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File:Middle East topographic map-blank.svg. Size of this PNG preview of this SVG file: 800 × 501 pixels. Other resolutions: 320 × 200 pixels | 640 × 400 pixels | 1,024 × 641 pixels | 1,280 × 801 pixels | 2,560 × 1,602 pixels | 3,097 × 1,938 pixels. This is a file from the Wikimedia Commons. Information from its description page there is ...
Al-Mahara, Yemen. Coordinates. 17°20′25″N 52°26′38″E / 17.34028°N 52.44389°E / 17.34028; 52.44389. Depth. 112 m (367 ft) The Well of Barhout (also nicknamed Well of Hell) is a sink hole in Al-Mahara, Yemen. It has a circular entrance that measures about 30 m (100 ft) wide at the surface, and it is 112 metres (367 ft) deep.
Göbekli Tepe. Göbekli Tepe (Turkish: [ɟœbecˈli teˈpe], [2] 'Potbelly Hill'; [3] Kurdish: Girê Mirazan or Xerabreşkê, 'Wish Hill' [4]) is a Neolithic archaeological site in the Southeastern Anatolia Region of Turkey. The settlement was inhabited from around 9500 BCE to at least 8000 BCE, [5] during the Pre-Pottery Neolithic.
The gas crater is near the village of Darvaza in the middle of the Karakum Desert. Located about 260 kilometres (160 mi) north of Ashgabat, the capital of Turkmenistan, it has a diameter of 60–70 metres (200–230 ft)[4][5] and a depth of about 30 metres (98 ft). [6] Another nearby gas crater is fenced off and has a distinct odor.
The Mariana Trench is an oceanic trench located in the western Pacific Ocean, about 200 kilometres (124 mi) east of the Mariana Islands; it is the deepest oceanic trench on Earth. It is crescent-shaped and measures about 2,550 km (1,580 mi) in length and 69 km (43 mi) in width. The maximum known depth is 10,984 ± 25 metres (36,037 ± 82 ft ...
File:Middle East topographic map-blank 3000bc crop.svg. Size of this PNG preview of this SVG file: 790 × 600 pixels. Other resolutions: 316 × 240 pixels | 632 × 480 pixels | 1,011 × 768 pixels | 1,280 × 972 pixels | 2,560 × 1,944 pixels | 1,426 × 1,083 pixels. Original file (SVG file, nominally 1,426 × 1,083 pixels, file size: 10.01 ...
The Qattara depression is a region that lies 60 m (200 ft) below sea level on average and is currently a vast, uninhabited desert. Water could be let into the area by connecting it to the Mediterranean Sea with tunnels and/or canals. The inflowing water would then evaporate quickly because of the desert climate.
The Jordan river, in the middle of the Jordan valley, was the border between these two entities. This agreement split the Jordan valley, which during Ottoman times was under a single administration, to two distinct entities. Following the division, the concept of an east and west bank of the Jordan, as separate territorial units took hold.
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