Berovo valley – The Berovo or Maleshevo valley extends in the final eastern part of the Republic of Macedonia, in the source of Bregalnica. It belongs to the oldest – Rhodopian land on the Balkan Peninsula. It is formed by radial tectonic movements during the Pliocene and is a southern tectonic part of the Berovo-Delcevan ditch. On three sides is enclosed with mountains: to the east with Mount Vlainina (Kadiica, 1,932 m), in the west Plachkovica (Lisec, 1,754 m and ointment, 1,181 m), and to the south are the Maleshevo Mountains (1,801 m). To the north with the choral Bejaz Tepe (1,348 m) is separated from the Delcevska valley. There is a meridian stretch of length of 20 km and a width of 10 km. The boiler bottom is at a height of 700 to Berovo 1,000 m, and the total area is 806 km². Due to the high altitude, a coniner climate is governed. Here, the lowest minimum temperature in the Republic of Macedonia -31 ° C is observed. Two city settlements were developed: Berovo and Pehcevo. Lit.: D. Manakovic, T. Andonovski, relief features of Eastern Macedonia, “Geographic reviews”, kn. 17, Skopje, 1979; A. Stojmilov, Physical Geography of R Macedonia, PMF, Skopje, 2003. T. And. Berovska, Lika Stojanova
Original article in Macedonian language Cyrillic alphabet
Кириличен напис БЕРОВСКА КОТЛИНА