Makhtesh

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Image:Makhtesh Sinai.jpg
One of the two makhteshim in Sinai
© DigitalGlobe

A makhtesh (Hebrew: מכתש‎, plural: מכתשים - "makhteshim") is a geological phenomenon in which a hard outer layer of rock covers softer rocks. The erosion process destroys the soft minerals relatively fast, and they are washed away from under the harder ones. The harder rocks eventually collapse under their own weight — the result is a crater-like valley structure.

This phenomenon is often said to be unique to the Negev desert (Israel) and the Sinai Peninsula (Egypt). However, similar features exist also in Turkmenistan (Yor-oilan-duz depression in Badkhyz Highlands) and Iran.

Although the Hebrew term "makhtesh" is usually translated as "crater", there is a difference between the two: Makhteshim are formed by water erosion whereas craters are formed by the impact of a meteor or volcanic eruption. A more accurate translation is "erosion cirque." [1]

In the Negev, there are 5 makhteshim: Makhtesh Ramon, Makhtesh Gadol ("Large Makhtesh"), Makhtesh Qatan ("Small Makhtesh"), and two tiny makhteshim on Mount Arif.

In the cases in the Negev and Sinai, the hard rocks are limestone and dolomites, while the inner softer rocks are chalk or sandstone. [2]

Though in most cases a makhtesh has only one drainage system, Makhtesh Ramon has three.

The two makhteshim in Sinai have no names for the basin, but the their walls have several names - like Jabal al-Manzur or Gebel Maghara.

[edit] References

  • Mazor, Emanuel and Krasnov, Boris, editors "The Makhteshim Country - a Laboratory of Nature". Pensoft Publishers, Sofia, 2001: , ISBN: 954-642-135-9, 411 pages
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de:Erosionskrater

he:מכתש אירוזי

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