Deep lake (Ruzsky district, Moscow region): description, fishing and recreation

2024 Author: Harold Hamphrey | [email protected]. Last modified: 2023-12-17 10:06

Lake Glubokoe (the photos below demonstrate the beauty of this body of water) is a body of water in the Ruza district of the Moscow region. Until the eighteenth century, it was called Monastic.

Description of water object

Among the dense forests, away from the main roads, in the very center of the vast basin of the Ruzsky district of the Moscow region, there is a Deep Lake. This is a small secluded body of water, mostly surrounded by forest. From the village of Novogorbovo, a dirt road leads here, leading directly to the shore and wooden structures of the MGU biological station. Lake Glubokoe (Ruzsky district) is interesting for the unique purity of its waters, thanks to which a huge number of microscopic crustaceans live here, in addition, there are many different fish. The depth of this water body reaches 32 meters, although its area is relatively small: only 1.2 km long and 0.8 km wide. Another interesting fact related to the lake is that repeatedly marked fish from it was found in the neighboring lake Trostnenskoye, not far from the village of Onufrievo, about ten kilometers away. Apparently, these two objects haveunderground communication.

Neighbourhood

From the east side, quite high hills approach the shore of the lake. From the west, it is adjoined by a swamp covered with a moss carpet and overgrown with small willow and birch forests. Cranberries grow in abundance on moss tussocks. The shore on this side is hanging, formed by quagmires. The southern side of the reservoir is bordered by a huge swamp. In the spring, it is overflowing with melt water. They, flowing into the lake, give the water a brown tint, but over time it disappears. The northern part has a bay with a flat bottom. The depth here is only five meters, for anglers this is of the greatest interest. The Malaya Istra River originates from the bay; it is almost completely overgrown with dense reeds. There is a large hill on the northwest coast. The locals called it "the island".

The Riddle of Origin

Deep Lake (Moscow region) is a rather unusual body of water. There are several theories about its origin. The most common are glacial, karst and meteorite versions. The literature indicates the glacial origin of the reservoir: melting waters filled a deep depression of the Smolensk-Moscow Upland and gave rise to its existence. However, some facts do not fit with this theory. For example, all glacial lakes have the property of aging. This occurs in connection with silty deposits, the onset of peat bogs. However, all these factors are powerless here, and the mystery of the lake is still notdisclosed. The meteorite theory seems more likely, but there is also no evidence in its favor.

Lake Glubokoe (Ruzsky district): fishing

Even in the summer heat at great depths, the water temperature in the reservoir does not exceed six degrees Celsius. As a result, in the warm season, the fish prefers to stay in the coastal zone. That is why the wide bay on the northern side of the lake, having a depth of five meters, is a spawning and feeding place for many species of fish. In addition, the presence of reeds on the shores of the bay attracts young animals here. And the predators are coming after him. A deep lake and a bay are separated by an underwater edge. You can find it by fishing in a plumb line using a heavy lure. The fish here prefer to stay on the underwater slopes, which are located at a distance of 18-20 meters from the shore.

The bottom of the lake is dense, there is very little vegetation. Due to the protection of the coast and the terrain, the winds here do not create large accelerating waves, and the surf does not force the fish to leave the coastal zone. Only service boats are allowed, in summer fishing from rubber boats and rafts is allowed. This is the Deep Lake!

Fishing here attracts with its variety. You can catch perch and pike on circles or fish roach and bream in a baited place. In calm, calm weather, from a boat without anchoring by rafting, you can enjoy fishing in a plumb line on a jig or lure. Tackle is best used for deep sea fishing. In addition, long-range shore fishing has proven itself well.float rod or bottom tackle.

How to get there

This body of water can be accessed at the beginning of winters with little snow and during dry periods along several routes. The first - from the city of Zvenigorod, bypassing the villages of Shikhovo and Rybushkino, Kariyskoye and Faustovo, as well as Andreevskoye. This path will be about thirty kilometers. The second - by bus from the city of Zvenigorod to the village of Gerasimovo, and then about six kilometers on foot. Another way is possible - past Tuchkovo and Kulyubakino, through the village of Novo-Gorbovo and further about five kilometers along a dirt road.

What else is interesting about this object?

The deep lake of the Moscow region is a favorite place of pilgrimage for tourists and a good rest for lovers of hiking for berries and mushrooms. In addition, it is believed that the water of this reservoir has miraculous, healing properties. As a result, many people come here to relax and improve their he alth, firmly believing in the power of the relic lake. Pilgrims stop directly on the shore, pitching tents, or rent an apartment in neighboring villages - all in order to swim in the lake and recharge with the energy of its healing waters.

In addition, collecting minerals has become a new entertainment, and there is something to collect. There are a lot of samples, brought here by a melting glacier. Now they lie in bulk on open areas of the earth, and sometimes covered with a layer of turf. They are interesting in that they are the same age as the reservoir and serve as a kind of geological greeting from our distant past.planets.

Science Station

The deep lake is of great scientific interest. Back in 1891, a hydrobiological station was founded here, which monitors the reservoir. Based on the results of more than a century of study, scientists have come to the following conclusions.

1. Currently, due to anthropogenic intervention, this lake is a reservoir filled with the purest water. It is surrounded by a relic forest, untouched even during the Second World War.
2. Despite the fact that the morphometric parameters of the object are determined, the accuracy of these calculations is insufficient to characterize the processes that occur in this aquatic biogeocenosis. So the question of significant changes in morphometric parameters remains open.
3. The following hydrochemical properties of the lake have been determined: regardless of the ratio of ground and surface waters, as well as the amount of precipitation, the water here is always low-mineralized; during dry seasons, it is bicarbonate-magnesium, and during wet seasons, it is bicarbonate-calcium. This phenomenon is due to special biological production-destruction processes in the reservoir.