Americus times-recorder. [volume] (Americus, Ga.) 1891-current, 1906-11-29
A LAND OF BLIZZARDS
THE FIERCE GALES THAT SWEEP AND
WRECK SEISTAN.

These Terrific WindstOrms Away
Blow, as They Have Done For Ages
From the Same DirectiOn-A Pan
denIOniUm of Noise, Sand and Dust.
| Every one who has visited Seistan o.
| written about Sestan has mentioned
its celebrated wind, called the 'bad-i
sad-o-bist roZ," or wind of 100 days
which blows in the summer. Few Of
these have had the misfortune to eX
perience it, but as we went through
two seasons of this wind we are ablt
to say something about it. 1t more
than iustifies its reputation. 1t sets il
at the end of May or the middle OF
| June and blows with appalling vio
lence and with little or no cessation til
about the end of September. 1t always
blows from one direction, a little west
of north, and reaches a velocity OF
more than seventy miles an hour. Ii
creates Il pandemonium of noise, sane
and dust and for a time gets on ones
nerves, but it is in reality a blessing il
disguise, for. it blows away the insects
which from April to June make life in
Seistan a perfect purgatory, mitigates
the awful summer heat and clears the
country of typhus, smallpox and other
diseases rife i'll the country in May and
June. One would think this 120 day
wind enough, but violent winds prevail
all through the winter from December
to April, and blizZards are of constant
occurrence. These winds always come
| from the same direction. The winter
blizzards are terrible, and the wind at
tains Il terrific velocity. In a blizzard
at the end of March the thermometers
| registered maximum of 120 miles an
hour. The average velocity for whole
sixteen hours was more than eighty
eight miles an hour.
The extraordinary frequency and VIC.
lence of the SeiStan wind and the reg.
ularity with which it blows from the
same quarter are very remarkable.
| That it has blown from the same quar-
ter in past ages is proved by the fact
that all the ruins of Seistan are built
at the same angle, with their front and
back walls at right angle to the
! wind and their side walls at the same
angle as the wind. No wind can blow
with such violence and frequency
without leaving its mark on the coun-
try Its effects are everywhere visible
| in Seistan. Everything looks wind
swept and wind stricken Over the
greater part of the country nOr Il single
| tree exists.
The present villages and habitations
| are all built with their backs present
| ing lines of dead walls on the wind
ward side. The Old ruins are oriented
at exactly the same angle on account
of the wind. The effect Of wind is ey-
erywhere visible on these ruins. Their
bases are undercut by wind as though
by water action The thickness of the
walls, the excellent quality of the
burned bricks made and used by the
ancient inhabitants for the lower
courses of their buildings and the ex-
treme hardness and durability of the
Seistan soil when made into the sun
dried bricks Of which the upper por.
tions of the ruins are composed, have
withStOod the destructive effect of the
wind in wonderful manner. but in
the older ruins we often find that the
walls facing the wind have entirely
disappeared. and only the side walls re.
main, while id still older ruins only
one or two solitary pinnacles remain to
mark what were once large, massive
and extensive buildings,
The wind has buried large tracts of
The country under sand. Many of the
old ruined towns are wholly or partly
buried In sand, and this burying process
goes on all the year and every year and
Is covering up not only valuable lands,
but inhabited villages. In Seistan. as
elsewhere, the invading army of sand
is preceded by lines of skirmishers in
the form of travelling "burkhans,"
horseshoe shaped sand hills. which
steadily advance until they meet some
obstacle which retards them until the
reserves come up to their support and
bury all before them under Hills Of sand.
On our arrival in Seistan we found
Kilainau. a big and fourishing village,
built on the south side of high "idge
for protection from the wind Before
we left The sand had attacked that
ridge, SUrmOunted it and buried the
village foGcing the Inhabitants t. build
new village elsewhere An example
of still greater rapidity was afforded
at the village of Kilaikohna Up to
June, 1904. this village had Il large
deep pond on its northern side. BY
Superintendent is. less than three
months-this deep pond was converted
into sand hill some ten feet high.
The wind, however. did not confine
its energy to buryiug only While it
covers some tracts deep in sand, it also
sweeps other tracts clear of sand, rem
dering valuable land available for cul-
tivation and exposing long buried ruins
once more to view These are. how
ever only the milder effects of wind
action The Seistan wind in it's more
destructive moods has in -places re-
moved not only sand from place to
place. but has secured away the whole
face of the country Everywhere we
find the sides and banks of the canals
which irrigated the lands on which the
dwellers of Athe old ruins depended left
standing like walls high above the pres
ent surface of the surrounding land
These banks. having been hardened by
water, have withstood the action of the
wind better than the surface of the
land. which has all been blown away
TO depth of several feet. This depth
IL nleees is very considerable and we
~ Dangerc
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