EUWENZORI AND ITS SNOWS 



157 



piecing together as correctly as possible all my separate sketches and photo- 

 gra2:)hs of each of the peaks covered with snow or glaciers which were seen 

 separately, I have arrived at a result (see p. 154) which may give an 

 approximately correct representation of this snowy range as seen from the 

 east. Eut this drawing, being intended to show the actual extent of snow, 

 is taken from an imaginary standpoint to the east-north-east of Kuwenzori, 



127. TKEE-FERXS OX KUWENZOKI AT 7,000 KEET 



which would be of an altitude nearly as high as the range itself. It does 

 not represent the actual aspect of the mountains from any accessible 

 point of view to the east of it, because from the lower altitudes of Tore 

 parts of the snow would be cut off by the intervening heights forming 

 parallel ridges or divergent spurs of the main mass. 



Kuwenzori is certainly, of all African mountains of my acciuaintance, that 



