4.7 Article

A sea-level database for the Pacific coast of central North America

Journal

QUATERNARY SCIENCE REVIEWS
Volume 113, Issue -, Pages 78-92

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.quascirev.2014.12.001

Keywords

Sea-level database; Cascadia subduction zone; Pacific North America; Glacial isostatic adjustment; Holocene

Funding

  1. NSF [EAR-1419844]
  2. BPH [EAR-1052848, EAR-1419824]
  3. REK [ARC-1203415]
  4. French government through the A*MIDEX project [ANR-11-LABX-0061, ANR-11-IDEX-0001-02]
  5. Earthquake Hazards Program of the U.S. Geological Survey (USGS)
  6. Division Of Earth Sciences
  7. Directorate For Geosciences [1419844, 1419366] Funding Source: National Science Foundation
  8. Division Of Earth Sciences
  9. Directorate For Geosciences [1419824] Funding Source: National Science Foundation
  10. Office of Polar Programs (OPP)
  11. Directorate For Geosciences [1203415] Funding Source: National Science Foundation

Ask authors/readers for more resources

A database of published and new relative sea-level (RSL) data for the past 16 ka constrains the sea-level histories of the Pacific coast of central North America (southern British Columbia to central California). Our reevaluation of the stratigraphic context and radiocarbon age of sea-level indicators from geological and archaeological investigations yields 600 sea-level index points and 241 sea-level limiting points. We subdivided the database into 12 regions based on the availability of data, tectonic setting, and distance from the former Cordilleran ice sheet. Most index (95%) and limiting points (54%) are <7 ka; older data come mainly from British Columbia and San Francisco Bay. The stratigraphic position of points was used as a first-order assessment of compaction. Formerly glaciated areas show variable RSL change; where data are present, highstands of RSL occur immediately post-deglaciation and in the mid to late Holocene. Sites at the periphery and distant to formerly glaciated areas demonstrate a continuous rise in RSL with a decreasing rate through time due to the collapse of the peripheral forebulge and the reduction in meltwater input during deglaciation. Late Holocene RSL change varies spatially from falling at 0.7 +/- 0.8 mm a(-1) in southern British Columbia to rising at 1.5 +/- 0.3 mm a(-1) in California. The different sea-level histories are an ongoing isostatic response to deglaciation of the Cordilleran and Laurentide Ice Sheets. (C) 2014 Elsevier Ltd. All rights reserved.

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