{"id":311,"date":"2025-08-28T10:03:00","date_gmt":"2025-08-28T01:03:00","guid":{"rendered":"https:\/\/geo-itoigawa.com\/en\/?page_id=311"},"modified":"2026-08-26T09:25:07","modified_gmt":"2026-08-26T00:25:07","slug":"area14","status":"publish","type":"page","link":"https:\/\/geo-itoigawa.com\/en\/igp\/area\/area14\/","title":{"rendered":"14. Renge"},"content":{"rendered":"\n\n<h1>Renge Area<img decoding=\"async\" src=\"\/wp-content\/uploads\/2022\/10\/yama_icon02.png\" \/><\/h1>\nVolcanic Fumaroles and Glacial Wetlands\n\n\t<p>The Renge Geosite is located in the northernmost part of the <b>Chubu Sangaku National Park<\/b>. It was here in <b>1902<\/b> where Professor Naokata Yamasaki of Tokyo University confirmed the <b>first example of glacial topography in the country<\/b>. In the region are several examples of glacial wetlands as well as ponds. <b>Heimanotaira Marsh<\/b>, created as a result of glacial activity, features a dazzling display of alpine flowers which come into bloom starting in early summer and continuing through autumn.<\/p>\n<p>Another feature of the area is the <b>asymmetric mountain ridges<\/b> formed by large-scale collapses. These collapses continue to shape the topography of the region today, even as recently as <b>2007<\/b>, when the peak of Mt. Korenge collapsed forming a large, new ridge and causing the mountain to lose <b>3 meters<\/b> in height. You can enjoy the beautiful, rugged landscapes formed by these collapses while relaxing in the hot spring baths of <b>Renge Onsen<\/b>, located in the middle of a region of intense fumarolic activity.<\/p>\n<p>Along a mountain trail leading to the peak of nearby Mt. Shirouma, the remains of the <b>Renge Mine<\/b>&#8216;s offices, smelting furnaces, and tunnel entrances can be seen. A silver and lead mine, Renge Mine operated from the 1840s until the 1920s. In <b>1894<\/b>, <b>Rev. Walter Weston<\/b> stopped by this mine while climbing the trail up Mt. Shirouma. Rev. Weston noted in his travel journals that the miners there asked him questions about the quality of the minerals in the area.<\/p>\n\t<img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/sites\/2\/2026\/01\/map14.png\" usemap=\"#area_illust\" id=\"area_illust_image\" width=\"992\" alt=\"Renge Area\" \/>\n    <map name=\"area_illust\">\n  <area shape=\"rect\" coords=\"279,395,477,458\" href=\"#n01\" alt=\"Heima-no-Traira Wetlands\" title=\"Heima-no-Traira Wetlands\" \/>\n  <area shape=\"rect\" coords=\"23,79,217,138\" href=\"#n02\" alt=\"Renge Onsen Outdoor Hot Springs\" title=\"Renge Onsen Outdoor Hot Springs\" \/>\n  <area shape=\"rect\" coords=\"20,256,217,313\" href=\"#n03\" alt=\"Shiraike Pond\" title=\"Shiraike Pond\" \/>\n  <area shape=\"rect\" coords=\"333,469,580,532\" href=\"#n04\" alt=\"Former Site of Renge Mine Office\" title=\"Former Site of Renge Mine Office\" \/>\n  <area shape=\"rect\" coords=\"56,160,294,218\" href=\"#n05\" alt=\"Renge Onsen Lodge\" title=\"Renge Onsen Lodge\" \/>\n  <area shape=\"rect\" coords=\"528,568,776,631\" href=\"\/en\/igp\/24area\/area10\/\" alt=\"Tsugami Shindo Area\" title=\"Tsugami Shindo Area\" \/>\n  <area shape=\"rect\" coords=\"121,14,360,76\" alt=\"Shirouma-Oike Volcano\" title=\"Shirouma-Oike Volcano\" \/>\n  <area shape=\"rect\" coords=\"541,13,732,67\" alt=\"Former Smelting Sites\" title=\"Former Smelting Sites\" \/>\n  <area shape=\"rect\" coords=\"749,14,952,67\" alt=\"Mt. Shirouma\" title=\"Mt. Shirouma\" \/>\n  <area shape=\"rect\" coords=\"773,125,976,177\" alt=\"Mt. Yukikura\" title=\"Mt. Yukikura\" \/>\n  <area shape=\"rect\" coords=\"784,195,972,247\" alt=\"Tunnel Entrance\" title=\"Tunnel Entrance\" \/>\n  <area shape=\"rect\" coords=\"222,587,428,647\" alt=\"Glacial Remains\" title=\"Glacial Remains\" \/>\n  <area shape=\"rect\" coords=\"692,491,887,550\"  alt=\"Mt. Asahi\" title=\"Mt. Asahi\" \/>\n    <\/map>\n\t<h2>1Heima-no-Traira Wetlands<\/h2>\n\t\t\t\t<img decoding=\"async\" src=\"https:\/\/geo-itoigawa.com\/wp-content\/uploads\/2023\/06\/heimanotaira.jpg\" alt=\"\" itemprop=\"image\" onerror=\"this.style.display='none'\" loading=\"lazy\" \/>\n\t<p>Renge Nature Trail &#8211; Heima-no-Traira Wetlands<\/p>\n\t<p>Located just west of Renge Onsen Hot Springs, this marshland becomes awash with color from early summer through autumn when its many native alpine plants come into bloom.