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Update: Sandy to Erode Many Atlantic Beaches


Update: Sandy to Erode Many Atlantic Beaches

Oct. 29 Update: USGS Revises Coastal Change Forecasts

ST. PETERSBURG, Fla. – On Oct. 29, 2012, USGS revised its forecasts for coastal change due to Hurricane Sandy. Now, the forecasts are as follows:

Delmarva Peninsula: 91 percent of the beaches are expected to experience erosion; 55 percent of the beaches are expected to experience overwash, and 22 percent are expected to experience inundation.

Coastal New Jersey: 98 percent of the beaches are expected to experience erosion; 54 percent of the beaches are expected to experience overwash, and 9 percent are expected to experience inundation.

South Coast of Long Island: 93 percent of the beaches are expected to experience erosion; 12 percent of the beaches are expected to experience overwash, and 4 percent are expected to experience inundation.

The new forecasts, along with maps showing the extent of the impacts, can be found online.

End Update


(Original post from Oct. 27, 2012)

ST. PETERSBURG, Fla. – Nearly three quarters of the coast along the Delmarva Peninsula is very likely to experience beach and dune erosion as Hurricane Sandy makes landfall, while overwash is expected along nearly half of the shoreline.

The predictions of coastal change for the Delaware, Maryland and Virginia peninsula is part of a larger assessment of probable coastal change released by the U.S. Geological Survey Friday. 

“Model forecasts are run anew for each hurricane, as each case has unique factors in terms of storm intensity, timing with respect to tides, angle of approach, and must account for ever-changing details of coastal dune configuration,” said USGS Director Marcia McNutt. “These models help us understand where emergency management resources might be most needed.”

Overwash, the landward movement of large volumes of sand from overtopped dunes, is forecasted for portions of the east coast with the projected landfall of the storm. The severity of overwash depends on the strength of the storm, the height of the dunes, and how direct a hit the coast takes.

 “On the Delmarva Peninsula, near the storm’s expected landfall, close to three quarters of the sandy coast is expected to see beach and dune erosion. Fifteen percent of the coast is very likely to be inundated by waves and storm surge,” said USGS Oceanographer Hilary Stockdon from the USGS St. Petersburg Coastal and Marine Science Center.

In these areas, waves and storm surge would transport large amounts of sand across coastal environments, depositing sand both inland and offshore and causing significant changes to the landscape, Stockdon noted.

The models show that along the New Jersey shore, 81 percent of the coast is very likely to experience beach and dune erosion, while 7 percent is very likely to experience overwash. It also indicates that on the south shore of Long Island, N.Y., including Fire Island National Seashore, 43 percent of the coast is very likely to experience beach and dune erosion. Overwash and inundation are not expected in these areas because of the relative high dune elevations.  

According to USGS geologist Cheryl Hapke, many of the sandy beaches along the mid-Atlantic Coast have become increasingly vulnerable to significant impacts such as erosion because of past storms, including Hurricanes Ida (2009) and Irene (2011), as well as large northeastern storms in 2005 and 2007.

“Beaches and dunes often serve as the first line of defense for coastal communities against flooding and other hazards associated with extreme storm” said Hapke, “Any compromise to these features means that storm-related hazards are more likely to threaten coastal property, infrastructure, and public safety during a future extreme storm event.”

Beach and dune erosion occurs when storm surge and waves collide with the base of a dune, termed collision in the model, and wash away significant amounts of sand. Overwash happens when these forces exceed dune height and move sand inland. Inundation is a process by which an entire beach system is submerged and, in extreme cases, can result in island breaching.

The USGS coastal change model forecasting likely dune erosion and overwash from the storm can be viewed online.

For the latest forecasts on the storm, listen to NOAA radio.  For information on preparing for the storm, visit Ready.gov or Listo.gov

USGS Newsroom


More information

Parameter Value Description
Magnitude mb The magnitude for the event.
Longitude ° East Decimal degrees longitude. Negative values for western longitudes.
Latitude ° North Decimal degrees latitude. Negative values for southern latitudes.
Depth km Depth of the event in kilometers.
Place Textual description of named geographic region near to the event. This may be a city name, or a Flinn-Engdahl Region name.
Time 1970-01-01 00:00:00 Time when the event occurred. UTC/GMT
Updated 1970-01-01 00:00:00 Time when the event was most recently updated. UTC/GMT
Timezone offset Timezone offset from UTC in minutes at the event epicenter.
Felt The total number of felt reports
CDI The maximum reported intensity for the event.
MMI The maximum estimated instrumental intensity for the event.
Alert Level The alert level from the PAGER earthquake impact scale. Green, Yellow, Orange or Red.
Review Status Indicates whether the event has been reviewed by a human.
Tsunami This flag is set to "1" for large events in oceanic regions and "0" otherwise. The existence or value of this flag does not indicate if a tsunami actually did or will exist.
SIG A number describing how significant the event is. Larger numbers indicate a more significant event.
Network The ID of a data contributor. Identifies the network considered to be the preferred source of information for this event.
Sources A comma-separated list of network contributors.
Number of Stations Used The total number of Number of seismic stations which reported P- and S-arrival times for this earthquake.
Horizontal Distance Horizontal distance from the epicenter to the nearest station (in degrees).
Root Mean Square sec The root-mean-square (RMS) travel time residual, in sec, using all weights.
Azimuthal Gap The largest azimuthal gap between azimuthally adjacent stations (in degrees).
Magnitude Type The method or algorithm used to calculate the preferred magnitude for the event.
Event Type Type of seismic event.
Event ID Id of event.
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Event IDS A comma-separated list of event ids that are associated to an event.

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