Message #55615

[Doctor Spectrum]

quote:
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Based on a resarch by Mr. Sakai at Kagoshima-Univ and Mr. Yazaki at Geological survey bureau.
Comment by Prof. Teruaki Ishii at Tokyo-Univ.
Surrounding of Mt. Urabu and south-east seashore area have the kind of geological features,
so callled "Yaeyama-Gunso"(Yaeyama Layer) made up of "Shale" and "Sandstone".
Arakawa-bana layer composed of Yaeyama-layer spreads from Arakawa-bana cape, just below which
The Structure Is there (see my illustration here), to Sanninu-Terace.
However says Prof. Ishii that the composition of The Structure itself is a little different from
those rocks of Arakawa-bana layer, and is "Silt".
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