
 
		,96  N  A  T  U  R  A  £   "   f l   I> f  |T'D  R  Y 
 quantityfufficient  to  conned  the  fendtogether;  tamotenoughl to  
 concrete  into  a  firm  hard  body.  Dr. Woodward’s Gat. vol.  II:  p.'"3,.  
 fays  the'inhabitants  calh-it  a  kefriecl  -ftone j  that  is,  a  -coagulated  
 ftone,  but-juft-congealed;  and  indeed  it  is no more  thanthe  blown»  
 fand  incrafted  into  ftone  in  fo many  thin  feparate'  layers;  one - over  
 another*  as  the  fend Was  -thrown  in,  mixed with  the  fparry  iprayg  
 at  feveral  fucceffive  times,  by the’Northerly; winds..  Let  !no  pne  
 wonder  that  the  fpray  of  the-fea  IhaU  produce  fufch/an . effei£|;j  
 5 for  that  fpar is  fufpended  in  all  water  is Hkely;  but,’  in  . particular  
 ■ waters,  is  evident  from  incruftations  formed  in  the^ bottom  of  cu%  
 nary  veffels,  and  in  water-pipes;  from  petrified  mofspand  many  
 other  phenomena;  and  that  fpar  isalfo  to  be found- infea-water;  
 muft  certainly  follow,  from  the  fea  being  open  W,  and  ready  
 to  receive,  all  that  "fprings  will  convey  into- it.  All  coralloeid  
 bodies  and  fhells  are  formed  of  fpar,  modified  and mixed  fo  as *to  
 comply with  the occafiom of .marine plants  arid  animalsg.  i  Laftly*  
 fpar  is wafhed  out  o f  die  cliffs and  rocks  expofed^to  the: power, of  
 the  fea;  nay,  great  degrees  o f  heat  will  raife  it  in  vapour,  and  
 what  rifes  fo into  the  atmofphere, - is  doubtlefs  again  conderifed  and  
 .  precipitated by wind,  cold,  and  rainh.  In  feveral  part’s ; o f  Corn--  
 wall we  have  a  lapis ■ arenaceus or. free-ftone,  confifbng  of  fend and  
 quartz.  Near  the  borough  of Micheli  there  is  a  pretty .ftone;  not  
 long  fince  difeovered;  o f a  cinereous  ground,:  fpeGkled with white  
 gravel:  it works very  fmooth,  and  keeps  a  neat  edget  5  In  Gwen^>  
 there  is  a whiter ftorie,  and  in  Stithien  one b f   the’ femerkirid.'  .''’  
 Polrudon  ftone  (commonly  tailed PentoWan)  is  likewife;®f the  
 arenaceous  kind.  This  ftone  lies -in- a  lode  about  fifteen  feet wide,  
 not interfered  by  horizontal  and  perpendicular fifiures,  as  in jlraita  
 o f free-ftone,  but  {helving,  and  in  irregular  maffes,  :aud  .o f thfee  
 different  colours;  the  firft  and  fineft  of  a  milk-white  ground,  
 thinly  befprinkled with  purple  fpecks  about  the twenty-fourth  part  
 o f  an  inch  in  diameter;  the  fecond  of  a  cinereous  ground,  with  
 more,  larger,  but  fainter  purple  fpecks;  the  third  of  a  yellow  
 ochreous  ground,  fpeckled,  but the  purple  lefe  diftinft,  with  feme  
 micaceous talc thinly interfperfed.  Dr. Woodward’s Gat. vol:  II.  page  
 4, had  two  fpecimens (b  z, b 3, ib.) from this quarryone: of an  jfoh-  
 - Colour,  and  indeed  an  irony-water,  I  obferved  here  to  difeolour  
 fomewhat of  the  fuperficies  of die  ftones;  but in the heart,  I  found  
 them  always  o f  one  of  the  three before-mentioned  colours:.  Dr.  
 Woodward,  ibid,  calls  this  a  free-ftone,  and  not improperly*  if  he  
 meant only a  lapis  arenaceus y  but . it  is  greatly  different,  both  as  to 
 *  See page  before,  84.  about  the  fhores uniting with"  the  fand,  make  a 
 h  See Woodward’s Cat. vol. 1.  pa.  116— 113,  folid  ftope,”  Linnajus  Amasn.  Academ.  page  
 &c.  “   About  Cappellham  the  corals  dijjjerled  -  463. 
 Oground