Central Asia, including arid and semi-arid plains, plateaus and highlands. V. limited on the southern part of the Great Khingan, Y. longitudinal tectonic depression of the upper Indus and Brahmaputra. On Z. C. and the border of Central Asia corresponds to the mountain ranges of the Eastern Kazakhstan, Altai, Western and Eastern Sayan.
Relief . Central Asia has a larger height, and clearly distinguished 2 basic tiers of relief. Form the lower tier of the Gobi, Alashan, Ordos, Tarim and Dzungarian plains, the average altitude of 500-1500 m. of which Upper tier — Tibetan plateau, within which the average height increase up to 4-4,5 thousand m. Plains and plateaus are isolated from each other linearly extended mountain ranges of the Eastern Tien Shan, Kunlun, Nan Shan, Mongolian Altai, Karakorum, etc. Gandisyshan the Highest point of the Central Asia — Chogori in Karakorum (8611 m). Axial geological structure of Central Asia is the Western continuation of the Sino-Korean platform. S. with this group of arrays is framed Mongol-Kazakh, and Y. — Kurlansky belts of Paleozoic folded structures. C. on the Tibetan plateau, within Changtan, manifested Mesozoic folding. The modern relief is notable for the complex combination of gravelly and sandy plains (with the areas of hummocks), mountain chains and massifs, the highest of which Continue reading
East Asia is the Eurasian outskirts, facing the Pacific ocean. It stretches from the Soviet Far East in the North to southern China. Eastern Asia also includes Sakhalin island, the Kuril, the Japan, Taiwan, Hainan.
In East Asia there is no structural-geomorphological unity. Its mainland is an ancient land, within which the medium fold-hat mountain combined with accumulative plains. Islands and their surrounding sea belong to the Pacific zone, where the dip of the oceanic lithosphere of the Pacific plate under the continental margin of the Eurasian plate and lying in front of her island arc. This belt is marked by the strong development of seismology and volcanism.
The natural integrity of the East Asia define the characteristics of its climate and the organic world.
The basic pattern of climate formation is the East Asia monsoon circulation, creating a marked difference between wet cold and dry warm seasons. East Asia lies in the temperate and subtropical zones, and in the South sets in the tropical belt and temperatures in its range in a direction from North to South vary, but the main features of the monsoon climate persisted throughout. Massonnet the climate that can be considered the most striking feature of East Asia has left an indelible imprint on almost all sides Continue reading
It is very important to inculcate the younger generation love to native culture.
Regardless of the place of residence of the Kazakhs must know the language and traditions of his people.
A. N. Nazarbayev, the President of the Republic of Kazakhstan
There are on the map village of the Omsk region under the sonorous, beautiful name Krasnogorka, which in 2010 will celebrate its 110th anniversary since the founding of migrants from Ukraine.
And once there was a village lane, on which lands and founded the settlement. Here’s what history tells us:
The village of Maina was called by name here wandering tribe of Kazakhs lane, that in translation from Kazakh means “rich steppes with an abundance of water and lush grass”. Why is the Kazakh? Because from the second half of the 19th century on the territory of this lot was occupied by yurts of Kazakh nomads. 12 kilometers to the South lived the nomad Sahasi, and West of USBI. It was rich Kazakhs, bred horses, and almost with their herds had no boundaries.
The first settler Continue reading