濟主道 南·北 斜面地形의 比較硏究

姜相培 濟州敎育大學校 1979 論文集 Vol.9 No.-

Jeju Island is a volcanic island which has begun to form by the volcanic activities from pliocene to quaternarv in geologic age. The main factors of landform in this island are composed of more 79 times of the lava eruption, patterns of volcauic activities by pyroclastic eruption, the diffential erosion being caused by the dissimilarity of rocks and the fluvial and the marine erosion carrying with the formation period and the upheaval. The original landform of this island is an Aspite whose top is Mt. Halla, but near the top of Mt. halla is like a Tholoide. This island have about 400 parasitic cones. The river system of this island has a radial pattern according the shield-shaped landform whose top is Mt. Halla. Development of river system in the eastern and the western slope in this island is poor, because these,in comparison with the northern and the southern ones, are relatively long and smooth and have the broad lava plateus. Many rivers, therefore, run down northerly or southerly. The tip of headward erosion toward the pick of Mt. Halla reaches 1600m above the sea-level, and most of the revers have the characteristics of the youth stage by the very activing downward erosion which reaches near the coastline. The northern and the southern slopes in this island show the different factors in precipitation, geological distributions, and amounts of upheaval. According to the geological observation comparision and analysis of the two slopes this island, it comes to the conclusions as follows: 1. The precipitation, the formation periods of lava, the difference in amounts of upheaval, the diffential erosion being caused by the dissimilarity of rocks, are the main factors which bring the different landfarms in the northern and the southern slopes of this island. 2. The southern slope operated more erosion than the northern under the influence of different precipitations. The gap between two slopes in precipitations is 346. 3mm a year on the everage in these 16 years. 3. The southern slope have also the larger relief energe with a large amount erosion, because it is covered more broadly, as compared with the northern slope, with the sedimentary rocks that are erupted at a relatively former period and the trachyte and trachy-andesites that are weak relatively against erosion. 4. Because of the different relief energy, the suthern slope is operated more erosion than northern and because the ratio of upheaval is rapidy than ratio of erosion, the deeping is operated actively near to coastline. In the northern slope, we can find the trace of marine erosion as far as 70m, but, in the southern slope, even 180m above the sea level. 5. Regarding the coastal dune, the northern slope is more developed than the southern by reason of the direction of the monsoon. In this island the northwesterly monsoon in winter is stronger than the southeasterly one in the summer season. 6. The differences in development of rivers on the two slopes are as follows: 1) About the curvature, the amounts of erosion, the drainage networks of rivers, the southern slope is larger and more developed than the northern. 2) About the degree of upheaval, the southern coast is more remarkable than the northern. 3) This is caused by the blocking that arises the trachytes or the trachy-and-esites in which the columnar joint are will developed.

濟州道의 地域別 人口增減에 關한 地理學的 硏究 (II)

姜相培 濟州敎育大學校 1984 論文集 Vol.14 No.-

The recent remarkable economic progress in Jeju-do faciliated the urbanization in Jeju-do. The urdanization has presented rapid population increase to urban area and has dought significant rural depopulation. This paper attempts to clarify the geographical characteristics between urban and rural population from 1960 to 1980 in Jeju-do and to map it out. Tte materials for the stuby are based on cunsus popalation: 1960, 1966, 1970, 1975, 1980. For the study data are divided into six : 1 Period (1960-1966), 2 Perio (1966-1970), 3 Period (1960-1970), 4 Period (1970-1975), 5 Period (1975-1980), 6 Period (1970-1980). The study area covers 1 city, 3"eups" and 10 "myons" in Jeju-do. Results are summarized as follows: 1) The population of Jejo-do has been mounting steadily since 1960, the increase rate of which exceeds that of the national level. 2) As for popula ion increasein "gun" districts, Namjeju-gun has been gaining in poplation which exceeds those of the provincial and national level, whereas Bugjeju-gun shows a slight increase in population. 3) The study has recegnized the difference in popalation increase at hte seperated districts in Jeju City. The fact of the investigations in that 5"dongs" in the midtown of the city and 4"dongs" in the secluded villages of mountains are have growm rapidly in poplation whereas the 5 coast"dongs" in outskirts of the city have increased slightly in population. 4) Population in crease in the urban and developing districts is remarkable in general, while in the rural districts, it remains slight or stationary. 5) Urbanization of Jeju-do has been accelarated, of which fact is verified by the fact that in 1970, "eup and Jeju city gained poplation increase of 50 percents over prervious years.

