Skip to main content

Goebel, Ted

The early prehistory of the Susitna River region, near the place where three major rivers, the Susitna, Talkeetna, and the Chulitna, converge, provides important regional information about the movement of small-scale foraging societies in southcentral Alaska as well as specific data concerning lithic use. Since 2004, ongoing research at the Trapper Creek Overlook (TCO) and Susitna River Overlook (SRO) sites has revealed three primarily lithic artifact assemblages from stratigraphically sealed cultural occupations spanning the early to middle Holocene (ca. 10,000-5000 cal B.P.). Radiocarbon, tephrochronology, and optically stimulated luminescence (OSL) dating techniques provide context for interpreting these sites...
The early prehistory of the Susitna River region, near the place where three major rivers, the Susitna, Talkeetna, and the Chulitna, converge, provides important regional information about the movement of small-scale foraging societies in southcentral Alaska as well as specific data concerning lithic use. Since 2004, ongoing research at the Trapper Creek Overlook (TCO) and Susitna River Overlook (SRO) sites has revealed three primarily lithic artifact assemblages from stratigraphically sealed cultural occupations spanning the early to middle Holocene (ca. 10,000-5000 cal B.P.). Radiocarbon, tephrochronology, and optically stimulated luminescence (OSL) dating techniques provide context for interpreting these sites...
The early prehistory of the Susitna River region, near the place where three major rivers, the Susitna, Talkeetna, and the Chulitna, converge, provides important regional information about the movement of small-scale foraging societies in southcentral Alaska as well as specific data concerning lithic use. Since 2004, ongoing research at the Trapper Creek Overlook (TCO) and Susitna River Overlook (SRO) sites has revealed three primarily lithic artifact assemblages from stratigraphically sealed cultural occupations spanning the early to middle Holocene (ca. 10,000-5000 cal B.P.). Radiocarbon, tephrochronology, and optically stimulated luminescence (OSL) dating techniques provide context for interpreting these sites...
thumbnail
The early prehistory of the Susitna River region, near the place where three major rivers, the Susitna, Talkeetna, and the Chulitna, converge, provides important regional information about the movement of small-scale foraging societies in southcentral Alaska as well as specific data concerning lithic use. Since 2004, ongoing research at the Trapper Creek Overlook (TCO) and Susitna River Overlook (SRO) sites has revealed three primarily lithic artifact assemblages from stratigraphically sealed cultural occupations spanning the early to middle Holocene (ca. 10,000-5000 cal B.P.). Radiocarbon, tephrochronology, and optically stimulated luminescence (OSL) dating techniques provide context for interpreting these sites...
The early prehistory of the Susitna River region, near the place where three major rivers, the Susitna, Talkeetna, and the Chulitna, converge, provides important regional information about the movement of small-scale foraging societies in southcentral Alaska as well as specific data concerning lithic use. Since 2004, ongoing research at the Trapper Creek Overlook (TCO) and Susitna River Overlook (SRO) sites has revealed three primarily lithic artifact assemblages from stratigraphically sealed cultural occupations spanning the early to middle Holocene (ca. 10,000-5000 cal B.P.). Radiocarbon, tephrochronology, and optically stimulated luminescence (OSL) dating techniques provide context for interpreting these sites...
ScienceBase brings together the best information it can find about USGS researchers and offices to show connections to publications, projects, and data. We are still working to improve this process and information is by no means complete. If you don't see everything you know is associated with you, a colleague, or your office, please be patient while we work to connect the dots. Feel free to contact sciencebase@usgs.gov.