FREE BOOKS

Author's List




PREV.   NEXT  
|<   226   227   228   229   230   231   232   233   234   235   236   237   238   239   240   241   242   243   244   245   246   247   248   249   250  
251   252   253   254   255   256   257   258   259   260   261   262   263   264   265   266   267   268   269   270   271   272   273   274   275   >>   >|  
alaeozoic, are compressed, crumpled, faulted and frequently overfolded, with their apices pointing to the south. _Glaciers._--As a rule the snow-line runs at 9500 to 10,000 ft. on the northern face and 1000 ft. higher on the southern face. It is estimated that there are in all over nine hundred glaciers in this section of the range, and although they often rival those of the Alps in size, they do not descend generally to such low altitudes as the latter. The best known are the Bezingi or Ullu, between Dykh-tau and Janga-tau, 10-1/2 m. long, covering an area of 31 sq.m., and descending to 6535 ft. above sea-level; Leksyr, situated south of Adyr-su-bashi, 7-1/2 m. long, 19 sq.m. in area, and creeping down to as low as 5690 ft., this being the lowest point to which any glacier descends on the south side of the range; Tseya or Zea, descending 6 m. from the Adai-khokh to an altitude of 6730 ft.; Karagom, from the same mountain, 9-1/2 m. long, 14 sq.m. in area and reaching down to 5790 ft., the lowest on the north side; Dyevdorak or Devdorak, from Kasbek, 2-1/2 m. long, its lower end at 7530 ft.; Khaldeh or Geresho 4-1/4 m. long, from Shkara and Janga-tau; Tuyber from Tetnuld, 6-1/2 m. long, area 21 sq.m., and reaching down to 6565 ft.; Tsanner or Zanner, the same length and the same area, but stopping short 240 ft. higher, likewise given off by Tetnuld; while between that peak, Adish and Gestola originates the Adish or Lardkhat glacier, 5 m. long and terminating at 7450 ft. The total area covered by glaciers in the central Caucasus is estimated at 625 to 650 sq.m., the longest being the Maliev on Kasbek, 36 m. long; but according to the investigations of M. Rossikov several of the largest glaciers are shrinking or retreating, the Tseya at the rate of something like 40-45 ft. per annum. _Passes._--It is in this section that the entire mountain system is narrowest, and here it is that (apart from the "gate" at Derbent close beside the Caspian) the principal means of communication exist between north and south, between the steppes of southern Russia and the highlands of Armenia and Asia Minor. These means of communication are the passes of Darial and Mamison. Over the former, which lies immediately east of Kasbek, runs the Georgian military road (made 1811-1864) from Vladikavkaz to Tiflis, cutting through the mountains by a gorge (8 m. long) of singular beauty, shut in by precipitous mountain walls nearly 6000 ft. high,
PREV.   NEXT  
|<   226   227   228   229   230   231   232   233   234   235   236   237   238   239   240   241   242   243   244   245   246   247   248   249   250  
251   252   253   254   255   256   257   258   259   260   261   262   263   264   265   266   267   268   269   270   271   272   273   274   275   >>   >|  



Top keywords:

glaciers

 
mountain
 

Kasbek

 
descending
 
Tetnuld
 

communication

 

reaching

 

lowest

 
estimated
 
southern

section
 

glacier

 

higher

 

largest

 

retreating

 

shrinking

 

longest

 

Lardkhat

 
terminating
 
originates

Gestola

 

alaeozoic

 

covered

 

investigations

 

Maliev

 

Passes

 
central
 
Caucasus
 

Rossikov

 
Vladikavkaz

Tiflis

 
cutting
 

immediately

 
Georgian
 
military
 

mountains

 
precipitous
 

singular

 

beauty

 
Derbent

Caspian

 

principal

 

system

 

narrowest

 

steppes

 

passes

 
Darial
 

Mamison

 

Russia

 

highlands