Northwestern North America (7,821 – 6,094 …
Years: 7821BCE - 6094BCE
Northwestern North America (7,821 – 6,094 BCE) Early Holocene — Salmon Villages, River–Bay Networks, and Broad-Spectrum Foraging
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: Cook Inlet–Prince William Sound, Inside Passage & Haida Gwaii, Skeena–Stikine–Fraser tributaries, Columbia headwaters, Puget Sound.
Climate & Environmental Shifts
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Warmer, wetter Holocene onset stabilized salmon runs and expanded conifer forests; rising seas created drowned river-mouths.
Subsistence & Settlement
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Semi-sedentary salmon villages emerged at confluences and tidal flats; smokehouses and racks proliferated.
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Diets blended salmon, shellfish, marine mammals, deer/elk, waterfowl, berries, and nuts (acorn, hazelnut, camas).
Technology & Material Culture
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Weirs and basket traps; barbed fishhooks; ground-stone adzes for hollowing dugouts; net weights.
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Early shell middens formed along protected bays; dog companionship aided hauling and hunting.
Movement & Interaction Corridors
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Canoe trunklines along the Inside Passage; portage paths across low divides linked interior lakes to the coast.
Cultural & Symbolic Expressions
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First-salmon observances inferred from curated heads/bones and patterned discard; ochre graves with bead ornaments.
Environmental Adaptation & Resilience
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Storage + territorial rotation across river reaches buffered run variability; multi-habitat rounds sustained year-round security.
Transition
Toward 6,094 BCE, village permanence and complex salmon engineering set foundations for later ranked coastal households.
Groups
Topics
- Neolithic Revolution
- Boreal Period
- 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
