
 
		too  ' N  A T ' U R   A  L  H  l ’S y  Û ' R Y   
 the £ro»Wflovercoloured tranfparent qifartz,  the grainfrom one-fixth  
 of  an  inch'diameter downwards  these'is  à  giyra-lline,  farinaceous,  
 fmall  fanfl,  inclofefl betwixt  the  grains,  with  a ^ f t 'quantity'of  fil-  
 v!i^'tÛc^iàÉei^ôt^^--'|S6Æé diftancp oFtwodricHes,'generally more,  
 is a  foot of black- cockle,  half inch  or under in diameter ;  when  the  
 foots  are larger,  they  are1 more  diftanri  *  If is  dqmmonly  called  the  
 Silver  Stone .;*  arid  indeed  is of great  lriftre  in  the  microfcope,  every  
 other  granite  placed  by  its: fide  looking  flat  and  -tame.  It' is much  
 coveted  for Walling  in  adder-work,  being  torigh;  keeping  a  good  
 edge,  and  working  eafy.  One  fpecimen  weighed  to  water  as  
 2 _ _ i î   to  i   ;  the  fécond,  of a more 'yellow ground, weighed  more,  
 v iz.  as  2 —   to  i .   It  imbibes  water  ftrongly,  makes  fip  effer-  
 véfcence with acids,  gives fire  with  fteel ;  being  calcined,  |he  black  
 fpots go olf,  éven in  a  fmall  firè;  the  talc will  perpetually  keep  its  
 colour,  though  the  other  parts  grow brown  with  age ;  perhaps  it  
 might do very well  for  filvering grounds  for  paper-hangings,  and  all  
 the  ulès ó f talc. 
 Yellow gra-  O f  yellow  granite  there is  a great  quantity  the ' g r o ^ f ^ & t h w h -   
 yellow,  fpeckled throughout with  black  foliacéous talc  of the fourth  
 o f  an  'inch  diameter  arid  under;  the  charge‘dark,-  cloudy,'many  
 grains o f cockle  from  the  fourth of an ’inch  arid'uiickf  in  diameter,'  
 intermixed  with  large,  toothy,  whitifh,  opake  prifms  of ..quartz,  
 from  an  inch  and  half  long  by  an  inch wide  and' brider., !  The  
 ground of this ftorié being fb porous, and the chargés to frequent,'large  
 and  hard,  make  it  one  o f  the  moft  fhattery  granites Vèykay^’ fit  
 only  for  rough  works,  where  neither  fquares,  fharp  edges^,  nor  
 moldings  are  required.  It weighs  to water  as  2  r -  to  1  :  it imbibes  
 water  ftrongly,  and  difcharges  it  as - fudderily ;  fb  that walls  
 o f it muft be very  damp. 
 Much  better  is  the  yellow  granite  of  Tregóriin.'  Its  ground  is  
 yellow,  and being fomewhat earthy,  riot more firm than the former ;  
 but  then  the  grains  of its\ charge  are  but  from  the  fixth  of  an  inch'  
 diameter  downwards,  and  its  black foecks  of talc  from  the  eighth  
 of an  inch  diameter  and  under,  feeded  fb  thick,  as  to  be ’ feldom  
 more  than  the  eighth  of  an  inch  diflan t.  This  is  a  very  beautiful  
 ftone,  works  as  well  as  the white  Tregonin  before-mentioned,  and  
 is  therefore  reckoned  among  our  beft  granites ;  although  I  muft  
 obferve,  that  the ground is  fo  very  earthy  and  tender  in  both,  that  
 it  can never  bear  a  high  polifh.  It weighs  to water  nearly  as  the  
 white of this place,  viz.  as  2  - - ,z|  to  1  :  imbibes  moifture  ftrongly,  
 but  evaporates  it  flowly,  and  is  therefore  much  dryer  for  walling  
 than  the  foregoing. 
