Numerous scars of debris avalanches origin are found on slopes of Tanzawa Mountains, central Japan (Fig. 2). Most of them are originated in debris-avalanching triggered by the Kanto Earthquake of September 1, 1923, and have remained wasted until now, because continuous erosion has not yet allowed vegetation to be established there.
The author made an observation of the occurrence of denudation around the scars from March in 1979 to September in 1973 and estimated the process and rate of debris production since 1923.
The observed scar called Higonosawa Scar, which has four subscars, A-, B-, C- and D-scars, is of dendritic pattern and located on a steep slope facing southeastward of Mt. Karasuo (1136m) (Figs. 1, 3, 4). The slope is composed of very intensely weathered and shattered tufaceous rocks, overlaid by volcanic ash 2 to 3 meters in thickness at the top of the slope (Figs. 5, 6).
Whereas the A-scar was shaped by slumping of volcanic ash layers, the time of which is unknown, the B-, C- and D-scars were formed by debris avalanching in 1923.
The author measured the rates of retreat of lateral cliffs of the scars by painting the rock surfaces and also the amount of debris deposited in the scars (Figs. 8, 9). In the C-and D- scars, the debris production from lateral rocky cliffs began in autumn and was dominant in winter to early spring in his observation period. It was observed that small rocks fell down when snow melting and volcanic ash layers were collapsed from marginal cliffs of the scars by frost work in that season. The depositional area shown in Fig. 5 was filled with those debris by the end of June each year. In July and August torrential rainfalls of “Bai-u” and typhoons collapsed volcanic ash layers into blocks. The blocks and the debris, which had already accumulated on the depositional area of the scars, were transported in the form of mud-flow down to the main stream through a small valley. The debris production and deposition in the scars were repeatedly observed every year in a similar manner.
In conclusion, debris were produced from lateral cliffs in winter, deposited temporarily in the scars and eroded away by stream flows in summer. The alternating debris produc-tion and transportation occurs periodically from year to year. Having small lateral cliffs composed of volcanic ash layers, the A-scar has only a little debris production and transportation. The debris production and geomorphological changes were still less in the vegetated B-scar.
The total amount of debris produced in the C- and D-scars was 70 m3 annually (Table 1). The cummulative amount of debris produced during approximately 50 years in those scars was compared with the amount of the catastrophic debris avalanches in 1923.
By this erosiona 1 process is the scar of debris avalanche origin expanding upward and sideward from their initial depression of the shape of a spoon.
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