Essay, Ec. 229 
and, near its union wich the Serayu. the River 
Pellus, which traverses the Eastern parts of 
Passir, and receives many Ku orcigate strcams, 
among: others the 
Another large. branch from the North unites 
the vaiious rivers and rivulets of the central 
portion of Passir, which, as well as those ffow- 
ing into the river Pellus, have their source from 
che declivities of the mountain of Tagal; ic is 
called Lo-gowok, a principal branch is the river 
Banjaran, nearly of equal size; both reccive 
numerous rivulets in the higher districts, of 
which the names were not ascertained wich accu- 
-racy. The Lo-gowok falls into the Seray u; 
several miles West of the api 
- The Western declivizies of the mountain of 
Tagal, and the adjoining central. Ranges i in that 
direction, furnish three rivers which unice 
southward of Aji-barang: “The Datar flows 
near the principal village of that District, the 
Kawung a few miles Westward, and still farther 
in the same direction the 7742/7505 the two 
dormer. having eniged s to the later, it Ed 
rayu sever les to ti | 
discharge of the river. pir ond 
Very near the mou:h of the No | icre- 
ccives hom the West a large branch, of nodis- 
tant source, conveying the waters of the lower 
marshy districts, which accumulate at the 
pu dcclivi.izs of the cc n TIDES. Aris 
