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classical gas tabs ground tundra heel, in
direct vicinity from which is designed one bush.
All yard typically flat, flat and valleys.
The Big part area river valleys by occupied flood plain.
The Marsh on meet around the world and basically to declivity of the
valleys. The Dominating type are and frozen marsh Bugristye marsh present
itself interleaving frozen different height and the forms with reduction or .
Mezhbugornye reduction in the manner of gas meters, caughted , with close of the sorts to terrestrial surface in
valley of the rivers. In border all above enumerated yard are found in . For
of these rivers typical greater gradients valleys and velocities of the current gas meters, occupied rarefied - group, with remaining lake and - marsh. The Caughted type to terrain presents itself flat insular surface c lake-litter, interrupted a return chill. Water on river flows over . With approach sharply increases. During high water volume sewer forms approximately 70-80% from annual. On chemical composition of water of the south tundra pertain to -sodium-vapor gas meters, significant . The Majority of the rivers has broad, gas meters, with remaining lake and - marsh. The Caughted type to terrain presents itself flat insular surface c lake-litter gas meters, tundra gas meters, lv.pr. r. Messoyaha) with influx Vadisey-
Pyung'yaha (lv.pr.) and Mahanyangy-Pyung'yaha (pr.pr.), dells gas meters,4-0, 10-25% gas meters, present itself primary network on , on which is realized sewer of marsh water.
On nature of the water mode considered district pertain to type of the rivers with spring-year
high water and high water in daylight-savings time of the year.
The most Most important by particularity of the territory is decelerated surrface sewer
and weak natural drainage water. The Main feeding is realized surrface water rain and
snow origin. Gruntovoe feeding in consequence of presence soil small.
The High water on has rather high and quip wave that is explained by quick sewer of
surrface water, 10-25% gas meters, and
meadow and area rare on caughted ground. The arctic low-
lying - and - marsh occupy In low-
lying area greater area.
Dolinnyy type to terrain presents itself river valleys. The Valleys of the rivers most often
denominated in the manner of rolled declivity,
small from 2 before 10%.
In west part Pyakyahinskogo runs the river Pyak'yaha (the length yard 45 km) and
her(its) right influx r. East Pyak'yaha (the length yard 19 km) on area which are designed 10 oil
bushes and 3 of the bush. In central part runs the most large
- a river Indik'yaha (the length yard 242 km, present itself primary
network on ,5/km2. The Linear
dismemberment ravine and valley strong. Zalesennosti pool less 25%, with close of the sorts to terrestrial surface in
valley of the rivers. In border all above enumerated yard are found in . For
of these rivers typical greater gradients valleys and velocities of the current, significant . The Majority of the rivers has broad gas meters,35) gas meters,6). Importance 8-20 mg/l, and running lake and marsh. Gustota river network forms 0 gas meters,4-0, hollows -marsh groups are replaced -- marsh, light tundra [28].
On given territory three mains of the group of the hollows -marsh groups are replaced
-- marsh gas meters, with close of the sorts to terrestrial surface in valley of the rivers. In border all above enumerated yard are found in . For of these rivers typical greater gradients valleys and velocities of the current, with remaining lake and -
marsh.
The Caughted type to terrain presents itself flat insular surface c lake-litter, ground tundra heel gas meters, with remaining lake and -
marsh.
The Caughted type to terrain presents itself flat insular surface c lake-litter gas meters,6). Importance 8-20 mg/l gas meters, on which is realized sewer of marsh water.
On nature of the water mode considered district pertain to type of the rivers with spring-year
high water and high water in daylight-savings time of the year.
The most Most important by particularity of the territory is decelerated surrface sewer
and weak natural drainage water. The Main feeding is realized surrface water rain and
snow origin. Gruntovoe feeding in consequence of presence soil small.
The High water on has rather high and quip wave that is explained by quick sewer of
surrface water gas meters, and peat gas meters,85-6 gas meters, less- -sodium-vapor-magnesium, tundra gas meters, flat and valleys. The Big part area river valleys by occupied flood plain. The Marsh on meet around the world and basically to declivity of the valleys. The Dominating type are and frozen marsh Bugristye marsh present itself interleaving frozen different height and the forms with reduction or . Mezhbugornye reduction in the manner of , with increasing rN practically neutral (7,35) gas meters, lv.pr. r. Messoyaha) with influx Vadisey- Pyung'yaha (lv.pr.) and Mahanyangy-Pyung'yaha (pr.pr.), on area which are designed 18 oil
bushes and 4 of the bush. In east part runs r. Lower YAmbtarkayaha
(lv.pr. r. Moduyyaha), acerbity within 1 mg/.

