tailieunhanh - The Aral Sea Encyclopedia - L,M,N

L Land reclamation and water management (formerly ‘‘Hydraulic Construction and Land Reclamation’’) – the monthly scientific-production journal of the USSR Ministry of Agriculture (later, the theoretical and scientific-practical journal of the USSR Ministries of Agriculture and of Water Management). It was founded in April 1949. Its first editor-in-chief was . Shubladze, then after 1952 . Shklyarevsky, then from 1971 . Nesterov. The journal highlighted the problems of land reclamation and water management in the Central Asian countries. Some issues were devoted to the Aral problems (No. 1, 2002). Large (Aral) Sea* – this is the name of the part of | L Land reclamation and water management formerly Hydraulic Construction and Land Reclamation - the monthly scientific-production journal of the USSR Ministry of Agriculture later the theoretical and scientific-practical journal of the USSR Ministries of Agriculture and of Water Management . It was founded in April 1949. Its first editor-in-chief was . Shubladze then after 1952 . Shklyarevsky then from 1971 . Nesterov. The journal highlighted the problems of land reclamation and water management in the Central Asian countries. Some issues were devoted to the Aral problems No. 1 2002 . Large Aral Sea - this is the name of the part of . located to the south of the largest Kokaral Island see formed as a result of the . drying and its division into the Large and Small . By hydrological characteristics its depths bottom relief and water dynamics can be divided into 2 parts - eastern and western - separated from each other by an underwater ridge that stretches from the Tokmak-Aty Island via the Lazareva Island see the Bellinsgauzen Bank Konstantin Island Vozrozhdenia Island and extending finally out to the western part of the Kulandy Peninsula. This underwater ridge which by 1990 has emerged from the receding water is known as the tectonic Arkhangelsky Rampart see . To the west of this underwater ridge an area of small depths is found that extends strip-like along the Ustyurt chink see . The maximum depth about 69 m was revealed by see near the western shore in a narrow trough between the Aktumsyk Cape in the south and the Baigubekmuryn in the north . In general depths over 60 m composes only of the whole sea area. An area with depths 30-60 m composes about 4 of the water area and extends as a narrow strip 22 km wide for 185 km along the western coast. The central part of the sea represents a rather flat plateau with depths varying from 20 to 28 m 1960 . The eastern part of the sea to the east of the underwater ridge is composed of a .