What is Mud Sliding?
At various locations along the river when the tide is low to mid high, the banks reach approximately 25ft. in height with an angle of 45-55 degrees sloping to the river. Due to the geology of the surrounding area, the river banks are formed primarily of soft mud with the outer layer (4-5 inches) more of a soupy composition. The soft mud is extremely slippery and if one proceeds to position ones self in a fashion similar to sliding, with a little push or running dive, the art of mud sliding is accomplished. Yeeha!
