The Wakhjir pass, crossing the head of the Taghdumbash Pamir into the sources of the river Hunza, almost marks the trijunction of the three great chains of mountains.
A second pass (the Wakhjir, 16,150 ft.) du ' 'mbash connects the head of the Wakhan valley of Afghanistan Pamir.
The Wakhan glaciers under the Wakhjir water-parting, Lake Chakmaktin near the sources of the Aksu, and Lake Victoria of the Great Pamir have all been claimed as indicating the Glacial of true source of the Oxus.
The same glacial beds of the Nicolas range send down tributary waters to the Panja or Wakhan river, below its junction with the ice stream from Wakhjir, and thus it becomes impossible to decide whether the glaciers of the Wakhjir or the glaciers of Nicolas should be regarded as effecting the most important contribution to the main stream.
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