 Red granite.  On  the  lands  of Treaflo,  in  the  parifh  of  Ludgvan,  there  is  a 
 granite of  a  red  ground,  quartz  laminated  with  oblong,  lucid, 
 rhomboidal 
 O  F  C O R N W A L L .   IOI 
 rhoriaboidal-fpak^,  ffom  the  foyr{h  of  an  inch  diameter and  ynder.  '  
 TZUiftfurgo  G°nfifts ’ ^{jlgltffky  ejpereous  granules,  in,  fome  places  
 darkiand  .fookle,  nqfjaqly  granuktej  butjveined; .flie 
 , ground atj,d*t|^^|3|e'quall,y- harcfflp^hjs  ftone  at Treaflb  is  exactly  
 in  ftry^yre^ancl  -colou||^’the  red  Egyptian  granite,  and  
 ife jin . a,vein  about#  bo-y  frofn&the jhqu&, • crofting the publipk  
 road  3f&hich  lead-Srftol/Saftelatadinas^t^td may  prove  better  at  depth  
 than-at  the top, f where  I  found  it:^,It, weighs  to watey,as ,2r- - I f lj  
 #,tQ. one. 
 -Of  a  richer, kind  is  the  $ed  granite  firft  taken  nqtice  -by, the'  
 difcerning  Righ^ Honourable  LordfEjfgcumbe,  by whole  direSons  
 Stables  tyere  firftlmade of^it,'. and vO|^h,apdfpme ftands  forlb-ufts  and  
 f 4fes.  In  th|  new  hajj,hA| MpunifEigg^mj^  hayeijbpen  lately  
 {erected  two  chimjigy-^pieces  prmcipally  c^M s k in d , o f  ftone; ^and  
 indeed  to this  noble Lord  this  beft^ojf our  Cornifh  granites' remark-  
 i able for; its  bold - ruddy  colouring  sjnd  high,  and^^urable  polidr^Tis  
 ,£hfefly  indebted  for  being  refeued^fiom pbfeurity,  and  eftipnated  at  
 To  high  a price  as  it  is'at  prefent hy.tfffi'curipi^.  5 
 fo  foe,panfh .bf jEridgyan .there  is?av granite,  of’ a, .bjatk  cocjde Black granite  
 ground^  charged  fb  thick with white fpots o f femitranfparcnt quartz,  
 from  an  irich^long  by  half inch wide’  and^under ;■   that  the  charge | ,  
 almoft 'rivals  the  ground  in  quantity,'  it  is much  harder  than cthe  '  
 ^ovp-coloured.* granite  .’of  thei feme parifh,  and weighs  to water, as' 
 ■ 2  to - one.  , 
 Abetter  ftonpiof the  black  kind  is  found ;;at  Bofworlas,  in ( th«e  
 -parifh  of St.  Juft;.  the ground jjsipf a blacker  cockle  than  the  fore-  
 igrifogj  and  is  interfiled" in  all directions by toothy mafles o f a warm  
 Jlefh-colpured  quartz,  moftly  in  die  parallelopiped  fhape;  fomey* 
 •times  curvpd,  now and  then in  a  zig-zag manner,  andrfometimes in  
 the' fbrm.ipf ri crofs;  in diameter,  ffom half to  one-fixth o f an inch,  
 by two  inchps  long  and  under.  The charge  in  depth  confifts o f  two  
 •Jivata  (fometitnes  three)  of laminee)  ffom  the twentieth  of an  inch  
 ilthick  and  undel||yyitli^ lttcid  furfaces  parallel to  one  another,  hut  
 dying  at  different-angles with  thofe  of  the. adjoining firatum\\fo  
 that when  one  is  oppofed  to  the light and  fhines,  the  other,  which  
 abutts  at  the  end  of it,  does not.  This  is  a moft .curious and  beautiful  
 ftone,  extremely  hard;  may  be  had  in  large  pieces,  and will  
 doubtfefs with  labour  attain, to  a high  polifh  for  tables, and  ornaments. 
   It weighs  to  water as  2  -  to  1. 
 The marble we  have  in  Cormyall  is not remarkable  either for  its  se c t . viri.  
 beauty or pfe.  In  the  parifh  of  Carantoc,  and  at New Kaye,  in  
 Lower  St.  Columb,  there  is  a  coarfe  cinereous  marble  veined with  
 white  fpar:  it  ferments  ftrongly with  aqua forth)  gives no  fire with 
 D  d  fteel,