Backgammon to bear off all of one's checkers, was also the same. Hitting a blot, reentering a piece from the bar, and bearing off, all followed the modern rules. The only differences with modern backgammon were the use of an extra die (three rather than two) and the starting of all pieces off the board (with them entering in the same way that pieces on the bar enter in modern backgammon). The name τάβλη is still used for backgammon in Greece, where it is frequently played in town plateias and cafes. The epigram of Zeno describes a particularly bad dice roll
Ridge push Ridge push Ridge push or sliding plate force is a proposed driving force for plate motion in plate tectonics that occurs at mid-ocean ridges as the result of the rigid lithosphere sliding down the hot, raised asthenosphere below mid-ocean ridges. Although it is called ridge push, the term is somewhat misleading; it is actually a body force that acts throughout an ocean plate, not just at the ridge, as a result of gravitational pull. The name comes from earlier models of plate tectonics in which ridge push was primarily ascribed to upwelling magma at mid-ocean ridges pushing or wedging the