Bajour
The name Bajour is of uncertain
originl, and nothing seems known as to when or why this name has been given to
this country. I am inclined to think it may be derived from the Persian baj
[tribute] and awardan [to bring]. Tradition has it that the country of Bajour
belonged to a tribe called Arab up to
the time of the Pathan conquest, and was ruled by the Chief of the Arab tribe.
The name may therefore donote the country which paid tribute to that Chief, or
the country for which he paid tribute to the Hindu dynasty of that day.
Bajour comprises eight
valleys,i.e.. Surkamar, Rud, Chaharmung, Watalai, Babukara, Jandol, Maidan and
Baraul. These are now all peopled by the Tarkanri [or Tarkilanri] tribem whol
are akin to their neighbours the Yusafzai of Dir and Swat. They entered the
country about the end of the sixteenth century.
The whol tribe acknowledged allegiance
to one ruling family, of whom Safdar Khan, the Khan of Nawagai, is the lineal descendant.
Owing to dissensions in the tribe the former power of the ruling Chief has in
course of time diminished. The rise of Umra Khan had much to say this. Not only
have the Baraul, Maidan and Jandol valleys now come into the possession of the
Khan of Dir and are iin Dir territory, but the rule of the Khan of Nawagai over
the+ remainder of Bajour is in places merely nominal.
The Bajour of to-day consists of only
five valleys; Sur Kamar, Chaharmung, Watalai,Babukara and Rud. Of these all
except Sur Kamar form part of one drainage system,I,e..of the Rud river which
joins the Panjkora near Sado. Sur Kamar is the name given to the tract in which
Nawagai is situated. The Nawagai, Chamarkand and Suran nullahs, which here
unite, become the Pipal and subsequently the Ambhar river, which joins the
Panjkora and Swat rivers at some distance below hteir junction.
The Chaharmung and Babukara valleys
are occupied by the Salarzai Tarkanri, the Watalai by the Mamund Tarkanris. The
Mamund also own a considerable tract of country in Shortan. Hinduraj and
Marawara, on the northern slopes of the watershed which separates the Kunar
valley from Bajour. These tracts now lie within Afghan territory and the
Mamunds therein are claimed by the Amir as his subjects. They have hitherto
refused to pay tribute to the Amir or to permit interference by the Amir’s
officials in these tracts.
The Rud valley is the main valley of
Bajour and the most important. It is peopled by a heterogeneous mixture of
Tarkanri, Mohmands, Safis, Utman Khel and others. It belongs throughout its
lengh to the Khan of Nawagai, and is divided by him between his brother Sardar
Khan, Khan of Khar, his cousin Wilayat Khan, Khan of Jhar, and his son Ahmad
Jan [recently appointed Khan of Rud]. The Babukara valley is also now in the
immediate possession of the Khan of Nawagai, who has appointed his cousin
Wilayat Khan of Jhar to be Khan of Pashat.
The Mamunds of the Watalai valley
and Salarzai of the Chaharmung valley, while nominally acknowledging the Khan
of Nawagai as their Tarkanri Chief, constantly dispute his authority over them.
Continued fighting takes place between them, and it is hard to say , from day
to day, what portion of those tribes acknowledge allegiance to him for the time
being, and from what portion of those valleys he enjoys tribute.
The boundary line between Bajour
and Afghanistan, as demarcated, runs along the crest of the eastern eatershed
of the Kunar river. It has only been demarcated as far south as a short distance
beyond the head of the Chaharmung valley. According to the terms of the Durand
Agreement of 1893 it continues thence along the same watershed to the Silala
Sar, but this portion is still disputed by the Afghan Governmet.
The total population of Bajour may
be estimated at about 100,000 persons. The main valley of Rud is very fertile
and productive. The Jandol and Maidan valleys now belonging to Dir are also
very fertile. The Babukara valley is not so productive, and the Chaharmung and
Watalai valleys are still less so. The rainfall in Bajour is less than in Dir
and the hills are consequently less wooded. Owing to the lower elevation of the
mountain range in which the affluents of the Rud river take their rise, the snowfall on
them is slight. The rivers not being snow-fed, unlike the Swat and Panjkora,
are lowest in summer and fullest in winter and spring.