전라남도 득량만 북측 해안에 분포하는 지질노두의 지질유산적 가치

김해경 ( Kim Hai-gyoung ) 한국도서(섬)학회 2017 한국도서연구 Vol.29 No.1

The aim of this study is to evaluate geoheritage values, and describe geological records in the geological outcrops distributed in the north coast of Deungnyangman, Jeollanamdo. The results of this study are listed below. Various geological records are distributed in the geological outcrops of about 1.2km coast of this study area. The area shows unconformity that involves a substantial break or gap in geological record, and meets with a fracture caused by spheroidal weathering and the intrusion of acidic and intermediate dykes in the 5 sites of this study area The explanations on geological records of this investigation are as follows. The unconformity of this study area is a nonconformity developed between sedimentary rocks and older metamorphic rock. The fault (about 2m displacement) showed in this area is mainly a normal fault developed in sedimentary rocks. The phenomenon of spheroidal weathering, which is a product of chemical weathering is developed in the outcrops of igneous and gneiss. The acidic and intermediate dykes around 3m to 5m in width are developed in the outcrops of gneiss. As for the geological records of these 5 sites, the values of academy, education, geomorphology and landscape were evaluated as excellent. This is due to the representativeness, scarcity and diversity of these geological outcrops. As this study indicates, these 5 sites have high value as geoheritages and thus, plans for the conservation and management on these geological outcrops should be provided.

오감활용 미술,과학통합활동이 유아의 미술능력 및 관찰태도에 미치는 영향

김해경 ( Hai Gyoung Kim ),오숙현 ( Sook Hyun Oh ) 미래유아교육학회 2009 미래유아교육학회지 Vol.16 No.2

여수시 낭도의 지형·지질경관 특성 및 활용방안

김해경 ( Kim Hai-gyoung ) 한국도서(섬)학회 2022 한국도서연구 Vol.34 No.1

Nangdo is located between Hwayang-myeon, Yeosu-city and Yeongnam-myeon, Goheung-gun, Jeollanam-do and is one of several islands located at the entrance of Yeoja Bay. In terms of its administrative district, Nangdo corresponds to Nangdo-ri, Hwajeong-myeon, Yeosu-city, Jeollanam-do. Nangdo is connected to Jeokgeumdo in the northwest by Jeokgeum Bridge and Dunbyeongdo in the north by Nangdo Bridge. Nangdo, where dinosaur footprints fossils and sedimentary layers are distributed, was selected as an island attractive to visitors implemented in Jeollanam-do in 2015. The dinosaur footprints and fossils site in the research area was designated as Natural Monument No. 434 in 2003. However, it is difficult to use it as a resource in terms of geotourism due to the lack of detailed information including detailed explanations of the geomorphological and geological landscapes of Nangdo. Therefore, in this study, the geomorphological and geological landscapes distributed along the coast of Nangdo were investigated and classified. The results of this study can be used not only as basic data for basic promotion of Nangdo, but also as geotourism or geoscience education data. In Nangdo, several hiking trails and Dulle-gils are mainly built on the east and south sides of the island for tourists. It is necessary to construct a dulle-gil and observation path on the west coast of Nangdo, where dinosaur footprints fossils and columnar joints are distributed. In order to reach the dinosaur footprint fossil site distributed on the southern coast of Nangdo, detailed information boards must be installed. In addition, in order to utilize various geomorphogical and geological landscapes as geotourism resources, it is necessary to install a description board that easily explains geological factors and create an observation path. The geomorphological and geological landscapes distributed in this area are very close to the learning contents of elementary school science, middle school science, and high school earth science I in the 2015 curriculum. Among the various geomorphological and geological landscapes, strata, sedimentary rocks, faults, and dinosaur footprints fossils are commonly related to the curriculum of elementary, middle, and high schools. In order to utilize these geomorphological and geological landscapes as an outdoor geological learning center, the need for follow-up research such as the development of outdoor learning programs is required. In addition, photos, videos, and VR materials can be produced and used as alternative learning materials in the classroom. In particular, fault-lines and fault-line scarps distributed on the southern coast of Nangdo are geologically uncommon structures and are worth preservation and there is need for follow-up studies.

