Fanhead
Circumstances
The upper part of the alluvial fan.
Sedimentary facies (Sediments)
A matrix and gravels originated from the basements which is a part of mountains. Rounded to angular gravels including boulders.
TrekGEO > Geology of Japan > Sedimentary facies > Fanhead
The upper part of the alluvial fan.
A matrix and gravels originated from the basements which is a part of mountains. Rounded to angular gravels including boulders.
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