fbpx
Wikipedia

Makhtesh Ramon

Makhtesh Ramon (Hebrew: מכתש רמון; lit. Ramon Crater/Makhtesh; Arabic: وادي الرمان; lit. The Ruman Wadi) is a geological feature of Israel's Negev desert. Located some 85 km south of the city of Beersheba, the landform is the world's largest "erosion cirque" (steephead valley or box canyon). The formation is 40 km long, 2–10 km wide and 500 meters deep, and is shaped like an elongated heart. Despite its appearance it is not an impact crater from a meteor nor a volcanic crater formed by a volcanic eruption.

Makhtesh Ramon
The "crater" is 40 km long, 2–10 km wide and 500 meters deep.
Location of Maktesh Ramon
LocationSouthern, Israel
Coordinates30°34′43″N 34°49′4″E / 30.57861°N 34.81778°E / 30.57861; 34.81778
Length40 km (25 mi)
Width2–10 km (1.2–6.2 mi)
Map of Makhtesh Ramon

The only settlement in the area is the small town of Mitzpe Ramon (מצפה רמון, "Ramon Lookout") located on the northern edge of the depression. Today the area forms Israel's largest national park, the Ramon Nature Reserve.

Formation edit

 
A Nubian ibex on the edges of Makhtesh Ramon

Hundreds of millions of years ago, the Negev desert was covered by the Tethys ocean. Slowly, it started to recede northwards leaving behind a hump-shaped hill. The hump was slowly flattened by water and climatic forces. Approximately five million years ago, the Arava Rift Valley was formed, with rivers changing their courses, carving out the inside of the crater which was a softer rock than that overlying. The crater bottom continued to deepen at a much faster rate than the surrounding walls, which gradually increased in height. As the crater deepened, more layers of ancient rock were exposed with rocks at the bottom of the crater being up to 200 million years old. Today, the crater is 500 metres deep with the deepest point being Ein Saharonim [he] (Saharonim Spring). This spring serves as the sole natural water source within the crater, supporting a significant portion of its wildlife population,including onagers and ibex.

Geology edit

Makhtesh Ramon contains a diversity of rocks including clay hills known for their fantastic red and yellow colors and forms. Impressive mountains rise at the borders of the crater - Har Ramon (Mt. Ramon) at the southern end, Har Ardon [he] (Mt. Ardon) at the north-eastern end, and two table mountains - Har Marpek (Mt. Marpek - "Elbow"), and Har Katum (Mt. Katum - "Cropped") along the southern wall. The hills to the north-eastern edge of the makhtesh were once entirely covered by spiral ammonite fossils, ranging from the size of snails to that of tractor wheels although these have mainly been extracted so only smaller fossils can be found here today.

Giv'at Ga'ash, a black hill in the north of the makhtesh was once an active volcano which erupted thousands of years ago and caused it to be covered in lava which quickly cooled in the open air, converting it into basalt. Limestone covered by basalt can also be found in smaller black hills in the southern part of the makhtesh, including Karnei Ramon.

Shen Ramon (Ramon's Tooth) is a rock made of magma which hardened whilst underground. It later rose up through cracks in the Earth's surface, and today stands in striking contrast with the nearby creamy coloured southern wall of the crater, as a black sharp-edged rock.

In the centre of the makhtesh is HaMinsara (The Carpentry Shop), a low hill made up of columnar jointed sandstone - polygonal prismatic columns of quartzite.

The pteriidan bivalve Family Ramonalinidae is found in early Middle Triassic rocks of Makhtesh Ramon and was named after this feature.

Nahal Ardon in the east of the makhtesh contains several vertical dikes. Occasional geodes of celestine can be found next to some of them.[1]

Fauna edit

 
A Nubian ibex on the edges of Makhtesh Ramon

The Asiatic wild ass has been reintroduced to Makhtesh Ramon. In 1995 the population had increased to 40 adults in the area. The animals are hybrids of two different subspecies of the Asian Wild Ass. It is derived from the Turkmenian kulan (E. h. kulan) and the Persian onager (E. h. onager). The original subspecies, the Syrian wild ass (E. h. hemippus), is completely extinct.[2]

Other larger mammals of the area include Nubian ibex, Dorcas gazelles, striped hyenas, Arabian wolves, caracals, golden jackals, and reintroduced Arabian oryx.[3] Historically, the area was home to Arabian leopards. However, they are likely extinct in Israel.[4]

History edit

 
Wadi Raman in the 1944 Survey of Palestine map

The ruins of a large prehistoric stone structure known as Khan Saharonim [he] are found in the makhtesh, as it lies along the ancient Incense Route, a trade route used by the Nabataeans 2,000 years ago. These ruins acted as a way station for the traders and their animals (khan is the Arabic word for a caravanserai) as they proceeded further westwards to the Mediterranean seaport city of Gaza.

