Mosaic of New Mexico's Scenery, Rocks, and History
History
Mosaic of New Mexico's Scenery, Rocks, and History
Geology -- New Mexico; New Mexico -- Description and travel; New Mexico -- History
The year 1926 was marked by the first of a series of important
archeological finds in New Mexico that were eventually to demonstrate
that man had occupied this area as much as 11,000 to 12,000 years ago.
During this period, Late Pleistocene ice sheets of continental glaciers
still blanketed parts of the northern tier of states in the vicinity of
the Great Lakes, and elephants (both mammoths and mastodons), horses,
camels, giant bison, tapirs, and ground sloths roamed the Southwest.
Excavations begun in 1926 near the small town of Folsom, in northeastern
New Mexico (fig. 1), disclosed a number of fossil skeletons of a large
form of extinct bison, forerunners of the modern bison or buffalo. Among
these bones were dart or spear points of distinctive form and
workmanship, characterized by broad, shallow flutes or channels on each
face (fig. 2). These artifacts, now known as Folsom points, have since
been recovered from a number of sites in New Mexico and elsewhere in
North America, commonly in association with the remains of extinct
bison. Evidently Folsom “Man” (whose skeletal remains have not been
discovered) was a nomadic hunter particularly dependent upon the bison
for his food supply, much as were the later Plains Indians of historic
time. Ages of from 10,000 to 11,000 years have been obtained from
charcoal and other organic remains at Folsom camp sites by the
radiocarbon method.
Succeeding years have seen an increasing number of valuable
archeological discoveries at camp and game-kill sites of Folsom Man and
other Early Hunters. Unquestionably, the most important of these sites
is the Blackwater Draw locality between Clovis and Portales in extreme
eastern New Mexico, where excavations for gravel disclosed a stratified
sequence of sediments that were deposited in an ancient pond and spring.
Here, too, were the characteristic Folsom points in association with the
bones of fossil bison. Below the Folsom layer, still older deposits
contained the fossil bones of mammoth, horse, camel, and bison
associated with fluted spear points that resembled those from Folsom but
were generally larger and less skillfully chipped and fluted. These
points, now known as Clovis points, are so commonly found beside the
remains of mammoths in a number of sites in the High Plains and the
Southwest that their makers are believed to have been adept at hunting
these extinct elephants. Radiocarbon dates place Clovis points in a time
range of from 11,000 to 12,000 years ago.
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