Title
Deciphering the Earliest Holocene: PostGlacial Landscape Evolution at Oneida Lake, New York,Used
Sold by Ergodebooks, an authorized reseller.
Returns accepted within 30 days | support@ergodebooks.com
Shipping Information
- Free Standard Shipping — United States only
- Processing Time: 1–3 business days
- Estimated Delivery: 3–5 business days after dispatch
- Double-boxed, fully insured & discreetly packaged
- Tracking number sent via email once dispatched
- Orders over $250 require signature upon delivery. Taxes calculated at checkout.
Returns & Refund
Returns accepted within 30 days of delivery.
Damaged or Defective Item
Free return shipping + replacement or full refund
Wrong Item Received
Free return shipping + replacement or full refund
Change of Mind
Return shipping at customer's expense · 25% restocking fee applies
Payment Option
Oneida Lake formed as a relict arm of glacial Lake Iroquois near the PleistoceneHolocene transition (138 ka). As the southeastern portion of the Lake Ontario Basin settled into its Holocene drainage patterns during the Younger Dryas period (1110 ka), Oneida Lake receded, leaving a series of exposed beach ridges on the southeastern lacustrine plain. The easternmost ridge of Oneida Lake, having been previously dated at 10.7 14C ka BP, marks the limit of the area under investigation; the western limit is the modern Oneida Lake shoreline ? Verona Beach. This demarcates a study area of 2.25 km2. With groundpenetrating radar, AMS shell dating, and sediment analysis I support the conclusion that the ancient beach deposits at Oneida Lake record earliest coastal development at Oneida Lake in the form of two consecutive series of beachridges representing (1) a cold, wet Younger Dryas phase and (2) a drier postYounger Dryas phase.
⚠️ WARNING (California Proposition 65):
This product may contain chemicals known to the State of California to cause cancer, birth defects, or other reproductive harm.
For more information, please visit www.P65Warnings.ca.gov.