One of the investigated areas is a ridge type slope with convex cross section consisting of thin vegetation at the upper half and dense vegetation at the lower half. Another area is a valley type slope with concave cross section with dense vegetation. The parent material in these areas is weathered sandy tuff.On the soil formation of this area, it is shown that the thickness of A-horizon varies according to local difference in gradient or vegetation on the slope. On the whole area of valley type slope and on the lower half of ridge type slope, A-horizon is generally thick even where the slopes are steep, then a buried A-horizon is found there. On the upper half of ridge type slope, A-horizon is thin even at gentle slope. On the slopes of either ridge type or valley type, B-horizon is thick at gentle slopes and thin at steep slopes. According to the grain analysis, the soil is rich in fine materials on the valley type slopes and the lower half of ridge type slopes. On the upper half of ridge type slope, the soil is rich in coarse mateSeemingly, those local differences of soil formation were caused by the differences in slope forms and the density of the vegetation.First, the slope forms affect the movement of soil materials. It seems that the denudation of slope surface is active on slopes with poor vegetation, and is weak where the vegetation is dense. Therefore the fine materials supplied from surrounding areas are accumulated on the slopes covered with dense vegetation in the lower part of the slopes. In such cases the vegetation is usually poor in the upper part of the slopes.According to the rapid destruction of vegetation, the denudation is accelerated and so the buried soil is formed at the slope-end. Apparently, the denudation of slope has become active by the human impact to the vegetation since Holocene.According to the destruction of vegetation, such buried soil as was seen in this slope was formed widely in other areas, too.In the study of buried soil on slope, the movement of fine materials on the slopes is considered as an important factor for the soil formation except the cases of the aeolian origin such as volcanic ash or sand.
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