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Jebel Boukornine
Jebel Boukornine (''jebel bū-qarnīn''), also spelled Djebel Bou Kornine or Mount Bou Kornine, is a 576-meter mountain in northern Tunisia, overlooking the Gulf of Tunis and Hammam Lif city. It consists of folded and faulted outcrops of Jurassic limestone. Its name "bou kornine" comes from Tunisian Arabic meaning "the one with two horns", originally from the punic language as "ba'al kornine", meaning "lord with two horns". It owes its name to the two highlights of altitude 576 and 493 meters at the top. During the times of ancient Carthage, the mountain was considered sacred and religious rituals were conducted there. The massif is part of Boukornine National Park, covering area of 1939 ha and protecting many species of plants and animals. The mountain slopes are covered with Aleppo pine and cedar. Djebel Ressas Djebel Ressas is a high and rugged outcropping of Jurassic limestone situated on the horizon southeast of Tunis, Tunisia. Competing in the foreground, the famili ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tunisia
) , image_map = Tunisia location (orthographic projection).svg , map_caption = Location of Tunisia in northern Africa , image_map2 = , capital = Tunis , largest_city = capital , coordinates = , official_languages = Arabic Translation by the University of Bern: "Tunisia is a free State, independent and sovereign; its religion is the Islam, its language is Arabic, and its form is the Republic." , religion = , languages_type = Spoken languages , languages = Minority Dialects : Jerba Berber (Chelha) Matmata Berber Judeo-Tunisian Arabic (UNESCO CR) , languages2_type = Foreign languages , languages2 = , ethnic_groups = * 98% Arab * 2% Other , demonym = Tunisian , government_type = Unitary presidential republic , leader_title1 = President , leader_name1 = Kais Saied , leader_ti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gulf Of Tunis
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The Gulf of Tunis () is a large Mediterranean bay in north-eastern Tunisia, extending for from Cape Farina in the west to Cape Bon in the east. Tunis, the capital city of Tunisia, lies at the south-western edge of the Gulf, as have a series of settled places over the last three millennia. Djebel Ressas rises to around south of the southern edge of the Gulf. The central part of the gulf, corresponding to the city of Tunis, is favorable to the implementation of a commercial port due to its location of being a well protected area. The famous city of Carthage was built on the gulf shores. References Tunis Tunis ''Tounsi'' french: Tunisois , population_note = , population_urban = , population_metro = 2658816 , population_density_km2 = , timezone1 = CET , utc_offset1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hammam Lif
Hammam-Lif ( ar, حمام الأنف, pronounced hammam linf) is a coastal town about 20 km south-east of Tunis, the capital of Tunisia. It has been known since antiquity for its thermal springs originating in Mount Bou Kornine. History Naro, which means fire, was Hammam-Lif's Punic name. In 1883, the French captain Ernest De Prudhomme discovered in his Hammam-lif residence the first archeological ruins of an ancient synagogue that once stood in Hammam-Lif in 3rd-5th century AD. Hammam-Lif was once the home of Italian, Greek and Jewish communities, especially before the end of the French colonial period. Hammam-Lif's most interesting site is probably Dar El Bey, which was the residence of Ali II Bey, the 4th bey of Tunis. Sport The local football team Club Sportif de Hammam-Lif won the Tunisian championship in 1952, 1954, 1955, 1956 and won the Tunisian Cup in 1946, 1947, 1948, 1949, 1950, 1985, 2001 Notable people * Ahmed Achour (1945-2021), conductor and composer * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fold (geology)
In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary strata, that are bent or curved during permanent deformation. Folds in rocks vary in size from microscopic crinkles to mountain-sized folds. They occur as single isolated folds or in periodic sets (known as ''fold trains''). Synsedimentary folds are those formed during sedimentary deposition. Folds form under varied conditions of stress, pore pressure, and temperature gradient, as evidenced by their presence in soft sediments, the full spectrum of metamorphic rocks, and even as primary flow structures in some igneous rocks. A set of folds distributed on a regional scale constitutes a fold belt, a common feature of orogenic zones. Folds are commonly formed by shortening of existing layers, but may also be formed as a result of displacement on a non-planar fault (''fault bend fold''), at the tip of a propagating fault (''fault propagation fold''), by differential compaction or due to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tunisian Arabic
Tunisian Arabic, or simply Tunisian, is a set of dialects of Maghrebi Arabic spoken in Tunisia. It is known among its over 11 million speakers aeb, translit=Tounsi/Tounsiy, label=as, تونسي , "Tunisian" or "Everyday Language" to distinguish it from Modern Standard Arabic, the official language of Tunisia. Tunisian Arabic is mostly similar to eastern Algerian Arabic and western Libyan Arabic. As part of a dialect continuum, Tunisian merges into Algerian Arabic and Libyan Arabic at the borders of the country. Like other Maghrebi dialects, it has a vocabulary that is predominantly Semitic Arabic with a minimal Berber, Latin Tilmatine Mohand, ''Substrat et convergences: Le berbére et l'arabe nord-africain'' (1999), in ''Estudios de dialectologia norteafricana y andalusi 4'', pp 99–119 and possibly Neo-Punic substratum. Tunisian Arabic contains a few Berber loanwords which represent 8% to 9% of its vocabulary. However, Tunisian has also loanwords from French, Turkish, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Punic Language
The Punic language, also called Phoenicio-Punic or Carthaginian, is an extinct variety of the Phoenician language, a Canaanite language of the Northwest Semitic branch of the Semitic languages. An offshoot of the Phoenician language of coastal West Asia (modern Lebanon and western Syria), it was principally spoken on the Mediterranean coast of Northwest Africa, and the Iberian peninsula and several Mediterranean islands such as Malta, Sicily and Sardinia by the Punic people, or western Phoenicians, throughout classical antiquity, from the 8th century BC to the 6th century AD. Punic is considered to have separated from its Phoenician parent around the time that Carthage became the leading Phoenician city under Mago I, but scholarly attempts to delineate the dialects lack precision and generally disagree on the classification. History The Punics stayed in contact with the homeland of Phoenicia until the destruction of Carthage by the Roman Republic in 146 BC. At first, there was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ancient Carthage
Carthage () was a settlement in modern Tunisia that later became a city-state and then an empire. Founded by the Phoenicians in the ninth century BC, Carthage reached its height in the fourth century BC as one of the largest metropolises in the worldGeorge Modelski, ''World Cities: –3000 to 2000'', Washington DC: FAROS 2000, 2003. . Figures in main tables are preferentially cited. Part of former estimates can be read at Evolutionary World Politics Homepage Archived 2008-12-28 at the Wayback Machine and the centre of the Carthaginian Empire, a major power in the ancient world that dominated the western Mediterranean. Following the Punic Wars, Carthage was destroyed by the Romans in 146 BC, who later rebuilt the city lavishly. Carthage was settled around 814 BC by colonists from Tyre, a leading Phoenician city-state located in present-day Lebanon. In the seventh century BC, following Phoenicia's conquest by the Neo-Assyrian Empire, Carthage became independent, gradually ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Boukornine National Park
Boukornine National Park (french: Parc national de Boukornine) is a national park in northern Tunisia. The park was established on 12 February 1987. , Mille et Une Tunisie, 24 Sept 2011. It is very near to the town of and just to the capital city of . [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
