
 
        
         
		put  to  the  waggons  without  delay,  and  all  were  soon  ready  to  
 depart. 
 The magnetic needle was here so much affected  by the particles  
 of iron  contained  in the  rocks  at this  station,  that  it was not to be  
 depended on.  It was my usual practice at every station,  to take the  
 bearings of as  many of our  former  stations  as were  either  in  sight,  
 or  of which  the  situation  could  be  indicated with  tolerable  exactness  
 ; and  at the same  time,  those of  any other  remarkable  objects,  
 and  of our  next  station  forward whenever  it was  known  and could  
 be  indicated  with  precision,  were  noted  down,  By  these  means,  
 the  bearings,  being  taken  both  backwards  and  forwards,  gave  a  
 double  check  to  any  inaccuracy which  might  arise  from  errors  of  
 the needle,  or  from  mistaking  the position of stations  not  actually  
 in sight. 
 In  order  that  this  very  necessary  part  of  a  traveller’s  duty  
 might not, in the confusion of a multitude of heterogeneous occupations, 
  be forgotten,  these  operations were almost always deferred till  
 the moment when the oxen were  brought  forward  to  be  put  in  the  
 yoke;  so that I thus became  habitually reminded  of  what was to be  
 done,  and my men were  by the same  means  prepared  for  pointing  
 out  the  bearing  of  these  stations  and  places  which  were  too  dis„  
 tant  to  be  visible.  On  such  occasions  I  generally consulted  them,  
 and placed more or less confidence in their opinions, as these proved  
 either unanimous or at variance. 
 Fearing that we  should  not  reach  our  next station before dark,  
 we hastened the oxen forward at their best pace, and advanced at the  
 rate of eighteen revolutions * in a minute;  which was equal to 3 miles,  
 1  furlong,  and  170  yards, in an hour.  As  our  road  was  over  deep  
 sands, this rate might be considered as very expeditious, for a waggon  
 on narrow wheels, heavily laden and drawn by oxen.  In some places,  
 a black mottled flinty rock, showed  itself through the surface of the  
 ground. 
 *  The mode in which this was  ascertained,  has.been already explained  at page 289.  
 of the preceding volume. 
 Although  the  sun  shone  pleasantly  the  whole  day,  the  air  
 was  cold,  and  the  thermometer  not  higher  than  56.  (13'3  Centig.;  
 or 10-6  lieauin.)  It was now the middle of winter, or, more properly  
 speaking, cold season :  for the word, •winter, seems  to an English ear,  
 to imply a severity of cold, and to raise ideas not consistent altogether  
 with the weather of these latitudes.  Occasionally, however, a degree  
 of cold is felt, which the  contrast of intervening warm days, renders  
 almost  as  chilling  as  the  wintry  weather  of  our  own  latitudes.  
 During the month  of June,  as  may  be  seen  by the  | Register,’  the  
 thermometer  sunk  several  times  below  the  freezing  point;  on one  
 day the ground was whitened with  snow;  and  hoar-frost  at  sunrise,  
 was  not  unfrequent.'  The middle of the day was  generally pleasant  
 and  moderately warm:  but  the mercury never rose higher than  71 j  
 (17'3.  R .;  21-6  C.)  and for the  greater part  of  the  four-and-twenty  
 hours, was  below the  temperate point. 
 At  a  little  after  sunset,  we  came  to  the Krumtin,  a  beautiful  
 little river running  in  a  plentiful  stream  of  the  clearest water.  At  
 this part of  its  course  it was  fifteen  feet broad and abounded in tall  
 reeds.  A sight so delightful for African travellers, had not been seen  
 since we left the Gariep.  This river, small as it was, as far surpassed  
 all the others in the intermediate country, if rivers they could be called,  
 as the Gariep surpassed this.  It is formed by the Klibbolikhbnni, the  
 most copious spring which  I have seen  in  Southern  Africa.  Unlike  
 other rivers, the Kruman is largest at its source, and rises from the earth  
 a full and broad stream, which, by the combined powers of evaporation  
 by the sun and of absorption by the sandy soil, is gradually lessened as  
 it flows on ;  till at last after a course of a few days-journeys, it is lost  
 in  the  sands,  and  entirely  disappears,  It  is  said,  that  in  the  wet  
 season,  it  is  joined  by  the  Moshva  (Moshowa);  and  that,  in  those  
 years when an unusual quantity of rain has fallen, the united streams  
 find their way to the Gariep. 
 We continued for an  hour,  travelling westerly  along  the  banks  
 of the Kruman, till, it becoming too dark to venture farther, we were  
 obliged to halt and unyoke for the night,  at  a  spot  distinguished on 
 q q  2