The Eemian - age chevron beach structures with consistent southwesterly direction throughout windward shores in the Bahamas, with
wave runup deposits at elevations as much as 20 — 40 m above today's sea level and reaching as far as a few kilometers inland, must have been formed by massive storms in the direction of the prevailing winds.
Not exact matches
While perhaps more mundane than the megaboulders (found only locally on Eleuthera), the sedimentological structures found within chevron ridge and
runup deposits across islands throughout the Bahamas and Bermuda point to frequent and repeated inundation by powerful storm
waves, in some locations leaving storm deposits tens of meters above sea level.
Concurrently, coastlines of the Bahamas and Bermuda were impacted by massive storms generated in the North Atlantic Ocean, resulting in a unique trilogy of
wave - transported deposits: megaboulders, chevron - shaped, storm - beach ridges, and
runup deposits on high dune ridges.
Just the other day I posted evidence that the recent
runup in US heat
waves, seen in the context of the last 100 years or so, is hardly unprecedented, a local effect paralleled by similar run - ups in the past.