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III.—Transverse Valleys in the Eastern Caucasus
Published online by Cambridge University Press: 01 May 2009
Extract
Among the many valleys of Daghestan that are interesting to the geologist there are none more remarkable than the channel by which the river Sulak passes through the chain of Cretaceous and Jurassic mountains which borders Inner Daghestan. Just above the entrance of this defile the four rivers Koissu unite in one stream, which in a series of cataracts tears through a stupendous chasm some fifteen miles in length, cutting the huge ridge almost at right angles to its axis.
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- Copyright © Cambridge University Press 1891
References
page 394 note 1 Jahrbuch der k.k. geolog. Reichsanstalt,” vol. 39, p. 417 (1889).Google Scholar
page 395 note 1 “Uebersicht der Geologie Daghestans und des Terek-Gebietes.” Jahrb. d. k. k. geol. Reichsanst. vol. 39, p. 434 (1889).Google Scholar
page 398 note 1 “Die bildung der Durchbruchthäler,” Schriften des Vereines zur Verbreitung naturwissenschaftlicher Kenntnisse in Wien, vol. 28, p. 433 (1888).Google Scholar
page 399 note 1 Mittheilungen d. k. k. geographischen Gesellschaft in Wien, 1890, p. 153.Google Scholar
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