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권동희 ( Dong Hi Kwon ) 한국지형학회 2014 한국지형학회지 Vol.21 No.1
In this study, total 87 rock formations were investigated and analyzed and the result is as follows. The most observed landform out of researched rock formations is weathering landform(35%) and it was followed by volcanic landform(10%), coastal landform(42%) and structural and other landforms(9%) in order. In the result of evaluating the resource value of rock formations as high, medium and low considering scarcity, academic value, size and accessibility, 29, 45, and 13 formations were classified as high, medium and low respectively. Of the landforms on high level, the highest landforms which received the highest scores(19 points) were 5 regions: Samjeongni Columnar Joint, Kongddeok Rocks, Sangdol, Fan Shape Columnar Joint, and Ddeoksiru Rocks. Of them, Samjeongni Columnar Joint and Fan Shape Columnar Joint are being utilized as tourist attractions and Kongddeok Rocks, Sangdol and Ddeoksiru Rocks are little known to ordinary people. The 29 landforms which were classified as high level including the highest 5 landscapes are expected to be utilized as the basic contents for experience tourism program such as “Searching for the interesting rock name(tentative name)” targeting ordinary people or “Exploring topography travel(tentative name)” targeting highschool students or university students who major in geography.
권동희 ( Dong Hi Kwon ) 한국사진지리학회 2009 한국사진지리학회지 Vol.19 No.3
Currently, 5 regions of Korea have become Slow Cities. Becoming an accredited Slow City has often produced satisfactory results, e.g., realizing higher geographical brand value for the city in question. For this reason, every local government in Korea develops a new tourism product, enjoying huge success by highlighting such geographical brand. In fact, their success in developing and selling such product is said to exceed their expectations. The popular slogan commonly found in these new products is excursion revealing the happiness of living slow that we have forgotten. Note, however, that the spirit of Slow City is predominantly indicated to have been eroded, losing much of its initial passion and resulting in the lack of sufficient effort to maintain the initial success and to develop further. Such stagnation was mainly attributed to the insufficient systematic financial and administrative support fit for the regional characteristics of Korea, inadequate basic geographical data of the region in question, and passive participation of the residents in the development program; all of these are believed to have stemmed from inadequate basic geographical data on the region in question and lack of understanding of such data. In this light, the study on the Slow City under such circumstances is believed to be significant. Slow Cities consist of myeon or ri, a small administrative unit but representing a basic unit of space showing the geographical features when viewed from the perspective of geography. In other words, that unit will also contribute greatly to reestablishing the true character of geography.
전국자연환경조사 전문인력 양성 프로그램을 위한 강의 구조화 -지형분야 산지지형 단원을 중심으로-
권동희 ( Dong Hi Kwon ) 한국사진지리학회 2009 한국사진지리학회지 Vol.19 No.4
The method of investigating the natural environment of national land will be changed beginning 2010. To address the problem of shortage in professional natural environment investigators, the Ministry of Environment has decided to operate a short-term investigator training program on a temporary basis. The effects of the program can be maximized by structuring the lectures as follows in the case of mountain landforms: 1. Divide the lectures into 4 themes: maountain landform (general), weathering landform, erosional landform, and depositional landform. 2. Allocate lecture hours to each of the 4 themes considering the number of landform units (mountain landform (general): 1 hour; weathering landform: 3 hours; erosional landform: 3 hours; depositional landform: 1 hour). 3. Give lectures on an hourly basis focusing on process by grouping each landform unit into several topics. 4. Maximize the use of pictures and photos. Note, however, that themes should be selected by fully considering the topographic units in the landform classification table. Limit photos to domestic cases considering the field practices.
지형경관과 관련된 천연기념물 지정 현황과 문제점 그리고 대안
권동희 ( Dong Hi Kwon ) 한국사진지리학회 2002 한국사진지리학회지 Vol.12 No.1
This research is to understand the status and problems of topographical landscape as natural monument in terms of management and utilization, and to present the alternative plan. In Korea, total 330 natural creatures have been designated as natural monument. Of them, 47 monuments are related with topographical landscape. Hereon, it is founded on solely the writer`s subjective judgment that any natural monuments are related with topographical landscape, and in fact, they are referred to Mineral and Nature Reserves from the viewpoint of classification of the Cultural Properties Administration. Minerals are subdivided into rock - mineral, cave, geological structure, topography - geology, and prehistoric life. However, this classification method has some problems in a realistic viewpoint, so it is desirable to improve the method shown in the Table 4. Recently, research `subjects of traditional physical geography (especially, geomorphology) are attracting considerable attention as the objects of natural monuments. It is now deemed that relevant academic societies, including The Association of Korean Photo-Geographers, The Geomorphological Association of Korea, etc., are required to configure, tentatively named, `the Steering Committee for Designation and Management of Natural Monuments`, in order to designate and manage the related affairs, as well as progress more systematic researches in terms of utilization.
권동희 ( Dong Hi Kwon ) 한국사진지리학회 2013 한국사진지리학회지 Vol.23 No.3
The glacier tour is centered on Anchorage, and typical tourist sites include Mt. McKinley, Matanuska Glacier, Exit Glacier, and Prince William Sound. These sites are all two or three-hour drive from Anchorage. In Mt. McKinley, huge valley glacier, moraine, migratory talus, and rock glacier, etc. can be observed. Piedmont glacier and erratic boulder can been seen in Matanuska Glacier; outwash plain, in Exit Glacier; and fjord and tidewater glacier, in Prince William Sound. Of these glacial landforms, however, only valley glacier, fjord, and tidewater glacier are used in the glacier tour for general tourists; the other topographies are not properly utilized even though they are academically important and worth observing. For the next several years, the development and use of specific contents (concept and viewpoint, etc.) on these glacial topographies are expected.