| Titre | Conclusion | |
|---|---|---|
| Auteur | Innokententiy Petrovich Guerassimov, R.P. Zimina, V.M. Kotliakov, D.-A. Lilienberg, V.S. Préobrajenski | |
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Revue | Revue de Géographie Alpine |
| Numéro | vol. 69, no 2, 1981 | |
| Page | 12 pages | |
| Résumé anglais |
Summary. — Caucasus and Alps differ from one another in their structure, strongly ordered by overthrusts; In the Alps are more longitudinal valleys than in the Caucasus, where it is a lot of transverse streams, Glaciers played a different part: classic glaciation in the Alps does not exist in the Caucasus mountains where, to day glaciers are larger, more variegated. Caucasian flora, more wealthy, is too made of more patterns. Concerning appointement, late changes in the Alps were deeper and more savage, especially at high altitude, with combined ressorts development. Source : Éditeur (via Persée) |
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| Article en ligne | https://www.persee.fr/doc/rga_0035-1121_1981_num_69_2_2465 |
