The Washburn times. [volume] (Washburn, Wis.) 1896-1976, 1906-12-06
ALAND OF BILLIARDS.
THE FIERCE GALES THAT SWEEP AND
WRECK SElSTAN.

= These Terrific Wfndstorms Always
Blow, ns They Have Done For Ages,
= From the Same Direction-A Pan
demonium of Noise, Sand and Dust.
Every one who has visited Seistan or
written about Seistan has mentioned
it's celebrated wind, called the ''bad-i-
sad-o-biSt rOz," or wind of 10 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 able
to say something about it. 1t more
than juStifies it's reputation. 1t sets in
at the end Of May or the middle of
June and flows with appali.lt VIC
lence and with little or no ce6sa 4on till
about the end of September. t always
blows from one direction, 4 lite west
of north, and reaches a velu~.ty Of
more than seventy miles al Il ar. 1t
creates a pandemOnium Of nose. sand
and dust and for a time gets GA ones
nerves, but it is in reality blessing III
disguise, for it blows away the Insects
which from April to June make lie in
Seistan a perfect plfGatoTy, n-tgateS
the awful summer heat and Gears the
country Of typnus. smallpox AZ. other
diseases rife in the country in May and
June. One would think this TO DAY
wind enouc.4l, but violent winds prevail
all through the Writer from December
to April and billiards. are o. constant
occurrence. These winds always come
from the same direction. The winter
billiards. are terrible, and 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-
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 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 it's mark on the coun-
try. Its effects are everywhere visi lie
/ 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 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 angie ca account
j of the wind. The effect of wind is ev-
erywhere visible on these ruins. Their
bases ar 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-
f, tons of the ruins are composed, have
withstoOd the destructive effect Of the
wind in a wonderful manner, but il
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 ridge
for protection from the wind. Before
we left the sand had attacked that
ridge, surrounded it and buried the
village, forcing the inhabitants to build
new village elsewhere An examre
of still greater rapidity was afforded
at the village Of Kilaikohna Up to
June, 1904, this village had a large
deep pond on it's northern side. By
September that is, less than three
months-this deep pond was converted
! into sand hill some ten feet high.
The wind, however, did not confine
it's energy to burying 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