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Map showing the extent of Mesopotamia. The geography of Mesopotamia, encompassing its ethnology and history, centered on the two great rivers, the Tigris and Euphrates.While the southern is flat and marshy, the near approach of the two rivers to one another, at a spot where the undulating plateau of the north sinks suddenly into the Babylonian alluvium, tends to separate them still more ...
Overland routes in Mesopotamia usually follow the Euphrates because the banks of the Tigris are frequently steep and difficult. The climate of the region is semi-arid with a vast desert expanse in the north which gives way to a 15,000-square-kilometre (5,800 sq mi) region of marshes, lagoons, mudflats, and reed banks in the south.
The south-central Levant experienced two phases of dry climate punctuated by a wet interval in between and thus the 4.2 ka event in the region has been termed a W-shaped event. [ 44 ] Enhanced dust flux coeval with δ 18 O peaks is recorded in Mesopotamia from 4260 to 3970 BP, reflecting intense aridity. [ 45 ]
The Mesopotamian shrub desert is a transitional region between the semi-arid steppes of northern Mesopotamia and the Levant to the north, and the Arabian Desert to the south. The western portion of the ecoregion consists of rocky or sandy plateaus, including the Syrian Desert in southern Syria and northern Jordan, and a portion of the Harrat al ...
Xeric shrublands can experience woody plant encroachment, which is the thickening of bushes and shrubs at the expense of grasses. [5] This process is often caused by unsustainable land management practices, such as overgrazing and fire suppression, but can also be a consequence of climate change.
Map of the Fertile Crescent A 15th century copy of Ptolemy's fourth Asian map, depicting the area known as the Fertile Crescent. The Fertile Crescent (Arabic: الهلال الخصيب) is a crescent-shaped region in the Middle East, spanning modern-day Iraq, Israel, Jordan, Lebanon, Palestine, and Syria, together with northern Kuwait, south-eastern Turkey, and western Iran.
The Babylonian Map of the World (also Imago Mundi or Mappa mundi) is a Babylonian clay tablet with a schematic world map and two inscriptions written in the Akkadian language. Dated to no earlier than the 9th century BC (with a late 8th or 7th century BC date being more likely), it includes a brief and partially lost textual description.
Mesopotamia does not have local, high-resolution climate proxy records such as the Soreq Cave does. This makes it difficult to reconstruct the region's past climate. Even so, it is known that the environment during the sixth and fifth millennium BC was not the same as today. A more temperate climate settled in around 10,000 BC.