• THE NATIONAL ATLAS OF KOREA I
    • Ver 2014
    • Ver 2019
    • Ver 2024
  • THE NATIONAL ATLAS OF KOREA II
    • Ver 2016
    • Ver 2020
    • Ver 2025
  • THE NATIONAL ATLAS OF KOREA IIII
    • Ver 2016
    • Ver 2021
  • Comprehensive Edition
    • Ver 2017
    • Ver 2022
  • for Children

    THE NATIONAL ATLAS OF KOREA 2025

    • Overview
    • Index
      • Preface
      • Contents
      • Korean Satellite Images
      • Map of Korea
    • THE LAND WE LIVE ON
      • Topography
        • Overview of the Topography of the Korean Peninsula
        • Rivers and Watershed Environments
        • The Five Major Rivers of South Korea
        • Mountainous Landforms
        • Mountainous Landforms2
        • Fluvial Landforms
        • Coastal Landforms
        • Volcanic Landforms
        • Karst Landforms
        • Natural Parks and Conservation Areas
        • Natural Monument Landforms·
        • Wetlands
        • National Geoparks
        • Outlying Islands
        • Dokdo
        • Shifting Perspectives on Geomorphology
        • Mountain Ridges
      • Geology
        • General Geology·
        • History of the Geological Survey in Korea·
        • Characteristics of Geological Time·
        • Distribution of Vertebrate Fossil Footprints
        • Geologic Resources
        • Faults and Earthquakes
        • Active Fault Investigation
      • Geohazards
        • Landslide
        • Earthquakes and Tsunamis
        • Ground Subsidence
        • Coastal Erosion
        • Overseas Resource Exploration and International Relief Activities
      • Soils
        • Soil Status
        • Soil Survey
        • Soil Ecosystem Services
    • COEXISTENCE IN ECOSYSTEMS
      • Ecosystems
        • Ecological and Natural Map
        • Nationwide Natural Environment Survey
        • Ecosystem Types
        • Ecosystem Productivity
        • Ecosystem Services
        • Ecosystem and Carbon Neutrality
        • Demilitarized Zone
        • Cultural Ecology of the Baekdudaegan·
      • Environmental Conservation
        • Ecosystem Management
        • Endangered Species·
        • Invasive Animal Species
        • Invasive Plant Species
        • 5th National Biodiversity Strategy
        • International Cooperation on Ecology·
    • WEATHER AND CLIMATE IN OUR DAILY LIVES
      • Weather and Climate
        • Climate Overview
        • Meteorological Observation
        • History of Meteorology
        • Weather Forecasts and Warnings
        • Regional Climate
        • Climate Elements and Days of Phenomena·
        • Applied Climate Indices
        • Climate Extremes
        • Start and End Dates of Seasons·
      • Climate Change
        • Climate Change
        • Global Climate Change
        • International Cooperation on Climate Change
    CollapseDownload
    • PDF Download
      • contens
      • korea_map
      • the land we live on
      • coexistence in ecosystems
      • weather and climate
      • photo sources
    • Lesson Plan Download
      • Introduction
      • ├ Supplemental Material 1
      • └ Supplemental Material 2
      • USA APHG Curriculum Articulation
      • └ Supplemental Material
        • Lesson 1 : Talking Sejong Metropolitan Autonomous City
      • ├ Supplemental Material 1
      • └ Supplemental Material 2
      • Lesson 2 : Global Diffusion of Korean Culture and associated Societal Impacts
      • ├ Supplemental Material 1
      • ├ Supplemental Material 2
      • └ Supplemental Material 3
      • Lesson 3 : South Korea’s Population Reality
      • ├ Supplemental Material 1
      • └ Supplemental Material 2
      • Lesson 4 : Korean Development – Where/When/ and Why?
      • └ Supplemental Material 1
      • Lesson 5 : Exploring Patterns of Development
      • └ Supplemental Material
      • Lesson 6 : Examining Korea’s Urban Dynamics
      • Lesson 7 : Cultural Landscapes of South Korea
      • └ Supplemental Material
      • Lesson 8 : Rice is Nice
      • └ Supplemental Material
      • Lesson 9 : Using the National Atlas of Korea to Teach about Scale and Types of Maps
        • └ Supplemental Materia
      • Lesson 10 : Life in South Korea Apartment Living_Baseball_Religions_Politics and American Food
    • KOREA_shape Download
      • Administration.zip
      • Basemap.zip
      • Economy.zip
      • Education.zip
      • Population.zip
      • Population_Gender and Age.zip
      • README.xlsx

