PLATE XXII. 



Fig. 1. — An exposure of a poor lignite seams, 2 Inn north of Cliyang gi 

 (^ ^). It occurs on the upper horizon of tlie interesting Tertiary 

 deposits on tlie east co.ist, as may be seen in tlie sectional column 

 (pp. 95-9G). 



Fig. 2. — The stone- walled evriwài of Cliyang-gi upon the sheet of blackish 

 eruptive flows, as seen from its southeast foot. It is a poor 

 enmnâi and the only one along the coast between the Yöng-il Bay 

 and the cove of Ul-san. It was often a landing place of the 

 Japanese bands which in former times threatened the peace of 

 Kyöng-jyu, the ancient capital of Sil-la (p. 95). People told me 

 that an enormously heavy bell of the Sil-la time Avas brought 

 hither over the coastal mountain by the Japanese to be carried 

 on a junk over the Sea of Japan ; and even now it is rumoured 

 tliat a number of speculative merchants at Fukuoka are endea- 

 voriug to organize a joint-stock company to raise the historic bell 

 imagined to have been sunk in the sea near the coast of Hakata. 



Fig. ?). — -Turning from the coast at Oa-cup, my route led westwards up a 

 desert-like valley to the Kana-chhi pass (;)[)P ^ \\f^) in the terrane 

 of the ' lilack shale series,' which is seen in the middle of the 

 picture. The conical peak to the right is a trachytic andésite 

 (pp. 97-98). 



