The Gates of India: Being an Historical NarrativeHoldich, Thomas Hungerford, Sir
History
The Gates of India: Being an Historical Narrative
Holdich, Thomas Hungerford, Sir
Afghanistan -- Description and travel; Balochistan (Pakistan) -- Description and travel
Before taking leave of these two most successful (and most
trustworthy) explorers of Afghanistan, it may be useful to sum up
their views on that little-known region, Badakshan. The plains, the
useful and beautiful valleys of Badakshan, lie in the embrace of a
kind of mountain horse-shoe, which shuts them off from the Oxus on the
north-east and east and winds round to the Hindu Kush on the south.
The weak point of the semicircular barrier occurs at the junction with
the Hindu Kush, where the pass between Zebak and Ishkashm is only 8700
feet high. From the slopes of the Hindu Kush mountain torrents drain
down through the valleys of Zebak (called the Wardoj by Wood), the
Minjan (or Kokcha) and the Anjuman into the great central river of
Kokcha. Of these valleys, so far as we know, only the Wardoj is really
practicable as a northerly route to the Oxus. Shutting off the head of
the Kokcha system, a lateral range called Khoja Mahomed by Wood (a
name which ought to be preserved), in which are many magnificent
peaks, sends down its contributions north-west to the Kunduz. We know
nothing about these valleys, and Wood tells us nothing, but the
geographical inference is strong that all this part of upper
Badakshan, including the heads of the Kokcha and Kunduz affluents, is
but a wide inhospitable upland plateau of a conformation similar to
that which lies east and west of it, cut into deep furrows and
impassable gorges by the mountain streams which run thousands of feet
below the plateau level. Within it will almost certainly be traced in
due course of time the evidences of those primeval parallel folds, or
wrinkles, which form the basis of Himalayan construction. Probably the
Khoja Mahomed represents one of them, and the heads of the streams
which feed the Kokcha and the eastern affluents of the Kunduz will be
found (as already indicated in the Wardoj, or Zebak, stream) to take
their source in deep, lateral, ditch-like valleys, which, closely
underlying these folds, have been reshaped and altered by ages of
denudation and seismic destruction.
Public-domain text, read in full here on John Shaqi.
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