Secţia de prelucrare a pietrei şi-a început activitatea in iulie  2007 cu sediul or. Soroca str. Feofania Budde, 8. Secţia  dispune   de utilaj italian  performant  firma “Pedrini” cu o capacitate de 250 metri  pătraţi de produse finite în schimb. Produsele din piatră au un nivel calitativ ridicat, fiind recunoscuta in România, Rusia. Gama produselor din piatra naturala este foarte larga, având capacitatea de a oferi clienţilor noştri soluţii complete pentru placări interioare si exterioare.

The Egoreni deposit is located 5km south of the village Cosauti and 1.5km north of the village Egoreni. The layer is narrow on the northern side and broad on the southern side, 370m long and 45m wide.
The deposit is a geomorphological part of the rippled Dniester plateau with absolute height in the range of 320 to 350m. The useful mineral component is the arcozoic grit stone and spatic quartz colored in grey and brown-yellow, very hard, mainly finely and medium granulated, containing large granulation portions on the bottom and the top region.
The grit stone layer 6.5 to 7.9m thick is intensely cracked both on horizontal and vertical direction. The horizontal fissures break the stone into pieces 0.1 to 1.0m thick, while the vertical cracks separate individual block. The upper grit stone layer with a thickness of 1.5 to 3.5m is extremely cracked and loose and it has stony texture.

The sand and gravel “Vasalcau” deposit, lentil shaped, 1650 long and 600 to 1300m wide, with an area of 14ha, is located between villages Trifauti and Vasalcau, in the Dniester valley. The useful mineral layer is composed mainly of sand and gravel 2.8 to 12.5m thick. The sand is grey-yellowish in color and it has fine to medium quartz granules. The gravel, of Carpathian type, is fine in structure and it has mixed pieces of flint, grit stone, jasper (matostat) and quartz. The overall gravel content varies between 2-3 to 54-60% of the deposit, with the larger percentage towards the bottom region.
The industrial reserves actually left in the deposit after previous extraction activity are about 10000 thousand m3, with a potential extraction volume of approximately 50000m3.
This deposit is a second group complexity geological structure.


The sand and gravel Slobozia-Cremene deposit is located 1km south west of Slobozia-Cremene village in Soroca County. The deposit is layered from south west towards north east 950m long and 140m wide. The useful mineral substance is composed of sand and gravel deposits between 1.5m and 11.7m thick. The sand is grey-yellowish in color, with fine and medium quartz particles and seldom clay granules. The gravel, of Carpathian type, is fine in structure and it is composed of mixed pieces of flint, grit stone, jasper and quartz. The gravel content varies between 2-3 and 54-60% of the overall deposit, with higher percentages located at the bottom.
This deposit is a second group in complexity of the geological structure.