Ellsworth American. [volume] (Ellsworth, Me.) 1855-current, 1907-03-06
A LANDOF BLIZZARDS|
FIERCE GALES THAT SWEEP AND
WRECK sEISTAN.
THESE TERRIFIC wrNDsroRMs ALWAYS
BLOW FROM THE SAME
pIREcrIoN.

| Every ont VINO mas Ni$iteu SeiStan OF
written about Seistan has mentioned
It's celebrated wind. called the ''bad-i-
sad -o-ulsg rox.~ or Wind OF 12O days.
which blows In the summer. Few OF
these have had the misfortune to ex-
perience IL. but as we went through
two seasons Of this wind we are able
to say something about 1t. Ii more
than justifics its reputation II sets In
at the end OF May or the middle Of
June and Flows with appalling VIC
lence and with little or no cessation till
about the end Of September. II always
blows from one direction. little west
OF north, and reaches velocity of
more than seventy miles an hour. II
creates a pandemonium OF noise. sand
and dust aud for time gets on ones
nerves. but II Is In reality blessing in
disguise. for II blows away the insects
which from April 70 June make life in
Seistan a perfect purgatory. mitigatcs
the awful summer heat and clears the
country Of typnas. smallpox and other
diseases rife In the country In May and
June One would think this I'D day
wind enough. but violent winds prevail
all through the winter from December
20 April. and billiards. are of constant
occurrence. These winds always come
from the same direction. The winter
blizzards are terrible. aud the wind at
tains a terrific velocity. In a blizzard
at the end Of March the thermometers
registered a maximum of 40 miles an
hour. The average velocity for whole
sixteen hours was more than eighty.
eight miles an hour.
The extraordinary frequency and vio-
ience Of the Seislan wind and the reg
uiarify with which IL blows from the
same quarter are very remarkable.
That il 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 a 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 not a single
tree exists.
The present villages and habitaticns
are all built with their backs present
ing lines OF dead walls on the wind
ward side. The OLD ruins are oriensed
ut exactly the same angle on account
OF the wind. The effect of wind Is ev-
erywhere visible on these ruins. Their
bases are uBdereut 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 inaahlIants for the lower
courses of their buildings and the ex-
IRENE hardness and durability OF the
SeIstan soil when made into the sun
dried bricks of which the upper por-
tons OF the ruins are composed. have
withstood the destructive effect Of the
wind In a 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 In 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. big and fiourishing village.
built on the south side OF a high .idge
for protection from the wind. Before
we left the sand had attacked that
ridge. surmounted IL and buried the
village. forcing the inhabitants to build
q new village elsewhere. An example
Of still greater rapidity was afforded
at the village OF Kilaikohna. Up to
June. 1904. this village had a large.
deep pond on its northern side. BY
Superintendent Is. less than three
montbs-this deep pond was converted
into sand hill some ten feet high.
The wind, however, did not coniine
its energy to burying only. While u
covers some tracts deep in sand. il also
sweeps other tracts clear Of sand. rem
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