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Topography and Geology of the Middle East

Apr 25, 2025

Lecture Notes: Topography of the Greater Middle East

Overview

  • Discussion of the landscape of the Middle East.
  • Region characterized by:
    • High, rugged mountain ranges.
    • Uplifted plateaus.
    • Vast tracts of dry lowland areas.

North Africa

  • General Characteristics:

    • Huge desert (Sahara) and semi-arid regions with minimal relief.
    • Most areas below 500 meters above sea level.
    • Vast coastal plains extending hundreds of miles inland.
    • Flat terrain allows easy traversal barring extreme temperatures.
  • Notable Features:

    • Tibesti Mountains: Northern Chad, highest point 3,445 meters.
    • Atlas Mountains: A series of ranges (Anti-Atlas, High Atlas, etc.) in Morocco, Algeria, Tunisia.
      • Peaks between 3,000 to 4,000 meters.
      • Impacts local climate by creating wetter, Mediterranean-like coastal regions.
      • Cultural and economic exchanges with Mediterranean Europe.

Arabian Peninsula

  • Escarpment: A geological feature causing a quick elevation jump, notably along the west coast.

    • Part of the Sarawat Mountain range in Saudi Arabia and Yemen.
    • Creates Mediterranean climate on western coastal fringe (Hejaz region).
    • Includes cities like Mecca and Medina.
  • Central Plateau: Uplifted and tilting towards the Persian Gulf.

    • Low-lying areas (below 100 feet above sea level) in eastern regions (Qatar, UAE, etc.).

Turkey and Iran

  • Turkey:

    • Anatolia Plateau: High central plateau with narrow coastal plains.
    • Mountain Ranges: Pontic (north), Taurus (south), home to Mount Ararat (5,127 meters).
  • Iran:

    • Zagros and Elburz Mountains:
      • Significant ranges influencing cultural and historical separations.
      • Zagros separates Iran from Iraq and the Arabian world.
    • Iranian Plateau: Uplifted area with varied climates and biomes.

Geologic Activity

  • Plate Tectonics: Influence on mountain formation and seismic activity.

    • Arabian plate moving into the Eurasian plate (Zagros Mountains).
    • Anatolian plate squeezed between larger plates, causing tectonic activity.
    • Earthquakes common in Turkey and Iran.
  • Rift Valleys:

    • Red Sea and Jordan Rift Valley: Part of African and Arabian plates pulling apart.
    • Dead Sea is the lowest point on Earth's surface (427 meters below sea level).
    • Red Sea widening due to plate movements.

Conclusion

  • The physical geography and topography of the Middle East profoundly influence cultural, climatic, and historical interactions within the region.