A makhtesh (Hebrew: מַכְתֵּשׁ‎ ([maχˈteʃ]), Hebrew plural: מַכְתְּשִׁים‎ ([ˈmaχteˌʃim]Makhteshim) is a geological landform considered typical for the Negev desert of Israel and the Sinai peninsula of Egypt. A makhtesh has steep walls of resistant rock surrounding a deep closed valley, which is usually drained by a single wadi. The valleys have limited vegetation and soil, containing a variety of different colored rocks and diverse fauna and flora. The best known and largest makhtesh is Makhtesh Ramon.

Although commonly referred to as "craters", these formations are "erosion cirques" (steephead valleys or box canyons). Craters are formed by the impact of a meteor or volcanic eruption, whereas makhteshes are created by erosion.[1]

The word makhtesh is the Hebrew word for a mortar grinder (מַכְתֵּשׁ‎).[2] The geological landform was given this name because of its similarity to a grinding bowl.

Where a hard outer layer of rock covers softer rocks, erosion removes the softer minerals relatively quickly, and they are washed away from under the harder rock. The harder rocks eventually collapse under their own weight, and a crater-like valley structure is formed. In Negev and Sinai makhteshes, the hard rocks are limestone and dolomites, while the inner softer rocks are chalk or sandstone.[3]

The center of the Negev is dominated by northeast-southwest anticlinal ridges. The crests of four ridges host five deep valleys surrounded by steep walls. The upper half consists of hard limestone and dolomite, and the bottom of friable sandstone. Each valley, known as a makhtesh, is drained by a narrow river bed.[4]

The Negev has five makhteshes: Makhtesh Ramon, Makhtesh Gadol, Makhtesh Katan, and two small makhteshes on Mount Arif, south of Makhtesh Ramon.

The two makhteshes in Sinai, Egypt, have no names for the basin, but their walls have several names including Jabal al-Manzur or Gebel Maghara.[citation needed]

Many similar geological formations are also found in Wadi Rum in southern Jordan.[citation needed]