Northwestern North America (4,365 – 2,638 BCE) …
Years: 4365BCE - 2638BCE
Northwestern North America (4,365 – 2,638 BCE) Late Holocene — Maritime Specialization, Estate Tenure, and Longhouse Emergence
Geographic and Environmental Context
Northwestern North America includes Alaska, western Canada (Alberta, British Columbia, Yukon and Northwest territory and Nunavut west of 110°W) Alaska, Washington State, northern Idaho, and the northwestern portions of Montana, Oregon, and California.
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Anchors: Outer Gulf of Alaska (Kodiak, Kenai), Haida Gwaii and Central Coast, Puget Sound inlets, Lower Columbia estuary.
Climate & Environmental Shifts
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Shorelines neared modern positions; stable estuaries and eelgrass meadows supported clams, herring, and salmon.
Subsistence & Settlement
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Shell-midden towns mark persistent occupation; weir estates and seal/sea-lion rookeries came under lineage control.
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Interior villages maintained pit-house traditions; cross-ecotone ties enhanced security.
Technology & Material Culture
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Plank-built canoes (mortise–tenon lashings, adze-finished strakes); robust net technologies; lamp–oil systems for winter light.
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Fine bone/antler harpoon heads, dentalium and shell beadwork as wealth items.
Movement & Interaction Corridors
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Inside Passage canoe highways; Fraser–Columbia trunk linked plateau lithics and furs to coastal oils and shell currency.
Cultural & Symbolic Expressions
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Lineage-ranking visible in burial goods and house platform size; ritual treatment of first salmon and sea mammals institutionalized.
Environmental Adaptation & Resilience
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Estate-based tenure and allied exchange networks buffered local failures; seasonal scheduling and storage maintained surpluses.
Transition
By 2,638 BCE, maritime societies with lineage estates and longhouse architecture were well established along many coasts.
Groups
- Paleo-Indians, or Paleoamericans
- Paleo-Arctic Tradition
- Athabaskans, or Dene, peoples
- Klamath (Amerind tribe)
Topics
- Neolithic Revolution
- Archaic Stage (Americas)
- Neolithic Subpluvial, or Holocene climatic optimum, or Holocene Wet Phase
- Atlantic Period during the Neolithic Subpluvial
- 8.2 kiloyear event during the Neolithic Subpluvial
- Chalcolithic Epoch, or Copper Ages
- Older Peron Transgression during the Neolithic Subpluvial
