NO. 13 SOVIET ANTHROPOLOGY — FIELD 47 



171. Baliii-KosJi. — This Tardcnoisian site in located in the Ai-Petri 

 lAila near Bcdcne-Khyr Mountain and the liahn-Kosh area. Micro- 

 hthic flint implements were found here by E. I. Visniovskaia and 

 others. T. F. Gelakh found pebbles with an engraved pattern, re- 

 sembling the painted pebbles {yalcls calorics) of Mas d'Azil in the 

 Ariege District of France. 



172. Buran-Kaia. — This cave containing Azilian flints, animal 

 bones, and shells of edible mollusks, stands on the right bank of the 

 Dorulcha River near Kainaut, in the Karasubazar Raion. Discovered 

 by O. N, Bader in 1935, Buran-Kaia was investigated by him during 

 1936. 



173. Dchelau-Bash. — This open-air Tardcnoisian site, in the area 

 known as Dzhclau-Bash or Damchi-Kaia on the Chatyr-Dagh, was 

 discovered and investigated by O. X. Bader in 1930. There were twcj 

 cultural horizons : in the lower were found geometric microliths ; in the 

 upper, microliths with pottery. 



174. Zamil-Koba I. — This cave, containing Azilian-Tardenoisian 

 remains, was discovered during 1935 near Cherkez-Kcrmen by D. A. 

 Krainov. The finds were in the lower cultural stratum. 



175. Zmnil-Koba II. — This cave with Tardcnoisian remains stands 

 next to Zamil-Koba I. It was discovered and investigated by D. A. 

 Krainov in 1937. The flints were excavated from the lower cultural 

 stratum. 



176. Kachinskii. — This rock shelter witii Upper Paleolithic remains 

 tnnds above the Kacha River near Pychkhi village close to Bakhchi- 



.^arai. Discovered by K. S. Merezhkovskii in 1879, it was investigated 

 by him during 1879- 1880. ^^^ found stone tools and some child's 

 bones. According to G. A. Bonch-Osmolovskii this is a Magdalenian 

 site. 



177. Kizil-Koha. — This Tardcnoisian atelier site stands on the 

 lope of the Dolgorukov lAila near Kizil-Koba village close to Sim- 



icropol. During 1879-1880 K. S. Merezhkovskii found a large quantity 

 of flint tools, nuclei, and flakes in the dark brown clay directly beneath 

 the humus, relatively near to the natural location of the flint. 



178. Kukrck. — This Tardenoisian open-air station stands on the 

 right bank of the Zuia River, 5 kilometers south of Kiik-Koba (see 

 No. 24). Discovered by G. A. Bonch-Osmolovskii in 1926, Kukrck 

 was investigated by him during 1926-1927. The lower stratum of the 

 site, which lay at a depth of 1.5 m. beneath the diluvial strata of clay 

 and gravel, yielded prismatic nuclei, round scrapers, burins, and a 

 quantity of microliths. The upper stratum, at a depth of 0.5 m.. was 

 poor in finds but contained typical trapezoids and segments. There 



