276 Essay, Fc. 
the Northern declivities is a nearly extinct vol- 
canic crater, forming one ofa series in this part 
of the Island which will be mentioned in the 
sequel. At the foot of the hill of Pagger- pella 
I crossed the river Urang : the fixed rocks near 
the banks are Pudding.stone and Basaltes; the 
pebbles in the basin are very much diversified ; 
1 selected the following, all evidently derived 
from a distant situation in the central ranges; 
12: 
1' “Lava of entirely vesicular constitution. 
2. T Lava of the kind of sub marine-lava 
above mentioned, conraining calcareous spar in 
narrow layers or irregular masses. 
3- ti Compact clay in tabular fragments, the 
angles of which are rounded by attrition. 
4. T1 Compact. | udding-stone (or Amygda- 
loid) consisting of — fragments of Basal- 
tes bedded in a claye 
5. § Sandstone in coined and recti-linear 
layers. 
6. §§ Petrified wood with stony concretions, 
The territory between the three principal hills 
of this part of the central ranges, the Pawinian, 
"Telogo-leli and Roggo-'ambangan, is covered 
by numerous inequalities irregularly dispersed, 
of which several deserve the name of hills: on 
the ascent of the ridge called Sari 1 met again 
stones of watery deposition. The village of 
Karang-kobar, the chief of the sevice of xn 
Bsp. Cut, Nag =: 
eia Exp. Cat. No. 525. a 
Exp. Cat. No 
: at. No. 54. 
DE NO ce a e CAS 
- Pang Cat, No. 534. Bet eich kins 
