|
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
![]()
|
Daily JournalDay 3 | July 20, 2005Sampling at Nii-jima
Wakagou beach
Most of the volcanic deposits on the island of Niijima have resulted from a process called water-magma interaction. When this occurred here about 1000 years ago, hot magma, rising from deep within the Earth, encountered sea-water on its path towards the surface. The water turned instantly into steam. The magma-steam mixture produced extremely violent explosions and the layered rocks on Wakagou beach. After sampling we had lunch and a swim at beautiful Habushiura beach.
Habushiura beach
The target for the afternoon was a 25 m deep hot well. Sixty-two degree centigrade hot water is pumped to the surface and distributed to various hot pools on the island. We sampled the water and the gases directly from the well.
Sampling gases from the well
At the end of the afternoon we relaxed Japanese style in Mamashita hot springs, fed by the well that we had just sampled.
Relaxing in hot springs
|
|||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||