    Ecosystem Types

    ❚ 고지도

    • Forest Ecosystem-NDVI

    A forest ecosystem refers to the state in which various organisms inhabiting a vegetated area coexist while maintaining close relationships. In forest ecosystems, plants are autotrophs that directly synthesize chemical energy using light energy and atmospheric carbon dioxide. Among organisms that cannot synthesize nutrients on their own, primary consumers obtain nutrients by feeding on plants. Secondary consumers then obtain nutrients by preying on primary consumers. Some organisms decompose dead organisms, enriching forest soils and contributing to nutrient cycling.

    Thus, plants—the starting point of the food web—form the basis of biodiversity in forest ecosystems. Among them, trees perform particularly diverse roles. In forests, vegetation of varying heights—from shrubs to tall trees—form layered structures that provide habitats for insects, birds, and many other organisms. In addition, tree root systems prevent soil erosion and thereby reduce the risk of landslides. Moreover, living trees, dead trees, plant litter, and soil act as major carbon storages that capture greenhouse gases in the atmosphere and mitigate climate change.

    In this way, plants are important components for both biotic and abiotic elements within forest ecosystems. Meanwhile, because plants lack locomotion and generally remain in place after germination, they respond more sensitively to environmental changes than other organisms. Given these traits, plants can easily die due to climate change and human disturbances, necessitating efforts to seek sustainable use and conservation of forest vegetation.

    The Normalized Difference Vegetation Index (NDVI), which identifies the spatial distribution of vegetation from remote sensing imagery, is useful not only for distinguishing vegetation from surrounding objects but also for measuring relative vegetation vigor. In Korea, more than 60% of the national territory is forested, providing a wide range of ecosystem services supported by a diversity of forest ecosystems and high biodiversity. Therefore, it is important to continuously monitor the health of forest ecosystems and establish conservation plans. However, conducting field surveys over vast forest areas requires substantial time and labor. By calculating NDVI from remote sensing imagery, it is possible to remotely and cost-effectively detect forest damage from natural disasters and assess tree vigor, thereby improving the efficiency of forest ecosystem monitoring. In Korea, the Korea Forest Service actively employs remote sensing techniques alongside field surveys for forest monitoring. Accordingly, forest type maps, forest soil maps, and forest water maps are produced and made publicly available through the Forest Spatial Information Service. This enables various stakeholders to conduct monitoring, establish conservation plans, and explore sustainable use strategies for Korea's forests.

    • Forest Ecosystem-Mountain Wetland Distribution Map

    Wetlands are generally areas where moisture determines habitat conditions and the survival of plants and animals. Because changes in microclimate, soil, or water supply can rapidly alter conditions, wetlands are among the ecosystems most vulnerable to climate change and human threats. Mountain wetlands host fewer species than typical wetlands but provide unique habitats for particular plants and continuously supply moisture to the headwaters of streams. Accordingly, mountain wetlands are recognized as refuges and hotspots of biodiversity. Because mountain wetlands excel at carbon storage and are often located in relatively inaccessible areas—making them highly conservable—they have been the focus of various studies.

    Mountain wetlands in Korea are broadly classified into natural wetlands, abandoned paddy wetlands, and artificial wetlands. Natural wetlands arise from natural causes, abandoned paddy wetlands are former cultivation sites in forests that have been left fallow, and artificial wetlands are constructed for agricultural activities, such as reservoirs. As of 2021, there were 455 mountain wetlands nationwide, covering approximately 276.2 ㎢. Vascular plants native to these sites comprise 927 taxa (113 families, 423 genera, 819 species, 23 subspecies, 78 varieties, and 7 forms). This accounts for about 20% of all vascular plants on the Korean Peninsula. Since forest ecosystem health stems from biodiversity and forest biodiversity is based on vegetation diversity, conserving the high plant species diversity of mountain wetlands is crucial.

