낙동강 상류지역의 지형분류에 관한 연구 = A Study of Landform Classification in the Upper Stream Area of the River Nackdong

다국어 초록 (Multilingual Abstract)

I. Statement of Problem
In the field of geography, the study of landform classification which is one of the most important factors on applied topography has been taken notice of these days.
Since 1956, the I.G.U. applied topography committee leaded by the director, Cailleux, Tricart has had a great influence on the applied topography and in August of 1960, I.G.U. Stockholm committee started the applied study of geography and the study has been developed on the world. At the London committee in 1964, by the resuilts of applied landform study for 4 years, the applied study of geography is discussed at the international committee. Since 1964, the applied topography committee has set up two sectional meeting for the landform classification map and the river enterprise. When the landform classification meeting made a big scale map, the common applied map used for every country is tried to be made. The team for making the map was formed and the landform classification map of a middle size scale of the whole europe was tried to be made.
In Japan, the landform classification map, the landform classification map for flood prevention, land condition map and other map were made by the Geography Survey Institute and the Ministry of Construction. The common and foundamental work made through that kind of map is to classify the land form. The sudden development of the topography and the applied topography and the study of landform classification for the land and the area exploition plan are prevalent widely now.
II. Significance of Study
The study of this field in Korea is inactive. Therefore the construcion enterprise plan brings about a failure. On the related books for the topography, it might be said that there was no one about the relief energy map and the summit level map which were written systematically by Korean topographer. Those maps made by foreign topographer are used without criticism in Korea today. Therefore, the aims of this study are;
(1) About the area of the northern parts of Yungnam district, a) Summit Level Map, b) Relief Energy Map, c) the Stage in Cycle of croson, d) Land Construction Map are made by the size of 1/50,000 scale landform map. those are used not only for the materials of this study but also for the materials of learning of landform classification.
(2) This study is intended to state clearly the coordinates of applied topography for the development of our country to choose the main industry area and to just life envirnment, as the materials of exploition and maitain for the River Nackdong.
(3) The upper area of the River Nackdong in the northern parts of Yungnam district is studied mainly in this paper and its resuilt is intended to be analyzised and estimated to classify the landform of the whole Yungnam district.
(4) With a view to finding out the different points of the area, this study will conclude to set up a small area and will be a pre-study to classify the perfect landform of the upper stream area of the River Nackdong.
III. Method of Study
(1) The Area for this Study The main area for this study is the upper stream area of the River Rackdong and related area of some parts of Chungbuk and Gangwon Provinces over Mts. Sobaek and of the east-side of Mts. Taebaek. The area of district, the sheet name of landform map by the scale 1/50,000, the name of main place, the water-vein, and the boundary of country and provinces are shown in the Fig. (1).
(2) Morphometry The showing of conclusion of morpho-map drawn perfectly by satistics of morphometry and numerical value on the map of 1/50,000 scale size is the characterics and value of this study.
(a) Drawing up the Summit Level Map The map about the whole area is drawn pointing one side of 4 km on the 1/50,000 scale map and poining the highest point on the graph. A part of the unit area is drawn on the Stmmit Level Map by the size of 1/50,000 scale.
(b) awing up the Reliefe Energy Map The differece between the highest point and the lowest point in the unit area; the highest undulations in the area is measured and the unit area has one side by 2 km long.
(c) The stage Measure of Cycle of Eroson To classify the landform making, the height of summit and the number of dultion were shown by the axis, X and Y on the graph. On the right angled coordinates, the numerical value was drawn. In the cycle of landform, the Sequential Form was subdivided into; Young Stage, Early Mature Stage, Fature Stage, Lature Stage and Old Stage. Mr. Humio Dada's theory is suppoted btt the lowest river level was omitted in this paper.
IV. Finding and Investigation
1. The finding and investigation of Hypothesis (1) is shown in the Fig. 2 and 3.
2. Those of Hypothesis (2) is shown in the Fig. 4, 5 and 6.
3. Those of Hypothesis (3) Is shown in the Fig. 7, 8, 9, 10, 11, 12, and 13.
4. Those of Hypothesis (4) is shown in the Fig. 14 and 15.
V. Conclusion
It was shown in the Fig. 16.

목차 (Table of Contents)

• 目次
• I. 序論
• 1. 問題意識
• 2. 硏究目的
• 3. 假說
• II. 硏究方法
• 1. 對象地域의 調整
• 2. 指標의 設定
• 3. 計測 및 處理 方法
• III. 結果 및 考察
• 1. 成因的 分類의 結果 및 考察
• 2. 數量的 分類의 結果 및 考察
• 3. 組織에 依한 分類의 結果 및 考察
• 4. 發達史的 分類에 依한 結果 및 考察
• IV. 結論