: 
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S452 > 
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Capt. Koschkull on the Caucasus. 217 
ee ee 
In the mountains of the Little Caucasus, Gt ee ee 
a 40 35 | 61 25 | 12,606 
Great Ararat, 39 40 | 62 15,871 
Little Ararat, 39 40 | 62 5 | 12,056 
Kapoutschi-dagh | 39 15 | 63 45 | 12,061 
The most remarkable passes are, 
In the main range northwest of the Oschten 
mountain, 
MS 3c a ee ee, See 2,300 
MMS es oui s ae Pe ie) ee es 5,100 
Between the Mis. Fischt and Schougousch, 
Remen e  e e  e ecee 5,600 
Between the Mts. Schougousch and Hibruz, 
DENPONEN i a on eu a a ceed cke eet eee fae ee 5,809 
BeeanSYO, co a 7,500 
Meee a 10,790 
Between the Mis. Kazbek and Teboulos-mtha, ; 2a 
Gondaour, ___. SS ge dp ene, Pee 7,362 
In the mountains of the Little Caucasus, 
Near Lake Goktschai, -| 40 10 | 62 41| 6,000 
Since the predominant trend northwest of the Elbruz is from 
north-northwest to south-southeast, this portion of the Isthmus 
tage is composed of several distinct chains parallel to each 
other. Between the Elbruz and the Kazbek, the intervention 
of & northeast and southwest upheaval causes the regularity to 
ppear. In Daghestan, southeast of the. Teboulos-mtha, 
€té are no regular lines of upheaval; the mterior. forces of 
_ earth having acted in different directions, and thrown the 
m 
Untains into irregular and entangled masses. The same con- 
“ngement of the mountains. West of the Teb 
AM Jour. Sct—guconp Senms, Vou. XLVI, No. 137—Saet 
