
 
		92  N  A   T "Ü   R A L   H H^ - 0   R  Y 
 nature  left-it  in ||iraÉra| not - found ^in  ftrata  or  qrfarrfes-But in  de-  
 ;taóhed-^^^.isa^^|6tijéirÈes:' i i^ ^ É ^ ^ è W d  ':is'  ufu^llj^of  
 a  grey  bluéiüi > colótir.  -  I f 'tlet'rièd'üles  of  tfi*fe-ftpne*are  found  ofc|*  
 :p0ifable?iize' and  a’plaüe  furface,  fo  aèto neediittle  poHfoöïgythey-'  
 .mal^fforfes  i§ r'grinding  the moft> precious colours,  fat' beyôhdiainymàrbfeantl  
 equal  to-any -porphyry.  ■  '  ‘  ^ ........... - 
 ( - ;TKere;is  another-fort  óf  Elvan,  'which  conflits  óf-’-a, yëllow-clay  
 >ti&k-fet  with  opaque,  -white  and  yejfow$gÿfedlihè- grà-.  
 niôlés,  and-  thëfe  thinly  befprinkled ’"with -cinereous  grains ;  both  
 •the  grains  and  granules  have  frriooth  and^ plane  •'foffàdes':  -This;  
 ftone rifes in aquany at Boreppa in Càtnborn,  and elfewher^S fopndl  
 ifiifegè;npdülesi  immerfed  five  feet  deep  and~more  in  Ïhe;rVórlik  
 çlay-pits: in  Ludgvani,  and  in  finoothed  nodules  on  the.*’ beach  be-  
 twixt Penzance  and Marazion ;  it  is not near,  fo  hard as .the: former. 
 sect. iv.  More  common - Hill,  of  more  various  appearance  and-necélîary  
 Killas.  nie, .is  thte  ffone which we  call  Kallas*.  It  is».of  ‘the  fchiftos .kind,  
 fome  forts'  more,  friable,  and  fome  more  laminated  than: the  refo; 
 ■ there  is icarce  any  field  or  common,  where in fome  ihapefor  cthi^  
 :we do not  find  thefe  ftones,  butjwhere  there' are  (any  quarries  of  
 -it,  the  top of  the  ftratum  is  covered  with- lopfe,  thin: ftones,t  int^n-  
 iperfed with  earth  and  clay, and a;few feet below,  lies thofi^âiÏQn^,  
 the crevices of which  are  nearly perpendicular, and horizontal;;  thefe  
 ftones generally  diptowards  the Weft,  .and! rife, fiât,  of.a -Very ‘.even  
 tViirknefg^  for whichrcafon I  imagine  they are callecbby (thetiTinnersj  
 -Raze  6  ;  . they  have  a ' finooth  : faqe : :for " .htrilding,  and ,'make': 'a  
 ftrong  wall,  but are.  apt  to  bg  feather-edged,^ ' which  makes  them  
 lodge  water,  and  throw  damps  into  the  walls.  There .aie  three  
 forts  of'thisftone,  the yellow, -thè  cinereous  or^blueifh^ and^ the  
 brown.  The yellow  is  hard and  lafong,  if laid, in .nearly-the feme  
 figure  as  it  rifes,  but breaks  eafily  into  ftuyersÿand  actpfs;the grain,  
 .fo that  it will not  bear hammering ;  it  doeslnot. fermerit -^ndv-oqua  
 ‘forth,  nör  give  fire with Heel,  o f  a  fendy  grit  and  üir&rm' texturê,,  
 with  a  yellow  ochreous  clay  in  it’s  commifiures,  and.  wfeighs  tó  
 water  as  2^ is  to  one. 
 The blueifh  killas  is  fometimes  fo exceeding  hard  and  ftubborn,  
 that  in  the .mine  they  give  five  pounds :a -fathom ‘ for  breaking  
 at other  times  it  is  as  ealy  to  break  as  pitcoal.  Round  the  town  
 .o f Marazion,  and  other  places,  (but  better  foil  in  a  large  and  
 ancient quarry  at  Hélfton  in  Kerrier,)  thére  rifes  a  very  , tender  
 killas,  of  the  cinereous,  and  alfo  . o f .  the  yellow  .cploqr^. bçth  
 fprigged with lpecks  of a darker  hue,  the  texture of both  tHe  lame, 
 * Dr. Woodward Cat. V. ii.pag, 6\ fays we call  1  Woodward’s Cat. vol. i*.pâg.;202»xn. 9 * • 
 I any ftone killas that fplits with a grain*  *  Six feet  long,  fix high,  and three wide. 
 viz.