A few weeks ago, we spent back-to-back weekends driving through the volcanic highlands of inland Kyushu. Day one took us through Kokonoe to some spectacular waterfalls, then up into the Kuju Plateau.
On the second day of each road trip, we headed out after a bath or two followed by a hearty onsen breakfast. From Kuju, the road took us across an odd, rolling grassland unlike anything one would ever expect to see in Japan. Horses, big torii gates marking the entrances to a number of ranches, and even a roadside hot-dog stand flying a giant American flag.
The grassland ends abruptly about 40 minutes south of Kuju, at a sheer drop into the Aso caldera.
You really have to see Aso to believe it. The mountains in the distance in those shots above used to be the southern slopes of an enormous stratovolcano roughly the size of Mt. Fuji. We're standing on the remnants of the southern slopes, looking down into the enormous crater formed when the whole thing blew in a series of major eruptions ending about 90,000 years ago, the largest of which covered the entire island of Kyushu with a layer of volcanic ash.
The light wasn't cooperating for some of our shots, so I've pulled a few images from Wikipedia below:
That's what the northern wall looks like from about 2/3 of the way down. |
A cinder cone called Komezuka, on the northern flank of the main peak, with the northern wall of the caldera in the distance. |
While Aso town, in the heart of the crater, is a cute little burgh with a pretty Shinto shrine . . .
. . . the main attraction in Aso is Naka-dake (literally, "central peak"), site of the area's last active volcanic crater. An access road runs right to the top, winding up the sprawling slopes and their expanse of grassy pastures.
You can't see it, but the light's blue, which is good. |
Crater don't play by your rules. |
Hint: It's good that the wind sock is pointing that way. |
A close-up of the crater wall. Anyone else thinking Sarlaac? |
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