• Journal of the Korean earth science society
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• v.28 no.2
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• pp.159-168
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• 2007

This study developed earth science learning materials based on paleolithic remains in the Youngsan River basin to provide students with curiosity and interest of science. These materials consist of four activities such as orientation, tour of museum, field trip to paleolithic sites, and making of remains. More than 60% of the teachers said that these materials are likely to improve the scientific process skills of students and also suggested that these could be applied to club activity, field trip, and homework. In addition, materials seemed to help students to understand the properties of the mineral and rock. We suggested that these materials could broaden teachers' subject of teaching in science.

• KOMUNHWA
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• no.64
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• pp.75-107
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• 2004

The Noeun-dong Paleolithic site located at the construction area of Daejeon World Cup Stadium, has been excavated two times between 1998 and 1999. The site is situated at 60-75m above sea level on a gentle slope. According to the absolute dating results a

• The Korean Journal of Quaternary Research
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• v.24 no.2
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• pp.13-21
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• 2010

The Piseo-ri site in Muan provides significant data in investigation on the Paleolithic sites in the southwest coast of Korea. Stratigraphic and geological analysis indicates that the characteristic of soil wedge can vary in accordance with soil property and relief of paleo-surface. Considering that the cultural layer was deposited after the Last Glacial Maximum, co-occurrence of the late Middle to early Upper Paleolithic stone tools suggests a possibility of redeposition of different ages resulted from active erosion. The result shows that the distribution of the Paleolithic tools and the property of soil wedge could be controlled by environmental conditions such as relief of paleo-surface and climate.

• The Korean Journal of Quaternary Research
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• v.2 no.1
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• pp.1-11
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• 1988

L'analyse des galets fractures decouverts sur les sols d'habitat de la grotto du Lazaret permet de penser que la cassure des galets se serait produite sur place dans la grotte, soit par des actions naturelles, soit par des actions des hommes prehistoriques. D'apres la comparaison des resultats obtenus par 1'etude exprimentale, les cassures des galets sont liees a plusieurs modes de fraturation. On peut seulement dire que les trois modes (1,3 et 5) sont susceptibles de donner des indications sur 1'aspect intentionnel de certains types de fracturation.

• The Korean Journal of Quaternary Research
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• v.12 no.1
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• pp.45-54
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• 1998

파주 금파리 구석기 유적에서 드러난 구덩이 유구들은 타원형이거나 약간 불규칙하 기는 하지만 타원형 또는 불규칙한 평면모양을 하고 있고 내부에 호소성 퇴적물이 보이는 경우도 있다. 그런데 내부에서 구석기 유물들이 집중 출토되어 주목된다. 이유구의 형성요인 은 현재로서 정확하지는 않지만 흐르는 물에 의해 침식이 된 흔적 거대한 나무가 쓰러지면 서 생긴 구덩이 그리고 인위적인 가공등을 들수 있는데 현재로서는 자연적으로 형성되었을 가능성이 가장 많지만 인위적인 변형이나 이용가능성을 전혀 배제 할 수는 없다. 여하간에 이러한 작업가설들 모두가 아직은 검증되지 못한 단계로 앞으로 이러한 현상에 대한 직접관 찰을 반복함으로써 설명될수 있을것으로 보이며 구덩이의 형성과정의 복원과 함께 이러한 구덩이가생길 수 있는 기후 및 지질환경의 복원은 구석기인들이 생활을 복원하는데 주용한 시사를 할 것으로 생각된다.

• 보일러설비
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• s.21
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• pp.67-78
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• 1990

한반도에 사람이 살기 시작한 것은 구석기 시대의 유물이 한반도 각지에서 발굴됨에 따라 이 시대부터라는 것이 자명한 사실로 인정된다. 그러나 이들 구석기인들이 우리의 직접적인 조상이 된다고 할 수 없는데, 구석기 시대를 뒤이은 중석기 시대의 유적발굴과, 연구의 부족으로 중석기문화에 대한 단절이 있으며 신석기 문화가 새로 생겨났기 때문이다. 따라서 현 한국인의 조상으로부터 시작되는 한국주거사, 나아가 주택난방의 시작은 당연히 신석기 시대부터 고찰해야 할 것이다. 본고는 조선시대까지의 한국전통주택건축의 난방설계를 이해케하며 이를 통하여 한국전통 생활사의 일부를 밝힌 고려대학교 주남철 교수의 논고 $ulcorner$한국의 주택난방 변천과정$lrcorner$을 전재한 것이다.