Located atop the northern cliff of the crater, one can find Metzad Mahmal, the remnants of a stronghold employed by the Nabataeans and the Romans to safeguard the Incense Route. The site was excavated by several archaeologists, and declared a World Heritage Site by UNESCO in 2005.

 
Wide panorama of the Makhtesh Ramon crater, Israel

Gallery edit

References edit

  1. ^ Michael Anenburg; Or M. Bialik; Yevgeny Vapnik; Hazel J. Chapman; Gilad Antler; Yaron Katzir; Mike J. Bickle (2014). "The origin of celestine–quartz–calcite geodes associated with a basaltic dyke, Makhtesh Ramon, Israel". Geological Magazine. 151 (5): 798–815. Bibcode:2014GeoM..151..798A. doi:10.1017/S0016756813000800.
  2. ^ David Saltz David, Mary Rowen, Daniel I. Rubenstein: The Effect of Space-Use Patterns of Reintroduced Asiatic Wild Ass on Effective Population Size. Conservation Biology, Vol. 14, No. 6, 2000
  3. ^ "Makhtesh Ramon Visitors Center". Israel Nature and Parks Authority. Retrieved 2023-03-25.
  4. ^ Stein, A.B., Athreya, V., Gerngross, P., Balme, G., Henschel, P., Karanth, U., Miquelle, D., Rostro-Garcia, S., Kamler, J.F., Laguardia, A., Khorozyan, I. & Ghoddousi, A. 2020. Panthera pardus (amended version of 2019 assessment). The IUCN Red List of Threatened Species 2020: e.T15954A163991139. doi:10.2305/IUCN.UK.2020-1.RLTS.T15954A163991139.en. Accessed on 25 March 2023.

External links edit

  • Ramon Crater on Google Maps
  • Ramon Crater Detailed trail and hiking info. from
  • , at the Israel Nature and Parks Authority's website.
  • Mazor, Emanuel and Krasnov, Boris, editors "The Makhteshim Country - a Laboratory of Nature". Pensoft Publishers, Sofia, 2001, ISBN 954-642-135-9, 411 pages