신안군 소룡도의 지형·지질경관 특성 및 활용방안

김해경 ( Kim¸ Hai-gyoung ),오강호 ( Oh¸ Kang-ho ) 한국도서(섬)학회 2021 한국도서연구 Vol.33 No.3

The purpose of this study was to investigate and classify the geomorphological and geological landscape of Soryongdo and to suggest ways to use it as an earth science education. The results of this study will be helpful not only as basic data for geological heritage evaluation but also as learning materials for earth science education. Soryongdo belongs to Haui-myeon, Sinan-gun, Jeollanam-do, and is an uninhabited island. Soryongdo is located on the west side of about 2.5km away from Hauido, located in the southwest of Mokpo-city. Jangdo is located on the east side of Soryongdo and Yongdo on the northwest side. The size of Soryongdo is about 190m long in the east-west direction and 110m in the north-south direction, with an area of about 5,950㎡. The entire coast of Soryongdo consists of rocky coasts, and extends to sea cliffs, notches, and wave-cut platforms toward the sea. Various types of taffoni are distributed on the sea cliffs of Soryongdo, so the scenery is beautiful, and various weathering and coastal erosion topography can be observed, so it has been evaluated as an uninhabited island with a very high academic value. The results of this study are as follows. The coast of Soryongdo is a rocky coast consisting of sea cliffs, notches, wave-cut platforms, and boulder beaches. Sea cliffs are developing on the entire coast of the island. The notches are distributed in the lower part of the sea cliffs and mainly develop on the southern coast of the island. The wave-cut platforms are connected to the sea cliffs and are up to 80m wide on the southern coast. The weathering and erosion topography observed on Soryongdo are taffoni and marine potholes. Taffoni mainly develop on the slopes of the sea cliffs on the southern coast. Marine potholes develop on the wave-cut platforms on the north coast. The rocks distributed in the study area are hard tuffs with developed stratification, and lapilli. On the southern coast, intermediate dykes with a width of about 2m and a length of about 50m are distributed. Joints developing on the south coast have a northeast-southwest orientation. Faults are observed in some tuff layers. The geomorphological and geological landscapes distributed in the research area were compared and analyzed with the learning contents of the geological unit of the 2015 curriculum for elementary school science, middle school science, and high school earth science Ⅰ. Sea cliffs, notches, wave-cut platforms, and boulder beaches are related to the learning contents of the “Changes in the earth’s surface” unit of in the 3rd grade of elementary school science. Taffoni and marine potholes are related to the learning contents of the 3rd grade “Changes in the earth’s surface” in elementary school science and the 1st grade “Changes in the earth’s crust” in middle school science. Stratification is related to the learning contents of the sections “ Strata and fossils” in the 4th grade of elementary school science, “Changes in earth’s crust” in the 1st grade of middle school, and “Geological structure and depositional environment” in high school earth science Ⅰ. The faults are related to the learning contents of the 4th grade of elementary school science, “Strata and fossils”, and the high school earth science Ⅰ “Geological structure and depositional environment” unit. Joints, dykes, and volcanic rocks, tuffs, and lapilli are related to the learning contents of the high school earth science Ⅰ chapter entitled “Geological structure and depositional environment”. VR contents were produced to utilize the geomorphological and geological landscape cases of the research area as learning materials for earth science education.

신안 임자도의 지형,지질경관 특성 및 교육적 활용방안

김해경 ( Hai Gyoung Kim ),오강호 ( Kang Ho Oh ) 한국도서(섬)학회 2014 한국도서연구 Vol.26 No.1

The purpose of this study is to provide the basic resources for education, tourism and geotourism through examining the characteristics of the geomorphological and gelogical landscapes of Imjado, Sinan-gun. According to the classification of the Ministry of Enviornment and National Institute of Environmental Research(2012) there are seven types of geomorphological and geological landscapes (sea cliff, wave cut platform, sea cave and etc) or eleven types (stratification, joint, dyke, volcanic rock, conglomerate, intrusive structure, flow texture and etc) based upon Korea Environment Institute``s (2003) categorization. The geomorphological and geological landscapes of this study area are useful materials for science textbooks such as earth science Ⅰ&Ⅱ, since they provide useful materials for on-the-spot learning activities. The landscapes also act as a basic data for ecotourism and geotourism for visitors in Imjado, Sinangun.

