2015년 5월 27일 수요일

Ocmulgee National Monument 2

Ocmulgee National Monument 2


Another peculiar condition in this region at this time was the presence
of considerable areas untouched by glacial ice. These included the
foothills and coastal plain along Alaska's northern coast as well as the
great central Yukon Valley. This surprising situation was probably due
to the small amount of moisture left in the winds which had passed over
the high and cold mountain chains bordering the southern coast and the
second great mass of the Brooks Range to the north. Furthermore, the
broad Mackenzie Valley, leading south along the eastern slopes of the
Rockies, was the area latest to be covered by glacial ice and first to
open up with the return of warmer conditions. It may even be that the
ice failed to cover this region during the last one or more of the minor
advances which together make up the latest, or Wisconsin, glacial
period.
 
Taken all together, therefore, the conditions described provided man
with a chilly but relatively dry and passable route from the Asiatic
mainland to Alaska and thence to the warmer interior sections of North
America. For a considerable period this route must have been flanked
with glacial ice lying only a few miles away on one side or both through
a total distance of some 2,000 miles. It is one of man's distinctive
qualities, however, that he is able to adapt himself to extremes; and it
is probable that the game he lived on was itself acclimated to living
close to the edges of the ice sheets. We are less certain about the
conditions under which this journey was begun at its Asiatic end; but it
seems likely that there, too, ice would have formed in the high mountain
masses, but that the valleys and lowland would have remained open as
they did farther east.
 
We are confident in our knowledge of where man came from to the New
World and how he was able to make the trip. We are on less certain
ground, however, when we try to determine when he arrived. Estimates
have varied widely, changing with every increase in our knowledge. From
the first enthusiastic attempts to fit the Indian into the Old Stone Age
chronology which was just then unfolding for the Old World, the cold
reasoning of skeptical scientists brought down the maximum age of human
occupation of this hemisphere to something like 3,000 years. Beginning
in 1925, however, a series of finds has provided unquestionable evidence
that men using very distinctive weapons were living on this continent,
largely by hunting the mammoth and a great bison, both now extinct,
during the period when the ice was receding for the last time. The
typical channeled or fluted spear point of this people has even been
found lately along the northern Alaska coast. So, while we still cannot
say that this characteristic artifact was brought from Asia rather than
being developed here in America, it is at least an interesting
coincidence that man hunted large and now extinct game in Alaska in
areas where conditions were at times particularly well suited to his
immigration.
 
Other evidence shows that the users of this telltale point were not the
first to live in the region of the western plains; at least some of
their numbers had been preceded by men whose stone work was almost as
unusual and equally easy to identify. Recently developed methods of
dating by the use of radioactive carbon-14 show that the span of time
when the channeled point users, Folsom man, roamed the Plains included
one date of about 8000 B. C. For his predecessors, we feel justified in
pushing this date a good 2,000 or 3,000 years further back; and there
are even hints taken quite seriously by leading archeologists that man
was here many thousands of years before that. We know that the great
climatic swings marking the principal stages of the Pleistocene Epoch
were actually composed of repeated lesser pulsations. Like a mighty
pump, the changing climate worked upon all life within thousands of
miles of the shifting ice fronts, driving it southward with icy winds
and then sucking it back toward the north as cold and damp were replaced
by heat and drought. Man followed the game; and this, rather than any
planned migration, probably accounts for the wide spread of his earliest
remains.
 
American Indians, then, are most closely related to the present
inhabitants of eastern Asia, where they, too, had their origin. They
came to this country as its first human inhabitants some 12,000 to
15,000 years ago at the very least. They did not come all at once, or
even in one limited period of time, but probably in a fairly continuous
succession of small hunting bands following the game. Their earliest
migrations hither were doubtless the indirect result of great
fluctuations in climate which marked the coming and going of the ice
during the glacial age; and it was the peculiar conditions existing
about the present region of Bering Strait that encouraged them to
explore the now accessible region to the east. Once they had reached the
New World, their hunting travels probably carried them back and forth in
both directions so that a knowledge of the seemingly limitless territory
beyond became fairly general.
 
[Illustration: Broken Clovis point and sharp-cornered scrapers from
Ocmulgee excavations. Point length 3^1^1/_1_{6} inches. Artist's
reconstruction of point at left.]
 
