Afghanistan; Asia, Central -- Description and travel; Eastern question (Central Asia)
If we take the upper stream and follow it from its source in the
glaciers which lie below the Wakh-jir Pass, it will be found that in
its immediate descent from this field, but without taking its name
from the adjacent pass, the waters of the Amu Daria in their higher
reaches are styled the Panja. This title extends along the Upper Oxus
until, at Bozai Gumbaz, it is joined by the first contribution from the
Nicholas glaciers. This affluent is described indifferently by the name
Burgutai, Little Pamir Daria and Kuntai-su; a little before the meeting
of the Burgutai with the Panja this stream divides east and west, the
eastern arm passing into the channel of the Ak-su above Lake Chakmaktin
so that the Burgutai stream feeds equally the Ak-su and Ab-i-Panja
rivers. The Burgutai is narrow, shallow and inconstant; from its start
to its junction with the Panja it possesses a course of only ten miles
and is solely of interest as indicating one of the tributaries which
go to swell the volume of the Oxus. Below Bozai Gumbaz the stream
which rises in the Wakh-jir glaciers bears the five names Ab-i-Wakhan,
Wakh-jir, Sarhad, Wakh-su and Ab-i-Panja, the several variations of the
name Panja.
The fall of the Panja from its source to its junction with the Sarhad
has been estimated at 1247 mètres in 75 kilomètres. It will be
gathered, accordingly, that it is a very rapid stream until it reaches
the Sarhad. At Bozai Gumbaz and for a short distance along the Wakhan
valley, the river slackens until, turning northwards beyond Ishkashim,
it recovers and tumbles swiftly forward. Before leaving the Wakhan
valley it receives, on the right bank, the stream which flows through
Lake Victoria and is known incorrectly as Ab-i-Panja and correctly
as Pamir Daria. At one time, in consequence of Wood’s error, it was
confounded with the head-waters of the Oxus. Neither in volume, length,
nor through the possession of any requisite characteristic can the
Pamir Daria be accounted the parent stream[7]. This river describes
from its source in the glacial fields of Mount Nicholas a fall of 153
mètres over the first 20 kilomètres of its course. From Lake Victoria
proper to Mazar-tepe, where the Khargosh river flows into it, the Pamir
Daria falls 285 mètres in 40 kilomètres. From Mazar-tepe to Langar
Kisht, where it unites with the waters of the Panja, Ab-i-Panja or
Ab-i-Wakhan, there is a further fall of 831 mètres in 60 kilomètres.
From Langar Kisht to Rang the fall is 327 mètres in 100 kilomètres,
the pace of the river in this stretch of the Wakhan valley being
comparatively sluggish. From Rang, which is a little east of Ishkashim,
to Khorok in Shignan there is a perceptible increase in the current of
the river, its mean fall being 702 mètres in 100 kilomètres.
Public-domain text, read in full here on John Shaqi.
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