
 
		g $ |   N   'A ,.T .:U  R   A   L ,;  H I S T O R Y   
 pasture,  or  fjfhery,  tin. muft  needs  .appear, Jo  be  a  great  bfeffing  
 jo  this  cquqty j  but  indeed  that  part  of  jt where  the mines ehaiiee  
 to.% at  prefent,  viz.  from St. Auftglweftwards,  feels  this advantage  
 moft fenfibly,  lands  bringing  a  higher  rept,;the number  of  people  
 being  greater,  and  the  markets  much  better  flocked with .buyers,  
 than  the  eaftern  parts  of  the  county where  there  are no mines. 
 s e c t .  .  ..The  ufes  o f  tin  are  many:  the  ancients  ufed  it  to make  their  
 Ufesof tb  mhtours,  which  ferved  all  the  purpofes of  looking-glades;  but  to  
 this  conlumption  luxury  put  a  flop  (lays  Pliny)  hy  introducing  of  
 filver:  in  other  particulars  their  ules  of .this metal were much  the  
 lame  as  thofe of  the prelent  age,  though  notffejmany.  Tin  is: ufed  
 in  tinning  brafs  and  copper  furniture ; q£  the  kitchen,  in fodering  
 pipe  and  fheet-lead,  in  making o f   latfin,  bell-metal,  hard-wares,  
 in  lining of looking-glafles,  in  fyrgery,  medicine,  and  painting,  frmfe  
 above  all  in making  pewter,  which  in  feme  meafure  is; ufed  in  all  
 civilized  nations,  by  every  degree,  from  the  pooreft  day-labourers  
 to  the prince upon the  throne,  there being hardly a houfe in Europe*  
 or any  part  of  the world where  commerce  reaches,,  but  has. feme  
 pewter:  in  all  thefe  particulars  the  confemption  is  as  general  as the  
 ufe,  and  frelh demands and  frelh  fepplies  are  perpetually  quickening  
 and urging on  one another. 
 s e c t . xx.  Tin  is   the  lightefrof all  metals, being reckoned  nearly to'water  as  
 SutsOT-  7321  to  io o o ';  the  lofteft- of  all  metals,  (lead  only  excepted)  and;  
 gine, con-  the  Icaft fixed  in  fire ;  it cafily. mixes with other metals,  but  imparts  
 -a brjttlenels.to  aUj  aqua  regia^is;itSfproper natural menfhmm; 
 Tin  in  its. natural  ftateandhardeft, bed muft,'  I  fhould  thinks be  
 Coeval to  reckoned  coeval with  the.  creation ;  for  it  is found in  bunches  and  
 the creation, fpof-g  in . the granite,  and> the much harder; ftone. o f  the Elvari. kind,,  
 ftones which can give no fefpicion of their having: ever  been  diflolved  
 and reformedfanicz the firft induration of fclids; in laxer nidus’s the particles  
 of tin  may have fluctuated and  changed  fitiigrions.  It has been  
 imagined  that  tin  fettled  in  fuch  bunches  by  the.  percolation,  of  
 waters  charged with  tin,  but  thefe  bunehes .are  frequently  found  in  
 feparate  blocks  of  ftone,  open to day,  and.  fubjedt  to  no  moifture  
 but that o f the heavens,  and  confequently to. no  percolation.  Again :  
 In  percolation,  either  the  texture  of  thefe  ftones would  in  a  great  
 meafure  refift  the  paflage  of  the  tin,  or  would  freely  permit  i t ;  in  
 the  firft  cafe,  we  fhould  find  the  tin,  condenfed  near  the  furface;  
 in  the.  latter,  find  it  fenk  and  collected  near  the  bottom;  but  it  
 is  difperfed without any  regard  to  either. 
