Apshinec' is a lake of glacial origin, located in Rakhiv district Transcarpathion region. It lies on the south-east slope of Svidovec' massif on the altitude 1487m. Length - 126m., width - 100m., area-1,2 hectares., a depth is to 3.3m. A hollow of prolonged form with the low stained billow. On south-west part of the lake a sedge bog is located. It feeds on mainly by spring waters which falls in western part of lake. Water is clean, transparent, its temperature in June +10 - +13 .Ñ. It freezes in winter. A bottom is plain, near the banks there are boulders. Among a flora widespread: a sedge, fauna, is presented by the separate types of microscopic crustaceans. Apshinec' affiliate to the Apshinec' zakaznic.
Brebeneskul is a lake of glacial origin in the Rakhiv district. It lies between the main spine of the Chornohora massif and Hutin-Tomnatik mountain on the altitude of 1801m., length 134 m., width 28-44 m., depth to 2,8 m. The lake have oval form. The banks are steep and high, with stone mineral deposits. It feeds on by atmospheric precipitates and ground waters. The water is clean, with low mineralization . A bottom rises in east direction, on a depth it is covered by grey silt. The microscopic crustaceas happens. An object of tourism.
Breskul - the lake of glacial origin in Rakhiv district, Transcarpathion region. It lies on the north-western slope of Breskul mountain, Chernogora massif on the altitude of 1750m. A hollow has the extended form, its length 52m., width 20m. Because of the intensive overgrowing of the lake it's sizes diminished, length became 37m., a width 12-15m., area 0,1 hectares, debth 1,2m. The lakes is drainles, it feeds on mainly by atmospheric precipitates. The water is clean, transparent, with low mineralization. The bottom is plain, covered by darkly grey silt. As about plants there is a sedge, from the representatives of fauna - the microscopic crustaceas. Breskul - located in the Carpathian Biosphere Reserve.
Verhne - the lake lies on the Chernogora massif on the altitude 1628 m. The length 105m., width to 26m., area 2400 m2, the depth more than 3m. The hollow of the extended form. It feeds on by the atmospheric precipitates. The water temperature in summer +13Ñ. It freezes in winter. The level of water mineralization is low (hard remnant 42 ìl/l). The bottom near the banks is covered by the wreckages of conglomerates, on the depth - by the grey silt.
Vorozheska - lies on the slopes of Svidovec' massif on the altitude 1460m. It consists of two small lakes. The overhead has a round form ( diameter 95m., area 0,7 hectares, depth to 4,5m, the lower lake, located on 15m. below, from overhead, it has extended form (length 76 m., width 28 m., area near 0,2 hectare, depth to 1,9m.). The lakes feeds on, with stream waters. The water is clean, transparent; temperature in summer +12Ñ. The bottom is declivous and silty. The fauna is presented by the separate types of microscopic crustaceans. The object of tourism.
A mother had two sons. They were beautiful, kind and strong. In summer they shepherded sheep on mountain valleys, in winter helped on an economy. Once youths met a very beautiful girl. Her name was Marichka, she had a long blond-brown plait and was very beautiful.
Both brothers felt in love. What to do? They decided to do the following: who first will swim across a mountain lake that could be seen in a cavity between the mountains, Marichka will fall to his lot. But as they swam to the middle of the lake, a black cloud suddenly appeared behind a mountain, and a frightful storm began. The water in lake rose, heavy wave spring up and brothers draw on the bottom, in a frightful abyss.
A long time their mother waited for them, but they did not return, Marichka did not see them anymore too. But not far from that lake shepherds pastured sheep, they saw and knew those youths. The shepherds got down in a village and told mother everithing that they saw.
The mother began to run to that lake, fall on knees and began to cry and yelling:
-Lake, lake! Why do you such hostile (vorozhe), to me, why did you killed my sons-twins?!
"Vorozhe.vorozhe.", - caught up wind. And the forests began to rustle higher lake. From those times that lake begun to name Vorozheska (Hostile).
Gerashaska - a lake lies on the Svidovec'massif slopes on the altitude 1577 m, length 125m., width 110m., area, is 1,2 hectares, depth to 1,2m. The hollow has a wrong rectangle form, limited by the wide stained billow. The north banks became over Sedge. It feeds on mainly by snow waters. The water temperature in summer low (in June +10-+11.Ñ). The water-plants are not many, from a fauna the most widespread microscopic crustaceas.
Dragobrat - is a lake of glacial origin. It is located in the Rakhiv district, Transcarpathian region. It is situated near the northern slope of Bliznica mountain on Svidovec' massif on the altitude 1600m. A hollow has an extended form. Length 55m., width 21m., area, is 0,1 hectares., depth to 1,2m. The banks consist of moraine. The lake feeds on with ground and atmospheric waters. The banks overgrow by Sedge. From ichthyofauna microscopic crustaceas happen only. The object of tourism.
Nesamovite (Furious) - is a lake of glacial origin. Located in Rakhiv district, Transcarpathian region. It lies on the slope of mountain Turkul, Chernogora massif, on the altitude 1750m. Length 88m., width 45m., an area is 0,3 hectares., a depth is to 1,5m. The hollow of extended form. The north banks limited by the low stained billow, on south by stone embankments. It feeds on atmospheric waters. Nesamovite freezes in winter. The bottom is covered by boulders, in south part sand deposits are prevalent.
Guzuls tells, that on Goverla there is a saddle and in it the lake. The lake is called Nesamovite (furious), because it worries all the time, even when the wind do not blow.
Near the lake there is the mountain Pip-Ivan and the Black rock on it. On that rock Dovbush killed the devil. That's why the rock become black.
NizhneNizhne (Lower lake) - the lake lies on the Chernogora massif on the altitude 1515m. Length 70m., width to 29m., area 0,2 hectares, depth to 2 m. The hollow has a form of wrong rectangle. The banks mainly steep, except the low south and north areas which are boggy. The lake feeds on by a superficial flow. The water in the lake is transparent, it has durty color. It freezes in winter. A bottom near the banks is covered by the wreckages of sandstones and conglomerates, on the debth by grey silt. A plankton is presented by microscopic crustaceas.
MaricheykaMaricheyka is a lake of glacial origin. It is located in Rakhiv district, Transcarpathian region. It lies on the north-east from a mountain Shurin-Gropa on the Chornohora massif, on the altitude 1510m. An area is 1 hectare, depth to 0,8m. The hollow of an extended form. The banks are low, surrounded by fir-trees and mountain pine-trees forest. The lake feeds on underground and partly by atmospheric waters. The water is fresh, clean. Along the banks lake is overgrows by sedge. The objekt of tourism.
It is told, that in old times Tatars attacked our land. They destroyed villages, killed people and that's why the populations escaped in mountains. The Tatars also went to the mountains, to take them in a captivity. Maricheyka, the shepherd Ivan's wife, noticed Tatars and sent Ivan to warn highlanders, but she stayed to keep off the enemy.
Ivan began to run. Maricheyka took the place way to the enemies, she was caught, and forced to show the way to the highlanders. She led them in the swamped wildernesses. Then Tatars rushed to kill her, but in the last minute earth began to tremble, a hurricane rose, began thundered, rocks fell down. Earth parted - a lake appeared and all Tatars perished in it. People named that lake Maricheyka.