국립공원 북한산의 자연경관에 대한 관광지형학적인 분석

고의장 한국관광산업학회 1988 Tourism Research Vol.2 No.1

Mt. Puk'ansan, forming in tricone, was designated as one of Korean National Parks in April, 1983. Among the tricorne mountains Paekundae, 836m high, is the highest peak of Mt. Puk'ansan, from which the entire city of Seoul may be seen below. Seoulites can get to this mountain, the unique National Park in Metropolitan area of more than 10 million population, and spend hours climbing on the rocks and return home all in a day. The region is located between 31°35'53$quot; and 37°43'54$quot; north latitude and between 126°56'05$quot; and l27°03'04$quot;east longitude, covering area of 78,45㎞s. this mountain is comprised of ridges to the north, the highest tricorne of Paekundae & Insubong and Mankyongdae in the midst, in some northern part of Seoul. The mountain chains including, hilliniss with many small monadnocks, have rugged landscapes and domes out of Seoul granite. In geology Puk'ansan is composed of, Kyunghee gneiss complex of pre-combrian period, and Daebo granite of Jura-period and porphy-granite of unknown period, in Kyunghee land block. Owing to oroganic movement Puk'ansan was erupted from the ground with bathholith, the rocks compositions of this mountain are black mica-granite and fresh red aranite. By the grade of rockhardness, there has been differential erosin and weathering which resulted in dome shaped peaks. The surveyed physical landscapes are as follows. 1. from Kukeedong to Daenamun 2. from Chongnungdong to Taesungmun 3. from Suyudong via Kalbawee to Taesungmun 4. from Suyudong via Jiudalae ridge to Taedongmun 5. from Vidong to Weemun 6. from Hyojari to Weemun 7. from Daeamun via Jindalae ridge to Kunghee.

국립공원 내장산의 자연경관 분석

고의장,송형경 한국관광산업학회 1991 Tourism Research Vol.5 No.1

The purpose of this study is to made an analysis of the microlandforms in the area of Naejangsan National Park, south-western part of Korea. Geology of the area is underline by gneisses complex of Precambrian age, metasedimentary rocks and later intrusives of an unknown age, Jurassic schistose granite, Cretaceous granite, sedimentary and volcanic rocks and Quarternary alluvial deposits. The geology of Naejangsan is $quot;Rhyolitic rocks$quot;, which are $quot;volcanic rocks$quot; of cretaceous periods , that is called $quot;Naejangsa volcanic rocks$quot;. In its climate, the annual mean temperature is about 12-13℃ and mean humidity A 75%, the mean wind velocity is 1.2m/s, and its annual mean precipitation is 1263.9㎜. The topographical features are placed as follows: (1) Its joint developed well but the shape of for is not well because of sheeting joint, shattering and exfoliation. (2) The top of mountain is developed vertical joint the top of sere Bong of shape is rounded by rock mass. (3) Its valley developed sheeting horizonal joint which the most development valley is keumsun valley, as a result, maked waterfall and rock cave. (4) Keumsun waterfall developed sheeting joint as one fall, maked small rock cave. (5) Talus and rockfall developed well in valley side.