    • River Ecosystem - River Aquatic Ecological Health Map (Riparian Habitat Index)

    River ecosystems in Korea encompass not only major rivers such as the Hangang, Geumgang, and Nakdonggang but also small local streams, forming a broad ecosystem. These rivers are divided into mountain streams, upper, middle, lower reaches, and estuaries according to terrain and flow velocity, and differences in the physical and chemical environments of each section lead to substantial variation in species composition and distribution. For example, upper reaches and mountain streams have low water temperatures, fast flow, and high oxygen levels, whereas in lower reaches and estuaries, increased temperature and nutrient inputs raise biodiversity. The basic structure of river ecosystems is linked through food chains: phytoplankton (producers) are consumed by herbivores (zooplankton, aquatic insects, minnows), which are preyed upon by primary carnivores (crucian carp, carp), and then by secondary carnivores (catfish, snakehead). However, in upper reaches and mountain streams, low temperatures limit phytoplankton growth, so food webs are primarily based on leaf litter and organic matter. There, herbivorous aquatic insects such as caddisflies break down and consume leaf litter, after which carnivorous insects or small fish prey on them, maintaining the energy flow.

    Currently, river ecosystems face serious threats from human activities. Chemical pollutants not only deteriorate water quality but, along with river channelization, have caused the loss of natural river morphology. In addition, the construction of various hydraulic structures has obstructed fish migration routes, making it difficult for them to reach spawning grounds and weakening ecological connectivity. As a result, biodiversity declines, food webs become imbalanced, and overall ecosystem functions deteriorate. These issues go beyond simple pollution, leading to the loss of ecosystem services and highlighting the need for sustainable management.

    • River Ecosystem - River Aquatic Ecological Health Map (Riparian Vegetation Index, Fish Index, Periphyton Index, Benthic Macroinvertebrate Index)

    For evaluating aquatic ecological health, biological indicators such as riparian habitat conditions, riparian vegetation, fish, periphytons, and benthic macroinvertebrates are measured to compute the Habitat and Riparian Index (HRI), Riparian Vegetation Index (RVI), Fish Assessment Index (FAI), Trophic Diatom Index (TDI), and Benthic Macroinvertebrate Index (BMI). Based on these results—considering species diversity and abundance and the physical environment—ecosystem health is evaluated and classified into five grades: Excellent (A), Good (B), Fair (C), Poor (D), and Very Poor (E). Thus, systematic accumulation and assessment of field survey data are essential to securing the sustainable health of river ecosystems and ultimately provide the foundation for long-term ecological stability and resilience.

    • Coastal Ecosystem-Coastal Dune Distribution Map

    Korea is surrounded on three sides by the sea, and the coastlines of the South and West Seas are particularly intricate, resulting in long shorelines. In addition, thousands of islands of various sizes further increase the total length of the coastline. The coast is the zone where land meets the sea, linking terrestrial and marine ecosystems. For this reason, unique transitional ecosystems not found elsewhere are observed at the interface between terrestrial and marine environments.

    Coastal dunes are sand ridges formed when beach sand, transported by ocean currents and coastal currents, is blown inland and accumulates parallel to the shoreline. In Korea, coastal dunes are mainly distributed along the West and East Seas. Coastal dunes act as reservoirs of beach sand and groundwater and, ecologically, as transition zones linking marine and terrestrial ecosystems. These areas are fundamentally terrestrial environments composed of sand, but when groundwater emerges at the surface to form dune wetlands, they also take on wetland characteristics. Moreover, because the sand originates from the sea, it tends to exhibit higher salinity than inland sand. Therefore, biotic communities inhabiting coastal dunes possess unique characteristics rarely found elsewhere. For example, plants commonly observed in Korean coastal dunes—such as Zoysia sinica, Glehnia littoralis, Calystegia soldanella, Messerschmidia sibirica, and Carex kobomugi—are terrestrial species that are specifically adapted to the high salinity of dune sands.

    Since 2003, the Ministry of Climate, Energy and Environment has collected ecological information on coastal dunes through a nationwide detailed coastal sand dune survey. Through this effort, detailed data on dune formation processes, conservation status, and ecological conditions are generated, enabling the development of effective management plans to protect high quality coastal dune ecosystems through evaluation of their functions and values.

