Grain size and sorting studies are of great importance in order to textural
ly characterize the sedimentary environments. These parameters are useful i
n order to characterize the dynamic beach environment, which is of potentia
l interest for research on natural resources and to interpret analogous anc
ient sedimentary environments. The main scope of this work deals with the i
nteractions, between grain size and sorting of beach sands and their possib
le relationship with the coastal plain width. More than 10 000 km of sandy
littoral were covered through 274 beach locations: five regions in the Paci
fic and Gulf of California and four regions from the Caribbean and Gulf of
Mexico. The samples were sieved and the grain size and sorting were obtaine
d. The sands were mostly well sorted to moderately sorted and the more abun
dant classes were medium to fine sands. The average grain size decreases fr
om inshore towards backshore; foreshore and backshore sands are better sort
ed than the inshore sands, the latter are probably greatly influenced by mi
xtures and variations in processes related to waves and currents. The sands
of terrigenous beaches exhibit finer grain sizes than those from beaches o
f carbonated provinces. A relationship between the coastal plain width and
the average grain size and sorting was found: better sorted and finer sands
are associated with wider coastal plains. A statistical correlation betwee
n grain size and sorting is observed (r(2) = 0.7957) when their average val
ues are plotted according to major physiographic coastal plain regions.