• (The)Study of the Eastern Classic
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• no.56
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• pp.9-33
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• 2014

This paper aims to look into text of Toegye Lee Hwang's poem Cheongryangsan (Mt. Cheongryang). For that, the poetic aspects of experiences in staying in mountains presented in the poem were classified into materialistic aspect, a method of subject proposal, subject recognition and orientation to examine such aspects, and their respective meanings and limits were considered. First, from the materialistic aspect, the poem about Mt. Cheongryang can be divided into a case of materializing acts in Mt. Cheongryang and a case of materializing an individual scenery of Mt. Cheongryang itself. Second, from an aspect of methods of subject proposal, the poem can be divided into a case in which the space of Mt. Cheongryang is proposed syntagmatically and abstractly and a case in which each scenery is proposed by it being divided partially. Third, from an aspect of subject recognition and orientation, in case Mt. Cheongryang is realized as a solitary space separated far from the world, poetic self aims at reflection. However, in case Mt. Cheongryang is realized as a space for staying with friends and disciples, poetic self aims at communication. The above-mentioned difference is caused by the fact that Toegye had such an experience in Mt. Cheongryang twice at the interval of 10 years. This study is significant in that it intensively looked into Toegye' experience in Mountains and the poetic text which have not been studied and that Toegye's recognition and orientation of a space were discriminatively revealed.

• The Journal of the Petrological Society of Korea
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• v.26 no.3
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• pp.167-181
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• 2017

Cheongryangsan area ($49.51km^2$) has been designated as the Provincial Park in 1982, because it has magnificent aspect and seasonally spectacular landscapes. Especially, Cheongryangsa sitey ($4.09km^2$) has been designated as Noted Scenery No. 23 in 2007, because it has the same topographical landscape as rock cliffs, rock peaks and caves. The most spectacular landscapes are exhibited in the Cheongryangsan Conglomerate and Osipbong Basalt. There are twelve rock peaks on the ridges of the two strata, and many rock cliffs in the several valleys of strata, in which a few caves are formed by differential weathering and erosion. The valleys, in which flow Cheongryang, Bukgok and Cheonae streams, are classified as fault valleys along WNW-ESE faults. The rock cliffs were generated from vertical joints parallel to WNW-ESE faults in the two strata, and the caves were formed by differential weathering and erosion along bedding of sandstones and shales intercalated in the conglomerates. The rock peaks are landscapes formed by differential erosion along crossed vertical joints in the ridges. The vertical joints are developed subparallel to two WNW-ESE faults and a NNE-WWS fault. Therefore the topographical features are caused by existence of the faults and Lithologic difference in the Cheongryangsan Conglomerate and Osipbong Basalt, and by differential weathering and erosion along them.

• Journal of the Korean association of regional geographers
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• v.11 no.1
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• pp.54-70
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• 2005

The purpose of this study is to clarify motives, itinerary and general patterns associated with the traveling of the upper class in the Chosun Dynasty based on twenty travel accounts of Mt. Chungryang. In addition, previous studies were referred to in order to compare these trips to Mt. Chungryang with those which were undertaken to Mt. Kumgang so as to identify the unique characteristics of those involved with the trips to Mt. Chungryang and of these trips in themselves. Through this process, unique characteristics, such as the travelers' academic backgrounds and place of origin, as well as how these travelers' relationship with their teachers influenced the motivation for these trips were uncovered, as were the processes through which travel schedules and companions were selected. Moreover, the researcher identified similarities and differences between the travel of Mt. Chungryang and Mt. Kumgang in terms of the travelers' motivation for the trip, the transportation methods they employed, and the kind of accommodation they sought. Moreover while similarities were also uncovered with regards to the travel practices of the literati class during this time, differences emerged in terms of their travel dates and schedules.

• Journal of the Korean Geographical Society
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• v.44 no.3
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• pp.260-281
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• 2009

This study analyzed people's travels to Mt. Jiri in the Joseon Dynasty; and more specifically, the purpose of such travels and the methods used to do so. Using previous studies dealing with travels to Mt. $K\breve{u}mgang$ and Mt. Chungryang under taken by Joseon people, this study strived to extrapolate the characteristics of the travelers who visited Mt. Jiri, the motivation for their travels, the journey itself, and the style of travel employed. As a result of this exercise, those who traveled to Mt. Jiri were found to exhibit common characteristics in terms of aspects such as their area of residence, personalities, and hobbies. As these were naturally reflected in their travels, the motivation for such trips, as well as the journey to Mt.Jiri itself, tended to differ from those associated with travels to Mt. $K\breve{u}mgang$ and Mt. Chungryang. As far as the style of travel was concerned, the study focused on such aspects as the length of the trip, preparations, nature of the companions, transportation, meals and accommodations, as well as the activities carried out during the travel itself. Here, the comparison with the travelers to Mt. $K\breve{u}mgang$ and Mt. Chungryang revealed no significant differences.

• Proceedings of the Korean Institute of Landscape Architecture Conference
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• 2011.10a
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• pp.91-93
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• 2011

• The Journal of the Petrological Society of Korea
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• v.18 no.3
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• pp.181-194
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• 2009

The Cheongryangsan Formation was reported to stratigraphically overlie the Gasongdong Formation and underlie the Dogyedong Formation in the northern part of the Yeongyang subbasin, and be divided into the lower Cheongryangsan Member and the Osipbong Member. But the members have more widely called as the Cheongryangsan Conglomerate and the Osipbong Basalt, because the latter have initially meant that thin basalt flows several times intercalate sedimentary rocks in the northern part but later must consider that they have a very dominant volume in the eastern one. Both formations are based on classifying the stratigraphy and play a role of an excellent key bed for stratigraphic correlation between local spaces in the subbasin dominant absolutely for reddish beds. Both formations play a role of excellent key bed in the northern and northwestern areas of the subbasin; the Osipbong Basalt, the midwestern, eastern and southern ones; the Cheongryangsan Conglomerate, the southeastern one.

• 공원문화
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• s.19
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• pp.5-24
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• 1981

• Proceedings of the Zoological Society Korea Conference
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• 1994.10a
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• pp.129.1-129
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• 1994

• 수목보호
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• s.2
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• pp.23-25
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• 1996

• Proceedings of the KGS Conference
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• 2005.05a
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• pp.183-184
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• 2005