Dolly Tubs are erosive forms produced by flowing water. A river with high energy (steep downward slope) transports sand, gravel and rocks. This hard material erodes the walls and the floor of the river bed and produces rounded forms. Maelstroms in the water, locations were the water swirls around on the same place for a long time, the gravel and sand starts to drill a hole into the floor. These are the dolly tubs.
As variegated as the swirls is the form of the dolly tubs. It is typically round or oval, normally it has a steep rim. Very characteristic are deep boreholes, much deeper than their diameter.
Depending on their formations this kind of holes is found everywhere where water flows. Gorges and river caves are a good place to look for them. Dolly tubs are common in caves, as many caves or at least parts of cave systems were formed by flowing water. But they are not restricted to caves and they are not even typical karst features. Dolly tubs are found in all kinds of rocks and everywhere on earth. Many are found at the mouth or the former location of glaciers, where centuries of flowing melting water formed the most extraordinary rockmills or glacier mills.
Often the bigger rocks which are turned and swirled around by the water and helped to drill the hole cannot leave the tub again and are now lying on the bottom. They were rounded by the movement and have a spherical form. They are sometimes called millstone or drillstone, or simply pebbles.