Essay, C. 277 
“game name, in a direction nearly E. N. E. of 
Pagger pella, is situated in a concavity sur- 
‘rounded by low mounds with obtuse summits, 
by which the prospect is much confined; They 
are all covered by a deep reddish soil. Pro- 
‘ceeding in a North East course 1 found agaiu 
‘an extensive sction of a hiil, composed entirely 
of the same substances which form the princi- 
“pal bulk of the stratified points at Ajibarang 
and the Pawiuian,. being a pile of clay and 
Sandstone, in various modifications, and separat- 
ing spontaneously into prismatical, rhomboidal 
and trapezoidal fragments, between which no- 
'dules consisting of concentric layers, formed of 
the same materials, and covered with an earthy 
* efflorescence, were thrust in. Traversing these 
hills in the direction above mentioned, after 
leaving the environs of Karang-kobar, 1 noticed 
dn several spots, extensive beds and masses of 
Basaltes in a state of entire decomposition, re- 
sembling those of Paggar-pella 5 and in the 
ther progress, the basaltic rocks, which projeté 
ed from a deep yellow soil, were much rounded 
ar the angles by attrition. 
Among the hills on the route to Kali-lunyar 
and in the environs of that village, are several 
elevated points projecting from the neighbour- 
ing unequal Kiteikors Cwhich are marked on the 
hap): mame hills Krang eang. Gaja and 
Lumbung, besides others of less note. The 
constitution of these is elucidated by the ap» 
pearances I noticed in a valley near this vil- 
lage: herethe depositions from water were ve 
abundant, they extended almost perpendicularly 
esl 
