The History of SuluSaleeby, Najeeb M. (Najeeb Mitry)
History
The History of Sulu
Saleeby, Najeeb M. (Najeeb Mitry)
Mindanao Island (Philippines) -- History; Muslims -- Philippines; Sulu Archipelago (Philippines) -- History
The districts of the island conform in a great measure to its natural
divisions. However, political reasons have modified the natural
boundaries and increased the districts to six by division. These
districts are Parang, Pansul, Lati, Gi'tung, Lu'uk and Tandu. The first
district on the west is Parang. A line joining the western limit of
Bwalu on the south coast, with a point slightly east of the summit of
Mount Tumantangis, and projected to the sea on the north, delimits
this district on the east and carves out of the western natural
division the district of Pansul. The eastern boundary of Pansul is a
line running from a point 2 or 3 miles east of Maymbung to Mount Pula
and Busbus. The chief reason for separating Pansul from Parang was
to reserve for the sultan direct control over Jolo and Maymbung. This
district has more foreigners residing in it than any other.
A line joining Su' and Lubuk marks the eastern limit of both Lati and
Gi'tung, the third and fourth districts. The watershed line joining
the summits of Mounts Dahu, Tambang, and Sinuma'an and falling on
the east to the vicinity of Su', divides Lati on the north from
Gi'tung on the south. For all practical purposes the district of
Lati may be said to lie between Jolo and Su', and the district of
Gi'tung or Talipao between Maymbung and Tu'tu'. The land joining
Si'it and Tu'tu' is low. Sulu traditions say that when the Samals
arrived in the island this neck of land was submerged and the island
was divided by a channel of water. The extinct volcano of Pandakan,
generally spoken of as the "Crater Lake," which lies in this vicinity,
may be of late origin and may have been the source of the geologic
deposits which helped to fill the channel. Spanish records speak of
a volcanic eruption in the vicinity of Jolo as late as 1840, and it
is very likely that other volcanic action occurred prior to that date
and after the arrival of the Samals in the fourteenth century.
A line joining Limawa on the north and Sukuban or Tandu Panu'an on
the south, divides Lu'uk from Tandu, thus forming the fifth and sixth
districts respectively. A line joining Mount Tayungan and Bud Tandu
divides both Lu'uk and Tandu into a northern and a southern part. In
both cases the southern parts are more fertile and better cultivated
and probably more thickly populated than the northern.
Public-domain text, read in full here on John Shaqi.
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