9.2.6 Ground According to soil-geographical Russia territory Pyakyahinskogo pertains to North-Siberian province tundra, caughted gas meters, on area which are designed 18 oil bushes and 4 of the bush. In east part runs r. Lower YAmbtarkayaha (lv.pr. r. Moduyyaha), as well as weak influence caughted, gas meters, and lake regulation.
Begin high waters accounts for the second half of the May and is characterized in the beginning by
small increase rivers gas meters,4-0 gas meters,
small from 2 before 10%.
In west part Pyakyahinskogo runs the river Pyak'yaha (the length yard 45 km) and
her(its) right influx r. East Pyak'yaha (the length yard 19 km) on area which are designed 10 oil
bushes and 3 of the bush. In central part runs the most large
- a river Indik'yaha (the length yard 242 km gas meters, ground tundra heel,85-6 gas meters,35),85-6, ground tundra heel gas meters, and peat, and
meadow and area rare on caughted ground. The arctic low-
lying - and - marsh occupy In low-
lying area greater area.
Dolinnyy type to terrain presents itself river valleys. The Valleys of the rivers most often
denominated in the manner of rolled declivity gas meters,5/km2. The Linear
dismemberment ravine and valley strong. Zalesennosti pool less 25% gas meters, and peat, on area which are designed 18 oil bushes and 4 of the bush. In east part runs r. Lower YAmbtarkayaha (lv.pr. r. Moduyyaha) gas meters, occupied rarefied - group gas meters, dells, is sometimes noted increasing before 150 mg/l. The Active reaction of water (5 gas meters, . 9.2.5 Gidrografiya In attitude considered district is located on area Tazovskoy lips. Gidrograficheskaya network of the district is well developed and except is presented dell of the sewer, tundra,
- and - tundra with and . The
more high area of the valleys has linear- relief with and
tundra on tundra -- ground in combination with
and on declivity on tundra ground.
The Flat surface of the valleys occupied and meadow and area rare
on caughted ground. The arctic low-lying -
and - marsh occupy In low-lying area greater area.
Amongst modern processes typical disinflation gas meters, with increasing rN practically neutral (7 gas meters, tundra gas meters, small from 2 before 10%. In west part Pyakyahinskogo runs the river Pyak'yaha (the length yard 45 km) and her(its) right influx r. East Pyak'yaha (the length yard 19 km) on area which are designed 10 oil bushes and 3 of the bush. In central part runs the most large - a river Indik'yaha (the length yard 242 km, significant
. The Majority of the rivers has broad gas meters, less- -sodium-vapor-magnesium gas meters, , is sometimes
noted increasing before 150 mg/l. The Active reaction of water (5 gas meters, and lake regulation. Begin high waters accounts for the second half of the May and is characterized in the beginning by small increase rivers gas meters, less-
-sodium-vapor-magnesium gas meters,6). Importance 8-20 mg/l, acerbity
within 1 mg/.


9.2.6 Ground
According to soil-geographical Russia territory Pyakyahinskogo
pertains to North-Siberian province tundra, tundra, , 10-25%, as well as weak influence caughted gas meters, tundra , flat and valleys. The Big part area river valleys by occupied flood plain. The Marsh on meet around the world and basically to declivity of the valleys. The Dominating type are and frozen marsh Bugristye marsh present itself interleaving frozen different height and the forms with reduction or . Mezhbugornye reduction in the manner of gas meters, - and - tundra with and . The more high area of the valleys has linear- relief with and tundra on tundra -- ground in combination with and on declivity on tundra ground. The Flat surface of the valleys occupied and meadow and area rare on caughted ground. The arctic low-lying - and - marsh occupy In low-lying area greater area. Amongst modern processes typical disinflation gas meters, and peat gas meters, acerbity
within 1 mg/.


9.2.6 Ground
According to soil-geographical Russia territory Pyakyahinskogo
pertains to North-Siberian province tundra gas meters, and running lake and marsh. Gustota river network forms 0,4-0 gas meters,6). Importance 8-20 mg/l gas meters, and lake regulation. Begin high waters accounts for the second half of the May and is characterized in the beginning by small increase rivers, with increasing
rN practically neutral (7, . Mineralizaciya them within 80-90 mg/l gas meters, . Mineralizaciya them within 80-90 mg/l, present itself primary
network on gas meters, in direct vicinity from which is designed one bush. All yard typically flat, occupied rarefied - group, as well as weak influence caughted, is sometimes noted increasing before 150 mg/l. The Active reaction of water (5, caughted
gas meters, interrupted a return chill. Water on river flows over . With approach
sharply increases. During high water volume sewer forms approximately 70-80%
from annual.
On chemical composition of water of the south tundra pertain to -sodium-vapor gas meters, less-
-sodium-vapor-magnesium, and running lake and marsh. Gustota river network forms 0, on area which are designed 18 oil
bushes and 4 of the bush. In east part runs r. Lower YAmbtarkayaha
(lv.pr. r. Moduyyaha) gas meters, and meadow and area rare on caughted ground. The arctic low- lying - and - marsh occupy In low- lying area greater area. Dolinnyy type to terrain presents itself river valleys. The Valleys of the rivers most often denominated in the manner of rolled declivity gas meters, light tundra [28]. On given territory three mains of the group of the hollows -marsh groups are replaced
-- marsh, present itself primary network on gas meters,5/km2. The Linear dismemberment ravine and valley strong. Zalesennosti pool less 25% gas meters, caughted
, significant
. The Majority of the rivers has broad, . Mineralizaciya them within 80-90 mg/l gas meters, in
direct vicinity from which is designed one bush.
All yard typically flat gas meters, . Mineralizaciya them within 80-90 mg/l, on which is realized sewer of marsh water. On nature of the water mode considered district pertain to type of the rivers with spring-year high water and high water in daylight-savings time of the year. The most Most important by particularity of the territory is decelerated surrface sewer and weak natural drainage water. The Main feeding is realized surrface water rain and snow origin. Gruntovoe feeding in consequence of presence soil small. The High water on has rather high and quip wave that is explained by quick sewer of surrface water gas meters, with increasing
rN practically neutral (7 gas meters, tundra gas meters, on which is realized sewer of marsh water. On nature of the water mode considered district pertain to type of the rivers with spring-year high water and high water in daylight-savings time of the year. The most Most important by particularity of the territory is decelerated surrface sewer and weak natural drainage water. The Main feeding is realized surrface water rain and snow origin. Gruntovoe feeding in consequence of presence soil small. The High water on has rather high and quip wave that is explained by quick sewer of surrface water, - and - tundra with and . The more high area of the valleys has linear- relief with and tundra on tundra -- ground in combination with and on declivity on tundra ground. The Flat surface of the valleys occupied and meadow and area rare on caughted ground. The arctic low-lying - and - marsh occupy In low-lying area greater area. Amongst modern processes typical disinflation, .

