All deltas undergo alternating construction to destruction phases due
to fundamental changes in the relative influence of sediment input fro
m rivers and redistribution by marine coastal processes. During the pa
st 7000 years world deltas, including the Nile, have been in an overal
l construction phase. However, the Nile delta has converted to a destr
uction phase during the past 150 years, triggered by water regulation
which has disrupted the balance among sediment influx, erosive effects
of coastal processes, and subsidence. This former depocenter has been
altered to the extent that it is no longer a functioning delta but, r
ather, a subsiding and eroding coastal plain. Symptoms of the destruct
ion phase of the Nile delta include accelerated coastal erosion and st
raightening of the shoreline, reduction in wetland size, increased lan
dward incursion of saline groundwater, and buildup of salt and polluta
nts to toxic levels in wetlands and delta plain. Without seasonal flus
hing by floods, the former delta plain surface is now incapable of rec
ycling and/or removing agricultural, municipal and industrial wastes g
enerated by Egypt's rapidly expanding population. Moreover, the remain
ing capacity of the system to regenerate itself will further diminish
as water is diverted away from the delta for new irrigation and munici
pal projects in the Egyptian desert, and water allocations to Egypt ar
e decreased by upstream countries. Reestablishing some level of natura
l hydrology is the only credible solution for attaining equilibrium am
ong sediment accretion on the delta plain to offset subsidence, progra
dation along the coast to offset erosion, and sufficient water influx
to flush and remove the high levels of salt and pollutants throughout
the system. However, increased Nile water and sediment discharge could
begin to restore a functioning delta system only if there is a substa
ntial reduction in human impacts.