Free fall to the world's centre and the flow of falling water
Indivisible instants of motion, and an argument that a water-jet keeps constant volume
Folio 217v treats the motion of heavy bodies: every free descent is directed toward the centre of the world, and because the instant of motion is indivisible while its time is divisible, no motion however slow ever contains a point of rest. Lettered triangles of motion (with a b equal to a c, bisected by d e f and quartered by g h i) relate the transverse motion of a mover to the natural fall of the moving body. Folio 216r applies the same reasoning to water, arguing against an adversary that a falling stream neither thins nor changes quantity along its length, so equal weights pass every section in equal time. A closing note compares the transverse and downward motions of evenly scattered sand.
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Heavy bodies fall toward the centre of the world
Every free descent of a heavy body is directed toward the centre of the world, provided the motions are equally swift. A companion note observes that of bodies released in sequence the one that departs first ends lowest and the last highest, the middle one threaded by the line joining the outer two.
No instant of rest in any motion
Because the instant of motion is indivisible while its time is divisible, no motion however slow contains any smallest part of time in which it could come to rest. With a b equal to a c, the line d e f bisects each side of the triangle and g h i cuts each side at its quarter; when the mover and the first moving body start at right angles, the positions of all the rest fall on the straight line r f g.
A stream of falling water keeps constant volume
Leonardo argues against an adversary that falling water never thins or loses quantity along its descent, so equal weights pass every cross-section in equal time. Were more water to enter a place than leaves it, all the water in the world would in time pile up there, as two casks entering against one poured out would accumulate without end.
Transverse and natural motion of scattered sand
A falling stream of evenly scattered sand illustrates compounded motion: the transverse motion is to the natural downward motion as the side a b is to the side a g. If the mover runs faster than the sand falls, its horizontal path exceeds the fall in the same proportion, measured in equal time.