makhtesh, ramon, hebrew, מכתש, רמון, ramon, crater, makhtesh, arabic, وادي, الرمان, ruman, wadi, geological, feature, israel, negev, desert, located, some, south, city, beersheba, landform, world, largest, erosion, cirque, steephead, valley, canyon, formation,. Makhtesh Ramon Hebrew מכתש רמון lit Ramon Crater Makhtesh Arabic وادي الرمان lit The Ruman Wadi is a geological feature of Israel s Negev desert Located some 85 km south of the city of Beersheba the landform is the world s largest erosion cirque steephead valley or box canyon The formation is 40 km long 2 10 km wide and 500 meters deep and is shaped like an elongated heart Despite its appearance it is not an impact crater from a meteor nor a volcanic crater formed by a volcanic eruption Makhtesh RamonThe crater is 40 km long 2 10 km wide and 500 meters deep Location of Maktesh RamonLocationSouthern IsraelCoordinates30 34 43 N 34 49 4 E 30 57861 N 34 81778 E 30 57861 34 81778Length40 km 25 mi Width2 10 km 1 2 6 2 mi Map of Makhtesh RamonThe only settlement in the area is the small town of Mitzpe Ramon מצפה רמון Ramon Lookout located on the northern edge of the depression Today the area forms Israel s largest national park the Ramon Nature Reserve Contents 1 Formation 2 Geology 3 Fauna 4 History 5 Gallery 6 References 7 External linksFormation edit nbsp A Nubian ibex on the edges of Makhtesh RamonHundreds of millions of years ago the Negev desert was covered by the Tethys ocean Slowly it started to recede northwards leaving behind a hump shaped hill The hump was slowly flattened by water and climatic forces Approximately five million years ago the Arava Rift Valley was formed with rivers changing their courses carving out the inside of the crater which was a softer rock than that overlying The crater bottom continued to deepen at a much faster rate than the surrounding walls which gradually increased in height As the crater deepened more layers of ancient rock were exposed with rocks at the bottom of the crater being up to 200 million years old Today the crater is 500 metres deep with the deepest point being Ein Saharonim he Saharonim Spring This spring serves as the sole natural water source within the crater supporting a significant portion of its wildlife population including onagers and ibex Geology editMakhtesh Ramon contains a diversity of rocks including clay hills known for their fantastic red and yellow colors and forms Impressive mountains rise at the borders of the crater Har Ramon Mt Ramon at the southern end Har Ardon he Mt Ardon at the north eastern end and two table mountains Har Marpek Mt Marpek Elbow and Har Katum Mt Katum Cropped along the southern wall The hills to the north eastern edge of the makhtesh were once entirely covered by spiral ammonite fossils ranging from the size of snails to that of tractor wheels although these have mainly been extracted so only smaller fossils can be found here today Giv at Ga ash a black hill in the north of the makhtesh was once an active volcano which erupted thousands of years ago and caused it to be covered in lava which quickly cooled in the open air converting it into basalt Limestone covered by basalt can also be found in smaller black hills in the southern part of the makhtesh including Karnei Ramon Shen Ramon Ramon s Tooth is a rock made of magma which hardened whilst underground It later rose up through cracks in the Earth s surface and today stands in striking contrast with the nearby creamy coloured southern wall of the crater as a black sharp edged rock In the centre of the makhtesh is HaMinsara The Carpentry Shop a low hill made up of columnar jointed sandstone polygonal prismatic columns of quartzite The pteriidan bivalve Family Ramonalinidae is found in early Middle Triassic rocks of Makhtesh Ramon and was named after this feature Nahal Ardon in the east of the makhtesh contains several vertical dikes Occasional geodes of celestine can be found next to some of them 1 Fauna edit nbsp A Nubian ibex on the edges of Makhtesh RamonThe Asiatic wild ass has been reintroduced to Makhtesh Ramon In 1995 the population had increased to 40 adults in the area The animals are hybrids of two different subspecies of the Asian Wild Ass It is derived from the Turkmenian kulan E h kulan and the Persian onager E h onager The original subspecies the Syrian wild ass E h hemippus is completely extinct 2 Other larger mammals of the area include Nubian ibex Dorcas gazelles striped hyenas Arabian wolves caracals golden jackals and reintroduced Arabian oryx 3 Historically the area was home to Arabian leopards However they are likely extinct in Israel 4 History edit nbsp Wadi Raman in the 1944 Survey of Palestine mapThe ruins of a large prehistoric stone structure known as Khan Saharonim he are found in the makhtesh as it lies along the ancient Incense Route a trade route used by the Nabataeans 2 000 years ago These ruins acted as a way station for the traders and their animals khan is the Arabic word for a caravanserai as they proceeded further westwards to the Mediterranean seaport city of Gaza Located atop the northern cliff of the crater one can find Metzad Mahmal the remnants of a stronghold employed by the Nabataeans and the Romans to safeguard the Incense Route The site was excavated by several archaeologists and declared a World Heritage Site by UNESCO in 2005 nbsp Wide panorama of the Makhtesh Ramon crater IsraelGallery edit nbsp Camel Hill Mitzpe Ramon Makhtesh Ramon nbsp Mount Ardon nbsp View of Makhtesh Ramon from its west nbsp The cliff nbsp Cloud gliding radiation fog falling in a katabatic wind into Makhtesh Ramon nbsp Dry Drimia maritima Urginea maritima at the northern edge of the makhtesh nbsp Rock formation dike nbsp Ha Minsara The Sawmill baked sandstone turned into hard quartzite nbsp Sandy rectangular and hexagonal prisms at the centre of Makhtesh Ramon Ha Minsara The Sawmill nbsp An ammonite in the Ammonite Wall nbsp Ammonite Wall Tamar Formation Cenomanian nbsp Sandstone color bands nbsp The remnants of Mezad Mahmal on the Incense Route between Petra and Avdat References edit Michael Anenburg Or M Bialik Yevgeny Vapnik Hazel J Chapman Gilad Antler Yaron Katzir Mike J Bickle 2014 The origin of celestine quartz calcite geodes associated with a basaltic dyke Makhtesh Ramon Israel Geological Magazine 151 5 798 815 Bibcode 2014GeoM 151 798A doi 10 1017 S0016756813000800 David Saltz David Mary Rowen Daniel I Rubenstein The Effect of Space Use Patterns of Reintroduced Asiatic Wild Ass on Effective Population Size Conservation Biology Vol 14 No 6 2000 Makhtesh Ramon Visitors Center Israel Nature and Parks Authority Retrieved 2023 03 25 Stein A B Athreya V Gerngross P Balme G Henschel P Karanth U Miquelle D Rostro Garcia S Kamler J F Laguardia A Khorozyan I amp Ghoddousi A 2020 Panthera pardus amended version of 2019 assessment The IUCN Red List of Threatened Species 2020 e T15954A163991139 doi 10 2305 IUCN UK 2020 1 RLTS T15954A163991139 en Accessed on 25 March 2023 External links edit nbsp Wikimedia Commons has media related to Makhtesh Ramon Ramon Crater on Google Maps Ramon Crater Detailed trail and hiking info from Tourism trips and travel in Israel Makhtesh Ramon s Visitors Center at the Israel Nature and Parks Authority s website Mazor Emanuel and Krasnov Boris editors The Makhteshim Country a Laboratory of Nature Pensoft Publishers Sofia 2001 ISBN 954 642 135 9 411 pages Retrieved from https en wikipedia org w index php title Makhtesh Ramon amp oldid 1214064442, wikipedia, wiki, book, books, library,

article

, read, download, free, free download, mp3, video, mp4, 3gp, jpg, jpeg, gif, png, picture, music, song, movie, book, game, games.