Презентация, доклад по английскому языку на тему Kamchatka

Russian Cossacks more then 300 years ago. Up to 1990 foreigners could not step into the Kamchatka area, and even to Russians the special admission was required. But those who wished to see the magic world of Kamchatka with their own eyes, went there, despite all barriers. Today Kamchatka is opened to everybody : to the tourists, and the scientists, and the businessmen.

1932 as a part of Khabarovsk territory. In January, 23rd, 1956 it was allocated to an independent area.

472,3 thousand sq. km.

the cold sea of Okhotsk, in the east by the Bering sea and the Pacific ocean. The northern point of the area is located almost at the Arctic circle, the southern point cape Lopatka towers over the First Kuril passage.

kilometers two basic ridges are stretched: the Sredinniy and the Vostochniy. The central Kamchatka lowland, with the Kamchatka river, is situated between them.

frosts in winter and hot days in summer. Summer here is cool with large amount of foggy and rainy days. In the north of the peninsula the climate is more continental.

Therefore each place has its own special climate.

makes this part of Russia unique.

riches including 227 kinds of fishes, are the most valuable. 15 species of crustacean, more than 30 species of mollusks, almost 200 species of sea seaweed, 18 species of sea animals are very important too.

gas, coal, native sulphur, thermal waters, gold and silver, nickel, copper, platinum, tin, lead, zinc.

forest products, fire wood, the major kinds of agricultural production are important.

active volcanoes; the volcanic plateaus, the Alpine meadows, canyons.

see the Ostryi Tolbachik and the Ploskii Tolbachik Volcanoes.

km south of Petropavlovsk-Kamchatskiy.

Volcano.
1n the foreground, one can see tuffs, structuring the outer slope of Мutnovskaya Sopka Volcano, severely demolished as a result of chemical weathering.

entire Кronotskiy Reserve, is inhabited by bears. Plant shoots browsed by Kamchatka bears appear on warm thermal grounds and near thermal springs early in spring.

and hunt the fishes with fervor, but when the mass run of the fishes is over, the bears return to their grasslands.

and power of endurance, excellent reaction and remarkable coordination of movements.

around the lake, confined to abyssal tectonic fault intersection zones. Кostakan cone is of most recent formation, it took shape around 600 years ago. The slag barren lands around the cone are gradually overgrown with white reindeer moss and cedar elfin wood.

sulfuric acid in Тroitskogo Crater of Мalyi Semyachik Volcano. Lake depth reaches 150 meters. Bubbles and sulfuric foam rise to the surface of the lake.
Кarymskiy Volcano can be seen in the background.

stream. The water gets into the lake in portions during floods and freshets on the tributaries, and flows out uniformly, seeping via system of crevasses in lava and filtering through slag.

alternation of igneous rocks, structuring the volcanic dome, is uncovered. The unique bright color of the lake is due to the unusually high acidity of the water.

Вurlyashchii ('Boiling') Volcano
A small volcano every now and then splashes out liquid mud or releases vapor with a low hissing. White depositions of salts may be seen on the slopes of the volcano. This is a miniature geyser with splashes of slurry instead of water.

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