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National Parks · Kagoshima, Miyazaki

Kirishima-Kinkōwan National Park

霧島錦江湾国立公園きりしまきんこうわんこくりつこうえんKirishima-Kinkōwan Kokuritsu Kōen

A chain of fire from Kirishima to the tip of Satsuma

Kirishima-Kinkōwan National Park covers the volcanic chain of southern Kyushu, from the Kirishima volcanoes on the Kagoshima–Miyazaki border to Sakurajima and the calderas of Kinkō Bay, Lake Ikeda and Kaimon-dake. Kirishima was one of Japan's first three national parks in 1934; the park took its present form in 2012.

Elevation: 1,700 mArea: 366.05 km²Active volcanoNational park · 1934Japanese Geopark · 2010Japanese Geopark · 2013

Overview

Kirishima-Kinkōwan National Park follows a line of volcanoes more than 100 km long through southern Kyushu. In the north stand the Kirishima volcanoes, a cluster of more than twenty cones and craters with crater lakes, hot springs and the sacred peak of Takachiho-no-mine. To the south, Kinkō Bay (Kagoshima Bay) fills a chain of calderas, with the ever-active Sakurajima rising opposite the city of Kagoshima, and at the southern tip of the Satsuma Peninsula lie Lake Ikeda and the cone of Kaimon-dake.

The park's history mirrors Japan's changing park system. Kirishima was designated on 16 March 1934 as one of the first three national parks. In 1964 it was enlarged with Sakurajima, the Ibusuki area and Yakushima and renamed Kirishima-Yaku. In 2012 Yakushima became a national park in its own right, the waters of Kinkō Bay were added, and the park received its present name.

Few places show so clearly how people live with volcanoes: ash from Sakurajima falls on Kagoshima on many days of the year, while the same volcanism provides the hot springs of Kirishima and the sand baths of Ibusuki.

Landscape and formation

Kinkō Bay is a line of volcanic depressions. Its northern basin is the Aira caldera, formed about 30,000 years ago by an eruption so large that its pyroclastic flows covered much of southern Kyushu with the Shirasu plateau deposits. Sakurajima grew on the southern rim of this caldera; its Taishō eruption of 1914 poured out enough lava to join the former island to the Ōsumi Peninsula. The southern part of the bay belongs to the older Ata caldera, near which Lake Ikeda and the conical Kaimon-dake (924 m) formed within the last several thousand years.

The Kirishima volcanoes lie on the rim of an older caldera to the north. Karakuni-dake (1,700 m) is the highest; Takachiho-no-mine (1,574 m) has a classic cone; Shinmoe-dake erupted violently in 2011 and again in 2017–2018; and crater lakes such as Ōnami-ike, one of the highest crater lakes in Japan, fill extinct vents.

Highlights

  • Kirishima volcanoes

    霧島山Kirishima-yama

    A group of volcanoes with Karakuni-dake, Takachiho-no-mine and the active Shinmoe-dake.

  • Ebino Plateau

    えびの高原Ebino Kōgen

    A high plateau at about 1,200 m, the starting point for Karakuni-dake and the crater lakes.

  • Ōnami-ike

    大浪池Ōnami-no-ike

    A round crater lake at about 1,400 m, encircled by a walking trail.

  • Sakurajima

    桜島Sakurajima

    One of Japan's most active volcanoes, rising 1,117 m from Kinkō Bay opposite Kagoshima.

  • Lake Ikeda

    池田湖Ikeda-ko

    The largest lake in Kyushu, a caldera lake on the Satsuma Peninsula.

  • Kaimon-dake

    開聞岳Kaimon-dake

    A symmetrical volcanic cone (924 m) at the southern tip of the Satsuma Peninsula, called Satsuma-Fuji.

  • Chiringashima

    知林ヶ島Chiringashima

    An islet off Ibusuki reached across a sandbar that appears at low tide.

Nature

Ecology

Altitude and volcanic disturbance create a varied mosaic. The Kirishima slopes carry evergreen forest below and Japanese fir, hemlock and deciduous forest above, with dwarf azaleas on the summits. On Sakurajima, lava flows of different ages show every stage of plant colonisation, from bare rock to mature forest. The deep, sheltered waters of Kinkō Bay support unusual marine life, including tube worms at volcanic vents at an exceptionally shallow depth.

Flora

  • Miyama kirishima azalea

    ミヤマキリシマmiyama kirishima

    The mountain azalea named after Kirishima, colouring the volcanoes pink in late spring.

  • Nokaidō crabapple

    ノカイドウnokaidō

    A wild crabapple found only in the Ebino Plateau area, a natural monument.

  • Japanese black pine

    クロマツkuromatsu

    A pioneer tree colonising the lava fields of Sakurajima.

Fauna

  • Satsuma tube worm

    サツマハオリムシsatsuma haorimushi

    A tube worm living at volcanic gas seeps in Kinkō Bay at depths of around 100 m, far shallower than its relatives.

  • Sika deer

    ニホンジカNihon jika

    Frequently seen grazing on the Ebino Plateau.

  • Bottlenose dolphins

    ハンドウイルカhandō iruka

    Seen in Kinkō Bay, sometimes from the Sakurajima ferry.

