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The Suez Canal (/ ˈ s uː. ɛ z /; Arabic: قَنَاةُ ٱلسُّوَيْسِ, Qanāt as-Suwais) is an artificial sea-level waterway in Egypt, connecting the Mediterranean Sea to the Red Sea through the Isthmus of Suez and dividing Africa and Asia (and by extension, the Sinai Peninsula from the rest of Egypt).
The Suez Company or Suez Canal Company, full initial name Compagnie universelle du canal maritime de Suez (Universal Company of the Maritime Canal of Suez), [1] sometimes colloquially referred to in French as Le Suez ("The Suez"), [2] [3] was a company formed by Ferdinand de Lesseps in 1858 to operate the Egyptian granted concession of the Suez Canal, which the company built between 1859 and 1869.
Suez (UK: / ˈ s uː ɪ z /, US: / ˌ s uː ˈ ɛ z /, [3] [4] Egyptian Arabic: السويس, romanized: as-Suways, pronounced [esseˈweːs]) is a seaport city with a population of about 800,000 as of August 2021 in north-eastern Egypt, located on the north coast of the Gulf of Suez on the Red Sea, near the southern terminus of the Suez Canal.
The location of the Suez Canal, which connects the Mediterranean and the Indian Ocean via the Red Sea. The Suez Canal was opened in 1869, after ten years of work financed by the French and Egyptian governments. [25]
Approximate location of Canal of the Pharaohs. The Canal of the Pharaohs, also called the Ancient Suez Canal or Necho's Canal, is the forerunner of the Suez Canal, constructed in ancient times and kept in use, with intermissions, until being closed in 767 AD for strategic reasons during a rebellion.
The Suez Canal was blocked for six days from 23 to 29 March 2021 by the Ever Given, a container ship that had run aground in the canal. [4]The 400-metre-long (1,300 ft), 224,000-ton, 20,000 TEU vessel was buffeted by strong winds on the morning of 23 March, and ended up wedged across the waterway with its bow and stern stuck on opposite canal banks, blocking all traffic until it could be freed ...
The Gulf of Suez Rift is a continental rift zone that was active between the Late Oligocene (c. 28 Ma) and the end of the Miocene (c. 5 Ma). [1] It represented a continuation of the Red Sea Rift until break-up occurred in the middle Miocene, with most of the displacement on the newly developed Red Sea spreading centre being accommodated by the ...
The Katipunan obtained overwhelming number of members and attracted the lowly classes. In June 1896, Bonifacio sent an emissary to Dapitan to obtain Rizal's support, but Rizal refused to participate in an armed revolution. On August 19, 1896, Katipunan was discovered by a Spanish friar, which resulted in the start of the Philippine Revolution.