    • Coastal Ecosystem-Tidal Flat Distribution Map

    Tidal flats are submerged at high tide and exposed at low tide. In Korea, tidal flats are mostly distributed along the West and South Seas. These areas consist mainly of silt and sand and are generally very flat. Tidal flats host numerous invertebrates such as polychaetes and crustaceans. Fish such as gobies also inhabit these areas, as well as microscopic phytoplankton. Birds use tidal flats as habitats and fly to them at low tide to feed on clams and small fish. Plants grow where tidal submergence is infrequent. Because tidal flat sediments are strongly influenced by seawater, halophytes inhabiting these areas are adapted to high salinity. Salicornia and Suaeda species, which redden the Yellow Sea tidal flats in Korea, are representative halophytes.

    In 1999, Korea enacted the Coastal Management Act and the Wetlands Conservation Act to protect these areas. As coastal wetlands, tidal flats are legally recognized for their ecological value, and biodiversity conservation is promoted through the establishment of a basic wetland conservation plan. Korean tidal flats also serve as stopover sites for internationally endangered migratory waterbirds and support exceptionally high levels of biodiversity. For these reasons, the Seocheon, Gochang, Shinan, and Boseong-Suncheon tidal flats have been inscribed as UNESCO World Heritage Sites.

    • Marine Ecosystem-Marine Ecological Index

    The East, West, and South Seas of Korea each display distinct marine-ecological characteristics. In the East Sea, the East Korea Warm Current and the North Korea Cold Current intersect, and differences in temperature and salinity create environments suitable for diverse fish species. In the Yellow Sea, river inflows from Korea and China result in relatively low salinity and high nutrient concentrations compared to other seas. The South Sea has high marine species diversity, including species typically found in warmer regions worldwide, such as the Indo-Pacific bottlenose dolphin, which can be found around Jeju Island.

    The Marine Ecology Map, based on the Marine Ecosystem Act, grades the ecological and landscape values of marine ecosystems nationwide using the National Comprehensive Marine Ecosystem Survey and the National Detailed Marine Ecosystem Survey. Basic data used for grading include planktonic organisms that drift with water flow, benthic organisms living on the seabed, nekton capable of swimming, and data from marine environmental surveys. A Grade 1 zone denotes areas and waters where marine ecosystems are particularly outstanding or marine landscapes are especially scenic. Such zones may include primary habitats, spawning grounds, or key migration routes of protected marine species; locations at the biogeographic limits of species; representative types of marine vegetation; and areas with particularly rich marine biodiversity and highly valuable marine biological resources. Grade 2 zones are areas with future conservation value or areas outside Grade 1 zones that are necessary for protecting the Grade 1 zones. Grade 3 zones are those not classified as Grade 1, Grade 2, or separate management areas and may be subject to development or use.

    • Marine Ecosystem-Conservation and Management Areas

    A Protected Marine Area is a zone designated and managed by the nation or local governments in specific public waters to conserve marine ecosystems and seascapes of special value. Protected Marine Areas designated under the Marine Ecosystem Act are selected based on criteria such as ecosystem naturalness, biodiversity, geomorphological, geological, and ecological uniqueness, productivity, presence of protected species habitats, ecological representativeness, and scenic beauty. Once designated, these areas are managed to protect marine organisms, ecosystems, and landscapes, with management objectives established for each area and progress evaluated through continuous monitoring. Local stakeholders—including residents, civic groups, and academia—participate as co-managers to enhance the ecological, economic, and socio-cultural values of Protected Marine Areas. Since the designation of the Sinduri Coastal Sand Dune as a Protected Marine Area in October 2002, additional protected areas have been continuously designated.

