
 
		i 
 ■  -Ì 
 20 MOUNT  SION. ALPINE  VIEW. 21 
 the  officers merely  looked into the  carriage,  
 and  suffered  us  to  proceed  without  further  
 molestation. 
 It  was  three  hours  after  leaving  Geneva  
 before we  reached  the  highest  part  of  the  
 road  on Mount  Sion,  though  the  distance  
 is  not more  than  twelve miles,  and we  had  
 two  stout  horses  to  our  coupé,  or  chariot.  
 The  elevation  we had  attained  was  about  
 1500  feet.  It  is  highly probable  that  this  
 mountain  once  formed  part  of  the western  
 barrier,  when  the whole  valley was  a lake,  
 and that the waters flowed over it, before the  
 passage  called I’Ecluse,  through  which  the  
 Rhone  escapes,  was  opened.  Enormous  
 blocks  of  granite  are  scattered  over  the  
 summit  of Mount  Sion,  though  no  rock  of  
 a  similar  kind  is  known  to  occur  in  situ  
 within  the  distance  of fifty miles. * 
 After  passing  the  ridge  of Mount  Sion,  
 we  lost  sight  of  the  vale  of  Geneva,  and  
 the  lofty mountains  near  the  lake  of Annecy  
 opened  on  our  view.  They  were  
 partly  clothed with  snow,  and  their  fantastic  
 turrets  were  intermixed  with  the  
 clouds,  which,  as  they  moved  along,  pre* 
   Some observations  on the blocks of granite scattered  
 over  the  calcareous  mountains  of  Savoy will  be  found  
 in  another  part of  this work. 
 sented  them  under  such  a  variety  of  
 forms,  that  we  were  frequently  in  doubt  
 whether what  we  saw  before  us  were  the  
 mountains we had lately observed, or  others  
 which  a  new  turn  in  the  road  had  discovered. 
   For  more  than  an  hour the  scene  
 might  be  called  an  Alpine  phantasmagoria, 
   where  all  the  great  masses  seemed  
 moving:  the  difficulty  of  distinguishing  
 the  snow  from  the  white  clouds  contributed  
 greatly to heighten the illusion.  But  
 even  when  the  clouds  were  all  removed,  
 one  of  these  lofty  turretted  summits,  the  
 Dent  D’Alencon,  appeared  to  change  its  
 form  in  so  remarkable  a  manner,  as  seen  
 more  or  less  in  profile,  that  we were  often  
 left uncertain  respecting  its  identity.  The  
 bottom  of  the  valley  on  our  right  was  so  
 covered with white stones  that at a distance  
 it  appeared  full  of  water.  Not  far  from  
 Cruseilles  the  limestone  rocks  on  the  left,  
 close  to  the  road, were  nearly white.  They  
 were  shattered  into  an  infinitude  of  small  
 pieces,  like  the  chalk  rocks  in  some  parts  
 of Kent,  but  the  fragments  were  as  indu^  
 rated  as  the hardest marble. 
 We  arrived  at  Cruseilles  about  twelve  
 o’clock.  The  church  is  placed  on  a  dec  
 3 .a