|
|
About
Beach and Coastal Erosion
|
Beach
erosion
and coastal erosion are not the same, but they are
related. Beach erosion is a reduction in the amount
of sand a particular beach has. On a global level,
sea level rise causes beach erosion. But beaches
also erode (and expand) on a seasonal basis.
Beaches
get sand from both the ocean and the land. Larger
waves move sand from the coastal sand dunes off
into the ocean. This raises the seafloor, flattens
the overall profile of the beach, and, therefore,
causes waves to break further offshore. This, in
turn, minimizes the waves' impact on coastal lands.
Beaches recover from these seasonal shifts when
the waves move the sand back onto the beach and
the winds blow the deposited sand into dunes. These
dunes will store the land-based sand until the next
large wave event.
|
 |
Coastal
erosion occurs when the beach migrates
toward the land in order to compensate for beach erosion
as it tries to maintain a constant supply of sand (see
the right side of the photo). If sand is not available
to a beach, such as when a wall is built to protect the
land, the land is stabilized, however beach erosion will
occur (see left side of photo).

Photo courtesy of Charles Fletcher
Installing
a seawall or revetment (i.e., hardening a shoreline) interferes
with the natural cycle of beach erosion. Rather than pulling
sand from a landward supply in order to promote waves
breaking further off-shore during the seasonal high wave
period, the seawall or revetment prevents this natural
phenomena from occurring. Thus, the land itself begins
to erode.
Therefore,
it is tragically ironic seawalls or revetments have been
installed to prevent coastal erosion, but their very presence
exacerbates the very problem they were supposed to resolve.
Source:
Fletcher, Charles, Eric Grossman, Bruce Richmond. Atlas
of Natural Hazards in the Hawaiian Coastal Zone. 2000.
|