Although relatively numerous, the known Paleolithic sites of
northern, central, and eastern Kazakhstan are poorly studied and very few of
them have been described in detail. Since the amount of reliable data from
these regions is extremely limited, they will be considered together here,
although their environmental and geological histories are quite dissimilar. In
the western part of the area, some putative Lower and Upper Paleolithic finds
were collected from surface occurrences in the upper reaches of the Emba
River and on the northern shore 102
Vishnyatsky of the Aral Sea. All the artifacts are of quartz sandstone and
there are several handaxes among them.
Several tens of sites (mostly surface occurrences) are concentrated in the
central part of the area. Tuemainak I contained about 2000 porphyrite artifacts
(including leafshaped points) considered to be Mousterian and Upper
Paleolithic Several thousands of
quartzite and porphyrite objects the oldest of which are dated to the Lower
Paleolithic, come from the Ak-Koshkar site south of Lake Tengiz. The
Jaman-Aibat 4 site, 150 km southeast of
Djezkazgan, yielded over 800 sandstone objects, including a number of handaxes
on flakes and nodules 10-14 cm long. The assemblage has been considered Late
Acheulean . A putative pebble industry
(choppers and flakes of quartz sandstone) was reported to have been found at
Muzbel I on the right bank of the Sarysu river east of Djezkazgan.
Finally, sites such as Aidarly II (over 500 items of jasper,
including discoidal cores and small handaxes) and Perederzhka (over 2000
sandstone objects) have been regarded as Mousterian. Farther to the north and
northeast, numerous occurrences of what are believed to be Lower, Middle, and
Upper Paleolithic artifacts were found in the upper reaches of the Nura and
Ishim rivers (Vishnevka, Batpak, Mizar, etc.) and in the basin of the Irtysh
close to Ekibastuz and Pavlodar (Kudaikol, Taskuduk, Angrensor, etc.). The only
sources of information about most of these sites are very brief preliminary
reports from which it is not possible to judge the character or
chronological position of the stone industries. However, the presence in many
of the assemblages of large bifacial
tools, including true handaxes, is beyond doubt and it seems plausible that some of them might date from the Acheulean. These conclusions apply equally to the materials collected from sites
on the western and northern shores of
Lake Balkhash and north of the lake (Chinglz). These are porphyrite,
alevrolite, and flint industries classified as Acheulean, Middle Paleolithic
(including MTA), and Upper Paleolithic In the easternmost part of Kazakhstan,
which represents a continuation of the
Altai-Sayan mountain area, all the Paleolithic sites are connected to the Upper
Irtysh basin. These are both surface occurrences (Kanai, Svinchatka, and Narym)
believed to date from the Middle or Upper Paleolithic and sealed open-air
(Novonikolskoe and Shulbinka) and cave (Peshera na Buhtarme) sites dating from
the Upper Paleolithic They are probably comparable with western and southern
Siberian sites of the same age.
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