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Levanna projectile points are stone projectile points manufactured by Native Americans what is now the Northeastern United States, generally in the time interval of 700-1350 AD. They are true arrowheads rather than atlatl dart points, and they derive their name from the specimens found at the Levanna site in Cayuga County, New York. [1]
The oldest projectile points found in North America were long thought to date from about 13,000 years ago, during the Paleo-Indian period, however recent evidence suggests that North American projectile points may date to as old as 15,500 years. [2] Some of the more famous Paleo-Indian types include Clovis, Folsom and Dalton points. [3]
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Susquehanna broad projectile point from central New York State. Made from rhyolite, probably quarried near Gettysburg, Pennsylvania.. Susquehanna broad projectile points are stone projectile points manufactured by Native Americans in what is now the Northeastern United States, generally in the time interval of 1200–700 BC.
Arrowheads are attached to arrow shafts to be shot from a bow; similar types of projectile points may be attached to a spear and "thrown" by means of an atlatl (spear thrower). The arrowhead or projectile point is the primary functional part of the arrow, and plays the largest role in determining its purpose. Some arrows may simply use a ...
A bodkin point arrowhead. A bodkin point is a type of arrowhead. In its simplest form it is an uncomplicated squared metal spike, and was used extensively during the Middle Ages. The typical bodkin was a square-section arrowhead, generally up to 11.5 cm (4.5 in) long and 1 cm (0.39 in) thick at its widest point, tapered down behind this initial ...
The Kansas City Chiefs plan to explore options that include leaving Arrowhead Stadium after voters in Jackson County, Missouri, soundly rejected a sales tax initiative that would have helped to ...
Examples of fluted and unfluted Dalton points. The Dalton tradition is a Late Paleo-Indian and Early Archaic projectile point tradition. These points appeared in most of southeast North America from c. 10,700 BCE to at least c. 8,400 BCE.