덕수궁 석조전 정원의 조성과 변천

김해경 ( Hai Gyoung Kim ),오규성 ( Kyusung Oh ) 한국전통조경학회 2015 한국전통조경학회지 Vol.33 No.3

As a result of analyzing the forming and the transformations of Seokjojeon Hall garden by linking it to the changes of Deoksugung Palace influenced by the social atmosphere, the Seokjojeon garden can be classified into four phases. The first phase starts from 1896 to 1914. Gyeongungung was built in the late 19th century(1896-1897) as an official palace and Junghwajeon Hall and Seokjojeon Hall was built for Gojong. J.M.Brown was in charge of the construction of Seokjojeon in the beginning but H.W.Davidson saw the end also set up the garden. In the process of forming the garden the incorporating of Dondeokjeon Hall and the demolishing of the west wing corridors of Junghwajeon Hall occurred. At this phase of the garden a statue of an eagle was put up in the garden but was soon taken down. The shape of the garden was quiet simple with a central axial pathway, a round assorted flower bed placed in front of Seokjojeon Hall. The second phase starts from 1915 to 1932 which lasted for 17 years. At the last years of the Great Han Empire the duties of Gungnaebu(宮內府) was transferred to Leewangjik(李王職) in 1911 and a research on the existing buildings was done by Jujeonkwa(主殿課) in 1915. According to the research drawings, the garden still maintained the axial pathway formed in the previous phase but the garden had an asymmetric form. The flower bed was formed in a round shape and an open-knot technique and boundary plantation was applied to the garden. The third phase starts from 1933 to 1937 and is the period when Seokjojeon Hall was made public. By the year of 1932 many buildings of Deoksugung Palace had been demolished in the preparation of the opening of Seokjojeon Hall as a permanent exhibition hall. The central axial pathway still remained in the new garden and added a pond with a turtle statue in the center. The fourth phase starts from 1938 until the liberation from Japan and is the period when Deoksugung Palace became a park. Yi Royal-Family Museum was built and linked to Seokjojeon Hall with a bridge and the garden transformed into a sunken garden. The garden adopted a fountain and a pagora. Despite the minor changes in the after years the garden still posses most of its form from the fourth phase. As we can see the current garden of Seokjojeon Hall is not the same as the initial garden and therefor the importance of this study lies in the fact that modifications to the statements regarding to Seokjojeon Hall garden should be made.

벚꽃을 통해 본 근대 행락문화의 해석

김해경 ( Hai Gyoung Kim ) 한국전통조경학회 2011 한국전통조경학회지 Vol.29 No.4

In landscape architecture, plants play an important role in realizing the intention of the architect and user-behavior as well as an ecology and appearance of the space for them. However, it is true that many researches have focused on ecological characteristics of plants, their cultivation environment and symbolic meanings in traditional terms, while relatively few for the analysis of the aspects of each period through plants. For this, cherry trees that we often see around are selected and their introduction, propagation, development and symbolism from the view of chronicle are studied and the results are followings; Firstly, three-year seedlings of 1,500 pieces of cherry tree from Osaka and Tokyo were planted for the first time in Oieseongdae, Narnsan Park, Seoul. Since then, they had been widely planted at traditional sites, modem parks, newly-constructed roads for street trees, and for this, the Japanese Government-General of Chosun had actively supported by its direct cultivation and selling of cherry trees. The spread of cherry trees planted raised the question of whether or not Prunus yedoensis is originated from Jeju Island. Secondly, such massive and artificial planting of them had become attractions over the time and mass media at that time also had actively promoted it. And such trend made the day and night picnic under the cherry blossoms one of the most representative cultures of enjoying spring in Seoul. Thirdly, although general people enjoyed cherry blossoms, but they had dual view and attitude for cherry trees. which were well expressed in their use of them: for example, cherry blossoms, aeng and sakura were used altogether for same meaning, but night aeng or night picnic under cherry blossoms were especially used instead of vojakura when mentioning just pleasure, which meant some saw night enjoying cherry blossoms a low culture. Fourth, symbolic space of Chosun had been transformed into the space for enjoyment and consumption. Anyone who paid entrance fee could enjoy performance of revugirl, cinema and entertainment along with enjoying cherry blossoms. The still-existing strict diffrentiation of enjoyment culture by social status, class and ethnicity was dismantled from that trend and brought about a kind of disorder. From this, we could find that cherry blossoms had made a great contribution to the change of traditional enjoyment culture over the Japanese colonial period and become a popular spring enjoyment.

