Common Rocks of the Georgia Piedmont and Blue Ridge
The Piedmont and Blue Ridge are composed of an agglomeration of pieces of the ancient North American continent, island arcs, oceanic crust, and scraps of old continents that were repeatedly metamorphosed, folded, faulted and welded together during collisions between North America, Africa, and smaller pieces of the earth's crust. Huge mountains, the ancient Appalachians, were formed during this process. They have weathered into the rounded ridges we see today. The most common rocks are described below.
Plant Communities and Rock Type
Different plant communities evolve to survive in different moisture and nutrient conditions created by the weathering of different rock types.
Some rocks weather into moreacidic soils, often encouraging plants of the Ericaceae family, which includes azaleas, mountain laurel, rhododendrons and sourwood.
Some rock types contain more nutrients, such as potassium and calcium, enabling a more diverse array of plants. There are many "indicator species" that, when seen in abundance on the landscape, will indicate more bases (calcium and/or magnesium) in the soil. These include redbud, eastern red cedar, and white ash; many others are described under particular natural communities.
In some cases, base-rich soils can weather to very clayey soils that drain poorly, but more often in the Georgia Piedmont, the bases are mixed with organic materials and other minerals to create more congenial conditions.
Metamorphic Rocks: form when any type of rock is compressed and heated, and so re-crystallize, usually during mountain building events when continents collide. Mafic metamorphic rocks have high levels of magnesium and iron, and often abundant potassium and calcium. Felsic rocks are usually less fertile
Quartzite: composed of quartz, usually from metamorphosed sandstone. Erodes to sterile, sandy soils that encourage many acid-loving plants.
Schist: any metamorphic rock in which the mineral grains align in one direction. Most often felsic, composed of mica and quartz, forming infertile soils that favor acid-loving plants.
Gneiss: any metamorphic rock with bands of different mineral composition, usually bands of light-colored quartz and feldspar (felsic) minerals alternating with dark-colored bands of black mica (biotite) and are non-mafic, with modest fertility. Some gneiss in Georgia, although unusual, contains the mineral hornblende, which is mafic and will support a higher diversity of species than biotitie gneiss.
Amphibolite: a mafic, black rock (that will weather to a red surface and bright orange soils) composed of hornblende, which contains varying proportions of potassium, sodium, calcium, magnesium, and iron. Amphibolite weathers to fertile soils and supports diverse plant communities.
Marble: forms from metamorphosed limestone (calcium-carbonate). Soils derived from marble are rich in calcium and host special plant communities - even thin beds of marble can create diverse communities. It is sparsely scattered in the the Georgia Piedmont and Blue Ridge.
Igneous Rocks: form when magma (molten rock) slowly cools and solidifies within the earth's crust, or rapidly "freezes" when it is extruded as lava and ash at the earth's surface.
Granite: a felsic rock made up of quartz and feldspars. Modest fertility, with some calcium and potassium contained in the feldspars and minor minerals in the granite.