Verkefnið er lokað til 20.06.2021.The City of Colwood, British Columbia, Canada, has struggled with the eroding coastline of Royal Roads Bay as a result of a sediment source deficit. The area suffers from strong longshore currents which extract the fine sediments of the sandy foreshore provided by the Metchosin Gravel Pit, which has been a source of sediment supply to the beach for over 100 years; operations ceased in 2007. The study site, a 600 m stretch of beach between the gravel pit and the sewage pump station at Lagoon Road, had not previously been studied quantitatively. This study was undertaken in order to ascertain the rate and causation of erosion, the future expectations of erosion, and provide appropriate mitigation strategies f...
Over the last three decades the beach area of Piçarras has undergone large changes. The river Piçarr...
The coastal dunes and beaches of southern Monterey Bay (the Bay) are eroding at approximately four f...
Shorelines are constantly changing structures and beaches move, shrink, and expand as natural forces...
Along Wreck Beach the existing headland cliffs are eroding and receding under attack from terrestri...
Pigeon Bay Recreation Reserve is a small beach ridge system at the head of Pigeon Bay, Banks Peninsu...
Pigeon Bay Recreation Reserve is a small beach ridge system at the head of Pigeon Bay, Banks Peninsu...
South Bay is situated in a small embayment on the south side of Quail Island. They bay is a popular ...
The waterfront and shoreline of the Town of Qualicum Beach, British Columbia, Canada is a defining c...
The coastline to the east of the Monwabisi Beach tidal pool has been subject to substantial visible ...
The ongoing erosion of the Negril Beach has become worse the past decade. In most places along the c...
The Rosslare and Wexford area has been subject to major changes over the past 150 years. This change...
Beachdune systems are valuable geomorphic assets providing a buffer between the coastal hinterland a...
Beachdune systems are valuable geomorphic assets providing a buffer between the coastal hinterland a...
At the edge of Vancouver and the Strait of Georgia the Point Grey cliffs experience marine and subae...
The northern sector of Waihi Beach is an example of chronic erosive tendency. The sediment deficit a...
Over the last three decades the beach area of Piçarras has undergone large changes. The river Piçarr...
The coastal dunes and beaches of southern Monterey Bay (the Bay) are eroding at approximately four f...
Shorelines are constantly changing structures and beaches move, shrink, and expand as natural forces...
Along Wreck Beach the existing headland cliffs are eroding and receding under attack from terrestri...
Pigeon Bay Recreation Reserve is a small beach ridge system at the head of Pigeon Bay, Banks Peninsu...
Pigeon Bay Recreation Reserve is a small beach ridge system at the head of Pigeon Bay, Banks Peninsu...
South Bay is situated in a small embayment on the south side of Quail Island. They bay is a popular ...
The waterfront and shoreline of the Town of Qualicum Beach, British Columbia, Canada is a defining c...
The coastline to the east of the Monwabisi Beach tidal pool has been subject to substantial visible ...
The ongoing erosion of the Negril Beach has become worse the past decade. In most places along the c...
The Rosslare and Wexford area has been subject to major changes over the past 150 years. This change...
Beachdune systems are valuable geomorphic assets providing a buffer between the coastal hinterland a...
Beachdune systems are valuable geomorphic assets providing a buffer between the coastal hinterland a...
At the edge of Vancouver and the Strait of Georgia the Point Grey cliffs experience marine and subae...
The northern sector of Waihi Beach is an example of chronic erosive tendency. The sediment deficit a...
Over the last three decades the beach area of Piçarras has undergone large changes. The river Piçarr...
The coastal dunes and beaches of southern Monterey Bay (the Bay) are eroding at approximately four f...
Shorelines are constantly changing structures and beaches move, shrink, and expand as natural forces...