PLATE XXVIII. 



Tig. 1.— T]io plain of Kn-jiii-ui (ji -^ ^) at the western loot ol tlio Clijüng- 

 n;ii-clilii piss (ri. XXVIL fig. 2 on tlie left, and fig. 3 in the middle). 

 Feldspar-conglomerate is found abundantly as blocks in the plain, 

 but the geological relation is yet unknown to me. The foothills 

 are of sheared gneiss (p. 1'22). 



Fig. 2. — The remarkable erosion-form, viewed from the soufh, looking like 

 a pair of erect pony's ears; hence the name of Mal-i-san (,^ ^ dÜ). 

 It is a transgressing double-peak of the Mesozoic conglomerate 

 resting directly upon a gneiss-granite, and is regarded sacred by, 

 and ^\oll known among the people, like the Tertiary conglomerate 

 of Kalabaka in Thessalia (pp. 121, 12:5). 



Fig. o. — The stretch between Keum-saii ('§{{', ^J) and Mu-jyu is mainly oc- 

 cupied by an orthogneiss, as may be seen in the background, but 

 4 l-m toward the latter an iron-glance-mica-schist was observed by 

 Mr. Yabé, having an appearance of a glaucophane-schist (the hills 

 in front). The view was taken by him toward the north from Ka- 

 chhon-cha (^fpj -^- ^), See page 124. 



Fig. 4.— Chyök-sang-san (^.^lÜ) or " Mt. Ked Skirt" of Mu-jya (^ J^), 

 viewed from the southwest. The basement of this castle-mountain 

 is built up of a porphyritic masauite capped with red, calcareous 

 tnffite and red felsophyre together Avith sandstone and conglomerate 

 having a slow southwest dip. The complex represents the Upper 

 Kyöng-sang formation, being at the east eud of the JNIesozoic of the 

 " spatulate area " (p. 124). 