The disappearance of the land bridge must have been very gradual by
human standards. Successive generations would have found the journey
increasingly difficult, but this would only have led to the adoption of
other measures such as waiting for winter ice or the use of rafts or
boats to cross the widening stretches of open water. Once arrived, they
began to spread out over the country, moving on as the game became
scarce to where it was more abundant, looking for new and unpeopled
areas whenever they began to catch sight too often of members of other
bands hunting the same territory. Not many years would be needed to
cover the vast expanse of the two continents. With movements of only 20
or 30 miles each year, it might have happened in as little as a dozen
generations; but we can say for sure that man had reached southern
Patagonia by about 6000 B. C., possibly far earlier. By then, we may
assume, the new homeland had been explored with some thoroughness; and
portions of it had already been inhabited for thousands of years. It was
by no means filled up; but many of its potentialities were known, and
American Indians were well started on their own peculiar course of
development.
 
 
 
 
Man Comes to Georgia
 
 
The roving existence led by these _Wandering Hunters_ brought them into
the region which is now Georgia at a relatively early date. We do not
know by what route they came here, for it is easier to seek out the
geographic limitations which restricted the first migrants to the New
World to a single point of entry than it is to trace the wanderings of
their descendants over some 8,000,000 square miles of North America.
Nevertheless, we are beginning to get a few hints.
 
[Illustration: Mammoth Hunters, from Museum exhibit panel.]
 
Fluted point sites have been found in Massachusetts, Pennsylvania, and
Virginia; and single fluted points have been found in a number of places
in Georgia, though possibly more often north than south of Macon. One
fluted specimen, however, was actually excavated from the Macon Plateau,
a designation adopted for the hilltop terrain of the Ocmulgee
excavations. The recovery here of other tools of the same greatly
decomposed flint strengthens the likelihood of a true "paleo-Indian"
occupation at Ocmulgee. The inclusion among them of many thumbnail
scrapers of a type recently shown to be distinctive of eastern fluted
point sites is especially significant.
 
The fluted point, missing the forward one-third of its length, was a
fine specimen of the so-called Clovis type of these artifacts, and so
typical of thousands of such implements which have been picked up at
random in the eastern United States as well as in the West. The Clovis
point is like its Folsom cousin in several ways, particularly in having
a long channel flake removed from one or both of its faces, possibly as
a means of reducing its total thickness, and in the grinding of the edge
along the lower sides and across the base to avoid cutting the lashings
which bound it to the shaft. Like the smaller Folsom point, too, it is
named for a site in the western High Plains, where its position
underlying Folsom on some sites and its association with mammoth bones
give us definite clues to its age west of the Mississippi.
 
Unlike Folsom, however, the Clovis fluted point is not limited to the
region on the east flank of the Rockies. Instead, it has been found from
Alaska to Costa Rica and from Vermont to Florida. Its use, too, seems to
have been less specialized. Folsom man was a bison hunter; and the
abundant grasses of the Plains probably account for the rather definite
limits of his range. The big Clovis points, on the other hand, were
certainly used on mammoth; but we do not know that this over-sized
quarry was their only target. Possibly the mammoth was more adaptable
than the bison and could seek out other areas as the changing climate
made its accustomed haunts unlivable; or it may have been the Clovis
hunters who were the more flexible and could shift more readily to other
kinds of game when the mammoth disappeared from the scene.
 
[Illustration: Hunting was hard work. Museum exhibit case.]
 
The wide geographic range of the point is matched by the variety of
shapes which are included in the type, though all have a family
resemblance built around the distinctive channel formed on one or both
faces. Until it is found in a context permitting direct dating, however,
the real problem in the East hinges on the significance of this family
resemblance. The question is whether this resemblance is a result of
chance, or whether it indicates contact with the makers of the fluted
points in the West whose age is now reasonably well established.
 
[Illustration: Hunter with atlatl (throwing stick).]
 
Perhaps the only thing we can say definitely about these early nomadic
hunters would be that their unusual fluted type of projectile point
occurs in the eastern United States and has been found in clearly
defined contexts which suggest a greater age than that known for any
other recognized types in these areas. This distinctive weapon is
thought to be a variety of the western Clovis fluted point, which has
been found in the West beneath Folsom, and therefore antedating 8000 B.C.

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