184:
feldspar, mica, and opaque minerals, and show foliations. Quartz are mainly made out of 70 - 80% of framework grains and the upper parts of the formation are formed by fauna of the middle Middle
Cambrian. The occurrence of fine sandstone layers is suggestive of deposition in relatively shallow to deep-water environments (Chough 93). Sambangsan Formation consists of a lot of light grey, green or brown, massive or thick-bedded sandstone (upper part) and red or green shale and sandy shale. Extreme tribes of Middle Cambrian age occur in light brown, thin-bedded medium to coarse-grained, micaceous sandstone beds in the upper part of the formations (Chough 22).
183:
The
Sambangsan Formations has diverse homogeneous, purple, to greenish gray fine sandstone and siltstone. Sandstones are generally massive, greenish gray, and fine grained, showing small-scale bands and are poorly to moderately sorted (Chough 90). They are mainly composed of fine to very fine quartz,
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242:"Chough, Sung Kwun. "Geology and Sedimentology of the Korean Peninsula." Google Books. Elsevier, 2013. Web. 07 Mar. 2016.
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175:. It has an elevation of 980 m (3,215 ft).
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226:한국의 산 여행 (Travel Guide to Korean Mountains)
263:Mountains of Gangwon Province, South Korea
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16:Mountain in Gyeonggi Province, South Korea
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159:) is a mountain in the counties of
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228:. Seoul: 관동 상억연구회 (Kwandong).
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19:For mountain in Seogwipo, see
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194:List of mountains in Korea
44:980 m (3,220 ft)
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258:Mountains of South Korea
224:Yu Jeong-yeol (2007).
114:Revised Romanization
34:Highest point
235:978-89-958055-1-0
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173:South Korea
161:Pyeongchang
153::
68:Korean name
58:South Korea
252:Categories
218:References
169:Gangwon-do
147:Sambangsan
134:Sampangsan
120:Sambangsan
29:Sambangsan
21:Sanbangsan
49:Geography
40:Elevation
188:See also
165:Yeongwol
54:Location
179:Geology
232:
151:Korean
74:Hangul
200:Notes
90:Hanja
230:ISBN
163:and
171:in
156:삼방산
81:삼방산
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149:(
104:山
101:芳
98:三
23:.
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