<\/p>\n<p>Sand and debris intrusion from the surrounding mountains threaten this marsh, which is becoming smaller and shallower over time.<\/p>\n\t<h2>2Renge Onsen Outdoor Hot Springs<\/h2>\n\t\t\t\t<img decoding=\"async\" src=\"https:\/\/geo-itoigawa.com\/wp-content\/uploads\/2023\/06\/rengeonsen.jpg\" alt=\"\" itemprop=\"image\" onerror=\"this.style.display='none'\" loading=\"lazy\" \/>\n\t<p>Outdoor Bath &#8211; Senki-no-yu<\/p>\n\t<p>Renge Onsen Lodge boasts five different baths: one indoor and four outdoor. However, unlike many other hot springs baths, these outdoor baths are truly outdoor, without walls or barriers of any kind.<\/p>\n<p>About 15 minutes from the lodge, the hiking trail enters a fumarolic field in which steam billows from the earth. Scattered about here are four baths, roughly at a height of 1550 meters, offering an unparalleled experience as you bathe not only in hot spring water, but in the majesty of the Northern Alps.<\/p>\n<p>The baths here are mixed bathing. Please pay at the lodge before entering.<\/p>\n\t<h2>3Shiraike Pond<\/h2>\n\t\t\t\t<img decoding=\"async\" src=\"https:\/\/geo-itoigawa.com\/wp-content\/uploads\/2023\/06\/siraike_1.jpg\" alt=\"\" itemprop=\"image\" onerror=\"this.style.display='none'\" loading=\"lazy\" \/>\n\t<p>This 112,000 sq. meter pond, found at about 1,090 m above sea level, formed in a basin created by lava flow off nearby Shirouma-Oike Volcano. It is only about 5 m deep at its deepest, but its water is exceptionally clear. The reflection of the mountains in Shiraike Pond is particularly stunning.<\/p>\n\t<h2>4Remains of Renge Mine<\/h2>\n\t\t\t\t<img decoding=\"async\" src=\"https:\/\/geo-itoigawa.com\/wp-content\/uploads\/2023\/02\/077_\u5869\u8c37\u7cbe\u932c\u6240\u8de1.jpg\" alt=\"\" itemprop=\"image\" onerror=\"this.style.display='none'\" loading=\"lazy\" \/>\n\t<p>Former Smelting Sites<\/p>\n\t<p>The remains of Renge Mine, which operated from the Edo Period until the Taisho Period, can still be seen today, including the foundations of the smelters, the mine office, and the mine tunnel entrance. Mountaineer Rev. Walter Weston, one of the first to bring modern mountaineering to Japan, visited Renge Mine in 1894 during his trek across the Japanese Alps. He wrote about this visit in his book &#8220;Mountaineering and Exploration in the Japanese Alps.&#8221;<\/p>\n\t<h2>5Renge Onsen Lodge<\/h2>\n\t\t\t\t<img decoding=\"async\" src=\"https:\/\/geo-itoigawa.com\/wp-content\/uploads\/2023\/06\/rengeonsenrojji.jpg\" alt=\"\" itemprop=\"image\" onerror=\"this.style.display='none'\" loading=\"lazy\" \/>\n\t<p>Located above the clouds at 1,500 m above sea level, the hot spring baths of Renge Onsen have been enjoyed for centuries. Enjoy majestic panoramas of the Northern Alps while soaking in natural hot spring waters. Pay at Renge Onsen Lodge before using the baths. Outdoor baths are mixed bathing.<\/p>\n\t<h2>Renge Nature Trail<\/h2>\n\t\t\t\t<img decoding=\"async\" src=\"https:\/\/geo-itoigawa.com\/wp-content\/uploads\/2023\/06\/kamosikatenboudai.jpg\" alt=\"\" itemprop=\"image\" onerror=\"this.style.display='none'\" loading=\"lazy\" \/>\n\t<p>he Renge Nature Trail circles around Heima-no-taira Marsh and includes many sections of boardwalk. It is a very long course if completely walked, so light hiking equipment is recommended.