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Example of land loss in coastal Louisiana between 1932 and 2011; detail of Port Fourchon area. Coastal erosion in Louisiana is the process of steady depletion of wetlands along the state's coastline in marshes, swamps, and barrier islands, particularly affecting the alluvial basin surrounding the mouth of the Mississippi River.
Land loss in coastal Louisiana 1932 vs 2011 Population density and low elevation coastal zones in Louisiana Aftermath of Hurricane Laura, Lake Charles. According to the EPA: "Rising sea level is likely to accelerate coastal erosion caused today by sinking land and human activities. The sediment washing down the Mississippi River created the ...
The system then began rapid deepening as a nor’easter it moved offshore early on February 13, bringing heavy snowfall to much of the Mid-Atlantic. The system departed later that day, but not before bringing impacts to Atlantic Canada before peaking and gradually weakening thereafter, eventually dissipating on February 18.
Wind gusts of 60 to 80 mph pounded south-central and southeast Louisiana Wednesday evening, downing trees and power lines in multiple parishes, including Terrebonne, Lafourche and St. James.
Damage in Louisiana totaled to $150,000 (2002 USD, $260,000 2024 USD). September 5, 2002 – Tropical Storm Fay develops offshore the Louisiana coast before making landfall in Texas as a moderate tropical storm. West of Cameron, Fay causes a storm surge as high as 2.5 ft (0.76 m), resulting in minor beach erosion and coastal highway flooding. [17]
A Southern California coastal area long prone to landslides continues to inch toward the ocean at a rising speed posing danger to human life and infrastructure, a new NASA report shows.. The Palos ...
Severe weather jolted parts of Texas and Louisiana on Thursday and Thursday night, spinning up multiple tornadoes to kick off a stretch of stormy weather for the Gulf Coast states. Two tornadoes ...
On non-rocky coasts, coastal erosion results in rock formations in areas where the coastline contains rock layers or fracture zones with varying resistance to erosion. Softer areas become eroded much faster than harder ones, which typically result in landforms such as tunnels, bridges, columns, and pillars. Over time the coast generally evens out.