
 
		164  N   A   T   U  R  ttS ffc t  H I S T O R Y   
 their  tin  into  the,purity:and toughnefe of :the;Tprefeirt;)age.^Sfl?hefe  
 nodules  I  look.upon ilfo. as  fragments  o f  melted  tin  fcattereji  from  
 the Jewilh metóog-houfes.: *| 
 sect, vi, f   ,, Tin  is^affo found,among  the Jhme  and  finds  óf  rite s  andiof the 
 h&id and  ,(as  iafomê  creeks  oLFélmouth' harbour  feveral  lords Lof 
 the  foil  havé  lately.experiencèd>ta-their  advantage)  walhed  down  
 probably  from  the  hiüs,. jmd.-refting  in  fuch  Iheltered  fttuations  
 that  the  fea has not power  to  carry  it  off.  This  was  pr'dbably  the  
 firft  pofition  in which  tin  was  difeovered ;  for  in  thp Ohaldee  
 fignifies  flime» mud,  or dirt;  and when  .the PhenioiaJis  came  here,  
 and  faw {this metal  in  its  fiimy  béd,, they  called  it the Mud, - by way  
 o f   eminence,  and thence has  the name Tin!  (in Cornubritifti  Stean,  
 in Latin  Stannum)  proceeded,  and  is  frill Continued. 
 Not  only  creeks  and, rivers,  fiutv^fometimes  the  opeu fea,  I   
 have  feea  in Mount’s Bay)  throws'in  the  fame.metal  to;tig  in  a pulverized  
 ftate.  In  fuch  open  bays  the  tin  Comes  probably from fome  
 lodes,  which,  lying  bare  to  the  fea-,  have  their  uppef-parts«fretted  
 off,  and  by  ftorms  thrown  in  among  the  lands. 
 sect.vh.  That  tin . grows,  or  is  formed  anew where  there was  none  Iw- 
 ^ ^ ^ f o r e ,   in  any  other  fenfe  than  by  approximation  of lik e   partieles 
 metals grow, mover!  from  cine  place^ to  another,:'.is,  dn, m^humble;» opjn^®)^^  a  
 miftake.  That  by  fortuitous  concourfe  (for what  ageh'ey as  it .that  
 condufls  them)  frilphur,  quickfilver,  -or  ar^'-othéf' 'principles in  different  
 proportions,  conipreflèd by  cold’,  or  evaporated  aridrfoppled  
 by heat,  can  be  fo  exactly  forted  as  to  form'a metal,' ièems tojne  
 altogether as  impoflible as  that  the types of a  printer fhould  beebme  
 words and  fentences by being cafually thrown together.  The parts o f  
 metals  are indeed varioufly irivo&ëd,  paft into difiercrit  nidus s. or ce-  
 ments, from malleable and metallic become, lapideous,  from lapideous  
 again metallic.  The  ore  is  tranflated  from önè  part  of the mine  to  
 another, and is renewed where it has been exhaufted;  the metal isrfry  
 fire  or  ufe wafted,  diffipated,  and loft;  yet,  i f  it could  
 ed,  might  again  become  metallic ;  but  tih  is . no  where  formed  
 but  by  the  peculiar metallic  principles  of  tin  concurring,  nor  iron  
 but by thofe  of  iron.  The  formation  óf  metals was  not  left  to  the  
 accidental  occafional  combinations  of  diftinét  ingredients:  their  
 principles  and  criterions  were  all  created  in  their  proper  kind-;  one  
 metal  or mineral  may  mix with  another,  and  remain  dilguifed  for  
 a  time,  but  never  changed.  Sulphur  and  quickfilver,  and  other  
 minerals as well  as metals,  may have  tin  in  their  fubftances,  and by  
 proper  magnets  and  folvents,  will  doubt-left  diftnifs  that  tin,  and  
 remain as much  fulphur  and  quickfilver  as  they were  before;  but 
 O F   G O R N W A L   L.  165 
 frfi adroit  and  exa£t  a  mixture  of  any  principles  in  the  bowels  of  
