Wadi Hamra (Gilf Kebir)

Wadi Hamra is a significant wadi (dry riverbed) located within the Gilf Kebir plateau in southwestern Egypt. The Gilf Kebir is a sandstone plateau characterized by dramatic cliffs, deep wadis, and rock art sites, situated in the extremely arid Libyan Desert.

Wadi Hamra, meaning "Red Valley" in Arabic (referencing the color of the sandstone), is notable for its size and accessibility compared to other wadis on the plateau. It acts as a natural corridor through the Gilf Kebir, providing a relatively easier route for travel and exploration. The wadi floor is typically sandy and gravelly, with occasional vegetation adapted to the harsh desert environment.

Historically, Wadi Hamra served as a crucial path for nomadic groups and traders traversing the region. Today, it attracts archaeologists, geologists, and adventurous tourists interested in exploring the unique landscape and ancient history of the Gilf Kebir. The area is known for its rich archaeological record, including rock engravings and evidence of prehistoric human habitation, offering insights into the past environment and human activity in this now hyper-arid region. Permission from the Egyptian authorities is generally required to visit and conduct research in the Gilf Kebir and Wadi Hamra due to its remoteness and sensitivity.