Produced by Donald R. Privett, Ph.D.- P.G. Environmental and Engineering Geologist Lower Catawba River Valley of Southern Chester and Lancaster Counties, S.C. - Geology - Archeology and History Part 1
Disrupted mafic dike (dark rock) OR mafic schlerien cutting the metagranite .
PURPOSE OF THIS PRODUCTION: 1. Provide an introduction to the general geology and geomorphology of the lower Catawba River Valley. 2. Show the areas natural history. 3. Summarize the understanding of the area geologic and human history. 4. Introduce the recreational opportunities of the area.
The Catawba River heads in the Blue Ridge Mountains as brook cascading high off the eastern slope of Chestnut Ridge in the Swannanoa Mountains near Old Fort, North Carolina. Collecting tributaries and picking up power on steep slopes it tumbles over falls and rapids and onto a broad valley flowing east for 120 km. It then makes two angular turns to flow south into South Carolina and into the Atlantic Ocean.
South Carolina consists of three distinct geologic regions, from northwest to southeast, they are 1. Blue Ridge 2. Piedmont and 3. Coastal Plain. Great Falls is located in the Piedmont more specifically in the Carolina terrane and at the boundary between the Carolina Slate belt and The Charlotte belt. The area is underlain by massive crystalline rocks, both metamorphic and igneous.
Among the igneous are granites, diorites, and diabase. The metamorphic rocks consist of gneiss, schists, phyllites, meta-sediments, and meta-volcanics. The Piedmont Province is the non-mountainous portion of the older Appalachians. Its surface is the result of eons of weathering.
<ul><li>Area Geomorphology </li></ul><ul><li>The river has cut a deep valley through granite, exposing bedrock. </li></ul><ul><li>Estimated down cutting occurred at rate of less than 1” per 100 years or at one hair width a year. 1’ per 1200 years, 10’ per 12,000 or 100’ per 120,000 years. </li></ul><ul><li>Hard bedrock resists erosion and produces waterfalls and shoals. </li></ul><ul><li>Evidence for the geologic history is found in the rocks. </li></ul>
<ul><li>Geology </li></ul><ul><li>The Great Falls Metagranite is the most common rock type in the area. </li></ul><ul><li>It is a circular, 40 square mile, 543 million year old +/- 63 million years, altered granite. It is composed of quartz, feldspar and mica. </li></ul><ul><li>Is one of the oldest igneous rocks in the Carolina Terrane part of the piedmont. </li></ul>
Part of the Great Falls 7.5 °Quadrangle Long channel Short or steep Great Falls channel
Gradient of the Catawba River, note steep slope at Great Falls .
Topographic profile. Duke Energy Drawing 1. Nitrolee 2. Great Falls Projections looking north
1879 map showing the correct location of the Great Falls of the Catwba. the Great Falls
Looking South Catawba River Valley Below the Great Falls.
Looking south -Catawba River Valley below the Great Falls.
<ul><ul><li>Potholes are : </li></ul></ul><ul><ul><li>1. abundant in the exposed rocks at the base of the Great Falls cascades (below the spillway dam of the Dearborn reservoir). </li></ul></ul><ul><ul><li>2. 25- 40-cm. wide and 30 cm. deep. </li></ul></ul><ul><ul><li>Bedrock is fluted and has been polished smooth by water flow and suspended sediments. </li></ul></ul>
Pothole in Granite. Potholes form over thousands of years by the scouring action of pebbles and cobbles caught in a depression and swirled by water.