tbele fiogly will not doe it-certaialy all three joy ntly 
willjat leaft tbefe and a thouland others muftjwhich upon 
a modeft conjecture, he computes muft needs pour forth 
Mto the Sea^ at leaft /oo times as much water in a year 
as falls upon the whole furface of theEarthinr^^V, w////, 
fnovps^ devps^ &c. in the fame fpaceoftime. And as he 
judges that all frejlj-ivater fprings cannot come from 
r^i;^-, neither can he beleive either that /'prints, ox [alt 
j[pri7igs are maintain'd thence. Ncr thinks he it likely 
thsit/prmgs, where there falls little of no r^^X or where 
the Cofifervatories muft needs be too fraall, as in thellles 
of Mago, 'E^tunday and the Strophades, the Rock where* 
on ftaads the maiden ToTvcr in the Thracic Bofphorus 
fliGuld be fupplyed from rains. Then he goes on to 
prove that there are fubterraneal communications be- 
tween the Seas zndi fount ains^j which they are fupplyed, 
and that there are Charybdes which fwallow the Sea^ 
which happening fometimes to beftopt, thegreateftT^^- 
^^r./ have ceafed to run, as tkcThames^ Trent ^ Medway^ 
in England '^ the Elve,Motala^ ai\d Gul/pang in Sweden ^ 
and fometimes being too much open d,frejh-water/pringf*: 
have tuTned fa/t, as Fliny fays it once happend in Carz4^ 
ne^T Neptunes Temple. This fubterraneal circulation, 
of waters he further evinces from diwtrsfprings he there ^ 
enumerates that and with the 5 an4 f roiji: 
divers Lakes that have Salt roater and fmFi/b in theft,: 
yet have no fuperterraneal communieation with any 
fuchas the Lake Haguygahon in Hifpanioia, th^ Cafpian^ 
and Mediterranean fcas, &c. He alfo fays that 'tis further 
evident that there are fuchpaflageSi ftom divers marine: 
heterogeneQus fubjlames that ha ve been found in diggings 
deep underground, faeh as peJi fijb^ ^ gc^. Where % the 
way he difcourfes of divers fuch Inhaughts there are in 
the feay more particularly of the fluxm M^fchomctiSi otr 
Maalftroom^ on the coaftpf iVarm?^^^ a^bdlbefeives there 
muft be fomefuch vaft Cbarybdis (belid^^hat t>n the coaft 
