, Pinus densiflora community, Quercus variabilis community, Quercus acutissima community. The importance value of Pinus densiflora, Quercus variabilis, Quercus mongolica, Quercus serrata and Styrax japonica were high. According to DBH analysis, Pinus densiflora and Quercus variabilis dominate currently, however, importance value of Quercus mongolica, Quercus serrata, Prunus sargentii would increase in the future. The result of ordination analysis, showed that Quercus mongolica community was located in high altitude and steep area, Pinus densiflora community was located in comparatively high altitude and medium slope area, Quercus variabilis community was located in low altitude and gentle slope area and Quercus acutissima community was located in the lowest altitude and relatively gentle slope area.