Kumanovo valley – extends to the final northern part of the Republic of Macedonia. The boundary of the valley is most clearly expressed in the western, northwest and north side, where it leads to the Bill of Skopska Crna Gora (represented by its branch of Karadak), Ruen (775 m) and Kozjak (1,326 m), and more difficult can be followed Southeastern border to Ovce Pole. It is similar with the northern border where it cuts the Kumanovo-Preseva valley. It covers an area of 1,290,5 km², and small section 66,5 km² of the Republic of Serbia. The Kumanovo valley is characterized by a hilly-corrugated relief that has occurred with a slowdown of smaller river flows in the former central lake plane. In that sense, two morphrostructural units can be distinguished: mountain relief and valuable relief. The middle part extends Kumanovo field. In it, two morphological units are erupted: Zhengigovo West, Sredorek with Stracin in the East and CR-but the field, Nagorican Zazina, hot field and Rudo Field as smaller units. The bottom of the Kumanovo field is covered with neogene sediments. During Pliocene Yi part of the valley is busy with strong volcanic activity. Proof of this is the formation of the large basalt plate in the village. Nagorichani, the only one of this kind of the Balkan Peninsula. The valley feels changing-based and alternative influences. This allows the cultivation of garden crops, corn, framing plants, etc. The city settlement Kumanovo has been developed. Lit.: T. Andonovski, I. Milevski, geomorphological characteristics of the Kumanovo valley, “Geographic reviews”, kn. 36, Skopje, 2001. T. And.
Original article in Macedonian language Cyrillic alphabet
Кириличен напис КУМАНОВСКА КОТЛИНА