Daikonshima Second Lava Tunnel (Ryukeido): Explore a 190,000-Year-Old Underground Volcanic Cave

Ryukeido (Dragon Valley Cave), a nationally designated Natural Monument beneath Daikonshima Island in Matsue, Shimane Prefecture, is a basalt lava tunnel formed approximately 190,000 years ago. Featuring Japan's only known intra-cave volcanic vent and endemic cave-dwelling species found nowhere else on Earth, this rare geological wonder can be explored on guided geopark tours.

Daikonshima Second Lava Tunnel (Ryukeido): A Rare Underground Journey into Japan's Volcanic Past

Hidden beneath the tranquil surface of Daikonshima Island in Shimane Prefecture lies a remarkable natural wonder — the Daikonshima Second Lava Tunnel, locally known as Ryukeido (Dragon Valley Cave). Designated as a National Natural Monument of Japan in 1935, this lava tube offers visitors a rare chance to step inside a 190,000-year-old volcanic formation and witness geological features found almost nowhere else on Earth.

Daikonshima sits in the middle of Lake Nakaumi, a brackish lagoon straddling the border of Shimane and Tottori prefectures. Despite its flat, unassuming landscape, the island is in fact a volcanic island — born from eruptions that took place approximately 200,000 years ago. The summit of Otsukayama, at just 42 meters above sea level, holds the distinction of being one of the lowest volcanoes in all of Japan. The Ryukeido lava tunnel is living proof of that fiery origin.

How the Lava Tunnel Was Formed

The Daikonshima Second Lava Tunnel was created during the Late Pleistocene period, roughly 190,000 years ago, when basaltic lava erupted from small vents on the island. As the surface of the lava flow cooled and hardened, the still-molten interior continued to flow, eventually draining away and leaving behind a hollow tube approximately 81 meters in length.

What makes this tunnel scientifically extraordinary is the discovery, during a detailed survey in 2004 by the Volcanic Cave Society (formerly the Fuji Volcanic Cave Research Association), that the tunnel contains an intra-cave lava vent — essentially a volcanic crater inside the cave itself. This is an extremely rare geological feature with no other known example in Japan. The formation, called "Kamidamari" (divine pool), is a dome-shaped cavity believed to mark the point where lava last erupted and then solidified as volcanic activity ceased.

Unlike the nearby First Lava Tunnel (Yukido), which was formed by gas pockets trapped within stagnant lava, the Second Lava Tunnel was created by the internal flow of lava beneath an already-hardened crust. This distinction makes the two tunnels complementary examples of different volcanic processes occurring on the same small island.

Why It Was Designated a Natural Monument

The Daikonshima Second Lava Tunnel was designated a National Natural Monument on June 7, 1935. The official designation noted the tunnel's nearly straight formation extending 81.1 meters from south to northwest, with a branch tunnel diverging from the central section. The cave floor displays distinctive ropy (pahoehoe-type) lava textures, with shelf-like ridges along both walls and short lava stalactites hanging from the ceiling — features comparable to those found in the famous lava tunnels at the base of Mount Fuji.

In Japan, only 13 lava caves have been designated as Natural Monuments. Of these, 11 are located near Mount Fuji in Yamanashi and Shizuoka prefectures. The remaining two are both on Daikonshima Island, making this tiny volcanic island an exceptionally significant site for volcanological research. The First Lava Tunnel holds the even higher distinction of Special Natural Monument status, though it is currently closed to the public due to the risk of collapse.

Highlights and What to See

Descending into Ryukeido is a true adventure. The entrance leads underground to a pitch-dark world where the temperature remains at a constant 15°C year-round — refreshingly cool in summer and surprisingly warm in winter. Visitors are equipped with flashlights and rubber boots for the approximately 40-minute guided exploration.

Inside, the cave walls vividly preserve the traces of ancient lava flows in both linear and swirling patterns. The ceiling features small lava stalactites — droplets of molten rock that solidified in mid-drip thousands of years ago. The dome-shaped Kamidamari chamber, believed to be an intra-cave volcanic vent, is a highlight that conveys the raw power of the island's volcanic origins.

