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"Diamond Mountain" redirects here. For other uses, see Diamond Mountain (disambiguation).
Mount Kumgang
Highest point
Coordinates
Geography
Wikimedia | © OpenStreetMap
Korean name
Chosŏn'gŭl 금강산
Hancha 金剛山
Revised Romanization Geumgangsan
McCune–Reischauer Kŭmgangsan
Mount Kumgang (Korean: 금강산; RR: Geumgangsan; MR: Kŭmgangsan; lit. Diamond Mountain) or the Kumgang Moun-
tains is a mountain massif, with a 1,638-metre-high (5,374 ft) peak, in Kangwon-do, North Korea. It is located on the east coast
of the country, in Mount Kumgang Tourist Region, formerly part of Kangwŏn Province, and is part of the Taebaek mountain
range which runs along the east of the Korean Peninsula. The mountain is about 50 kilometres (31 mi) from the South Ko-
rean city of Sokcho in Gangwon-do.
Seasonal names[edit]
Japanese map of Kongō-san, or Mount Kumgang in 1939.
Mount Kumgang has been known for its scenic beauty since ancient times[1][2][3] and is the subject of many different works of art.
Including its spring name, Kŭmgangsan (금강산; 金剛山, Korean pronunciation: [kɯmɡaŋsʰan]), it has many different names for
each season, but it is most widely known today in the Korean language as Kŭmgangsan. In summer, it is called Pongraesan (봉
래산; 蓬萊山; lit. the place where a spirit dwells); in autumn, Phung'aksan (풍악산; 楓岳山; 楓骨山; lit. great mountain of colored
leaves[4]); in winter, Kaegolsan (개골산; 皆骨山; lit. stone bone mountain).
Formation[edit]
The creation of Mt. Kŭmgang is closely related to the unique climate and distinctive geological activity of the area.[5] Mt. Kŭm-
gang is a region where rain and snow fall relatively heavily, and the climate varies depending on altitude and even east-west lo-
cation.[5] The Kŭmgang geological layer is composed of several types of rocks from ancient geological periods.[6] The most widely
distributed rocks are granites of two types (mica mixed and stained), with granite-gneissic fertilization zones being formed in
some areas.[6] The rocks are transversely oriented and form a joint in various directions, forming unusual terrains and strange
rocks, which have been formed as a result of erosion for a long period of crustal activity and weathering, from 10 million years to
the present.[5][6]
Geography[edit]