Monastery – Face of Travertine. It is located about 500 m southeast of the village. Monastery. The site is very specific, it is a pliocene sedimentary pool, in which in addition to the types of desk that occur in the form of plates with thickness and up to 10 meters, there are also deposits of diatomaceous country. Namely, it is about the variety of types of desalination, sands and silicles with a diatomaceous country, mostly white-gray, which is also a particular interest in eventual exploitation. The joint package of species desk, sands and diatomaceous country at the site monastery reaches power and up to 15 m. Travertors are of emphasized quality that is reflected through the cavity and medo-yellow color. Lit.: Todor Serafimovski, deposits of non-metal mineral raw materials, RGF, Stip, 2006. T. Sir.
Original article in Macedonian language Cyrillic alphabet
Кириличен напис МАНАСТИР