 r But  in  the  computation  allowance  ihould  be  made  fox  the  different  purity  of  the weighed  
 specimen.  ’•  1^31  i  ~  ' 
 T i n 
 ,  Tjnyearly:approaches  toTilvei? in  coldur,  but has  fo much. more Its connex-  
 fulphu-r  ifmt,  that fr? .quickly-tarnifhes  iri the  air Or moifture-,  arid  is ^  witil f f   
 re^My- not"fev-fubje£t  toehold  ffl^Cpas'itsTifter  lead,  which  is  teekon-  
 ;e§r?n inferior  ifietal;;  frpi, • befilfes: - the. ■ colour,  it  has  feveral  properties  
 in  eorympayCth filver, anctfigquient connexions with ft;  diflolved  
 Atfttong^qi(Mil®raws  ■ bitteTfl 'a#well' ’.as;  filled with  filver 
 obftinaiMy  adher y to -i&-  an,d  rqfift's0 lead  almort^s much  as  filver.  ’  
 ^ilvMrt^hpygh ,npt '-of  the .purejfewiid^ ^ may  be  estfta&ed .from  tin \ ' 
 In  tti|~neigIb<^rooodrpf Grq^M|ai,m^vja-.  in  Pemlfefnpus  for'the  
 mines heat-fe) ,|^tEe Gqlloquirijf^hich  although  a mane ‘of  tin,  yet  
 ,%oW  and  thgn ui^fQllowing> thfe^eins .thereof,, .th^y meet with  rich  
 'ores  of  filveiyHwhich  they  call  Lipta '. 
 4  Native hinjp'or  tin  found  irt'the  Cornifh mines  in*,,a metallic ftate, Native tin.  
 [1  am  not certafefthat  lever  faw;  frut March  :2T,  1747,  tyiewinga  
 rich  .piece!  of  tin-ore* from Boflehari  in^the Iparifh o f 'M   juft  ima  
 microfeope,  I  thought  I &w,sa  fmall  lift, of-maturate.# fin,  white, 
 {fhining  like  a  thread  of melted  pewter;  I then..took a, greater magnifier,, 
  and  plainly  perceived  the  fame  "lift;  but  intepding . to  try  
 further  experiments  to  afcertain  the  tfut-h,  I  could, not  afterwards  
 .find  the  fpecimen,.  and  therefore  do  not  aftert  the  matter  of  fad.  
 Agricola,  affetts,  .that  this metal is^nO where )found  fo -pbre as  to  be  
 mafledhle?;  but .the * learned' Df.:Qrew7 (Mufeum ■ R.  S.  page' 3-28!)  
 .deferipeb] one  fpecimen j of  cc native  tin  lying  as"  it were  in  bright  
 jdrops  in a  brown  ftone,’’"'and  I «fee no  reafbn why tin may hpt” pof-  
 fibly- bp Refined,'  and  the impurities  of .its pabulum  feparated by  diT-  
 folvent. juicesrin  the  bowels pf "the*  earth,,  in  like manner  as copper  
 sis.  Metals  fas'it  feems  ‘ to ' mo)vare  only  enfhrined,  more  or  lefs  
 concealed,  and' wrapt  up "into  ores  "by’  falts,  felphur,  .and  ftone,  
 which, are,Sometimes  removed  by  a  fubtal menfiruum  in" the  ehth. 
 This is frequently the cafe o f copper,'femetim.es bf filve5; and gold, the.  
 moft perfect of paetals; .is-ftill more frequently found in a metallic than  
 any  othpr^ftate;  but with  tin  this  very  rarely happens,  by  rcafoh  of  
 the  fcarcity  of  its  proper menfiruum.  Sea-falt  (the  bafis  of  aqua  
 regia))  being  the  only  fait we know which will  operate  qn  tin,  dif-  
 perfe  the  impurities,  and  releafe the  metal. 
 . '  As white  as  tin  is when  melted,  yefcyin-  the  ore  it  is  generally Tmcryftais.  
 black,  and  the  cryftals,  -which  ■ inclofe  the  metal,  are  like  black  
 glafs.  We  have  however  feme white,  feme  cinereous,  and  feme  
 red  tin  grains,  and  feme  of  a  refinous  colour,  but  they are  rare,  
 and  I  fear  often  thrown  away  by  the  heedlefs,  although  curious  as  
 well  as  profitable.  Stamping  and  dreffing  do  but  phl^rizeb and  
 reduce  die  ore  to  fmaller  cryftals,  and  the  fordes which  intervene 
 v  •  See Boerh; Chem. by Shaw?  P*ge 97» 
 1  Alonfo Bsurba»  page 92. 
 B  b  b 
 "  Page 421,  fee  alfo Woodward’s CatVvol.I.  
 clafs ii.  part  fécond. 
 being