SEC. VII.] OF NATURAL PHILOSOPHY. 331 SCHOLIUM. I have exhibited in this Proposition the resistance and retardation of spherical projectiles in mediums that are not continued, and shewn that this resistance is to the force by which the whole motion of the globe may be destroyed or produced in the time in which the globe can describe two thirds of its diameter, with a velocity uniformly continued, as the density of the medium to the density of the globe, if so be the globe and the particles of the medium be perfectly elastic, and are endued with the utmost force of reflexion ; and that this force, where the globe and particles of the medium are infinitely hard and void of any reflecting force, is diminished one half. But in continued mediums, as water, hot oil, and quicksilver, the globe as it passes through them does not immediately strike against all the parti cles of the fluid that generate the resistance made to it, but presses only the particles that lie next to it, which press the particles beyond, which press other particles, and so on ; and in these mediums the resistance is di minished one other half. A globe in these extremely fluid mediums meets with a resistance that is to the force by which its whole motion may be destroyed or generated in the time wherein it can describe, with that mo tion uniformly continued, eight third parts of its diameter, as the density of the medium to the density of the globe. This I shall endeavour to shew in what follows. PROPOSITION XXXVI. PROBLEM VIII. To define the motion of water running out of a cylindrical vessel through a hole made at the bottom. Let AC D B be a cylindrical vessel, AB the mouth p = Q: of it, CD the bottom p irallel to the horizon, EF a circular hole in the middle of the bottom, G the c-?ritre of the hole, and GH the axis of the cylin- Kj cler perpendicular to the horizon. And suppose a cylinder of ice APQ,B to be of the same breadth with the cavity of the vessel, and to have the same axis, and to descend perpetually with an uniform motion, and that its parts, as soon as they touch the superficies AB, dissolve into water, and flow ( wn by their weight into the vessel, and in their fall compose the cataract or column of water ABNFEM, passing through the hole EF, and filling up the same exactly. Let the uniform velocity of the descending ice and of the contiguous water in the circle AB be that which the water would acquire by falling through the space IH ; and let IH and HG lie in the same right line ; and through