Greywacke is a gray to green-gray rock consisting mainly of sandstone with a high proportion of feldspar and matrix. The term "Grauwacke" originates from the miners' language of the Harz region and is usually used for rocks belonging to the Paleozoic or an older geological period.
Grauwacke was formed primarily as marine, clastic sedimentary rocks in sedimentary basins that preceded the precursors of folded mountains. The parent material was transported to the sea by rivers and deposited on the continental shelf. Geological processes such as instability of the deposits and folding of the rock formed thick graywacke beds.
The composition of graywacke varies, but it usually contains a high proportion of quartz and feldspar. Other constituents include clay minerals such as chlorite and mica, and occasionally carbonates. The grains in graywacke are usually poorly rounded, and the matrix consists of a fine-grained groundmass in which the rock fragments and mineral grains are embedded.
Graywacke can have different colors, from light to dark gray, brown-gray or green-gray, depending on the chemical composition of the mixture particles and the mineral stock. Accurately distinguishing graywacke from other rock types such as arkose can be difficult. One main distinguishing characteristic is the clay minerals in the matrix. Graywacke contains mainly chlorite and mica, while arkoses contain mainly kaolinite.
Graywacke occurs in various regions, especially in Central Europe. In Germany, graywacke is found in the old rump mountains such as the Harz, the Rhenish Slate Mountains and the Thuringian Slate Mountains. In the Alps, graywacke occurs as a narrow strip north of the central Alps in the so-called graywacke zone. It should be noted, however, that not all sandstones in these areas are classified as graywacke.
Because of its properties and hardness, graywacke has many uses. It is often used as paving stone, ballast material, and railroad track superstructure material. In addition, graywacke is also used as masonry stone.