Презентация на тему Рельеф Казахстана

Saur-Tarbagatay, Tien-Shan)

the Kazakhstan is divided into 2 parts: large –

lowlands and plateau (west, north and central KZ), small – high mountains (east and south-east). The surface has a slope from south-east to north-west.
The structure of a surface has the large meaning for economic activity of the population:
1) The lowlands, plains and intermountain valleys are most useful for agriculture.
2) The mountain slopes covered with rich vegetation are perfect pastures for cattle.

the territory of Kazakhstan are occupied with 3 lowlands:

West-Siberian, Turan and Caspian.

West-Siberian lowland is monotonous. Only in some places there

are chains of small lakes. This lowland has a slope from the south to the north. In the south it is 200 m above the sea level, an in the north only 100.

south and south-west of the republic. It raises in

the south on 200 m. In north and the south of lowland it’s broken with sand deserts.

monotonous. It consists of clay plains and sandy files.

On the West from the river Ural there are sand-markets.

plateaus. The biggest of them are: Ustyurt, Turgay, Pre-Ural.

Ural and Caspian seas. It’s average height is 200

m above the sea level. It is combined from thickness clay, sandstone and limestone.

the east f Mugodzhary. It’s average height above the

sea level is 100 m. It connects with West-Siberian lowland.

Caspian lowland and Mugodzhary. It’s average height above the

sea level is about 300 m. It consists of limestone, chalk and is watering by river Emba.

the territory of Kazakhstan: Tien-Shan, Altai, Saur-Tarbagatay.

Saur and Tarbagatay. It consists of clay, crystal schist,

granite and limestone. It is located between Alakol basin in the north and river Orin in the south.

Southern, Central and Kolbinsky. There are glaciers and hollows,

deposits of polymetal ores. Altai consists from gneisses, crystal schist, marble and limestone.

Kazakhstan. In the Central part of Tien-Shan is the

highest point – Khan Tengri (6999 m).