• Proceedings of the Korea Information Processing Society Conference
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• 2003.11c
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• pp.1489-1492
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• 2003

고고학자들은 발굴 후 발굴과정에서 기록된 사진, 그림, 구덩에 대한 데이터를 분석하는 것에 기초하여 연구한다. 각 데이터들은 연구자들의 연구 분야별로 석기, 식생, 지질, 유적지 및 지구 등으로 나뉘어져 있으며 한 유적지의 자료들을 각각 별도의 파일로 저장하고 있다. 따라서 현재 연구자들이 이러한 자료들을 연구에 활용한 수 있는 통합적 환경을 제공하지 못할 뿐만 아니라, 기존의 유적 및 유물들에 대한 체계적인 관리, 자료 상호간의 연관성 문제 등이 대두되고 있다. 따라서 이 논문에서는 중원지역의 구석기 유적지, 유물 및 지질 자료들을 하나의 데이터베이스로 저장하기 위한 모델링을 수행하였다. 이로 인해 기존의 개별적인 자료들을 하나의 자원으로 체계적 관리가 가능할 뿐만 아니라 각 자료들간의 상호 연관성 파악을 위한 기반을 마련한다.

• KOMUNHWA
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• no.59
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• pp.3-34
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• 2002

The researches on the prehistoric sites in Jeonnam Province started in 1970s. During 1980s and 1990s, excavations increased and their results also became larger than before. For example, the paleolithic sites were excavated along the Yeongsan River basin

• KOMUNHWA
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• no.32
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• pp.3-13
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• 1988

Stone artefacts when flaked or used retain traces. It is my objectives to analyze such traces as observed on the artefacts collected and excavated from Chongong-ni and Suyanggae sites attributed to palaeolithic ages. Observations were made with 1) naked e

• The Korean Journal of Quaternary Research
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• v.16 no.2
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• pp.9-21
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• 2002

In Korea, many open-air upper palaeolithic sites are located at the river valley, particularly exposed in gently rotting terrain along the river course. They are situated at an altitude less trail 30 m above present river bottom, and covered with the blankets of slope deposits of several meters in thickness. The purpose of this research is to eluridate depositional and vegetational environment of the alluvial upper palaeolithic Jangheung-ri sites on the basis of analytical properties of grain size population, chronology, palynology, soil chemistry and clay mineralogy and magnetic susceptibility of the Jangheung-ri Quaternary formations. The lithostratograpy of Jangheung-ri sit is subdivided into 3 layers based on the depositional sequence and radiocarbon ages. From bottom to top, they are composed of slope deposits with lower paleosol layers, young fluvial sand and gravel with backswamp organic muds, and upper paleosol layers. The upper paleosol was formed under rather dry climatic condition between each flooding period. Dessication cracks were prevalent in the soil solum which was filled with secondarily minuted fragments due to pedogenetic process. The soil structure shows typical braided-typed cracks in the root part of cracking texture, and more diversified pattern of crackings downward. The young fluvial sand gravel were formed by rather perennial streams after LGM. The main part of organic muds was particularly formed after 15Ka. Local backswamp were flourished with organic muds and graded suspension materials in the flooding muds were intermittently accumulated in the organic muds until ca. 11Ka. This episode was associated with migration of Nam River toward present course. Organic muds were formed in backswamp or local pond. Abies/Picea-Betula with Ranunculaceae, Compositae, Cyperaceae were prevalent. This period is characterized with B$\Phi$lling, Older Dryas, Allerod, and Younger Dryas (MIS-1). Stone artefacts were found in the lower paleosol layers formed as old as 18Ka-22Ka. Based on the artefacts and landscape settings of the Jangheung-ri site, it is presumed that settlement grounds of old people were buried by frequent floodings of old Nam River, the river-beds of which were heavily fluctuated laterally and river-bed erosions were activated from south to north in Jangheung-ri site until the terminal of LGM9ca 17Ka).