Perhaps the most fascinating aspect of Ryukeido is its unique cave ecosystem. The perpetual darkness has given rise to highly specialized organisms, including eyeless amphipod crustaceans that have adapted to life without light. The cave is also home to a species of ground beetle (genus Trechiama) found nowhere else in the world — with only nine individuals ever recorded. Encountering these rare creatures during a visit is a matter of extraordinary luck, but their very existence underscores the cave's immense scientific value.

Visiting Information and Guided Tours

The Daikonshima Second Lava Tunnel is normally kept locked and can only be entered with a guided tour. Tours are conducted by members of the Izumo-no-Kuni Geoguide Association, who provide expert commentary on the cave's geology, biology, and cultural significance.

Scheduled guided tours are available on Saturdays and Sundays at 2:00 PM (subject to weather conditions and schedule changes). Private group tours can also be arranged by contacting the geoguide association in advance. The guide fee is 500 yen per person, with free admission for junior high school students and younger. Each tour accommodates up to 15 participants.

Flashlights and rubber boots are provided free of charge. The cave interior is completely dark and the floor can be slippery, so visitors should wear clothing that can get slightly dirty. Children's rubber boots may not be available, so families are advised to bring their own.

Daikonshima Island and Surrounding Attractions

Daikonshima is a compact island — just 3 kilometers east to west and 2 kilometers north to south — that can be circled by car in about 30 minutes. Despite its small size, the island offers a surprising variety of attractions beyond the lava tunnels.

Yuushien Garden

The island's most famous attraction is Yuushien, a magnificent stroll-style Japanese garden spanning over 40,000 square meters. The garden is renowned for its year-round peony displays, with over 250 varieties cultivated on the island — Japan's largest peony production area. During Golden Week (late April to early May), the spectacular sight of 30,000 peony blossoms floating on the garden's pond draws visitors from across the country. Seasonal highlights include iris in summer, vivid autumn foliage illuminations, and delicate winter peonies.

Eshima Ohashi Bridge (Betabumi-zaka)

Connecting Daikonshima to Sakaiminato in Tottori Prefecture, the Eshima Ohashi Bridge became an internet sensation for its dramatic, seemingly impossibly steep incline when photographed from a certain angle. Often called "Betabumi-zaka" (full-throttle slope), it is one of the largest rigid-frame bridges in Japan and offers panoramic views of Lake Nakaumi.

Shimane Peninsula and Nakaumi Geopark

Daikonshima is part of the Shimane Peninsula, Lake Shinji, and Lake Nakaumi Geopark, which was certified as a Japanese Geopark in 2017. The geopark encompasses geological sites spanning millions of years of Earth's history, from ancient seabed formations to volcanic islands. Visiting the lava tunnel as part of a broader geopark itinerary provides a deeper understanding of the region's geological story.

Korean Ginseng Heritage

Daikonshima has been a center for Korean ginseng (Unshu Ninjin) cultivation for over 200 years. The volcanic soil provides ideal growing conditions, and the island's ginseng is considered among the finest in the world. Visitors can learn about ginseng processing at Yuushien's museum and purchase ginseng products including tea, extract, and even ginseng ice cream.

Access

By car, Daikonshima is approximately 20 minutes from central Matsue via Route 431, crossing the Nakaumi Ohashi Bridge. From Sakaiminato, the island is about 15 minutes by car via the Eshima Ohashi Bridge. Public bus service is available from Matsue Station (Matsue City Bus), with the nearest stop at Yushien-iriguchi. Visitors arriving by bus should note that the lava tunnel is a short walk from the main road, and having a rental car or taxi is recommended for the most convenient access.

