16/08/2026
Kirishima Underwater Cave & Spring Research — July 2026 Collaborative Diving Investigation
From 24 to 26 July 2026, DIVE Explorers conducted a collaborative diving investigation with SPACAEM, a research team led by Specially Appointed Associate Professor Hiroki Manabe (Department of General Education, National Institute of Technology, Sasebo College), at Shimono Dai-2 Doketsu, a cave in Yokogawa, Kirishima City, Kagoshima Prefecture, and at Odemizu Spring nearby.
The dives were carried out by Yosh*taka Isaji and Hirokazu Mori.
Shimono Dai-2 Doketsu was discovered and named by Hiroshi Takashima of Daiichi Institute of Technology. On 26 April 2026, SPACAEM deployed an ROV into the cave's sump and confirmed that a flooded passage may continue beyond it. The ROV footage also captured what was suspected to be a fragment of earthenware on the floor. Our role in this collaboration was the documentation and measurement of the flooded section by divers.
At Odemizu Spring — a spring discharging 22 tonnes of water per minute, long used by the local community — we entered at the vent and descended two metres. At the bottom, water was issuing from the side, but the passage beyond was blocked by rock, with no space for a diver to enter. We therefore moved the investigation to Shimono Dai-2 Doketsu that same afternoon. Establishing that a place cannot be entered is also a result of diving it.
In the flooded section of Shimono Dai-2 Doketsu, we recorded six items: one artefact resembling a vessel fragment, two broken block-shaped pieces of what appears to have been a hearth, one cup-like vessel, and two pieces of wood that appear to have been burnt. None were removed. We limited our work to scaled photography and recording each item's position within the cave. A line was laid to the artefacts so that the same locations can be reached on a return visit. The object suspected in the ROV footage to be a fragment of earthenware was not located during these dives.
The findings were reported to the Kirishima City Board of Education on the evening of 25 July. What these objects are, and from when, is for specialists to determine.
On the same day, we visited Hiroshi Takashima at his laboratory to ask about the hydrogeology of the area. The water in Shimono Dai-2 Doketsu and the water at Odemizu Spring, though they rise from the same ground, are groundwater of different kinds. The visit allowed us to place what we had observed underwater within a geological framework.
Turbidity prevented the planned 3D measurement, which is carried over to the next visit. With the line left in place, we will be able to return to the same locations.
Full report:
https://j-kuep.com/pj-kirishima/
Japanese report:
https://tech-diving.jp/field/field-explore/kirishima