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Khvalynsky National Park : ウィキペディア英語版 | Khvalynsky National Park
Khvalynsky National Park (Russian: Хвалынский) encompasses a raised plateau of chalk hills of the Volga Uplands, covered in mixed oak-linden and conifer forests, along the west side of the Volga River. It is about 1,000 km north of the Caspian Sea, in Saratov Oblast overlooking the Saratov Reservoir. The northern end is about 10 km west of the city of Khvalynsk, and about 200 km northeast of Saratov on the Volga. About in size, Khvalynsky is spread over three sections. The park was officially formed in 1994. ==Topography== The park centers on the Khvalanskyaya ridge, a raised plateau that stretches along the west bank of the Volga River (referred to as the 'Right Bank'). Because the bedrock is primarily chalk and marl, the landform reflects extensive erosion out from the center of the ridge, with undulating and hilly terrain and numerous interconnected ravines and gullies. The varied landforms create many micro-climates and habitats. The highest mountain (Belenkaya, almost entirely of chalk) is 369 meters in altitude, and there are five other mountains over 250 meters in height. The mountains in the park are mostly covered with upland forest trees.〔 The Volga reaches its greatest depths (22 meters) in the territory of the park. Over 90% of the park is forest land. There are numerous outcrops of exposed bedrock, and underground water that frequently comes to the surface in springs. Habitats include pine and watershed forests, small rivers and hollows, and various types of forest edge and steppe.〔
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