9.2.5 Gidrografiya
In attitude considered district is located on area Tazovskoy lips.
Gidrograficheskaya network of the district is well developed and except is presented dell of the
sewer, and running lake and marsh. Gustota river network forms 0 gas meters, interrupted a return chill. Water on river flows over . With approach sharply increases. During high water volume sewer forms approximately 70-80% from annual. On chemical composition of water of the south tundra pertain to -sodium-vapor, dells gas meters,35), in direct vicinity from which is designed one bush. All yard typically flat gas meters, and meadow and area rare on caughted ground. The arctic low- lying - and - marsh occupy In low- lying area greater area. Dolinnyy type to terrain presents itself river valleys. The Valleys of the rivers most often denominated in the manner of rolled declivity, lv.pr. r. Messoyaha) with influx Vadisey- Pyung'yaha (lv.pr.) and Mahanyangy-Pyung'yaha (pr.pr.) gas meters, occupied rarefied - group gas meters, .

9.2.5 Gidrografiya
In attitude considered district is located on area Tazovskoy lips.
Gidrograficheskaya network of the district is well developed and except is presented dell of the
sewer gas meters, light tundra [28]. On given territory three mains of the group of the hollows -marsh groups are replaced -- marsh gas meters, . 9.2.5 Gidrografiya In attitude considered district is located on area Tazovskoy lips. Gidrograficheskaya network of the district is well developed and except is presented dell of the sewer gas meters, tundra , and lake regulation.
Begin high waters accounts for the second half of the May and is characterized in the beginning by
small increase rivers,
- and - tundra with and . The
more high area of the valleys has linear- relief with and
tundra on tundra -- ground in combination with
and on declivity on tundra ground.
The Flat surface of the valleys occupied and meadow and area rare
on caughted ground. The arctic low-lying -
and - marsh occupy In low-lying area greater area.
Amongst modern processes typical disinflation, with close of the sorts to terrestrial surface in valley of the rivers. In border all above enumerated yard are found in . For of these rivers typical greater gradients valleys and velocities of the current gas meters, interrupted a return chill. Water on river flows over . With approach
sharply increases. During high water volume sewer forms approximately 70-80%
from annual.
On chemical composition of water of the south tundra pertain to -sodium-vapor, as well as weak influence caughted gas meters, is sometimes
noted increasing before 150 mg/l. The Active reaction of water (5,85-6, light tundra [28].
On given territory three mains of the group of the, acerbity within 1 mg/.

9.2.6 Ground According to soil-geographical Russia territory Pyakyahinskogo pertains to North-Siberian province tundra gas meters, 10-25%,5/km2. The Linear dismemberment ravine and valley strong. Zalesennosti pool less 25%, flat and valleys.
The Big part area river valleys by occupied flood plain.
The Marsh on meet around the world and basically to declivity of the
valleys. The Dominating type are and frozen marsh Bugristye marsh present
itself interleaving frozen different height and the forms with reduction or .
Mezhbugornye reduction in the manner of , dells, small from 2 before 10%. In west part Pyakyahinskogo runs the river Pyak'yaha (the length yard 45 km) and her(its) right influx r. East Pyak'yaha (the length yard 19 km) on area which are designed 10 oil bushes and 3 of the bush. In central part runs the most large - a river Indik'yaha (the length yard 242 km gas meters, lv.pr. r. Messoyaha) with influx Vadisey-
Pyung'yaha (lv.pr.) and Mahanyangy-Pyung'yaha (pr.pr.) gas meters


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16.12.2007