📍 Plan Your Visit to Shimane
Find tours, activities & transport passes near Daikonjima Second Lava Tunnel
[ Izumo Taisha Shrine & Adachi Museum Gardens ]

Q&A

QCan I visit the Daikonshima Second Lava Tunnel without a reservation?
AThe tunnel is normally locked. Scheduled guided tours are available on Saturdays and Sundays at 2:00 PM, but advance reservation is recommended. For weekday visits or group tours, please contact the Izumo-no-Kuni Geoguide Association in advance by email at izumo.geoguide@gmail.com.
QIs the tour available in English?
ATours are primarily conducted in Japanese. International visitors are encouraged to bring a Japanese-speaking companion or use a translation app. Informational signboards near the entrance include some English explanations.
QWhat should I wear for the cave tour?
ARubber boots and flashlights are provided. Wear comfortable clothes that you don't mind getting slightly dirty. The cave maintains a year-round temperature of about 15°C, so a light jacket may be useful even in summer. Children's boots may not be available, so please bring your own if visiting with small children.
QIs the cave accessible for people with mobility difficulties?
AThe cave requires descending steps and walking on uneven, slippery surfaces in complete darkness. It is not wheelchair accessible and may be challenging for visitors with significant mobility limitations. Please consult with the geoguide association regarding your specific needs.
QWhat is the difference between the First and Second Lava Tunnels?
AThe First Lava Tunnel (Yukido / Ghost Cave) is a Special Natural Monument with a loop-shaped formation totaling about 207 meters, but it is currently closed to the public due to collapse risk. The Second Lava Tunnel (Ryukeido / Dragon Valley Cave) is a Natural Monument with a straight formation of about 81 meters and is open for guided visits. Despite different formation mechanisms, both offer invaluable geological insights.

Basic Information

Official Name Daikonshima Daini Yougan Zui-do (Daikonshima Second Lava Tunnel)
Common Name Ryukeido (Dragon Valley Cave)
Designation National Natural Monument (designated June 7, 1935)
Location Teratsu, Yatsuka-cho, Matsue City, Shimane Prefecture
Total Length Approximately 81.1 meters
Age Approximately 190,000 years old (Late Pleistocene)
Rock Type Basalt (porous volcanic basalt)
Internal Temperature Approximately 15°C year-round
Guided Tour Fee 500 yen per person (free for junior high school students and younger)
Tour Duration Approximately 40 minutes
Scheduled Tours Saturdays and Sundays at 2:00 PM (subject to change)
Tour Operator Izumo-no-Kuni Geoguide Association (izumo.geoguide@gmail.com)
Managing Body Matsue City

References

大根島第二熔岩隧道 - 文化遺産オンライン
https://bunka.nii.ac.jp/heritages/detail/210990
国指定天然記念物「大根島第二溶岩隧道」竜渓洞(見学可)- 大根島観光協会
https://kankou-daikonshima.jp/tourist_info/lava_tunnels/lava_tunnels_02
大根島第二熔岩隧道 - Wikipedia
https://ja.wikipedia.org/wiki/%E5%A4%A7%E6%A0%B9%E5%B3%B6%E7%AC%AC%E4%BA%8C%E7%86%94%E5%B2%A9%E9%9A%A7%E9%81%93
大根島第二熔岩隧道(竜渓洞)- 松江市ホームページ
https://www.city.matsue.lg.jp/soshikikarasagasu/bunkasportsbu_bunkazaika/rekishi_bunkazai/3/1/1/ryukeido.html
竜渓洞(熔岩洞窟)- 神々のふるさと山陰
http://furusato.sanin.jp/p/area/matsue/7/
竜渓洞ガイドのご案内について - 島根半島・宍道湖中海ジオパーク
https://kunibiki-geopark.jp/news/%E7%AB%9C%E6%B8%93%E6%B4%9E%E3%82%AC%E3%82%A4%E3%83%89%E3%81%AE%E3%81%94%E6%A1%88%E5%86%85%E3%81%AB%E3%81%A4%E3%81%84%E3%81%A6/
溶岩トンネル - 大根島観光協会
http://kankou-daikonshima.jp/tourist_info/lava_tunnels

Last verified: 2026.03.03

Nearby heritages