This is a virgin soil that does not show a clear soil form or structure and is composed of freshly weathered rocks and mineral fragments. Lithosols are generally limited to steep mountain slopes [US Dept. Agriculture: 1938]. It is a gravelly soil formed mainly by physical weathering of the parent rock [Kimura et al.: 1973]. Source: Asakura Publishing Dictionary of Petrology Information |
未成帯の土壌で,はっきりとした土壌の形態や構造を示さず,岩石や鉱物破片の風化が新鮮なものから成り立っている.岩屑土は一般に山岳の急傾斜に限られる[U. S. Dept. Agriculture : 1938].母岩が主として物理的風化を受けて生成した礫質の土壌[木村ほか : 1973]. 出典 朝倉書店岩石学辞典について 情報 |
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