The place used to be known as the Tōmigahana (look-off nose) but in 1922 the writer Tokutomi Sohō rebranded it as the Daikanbō (great viewpoint), apparently at the local mayor’s request.
The mayor was right. For this viewpoint did deserve a more dignified appellation. And it takes a moment before we can calibrate our eyes to the view's sheer scale.
We’re standing on the brink of the “gairin-kan” – the outer rim of Aso’s giant caldera – and far off, over a sea of morning haze, float the five central peaks, including the two we visited yesterday. Everything within our gaze is part of one huge volcano.
“So they really do look like a reclining Buddha,” says the Sensei. We agree that the crags over on the left of the central mountains do indeed resemble an upturned face. The likeness is so often remarked that it even has a name: the Nehanzō, although the bronze versions seen at temples are usually lying on their sides.
Whether recumbent or reclining, no Buddha was mentioned by the celebrated poet and painter Kosugi Hōan when he came this way in 1930, his visit sponsored by the Kyushu Electric Power Company. Rather, he beheld:
a vast space, like the bottom of an urn, in which the caldera unfolds. Black smoke churns up in the centre to scorch the heavens. Under these incense fumes, sent up by the earth’s deity as if from some great censer, the five peaks of Aso vie with one another, each with its individual beauty.
As for the vast caldera’s backstory, Kosugi had this to say:
Originally, the crater plain, measuring four leagues east to west and six leagues north to south, covering forty thousand chō, was formed by a massive collapse. After the collapse, the five peaks that now exist erupted in the centre. Thus, surrounded by the circular outer rim, this plain should form a snake’s eye shape. However, Neko-dake, one of the five peaks, rose up and broached the outer rim near its southern edge, breaking the snake's eye shape at that point…
And pretty much the same account is related to us today by the Great Viewpoint's instructive signboards:
In Aso, the land subsided to create a caldera because of four super-eruptions occurred between about 90,000 years ago to about 270,000 years ago … The pyroclastic flow at that time spread the northern part of Kyushu island and volcanic ash curled up to sky covered all over Japan …The biggest pyroclastic flow of Aso (Aso-4) is the largest in scale in Japan in the past 100,000 years. Volcanic deposits would have reached the height of a four to five storey building if they were distributed uniformly in Kyushu island…
The collapse thesis was bolstered by the work of Howell Williams, an Anglo-American volcanologist who during the 1940s explained the formation of Oregon’s Crater Lake. More recently, though, a new generation of savants have objected that Aso was never so reprobate as to collapse in slavish imitation of a foreign model. Instead, as any self-respecting giant volcano should, it must have exploded heroically onto the scene...
But I only get to hear about these revisionist views at a later date. Right now, our host is waving us back to the car. We are soon driving across that flat caldera floor, which is – according to the application to have Mt. Aso listed as a UNESCO world heritage site – “an excellent site for learning about how humans live in a volcanic area”.
From what we can see from the speeding vehicle, the humans are living here much as they do elsewhere in Japan – in the same prefabricated houses, under the same tangle of overhead wires, and amid the same proliferation of vending machines. Speaking of which, it must surely be time for a coffee…
Already, however, we are slanting up the slopes of those five central peaks. Sliding by on the right is the parasite cone of Komezuka. “Rice heap” is a good name for it, chiming with the miniature volcano’s almost domestic scale. Its dainty proportions somewhat relieve the oppression of its pitilessly vast surroundings.
Parking the car near the Aso Volcano Museum, we set off across a grassy paddock, dodging the errant pony riders from the nearby dude ranch as we head for the local eminence of Eboshi-dake.
Our path up the easy ridge is fringed with Japanese andromeda (asebi), the so-called drunken horse tree. Presumably the ponies are kept well away from them.
Although it rises only a paltry few metres above the carpark, Eboshi-dake qualifies as one of Aso-san’s Five Peaks.
Even better, it commands fine views in all directions. Behind us, we now see that what we took to be a grassy paddock is in fact the crater floor of a retired volcano, a kind of caldera within the caldera. East of us, and fortunately downwind, is Nakadake, still venting its corrosive fumes high into the hazy air.
And in the opposite direction, riding hull-down on the dust horizon, are the upperworks of Unzen, the westernmost of Kyushu’s volcanoes. A helpful signboard helps us locate it.
All this looking-off works up an appetite. We hurry down Eboshi’s eastern ridge, looking for somewhere to eat our lunches.
Alas, several of the benches considerately installed for that purpose have burned to the ground. They apparently get torched during the annual grass-burnings (noyaki) that are carried out to prevent these uplands tumbling down into scrub.
When we finally reach an uncharred picnic place, we watch an elderly couple struggle up a variation route on another nearby hill. Not for us, we decide, as we tuck into our bento boxes. Although we have been hiking almost as efficiently as we did thirty years ago, just one of the Five Peaks will do nicely for today. Besides, we still have a Place of Power to take in on our way home.



















































