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STOP! - Arrowhead Collecting On The Web

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ACOTW<br />

<strong>Arrowhead</strong> <strong>Collecting</strong> <strong>On</strong> <strong>The</strong> <strong>Web</strong><br />

<strong>Arrowhead</strong> <strong>Collecting</strong> <strong>On</strong> <strong>The</strong> <strong>Web</strong><br />

TM<br />

How Can We Tell <strong>The</strong> Difference Between An Ancient <strong>Arrowhead</strong><br />

And A Modern-Made Reproduction Point? Let’s Take A<br />

Look At Some Of Each Side By Side And Note <strong>The</strong> Differences.<br />

<strong>The</strong>se two points are magnified<br />

about six times their actual size, so<br />

that we can look closely at a few<br />

details which can help us note age<br />

and authenticity.<br />

<strong>The</strong> first thing which we can<br />

observe is the surface of the stone<br />

from which each point is knapped.<br />

<strong>The</strong> agate point on the left has a<br />

surface patination wich makes it<br />

appear aged. It has changed color<br />

from exposure, since we can see<br />

the true color of the stone at the<br />

very tip of the point, where there<br />

has been a tiny break. <strong>The</strong> tip was<br />

split when found. A remaining<br />

portion came off after the point<br />

was found by the author in 1963<br />

or 1964 in western Oregon.<br />

<strong>The</strong> Texas flint arrowhead on the<br />

right shows a number of thin,<br />

clear hinge pieces still holding on<br />

at the end of the pressure flake<br />

scars. In an ancient point most of<br />

these would have fallen off due to<br />

uncounted freeze/thaw cycles.<br />

Any remaining hinge flakes<br />

would also have soil or mineral<br />

deposits accumulating at the<br />

hinge line, in the notches and even<br />

under the remaining flake ends, as<br />

with the agate point. This point<br />

was made in 2009 by the author.<br />

Volume I, Number 7 10<br />

November 2009

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