수도권 운하망의 지형적 분석

高義長 祥明女子大學校 人文社會科學大學 地理學科 1995 地理學論考 Vol.13 No.-

변산 채석강의 해안경관

고의장,Go, Ui-Jang 한국자연공원협회 1997 한국자연공원 Vol.67 No.-

지질학적으로 본 북한산

고의장,Go, Ui-Jang 한국자연공원협회 1994 한국자연공원 Vol.61 No.-

국립공원 지리산 동부지역의 자연경관에 대한 지형학적 특성

고의장 국토지리학회 2002 국토지리학회지 Vol.36 No.2

國立公園 周王山의 自然景觀分析

高義長 세종대학교 1986 세종대학 논문집 Vol.13 No.인문사회

Chuwangsan, which is located in the tip of the Teabak mountains and in the southeastern part of Korea, has been long named Suk-byongsan, Taedunsan, Chubangsan or Sokumgang and so forth. This mountain extends over five Myons and 17Dongs including Cheongsong district and Youngduk district. It's location is at 36°19' 56"N-26°27' 46"N and 129°04'51"E129°14' 55"E, which is equivalent to 13.5㎞ away south east from Cheongsong. The Chuwangsan is 106㎢ wide and its main part of physical landscape is ranged within the radius of 10㎞ of Cheongsong. In its climate, the annual mean precipitation is 1,029㎜ and its annual mean temperature is 8.10℃, January mean temperature is -4.10℃ and July mean temperature is 26°10'C. Those conditions are explaining its cold humid region. The topography of this area corresponds to a part of the Taebak mountains and its mountain system is composed of 910m of sea level from the top of which 720m of Chuwangsam and from of Kumeunkwangi extend over west-south-east and east-south-west respectively. Their mean sea level is 300m, consisting of heights whose south-west is gently slopy and cliffy and the land is the source of Chubangchun and Chusanchun. So the stream system is west-south-east. In the east area mountains are comparatively steeper and higher, because they are chiefly composed of felsite and andesite comparatively hard and compact not to be eroded out easily. The topography of the region shows middle mature stage. But in the west region mainly composed of coarse granite was very much weathered to reach landform of an old mature stage. So, Its predominent trend of the topography run after the general direction of the rock distributions. The geology is mainly composed of Cretaceous sedimentary formations and igneous rocks, and partially of age unknown Pre-Cretaceous metamoprhic rocks and granite. The most important problem have been focused on the relation between the sedimentary formation and the older granite in the guard rangle. The formation of the area where the physical landscapes are placed as follows; 1. The Arkosic Sandstone Formation developed its distribution along the contact parts with the Cheongsong Granite, and formed the basal one of the Gyenongsang system in the area. 2. The Reddish Sandstone Formation overlaid the Arkosic Sandstone Formation in conformable relation. It is formed by the rocks, reddish sandstone, shale and mud with thin intercalations of some other rocks. 3. The Greenish Sandstone Formation overlaid the Reddish Sandstone Formation in conformable relation as the uppermost one of the sedimentary part of the Gyeongsang system in the quard rangle. All the Physical landscapes of the National Park, Chuwangsan is spreaded within the diameter of 5Km of Daejunsa, Kwangamsa, Yonhwasa, Baekyonam. Chuwangam, all of which are located in Sangeuidong, Budongmyon, Cheongsonggun district. The surveyed physical landscapes are as follows. 1. Being named as rock ridge there are; Changgunbong, Nahanbong, Hyangrobong, Chotdaebong, Sukgabong, Mireukbong, Chijangbong, Kwaneumbong, Yonhwabong, Mearibong, Sirubong. 2. Being pointed as rocks of strange formation; Kiam, Sansinam, Chahasung, Mangwoldae, Keupsudae, Haksodae, Sinsundae, Buam, Sukbyongam, Manhwabong. 3. As cave; there are mujanggul, Chuvanggul, Yonhwagul. 4. As water fall; there are the first fall, the second fall, and the third fall. Judging from the surveyed report mentioned before the physical landscapes of the National Park, Chuwangsan has well developed dliffs, rock ridges and magnificent water falls which have resulted form the weathering, erosion and exfoliation caused by the difference of hardness and softness in and site and sandstone.

변산반도 국립공원의 자연경관에 대한 지형학적 특성

고의장 국토지리학회 2003 국토지리학회지 Vol.37 No.3

국립공원 월악산지역의 자연경관에 대한 지형학적인 분석적 연구

고의장 한국관광산업학회 1996 Tourism Research Vol.10 No.1

The Wol-ak-san national park covers Chungwon-kun, Danyang-kun in Chung cheung buk-do and Munkyung-kun in Kyung sang buk-do. This area including the Song gae, Deuk ju, Yang ha river valleys and Wol-ak valley has been designated as one of the National Parks since 1984. Geologically, it is made of the great limestone Series and biotite granite in which the latter is more abundant.. The representative physical landscapes of this area consist of plunge pool like pond and pool, rock cliff, rock talus, rock table, water fall and riffle. The characteristics of physical landscape of the Wol-ak-san national park are as follows First, the rock table, pond and pool and rock cliff, etc. are located in the vicinities of the Song gae and Deuk ju river valleys, whereas rock talus is at the mountain slope. Second, the Wol-ak valley has a sharp slope which represents a typical valley, Third, the Yang ha river valley has been formed by the development of rivet landscapes such as rock table, water fall, and plunge pool like pool and pond which constitute the most beautiful physical landscapes of the Wol-ak-san.

鬱陵島에 對한 觀光地形的인 硏究

高義長 세종대학교 1984 세종대학 논문집 Vol.11 No.-

The tourism of this island lays behind compared to its blissful scenery. The island is three-nil and five-plenty. In this blissful island it is the pride that there are no snakes, thieves or beggars but plenty of Chinese junipers, wind, beautiful women, fresh water and stones. The volcanic island, formed by the eruption of the lava in the Quaternary Period about 2 millions ago, lies to the easternend of the Korean peninsular, to the N.E. 217㎞ from Pohang city, or to the east 137㎞ from Yimwon-ri, Samcheok-kun, Kangwon-Do. Historically this island had been named Moo-renung, Woo-renung or Woo-san state before it was named Ulleung-Do. During Yidynasty there were patrol to this island at regular intervals by government patrol system and the island was carried by a law of empty-island policy because of poor transportation with the peninsular. The volcanic island, peaked by Mt. Seongin-bong 984㎞ above the sea level in pantagon shape, has all the volcanic landscape attributes worth seeing. Still more the maritime climate has sculptured the whole volcanic rocks of the island into various natrual wonders for the countless years on the sea. But the poor transportation with the main land still cause to hide its beautiful vista from the outside. Thus the writer's interest in this island are the inherited human life style, geology, landforms, climate and vegetations, there of acceleration the tourism development of this blissful island. Descriptions shall go into the geographycal, topographical and geological scenery about 23 items in details.