Jablonica quarry

The Jablonica deposit, which is made up of rocks from the Mesozoic period with Quaternary overburden, lies on the edge of the Little Carpathians. The area itself is highly rippled and marked by tectonic disturbances. Limestone alternates with clay and claystone overburden, and tectonic faults are also filled with clays, breccias, shales and loess.

We deliver quarried rock in both sorted and unsorted fractions, and as quarried rock with weights of up to and over 200 kg and fraction 63/180 mm quarried rock suitable for the construction of water works.