Ziyaret Tepe and its neighboring archaeological sites are located within the broad alluvial plain carved by the Tigris River as it flows through Miocene-Pliocene tablelands composed of limestone, shale, and conglomerate bedrock. Ziyaret Tepe sits atop one of the Pleistocene terraces which flank the river. The site sits approximately 10m above the flood plain of the modern Tigris River.

The scenery near Ziyaret Tepe alternates between hills with an elevation of 600m above mean sea level and wide, open plateaux at an elevation of roughly 540m. The latter are commonly irrigated for cotton cultivation in the present day. This topography probably reflects the underlying rocks: conglomerates, limestones and young basalt caprock are more resistant to erosion in this climate.

Of particular importance to ancient inhabitants of Ziyaret Tepe was access to the Tigris River and to the small streams which serve as its perennial tributaries. The river served both as a source of water for consumption and agriculture, as well as means of transport. This region has been of particular importance during antiquity because it is located along a major confluence of trade routes connecting the Mesopotamian lowlands to the south with the Anatolian highlands of the Taurus Mountains to the north.

In the present day, this part of southeastern Turkey has hot summers and cold winters with an average annual rainfall of about 580mm which falls almost exclusively in the winter months and is enough to sustain a vegetation typical of the Oro-Mediterranean and steppe forest. Cuneiform tablets found at the site tell us that wheat formed a major crop in the area in the mid-1st millennium BC. Today the natural flora of the area has been perturbed by farming of crops, including cotton and tobacco, which require intensive irrigation efforts within the Tigris River valley.