Map of the Crimea, showing the Syvash in black
|Location||Sea of Azov|
|Basin countries|| Ukraine,
|Max. length||200 km (120 mi)|
|Max. width||35 km (22 mi)|
|Surface area||2,560 km2 (990 sq mi)|
|Average depth||0.5–1 m (1.6–3.3 ft)|
|Max. depth||3 m (9.8 ft)|
The Syvash or Sivash (Russian and Ukrainian: Сива́ш; Crimean Tatar: Sıvaş or Сываш, "dirt"), also known as the Putrid Sea or Rotten Sea (Russian: Гнило́е Мо́ре, Gniloye More; Ukrainian: Гниле́ Мо́ре, Hnile More; Crimean Tatar: Çürük Deñiz or Чюрюк Денъиз), consists of a large system of shallow lagoons on the west coast of the Sea of Azov. Separated from the sea by the narrow Arabat Spit, the water of the Syvash covers an area of around 2,560 km2 (990 sq mi) and the entire area spreads over about 10,000 km2 (3,900 sq mi). Its eastern connection to the Sea of Azov is called the Henichesk Strait. The Sivash borders the northeastern coast of the main Crimean Peninsula; Ukraine and Russia dispute control of the area.
The Syvash nearly cuts the Crimean Peninsula off from the mainland, serving as a natural border for its autonomous republic. The long (110 km or 68 mi) and narrow (0.27–8 km or 0.17–5.0 mi) Arabat Spit runs to its east, separating it from the Sea of Azov. The two bodies are connected in the north at the Henichesk Strait beside the port of Henichesk. To its west, the isthmus of Perekop separates it from the Black Sea and connects Crimea to Ukraine.
The Syvash is extremely shallow. The deepest place is about 3 meters (9.8 ft), with most areas between ½ and 1 meter (18 in to 3 ft) deep. The bottom is covered with silt up to 5 m (16 ft) thick. Being very shallow, the waters in the Syvash heat up in the summer and produce a putrid smell. The wide area for evaporation also leaves the water extremely salty. The amount of various salts is estimated at 200 million metric tons. Several plants[clarification needed] harvest the mineral resources of Syvash. The Syvash area is a wetland of international importance. The shores are low, slightly sloping, swampy and salty. In summer, the water level of Syvash decreases significantly, revealing barren solonets soils called "syvashes" by locals.
The Syvash is sometimes divided into the Western Syvash and Eastern Syvash. These are connected to each other by the Chongar Strait.
Soviet soldiers crossing the Syvash during World War II.
- Baynes, T.S., ed. (1878). "Sea of Azoff". Encyclopædia Britannica. 3 (9th ed.). New York: Charles Scribner's Sons. p. 169.
- V. Siokhin; I. Chernichko; V. Kostyushyn; N. Krylov; Yu. Andrushchenko; T. Andrienko; Ya. Didukh; V. Kolomijchuk; L. Parkhisenko; R. Chernichko; T. Kirikova (2000). V. Siokhin; V. Kostyushyn, eds. Sivash: the lagoon between two seas (PDF). ISBN 9058829960.
Media related to Syvash at Wikimedia Commons