Culture

According to the Kojiki and Nihon Shoki, Ninigi, grandson of the sun goddess Amaterasu, descended from heaven to the peak of Takachiho, and Kirishima Jingū is dedicated to him. A bronze 'heavenly spear' (Ama-no-sakahoko) stands on the summit of Takachiho-no-mine. In 1866 Sakamoto Ryōma and his wife Oryō travelled to the Kirishima hot springs and climbed the peak, a trip often described as the first honeymoon in Japan.

Around Kinkō Bay, the Shimazu lords of Satsuma ruled from Kagoshima with Sakurajima as the backdrop of their garden Sengan-en. Life with ash is part of local culture: residents collect it in special yellow bags, and Sakurajima's volcanic soil produces giant radishes and tiny mandarins.

  • Kirishima Jingū

    霧島神宮Kirishima Jingū

    A vermilion shrine rebuilt in 1715 by the Shimazu, dedicated to Ninigi.

  • Ama-no-sakahoko

    天逆鉾Ama-no-sakahoko

    The legendary spear planted on the summit of Takachiho-no-mine.

  • Kurokami buried torii

    黒神埋没鳥居Kurokami Maibotsu Torii

    A shrine gate on Sakurajima buried to its crossbeam by ash from the 1914 eruption.

  • Ibusuki sand baths

    砂むし温泉sunamushi onsen

    Bathers are buried in naturally heated sand on the beach at Ibusuki.

History

  1. c. 30,000 years ago

    The eruption of the Aira caldera forms the northern basin of Kinkō Bay.

  2. 1716–1717

    Shinmoe-dake erupts violently, burying villages and farmland on its flanks.

  3. 1866

    Sakamoto Ryōma and Oryō visit Kirishima and climb Takachiho-no-mine.

  4. 1914

    The Taishō eruption of Sakurajima joins it to the Ōsumi Peninsula.

  5. 1934

    Kirishima National Park is designated on 16 March, one of the first three.

  6. 1964

    Enlarged with Sakurajima, Ibusuki and Yakushima and renamed Kirishima-Yaku.

  7. 2011

    Shinmoe-dake has its first major magmatic eruption since 1716–1717.

  8. 2012

    Yakushima becomes a separate park; Kinkō Bay is added and the park is renamed Kirishima-Kinkōwan.

Through the seasons

Spring

Miyama kirishima azaleas bloom on the Kirishima peaks from May into early June.

Summer

Cool walking on the Ebino Plateau; the prevailing winds tend to carry Sakurajima's ash over Kagoshima city.

Autumn

Maple colour on the Ebino Plateau and around the crater lakes; clear views of Kaimon-dake.

Winter

Rime ice on the Kirishima summits; the mild coast around Ibusuki is at its most pleasant, and rape blossoms appear there in January.

Routes and trails

  • Karakuni-dake from Ebino Plateau

    The ascent of the highest Kirishima peak, with views over Shinmoe-dake and Takachiho; open only when the volcanic alert level allows.

  • Takachiho-no-mine from Takachiho-gawara

    A steep climb on loose scoria to the summit and its spear, about one and a half hours up.

  • Sakurajima lava trails

    Walking paths across the Taishō lava field near the ferry port, with views of the summit.

  • Kaimon-dake spiral trail

    A path that winds around the cone to the summit, with views over the sea and Lake Ikeda.

Practical notes

  • Frequent car ferries cross from Kagoshima to Sakurajima in about fifteen minutes.
  • Entry restrictions around Shinmoe-dake, Iōyama and Sakurajima's summit craters change with the volcanic alert level; check the Japan Meteorological Agency and local announcements.
  • Ash falls on Kagoshima on many days; eye protection and an umbrella are useful.
  • Kirishima is reached from Kagoshima by train or from Kagoshima Airport by bus; a car helps to explore the plateau.

Frequently asked questions

Why was the park renamed in 2012?

Yakushima, which had been part of Kirishima-Yaku National Park since 1964, became a separate national park, and the sea of Kinkō Bay was added; the park was renamed Kirishima-Kinkōwan.

Is it safe to visit Sakurajima?

The island is inhabited and much visited; the summit area is permanently closed and a restricted zone surrounds the active craters. Follow local guidance and the JMA alert level.

What is Kinkō Bay?

The local name for Kagoshima Bay, a sea-filled chain of calderas formed by huge eruptions, with Sakurajima in its midst.

What does Kirishima have to do with Japanese mythology?

Takachiho-no-mine is one of the places where the heavenly grandson Ninigi is said to have descended to earth, and Kirishima Jingū is dedicated to him.

Which peak is the highest?

Karakuni-dake in the Kirishima group, at 1,700 m.

Sources

  1. 1.環境省_霧島錦江湾国立公園 (opens in a new tab) — 環境省 (Ministry of the Environment)
  2. 2.環境省_国立公園_国立公園一覧 (opens in a new tab) — 環境省 (Ministry of the Environment)
  3. 3.全国の活火山 (opens in a new tab) — 気象庁 (Japan Meteorological Agency)
  4. 4.日本ジオパークネットワーク (opens in a new tab) — 日本ジオパークネットワーク (Japanese Geoparks Network)

Editorial team · Published: