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Untitled - the Digital Library of Georgia

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GEORGIA AND GEORGIANS 27<br />

<strong>the</strong> Town <strong>of</strong> Blakely, testify to <strong>the</strong> existence <strong>of</strong> this prehistoric race, giv<br />

ing us at <strong>the</strong> same time some <strong>of</strong> its peculiar habits and characteristics.<br />

Perhaps nowhere on <strong>the</strong> continent can <strong>the</strong>re be found today memorials<br />

<strong>of</strong> a more colossal character or <strong>of</strong> a more pr<strong>of</strong>ound interest to antiquar<br />

ians, telling <strong>of</strong> <strong>the</strong> former existence <strong>of</strong> this unknown race than we find in<br />

<strong>the</strong> famous monumental structures on <strong>the</strong> Etowah, some two miles distant<br />

from <strong>the</strong> present Town <strong>of</strong> Cartersville. These ancient relics <strong>of</strong> an un<br />

known race are located on what was formerly <strong>the</strong> property <strong>of</strong> Col. Lewis<br />

Tumlin. There are similar structures to be found in <strong>the</strong> Valley <strong>of</strong> <strong>the</strong><br />

Mississippi and along <strong>the</strong> Ohio and <strong>the</strong> Scioto rivers, but none to com<br />

pare in magnitude with <strong>the</strong>se splendid piles. Col. Charles C. Jones, Jr.,*<br />

who visited <strong>the</strong> locality some time in <strong>the</strong> '50s for <strong>the</strong> purpose <strong>of</strong> making<br />

scientific investigations, has put on record an exhaustive monograph,<br />

dealing with <strong>the</strong> subject from almost every point <strong>of</strong> view. Pie thus<br />

describes <strong>the</strong>se immemorial mounds:<br />

'' Situated upon <strong>the</strong> right bank <strong>of</strong> <strong>the</strong> Etowah River, in <strong>the</strong> midst <strong>of</strong> a<br />

perfectly alluvial bottom, <strong>the</strong>y tower above all surrounding objects,<br />

changeless amid <strong>the</strong> revolutions <strong>of</strong> centuries. They consist <strong>of</strong> a series <strong>of</strong><br />

mounds, surrounded by a large and deep moat—<strong>the</strong> traces <strong>of</strong> which are<br />

quite distinct; and, when filled with <strong>the</strong> tide <strong>of</strong> <strong>the</strong> river it effectually<br />

isolated <strong>the</strong> entire space included within its boundaries. The Etowah<br />

River here turns to <strong>the</strong> south; and, after a gentle sweep again recovers<br />

its wonted course, thus forming a graceful bend. This moat originally<br />

communicated at ei<strong>the</strong>r end with <strong>the</strong> river, a fact which is still apparent,<br />

although <strong>the</strong> current <strong>of</strong> <strong>the</strong> stream, in its flow <strong>of</strong> years, has filled to a<br />

very great extent, <strong>the</strong> mouths <strong>of</strong> <strong>the</strong> ditch, thus preventing <strong>the</strong> influx and<br />

reflux <strong>of</strong> <strong>the</strong> tide. Formerly <strong>the</strong> water must have coursed freely through<br />

it, thus isolating <strong>the</strong> entire space and constituting quite an obstacle in<br />

<strong>the</strong> path <strong>of</strong> an attacking foe. This ditch varies in depth and width; in<br />

some places possessing still a depth <strong>of</strong> twenty feet—in o<strong>the</strong>rs, <strong>of</strong> not more<br />

than eight or ten; and differing in width from fifteen to forty feet. North<br />

and west <strong>of</strong> <strong>the</strong> mounds situated within this enclosure, and along <strong>the</strong> line<br />

<strong>of</strong> <strong>the</strong> moat, are two excavations, each having at present a conjectured<br />

area <strong>of</strong> about an acre, and a depth <strong>of</strong> some twenty-five or thirty feet.<br />

With <strong>the</strong>se excavations <strong>the</strong> moat communicates directly, so that <strong>the</strong> same<br />

rising tide in <strong>the</strong> river, which flowed into <strong>the</strong> ditch, would also convert<br />

<strong>the</strong>m into deep ponds or huge reservoirs. The reason why <strong>the</strong>se excava<br />

tions were made is evident. The earth removed in constructing <strong>the</strong> moat<br />

was not sufficient to build even a moiety <strong>of</strong> <strong>the</strong> immense tumuli within <strong>the</strong><br />

enclosure. Hence' <strong>the</strong> Mound Builders were compelled to resort to <strong>the</strong>se<br />

enormous excavations, which still exist and will remain for ages yet to<br />

come. The space included within <strong>the</strong> limits <strong>of</strong> <strong>the</strong> moat is between forty<br />

and fifty acres. From <strong>the</strong> general appearance and nature <strong>of</strong> <strong>the</strong> works,<br />

we are induced to believe that <strong>the</strong>se excavations were designed to answer<br />

ano<strong>the</strong>r.purpose. They might have been, and probably were, intended<br />

as huge reservoirs, wherein a supply <strong>of</strong> water, sufficient to flood <strong>the</strong><br />

entire moat, might have been detained and preserved ready for an emer<br />

gency. The streams <strong>of</strong> this region, springing as <strong>the</strong>y do from hilly<br />

* '' Historical Btemains <strong>of</strong> <strong>Georgia</strong>,'' by Charles C. Jones, Jr., pp. 27-29, Savannah,<br />

1861.

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