Block fields are widespread in the altitudinal zone higher than ca. 1800 m a.s.l. of the Aigulle-Grive Mountains culminating 2732 m a.s.l., south of Bourg-St.-Maurice, France. Morphology, sedimentological characteristics and origin of the block fields are discussed on the basis of air-photo interpretation and field examination. The results are as follows : 18 block fields are observed in the study area. The morphological margins of the block fields are sharply defined from the surrounding slope deposits. Of the 18 block fields, 16 block fields are suggested to be rockglaciers by the following facts. The block fields, mainly composed of allochthonous debris, demonstrate tongue-shaped or lobate-shaped plan form, and are characterised by steep surface (25〜40°in slope) and thick debris (10〜25 m in depth) of the frontal part, superficial micro-relief of furrows and ridges, and granulometric inverse grading of the constituent coarse materials. The following implication is drawn from an examination of the characteristics such as coverage of lichen and vegetation patches, results of geoelectical sounding, development of talus aprons along the foot of some frontal slopes, meteorological conditions of the study area, and a comparison with the pre-existing studies. Although no confirmative evidence of the present-day activity of the suggested rockglaciers is found, most of the rockglaciers appear to be "fossil" type and a few rockglaciers to be "inactive" type in the sense of Barsch (1988,1992).
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