
 
		T H E  R H j E T I A N  ALPS .  2?  
 "  at  prefent  form a kind of  canal  to  the Adigc,  united  fotmcrly,  at  an  imraenfe  lieiglit  ;  
 "  fo  that  the  rivet  being  pent  np  within  dofe  rocky  banks,  and  the  channel  being  
 "  fteep,  the  water  precipitated  itfelf  from  the  fnmmit of  tl.ofe  monntains,  forming  a  
 "  large water-fall."  He  alfo  adds,  "  that,  the  conrfc of  the  river  being  thns  flopped,  
 "  the waters  had  naturally  formed  an  extenfive  lake  in  the  valley  of  Lagarina."  His  
 affertion  is  very  probable,  as  every  appearance  indicates  that  the  pafs  of  Chiufa  is  as  
 much  indebted  to  art  as  nature.  
 TH.  relative height  of  the  different  ftrata,  as  alfo  the parallelifm  in  their  inclination,  
 clearly  feen  on  the  fides  of  the  two  lateral  mountains,  which  ferve  a.  limits  to  the  
 Adige,  appear  to  corroborate  what  that  writer  fnppofes  to  have  been  the  cafe;  for,  
 if  one  obferves attentively  the  fearps  of  the  greateft  part  of  thofc mountains  which  are  
 turned  towards  the  valley,  they will  be  found  furrowed,  forming  feveral  parallel  excavations  
 in  the  rock,  greatly  rcfembling  the  northern  fide  of  mount  Salive  in  Savoy;  
 which  feem. to prove  that  the waters  retired  reludanlly  from  thofe motintaks.  
 TH,  paffage  of  the  Adige,  at  the  fort  of  Chiufa,  is  very  like  that  of  the  Rhone  
 between  the extremity  of  mounts  Jura  and  Vouache,  below  the  fort  of  Clufc.  Thofe  
 places  have  likewife  a  fimilarity  in  their  names,  the  word  CUuJa  implying  a  itor  or  
 a  term  generally made  ufc  of  by  the  inhabitants  of  the Alps  and  Pyrenees, 
  when  fpeaking  of defiles.  
 TH,  fort of  Chiufa  is  f,mated  on  the edge of a high  rock,  which  commands  the  road,  
 is  nearly  perpendicular  to  it,  and  a  continuation  of  mount  Valcrgue.  It  ferves  as  a  
 barrier  to  the  defile;  and  the Venetians,  to whom  it  belongs,  keep  a  fmall  garrifon,  in  
 order  to  protefl  it.  They have  alfo  ftrengthcned with  a wall  and  parapet,  the  finnations  
 or windings  of  the  rock, which  extend  to  the  bottom  of  the  mountain,  and  are  there  
 terminated  by  a  large  fquare  tower,  where  a  few  invalids  are  ftatloned  to  collefl  tire  
 duty  on all  mcrchandife  imported  into  the  flates  of  the  republic.  This  fpot  is  as wild  
 and  barren,  as  the valley  I  fpokc of  with  fo much  pleafure  is  rural  and  well  cultivated.  
 The  pafs  of  Chiufa  is  even  dangerous  in  the  night,  being  infcfted  by  a  number  of  robbers, 
  who  are  frequently  lurking  on  the  frontiers,  in  hopes  of  confiderahle  booty,  by  
 plundering  tl,e  unfufpedhig  traveller.  At  a  fmall  diftanec  from  the  Fort,  the  valley  
 widens  in°fenfibly;  and  the  firft  village  on  that  road  is  called  Peri,  which  is  fmall,  
 confining  only  of  a  few  houfes.  Thence  one  proceeds  to  Offenigo,  the  laft  village  
 leading  towards  Tyrol,  belonging  to  the  ftates  of  Venice ;  for,  in  the vicinity  of  that  
 village  is  a  fmall  wooden  crofs,  which  ferves  to  mark  the  boundaries  of  the  two  
 foverdgnties  of  Verona  and  Trent,  or,  perhaps more properly,  the  limits  of  the  county  
 of  Tyr°ol;  as  the  four Vicariati,  f.tuated  in  the  valley  of  Lagarina,  and  on  the  road  to  
 Rcvcredo,  certainly  form  part  of  the  bifiloptic  of  Trent  t  but  the  Houfe  of  Auftria  
 having