Chott el Fejej
| Chott el Fejej | |
|---|---|
| General information | |
Height above mean sea level (en)  | 25 m |
| Tsawo | 110 km |
| Labarin ƙasa | |
 | |
| Tsarin Daidaiton Labarin Kasa | 33°54′16″N 9°10′44″E / 33.9044°N 9.1789°E |
| Bangare na | Tafkunan gishiri na Tunisia |
| Kasa | Tunisiya |
| Territory |
Kebili Governorate (en) da Gabès Governorate (en) |
Chott el Fejaj', wanda aka fi sani da Chott da Fedjedj da Chott al Fejaj, tsayi ne mai tsawo, mai kunkuntar ruwa na tafkin gishiri na endorheic Chott el Djerid a kudancin Tunisiya.
Tarihi da yanayin ƙasa
[gyara sashe | gyara masomin]Ƙashin Chott el Fejej yana ƙasa da matakin teku kuma yana gudana a cikin ƙanƙanin hanya daga babban jikin Chott el Djerid zuwa hamadar hamadar Tunisiya ta El Hamma, kusa da Tekun Gabès a kan Bahar Rum. Tsakanin daga inda Chott el Fejej ya haɗu da Chott el Djerid zuwa ƙarshen kusa da El Hamma kusan mil 70 ne (kilomita 110). Tare da tsawonsa, Chott el Fejej ba ya faɗaɗa fiye da kilomita 20 (32) kuma a wurare da yawa ya fi ƙanƙanta. Ƙarshen gabas na Chott el Fejej ya rabu da Bahar Rum ta kusan kilomita 13 (21 mai faɗi na yashi kusa da El Hamma .[1]
Wannan karamin yashi ne, wanda ke raba Chott el Fejej daga Bahar Rum, wanda ya kawo shi ga masu ilimin ƙasa daban-daban, injiniyoyi da diflomasiyya. Wadannan adadi sun nemi ƙirƙirar "Teku na Sahara" ta hanyar tura ruwan Bahar Rum zuwa cikin tafkin hamadar Sahara wanda ke ƙasa da matakin teku. An gabatar da wata sananniyar shawara game da wannan sakamako a ƙarshen 1800s daga masanin ilimin ƙasa na Faransa François Élie Roudaire da mahaliccin Suez Canal, Ferdinand na Lesseps, amma ya tsaya bayan gwamnatin Faransa ta janye kudade.[1][2] Daga baya shawarwari, waɗanda aka yi a matsayin wani ɓangare na Operation Plowshare, sun nuna cewa za a iya amfani da fashewar nukiliya don tono tashar da aka tsara daga Bahar Rum zuwa Chott el Fejej da sauran wuraren da ke ƙasa da Sahara; waɗannan shawarwari ma ba su da amfani.
Ilimin ƙasa
[gyara sashe | gyara masomin]chott el Fejej wani tafki ne na musamman, ko tafkin bushe, na Sahara. Duk da haka, babban anticline da aka sani da Fejej Dome ne ya kafa shi. Wannan anticline da sauran tsarin da ke kewaye da su ana jayayya da su ne sakamakon rifting a lokacin Cretaceous.[3]
Manazarta
[gyara sashe | gyara masomin]- 1 2 Plummer, Harry Chapin (1913). "A Sea in the Sahara". National Waterways: A Magazine of Transportation. National Rivers and Harbors Congress. 1 (2): 131–138. Retrieved 16 December 2012.
- ↑ McKay, Donald Vernon (1943). "Colonialism in the French geographical movement 1871-1881". Geographical Review. American Geographical Society. 33 (2): 214–232. doi:10.2307/209775. JSTOR 209775.
- ↑ Gharbi, Mohamed; Masrouhi, Amara; Espurt, Nicolas; Bellier, Olivier; Amari, El Amjed; Ben Youssef, Mohamed; Ghanmi, Mohamed (March 2013). "New tectono-sedimentary evidences for Aptian to Santonian extension of the Cretaceous rifting in the Northern Chotts range (Southern Tunisia)" (PDF). Journal of African Earth Sciences. Elsevier Ltd. 79: 58–73. doi:10.1016/j.jafrearsci.2012.09.017.