Sinite Kamani Nature Park is situated in the Sliven Mountain subdivision of the Balkan Mountains, lying just north of the
Sliven Valley. The formation of the contemporary relief of the region began during the early
Neogene period. Due to the complex geological composition, the relief is highly dissected. Its lowest point is at an altitude of about 290 m; the highest point of is the summit of Bulgarka (1181 m), which is also the highest peak in the eastern Balkan Mountains. The elevation increases northwards, with the northern section of the park being the highest, where the main ridge of the Sliven Mountain is located. The northern slopes of the mountain are very steep and difficult to access, and are covered with extensive beech forests. The southern reaches of the park are occupied by ravines and crevices with sparse vegetation, represented mainly by individual trees. There are numerous caves, such as Zmeevi Dupki, Haydushkata Peshtera, Bachvata, Starite Dupki, etc. Sinite Kamani itself is the name of a rock massif located on the territory of the nature park, formed under the influence of erosion and denudation processes. The massif is made up mainly of quartz rocks with various impurities and contains various rock formations, shaped under the influence of erosion processes, forming, valleys, caves, ravines, etc. The massif, as well as the surrounding areas, are one of the main tourist sites in the area. Sinite Kamani Nature Park falls within the
temperate continental climatic zone with
Alpine influences at higher altitudes. The high areas have relatively low temperatures and high precipitation, while in the lower parts the temperatures are high and the precipitation is less abundant. The highest measured temperature is 41 °C, while the lowest is −20 °C. Snow cover lasts for about 3–4 months, with the earliest date for the appearance of permanent snow cover in the middle altitudes of the park being the beginning of November. The winds are predominantly northwesterly and northerly. The main types of soils in the nature park are brown forest soils and cinnamon forest soils. The cinnamon forest soils cover the lower parts of the nature park, at an altitude below 800 m; the main soil-forming rocks for are conglomerates, limestones, tuffs and others. The brown forest soils are located at higher altitudes, between 800–1200 m. Their predominant soil-forming rocks are sandstones, limestones and dolomites. == Biology ==