• Journal of the Korean Society of Surveying, Geodesy, Photogrammetry and Cartography
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• v.17 no.2
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• pp.153-160
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• 1999

On this study, We apply terrain analysis method using DTM(Digital Terrain Model) to mountainous district development to present the example of terrain-change modeling when we develop mountainous district, and the landscape-change modeling which is geographically referenced when a large scale utility was constructed on mountainous district. Finally, we present an one way which raise a efficiency of national land use and future oriented, environmentally friendly national land development.

• Journal of the Korean Institute of Traditional Landscape Architecture
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• v.37 no.3
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• pp.37-48
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• 2019

This study, which starting from Yangyang Jukdo's topography formation and questioning revealed in landscape guide and landscape commentary board, is to sort out the characteristics of Jukdo natural landscape through literature research, field observation research and stakeholder interview as part of the proper recognition of Jokdo landscape and search for landscape resources, and pursued a review of nominations and criticism. The results of this study are summarized as follows. Yangyang Jukdo is an island named because it was full of blue bamboo. From before the first half of the 14th Century. to the middle of the 18th Century., there was a Gwanlan-pavilion to see the sea and the bamboo in the west. The time when the original island, the Jukdo, have been a land-tied island connected with the land by the tombolo formed by the erosion of the sand. It is located at the end of the 14th Century. and before the middle of the 18th Century. In Jukdo, colorful weathered terrains, coastal terrain, and structural terrain formed by long-time weathering are found. Among them, the type of weathering, the tafoni style and the gnamma style are the scenic landscapes with the key stories of legend and poetry that are brought to Jukdo. In addition, there are seven kinds of letters caved in the rocks in Jukdo. The rocks found on the coast, basketball cannons, shrines, and sutras are seen as shrouds based on a Taoist hermit motifs and style. In addition, it can be interred from the photography of "jeongssisejeog" that the souvenir of Jukdo was the family of Chogyejeong of mid 18th Century. In terms of observational geography and poetry, Jukdo has been handed down a great deal of missionary color with key motifs such as 'Jukdo-seongoo', 'Jukdo-Dolgooyoo', or 'Stone mortar of Taoist hermit' It is proved that the pearl which is called 'The stone of the Taoist hermit' is a porthole formed in a separate space rather than the topography of the geomorphology in terms of shape, size and function. Currently named Shun-tang is a product of the ridiculous 'naming' of interest. The present landscape guide and commentary is not only incompatible with the place of Jukdo, but also does not match the traditional cultural landscape. Future scenery information such as guide signs and commentary boards should be improved in the direction of positively highlighting the stories and motifs related to the present that are present in order to enhance the landscape identity of Yangyang Jukdo.

• The Journal of the Petrological Society of Korea
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• v.26 no.3
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• pp.167-181
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• 2017

Cheongryangsan area ($49.51km^2$) has been designated as the Provincial Park in 1982, because it has magnificent aspect and seasonally spectacular landscapes. Especially, Cheongryangsa sitey ($4.09km^2$) has been designated as Noted Scenery No. 23 in 2007, because it has the same topographical landscape as rock cliffs, rock peaks and caves. The most spectacular landscapes are exhibited in the Cheongryangsan Conglomerate and Osipbong Basalt. There are twelve rock peaks on the ridges of the two strata, and many rock cliffs in the several valleys of strata, in which a few caves are formed by differential weathering and erosion. The valleys, in which flow Cheongryang, Bukgok and Cheonae streams, are classified as fault valleys along WNW-ESE faults. The rock cliffs were generated from vertical joints parallel to WNW-ESE faults in the two strata, and the caves were formed by differential weathering and erosion along bedding of sandstones and shales intercalated in the conglomerates. The rock peaks are landscapes formed by differential erosion along crossed vertical joints in the ridges. The vertical joints are developed subparallel to two WNW-ESE faults and a NNE-WWS fault. Therefore the topographical features are caused by existence of the faults and Lithologic difference in the Cheongryangsan Conglomerate and Osipbong Basalt, and by differential weathering and erosion along them.

• The Journal of the Petrological Society of Korea
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• v.18 no.3
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• pp.195-209
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• 2009

Juwangsan area($107.4km^2$) has been designated as the twelfth National Park in 1976, because it has magnificent aspect and seasonally spectacular landscapes. Juwang valley($9,177.5m^2$) has been designated as Noted Scenery No. 11 in 2003, because it has the same topographical landscape as rock domes, rock cliffs, caves, waterfalls and plunge pools. The most spectacular landscapes are exhibited in the densely welded zone of the Juwangsan Tuff. The rock cliffs generated from vertical joints in the densely welded zone, in which there are the same many rock cliffs as Geupsudae, Haksodae, Sinseondae, Mangwoldae, Giam and Byeongpungbawi, three caves such as Juwanggul, Mujanggul and Yeonhwagul in the cliff. The cliffs and caves are landscapes that were generated from vertical joints in the densely welded zone, and the rock domes and waterfalls are landscapes of erosional vertical joint planes in the zone. The vertical joints are columnar joints formed during cooling of the Juwangsan Tuff. Therefore the topographical features cause the cooling columnar joints that are vertically intersected in the densely welded zone of the Juwangsan Tuff.

