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List Of Ramsar Wetlands Of International Importance
Ramsar sites are protected under by the Ramsar Convention, an international treaty for the conservation and sustainable use of wetlands, recognizing the fundamental ecological functions of wetlands and their economic, cultural, scientific, and recreational value. The convention establishes that "wetlands should be selected for the list on account of their international significance in terms of ecology, botany, zoology, limnology or hydrology." Over the years, the Conference of the Contracting Parties has adopted more specific criteria interpreting the convention text. The Ramsar List organizes the Ramsar sites according to the contracting party that designated each to the list. Contracting parties are grouped into six "regions": Africa, Asia, Europe, Latin American and the Caribbean, North America, and Oceania. , 171 states have acceded to the convention and designated 2,531 sites to the list, covering ; one other state has acceded to the convention but has yet to designate any s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ramsar Site
A Ramsar site is a wetland site designated to be of international importance under the Ramsar Convention,8 ha (O) *** Permanent 8 ha (P) *** Seasonal Intermittent < 8 ha(Ts) ** es on inorganic soils: *** Permanent (herb dominated) (Tp) *** Permanent / Seasonal / Intermittent (shrub dominated)(W) *** Permanent / Seasonal / Intermittent (tree dominated) (Xf) *** Seasonal/intermittent (herb dominated) (Ts) ** Marshes on soils: *** Permanent (non-forested)(U) *** Permanent (forested)(Xp) ** Marshes on inorganic or peat soils: *** Marshes on inorganic or peat soils / High altitude (alpine) (Va) *** Marshes on inorganic or peat soils / Tundra (Vt) * Saline, [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chott De Zehrez Chergui
In geology, a chott, shott, or shatt (; ) is a salt lake in Africa's Maghreb that stays dry for much of the year but receives some water in the winter. The elevation of a chott surface is controlled by the position of the water table and capillary fringe, with sediment deflation occurring when the water table falls and sediment accumulation occurring when the water table rises.Swezey, C.S., 2003, The role of climate in the creation and destruction of continental stratigraphic records: An example from the northern margin of the Sahara Desert, in Cecil, C.B., and Edgar, N.T., eds., Climate Controls on Stratigraphy: SEPM (Society for Sedimentary Geology) Special Publication 77, p. 207-225. They are formed—within variable shores—by the spring thaw from the Atlas mountain range, along with occasional rainwater or groundwater sources in the Sahara, such as the Bas Saharan Basin. Water sources The chotts of the Sahara are fed intermittently during periods of infrequent rainfa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chott Tinsilt
Chott Tinsilt is a saline lake situated within the High Plateau Wetlands, located in the Oum El Bouaghi Province.The site was designated as a Ramsar Convention, Ramsar site on December 12, 2004. Its administration is overseen by the Forestry Governorate of Ouled Zouaï, Ouled Zouai, the Directorate of Water Resources, and the Regional Environment Inspectorate. Geography Topography and hydrography Chott Tinsilt is situated in the northern sector of the Ouled Zouaï, Ouled Zouai Plain, bordered by hills. The majority of Chott Tinsilt is sustained by precipitation from the Wadi Ben Zerhaib. Additionally, sewage from the Souk Naamane is discharged into the north-west side in small quantities. The water outlet is situated on the south-western side of the site and traverses the area until it reaches the Sabkhet Al-Zamoul. Chott Tinsilt has a catchment area of 10,300 ha, with a maximum depth of approximately half a metre. Location Chott Tinsilt is a shared resource between t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chott Sidi Slimane
In geology, a chott, shott, or shatt (; ) is a salt lake in Africa's Maghreb that stays dry for much of the year but receives some water in the winter. The elevation of a chott surface is controlled by the position of the water table and capillary fringe, with sediment deflation occurring when the water table falls and sediment accumulation occurring when the water table rises.Swezey, C.S., 2003, The role of climate in the creation and destruction of continental stratigraphic records: An example from the northern margin of the Sahara Desert, in Cecil, C.B., and Edgar, N.T., eds., Climate Controls on Stratigraphy: SEPM (Society for Sedimentary Geology) Special Publication 77, p. 207-225. They are formed—within variable shores—by the spring thaw from the Atlas mountain range, along with occasional rainwater or groundwater sources in the Sahara, such as the Bas Saharan Basin. Water sources The chotts of the Sahara are fed intermittently during periods of infrequent rainfa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chott Melghir
Chott Melrhir, () also known as Chott Melghir or Chott Melhir, is an endorheic chott-kind of salt lake in northeastern Algeria. It is the westernmost part of a series of depressions which extend from the Gulf of Gabès into the Sahara. It was formerly known as Lake Tritonis. They were created between Miocene and Early Pleistocene as a result of compression accompanying the formation of the Atlas Mountains. With the maximum area of about , it is the largest lake in Algeria.В. М. Котляко�Мельгир (Chott Melrhir) Словарь современных географических названий (Dictionary of modern geographical names), 2003–2006 It lies almost entirely below sea level and contains the lowest point in Algeria, . Its size varies over the year and is usually larger than from east to west.Chott Melrhir [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
