
 
        
         
		close of  tlie  dry  season,  and  therefore  very  hot  and  
 dry. 
 Aug.  10th.—Leaving Pudi for the Marudu, we took a  
 N.N.W. direction; Madalon, thesourceof the river, bearing  
 295° from Pudi.  Curious rumours about the Marudu  
 native  chiefs  had  bee$  current  ever  since  we  left  
 Kinoram.  Kambigging,  a  very friendly chief,  asked  
 me  not to go there.  “ I  took h e a t;  and Gensalong  (the  
 Marudu  chief)  did not want  either heat or me.”  After  
 some  difficulty, however, we persuaded a guide to come  
 with us,  and pushed  on in  earnest. 
 Having  crossed  several  streams,  we  got  a  splendid  
 view  of the Bornean  highlands, with Nabalu towering  
 far  away  above  all  the  others;  although  Waleigh-  
 waleigh,  Nonohan,  and Tumboyonkon are of no inconsiderable  
 height.  Shortly  afterwards  we  crossed  the  
 Tonaran,  running  E.N.E.  into  the Marudu, which  it  
 enters  on the right bank, rising to the east of Madalon,  
 while the Marudu rises on the west.  Madalon is  about  
 4500  feet,  a  long  high  ridge,  separated  by  a  wide  
 valley  from  the  igneous  mountains  of  Borneo;  and  
 composed,  judging  from  the  rivers,  entirely  of  limestones  
 and  sandstones.  Our course being  still N.,  we  
 crossed  several  tributaries  of  the  Tonaran;  one  of  
 these, which  entered the  Tonaran on the left bank, we  
 followed for  some  distance,  but  at length  left  it to  the  
 south, and climbing a high hill, we descended, and  once  
 more  struck the  Tonaran,  running N.N.W. 
 Our  road now lay right in  the bed  of  the river,  and  
 we had many opportunities  of  examining  the boulders  
 in  the  bed,  and  of  seeing  capital  sections  of  strata  
 exposed  by the  river.  The  boulders  consisted  exclusively  
 of  limestone  and  sandstone.  The  former  was 
 a hard, blue  stone,  similar in appearance to the mountain  
 limestone  of England;  the latter a coarse-grained,  
 lightish-yellow rock, hard, and but slightly ferruginous.  
 The limestone  in  places  contained veins of the crystallized  
 carbonate  of  lime,  and  often  interbedded  clays  
 of a reddish  and  sometimes  greenish colour,  evidently  
 altered by pressure,  as  the  cleavage of these  clays was  
 quite  slaty in  character. 
 Travelling  down  the  river-bed  we  soon  arrived  at  
 the  junction  of  the  two  sources  of  the  Marudu,  the  
 Tonaran rising  to  the  west,  and  the  Nonohashan,  or  
 true  Marudu,  rising  to  the  east  of  Madalon.  The  
 course  of the Marudu from Madalon  is  N.N.E., while  
 the  Tonaran runs N.N.W.;  from  the  junction  of  the  
 two  streams  Madalon  bears  S.S.W.  At  four  we  
 arrived  at  Pampang,  the  first  of  the  chief  Gensa-  
 long’s villages.  Pampang:  1 house;  old man, Louma-  
 haigne,  but  under  Gensalong;  10  families,  26  men,  
 and  30  women.  Pudi  to  Pampang  about  twelve  
 miles. 
 The people here  were  also  “ praying  me  for  rain,”  
 and  would  not  be  convinced  that  it  was  not  in  my  
 power to  alter the  state  of the weather. 
 Leaving Pampang  we still continued down the river,  
 passing  the  village  of  Moligo,  arrived  at Gensalong’s  
 country,  Madanao  or  Kombaione,  early  in  the  afternoon. 
   I  explained to Gensalong, who  received me in  a  
 very friendly  way,  that  I  did  not  intend  to  damage  
 his  country, but  that I  had.  been  informed  that  there  
 existed  both  birds’-nests  and  antimony in  the  neighbourhood. 
   He said he did not know of  any, and, indeed,  
 could say certainly that there were none, and he pointed  
 out that had  such  things  existed  in  his  country,  they