| Moroccan meadow brown | |
|---|---|
 | |
Scientific classification  | |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Arthropoda |
| Class: | Insecta |
| Order: | Lepidoptera |
| Family: | Nymphalidae |
| Genus: | Hyponephele |
| Species: | H. maroccana |
| Binomial name | |
| Hyponephele maroccana | |
| Synonyms | |
Epinephele lycaon var. maroccana Blachier, 1908 | |
Hyponephele maroccana, the Moroccan meadow brown is a butterfly of the family Nymphalidae. It is endemic to Morocco (Atlas Mountains) [2]
It flies in rocky places in one generation from June to August.
The French protectorate in Morocco, also known as French Morocco, was the period of French colonial rule in Morocco that lasted from 1912 to 1956. The protectorate was officially established 30 March 1912, when Sultan Abd al-Hafid signed the Treaty of Fez, though the French military occupation of Morocco had begun with the invasion of Oujda and the bombardment of Casablanca in 1907.
Charles Oberthür was a French amateur entomologist specializing in lepidoptera.
Cyaniris semiargus, the Mazarine blue, is a Palearctic butterfly in the family Lycaenidae.
Tazoudasaurus is a genus of gravisaurian, probably a vulcanodontid sauropod dinosaurs hailing from the late Early Jurassic (Toarcian), that was recovered in the "Toundoute Continental Series" located in the High Atlas Mountains of Morocco in North Africa. Along with Patagosaurus, Volkheimeria, Bagualia and Perijasaurus represents one of the few sauropods named from this stage on Gondwana, as well the only one from Africa.
Berberosaurus is a genus of neotheropod dinosaur, possibly a ceratosaur, from the Toarcian-age "Toundoute Continental Series" found in the Central High Atlas of Toundoute, Ouarzazate, Morocco. The type species of the genus Berberosaurus is B. liassicus, in reference to the Lias epoch. Berberosaurus might be the oldest known ceratosaur, and is based on partial postcranial remains. This genus represents the oldest formally identified theropod from the North of Africa, as well one of the few from the region in the Early Jurassic.
Otala lactea, known as the milk snail or Spanish snail, is a large, edible species of air-breathing land snail, a terrestrial pulmonate gastropod mollusk, in the family Helicidae, the typical snails.
The Argana Group is a Permian to Triassic geological group in the western High Atlas northeast of Agadir, Morocco. Sometimes known as the Argana Formation, it contains eight geological members often divided into three formations. They include the Late Permian Ikakern Formation, the Early Triassic to Carnian Timezgadiouine Formation (T3-T5), and the Late Triassic Bigoudine Formation (T6-T8). Ornithischian tracks are geographically located in Marrakesh province. Indeterminate theropod remains and tracks are geographically located in Marrakesh province.
Chefchaouen is a province in the Moroccan economic region of Tanger-Tetouan-Al Hoceima.
The Tilougguit Formation, also known as the Tillouguit Formation, is an Early Bathonian geologic formation in Morocco. An indeterminate sauropod is known from the formation
The Aganane Formation is a Pliensbachian geologic formation in the Azilal, Béni-Mellal, Ouarzazate, Tinerhir and Errachidia provinces, central Morocco, being the remnant of a local massive Carbonate platform, and known mostly for its rich tracksites including footprints of thyreophoran, sauropod and theropod dinosaurs. This formation has been dated to the Pliensbachian stage of the Lower Jurassic, thanks to the find of the ammonite Arieticeras cf. algovianum, indicator of Middle Domerian in the upper zone, and lower delimitation by the foraminifers Mayncina termieri and Orbitopsella praecursor. The dinosaur tracksites are all located a few metres below the Pliensbachian-Toarcian limit, being coeval and connected with the lowermost layers of the continental Azilal Formation. The Aganane Formation was also coeval with the Jbel Taguendouft Formation and the Tamadout 1 Formation, all developed along a local "platform-furrow" in the Middle Atlas Mountains, that act as a barrier controlling the western border of the Jurassic Atlas Gulf. The nearshore sections, including both carbonate platforms and close to sea terrestrial facies where located on an isolated internal domain thanks to the control of the barrier, allowing the Aganane Formation to develop on a hot and humid climate, where a local algal marsh had intermittent progradations, intercalated with a layer of terrigenous continental origin. The ichnosites were developed in tidal flats and coastal deposits suitable to sea flooding.
Ait Seghrouchen Berber, or Seghroucheni (Seghrusheni), is a Zenati Berber language of the Eastern Middle Atlas Berber cluster. It is spoken by the Ait Seghrouchen tribe inhabiting east-central Morocco.
The following is a timeline of the history of the city of Fez, Morocco.
Harold Powell was a British entomologist who specialised in Lepidoptera.
The El Mers Group is a geological group in the Middle Atlas of Morocco. It is subdivided into three formations named the El Mers I, II, and III Formations, respectively. It is a marine deposit primarily consisting of marl, with gypsum present in the upper part of unit 3. It is the lateral equivalent of the terrestrial Guettioua Sandstone. Dinosaur remains are among the fossils that have been recovered from the group, most notably those of sauropods and the unusual thyreophorans Adratiklit, Thyreosaurus, and Spicomellus.
The Azilal Formation, also known as Toundoute Continental Series and Wazzant Formation, is a geological unit in the Azilal, Béni-Mellal, Ouarzazate, Tinerhir and Errachidia provinces of the High Atlas of Morocco, that cover the Early Toarcian to Middle Aalenian stages of the Jurassic Period. While there have been atributions of it´s lowermost layers to the Latest Pliensbachian, the current oldest properly measured are part of the Earliest Toarcian regresion ("MRST10"), part of the Lower-Middle Palymorphum biozone. The Azilal Formation consists mainly of claystones rich in continental plant debris and laminated microbial facies. It is a continental deposit which overlies marine dolomites of equivalent age to the Rotzo Formation of Italy, mostly part of the Aganane Formation. The formation is best assigned to an alluvial environment occasionally interrupted by shallow marine incursions and marks a dramatic decrease of the carbonate productivity under increasing terrigenous sedimentation. Dinosaur remains, such the sauropod Tazoudasaurus and the basal ceratosaur Berberosaurus are known from the unit, along with several undescribed genera. The strata of the group extends towards the Central High Atlas, covering different anticlines, and topographic accidents along the range of the Mountains. Although new studies have suggested that the strata is coeval in age, and should be referred to as a unique unit. The toarcian High Atlas is divided in 5 units: the continental layers with paralic deposits belong to the Azilal, along the shoreface layers of the Tagoudite Formation and Tafraout Formation, both connected with the offshore Ait Athmane Formation and the deeper shelf deposits of the Agoudim 1 Formation.
Jewelleryof the Berber cultures is a historical style of traditional jewellery that was worn by women mainly in rural areas of the Maghreb region in North Africa and inhabited by indigenous Berber people. Following long social and cultural traditions, Berber or other silversmiths in Morocco, Algeria and neighbouring countries created intricate jewellery with distinct regional variations. In many towns and cities, there were Jewish silversmiths, who produced both jewellery in specific Berber styles as well as in other styles, adapting to changing techniques and artistic innovations.
Cigaritis allardi, Allard's silverline, is a butterfly in the family Lycaenidae. It is found in Algeria and Morocco.
Lycaena phoebus, the Moroccan copper, is a butterfly in the family Lycaenidae. It is endemic to the Atlas Mountains of Morocco. It flies according to the place from April to September or simply from August to September in a variable number of generations. Its host plant is Polygonum aviculare in the High Atlas and possibly Polygonum equisetiforme in the Anti-Atlas. The biotope is flowery meadow.