[1] Mil plain is located in the southwestern part of the Kur-Araz lowland, where the Kura and Araz rivers meet.
The absolute altitude decreases about 8 m to north (to the Kura River) and varies from 200 to 250 to the west (harami plain).
Seismic activity is high as the plain is in the convergent border the Alpine-Himalayan orogenic belt.
Wormwood, gavan, kangiz, camel thorn, saline plants constitute the majority of the vegetation.
The maximum annual temperature is 44380 C. The cold air masses reaches the plain in the autumn after November 20.
Average relative humidity of the air varies between 58-82%.The annual amount of precipitation is 312 and evaporation is 1000 mm.
The prevailing winds blow from the east southeast, with average annual speed not exceeding 2.2 m / sec.
The rivers of the past and modern times has led to formation diverse relief forms such as dry valleys, lakes and ponds, etc.
Aggol, Sarisu, and some other small lakes created by mainly Kura River.