Volltext : Burckhardt, Johann Ludwig: Travels in Syria and the Holy Land

DJEBEL  KOULA.
440
tern  hills  of  Djebel  Shera.  After  two  hours  march  we  began  to
descend,  in  following  the  course  of  a  Wady.  At  the  end  of  four
hours  is  a  spring  called  Ibn  Reszeysz  (e,  „).  The  highest  point
of  Djebel  Hesma,  in  the  direction  of  Akaba,  bears  from  hence
S.  W.  Hesma  is  higher  than  any  part  of  Shera.  In  five  hours  we
reached  Ain  Daleghe  (a  ),  a  spring  in  a  fertile  valley,  where
the  Howeytat  have  built  a  few  huts,  and  cultivate  some  Dhourra
fields.  We  continued  descending  Wady  Daleghe,  which  in  winter
is  an  impetuous  torrent.  The  mountains  are  quite  barren  here;
calcareous  rock  predominates,  with  some  flint.  At  the  end  of
seven  hours  we  left  the  Wady,  which  takes  a  more  northern  direction, ¬
  and  ascended  a  steep  mountain.  At  eight  hours  and  a  half  we
alighted  on  the  declivity  of  the  mountain,  which  is  called  Djebel
Koula  (,),  and  which  appears  to  be  the  highest  summit  of
Djebel  Shera.  Our  road  was  tolerably  good  all  the  way.
August  27th.—After  one  hour’s  march  we  reached  the  summit  of
Djebel  Koula,  which  is  covered  with  a  chalky  surface.  The  descent ¬
  on  the  other  side  is  very  wild,  the  road  lying  along  the  edges
of  almost  perpendicular  precipices  amidst  large  blocks  of  detached
rocks,  down  a  mountain  entirely  destitute  of  vegetation,  and  composed -
  of  calcareous  rocks,  sand-stone,  and  flint,  lying  over  each
other  in  horizontal  layers.  At  the  end  of  three  hours  we  came  to
a  number  of  tombs  on  the  road  side,  where  the  Howeytat  and  other
Bedouins  who  encamp  in  these  mountains  bury  their  dead.  In
three  hours  and  a  half  we  reached  the  bottom  of  the  mountain,
and  entered  the  bed  of  a  winter  torrent,  which  like  Wady  Mousa
has  worked  its  passage  through  the  chain  of  sand-stone  rocks  that
form  a  continuation  of  the  Syk.  These  rocks  extend  southwards
as  far  as  Djebel  Hesma.  The  narrow  bed  is  enclosed  by  perpendicular -
  cliffs,  which,  at  the  entrance  of  the  Wady,  are  about  fifteen
or  twenty  yards  distant  from  each  other,  but  wider  lower  down.
            
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