    Environmental Management Sea Areas began to be designated in 2000 following legal revisions in the 1990s, and include the environmental conservation water and special management water. An environmental conservation water refers to waters designated within natural environment conservation areas for the protection and cultivation of fishery resources or waters requiring continued conservation due to their good marine environmental condition. A special management water denotes waters where maintaining marine environmental standards is difficult and where serious obstacles to marine environmental conservation exist or are likely to occur. The management of Environmental Management Sea Areas follows five principles: sustainability, integrated management, precautionary management, ecosystem-based management, and participatory and cooperative management.

    prevnext

    대한민국 국가지도집
    ×
    • Index
      • Preface
      • Contents
      • Korean Satellite Images
      • Map of Korea
    • THE LAND WE LIVE ON
      • Topography
        • Overview of the Topography of the Korean Peninsula
        • Rivers and Watershed Environments
        • The Five Major Rivers of South Korea
        • Mountainous Landforms
        • Mountainous Landforms2
        • Fluvial Landforms
        • Coastal Landforms
        • Volcanic Landforms
        • Karst Landforms
        • Natural Parks and Conservation Areas
        • Natural Monument Landforms·
        • Wetlands
        • National Geoparks
        • Outlying Islands
        • Dokdo
        • Shifting Perspectives on Geomorphology
        • Mountain Ridges
      • Geology
        • General Geology·
        • History of the Geological Survey in Korea·
        • Characteristics of Geological Time·
        • Distribution of Vertebrate Fossil Footprints
        • Geologic Resources
        • Faults and Earthquakes
        • Active Fault Investigation
      • Geohazards
        • Landslide
        • Earthquakes and Tsunamis
        • Ground Subsidence
        • Coastal Erosion
        • Overseas Resource Exploration and International Relief Activities
      • Soils
        • Soil Status
        • Soil Survey
        • Soil Ecosystem Services
    • COEXISTENCE IN ECOSYSTEMS
      • Ecosystems
        • Ecological and Natural Map
        • Nationwide Natural Environment Survey
        • Ecosystem Types
        • Ecosystem Productivity
        • Ecosystem Services
        • Ecosystem and Carbon Neutrality
        • Demilitarized Zone
        • Cultural Ecology of the Baekdudaegan·
      • Environmental Conservation
        • Ecosystem Management
        • Endangered Species·
        • Invasive Animal Species
        • Invasive Plant Species
        • 5th National Biodiversity Strategy
        • International Cooperation on Ecology·
    • WEATHER AND CLIMATE IN OUR DAILY LIVES
      • Weather and Climate
        • Climate Overview
        • Meteorological Observation
        • History of Meteorology
        • Weather Forecasts and Warnings
        • Regional Climate
        • Climate Elements and Days of Phenomena·
        • Applied Climate Indices
        • Climate Extremes
        • Start and End Dates of Seasons·
      • Climate Change
        • Climate Change
        • Global Climate Change
        • International Cooperation on Climate Change

    Overview of the Topography of the Korean Peninsula

    THE LAND WE LIVE ON
    | Topography

    The Korean Peninsula, surrounded by the sea on three sides, possesses a longer coastline than other countries with similar land areas. The East Coast, which has a relatively straight shoreline, stands in stark contrast to the South and West Coasts, which feature highly indented coastlines. As of 2023, South Korea’s total coastline length was measured at 15,297 km, consisting of 9,682 km of natural coastline and 5,615 km of artificial coastline. Since the first official coastline statistics were released, the length of the natural coastline has been decreasing, while the artificial coastline has been increasing.

    One of the most significant characteristics of the Korean Peninsula’s topography is the prominence of mountainous terrain running in a NNW-SSE (North-Northwest to South-Southeast) direction, specifically the Nangnimsanmaek (Nangnim Mountain Range) and Taebaeksanmaek (Taebaek Mountain Range). The Sikhote-Alin Mountains in the northeast, along with the Hamgyeongsanmaek (Hamgyeong Mountain Range) and Taebaeksanmaek in Korea, were formed as the northern and western margins of the East Sea rim were uplifted during the creation of a back-arc basin along the continental margin. The formation of the Ulleung Basin in the East Sea is closely linked to tectonic uplift of the Taebaeksanmaek.

