Напишете рассказ о Ладожском озере на английском. Пожалуйста!!! Очень безотлагательно!!!

Напишете рассказ о Ладожском озере на английском. Пожалуйста!!! Очень безотлагательно!!!

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Lake Ladoga is the largest in Europe. It implies the Neva river into the Gulf of Finland of the Baltic sea.
The lake basin is of glacial origin. About 12 thousand years ago, she was finally free of ice. And now the lake is inhabited by seals, which liked its natural environment.
The area of the Ladoga Islands more than 18 thousand sq. km. Vast expanses of the lake reminiscent of the sea. In its open part is not visible the coast, and strong winds sometimes turn it into a stormy mess, more insidious than some of the seas. The greatest length of lake Ladoga - 219 km, average width is 83 km, Average depth 50 m.
In lake Ladoga carry their waters major rivers, the Svir, the Vuoksa and the Volkhov, several dozen medium-sized rivers and hundreds of small. Derived from the one-the Neva river.
Ladoga's shores are diverse. In the North they are rocky and steep and have complicated shapes: cut by numerous bays and peninsulas jutting into the lake. Here are concentrated the greatest depths reaching 230 meters. The Northern shores and Islands of Ladoga have long served as quarries of building and decorative stone. Particularly intense Ladoga granite was developed during the building of St. Petersburg. For 150 years it was the main material for monumental building of the Northern capital. Ladoga granite мейд, for example, the famous Atlantes of the Hermitage, the Foundation of St. Isaac's Cathedral, Palace bridge across the Neva, the base of the monument "Millennium of Russia" in Novgorod.
The southern shores are low, swampy, they have smooth contours, are almost not dissected. The coastal part of the lake is characterized by a flat bottom with depths not exceeding 50 meters. Here are three wide, shallow land jutting out into the Gulf, called Svirskaya, Volkhovskaya and Schlisselburg. The shrubby areas interspersed with pine forests, sandy beaches, alluvial deposits of gravel and boulders. To the southern shores of the layers of limestone come close. Flowing down the cracks water
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