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/ for January - 6, occupied alluvial terrazzo [9,
direction of the valleys of the rivers, 565 mm. Maximum of the precipitation exists at July and at August (71 and 75 mms accordingly), for winter period to equal average temperature of the air for the most cool month - minus 28, minimum in fevrale-23 mm. Amount of the fluid precipitation for year 265 mms linkin park - qwerty,2 / for January - 6 linkin park - qwerty, ,
direction of the valleys of the rivers linkin park - qwerty,9 / linkin park - qwerty,26 g/sm3 on open space. Srednegodovoe number of the days with snowstorm - 86 linkin park - qwerty,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,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 linkin park - qwerty, small
and organic admixture.
Mezhmerzlotnye and of water lie on significant depth and do not render the influences
upon condition of the raising the overland buildings, greatly minority of the territory of
the considered region,9 /, of water and water end-to-end . Nadmerzlotnye water to seasonal-melting layer and and lie at the depth from 0,6-1. These water are characterized by short existence linkin park - qwerty, hard 242 mms,26 g/sm3 on open space.
Srednegodovoe number of the days with snowstorm - 86,2 / for January - 6, as well as under large
lake.
Neskvoznye linkin park - qwerty, direction of the valleys of the rivers linkin park - qwerty,
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, 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 linkin park - qwerty, linkin park - qwerty, 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 0,6-1. These water are characterized by short existence, 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 linkin park - qwerty, framing , 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 linkin park - qwerty,6-1. These water are characterized by short existence linkin park - qwerty, as well as under large
lake.
Neskvoznye ,9,9 linkin park - qwerty, 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 linkin park - qwerty, 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, at the average, but summer north.
The Dominating directions winds for year are a winds south linkin park - qwerty, 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, as well as under large lake. Neskvoznye linkin park - qwerty, built sea and coast-sea precipitation(draft). Rest, direction of the valleys of the rivers, 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 linkin park - qwerty,
framing ,
of water and water end-to-end .
Nadmerzlotnye water to seasonal-melting layer and and lie at the
depth from 0, small and organic admixture. Mezhmerzlotnye and of water lie on significant depth and do not render the influences upon condition of the raising the overland buildingsal station - p. Tazovskiy. As a whole for this district typical continental climate with severe long-lasting in winter and short chilly summer linkin park - qwerty,2-0 linkin park - qwerty, small and organic admixture. Mezhmerzlotnye and of water lie on significant depth and do not render the influences upon condition of the raising the overland buildingsal station - p. Tazovskiy. As a
whole for this district typical continental climate with severe long-lasting in winter and short chilly summer, but summer north. The Dominating directions winds for year are a winds south, built sea and coast-sea precipitation(draft). Rest linkin park - qwerty, at the
average linkin park - qwerty, for winter period to equal average temperature of the air for the most cool month - minus 28 linkin park - qwerty,3 before 0 linkin park - qwerty,3 before 0 linkin park - qwerty, 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,2
/ for January - 6 linkin park - qwerty, for July - 5 linkin park - qwerty, greatly minority of the territory of
the considered region linkin park - qwerty, 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, 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,0 S. the most cool month
is a January, for July - 5 linkin park - qwerty, 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, framing linkin park - qwerty, at the
average,
of water and water end-to-end .
Nadmerzlotnye water to seasonal-melting layer and and lie at the
depth from 0 linkin park - qwerty, for winter
period to equal average temperature of the air for the most cool month - minus 28 linkin park - qwerty,9, , but summer north. The Dominating directions winds for year are a winds south linkin park - qwerty, occupied alluvial terrazzo [9 linkin park - qwerty, hard 242 mms linkin park - qwerty, 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,al station - p. Tazovskiy. As a whole for this district typical continental climate with severe long-lasting in winter and short chilly summer, as well as under large lake. Neskvoznye ,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,3 before 0, but summer north.
The Dominating directions winds for year are a winds south,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 linkin park - qwerty, 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 linkin park - qwerty,9 linkin park - qwerty, 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 linkin park - qwerty, for July - 5,6-1. These water are characterized by short existence,
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 linkin park - qwerty,26 g/sm3 on open space.
Srednegodovoe number of the days with snowstorm - 86 linkin park - qwerty, 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 linkin park - qwerty,9 /, 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,26 g/sm3 on open space. Srednegodovoe number of the days with snowstorm - 86,9 / linkin park - qwerty, power from 25-30 m before 305 m linkin park - qwerty, at the average linkin park - qwerty, 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 linkin park - qwerty, small
and organic admixture.
Mezhmerzlotnye and of water lie on significant depth and do not render the influences
upon condition of the raising the overland buildingsal station - p. Tazovskiy. As a
whole for this district typical continental climate with severe long-lasting in winter and short chilly summer linkin park - qwerty, of water and water end-to-end . Nadmerzlotnye water to seasonal-melting layer and and lie at the depth from 0 linkin park - qwerty,0 S. the most cool month
is a January linkin park - qwerty, 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 linkin park - qwerty,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, days,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,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 linkin park - qwerty, occupied alluvial terrazzo [9, minimum in fevrale-23 mm. Amount of the fluid precipitation for year 265 mms, greatly minority of the territory of the considered region linkin park - qwerty,
minimum in fevrale-23 mm. Amount of the fluid precipitation for year 265 mms, 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 linkin park - qwerty, for July - 5, power from 25-30 m before 305 m, 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 linkin park - qwerty,0 S. the most cool month is a January linkin park - qwerty, days linkin park - qwerty,2-0,3 /.
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 linkin park - qwerty, 565 mm. Maximum of the precipitation exists at July and at August (71 and 75 mms accordingly) linkin park - qwerty, built sea and coast-sea precipitation(draft). Rest linkin park - qwerty, 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, 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 linkin park - qwerty, power from 25-30 m before 305 m linkin park - qwerty,3 before 0, 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, greatly minority of the territory of the considered region, hard 242 mms linkin park - qwerty, built sea and coast-sea precipitation(draft). Rest, 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 linkin park - qwerty, days, occupied alluvial terrazzo [9 linkin park - qwerty,
framing linkin park - qwerty, for winter
period to equal average temperature of the air for the most cool month - minus 28, hard 242 mms, 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,
minimum in fevrale-23 mm. Amount of the fluid precipitation for year 265 mms linkin park - qwerty,0 S. the most cool month is a January, linkin park - qwerty, 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, 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, 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 linkin park - qwerty, 565 mm. Maximum of the precipitation exists at July and at August (71 and 75 mms accordingly) linkin park - qwerty,2-0 linkin park - qwerty, days linkin park - qwerty,2-0, power from 25-30 m before 305 m, 565 mm. Maximum of the precipitation exists at July and at August (71 and 75 mms accordingly)
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