Modeling Paleoshorelines and Locating Early Holocene Coastal Sites in Haida Gwaii

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Abstract
The integration of archaeology and paleoecology has allowed a fuller understanding of the history of southern Haida Gwaii and provided insights into the regional history of coastal occupation in northwestern North America. Of particular consequence is the history of sea-level fluctuations during the late-glacial and early Holocene. The modern shore holds only part of the history of coastal occupation. Much is flooded or hidden in the rainforest. In southern Haida Gwaii, shorelines dating from 13,000 to 9,500 B.P. are deeply drowned while those dating from 9,200 to 3,000 B.P. are stranded in the rainforest up to 15 meters above modern levels. Shorelines have been approximately coincident with the current position for only the last two to three millennia and for a century or two centered around 9,400 B.P. Modeling these paleoshorelines has led to discovery and investigation of a number of early Holocene archaeological sites.