Modern fan deltas from the Gulf of California are common along the high-rel
ief cliffed peninsular margin. Most of the fan deltas are wave dominated, a
ffected also by the longshore drift. Human impact on these fan deltas is mi
nimal. Thus, El Coyote is an example useful for obtaining a better understa
nding of fan delta depositional systems in the stratigraphic record. Local
rapid changes reflect the interaction of short-term summer flash floods and
wave energy which rapidly removes the evidence of high discharges. The Baj
a California peninsula has been relatively stable, at least in the last few
hundred thousand years, with an uplift rate of 100 mm/ka. Thus, changes in
sea level and climate have been recorded on the fan delta as: (1) Pleistoc
ene marine and fluvial terraces (possible stages 5e or 5c), (2) erosion of
the subaerial portion due to lowering of sea level from a + 1 to 1.5 high s
ea-level standard in the last 6000 years and a decrease in the rate of sedi
ment discharge, and (3) the submerged fan form at a water depth of 40 m rel
ated to the high sea-level stands of stages 2 (28 ka) and 3 (40-45 ka). (C)
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