• 한국의류학회지
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• 제32권10호
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• pp.1559-1570
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• 2008

Since brought into from the economic life of nomads, the felt, the target of this study, has been developed in various ways of giving the functions of class symbol as well of protection against the cold and of ornamentation. Therefore, the study on how the felt was developed in Joseon Dynasty and how different culture from nomadic tribes it formed is significant in comprehensively under,;landing the economic, social and natural environmental factors in the Dynasty. The felt named "Jeon" has been constantly appearing in Korea from the ancient time, but it was not produced actively in the early part of Joseon Dynasty. That's why it was not a climatic condition suitable for sheep-breeding, and the government managed sheep-breeding but it aimed primarily at not producing clothing materials but having memorial ceremonies. Since sheep-breeding was not widely spreaded, production of Jeon was limited and some part was imported from China, so it was one of rare valuable goods. Therefore, the felt of wools named "Yangmojeon", the colored felt named "Chaejeon", etc. were used as liking items in the high-class society, and their materials and components were a little different depending on the official post. On the other hand, people in the low-class society used to wear the felt hats made of cattle feathers and miscellaneous fur, named "Jeonlip" and "Beougeoji". Since the middle of Joseon Dynasty, use of the felt was divided into two groups according to the users and the function, along with successful spreading of cotton and development of market economy. The function of Jeon to protect against the cold was replaced by cotton, but the felt hats of Beongeoji, Jeonlip, etc. were worn by common people continuously. As seen above, it is considered that the felt culture in Joseon Dynasty was formed very differently from the nomadic culture, because of its historical and sociocultural characteristics, and it had unique developing progress among all available fabrics.

• 한국석유지질학회지
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• 제2권2호
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• pp.71-81
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• 1994

선상지 삼각주는 흔히 깊은 분지로 전진하여 급경사의 전면층을 형성한다. 현생의 급경사 선상지-삼각주는 사태흔적, 츄트/협곡, 스웨일(swale), 로브(lobe), 스플레이(splay). 및 암설낙하(debris fall) 등의 표층 지형에 의해 특징지워진다. 이들은 강하구에서 발생하는 퇴적물 붕괴나 중력류에 의해 생성된다. 고기의 선상지-삼각주 퇴적상은 경사가 급한 전면층과 비교적 경사가 완만한 기저층 및 전삼각주(prodelta)층을 구성한다. 이는 다시 판상 또는 쐐기 모양의 역암 및 사암, 사태 충진층, 츄트/협곡 충진층, 판상층, 열편층, 사태층 등으로 구성된다.