Bazman Do (II) Thermal Spring – Iran Shahr

The said tower is at a distance of 8 miles east of Chechoo hillocks. The structure resembles a minaret and has been constructed on an elevation. From this point a birds eye view of the surroundings is possible, as the tower offered an excellent view. It is said that in past, at times of war or...

The Bazman Village lies in the northwest of Iran Shahr and the above mentioned spring is located in the northwest of this village. This spring gushes out from a crevice in the earth and a pool has formed here in which the inhabitants bath. Due to volcanic activities the water of this spring is...

These mountains are located to the northeast of Challeh-e-Jazmoorian, and its height is approximately 3,489 m. and extends towards the west, adjoining the Barez range in the province of Kerman. This mountain segregates the Challeh-e-Loot from Jazmoorian, and is covered with molten volcanic...

The said castle was a seat of power or command in the past in Baluchestan. It is a brick construction, built during the reign of Naseredin Shah by Firooz Mirza in the year 1264 AH.

The remnants of crypts or towers of silence (Sokoot) can be observed in various parts of the province. Till centuries after the Arab conquests, the Zoroastrian preaching and religion held good in Sistan. Vestiges of these towers (of silence ) or fire-temples of the province are reminders of such...

The Bampour River takes its source in the summits to the east of Iran Shahr and is a factor regarding agriculture in the territory of Iran Shahr and Bampour. A diverting dam has been constructed here. After the river flows through the plains of Bampour it deposits itself in the seasonal lake of...

The Bahookalat River is one of the gushing rivers of the region of Sistan Va Baluchestan, and is one of the major factors of livelihood and flourishment in the south of this area. This river collects the surface waters from vast areas of south of the townships of Iran Shahr and Chabahar, before...

The said mountains are located to the south of the Sistan Mountains and extend between the Challeh-e-Loot, Jazmoorian, and the desert area of Mashekl and the Oman Sea.

This spring lies on the Bazman-Delqan-Hoodian Road and the water of this spring gushes out of a crevice from the volcanic rocks of the Quaternary period. This water is of a chloro-sulfate category in composition with different virtues.