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Kirishimayama

Sacred Volcanic Complex of Southern Japan

Elevation

1,700 m

Last Eruption

2025

Type

Shield volcano complex

Country

Japan

Location

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Volcanic Hazards & Risk Assessment

Primary Hazards

  • Lava flows and fountaining
  • Volcanic gas emissions
  • Local explosive activity

Risk Level

Population at RiskHigh
Infrastructure RiskHigh
Aviation RiskSignificant

Geological Composition & Structure

Rock Types

Primary
Unknown
Silica Content
Varied composition

Tectonic Setting

Unknown
Intraplate setting with hotspot or regional volcanic activity.

Age & Formation

Epoch
Unknown
Evidence
Unknown

Eruption Statistics & Analysis

MetricValueGlobal RankingSignificance
Total Recorded EruptionsUnknownLowModerately active volcano
Maximum VEIVEI UnknownMinorLocal impact potential
Recent Activity1 years agoVery RecentCurrently active

Monitoring & Alert Status

Monitoring Networks

Japan Meteorological Agency (JMA)
Real-time seismic monitoring
Geological Survey of Japan
Geochemical monitoring
Global Volcanism Program
International eruption database

Current Status

Active
Recent volcanic activity detected. Continuous monitoring in place.

Other Volcanoes in Japan

Interesting Facts

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Kirishimayama comprises more than 20 individual volcanic centers packed into a 20 x 30 km area β€” one of the highest concentrations of volcanic vents in Japan.

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The complex has produced four VEI 4 eruptions in the past 6,000 years, at different vents, demonstrating that explosive potential shifts between centers over time.

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Shinmoedake erupted in 2011 after 52 years of silence, hurling volcanic blocks more than 3 km and producing shockwaves felt in nearby cities.

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The filming of the James Bond movie 'You Only Live Twice' (1967) took place in the Kirishima area, with the volcanic landscape serving as the villain's secret lair.

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According to Japan's oldest mythological texts, Takachiho-no-mine is where the god Ninigi descended from heaven β€” making it one of Japan's most sacred volcanic peaks.

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Kirishima Shrine has been relocated multiple times throughout history because previous sites were destroyed by volcanic eruptions.

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The 2018 eruption of Shinmoedake produced the first lava overflow from the crater rim in the modern historical record, representing a new hazard mode for the complex.

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Ohachi, once the most active vent, has been essentially dormant since 1923, while Shinmoedake has taken over as the primary eruptive center β€” a textbook example of vent migration in a volcanic field.

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The Miyama Kirishima azalea, which blooms spectacularly across the volcanic highlands each spring, is named after the mountain and is a symbol of Kyushu's natural beauty.

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The name Karakunidake means 'Korea Peak' because Korea was supposedly visible from its 1,700 m summit on exceptionally clear days.

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The Ebino Plateau, the primary visitor gateway at 1,200 m elevation, is surrounded by volcanic crater lakes and active steam vents.

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Kirishimayama has erupted 7 times in the 21st century alone (as of 2025), making it one of the most frequently active volcanic complexes in Japan.

Frequently Asked Questions

Is Kirishimayama still active?
Yes, Kirishimayama is one of Japan's most active volcanic complexes. The most recent eruption occurred on June 22, 2025, and the complex has produced 7 eruptions in the 21st century alone. Shinmoedake, the most currently active vent, erupted significantly in 2011, 2017, and 2018. The Japan Meteorological Agency maintains continuous monitoring across the complex, with varying alert levels for different vents. The complex's 85 recorded eruptions spanning more than 9,000 years confirm that it is a persistently active volcanic system with no indication of waning activity.
What is Kirishimayama β€” is it one volcano or many?
Kirishimayama is a volcanic complex, not a single volcano. It comprises more than 20 individual volcanic centers β€” including stratovolcanoes, pyroclastic cones, maars (volcanic explosion craters), and underlying shield volcanoes β€” spread across a 20 x 30 km area in southern Kyushu, Japan. The highest peak is Karakunidake at 1,700 m. Different vents within the complex have been active at different times: Ohachi dominated historical activity from the 8th through early 20th centuries, while Shinmoedake has been the primary eruptive center since the mid-20th century.
Can you hike Kirishimayama?
Yes, Kirishimayama offers excellent hiking within Kirishima-Kinkowan National Park. The Ebino Plateau (1,200 m) serves as the main trailhead, with popular routes to Karakunidake summit (90 minutes one way), the crater lake circuit, and Takachiho-no-mine. However, trail access depends on volcanic activity β€” during periods of elevated JMA alert levels, trails within exclusion zones around active vents like Shinmoedake are closed. Always check current JMA volcanic advisories before hiking. The area is accessible from Kagoshima (45 minutes by car) and well-connected by rail.
What happened during the 2011 Shinmoedake eruption?
On January 19, 2011, Shinmoedake erupted explosively after 52 years of quiet, producing an eruption column approximately 3 km high and depositing ash across surrounding communities. Vulcanian explosions on January 26-27 hurled volcanic blocks more than 3 km and produced shockwaves felt in nearby cities. A lava dome approximately 600 m wide grew within the crater. The eruption triggered evacuations, trail closures, agricultural damage, and disruption to Kagoshima and Miyazaki airports. The event was rated VEI 3 and continued episodically through September 2011.
Why is Kirishimayama sacred in Japanese culture?
Kirishimayama is sacred because Takachiho-no-mine, one of the complex's peaks, is identified in the Kojiki and Nihon Shoki (Japan's foundational mythological texts) as the place where the god Ninigi-no-Mikoto descended from heaven to earth β€” an event called Tenson Korin that marks the mythological origin of the Japanese imperial line. Kirishima Jingu shrine at the mountain's base is one of Japan's most important Shinto shrines. Notably, the shrine has been relocated multiple times throughout history because volcanic eruptions destroyed previous sites.
How does Kirishimayama compare to Sakurajima?
Kirishimayama and Sakurajima are both active volcanic systems in southern Kyushu, separated by only about 45 km. Sakurajima erupts far more frequently β€” it produces thousands of small explosive events annually and is one of the world's most continuously active volcanoes. Kirishimayama erupts less frequently but its individual eruptions tend to be larger, with VEI 3-4 events documented in historical and geological records. Kirishimayama is a multi-vent complex with 20+ centers, while Sakurajima is a single stratovolcano within the Aira caldera. Both are monitored by JMA.
What is the connection between Kirishimayama and James Bond?
The 1967 James Bond film 'You Only Live Twice,' starring Sean Connery, was partly filmed in the Kirishima volcanic area. The volcanic landscape of the region served as inspiration for the villain's secret rocket base hidden inside a volcano. When Shinmoedake erupted dramatically in January 2011, international media drew widespread comparisons to the Bond film, noting the visual similarity between the real eruption and the movie's fictional volcanic lair. This pop-culture connection has given Kirishimayama a degree of international recognition unusual for a Japanese volcanic complex.
What are the main hazards from Kirishimayama?
Kirishimayama's primary hazards include ballistic blocks (volcanic projectiles hurled up to 3+ km from vents), pyroclastic flows, ashfall affecting communities within 20-50 km, and volcanic gas emissions. During heavy rainfall, lahars (volcanic mudflows) can mobilize loose deposits on steep slopes. The complex's location within a popular national park means hikers are frequently exposed to hazard zones. Major eruptions (VEI 4) could produce pyroclastic flows reaching 5-10 km from vents. Aviation disruption at Kagoshima and Miyazaki airports is a recurring concern during eruptions.