GREAT EARTHQUAKE TS JAVA, 36/# 
fcrachite pillar of which the Palimanang mountains consist. It 
then went northwards, and, after having passed Ardjowinangon , 
proceeded again in the direction of west to east; whence also it can 
be explained why the shocks were felt much heavier in the immediate 
neighbourhood of the Palimanang mountain them elsewhere. On 
all places which lie in the volcanic district of the Tjermae the shocks 
were felt little or not at all, hut heavily in the alluvial and tertiary 
district between Cheribon and the river Tijmanok .—Translated 
from the Javasche Courant. 
