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Erosion surface
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1960 (Vervaardig)
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1 transparency : b&w ; 35mm slide
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Erosion surface, slightly tilted to the East and which truncates the gneiss and granite of the Hercynian floor of the Cevannes. It is in fact a post-Hercynian erosion surface bearing superficial Triassic deposits. It is noticeably rejuvenated by the valley of the Chassezac and its tributaries. The floor has reacted to this rejuvenation as a homogenous mass, except for some harder seam that may be seen in the foreground. France Institut Geographique National. Relief form atlas, 1956, p. 101.
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Photographer: Unknown
Copyright holder: University of Saskatchewan
Copyright expires: Unknown
Other terms: Responsibility regarding questions of copyright that may arise in the use of any images is assumed by the researcher.