<\/p>\n\t\t\t\t<img decoding=\"async\" src=\"https:\/\/geo-itoigawa.com\/wp-content\/uploads\/2023\/02\/44\u30a6\u30a7\u30b9\u30c8\u30f3.jpg\" alt=\"\" itemprop=\"image\" onerror=\"this.style.display='none'\" loading=\"lazy\" \/>\n\t<p>Statue of Rev. Walter Weston<\/p>\n\t<p>An English clergyman and mountain climbing enthusiast, he is called &#8220;the father of modern Japanese mountaineering&#8221; for his extensive mountaineering exploits in Japan during the late 19th and early 20th century.<\/p>\n\t<h2>Rev. Walter Weston<\/h2>\n\t     View Map\n<iframe src=\"https:\/\/www.google.com\/maps\/d\/embed?mid=1ad_pjaBEGKS7DF4KZUHg2pfqGnopViA&#038;ehbc=2E312F\"><\/iframe>\n<h3>\n\t\t\t Area Access &#038; Closures\t<\/h3>\n\t<p>\u3010Renge Road (Hiwa-daira to Renge Onsen\u3011Closed for Winter from 19 November 2026 until July 2027.<br \/>\n\u3010Shiraike Forest Road (Kijiya to Shiraike Pond and Hiwa-daira\u3011Currently Open. Closed most years from November until June.<\/p>\n\n<img loading=\"lazy\" decoding=\"async\" src=\"\/wp-content\/uploads\/2023\/03\/mont-bell_logo.jpg\" alt=\"mont-bell\" width=\"120\" height=\"60\" \/>\n<p><a href=\"https:\/\/club.montbell.jp\/privilege\/fshop\/aboutarea\/disp.php?friendarea_id=18\" target=\"_blank\" rel=\"noopener\">Friend Area Special<\/a><br \/>Mt. Shirouma &#8211; Renge Hot Springs Lodge<\/p>\n\t<ul>\n    <li><a href=\"..\/area13\/\"><u>13. Himekawa Gorge Area<\/u><\/a><\/li>\n    <li><a href=\"..\/area15\/\"><u>15.Itoigawa Coast Area<\/u><\/a><\/li>\n<\/ul>\n\t<ul class=\"d-md-flex area_link ml-0\">\n    <li class=\"bg-hisui\"><div><a href=\"\/en\/igp\/area\/#hisui_area\">\n        <span>Discover Jade<\/span>\n        <img decoding=\"async\" src=\"\/wp-content\/uploads\/2022\/10\/hisui_icon.png\">\n        <\/a><\/div>\n    <\/li>\n    <li class=\"bg-history\"><div><a href=\"\/en\/igp\/area\/#history_area\">\n        <span>Birth of the Japanese Archipelago<\/span>\n        <img decoding=\"async\" src=\"\/wp-content\/uploads\/2023\/01\/history_icon_w.png\">\n        <\/a><\/div>\n    <\/li>\n    <li class=\"bg-yama\"><div><a href=\"\/en\/igp\/area\/#yama_area\">\n        <span>Breathtaking Mountains<\/span>\n        <img decoding=\"async\" src=\"\/wp-content\/uploads\/2022\/10\/yama_icon02.png\">\n        <\/a><\/div>\n    <\/li>\n<\/ul>\n\n","protected":false},"excerpt":{"rendered":"<p>Renge Area Volcanic Fumaroles and Glacial Wetlands The Renge Geosite is located in the northernmost part of the Chubu Sangaku National Park. It was here in 1902 where Professor Naokata Yamasaki of Tokyo University confirmed the first example of glacial topography in the country. In the region are several examples of glacial wetlands as well as ponds. Heimanotaira Marsh, created as a result of glacial activity, features a dazzling display of alpine flowers which come into bloom starting in early summer and continuing through autumn. Another feature of the area is the asymmetric mountain ridges formed by large-scale collapses. These collapses continue to shape the topography of the region today, [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":103,"menu_order":10,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"inline_featured_image":false,"footnotes":""},"class_list":["post-311","page","type-page","status-publish","hentry","no-featured-image"],"acf":[],"aioseo_notices":[],"aioseo_head":"\n\t\t<!-- All in One SEO 5.0.3 - aioseo.com -->\n\t<meta name=\"description\" content=\"Volcanic Fumaroles and Glacial Wetlands\" \/>\n\t<meta name=\"robots\" content=\"max-image-preview:large\" \/>\n\t<link rel=\"canonical\" href=\"https:\/\/geo-itoigawa.com\/en\/igp\/area\/area14\/\" \/>\n\t\t<meta name=\"generator\" content=\"All in One SEO (AIOSEO) 5.0.3\" \/>\n\t\t<meta property=\"og:locale\" content=\"en_US\" \/>\n\t\t<meta property=\"og:site_name\" content=\"Itoigawa UNESCO Global Geopark -\" \/>\n\t\t<meta property=\"og:type\" content=\"article\" \/>\n\t\t<meta property=\"og:title\" content=\"14. 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