• Journal of the Korean Institute of Traditional Landscape Architecture
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• v.32 no.3
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• pp.168-182
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• 2014

Several Sungsi Gardens were built up in Old West Village during the period of the Joseon Dynasty. Most of them were painted as True-View landscape painting. This study aims at examining original locations of representative gardens of the Old West Village by empirical investigation of related True-View landscape paintings. It seeks to demonstrate the garden landscape in True-View landscape painting by utilizing ArcGIS, 3D topographic modeling to observe geographical locations and landscape more realistically. After forming 3D topographic modeling of estimated locations of the gardens, location of objects at composition of 3D modeling similar to True-View landscape painting was found by shifting viewpoints. And by overlapping the cadastral map on the modeling, we could verify the current lot number of the garden sites. The interpretation of processes and results are as follows. In the early stage, Chungpunggye garden was built at the very end of Mt. InWang valley. The site is hidden from the outside, and appeared as 'Enclosed Landscape'. In the middle stage, Chunghuigak garden was built between Okryu-dong valley and the surrounding ridge. It appeared as 'Semi-Opened Landscape'. In the late stage, Seowon garden was built at the highest level of the ridge among the research areas. It appeared as 'Prospective Landscape'. In the last period, Songsukwon garden, was built at a point of contact of the ridge end and surrounding residential area. So it appeared as 'Opened Landscape' to the town. In other words, the location, landscape and social function of the gardens in Old West Village had been gradually opened in Joseon Dynasty.

• Journal of the Korean association of regional geographers
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• v.14 no.3
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• pp.189-198
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• 2008

This research is undertook as a preliminary study for cultural and ecological environments of Daegu city which is required to improve urban image as the host city of 2011 World Championship in Athletics. The main findings of this research are as follows: Firstly, it is necessary to correct some errors in the natural scenery, such as Shincheon and Ibam which are known as important natural scenery of Daegu city. and also necessary to correct some errors in the name of places. Secondly, according to the old literature, it is known that there are two famous rocks in Daegu. Ibam, one of the two, is known as already disappeared. However, Hwaam, the other one, has been recently revealed as substantial. Therefore, the city needs to preserve the natural inheritance. In this sense, the city needs to consider to utilize natural scenery as cultural eco-tourism resources. Lastly, some part of landforms are related to culture and history. Thus, I proposes to name them as 'cultural landforms'.

• Proceedings of the Korea Contents Association Conference
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• 2017.05a
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• pp.241-242
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• 2017

본 연구는 소형 UAV를 이용하여 수시로 변하고 있는 국가지정문화재 명승 주변의 지형경관 변화를 주기적으로 취득함으로서 자연유산에 대한 효과적인 모니터링을 위한 목적으로 수행되었다.

• Journal of the Speleological Society of Korea
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• no.53
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• pp.29-38
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• 1998

화산동굴로서는 한 때 세계 제1이었던 단일 화산동굴인 빌레못굴은 그야말로 세계적인 화산동굴의 대표적인 화산동굴일 뿐만 아니라 우리나라의 자랑이다. 본 연구는 이 동굴 속에 간직되어온 화산동굴의 지형, 지물들에 대하여 그 형성과정과 경관적 특성 등을 밝히고자 한다. 여태까지 발표된 연구 중에는 빌레못동굴의 학술적인 가치를 밝힌 연구는 몇 가지 발표된 바 있으나 이 동굴 속의 경관형태는 물론 지형지물에 대한 상세한 연구발표는 학술조사 이외에 거의 없는 실정이다.(중략)

• Journal of Korean Society for Geospatial Information Science
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• v.3 no.1 s.5
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• pp.105-113
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• 1995

Three-dimensional landscape map is very useful in terrain analysis as it looks like real shape of terrain. When three-dimensional landscape map is needed, landscape photos achieved at a position of high elevation or by airplane are generally used. But, this approach can not fully satisfy the user's need to get pictures from various view points. In addition, because photos have some geometric displacement caused by the principle of central projection of camera, it is hard to get accurate locations from the photo. This paper aims to get three-dimensional landscape map similar to real terrain feature from vertical stereo aerial photos by digital photogrammetric techniques. This approach can provide a very useful data for three-dimensional terrain analysis as a function of Geo-Spatial Information System.

• Proceedings of the KGS Conference
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• 2001.12a
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• pp.18-34
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• 2001

량강도 북부지역에서는 지질시대로부터 현대에 이르기까지 여러차례의 화산활동이 있어 자연경관을 훼멸, 복구하였다. 특히 갱신세에 분출된 현무암용암, 백두산 소백산에서의 알칼리성조면암의 발생, 800여년전에 분출한 부석은 원래의 자연경관을 훼멸,매몰하고 새로운 자연경관을 형성하기 시작하였다. 자연경관 형성에서 지질,지형,기후,식생,토양 등요소들이 종합적으로 작용하나 그중에서도 화산활동을 위주로한 지질작용이 주되는 인자로 되었다. 즉 용암의 분출에 의하여 본 지구의 지형을 1600m 높여 기후,식생,토양의 산지수직지대성을 형성하였고 강,호수의 형성도 식생,토양의 특성도 화산활동의 제한을 받았다. 모두어 말하면 본 지역의 자연경관은 800 여년 역사를 갖고 지금도 발전, 성숙과정에 있다. 본문에서는 백두산과 가까이 자리잡고 있는 량강도의 삼지연군, 대홍단군, 백암군, 보천군, 운훈군, 갑산군과 함경북도의 무산군, 연사군, 어랑군, 길주군의 일부지역 및 함경남도의 단천서북부가 포함된다. 지리위치로 보면 동경 128 도 16 분으로부터 동경 130 도 02 분까지이고 북위 42 도 10 분부터 북위 41 도 좌우이다.