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F Y3 ]<br />
.I-IElltd EXCeption. Now if compound Bodies<br />
are fo w-y hard as we find fork Of them to<br />
IX, and yet are verg porous, and confiit of Parts<br />
which are only lard together ; the dimple Particles<br />
which are void Of Pores, and were never<br />
yet divided, n-~ufi be much harder. For fuclz<br />
hard Particles being heaped rfp together, can.<br />
fcarce touch one another in more than asfew<br />
Points , and therefore muj% be .kparable by<br />
lnuch MS Force than is requiiite to breal~ a iblid<br />
Particle, whofe Parts touch in all the Space<br />
between them, -\;rrichout any Pores or Interitices<br />
to weaken their Cshefion. An,d how ‘fuch ve?<br />
ry hard Particles which are ohly”laid together<br />
and touch only in a few Points, can itick together,<br />
and that fo firmly as they do, without the<br />
aifiltance of fomething which caufes them to<br />
bc attraAed or prefs’d towards one another, is<br />
very diEicult to conceive.<br />
The fame thing I infer alfo from the cohering<br />
of two polifh’d .Marbles i;lz WWM, and from<br />
the Standing of Quick-filver in the Barometer at<br />
t-he height of 70, 60 or 70 ‘Inches, or above,<br />
when ever it is well purged of Air and careful-<br />
Ily po~md in, fo that its Parts be every where<br />
contiguous both to one another and to the<br />
Glafs. The &moQhere by its weight preik<br />
the Quiclr-iilver into the Glafs, to the height of<br />
29 or 30 Inches. And fame other Agent saifes<br />
it higher, not by pre1ling it into the Glafs, bun.<br />
by majiing its Parts iticlc to the Glnfs, and to’<br />
one another. For upon any dikontinuation of<br />
Parts, made eithqr. by Bubbles Or by fhakin the.<br />
.8 MS*