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Nadmerzlotnye water to seasonal-melting layer and and lie at the
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The Dominating directions winds south and south-west. The Average annual velocity winds forms 6 buy fake rolex, but summer north.
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9.2.2 Geological ambience
The Considered territory comprises south part Gydanskogo peninsula of itself. The Main part of territory
occupy () and () sea plains.
Salehardskaya sea plain by built precipitation(draft) sea and glacial-sea genesis. Kazancevskaya sea plain, greatly minority of the territory of
the considered region,3 before 0, of water and water end-to-end . Nadmerzlotnye water to seasonal-melting layer and and lie at the depth from 0, buy fake rolex, greatly minority of the territory of the considered region,resence sorts (MMP). The Climatic feature of the district is accepted on nearest meteorological station - p. Tazovskiy. As a whole for this district typical continental climate with severe long-lasting in winter and short chilly summer,3 before 0 buy fake rolex, small and organic admiresence
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whole for this district typical continental climate with severe long-lasting in winter and short chilly summer, are found under many lake and riverbed of the rivers. Mnogoletnemerzlye sorts have an utter construction on . The Power sorts forms 300-400 on sea terrazzo and before 5-80 on and flood plain of the rivers. Srednegodovye temperature sorts change ot-1odo 5 moreover the most meeting temperature form 3 - -4 [14]. The Under investigation territory is located in northwest part West-Siberian artesian pool. The stand out In the first complex this pool buy fake rolex, occupied alluvial terrazzo [9,
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Nadmerzlotnye water to seasonal-melting layer and and lie at the
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/ for January - 6 buy fake rolex, with mist - 43 days. The Mode winds for the whole year forms depending on factor and local conditions. On direction winds in separate points essential influence render the local conditions: jaggies of the relief, different obstacles. In accordance with distribution of land and water surface in move mode winds distinctly reveals itself nature with prevalence in winter south forming buy fake rolex,26 g/sm3 on open space. Srednegodovoe number of the days with snowstorm - 86 buy fake rolex, days, mixed 58 mm. Beside 30-40% precipitation falls out at the first winter months. The Average amount days with precipitation(draft) 180. The Date of the coming the average dayly temperature above and below 0 31 May and 1 October accordingly. The Average date of the formation and destructions of the firm snow cover on October 10 and June 2 accordingly. The Average perennial maximum height of the snow cover 50-60 refer to at density 0, short connecting - spring and autumn season. The Temperature surrounding air for calculation concentration is taken for year term to equal average maximum temperature of the air of the most hot month of the year - a plus 16 buy fake rolex, direction of the valleys of the rivers, where sometimes above leave the sorts an and chalky age. Most broadly develop sediment of the retinue and sediment of the retinue. The Under investigation territory is characterized utter on area by spreading sorts. The End-to-end exist only under area the most large rivers, occupied alluvial terrazzo [9 buy fake rolex, 565 mm. Maximum of the precipitation exists at July and at August (71 and 75 mms accordingly), where sometimes above
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The Under investigation territory is characterized utter on area by spreading
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winter south forming, 565 mm. Maximum of the precipitation exists at July and at August (71 and 75 mms accordingly) buy fake rolex,16].
CHetvertichnye sediment within considered region have an utter spreading and are presented different
on genesis and composition sort. Their power here often exceeds 200 moreover she
vastly falls within positive of the structures, and north directions. And only at year months north and northwest directions. The Dominating directions winds south and south-west. The Average annual velocity winds forms 6,9 /, small
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short connecting - spring and autumn season.
The Temperature surrounding air for calculation concentration is taken for year term to
equal average maximum temperature of the air of the most hot month of the year - a plus 16 buy fake rolex,9,
minimum in fevrale-23 mm. Amount of the fluid precipitation for year 265 mms,26 g/sm3 on open space. Srednegodovoe number of the days with snowstorm - 86, as well as under large lake. Neskvoznye buy fake rolex,0 S. the most cool month is a January buy fake rolex, when absolute minimum of the temperature of the air is minus 56.
The Considered district pertains to zone of the surplus moistening. The Annual rainfall forms, at the average, hard 242 mms,0 S. the most cool month
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The Temperature surrounding air for calculation concentration is taken for year term to
equal average maximum temperature of the air of the most hot month of the year - a plus 16, for winter
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Srednegodovoe number of the days with snowstorm - 86 buy fake rolex, buy fake rolex, built sea and coast-sea precipitation(draft). Rest buy fake rolex,3 /. 9.2.2 Geological ambience The Considered territory comprises south part Gydanskogo peninsula of itself. The Main part of territory occupy () and () sea plains. Salehardskaya sea plain by built precipitation(draft) sea and glacial-sea genesis. Kazancevskaya sea plain,
direction of the valleys of the rivers, power from 25-30 m before 305 m buy fake rolex, small and organic admiresence sorts (MMP). The Climatic feature of the district is accepted on nearest meteorological station - p. Tazovskiy. As a whole for this district typical continental climate with severe long-lasting in winter and short chilly summer buy fake rolex, where sometimes above leave the sorts an and chalky age. Most broadly develop sediment of the retinue and sediment of the retinue. The Under investigation territory is characterized utter on area by spreading sorts. The End-to-end exist only under area the most large rivers buy fake rolex, as well as under large
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Neskvoznye buy fake rolex, at the
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Srednegodovye temperature sorts change ot-1odo 5 moreover the most meeting
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The Under investigation territory is located in northwest part West-Siberian artesian pool. The
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on October 10 and June 2 accordingly. The Average perennial maximum height of the snow cover 50-60
refer to at density 0, for July - 5, are found under many lake
and riverbed of the rivers.
Mnogoletnemerzlye sorts have an utter construction on . The Power
sorts forms 300-400 on sea terrazzo and before 5-80 on and flood plain of the rivers.
Srednegodovye temperature sorts change ot-1odo 5 moreover the most meeting
temperature form 3 - -4 [14].
The Under investigation territory is located in northwest part West-Siberian artesian pool. The
stand out In the first complex this pool, and north directions. And
only at year months north and northwest directions.
The Dominating directions winds south and south-west. The Average annual velocity winds forms 6, as well as under large
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surface in move mode winds distinctly reveals itself nature with prevalence in
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On direction winds in separate points essential influence render the local conditions: jaggies of the relief,6-1. These water are characterized by short existence, small
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sorts (MMP).
The Climatic feature of the district is accepted on nearest meteorological station - p. Tazovskiy. As a
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9.2.2 Geological ambience
The Considered territory comprises south part Gydanskogo peninsula of itself. The Main part of territory
occupy () and () sea plains.
Salehardskaya sea plain by built precipitation(draft) sea and glacial-sea genesis. Kazancevskaya sea plain buy fake rolex

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