협제동굴지대의 동굴지형연구

강상배,홍현철 한국동굴학회 1991 동굴 Vol.26 No.-

이 동굴지대의 지형을 개관하면 한라산서북사면 기슭의 해안저평지대라고 하겠다. 주로 해안사구가 전개되고 있는 솔밭이 많은 지형이다. 우선 분포 지역을 살펴보면 북서 해안의 한림읍 금릉리 동쪽으로부터 협재리에 이르는 해안인데, 내륙으로 2.7km까지 사구가 발달되어 있고, 애월읍 곽지리 해안에도 약간 분포하고 있다.(중략)

濟州道內에 人口에 對한 硏究

姜相培 濟州敎育大學校 1975 論文集 Vol.5 No.-

濟州道의 地域에 對한 硏究 : 自然環境을 中心으로

姜相培 濟州敎育大學校 1971 論文集 Vol.2 No.-

濟州道人口의 性比變化에 對한 硏究

姜相培 濟州敎育大學校 1982 論文集 Vol.12 No.-

涯月邑의 綜合開發에 關한 硏究

姜相培 濟州敎育大學校 1983 論文集 Vol.13 No.-

濟州道의 地域別 人口增減에 關한 地理學的 硏究

姜相培 濟州敎育大學校 1978 論文集 Vol.8 No.-

A five-year economic plan commenced in 1962 made great strides in economic growth, which, in the meantime, gave impetus to industriali zation and urbanization in Korea. The urbanizatin resulted in the movement of surplus labor manpower of the rural community to cities, and a decrease in population of the rural community has brought about a shortage of manpower in the rural community. Jeju-do which was moving out population owing to migration to largest cities has flown in population, on account of the moving in population to the province as the provincial development in Jejn-do has advanced. And at the same time, urbanization in the province has been accelerated, of which fact is verified by the fact that in 1970, "eups" (towns) and Jeju City gained population increase of 50 percent over previous years. The object of this study is to investigate geographical characteristic of the movement of population in the cities and rural community in Jeju-do from 1960 to 1975. The date of the research have been extracted from the census of population taken in the province iu 1960, 1966, 1970, and 1975, and the study has been made separately by four perild for convenience' sake. Division of the period is as follows : The Ist period (from 1960 to 1966) : the 2nd period (from 1966 to 1970) : the 3nd period (from 1960 to 1970) : the 4th period (from 1970 to 1975). The research has been conducted on 1 city, 2 "guns" 3 "eups", and 10 "myeons" throughout the province. The following summarizes the results of the investigations : 1. The population of Jeju-do has been mounting steadily since 1960, the increase rate of which exceeds that of the national level. 2. As for population increase in 'gun' districts, Nam-Jeju-gun has been gaining in population which exceeds those of the provincial and national level, whereas Bug-JeJu-gun shows a slight increase in population. 3. The study has recognized the difference in population increase at the three separate districts in Jeju City. The fact of the investigations is that 5 "dongs" in the midtown of the City. and 4 "dongs" in the secluded villages of mointainous area have grown rapidly in population, whereas the 5 coast "dongs" in the outskirts of the City have increased slightly in population. 4. Population increase in the urban and developing districts is remarkable in general, while in the rural districts, it remains slight or stationary.

濟州島地域의 颱風에 關한 硏究

姜相培 濟州敎育大學校 1988 論文集 Vol.18 No.-

The purpose of this study is to clarify the pattern and characteristics of typhoon that have an effect on the residents in Cheju island. Typhoon data includes the observation data resulting directly from typhoon and from frontal activities affected by typhoons in Cheju island. The annual and monthly frequency of typhoons that have influenced in Cheju island for a period 63 years (1923∼1985) are analysed. The results of this study are summerized as follows; 1) Typhoon intensity as for minimum air pressure, maximum wind speeds and moment maximum air pressure, there are wholly lacking a special large size(a special A class) and a large size(A class). All are a medium size(B class) and a minimum size(C class), then there is absolutely much minimum size(C class). 2) For 63 years(1923∼1985) the mean annual frequency of typhoons that influences Cheju island is about 2. The month with highest frequencies are August. For three month, to attack typhoons July, August and September is 89.1%. 3) The monthly distribution pattern of typhoon precipitation is closely connected with the tracks of typhoons and theirs frequencies. 4) Typhoon tracks that have influenced in Cheju island typhoon precipitation is the type advancing northeastward across the Daehan Strait, the type landing the southern coast, the type advancing from the Yellow Sea northward and the type passing through continental China, etc. 5) The damage aspect in recent years is a same as a level in all country. On the other hand death decrease, but the fortune damage is toward suddenly increased. In the fortune, the marine damage like the vessel damage rather than the farm produce damage is much characteristics.

敎育大學 人口敎育課程 試案을 위한 探索的 硏究

姜相培 濟州敎育大學校 1980 論文集 Vol.10 No.-