XXXIII.

From beneath the eastern aspect of the mountains of Alabama, a broad belt of metamorphic rocks bursts forth, and trends to the north-eastward, following the mountain ranges in almost parallel lines through the States of Georgia, South and North Carolina, and disappearing in Virginia beneath the waters of the Potomac. These lands of decomposed mica and talcose schists contain throughout their broad extent particles of gold; and some of the narrow and circumscribed fields are unsurpassed in their undeveloped richness by any of the known gold fields of similar extent in the world. These auriferous soils, owned or controlled by the slaveholder, have yielded, by the superficial scratchings and washings of the slave and the poor white, during the period since the discovery of the precious metal, about forty millions of dollars. There are not less than one hundred millions more within the reach and grasp of skilled and determined labor.

Along beside, and traversing through and through these golden rocks and sands, occur immense bands of itacolumite, known, from its flexibility, as the elastic sandstone. They stretch from Alabama to the interior of North Carolina, bursting forth now as great flexible bands of stone, and then bulging out as entire mountains. This singular formation is the same that has been recognized in Brazil, Ural Mountains, and Hindostan, as the matrix of the diamond; and here, nearly one hundred of the precious gems of fine water have been picked up from the earth, from time to time, by the careless observer.