Description
Mountainous relief with steep slopes. Altitude's displacement within the park's territory is 1900 m. Four altitude belts are clearly distinguished, and the upper parts are habitats of alpine type. Old beech forests (40% of the park's territory) predominate in the forest belt. Dry heaths with predomination of the Siberian juniper (Juniperus sibirica) and mesophyllous meadows (40%, too) are dominant in the highlands zone. Northern slopes are covered with forests and the highest rainfalls in the country are given there (1200-1360 mm). Southern slopes are rocky, very steep, cut through by gorges.
Park's area is made up by magma plutonic bodies, sediment and metamorphous rocks of the Prepaleozoic, Mesozoic and Paleogenic age. Four denudation levels are observed in the park with various geomorphologic elements. These include flattened ridges, sloping steps, sloping declivities, granite over-thrusts and well expressed surface and underground limestone (karst) forms. Approximately one quarter of the forested area of the park is on granite rock. Next in distribution are the crystalline schists. Third is sandstone. The Stara Planina karst covers a small area of the park.
The site is with national, European and global significance for the preservation of examples of the Mixed Mountainous Systems with Complex Zoning Biome. 27 types and subtypes recognized in the park are natural habitats with European and national significance and they cover 94.7% of the park's territory. Fagus sylvatica forests take 40 % of it. They are distinguished for their high degree of naturalness, forests of between 100 and 250 years are prevailing.
Park's area is made up by magma plutonic bodies, sediment and metamorphous rocks of the Prepaleozoic, Mesozoic and Paleogenic age. Four denudation levels are observed in the park with various geomorphologic elements. These include flattened ridges, sloping steps, sloping declivities, granite over-thrusts and well expressed surface and underground limestone (karst) forms. Approximately one quarter of the forested area of the park is on granite rock. Next in distribution are the crystalline schists. Third is sandstone. The Stara Planina karst covers a small area of the park.
The site is with national, European and global significance for the preservation of examples of the Mixed Mountainous Systems with Complex Zoning Biome. 27 types and subtypes recognized in the park are natural habitats with European and national significance and they cover 94.7% of the park's territory. Fagus sylvatica forests take 40 % of it. They are distinguished for their high degree of naturalness, forests of between 100 and 250 years are prevailing.