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.


