• 한국제4기학회지
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• 제24권1호
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• pp.11-24
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• 2010

성류굴은 전체적으로 북동-남서방향으로 하부고생대 조선누층군 탄산염암층 내에 발달하고 있는 수평동굴이며, 동굴 내 3개 구간에 규모가 큰 호수가 분포한다. 성류굴의 주굴의 길이는 약 330m, 지굴의 길이는 약 540m로 총 연장은 약 870m이며, 이중에서 수중탐사를 통해 약 85m 정도의 수중구간을 발견하였다. 성류굴 내에는 종유관, 종유석, 석순, 석주, 유석, 휴석, 동굴방패, 커튼(혹은 베이컨시트)과 일부구간에 동굴진주, 석화, 곡석, 부유방해석 등이 분포한다. 특히 수중구간 내에서도 과거에 성장하였던 동굴생성물이 발견되었으며, 물속에서 분포하는 종유석, 석순, 유석, 석주 등에서는 과거 동굴바닥을 흐르던 동굴수에 의해 침식(혹은 용식)된 흔적이 발견된다. 동굴생성물 중에서 종유석, 석순, 유석, 석주와 같은 동굴생성물은 동굴 내 물 속에서는 자랄 수 없기 때문에, 이들은 과거 동굴 내에 호수가 존재하지 않던 시기에 성장하였다가 호수물의 수위가 높아 지면서 호수 내에 잠긴 것으로 판단된다. 이러한 사실은 성류굴 내 수중구간의 동굴생성물이 과거 해수면이 낮았던 빙하기 동안에 형성되었음을 시사한다. 따라서, 이 동굴생성물에 대한 지속적인 연구는 한반도 주변의 해수면 변동과 고기후 변화를 추정하는데 매우 중요한 자료를 제공할 것으로 판단된다.

• 동굴
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• 제81호
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• pp.47-54
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• 2007

The role of the rescue party only function of accident hour relief activity it knows against the technique and an immediacy of Hum who burns executes an education and training and the accident it will be able to occur in advance and Hum activity hour which burns it prevents the place where it reduces it contributes a lot role is the importance is a possibility of saying that compared to it grows more. It must establish the cave structure commission inside Korean cave academic society and it must cooperate with the instance of the foreign nation together and with each other it must improve a cave structure setup and equipment and the countermeasure which is appropriate and prevention of accident inside the cave and accident occurrence hour it must consider feed with the fact that it must become.

• 한국제4기학회:학술대회논문집
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• 한국제4기학회 1990년도 국제심포지움 요약문
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• pp.62-62
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• 1990

No abstract, See Full-text

• The International Journal of Costume Culture
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• 제12권2호
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• pp.210-214
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• 2009

Cave 79 of Kumtura grottoes, is the best preserved cave, which has an important meaning for research on Uighur costume. This paper is intended to analyze the costume characteristics of female donors in Cave 79 by comparing image materials between Dunhuang murals and other murals in Xinjiang province. In Cave 79, female donor wears red robe with tight sleeve, whose collar is crescent-shaped decorated. Two different opinions are upheld for this decoration. One regards this as the turn-down collar, while the other believes this as decoration on V-neckline. Red robe is quite common in female donors of Xinjiang and Dunhuang murals and a female in fresco is wearing a crown in a triangle red headwear style, regarded as red silk and drooping at head. Female donors wear an extra coat, kame hair clasp, red jacket, light-colored high-waist skirt with a long-tail waistband, and tangerine Pibo (silk ribbon) with scattered small flowers. All these costume styles are commonly-used by Han females. The kame headwear is also the common ornament for Han females and the female's hairstyle is in cone shape on head by a white kame. Current costumes are similar but not completely same.

• 한국제4기학회지
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• 제17권2호
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• pp.145-148
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• 2003

The Kunang cave paleolithic site is located at Tanyang [$N37^{\circ}2'$, $128^{\circ}21'E$], Chungbuk Province, which is in the Central part of the Korean peninsula. The cave is developed at 312 amsl in a karstic mountainous area. The South Han River flows across this region and other caves can also be found near the river. The site was discovered in 1986 and excavated 3 times by the Chungbuk National University Museum until now. The cave was wellpreserved from modem human activities until the first discovery. The full length of the cave is estimated to be ca. 140 m. However, a spacious part up to 11 m from the entrance has been excavated. Eight lithological units are divided over the vertical profile at a depth of 5 m. Each unit is deposited in ascending order as follow: mud layer (Unit 9), lower complex (Unit 8) which is composed of angular blocks and fragments with a muddy matrix, lower travertine layer (Unit 7； flowstone), middle complex (Unit 6; cultural layer) which is composed of fragments with a muddy matrix, middle travertine layer (Unit 5； flowstone), yellowish muddy layer (Unit 4), upper complex (Unit 3； cultural layer) which has a similar composition to Unit 8. the upper travertine layer (Unit 2； flowstone), and finally surface soil layer (Unit 1). The most abundant vestiges in the cultural layers are the animal bones. They are small fractured pieces and mostly less than 3 cm in length. About 3,800 bone pieces from 25 animal species have been collected so far, 90 percent of them belonging to young deers. Previous archaeological study of these bone pieces shows thatprehistoric people occupied the cavenot for permanent dwelling but for temporary shelter during their seasonal hunting activity. More extensive studies of these bones together with pollen analysis are in progress to reconstruct the paleoenvironment of this cave. Only a single date (12,500 BP) obtained from a U-Th measurement of the upper travertine layer was previously available. In spite of the importance of the cave stratigraphy, there was no detail chronological investigation to establish the depositional process of the cultural layers and to understand the periodic structure of the cave strata, alternating travertine floor and complex layers. We have measured five 14C age dating (38900+/-1000, 36400+/-900, 40600+/-1600, more than 51000 and 52000 14C BP) using Seoul National University 14C AMS facility, conducted systematic process of the collagen extraction from bone fragments samples. From the result, we estimate that sedimentation rate of the cave earth is constant, and that the travertine layers, Unit 2 and Unit 3, was formed during MIS 5a(ca. 80 kBP) and MIS 5c (ca. 100 kBP) respectively. The Kunang Cave site is located at Yochonli of the region of Danyang in the mid-eastern part of Korea. This region is compased of limestones in which many caves were found and the Nam-han river flows meanderingly. The excavations were carried out three times in 1986, 1988, and 1998.

