Experiments are described in which artificial beaches were attacked by a combination of running waves parallel to the coast and superposed standing waves at right angles to the former. Beach cusps were formed only when a steep beach was eroded by the waves. Observations in nature are cited that appear to support the view that standing waves may be the cause of beach cusps, but further data are needed before a definite conclusion can be arrived at
Beach cusps are common features of steep reflective and intermediate beaches. However, very few obse...
Large beach cusps (LBC, wavelength of ~ 30 m) are intertidal features that can alternately exist in ...
Application of non-linear forecasting and bispectral analysis to video observations of run-up over c...
Beach cusps are crescentic shoreline accumulations of unconsolidated sediment that are characterized...
International audienceA field of beach cusps formed during a field experiment at Nha Trang Beach, Vi...
Beach cusps are a common feature of steep reflective and intermediate beaches. Although many observa...
Computer simulations of flow and sediment transport in the swash zone on a beach demonstrate that a ...
Beach cusps are rhythmically spaced, crescentic beach features which consist of cusp shaped seaward ...
Beach cusps, formed during a storm are observed. The storm acted for three hours together with high ...
Distinguishing beach cusps from cuspate deposits, descriptions and illustrations are presented based...
The Houtribdijk is a dike intersecting the IJsselmeer and Markermeer, and is partly reinforced by th...
The morphology of beach cusps on a number of beaches around the South Island, New Zealand is describ...
Vita.A series of experiments was conducted to investigate the processes involved in the formation of...
International audienceBeach cusps are common feature of steep reflective and intermediate beaches. H...
Morphological observations (terrestrial laser scanning) and sediment analysis are used to study beac...
Beach cusps are common features of steep reflective and intermediate beaches. However, very few obse...
Large beach cusps (LBC, wavelength of ~ 30 m) are intertidal features that can alternately exist in ...
Application of non-linear forecasting and bispectral analysis to video observations of run-up over c...
Beach cusps are crescentic shoreline accumulations of unconsolidated sediment that are characterized...
International audienceA field of beach cusps formed during a field experiment at Nha Trang Beach, Vi...
Beach cusps are a common feature of steep reflective and intermediate beaches. Although many observa...
Computer simulations of flow and sediment transport in the swash zone on a beach demonstrate that a ...
Beach cusps are rhythmically spaced, crescentic beach features which consist of cusp shaped seaward ...
Beach cusps, formed during a storm are observed. The storm acted for three hours together with high ...
Distinguishing beach cusps from cuspate deposits, descriptions and illustrations are presented based...
The Houtribdijk is a dike intersecting the IJsselmeer and Markermeer, and is partly reinforced by th...
The morphology of beach cusps on a number of beaches around the South Island, New Zealand is describ...
Vita.A series of experiments was conducted to investigate the processes involved in the formation of...
International audienceBeach cusps are common feature of steep reflective and intermediate beaches. H...
Morphological observations (terrestrial laser scanning) and sediment analysis are used to study beac...
Beach cusps are common features of steep reflective and intermediate beaches. However, very few obse...
Large beach cusps (LBC, wavelength of ~ 30 m) are intertidal features that can alternately exist in ...
Application of non-linear forecasting and bispectral analysis to video observations of run-up over c...