"Here in the mountains there are several caves, of which Marusinskaya the largest and most interesting.
The entrance to the cave has a triangular shape and is located quite high above the ground (40-50 meters.).
First researcher is mired in the first hall, length 35-40 meter. and a height of 30 meters. At the end of it is a deep well, into which it is easy to fall. Before reaching the well it is necessary to turn to the left, into a niche; there is a long passage in it, having an ascent and descent. At the top of the rise, the passage narrows between two stalagmite pillars. Next, we have to move on all fours. This passage is up to 50 meters long., after which the Explorer enters a wide corridor that leads him into a second hall of snowy whiteness. It is small, but very beautiful. From here again through a narrow corridor you can get to the third hall, the most majestic. It is much larger than the first two taken together. Here stalactites and stalagmites formed magnificent colonnades. Throughout the walls are layers of lime, giving the impression of frozen waterfalls. Here and there, in the hollows, water has collected, so pure and clear that the researcher notices it only when he gets into it with his foot. Here again there is a very deep well and side passages. In this great hall, the observer is involuntarily struck by the amazing acoustic effects — every loud word is answered by a hundred-voice echo, and when a stone falls into the well, a roar rises, like cannon fire; it seems as if collapses occur and the vaults collapse»
Объяснение:
Мне сложно писать о самих пещерах, я написал текст о Маркуинских пещерах. Тут можно всё списать и без использования ''Маркуинских пещер''
Flood — district flooding as a result of water level lifting in the rivers, lakes, the seas because of rains, rough thawing of snow, a wind setup of water on the coast and other reasons which causes a loss to human health and even leads to their death, and also causes a material damage. Floods quite often are caused by water level increase in the river owing to course blocking up by ice at an ice drift (jam) or owing to a course blockage under a motionless ice cover congestions of intra water ice and formation of an ice stopper (zazhor). Quite often floods arise under the influence of the winds making up for water from the sea and causing increase of level at the expense of a delay in the mouth by the brought river of water. Floods of this kind were observed in Leningrad (1824, 1924), the Netherlands (1953). On sea coasts and islands of flood flooding of a coastal strip by a wave which is forming at earthquakes or eruptions of volcanoes at the ocean (can result see. Tsunami). Similar floods are frequent on coast of Japan and on other islands of the Pacific Ocean. Floods can be caused by breaks of dams, protective dams. Floods happen on many rivers of Western Europe — Danube, Seine, Rhone, On and others, and also on Yangzi's rivers and Huang He in China, Mississippi and Ohio in the USA. In the USSR big floods were observed on the Dnepr Rivers (1931) and Volga (1908 and 1926).
"Here in the mountains there are several caves, of which Marusinskaya the largest and most interesting.
The entrance to the cave has a triangular shape and is located quite high above the ground (40-50 meters.).
First researcher is mired in the first hall, length 35-40 meter. and a height of 30 meters. At the end of it is a deep well, into which it is easy to fall. Before reaching the well it is necessary to turn to the left, into a niche; there is a long passage in it, having an ascent and descent. At the top of the rise, the passage narrows between two stalagmite pillars. Next, we have to move on all fours. This passage is up to 50 meters long., after which the Explorer enters a wide corridor that leads him into a second hall of snowy whiteness. It is small, but very beautiful. From here again through a narrow corridor you can get to the third hall, the most majestic. It is much larger than the first two taken together. Here stalactites and stalagmites formed magnificent colonnades. Throughout the walls are layers of lime, giving the impression of frozen waterfalls. Here and there, in the hollows, water has collected, so pure and clear that the researcher notices it only when he gets into it with his foot. Here again there is a very deep well and side passages. In this great hall, the observer is involuntarily struck by the amazing acoustic effects — every loud word is answered by a hundred-voice echo, and when a stone falls into the well, a roar rises, like cannon fire; it seems as if collapses occur and the vaults collapse»
Объяснение:
Мне сложно писать о самих пещерах, я написал текст о Маркуинских пещерах. Тут можно всё списать и без использования ''Маркуинских пещер''
Flood — district flooding as a result of water level lifting in the rivers, lakes, the seas because of rains, rough thawing of snow, a wind setup of water on the coast and other reasons which causes a loss to human health and even leads to their death, and also causes a material damage.
Floods quite often are caused by water level increase in the river owing to course blocking up by ice at an ice drift (jam) or owing to a course blockage under a motionless ice cover congestions of intra water ice and formation of an ice stopper (zazhor). Quite often floods arise under the influence of the winds making up for water from the sea and causing increase of level at the expense of a delay in the mouth by the brought river of water. Floods of this kind were observed in Leningrad (1824, 1924), the Netherlands (1953). On sea coasts and islands of flood flooding of a coastal strip by a wave which is forming at earthquakes or eruptions of volcanoes at the ocean (can result see. Tsunami). Similar floods are frequent on coast of Japan and on other islands of the Pacific Ocean. Floods can be caused by breaks of dams, protective dams.
Floods happen on many rivers of Western Europe — Danube, Seine, Rhone, On and others, and also on Yangzi's rivers and Huang He in China, Mississippi and Ohio in the USA. In the USSR big floods were observed on the Dnepr Rivers (1931) and Volga (1908 and 1926).