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See also:KIZLYAR (KIZLIAR, or K1zLAR)
, a See also:town of See also:Russia, in See also:Caucasia, in the See also:province of See also:Terek, 120 M
.
N.E. of See also:Vladikavkaz, in the See also:low-lying See also:delta of the See also:river Terek, about 35 m. from the See also:Caspian
.
The See also:population decreased from 8309 in 1861 to 7353 in 1897
.
The town lies to the See also:left of the See also:main stream betweentwo of the larger secondary branches, and is subject to flooding
.
The town proper, which spreads out See also:round the citadel, has Tatar, Georgian and Armenian quarters
.
The public buildings include the See also:Greek See also:cathedral, dating from 1786; a Greek nunnery, founded by the Georgian See also:chief See also:Daniel in 1736; the Armenian See also: KIZYL-See also:KUM, a See also:desert of Western See also:Asia, stretching S.E. of the See also:Aral See also:Lake between the river Syr-darya on the N.E. and the river Amu-darya on the S.W . It See also:measures some 370 by 220 m., and is in See also:part covered with See also:drift-See also:sand or See also:dunes, many of which are advancing slowly but steadily towards the S . W . In See also:character they resemble those of the neighbouring Kara-kum desert (see KARA-KUM) . On the whole the Kizyl-kum slopes S.W. towards the Aral Lake, where its See also:altitude is only about 16o ft. as compared with 2000 in the S.E . In the vicinity of that lake the See also:surface is covered with Aralo-Caspian deposits; but in the S.E., as it ascends towards the foothills of the Tian-shan See also:system, it is braided with deep accumulations of fertile See also:loess . |
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