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 G O R G E   D E   B E L L E N T R E . 279 
 minisli rapidly, in  those parts which  are unprotected  
 by  a  covering  of  soil  or vegetation, 
   and  such  appears  to be  the  case. 
 At  Villard  Goitrou  the  valley  terminates, 
   or  rather  divides  into  two branches,  
 through  each  of’  which  there  runs  a  considerable  
 to rre n t;  these  unite  here,  and  
 form  the  Doron.  It  was  down  the valley  
 on  the  left,  that  the  great  inundation  descended, 
   which  occasioned  so  much  damage  
 in  1819.  It gave  no  previous  notice  
 of  its  approach,  except  by  a  tremendous  
 roaring,  the  cause  of which was  unknown  
 to  the  inhabitants  of  the  village  of  Villard  
 Goitrou ;  they  had  scarcely  time  to  escape  
 on  the  rocks behind  the  town,  when  they  
 saw  the  water  instantly  rise  nearly  to  a  
 level  with  the  roofs  of  their  houses,  and  
 many  of  the  houses  were  entirely  swept  
 away.  Near the junction  of the two  rivers,  
 or torrents,  that  form  the  Doron,  there  is  
 a  small  plain;  this  is  almost  entirely  covered  
 with  immense  blocks,  chiefly  of  
 quartz  rock,  which  were  brought down  by  
 the  inundation,  and  left  there.  A few  of  
 the blocks  are mica and talc  slate,  shewing  
 the  nature  of  the  rocks  in  the  upper  part  
 of  the  valley.  The  cause  of  this  inundation  
 is  supposed to  be the  sudden  breaking  
 up  of  a wall  of  ice, which  had dammed up  
 the waters  in  a  narrow  valley  upon  the  
 mountains,  forming  a  small  lake.  On  the  
 breaking  of  the  ice,  the  whole  body  of  
 water  rushed  instantly  down,  tearing  up  
 and  carrying  away,  by  its  velocity  and  
 weight,  every  thing  that  opposed  its  passage. 
 We walked  along the branch  of  the  valley  
 which  turns  to  the  right,  thinking  to  
 have  a nearer view of  the  Aguille  de  Pla-  
 nois,  but the view was here  intercepted by  
 intervening  rocks.  On  the  right  of  our  
 road  we  observed  a  tremendous  cataract,  
 formed  by  the  fall  of  the  river,  which may  
 be  called  the  right  branch  of  the  Doron.  
 The bed of  the  river  is  a profound  chasm  ;  
 but  from  an  elevated  part  of  the road,  we  
 scrambled  along  the  side  of  a  precipice  
 which  brought  us  to  some  rocks  that  
 form  a  natural  arch,  over  the  lower  part  
 of  the  cataract.  Imagine  a  considerable  
 river, which had  acquired  a  great velocity  
 by  previous  descent,  bounding  down  between  
 overhanging  rocks  into  a  chasm  200  
 feet  deep,  with  a  noise  like  the  loudest  
 thunder,  and  with  a percussion  that made 
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