Liman (landform) in the context of "Lake Razelm"

Play Trivia Questions online!

or

Skip to study material about Liman (landform) in the context of "Lake Razelm"

Ad spacer

⭐ Core Definition: Liman (landform)

A liman is a wide estuary formed as a lagoon at the mouth of one or more rivers where flow is constrained by a sediment bar created by sea or river current. The hydrological term comes from the Russian language and is used in various national and regional languages for estuary lagoons all around the Black Sea and Sea of Azov coasts.

A liman is classified as either maritime or fluvial: "maritime" if its sediment bar was formed by sea current; "fluvial" if the bar is created by obstructed flow in a saturated river.

↓ Menu

>>>PUT SHARE BUTTONS HERE<<<

👉 Liman (landform) in the context of Lake Razelm

Lake Razelm or Lake Razim (Romanian: Limanul Razim, Limanul Razelm) is a large freshwater lagoon on the shores of the Black Sea in Romania, south of the Danube Delta and part of its World Heritage Site. It is the largest liman in Romania.

The name is also sometimes applied to the complex it forms with several other limans and lagoons. This complex can be separated into two subgroups. The northern subgroup contains freshwater Razelm and Lake Golovița, which are connected by a channel 3.1 km (1.9 mi) wide, whereas the southern group is made up of salt lakes. All these lakes cover an area of about 1,000 km (390 sq mi), of which 400 km (150 sq mi) is the area of Lake Razelm alone.

↓ Explore More Topics
In this Dossier

Liman (landform) in the context of Sea of Azov

The Sea of Azov is an inland shelf sea in Eastern Europe connected to the Black Sea by the narrow (about 4 km (2.5 mi)) Strait of Kerch, and sometimes regarded as a northern extension of the Black Sea. The sea is bounded by Russia on the east, and by Ukraine on the northwest and southwest (the parts of Ukraine bordering the sea are currently under Russian occupation). It is an important access route for Central Asia, from the Caspian Sea via the Volga–Don Canal.

The sea is largely affected by the inflow of the Don, Kuban, and other rivers, which bring sand, silt, and shells, which in turn form numerous bays, limans, and narrow spits. Because of these deposits, the sea bottom is relatively smooth and flat, with the depth gradually increasing toward the middle. Because of the river inflow, water in the sea has low salinity and a high amount of biomass (such as green algae) that affects the water colour. Abundant plankton result in unusually high fish productivity. The sea shores and spits are low; they are rich in vegetation and bird colonies. The Sea of Azov is the shallowest sea in the world, with the depth varying between 0.9 and 14 metres (3 and 46 ft). There is a constant outflow of water from the Sea of Azov to the Black Sea.

↑ Return to Menu

Liman (landform) in the context of Dnieper-Bug estuary

The Dnieper–Bug estuary (Ukrainian: Дніпровсько-Бузький лиман, romanizedDniprovsko-Buzkyi lyman), also called the Dniprovska Gulf, is an open estuary, or liman, of two rivers: the Dnieper and the Southern Bug (also called the Boh River). It is located on the northern coast of the Black Sea and is separated from it by the Kinburn Spit and the Cape of Ochakiv.

↑ Return to Menu

Liman (landform) in the context of Dniester Liman

Dniester Estuary, or Dniester Liman (Ukrainian: Дністровський лиман; Romanian: Limanul Nistrului) is a liman, formed at the point where the river Dniester flows into the Black Sea. It is located in Ukraine, in Odesa Oblast, and connects Budjak to the Ukrainian mainland. The city of Bilhorod-Dnistrovskyi lies on its western shore and Ovidiopol on its eastern shore. Shabo, situated downstream of Bilhorod-Dnistrovskyi, is known for its wine. The estuary hosts the Bilhorod-Dnistrovsky Seaport.

The area of the liman varies between 360 and 408 km, it is 42.5 km long and has maximum width of 12 km. The average depth is 1.8 m, the maximum depth 2.7 m.

↑ Return to Menu

Liman (landform) in the context of Nikolaevsk-on-Amur

Nikolayevsk-on-Amur (Russian: Никола́евск-на-Аму́ре, romanizedNikoláyevsk-na-Amúrye) is a town in Khabarovsk Krai, Russia located on the Amur River close to its liman in the Pacific Ocean. Population: 17,815 (2024); 22,752 (2010 census); 28,492 (2002 census); 36,296 (1989 Soviet census).

↑ Return to Menu

Liman (landform) in the context of Lake Varna

Lake Varna (Bulgarian: Варненско езеро, Varnensko ezero) is the largest by volume and deepest liman or lake along the Bulgarian Black Sea Coast, divided from the sea by a 2 km-wide strip of sand and having an area of 19 km, maximal depth 19 m, and a volume of 166 million m.

The lake has an elongated shape, its south shores are high, steep and wooded, and the north slant. Lake Varna was formed in a river valley by the raising of sea level near the end of the Pleistocene. Its bottom is covered by a thick alluvium of slime and hydrogen sulphide mud in the deepest parts; there are large deposits of medicinal fango (mineral mud). A number of rivers pour into the lake, including Devnya and Provadiyska that empty near the western shores of Lake Beloslav, which is connected to Lake Varna.

↑ Return to Menu