CONTINENTAL SLOPE
SUBMARINE CANYONS FOUND AS LARGE V-SHAPED FEATURES OF SHELF AND SLOPE ENDING IN FAN SHAPED WEDGES OF SEDIMENT AT BOTTOM OF SLOPE (RIGHT ANGLE TO SHORELINE)
FOUND IN AREAS WHERE MAJOR STREAMS EMPTY LARGE QUANTITIES OF SEDIMENTS INTO THE OCEAN
SEDIMENTS HAVE GOUGED THE CANYONS -TURBIDITY CURRENTS
TURBIDITY CURRENT AVALANCHE LIKE ACTIVITY