Tours in Germany: curative tourism and recreation, resorts, attractions, excursions
  Going on vacation? Note Germany is one of the richest European countries with a controversial past, but at the same time attracting many tourists a variety of excursions and…

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Rezekne Attractions Guide Area
  Rezekne (Rezekne) - large Republican city in Eastern Latvia, the geographical centre of Latgale, located on the eponymous river. The city's area of 17.5 sq. km population 33042 residents,…

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The largest lakes of the world

 

o lake Michigan 58 thousand km2;

o lake Huron – 59,6 thousand km2;

o lake Victoria 68 thousand km2;

o lake superior is estimated at 82.4 thousand km2;

o sea-Caspian lake – 376 thousand km2.

The deepest lakes of the world are:

o Issyk-Kul – 668 meters;

o Niassa – 706 meters;

o the Caspian sea – lake – 1025 meters;

o Tanganyika is 1470 meters;

lake Baikal is 1620 meters.

The largest lake on the planet Earth is the Caspian sea, it is located in the internal regions of Eurasia and contains 78 thousand cubic kilometers of water – more than 40% of the total water lakes in the world, by area, the lake superior even to the Black sea. The sea, the lake is called that only because it has the most marine of the properties of large – area, large volume of water, severe storms, and specific hydrochemical conditions.

From the South to the North of the lake, the Caspian sea stretches for almost 1,200 miles, and from West to East it stretches from 200 to 450 kilometers.

Origin this is the oldest part of the salted lake bluff, which existed 5 to 7 million years ago. In the ice age into the Caspian sea from Continue reading

LONG – Lake Blue

 

Children’s camp “Blue lake” was founded in 1991 for the children of workers and employees of the Leningrad plant “Engine”. The DOL “Blue lake” is a celebration of summer, joy, peace, understanding and creativity. The camp is located in the Vyborg district on the shore of one of the most beautiful lakes of the Karelian isthmus. Water space, scenic natural landscapes, fresh air, and help you create a unique microclimate. Each year, it welcomes hundreds of boys and girls, but not because “magical lake blue magnet”. Children and parents know that the experienced teaching staff of the camp is always ready to organize their stay and make it informative and interesting. Highly professional, friendly team “Blue lake” invests a lot of effort in improving his beloved camp. For better organization of summer recreation here. The large well-landscaped area of twelve hectares, is conveniently and compactly located.

– winter seven two-storey buildings with rooms for 4-6 people. The total capacity of the camp is 550 people per shift. All residential buildings have toilets and wash areas with nogometni on the floor. There are also showers on the floor, clothes dryer and bathroom hygiene, Laundry at the camp.

– sports grounds for playing basketball, volleyball. football, mini football, badminton; the pride Continue reading

The Caldera of Uzon volcano description

 

The Uzon Caldera is a unique area manifestation of modern volcanism. The Caldera of Uzon volcano is on the Kamchatka Peninsula on the territory of the Kronotsky reserve, South of Kronotsky lake. This is the place that shaped a unique symbiosis of wild nature and volcanism.

The Uzon Caldera was formed about 40 thousand years ago on the site of a huge volcano destroyed near a powerful explosive eruptions. Caldera is a massive bowl-shaped depression about 150 sq km, surrounded by steep ledges, the height of which ranges from 200 to 850 m.

The hydrothermal system of the Caldera of volcano Uzon is one of the most powerful on the Kamchatka Peninsula. On the territory of the width of 200-350 m and is located more than a thousand thermal springs in various sizes and shapes, a large number of thermal lakes, the outputs of the gas-steam jets, mud volcanoes and mud pots. There are also outputs of Seltzer.

The Uzon Caldera is a unique place where there are a variety of existence of young volcanism of different composition, the products of glaciation, as well as connection with sulfatar fields with native sulphur deposits and accumulations of hydrothermal altered rocks of all colors.

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