• 한국제4기학회지
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• 제4권1호
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• pp.1-13
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• 1990

두루봉 흥수굴에서 홍적세 시기에 속하는 어린아이뼈 화석이 남한에서는 처음으로 발굴되었다. 이 화석은 흥수아이로 이름지어졌고, 몇 개의 돌연모가 함께 발굴되었다. 유적지의 정확한 연대는 아직 밝혀지지 않았으나 동물화석에 따르면 후기 홍적세 따뜻한 시기로 여겨진다. 흥수아이뼈들의 크기를 측정하고 해부학상 특징을 밝혔다. 이 아이는 약5살로 여겨지고, 머리부피는 1260㏄에서 1300㏄ 사이에 속하며, 키는 약 110에서 120cm 정도이다. 머리뼈는 길이와 높이가 아주 크며, 특히 위머리뼈의 굽은길이는 매우 길다. 흥수아이의 머리뼈는 동북 아시아에서 발굴된 화석인류 및 현대 인류와 비교되었는데, 흥수아이 화석은 "해부학상 현대인 또는 해부학상 슬기사람"으로 분류된다.t;으로 분류된다.

• 한국제4기학회지
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• 제19권2호
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• pp.68-69
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• 2005

• 한국제4기학회지
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• 제1권1호
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• pp.47-67
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• 1987

우리나라 구석기시대에 보편적인 것으로 알려진 동굴입구나 움푹 들어간 바위절벽밑의 바위그늘을 이용한 주거지 유적이 제주도 신석기시대 이후까지 상당한 기간 지속되었음이 발견되었다. 그러나 그후 청동기시대에서 철기시대에 이르러 이러한 주거지는 캠핑지역으로 변한 증거가 있다. 그런데 제주도에는 해안가와 하천에 따라 동굴입구 또는 용암턴넬이 많이 발달하여 화산도로서의 특징이 있으며 이들이 선사시대의 인류에 의하여 사용된 것이 특기할 만하다.

• 한국지형학회지
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• 제27권4호
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• pp.53-70
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• 2020

Silgyeong sansuhwa (Realistic landscape paintings) are drawn in Korea since 17th century. It has characteristics of more realistic description of landscape than painting from previous periods. Kim Hong Do's 'Haedong Myeongsan docheop (The album of paintings of famous mountains in Korea)' has been recognized as fine example of realistic description of geomorphic landscapes. Kim Hong Do and Kim Eung hwan did official travel to Gwandong and Geumgangsan area by order of King Jeongjo in 1788. As a result of that travel they draw about 100 piece of landscape painting. About 60 pieces of the paintings are still remaining. These are open to public by Korea National Museum in 1996. 14 pieces of painting, Daegwanryeong and Gangneung, Gyeongpo-dae, Hohae-jeong, Gahak-jeong, Cheonggan-jeong, Mun-am, Mangyang-jeong, Wolsong-jeong, Neungpa-dae, Naksan-sa, Mureung-gye, Gyejo-gul, and Hyeonjong-am, are analysed in this study. Coastal depositional landforms, like lagoon, sand beach and spit or barriers, erosional forms, like sea stack, sea cliff and sea cave, depicted in the paintings are analysed. In addition, structural landforms, colluvial landform and bedrock incision form by the running water in mountain area were analysed and weathered forms of granite and excursion to karst cave also discussed. It is found that sea arch in the printing destroyed since 1788, though exact position and reason is still unknown. There are strong need for discovery and identification of geomorphic landscape resources, for applied geomorphological studies and for prepare educational materials for non-face-to-face education. It also be emphasized that it can be used of the course work materials for future education using augmented reality and virtual reality technology.

• 한국제4기학회지
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• 제25권1호
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• pp.41-49
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• 2011

고대의 인간거주의 흔적을 확인하기 위하여 중부 내륙의 석회암 지대인 평창, 단양, 진천, 괴산, 제천, 문경, 보은, 상주 등지에 대한 조사에서 모두 고고학적으로 기조사된 동굴 6개소 및 31개소의 동굴이 지표조사 되었다. 조사는 주로 입지와 퇴적층의 유무 그리고 문화유물의 부존가능성에 대한 확인을 포함하였다. 조사된 동굴 중에서 평창의 광천선굴이나 문경의 모산굴을 비롯한 11개소가 퇴적층의 잔존상황이나 토기나 동물 뼈 등의 유물의 산포상황으로 미루어 고고학적으로 의미가 있을 것으로 보이며 이 중에 문경 모산굴은 크기나 내부의 퇴적층 그리고 발견된 토기로 미루어 고고학적인 가치가 분명하게 확인되었다. 이러한 새로운 자료는 그동안 이 지역에서 조사된 인간거주의 증거들과 함께 구석기시대 이래의 생활사를 잘 보여줄 것으로 기대된다.