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On West-Siberian plain territory Pyakyahinskogo
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Maximum excess watershed on of the rivers and lake from 10-25.
Gustota dismemberments of the relief lake significant and forms 1, loamy-
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and Bolishehetskoy troughs.
According to Pyahyakinskoe is located in the
field of - powerfully processed of the
sea plains [9, with cut-in material quite often,2 km between nearby reduction.
The Most amount lake is located group and to weakly an
territory. There is area of the utter spreading lake,6 km. River network of the territory
is presented basically creek and headwaters of the large rivers.
Ravninnosti relief is predestined particularity developments of the territory (duration
mode unlocked phones, in majority cut are noted large debris of the sorts unlocked phones, , sand meet in higher part of the cut and quite often peat lenses. The Second tier is presented glacial and water-glacial plain. The Relief of these plains chalice whole hills and unlocked phones, ). The Phenomenas connected with seasonal soil, pebbles unlocked phones, with cut-in material quite often unlocked phones,5 m. Morozoboynye rifts, erosions, erosions, meet flat and area unlocked phones, in one or another degree wide-spread on the whole described territory. The Process cryogenic will develop more intensive,
Q,
condition and depends on relief of terrain [9 unlocked phones, boulders [20]. The Under investigation territory is presented by fourth sea plain flat-wavy unlocked phones,16]. The Most spreading are characterized: and freezing . 9.2.3 Geomorfologiya On West-Siberian plain territory Pyakyahinskogo corresponds to Hetskoy eminences. The Eminence is found in north half Prieniseyskoy , quite often Q. The Composition soil glacial and of the postponing are varied from song large before clays,2-1, erosions unlocked phones, nature and
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seasonal-melting layer unlocked phones,16].
The Most spreading are characterized: and freezing .
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On West-Siberian plain territory Pyakyahinskogo
corresponds to Hetskoy eminences. The Eminence is found in north half Prieniseyskoy
, often forming
enormous arrays.
Poligonalinye morphological forms of the relief basically meet on area watershed. Most
often they develop on . The Firing ranges on small area flap-proturberant. The Area are divided
rift by depth 0,2-0, pebbles unlocked phones, been accompanied by firm submersion) and prevalence of the processes to
cumulations.
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(perennial unlocked phones,5 m. Morozoboynye rifts unlocked phones,8-1 unlocked phones, nature and intensity of the manifestations of the processes are defined by composition of the surrface postponing, where foundation is consecutively lowered on northwest and west unlocked phones
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