    The average elevation of the Korean Peninsula is approximately 448 m, which is significantly lower than the East Asian average (910 m). However, its average slope is 5.7°, which is about 2° steeper than the overall East Asian average of 3.9°. While the Peninsula’s elevation is not high compared to the East Asian average, it is characterized by a high distribution of steep mountainous terrain. Korea’s high mountains are asymmetrically distributed, concentrated in the east and north along the axes of the Taebaeksanmaek, Nangnimsanmaek, and Hamgyeongsanmaek. The Hamgyeongsanmaek includes peaks such as Dojeongsan, Gwanmobong, and Duryusan, while the Nangnimsanmaek features Huisaekbong, Maengbusan, and Nangnimsan, all of which exceed 2,000 m in elevation. The Taebaeksanmaek, stretching approximately 500 km from near Yeongheung Bay in North Korea to Busan, is the principal mountain range of the Korean Peninsula. However, its elevation is much lower than that of the Hamgyeongsanmaek or Nangnimsanmaek, with major peaks like Geumgangsan, Seoraksan, and Odaesan reaching heights of around 1,500 to 1,700 m.

    • Area Distribution by Elevation
    Overview of the Topography of the Korean Peninsula
    • Relief and Cross-Section of Korean Topography
    대한민국 고대의 역사는 만주와 한반도를 중심으로 전개되었다. 기원전 2333년 최초의 국가인 고조선이 만주와 한반도를 중심으로 성립되었으며, 고조선 시대는 기원 전 108년까지 지속되었다. 이후 부여와 동예, 옥저, 삼한의 부족 국가가 성립되었다. 이 시기를 일반적으로 원삼국 시대라 하는데, 이 당시에는 만주와 한반도 전체가 우리나라 역사의 강역이었다. 부여의 세력권은 주로 만주를 중심으로 하였으며, 동예와 옥저는 한반도의 북부와 중부, 마한  진한  변한의 삼한은 한반도의 중부와 남부에 위치하였다.
    기원 전 1세기에서 서기 1세기 사이 이전의 부족 국가들을 계승하고 병합하며 고구려, 백제, 신라, 가야가 건국되었다. 이 시기를 삼국 시대라하며, 이 시기 역시 만주와 한반도 전체가 우리나라 역사의 강역이었다. 고구려는 주로 만주와 한반도 북부를 중심으로 하였고, 신라는 한반도의 동남부, 백제는 서남부를 중심으로 하였다. 7세기를 전후로 신라가 고구려와 백제를 병합하며 대동강에서 원산만에 이르는 한반도 내부 영역에서 통일 국가를 이루었다. 그리고 698년 고구려 유민에 의하여 발해가 건국되었다. 이 시기를 남북국 시대라고 한다.
