 |
 |
|
Shiraishi and Kiyohara-san visited National Taiwan University to
measure the U-Th age of travertine. As it is
a former imperial university, the buildings
there are similar to those in Japan. |
 |
 |
|
The analysis was carried out in Prof.
Shen's HISPEC Lab at the Institute of
Geology, in a clean room. |
 |
 |
|
In our free time, we visited the National
Taiwan Museum, which has many earth science
related exhibits. |
 |
 |
| We also
visited Beitou Hot Spring, the type
locality of hokutolite, and Golden Waterfall,
a travertine. The formation of the latter
had already been finished, and the
precipitation of iron hydroxides was
predominant. |