Binghamton University will conduct its 2007 Archaeological
Field School in the Hale Eddy Prehistoric Archaeological District (HEPAD).
The district is located along the West Branch of the Delaware River in the
Towns of Deposit and Hancock, Delaware County, New York. Over 22 prehistoric
sites, ranging from the late Paleo-Indian period to the Late Woodland period,
form the district and contribute to several research themes. This year's
field school will focus on two major themes: adaptations to the riverine
environment in the Late Archaic Period, and the local adaptation and occupation
by Paleo-Indian people.
From
the more than 22 sites in the HEPAD, the University has selected the Beaver
Lodge, Evans, and Delaware Pines sites as the focus of investigations for
the field school. Beaver Lodge represents a late Paleo-Indian camp. The
prehistoric assemblage consists of chipped stone debitage, utilized flakes,
projectile point fragments, bifacial and unifacial tools. The artifacts
are composed mainly of high-quality raw materials, mainly from the Normanskill
chert formations.
The
Delaware Pine site includes vertically stratified cultural deposits dating
to the Early Archaic, Late Archaic, Transitional, Middle Woodland, and Late
Woodland periods. Preliminary excavations recovered 5,188 prehistoric artifacts,
including chipped stone debitage, utilized flakes, bifacial tools, projectile
points and fragments, drill fragments, scrapers, pitted stones, and fire
cracked rock. Preliminary investigations at the Evans
Site indicate a horizontally stratified multicomponent site dating to the
Late PaleoIndian period. >>
From
the more than 22 sites in the HEPAD, the University has selected the Beaver
Lodge, Evans, and Delaware Pines sites as the focus of investigations for
the field school. Beaver Lodge represents a late Paleo-Indian camp. The
prehistoric assemblage consists of chipped stone debitage, utilized flakes,
projectile point fragments, bifacial and unifacial tools. The artifacts
are composed mainly of high-quality raw materials, mainly from the Normanskill
chert formations.
The
Delaware Pine site includes vertically stratified cultural deposits dating
to the Early Archaic, Late Archaic, Transitional, Middle Woodland, and Late
Woodland periods. Preliminary excavations recovered 5,188 prehistoric artifacts,
including chipped stone debitage, utilized flakes, bifacial tools, projectile
points and fragments, drill fragments, scrapers, pitted stones, and fire
cracked rock. Preliminary investigations at the Evans
Site indicate a horizontally stratified multicomponent site dating to the
Late PaleoIndian period. >> Read
the
research proposal.
Excavations
produced cortical and non-cortical flakes of Onondaga chert, jasper, and
unidentified cherts, pitted stones, dentate stamped pottery, projectile
points, fire cracked rock, biface fragments, scrapers, and a unifacial drill.
The latter was made from jasper and one projectile point was made from a
light tan stone of unidentified origin.
Of particular importance to the HEPAD research themes, the Evans site includes an "early Early Archaic" jasper workstation. This tightly bounded cluster includes a jasper uniface, which resembles artifacts from a deeply buried horizon at the Shawnee-Minisink site (McNett 1985). This horizon has not been dated, but lies above the Paleo-Indian horizon (ca. 8700 BC) and below the Early Archaic horizon (6900-5000). Other clusters on the site produced a Hardaway-Dalton point (Late Paleo-Indian/Early Archaic) and a Kirk Corner Notched point (Early Archaic), as well as several Lamoka points (Late Archaic), and Middle Woodland pottery.
research proposal.
Excavations
produced cortical and non-cortical flakes of Onondaga chert, jasper, and
unidentified cherts, pitted stones, dentate stamped pottery, projectile
points, fire cracked rock, biface fragments, scrapers, and a unifacial drill.
The latter was made from jasper and one projectile point was made from a
light tan stone of unidentified origin.Of particular importance to the HEPAD research themes, the Evans site includes an "early Early Archaic" jasper workstation. This tightly bounded cluster includes a jasper uniface, which resembles artifacts from a deeply buried horizon at the Shawnee-Minisink site (McNett 1985). This horizon has not been dated, but lies above the Paleo-Indian horizon (ca. 8700 BC) and below the Early Archaic horizon (6900-5000). Other clusters on the site produced a Hardaway-Dalton point (Late Paleo-Indian/Early Archaic) and a Kirk Corner Notched point (Early Archaic), as well as several Lamoka points (Late Archaic), and Middle Woodland pottery.


