[{"data":1,"prerenderedAt":74},["ShallowReactive",2],{"$fgAbQlSFvFskDbb55oxvzEC-x2q1a5DJZDFck8Gu5iCM":3},{"heritage":4,"country":27,"related":32},{"id":5,"nameJa":6,"nameEn":7,"nameKo":8,"descriptionJa":9,"descriptionEn":10,"descriptionKo":11,"category":12,"countryCode":13,"region":14,"latitude":15,"longitude":16,"dateInscribed":17,"isInDanger":18,"criteria":19,"image":21},1698,"佐渡島の金山","Sado Island Gold Mines","사도 섬 금광","佐渡島の金山は、新潟県沿岸から西方約35kmの佐渡島に位置する連続遺産である。異なる非機械化採掘方法を示す3つの構成要素からなる。佐渡島は火山性の島で、南西から北東に伸びる2つの並行する山脈が国仲平野で隔てられている。金銀鉱床は熱水が地表近くに上昇して岩石に脈を形成することで生じた。構造運動により地表の鉱床は海底に沈み、後に再び隆起した。西三川地区では砂金が採取され、大佐渡山脈南端の相川鶴子地区では風化した火山岩の露出した鉱脈が地表や地下深くで採掘された。採掘活動や社会・労働組織を反映する有形遺構が、地上・地下の考古学的要素および景観として保存されている。","The Sado Island Gold Mines is a serial property located on Sado Island, some thirty-five kilometres west of the Niigata Prefecture coast. It is formed of three component parts illustrative of different unmechanised mining methods. Sado Island is of volcanic origin and features two parallel mountain ranges stretching from southwest to northeast and separated by one alluvial plain, the Kuninaka Plain. Gold and silver deposits were formed by the rising of hydrothermal water close to the land surface and forming veins in the rock; tectonic activity first submerged the surface deposits to the seabed, which was later raised again by tectonic movements. Placer deposits were exploited in Nishimikawa Area, located on the north-western side of the Kosado Mountains. In addition, the weathering of the volcanic rock exposed ore veins, which were mined underground at the land surface and deep underground in the Aikawa-Tsurushi Area, at the southern end of the Osado Mountains range. Mostly tangible attributes reflecting mining activities and social and labour organisation are preserved as archaeological elements, both above and below ground, and landscape features.","사도 섬 금광은 니가타현 해안에서 서쪽으로 약 35km 떨어진 사도 섬에 위치한 연속유산이다. 서로 다른 비기계화 채광 방법을 보여주는 3개의 구성 요소로 이루어져 있다. 사도 섬은 화산 기원으로 남서에서 북동으로 뻗어 있는 두 개의 평행한 산맥과 그 사이의 쿠니나카 평야로 이루어져 있다. 금은 퇴적물은 열수가 지표 가까이 상승하여 암석에 광맥을 형성하면서 생성되었으며, 지각 활동으로 표면 퇴적물이 먼저 해저로 침강한 후 다시 지각 운동에 의해 융기되었다. 사금 퇴적물은 코사도 산맥 북서쪽의 니시미카와 지역에서 채굴되었다. 또한 화산암의 풍화로 노출된 광맥은 오사도 산맥 남단의 아이카와-쓰루시 지역에서 지표 및 지하 깊숙한 곳에서 채굴되었다. 채광 활동과 사회적·노동 조직을 반영하는 유형적 속성이 지상과 지하의 고고학적 요소 및 경관 특징으로 보존되어 있다.","Cultural","JPN","Asia",38.0408333333,138.2577777778,2024,false,[20],"iv",{"url":22,"author":23,"license":24,"licenseUrl":25,"sourceUrl":26},"https://d1irxcpmeew2vr.cloudfront.net/heritage-commons/1698.jpg","Indiana jo","CC BY-SA 4.0","https://creativecommons.org/licenses/by-sa/4.0","https://commons.wikimedia.org/wiki/File:%E9%B6%B4%E5%AD%90%E9%8A%80%E5%B1%B1_03.jpg",{"code":13,"nameJa":28,"nameEn":29,"nameKo":30,"region":14,"flagUrl":31},"日本","Japan","일본","https://flagcdn.com/w160/jp.png",[33,38,43,49,54,59,64,69],{"id":34,"nameJa":35,"nameEn":36,"nameKo":37,"category":12},660,"法隆寺地域の仏教建造物群","Buddhist Monuments in the Horyu-ji Area","호류지 지역의 불교 기념물",{"id":39,"nameJa":40,"nameEn":41,"nameKo":42,"category":12},661,"姫路城","Himeji-jo","히메지성",{"id":44,"nameJa":45,"nameEn":46,"nameKo":47,"category":48},662,"屋久島","Yakushima","야쿠시마","Natural",{"id":50,"nameJa":51,"nameEn":52,"nameKo":53,"category":48},663,"白神山地","Shirakami-Sanchi","시라카미산치",{"id":55,"nameJa":56,"nameEn":57,"nameKo":58,"category":12},688,"古都京都の文化財（京都市・宇治市・大津市）","Historic Monuments of Ancient Kyoto (Kyoto, Uji and Otsu Cities)","고대 교토의 역사 기념물 (교토, 우지, 오쓰 시)",{"id":60,"nameJa":61,"nameEn":62,"nameKo":63,"category":12},734,"白川郷・五箇山の合掌造り集落","Historic Villages of Shirakawa-go and Gokayama","시라카와고와 고카야마의 역사 마을",{"id":65,"nameJa":66,"nameEn":67,"nameKo":68,"category":12},775,"広島平和記念碑（原爆ドーム）","Hiroshima Peace Memorial (Genbaku Dome)","히로시마 평화 기념관 (원폭 돔)",{"id":70,"nameJa":71,"nameEn":72,"nameKo":73,"category":12},776,"厳島神社","Itsukushima Shinto Shrine","이쓰쿠시마 신사",1782463016883]