SockMonkey.com
Field Guide · Entry № 003

Aogashima

Around a hundred and seventy people live on the floor of an active volcanic crater, inside a second, larger crater, on an island the ferry usually cannot reach.

Vertical aerial view of Aogashima, an oval island ringed by sheer cliffs, its interior a green crater basin with a smaller forested cone standing inside it

Photograph: Geospatial Information Authority of Japan (Kokudo Chiriin) · Attribution only licence (GSI Japan)

Where
Izu Islands
Tokyo Metropolis, Japan
Coordinates
32.4570° N
139.7670° E
Biome
Subtropical volcanic island
Area
c. 6–8.75 km² (sources vary)
pop. c. 156–170
Status
Active volcano, continuously
monitored by JMA
Best visited
April–June, Sept–Nov
From Tally’s diary

An island that is a volcano wearing a smaller volcano like a hat. Dinner was cooked by the ground itself, which I thanked, quietly, in case it heard. The boat could not promise to come back on time. I could not promise to want it to.

The short answer

Aogashima is a volcanic island in the Izu chain, about 350 kilometres south of Tokyo and administered by it, covering somewhere between about 6 and 8.75 square kilometres depending on the source. Around 160 to 170 people live there, making it the least populated village in Japan. The island is a double caldera: a large outer crater called Ikenosawa with a secondary cone, Maruyama, rising from its floor, and the village sits inside. The Japan Meteorological Agency lists it among Japan's continuously monitored active volcanoes and applies its five-level eruption warning scale; the older A/B/C activity ranking that appears in some travel writing is no longer JMA's current framework.

Why it's worth knowing

The shape is the thing. Sheer cliffs rise straight out of the Pacific on every side, then drop away inwards into a green bowl, and inside that bowl is another, smaller volcano. People live in the gap between them. Seen from the air it looks less like geography than like a diagram of itself.

The second thing is that this is Tokyo. Administratively, legally, postally: Tokyo. The same metropolis that contains Shibuya Crossing also contains a village of 170 people on the rim of an active crater, reachable only when the sea permits.

It is the least populated municipality in Japan, and it is governed from one of the largest cities on Earth.

The field notes

1785

The island's current shape dates from a catastrophic eruption in 1785, following several years of increasing seismic activity. It destroyed nearly all vegetation and killed a large proportion of the roughly 327 people then living there. The survivors evacuated to Hachijōjima, and Aogashima stood empty for around fifty years before people returned.

They returned because the island, for all its obvious hostility, offers a rare combination: volcanic soil that grows crops, fresh water from natural springs, fish in the surrounding Kuroshio Current, and free geothermal heat. That last item is not incidental.

Hingya

Steam vents constantly from fissures between the inner and outer craters. The islanders call it hingya, and they have built the practical life of the village around it. There is a communal steam cooker where you can put in eggs or sweet potatoes and come back later. There is a public geothermal sauna and bathhouse. And there is a salt works: seawater from the Kuroshio Current evaporated using nothing but volcanic steam, producing Hingya salt, which is sweeter than ordinary salt because the current's water carries markedly more calcium.

It is a closed loop of a kind almost nowhere manages — the hazard and the utility are the same object.

Getting on and off

Access is the defining fact of life here. There is no airport. One ferry a day runs from Hachijōjima, and by widely repeated local accounting it is cancelled roughly 60 per cent of the time, sometimes for a week at a stretch, because of wind and swell at the tiny harbour. A helicopter runs once daily with around nine seats, cancelled perhaps 30 per cent of the time.

The practical strategy is to base yourself on Hachijōjima near the port and go when conditions allow — and to accept that you may also be stuck on Aogashima for several days longer than planned. Some visitors consider that the good outcome.