    고려 시대와 조선 시대에는 북방 영토를 개척하고 확장하려는 노력이 이루어졌다. 고려는 993년 거란의 1차 침입을 막아 내며 강화 회담을 통하여 강동 육주의 점유를 확인하였고, 1033년부터 천리장성을 축조하여 거란·여진과의 경계로 삼았다. 이를 통하여 현재의 신의주에서 함흥 인근을 잇는 영역으로의 북방 영토 회복을 이루었고, 이후 고려 후기에 이르기까지 북방 영토 확장 노력을 지속하였다. 조선 시대에도 북방 영토 확장을 위한 노력은 계속되었다. 이와 같은 노력의 결과, 15세기 조선은 압록강 유역에 사군을, 두만강 유역에 육진을 설치하였다. 이는 압록강과 두만강에 이르는 현재 대한민국 영토의 회복을 의미한다. 18세기 조선은 백두산 정계비를 세워 당시 중국 청(淸)과의 국경을 표시하기도 하였다.
    근대와 현대, 대한민국의 역사는 조선에 이은 대한 제국의 성립, 일본에 의한 강점과 독립, 미국과 구소련에 의한 군정과 한국전쟁으로 이어졌다. 당시 국제 사회의 제국주의 움직임에 대응하여 고종은 1897년 대한 제국을 선포하고 내부적인 개혁을 추진하였으나, 결국 동아시아에서 세력을 확대하던 일본에 의하여 1910년 강점당하여 일시적으로 대한민국은 영토를 상실하게 되었다. 이 시기를 일제 강점기라 하며, 일제 강점기는 1945년까지 지속되었다. 국권 회복을 위한 독립 운동은 국내외에서 지속되었고, 일본의 제2차 세계 대전 패전과 함께 우리 민족은 독립을 맞이하였다.
    그러나 대한민국 영토는 북위 38도선을 기점으로 남북으로 분단되었으며, 이와 같은 분단은 1948년 남한과 북한에 각각의 정부가 수립되며 고착화되었다. 이후 남과 북은 1950년 한국전쟁이라는 비극을 겪게 되었다. 3년 넘게 지속된 한국전쟁은 1953년 7월 27일 휴전으로 중단되었고, 대한민국은 현재까지 70여 년 간 휴전 상태인 채로 분단 상황이 지속되고 있다. 70여 년 간 남한과 북한은 경쟁과 대립의 역사를 이어왔으나, 이산가족 상봉과 정상 회담, 개성 공단의 운영 등을 통하여 상호 신뢰를 구축하여 분단을 극복하려는 노력도 이어가고 있다.
    일반적으로 고조선에서 기원 전후의 시기를 요하 시대라고 한다. 요하를 둘러싸고 기원 전 4세기부터 기원 후 4세기까지 1,000여 년 동안 한민족 세력, 중국 세력, 북방 세력이 각축을 벌였다. 한민족의 역사로 보면, 고조선과 고구려가 활약하던 시대로, 요하를 둘러싸고 중국 세력과 고조선, 고구려가 쟁패를 벌이던 시대이다. 한민족 최초의 국가를 이룬 고조선이 세력을 확장하여 요하로 진출하면서 요하 일대는 중국의 연과 세력 다툼이 시작되었다. 고조선은 기원 전 4세기 말경 요하 일대를 연에게 빼앗긴 이래 끝내 요하를 회복하지 못하고 멸망했다. 기원 후 1세기부터 성장한 고구려는 요하를 확보하기 위해 북방 세력의 선비족과 전쟁을 치루었다. 결국 4세기 말 고구려 광개토대왕 때에 이르러 요하를 확보하였다. 이 시대의 고조선과 고구려의 요하 영유권은 한민족 국가들에게 요동(요하의동쪽 지역)에 대한 역사적 연고권을 마련했고, 이 연고권을 바탕으로 요동정벌이 여러 차례 단행되었다.
    5세기 전후, 즉, 4~7세기는 한강 시대라고 한다. 이 시기는 고구려, 백제, 신라가 한강에서 대치하여 한반도 주도권을 두고 각축을 벌이던 시대이다. 한강은 백두대간 줄기에서 발원하여 황해로 흘러들면서 한반도 허리부를 가로지른다. 북쪽으로는 광주산맥과 철령 부근까지 물줄기가 뻗쳐 있고, 남쪽으로는 소백산맥과 광주~음성을 연결하는 산지에 둘러싸여 그 유역이 광대하다. 4세기 말 이래 7세기까지 300여 년은 한강을 둘러싸고 패권 다툼이 벌어진 시대로, 이른바 고구려, 백제, 신라의 삼국 시대에 해당한다.
    가장 먼저 한강을 선점한 국가는 한강 유역에서 건국한 백제였다. 4세기 말 고구려가 남하하여 한강을 차지하면서 한강은 백제와 고구려의 대치선이 되었다. 그리하여 한강을 둘러싼 삼국의 영토 경쟁은 치열해졌다. 결국 신라는 당과 연합해 고구려와 백제를 멸망시켰다. 그러나 신라는 한반도 전역을 차지하려는 당과 결전을 치루어 당을 몰아냈다. 이때 만들어진 통일 국가의 골격은 고려와 조선을 지나면서 거의 그대로 유지되었다.
