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Matthew Campbell
Matthew Campbell

The Best Car Wash Solutions from Grass Azerbaycan

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He specified that several residents of Tegh village went to their property lands to collect the grass they had harvested on June 23 and 24. When they were about 300 meters away from the Azerbaijani position in the administrative territory of Tegh community, they noticed that 5 Azerbaijani armed servicemen were approaching them shouting aggressively.

The villagers were able to collect the grass only on June 27, when the commanders of the 1st Army Corps of the Armenian Armed Forces, the heads of the local self-government bodies went to that place.

The next zone to the north is the steppe zone [14, p. 94-95], the grassland known to medieval travelers as the "wilderness" [23, p. 112] and home to the nomadic population of the Golden Horde and the so-called "empires of the steppe" throughout history. The steppe begins in the east in Manchuria and extends west through Mongolia in a band roughly 300-1100 km wide to as far west as Romania, beyond where the Danube River empties into the Black Sea, and the Alfold or Great Hungarian Plain. This zone extends westward from Mongolia in only two spots: the elevated southern steppe passing through the Dzungar Gate [14, p. 50] and encircling Lake Issyk-kul (this area formed a part of the Chagatay Khanate) and the northern steppe gate passing through the Altay Mountains along the Black Irtysh River to Lake Zaysan and then continuing northwest along the Irtysh River. One must also add to this the figures for the adjacent mixed forest-steppe north of the steppe zone, since this transition zone of grasslands and trees roughly 200-500 km in width [14, p. 93-94] often offered easy access for nomads, though there were also sedentarists inhabiting this zone.

Additional factors to consider for the steppe and forest-steppe zones include the length and depth of winter snow cover, which are critical factors for the pastoral nomad and his herds [18, p. 22ff.]. To the east of the Ural Mountains the grass of the northern steppe can be covered with snow for up to 180 days per winter, and this far east even the southern steppe of the Golden Horde (not including the elevated southern steppes which would fall under the Chagatay Khanate) can be covered with snow over 120 days per winter. On the other hand the grass of the lush northern part of the steppe zone west of the Urals is covered with snow over 140 days per winter, while along the Black Sea the southern edge of the steppe this figure drops to as little as 40 days. Around Azerbaycan and in the Crimea the duration of winter snow cover can be even less [14, p. 85; 2, p. 117].

A related consideration is the depth of winter snow cover. Although the horses native to this area have adapted to snow up to about 40 cm in depth, cattle, sheep, and goats can survive in snow-covered pasturage only if there is tall grass and it is not covered by snow deeper than about 20 cm2. For this reason it is also worth considering the data on the depth of winter snow cover: the line of 20 cm mean maximum depth of snow cover crosses the Volga River south of the great bend of the Volga, thus including within it most of the southern-most sub-zone of steppe and all of the dry steppe. On the other hand the situation further to the east is far worse: the line of 20 cm mean maximum depth of snow cover dips somewhat to the southeast, skirting the Aral Sea and running parallel to the Syr Darya [14, p. 83], which can only mean that all the sub-zones of steppe east of the Ural Mountains fall north of this crucial line.

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The significance of this amount of precipitation is better understood if it is considered that during this period the Pontic steppe (north of the Black Sea) was receiving rainfall equivalent to what the southern part of the forest zone receives [38, p. 15]. Additional supporting evidence for such a scenario in the south in this period is seen in the decline of the upper limit of the food line in the Caucasus mountains, which would correspond to a .7-.8 degree C drop in temperature or to a 250 mm rise in precipitation [30, p. 32]. Of course, it is not clear for how large a territory one can generalize based on the data for Lake Saki, but one may assume that such major increases in precipitation would have led to increased growth in grasses in the drier southern zones of semi-desert and dry steppe; conversely the end of this wet period would lead to decreased growth in grasses in those zones.


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