
 
		I l l ; 
 I 1 
 J R j lL   N   A ,ST   tJ  R  A:  L  H I S T O R Y ' 
 for  fofrah|e,  or  the  IiKfejSieY w ilf  hot: ’ ccffi^re 
 nqr  reft, by  one  the  ,other  without  forqe,jbut  will  nbvf*on  e\sj|y*  
 fide,  till  they meet  \Vith  men  refinance  from  external  Boditesj  or,  
 thefo internal  .grarit&tfop;. as  fhall  ferthei  motion. 
 The  particles,  of  Water, i,are  'unalterable;  tor,  pailing  into.To  
 maqy bodies,  a^d through  ftich Alternate' artremes. of Heat  and  cola,  
 if  they  had  not  conftantly #.pfeferv’d (then  enential  properties,  
 moifturep  fince  the  beginning  of  the world, Jnnift  have Tenfibly'di-  
 minilhed^  but  feeing  nb  fitch deficiency  appears,  ana  that" fpririgs,  
 j^insf j§tn^  lifers  £as  abundant  now. as they  ahqiently were  (as By  
 theobferyationson the rifing of me Nile  for riiany ages, among other  
 teafons  inay-appearf we  are  to  conclude,  that  though Wafers'may  
 bf  transplanted^  they  c^n  neither  be  trammuted  nor  deltroyra,  ana  
 whelpev^r removed;  will mdlfo their appearance  Sgain when at liberty, 
   in  the feme liquid  Rate  as  they were  in  before. 
 The particles of Water are  exceedingly fmall,  for  they  may Be  to  
 divided  from  each  other,  as  that  one  fquare inch of‘coifemoh Water  
 fhall when  rarefied,  fill '4  ipace Vhich  will  .contain  fquare 
 inchesfgjj apd.itft  computed'diat  at leaf! -t  particles^fo Vfeter  
 may  be held  on  the point oF,‘a  needle  , " by whffcn  it Sappers, '^hat  
 what we  call Water is- an .aflemblage  o f  a  great  number  of. fmajl  
 {ramparentigfobules,  which  are cbmpofed .agam ^  a h ^ finiteirfairt-  
 ber  of ftnalfer. partfejesibr  atoms of  this  dem^uary  liqiTOr.  'The   
 ufes  anq  appucation o f   tfieie  general’ oDfSvatfoiis wul  foon  bccun 
 Pure Water,  without  any hnxtureof e a r t h f (m t t p | | f ; o f  on^  
 we  know not any  ip  ft’s  natural  nate,  but  ft  is, in fome^arts  pftfer  
 than  in  others,  hnd  beft,  where  itTs  fbunft-TupcienCm  qusanttf£  
 and  in greateft  degree  of  purity. 
 With Water in general few counties are fupplied fo well as Cornwall,  
 and  yet "fewer  are  the  places  where Water ft- m ^  precious ';r‘the  
 moft impure  and  infedted Wafers  being, of great'foe  for  m il ls ,  engines, 
   and cleanfing  the ores,  and  oftentimes  rented  at  ah “exorbitant  
 price..  I  haye, known. twenty  pounds V a  month  given  annually for  
 one .Water-courfe ,to- drive  an Engine-wheel,  three  years  following ^  
 nay  I am  aiforepthat  fifty hounds  a month  have  been'given  for  the  
 feme puroofe,  . Thefe Water-coiirles  are  ufilaDy not  above  the  fize  
 o f  an  ordinary  Mill-ftream. 
 Vapomiaad  * ;  part»  pf. Wat&.3 Being 'Fo  fmall 'anti  mdveaBle,  ate  eafily  
 their rife,  jfepacat^l  one  from  another;  and when’  they  ate 'fo''divided  info  
 hnaU  parcels  as  to  ftepome  about Uqo  rihies  lighter  than  cdmnioh  
 Water,  they  are  atTeaft  'as  light  as  the  hirfoarid’fvill,  By  every ‘fuc- 
