Publication | Closed Access
10.1016/s0967-0653(97)88599-7
32
Citations
0
References
2000
Year
The Cape Espenberg beach ridge plain is capped by a succession of primary and secondary dune and/or blowout ridges whose 5000 yr chronostratigraphy is based on landform evolution, peat formation, pedogenesis, tephro-chronology, and geological (n = 23) and archaeological (n = 32) radiocarbon ages. Landform evolution reflects several sets of conditions: beach ridges form under fair weather wave climates and/or following subsiding storm levels, dunes build in fall and winter in conjunct ion with onshore N or NW winds, while net offshore sediment transport and erosion predominates during fall storms. Inter-ridge swales foster peat and paIsa growth atop driftwood in conjunction with thin snow cover. Dunes built during stormy intervals correlative with montane Alaska glacial expansions 3300 - 1700 14 C yrs BP and from 1200-200 14 C yrs BP.