 thfe éarib,  as  to  conftitute one peculiar metal  unalterably  remaining  
 itfelf, "and not tranlmutable intoany other, feems to me inconceiyeable,  
 if not  impoftible ;  the  conftancy, and immutability  o f metals, muft  
 be  irrefragable arguments  of  thçir  being  created bodies fu i  gmeris,  
 diftina  from  each  other,  and  from  all  other  bodies of  the univerfe,  
 and  o f  their growing  only  by  juxta  pofition.  However,  learned  
 men  are  of various  opinions,  and.-tfiofe  more  efpecially whofe  pro-  
 feftion  it  is  to  .refolve  bodies .inf§  |heir  original  principles,,  a rid   determine  
 the’ number,  Ipits,  and «quantity  of  the  ingretifeajts which  
 compofe  them”.  It  is true  all  bodies whichcome,under  our  obler-  
 vation  are  compounded,  hut,  not  to  range  beyond  the! fpbjeâ: .of  
 our.  prefent?  enquiry,  every  metal  has  -.its'  peculiar  çiara&.erilHcle  
 from which  it will  not  depart,  nor  change  into  any  other  metal ;  
 each  therefore .has.,fome  diftinét  principle which others  have riot ;  
 for  i f  ^11 metals, are  but  mixtures  of  the  fame  principles  in.  different  
 portions  and different  degrees  of  refinement,  why will  they  not by  
 ,any  lubtraâion  .pf  fire  or  ipfeents,  or  addition  made  to  any  one  
 principle,  become  a  left  refined and  inferiour,  an  intermediate  or  
 new,  or  a more  refined and more  valuable metal ?  In other words,  
 why will  not  tin  become  lead  or  filver;  and  gold  become copper,  
 and  vice verja? 
 Having now confidered  the  feveral  ftates and  fituations  in which sEcr.vnr.  
 tin-is  found,  it muft  be  obferved,  that  tin  does  hot .appear  fo  fre- Several way*  
 quently  in  either  or  all  of  them  together,  but  that people  are. per- ^^Sda?  
 petually  fearching  after  more,  and  endeavouring  to  make  frefti covering tin.  
 difcoveries. 
 -, T o  fiy nothing  of  dreams  and  fires  by night,  motives  equally  
 illufive,  though  prevalent  ftilj.  among  the Vulgar,  few  of  the  Cor-  
 nifh  have  ever  heard  of  the  virgula  divinatoria,  and  its  virtue  in  
 difeovering metallic  lodes ",  neither  are  they  often  (perhaps not  fo  
 often  as they ftiould  be)  directed  by  the  tafte  and  colour  of waters:  
 the  run  of  a  lode  is  fometimes  difeovered  by  the  barrennefi  of  the  
 furface  and want  or  weaknefs  of  graft  in a. particular  furrow;  thus  
 in  the  tenement  of  Trenethick,  in  St.  Agnes  parifh,  though  the  
 field  is  cultivated  equally  in  every part,  you  can  diftinguilh  the  
 courfe  of  the  lode,  by  the  unequal  growth  of  the  graft ;  this  
 muft  be  owing  to  one of  thefe  two  caufes,  either  there  is  fo much  
 mineral filt  below  the  foil,  that  the  roots  of  plants  are  parched, 
 m  See Agricola de re met.  lib, v.  Ni  dine its  upper twigs,  (by admitting into it’s pores 
 ,  the  mineral  (team)  in  cale  it  pa lies  over  any  
 "  The  virgula  divinatoria  is  a  (mall  forked  metallic  vein.  Some  perfons  in  Germany  are  
 hazel wand',  which,  being carried (lowly over any  ftill  credulous enough to be fond of thefe magical  
 area of  ground,  Will bend,  it is iuppofed,  andin-  inveftigatians. 
 U  u or