The Westerwald clays were formed by weathering of the approximately 400 million‒year‒old Slate Mountains of the Rhine. However, the actual deposition of the clays took place much later, mainly in the Tertiary Period about 15 to 30 million years ago. At this time, the weathered rock components were transported by water and deposited in depressions in the landscape.
Many Westerwald clays originate from secondary deposits. After weathering, they were relocated, which is why they are particularly homogeneous and have high‒quality ceramic properties. Clays that are found at the original site of weathering, and show traces of the old weathering crust of the Rhine Slate Mountains, are referred to as primary deposits.
One such primary deposit is our Mehl clay quarry in Nentershausen. The soft shale clays extracted there correspond to rarer clay deposits and have special properties making them interesting for numerous ceramic applications.