Tally’s list
  1. Cook something in the steam and eat it while the ground stays warm underfoot.
  2. Watch the boats being lifted from the sea like teacups.
  3. Stand on the rim at dusk and look inward, then outward, then inward again.
  4. Try the local drink where every bottle holds its own opinion.
  5. Check the ferry. Check it again. Shrug magnificently.
The Relic

An egg cooked in the ground. At the hingya vents there is a communal steam cooker: a lidded box over a fissure where the island's own heat comes up. You lower in eggs or sweet potatoes, wait, and eat something warmed by the volcano you are standing inside. It costs nothing and it has never once been switched off.

Tally, in the marginBreakfast cooked by a volcano — the earth showing off, and me applauding with a spoon.

Getting there

Everything routes through Hachijōjima, 70 kilometres north, which has an airport served from Tokyo and an overnight ferry. From there, the Aogashima ferry takes about two and a half hours; the helicopter takes twenty minutes and needs booking well in advance.

Accommodation is a handful of small minshuku guesthouses and a free island campsite — all of which must be reserved before arrival. There is one general store. A rental car is close to essential, since the single road climbs from the port over the crater rim to the village. The Oyama Observation Park viewpoint gives the classic view down into the double caldera, and the absence of light pollution makes the night sky extraordinary.

Mark this place

Asia →

Common questions

Where is Aogashima?

Aogashima is a volcanic island in the Izu chain, roughly 350 kilometres south of Tokyo in the Philippine Sea, and is administered as part of Tokyo Metropolis. It covers roughly 6 to 8.75 square kilometres depending on the source, and is the southernmost and most isolated inhabited island of the Izu group.

How many people live on Aogashima?

Around 160 to 170 people live on Aogashima — recent figures trend toward the lower end and continue to fall — which makes it the least populated village of any municipality in Japan. Accommodation for visitors is limited to a few small guesthouses and a single island campsite, all of which must be booked in advance.

Is Aogashima an active volcano?

Yes. The Japan Meteorological Agency lists Aogashima among Japan's continuously monitored active volcanoes and began Volcanic Alert Level operation for it, alongside Hachijōjima, on 30 May 2018; the level has stood at 1 — the lowest of five, meaning the volcano is active but no eruption is forecast — since then. Its last major eruption was in 1785; geothermal steam still vents continuously from fissures between the inner and outer craters.

What happened on Aogashima in 1785?

A catastrophic eruption in 1785 destroyed nearly all vegetation on Aogashima and killed a large proportion of the roughly 327 residents. Survivors evacuated to Hachijojima, and the island remained uninhabited for around fifty years before people returned.

What is hingya?

Hingya is the local name for the geothermal steam that vents from fissures on Aogashima. It is odourless and non-toxic, and islanders use it to run a communal steam cooker, a public sauna and bathhouse, and a salt works that evaporates Kuroshio Current seawater using volcanic steam alone.

How do you get to Aogashima?

Aogashima is reached only via Hachijojima, 70 kilometres north, by a daily ferry taking about two and a half hours or a helicopter taking twenty minutes with around nine seats. The ferry is reportedly cancelled roughly 60 per cent of the time due to wind and swell, so visitors are advised to base themselves near the Hachijojima port and travel when conditions allow.

Field Correspondence

Know somewhere that belongs here?

The Field Guide grows by recommendation. If there is a place you love — somewhere strange, overlooked, or simply worth the trip — tell us about it and why it matters. Good suggestions get researched, written up, and credited to the person who sent them in.

Suggest a place →

Notes on sources. This entry draws on Tokyo Metropolitan Government and official Tokyo travel materials, Japan Meteorological Agency volcanic classification, and published accounts of the island's geology and settlement history. The frequently cited ferry cancellation rate of around 60 per cent is a widely repeated local figure rather than a published statistic. Population figures vary slightly by year. The frequently repeated description of Aogashima as a “Class C” volcano does not come from any JMA alert scale: it traces to the active-volcano ranking the Coordinating Committee for Prediction of Volcanic Eruptions published in January 2003, which sorted volcanoes by a 10,000-year activity index rather than by current risk. JMA's own five-level Volcanic Alert Level scheme is a separate thing and has applied to Aogashima only since 2018. Written and fact-checked by SockMonkey. Last reviewed 24 August 2026.