    한편, 고구려 멸망 30년 후 고구려 계승국을 자처하는 발해가 고구려 옛땅에서 건국했다. 발해와 통일신라는 대동강 선에서 7세기 말에서 10세기초에 이르는 200여 년 동안 대치했다. 이 시대를 대동강 시대, 이국(二國)시대, 혹은 남북국 시대로 부른다. 5경, 15부, 62주로 구성된 발해는 건국 후 비약적인 영토 확장을 이루었다. 동북 만주의 쑹화강, 헤이룽강 일대를 확보한 후에 발해는 한반도 방향으로 남진했다. 이를 견제하던 당은8세기 초 신라에 발해 공격을 요청했고 신라는 원병을 보냈다. 이후 9주5소경의 행정구역을 둔 통일신라는 대동강 일대를 영토로 편입하기 위한 북진 정책을 가속화하였다. 남진하려는 발해와 북진하려는 신라는 대동강선에서 대치하였으나 이 시대에는 두 세력이 공존하던 대치선이라는 특징이 있다. 한강 시대와는 달리 대동강 시대는 별다른 전쟁이 없었다. 이는 두 나라가 평화 공존의 관계였음을 나타내며, 두 나라 모두 당의 견제를 받고 있었다는 점을 보여 준다. 하지만 10세기 초 당의 멸망으로 인한 혼란은 동북아시아 국제 정세를 개편시켰고 이 과정에서 발해가 멸망했다. 발해의 멸망은 한민족 영토사에서 만주 지역에 대한 실효적 지배가 상실된 것을 의미한다. 같은 시기에 통일신라도 쇠퇴했고, 이후 후삼국 시대가 시작되었다.
    비무장 지대(DMZ: Demilitarized Zone)는 조약이나 협정에 의하여 무장이 금지된 완충 지대로 군대 주둔과 무기 배치, 군사 시설 설치가 금지되는 지역이다. 우리나라의 비무장 지대는 한국전쟁을 끝내기 위해 체결된 휴전협정(1953년)에 의해 설정되었다. 당시의 군사 접촉선이 군사 분계선이 되었으며, 이 군사 분계선으로부터 남쪽과 북쪽으로 각각 2 km, 총 4 km 구역을 비무장 지대로 설정하였다.
    민간인 통제 구역은 비무장 지대와 민간인 통제선 사이의 구역이다. 민간인 통제선은 고도의 군사적 활동이 이루어지는 군사 분계선 인접 지역으로의 민간인 출입을 통제하기 위하여 법적으로 지정한 출입 통제선이다. 민간인 통제선은 1954년에 처음 설정되었으며, 재산권의 제약을 해소하는 측면에서 현재까지 3차에 걸쳐 민간인 통제 구역의 범위를 축소하는 조정이 이루어졌다. 현재의 민간인 통제선은 군사 분계선 이남 10 km 범위 이내에서 지정되어 있다.
    비무장 지대와 민간인 통제 구역은 일부 민통선 마을의 경작을 제외하고는 상대적으로 인간의 접촉이 최소화된 공간이다. 이에 따라 비무장 지대와 민간인 통제 구역에는 자연환경이 잘 보전되어 있으며, 다양한 생물종이 서식하고 있다. 특히 사향노루, 산양, 수달, 흰꼬리수리, 검독수리와 같은 멸종위기 야생 동식물 1급 동물들과 담비, 하늘다람쥐, 참매, 날개하늘나리 등의 멸종위기 야생 동식물 2급 동식물들이 서식하고 있는 것으로 알려져 있다. 최근에는 이와 같이 잘 보전된 자연환경과 전쟁 및 군사와 관련된 역사적 유적 등을 관광 자원으로 활용하는 접경 지역 관광도 점차 활성화되고 있다.
    2018년에는 ‘남북 정상 간 합의 및 부속 합의’ 등을 통해 DMZ 평 화 지대화의 여건을 마련했으며, 남 북 정상은 2018년 4월 27일 판문점 선언에서 비무장 지대를 실질적 평 화 지대로 만들어 나가기로 합의하였다. 대한민국 정부는 비무장 지대에 평화를 공고히 정착시키고, 접경 지역의 번영·발전을 촉진하기 위해 ‘DMZ 평화의 길을 추진하고 있다. 현재 ‘DMZ 평화의 길’ 체험은 2018 년 9월 19일 남북 군사 합의에 따라 감시 초소(GP) 철거, 유해 발굴 등 긴장 완화 노력이 이루어지고 있는 3개 지역(파주, 철원, 고성)에서 할 수 있다.

     

    4,320
    7,108,250
     

     

    National Geography Information Institute (NGII) Copyright,

    Ministry of Land Infrastructure and Transport 

    국토교통부 국토지리정보원 

     

     

     

    4,320
    7,108,250

    National Geography Information Institute (NGII)

    Copyright,

    Ministry of Land Infrastructure and Transport

    국토교통부 국토지리정보원