 1  Muflchenb.  pag.  738, Nicuwerityt’s  Exper.  Muflchenbr.  p.  425. 
 cefilve 
 O  P  C t o   R  M W A   ,L ;L«  ,  2$ 
 c-effiVe degree  of  feparation,  rife  in  the  air  in  proportion  to  their  
 lightfiifsj  the  heavier air  forcing  the  rarefied  fluid  to  afcend  into  the  
 Atmo'fphe'rfc  rill  it  finds  a  place where  it  refts  in  equilibrium  among:  
 bfiflids  of equal  lightnefs  to  itfelf.  This  reparation  or  comminution  
 (if  I  in ay  fo  call  it)  of Water  into  fmall  parcels,  may be  perfortned  
 either  'fey  collifipn^againft  harder‘and more  compaft bodies',  or  by  
 h e fo^ T h e   firftlwe Often fee  pelflpkrned  at fob  boftdfn vof< Cafeades[v  
 Whdfe  thi Water  that  fells  bdt  a  Few  fathoms,  fliall /rife  fo a   toift  
 frdfn  Ihf bottem Where it is broke'?-  and  therie'kre inftances o f clouds  
 fifiiig from the fall bf Waters wluehanay be feen fiveimileg  Col-  
 fiflbffwill ^Srgfot'e exeite vapours-^lbut  thatwM'ch is more,coiaffeift^ir  
 ill every  part o f :tbe univerie,  is Heaty whether  
 fostri  the  §U&,  Which  is  al^ayt  bufy  this .Wayi  'or  from ■ artificial,  
 fgnMoh, ©f ithat gefteraMy invifibfe .elemental fire which  is diftributed  
 all ^natter.  It has  been  by many NafuraKfts  iniaginodj  that.  
 beat  i^ifes  va*pfctof6  ‘by extending  the  air  inclofed  fo  the. pores  of  
 and  feiSniftg  gradually  a thin  film  or  bubble o f Water  of  
 fitch dteetifiofis  that it  becomes  greatly  lighter  than  the fame  Ipace  
 t>T comifiefi  air,  &iid therefore  rifes^ateve  I t :  but  this ft^jfofition &   
 hot  tCfeaMe j  for it  is obferved,  .'that ifoamstnll, rife M  ik e '’ peowifP  
 8f  Sn  <air^pUmp,  where,  though  there  .«remains  .fofoe:for,tidfefe jp  
 to  t©(mitqtefudh  a procels.  R>may:hefe  he added,  
 ^fat  mid  -ftcMes  aad  iSfews'^hay  sailed'''into'.'stiife 'i^Ltofo&  
 ■ phteto,  ^thoflgh  theh:  parts  will  not  Term  'haftMes';^s;jfosSfe:i;qf  
 Wtfter'Wfll.  As this  too ^eiieidly alewed^fippsfirian  is.o@tfo  
 fepported 'Whbn  ftriftly exanrined,  fb  neither  is  it  i at  all  necefiary  
 f e   ’ Cialifider  sa  this  scafe  any rotfier  than  the  Avtfifodity. rif  
 ■ Water,  -aftd  the  infeuating  and  difperfive  quaBties  of'jfi®e j  both  
 ‘©riderit -ih 'their Offegts.  Fire,  we  fee,  feparates  more 'orsiefenthe parts  
 ©f a ll  bbdifes,  whether  fluid ot  fblid,  and raaal^ ^ em  iiferfo the  ain:  
 "afeparatiClfi',tterfefore ds  all  that , needs1 be  sfbppofed ;  .and/fire does  no  
 zifiibre! to  than  to all  other  bodies under its povier : .jtffcpa- 
 ^tesffkSto'fodhTEaadl.qjctrrions,  that thehir  is more  p©jfoemwis,‘thEn  
 ihe ’ Ream,  ^iid 'df coftfeqaence ‘remains  nearer /tDafheiistt3i".rby'As  
 lfop’eriour ‘gravitation,  s 
 ’  'JTife  pafts *bf  vapour fore- not sail bqnally.sfmall,  ibut firiall raoceafd-  
 1iHg ^to  gree ‘Of heat which  rarifies  them  :  they will,rife in  air,  
 '<Whdn:  rarififed  only' tdO rimes;; but  they will rife  qufekec, «(tbatris,  
 'Wilh Jpgsftfer' ifofcfe}  arid' hfoheft faccordihg ;• fo  sail1  |lfo: -anteirmediate  
 'degfee§U#t8£refe<ftion,  fromsSorijio  140®.  ' Vapour igreatly heafed  
 'bedoffiKt-'fb idteflfek ithtttrit will^ove  vaft weaghtsf  aiay,vdt fappears  
 -firirn! 'e^eritrtftit,  thratj 'Whe'nbifois  fufficientlybrarified,  i f  fexeeeds 
 •  K  The' fall • of 'Watersicat  Niagara .iin TNortli  America,  andT that poJt;' Ihe A.riT;er :yelino., in  Italy,  
 Muflchenbr.  page  740.  .  , 
 .  the