References in periodicals archive ?
the possibility of obtaining tax incentives and subventions for the implementation of priority investment projects for the region; openness and accessibility of information for the investor;proximity to Moscow as the largest consumer market (the region is located only 282 kilometers from Moscow); The Yaroslavl Region is located in the center of the East European Plain, bordering the Vladimir, Vologda, Ivanovo, Kostroma, Moscow and Tver regions
The region which is favorable for the latitudinal zonation of soils and vegetation study is the East European Plain (the area of which makes about 4 million km2): it includes 8 natural areas and more than 30 provinces within these areas.
In order to determine the dependence for all zonal soil types of the East European Plain of empirically determined humus horizon limit values from climatic potential, we summarized the data of numerous soil surveys.
This dependence was obtained for the flat part of the East European Plain [7]:
lim]) for region zonal soils are justified (for example, on the East European Plain they make at least 9 of the main soil types), the equation (4) may be graphically represented as a series of curves.
com was registered by Maxim Selikhanovich in Saransk, the capital city in Mordovia, a republic in the eastern region of the East European Plain of Russia.
About the current trend of erosion in the steppe and forest-steppe zone of the East European Plain // Geomorphology, 3: 39-43.
The evolution of terrestrial environments has been recorded in several complete reference sections in the glacial-periglacial and extraglacial zones of the East European Plain (Bolikhovskaya 1976, 1984, 1991a, 1991b, 1993, 1995, 2000; Bolikhovskaya & Sudakova 1996).
Therefore, loess-palaeosol sections of the southern and central parts of the East European Plain covering up to eight cycles can be regarded as unique and of special interest.
A comprehensive layer-by-layer spore-and-pollen study of the whole sequence represented in the reference sections permitted its detailed subdivision and reconstruction of the diversified environmental and climatic events in the centre and south of the East European Plain.
Periglacial forest-steppe and steppe prevailed in the southern part of the East European Plain beyond the limits of ice sheets.

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