신안 상서고분군 일대의 지형 및 지질 특성에 관한 연구

김해경 ( Hai Gyoung Kim ),오강호 ( Kang Ho Oh ),윤석태 ( Seok Tai Youn ),고영구 ( Yeong Koo Koh ) 한국도서(섬)학회 2015 한국도서연구 Vol.27 No.3

This study focuses on the geomorphological and geological characteristics of Sangtae island. Specifically, it highlights the mutual relationship between the stones of Sangseo tumuli and the geomorphological and geological environment surrounding the island. Unlike simple burial structures, the building styles of ancient tombs mostly reflect the political and social states of a certain period, which in many cases may involve a sinister group or trading partners of that time. The stones used in the building of ancient tombs is likely to have been taken from the surrounding areas. Thus in order to complete the systematic study on ancient tomb stones, the geomorphological and geological studies on areas must proceed. The subject of this study, the Sangtae Island is classified as a coastal terrain, and subdivided into six geomorphological types of sea-cliff, wave-cut platform, marine pot-hole, gravel coast, and mud flat. The study area includes in total 12 types of geomorphological and geological characteristics. 3 of the 12 types include sea-cliff, wave-cut platform and rocky coast, while the other 9 include stratification, conglomerate, sandstone, mudstone, shale, joint, volcanic rocks and faults. Also along with these items, the island mainly comprises tuffs, clastic sedimentary rocks, acidic and intermediate volcanic rocks. Based on the scientific analysis, this study aims to investigate the stones of ancient tombs in Honam area. The results can be used as data to restore the distribution network of stones used in Sangseo tumuli.

여수 오동도의 지형·지질경관 특성 및 활용방안

김해경 ( Hai Gyoung Kim ),오강호 ( Kang Ho Oh ) 한국도서(섬)학회 2014 한국도서연구 Vol.26 No.3

The purpose of this study is to provide the basic resources for education and geotourism by investigating the geomorphological and geological landscapes of Odongdo, Yeosu-city, Korea. A geological survey in the rocky coast of Odongdo was performed for this study. The results of this study are listed below. According to the classification of the Ministry of Environment and National Institute of Environmental Research(2012), the investigated area covered six different types(sea cliff, wave cut platform, sea cave, weathering pit and so on) of geomorphological and geological landscapes. Also, based on the categorization of the Korea Environment Institute(2003), the number added up to thirteen (stratification, cross bedding, joint, dyke, volcanic rock, conglomerate, intrusive structure, etc.). The geomorphological and geological landscapes of the study area are useful materials for on-the-spot learning activities for elementary school science textbooks(4th grade) and can also provide data regarding geotourism for visitors in Odongdo, Yeosu-city, Korea.

목포 허사도와 고하도 일대의 지형 및 지질경관 특성

김해경 ( Hai Gyoung Kim ),오강호 ( Kang Ho Oh ),문병찬 ( Byoung Chan Moon ) 한국도서(섬)학회 2014 한국도서연구 Vol.26 No.4

The purpose of this study is to provide basic resources for educational application and geotourism by investigating the characteristics of geomorphological and geological landscapes distributed in Heosado and Gohado, Mokpo city, Korea. For this study, geological survey was performed in roadside out crops, sea cliff, gavel and rocky coast of Heosado and Gohado. The results of this study are as follows: According to the classification from Ministry of Environment and National Institute of Environmental Research(2012) and Korea Environment Institute(2003), three types and sixteen types of geomorphological and geological landscapes are distributed in the study area. Geomorphological and geological landscapes have value as geoheritage and basic data for geotourism in Heosado and Gohado, Mokpo city, Korea. In addition, various weathering phenomenons (dendrite, spheroidal weathering, weathering rock and weathering process by roots of plant), convolute bedding and plant fossil. Moreover, the geomorphological and geological landscapes of the study area are useful local outdoor learning materials for on-the-spot learning activities on geomorphological and geological features which are covered in science textbooks of elementary, middle and high school. More detailed investigating on the study area’s geomorphology and geology is necessary for the development of field learning programs that can be used in earth science education and geotourism.