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Stara Planina ( Old Mountain ) is the main inspiration of the web site. Main characteristics of mountain Stara Planina you can find here. Stara Planina is almost five months under snow at an altitude above 1,700 m. Central annual air temperature at an altitude between 1,100 and 1,400 m is about 5 oC. Central winter air temperature range between -1 to -3 oC, a summer about 15 oC. After the Alps and Carphatian, Stara planina is the highest mountain range in Europe. Main Peaks on Stara planina are: Botev Peak 2,376 m (named after Hristo Botev), Vezhen Peak 2,198 m, Midzhur 2,169 m (the highest peak in Serbia and north-western Bulgaria, 12th in Stara Planina), Kom Peak 2,016 m, Todorini Kukli 1,785 m, Murgash 1,687 m, Shipka Peak 1,523 m, Buzludzha 1,441 m, Balgarka Peak 1,181 m and Levski Peak (named after Vasil Levski). The main potentionals of Stara Planina mountain are:
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The mountain Stara Planina can be divided into three sections:
The highest top in Serbian part of Stara planina is the Midžor 2,169 meters.
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Područje Stare planine karakteriše raznovrstan litološki sastav, predstavljen sedimentnim, manje magmatskim i metamorfnim stenama, od najstarijih, paleozojskih, preko mezozojskog flišnog i krečnjačkog kompleksa i neogenih jezerskih i marinskih sedimenata, do najmla|ih kvartarnih rečnih i bigrenih naslaga.
Posebno je značajna facijalna raznovrsnost mezozojskih sedimenata, sa punim stratigrafskim razvićem trijasa, jure i krede i obiljem fosila u stenama pojedinih odeljaka ovih perioda. Geostrukturna gra|a terena je veoma složena i izražena je kroz brojne i reprezentativne pojave rasedne i naborne tektonike. Po svojim stratigrafskim,
petrološkim, paleontološkim i geotektonskim odlikama Stara planina predstavlja izuzetnu riznicu " dokumenata "
o istoriji razvitka zemljine kore, složenosti geoloških procesa i promenama paleoekoloških uslova.
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