Big Yaly-Maynaksky lake ( Ukrainian Veliky Yali-Maynatsky lake , Crimean-Tat. Büyük Yalı Moynaq gölü, Buyuk Yaly Moynak golyu ) - a lake located in the west of the Evpatoria City Council ; The 3rd largest lake in the Evpatoria City Council . The area is 0.6 km² [2] . The type of general mineralization is salty [3] . The origin is estuary . The hydrological regime group is closed .
| Big Yaly-Maynak Lake | |
|---|---|
| ukr Veliké Yali-Mainack Lake , Crimean Tat. Büyük Yalı Moynaq gölü | |
| Morphometry | |
| Dimensions | 1.5 × 0.75 km |
| Square | 0.6 km² |
| Deepest | 0.6 m |
| Average depth | 0.4 m |
| Hydrology | |
| Mineralization type | salty |
| Pool | |
| Pool area | 17.4 km² |
| Location | |
| A country |
|
| Region | Crimea |
| Areas | Evpatoria City Council , Evpatoria City District |
Content
Geography
Included in the Evpatoria group of lakes . The catchment area is 17.4 km². The length (maximum, between the two extreme points of the water mirror) is 1.5 km. The greatest width is 0.75 km, the average is 0.5 km. The average depth is 0.4 m, the greatest is 0.6 m. Height above sea level: m. The nearest settlement is Zaozernoye , located directly east of the lake.
The Big Yaly-Maynakskoe Lake is separated from the Black Sea by the isthmus along which the Friendship Alley passes. Zaozerny , and also located pensions and recreation centers. The lake basin of a reservoir of irregular round elongated shape, elongated from north to south. The banks are gentle, the coastline is indented. Rivers do not flow; in the north, rhizome flows into the lake. The southwestern part of the lake is separated from the main part by a dam along which the road passes.
At the bottom lies a thickness of bottom sediments: silty black in the upper layer, then gray and steel-gray, sometimes with a bluish tint. Higher aquatic vegetation develops successfully only in the desalinated upper reaches of lakes and at the outlets of low-mineralized groundwater. The lake is overgrown with aquatic vegetation mainly in desalinated areas - in lagoons near embankments, in the mouths of flowing beams, in the area of groundwater outlets. Here, various algae intensively develop, up to the flowering of water. In some years, algae give a reddish or greenish tint to lake brine in summer.
The average annual rainfall is about 400 mm . Nutrition: mixed - surface and groundwater of the Black Sea artesian basin , sea filtration water.
Economic Significance
Mud (silt sulfide of the coastal type) of the lake as a result of economic activity lost their therapeutic purpose [4] .
Notes
- ↑ This geographical object is located on the territory of the Crimean Peninsula , most of which is the object of territorial disputes between Russia , which controls the disputed territory, and Ukraine , within the borders of which are recognized by the international community, the disputed territory is located. According to the federal structure of Russia , in the disputed territory of the Crimea, the constituent entities of the Russian Federation are located - the Republic of Crimea and the city of federal importance Sevastopol . According to the administrative division of Ukraine , in the disputed territory of the Crimea are located the regions of Ukraine - the Autonomous Republic of Crimea and the city with a special status Sevastopol .
- ↑ Surface water resources of the USSR. Volume 6: Ukraine and Moldova. Issue 4: Crimea
- ↑ Map sheet L-36-103 Evpatoria . Scale: 1: 100,000. State of the terrain for 1986. 1988 edition
- ↑ Catalog of mud deposits of the USSR, 1970
Sources
- GNPP Cartography (Atlas of Geography of Ukraine ), 2003
- On the site of the Reskomvodkhoz ARC (Inaccessible link - history ) .