Lycaena phoebus | |
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Scientific classification | |
Kingdom: | Animalia |
Phylum: | Arthropoda |
Class: | Insecta |
Order: | Lepidoptera |
Family: | Lycaenidae |
Genus: | Lycaena |
Species: | L. phoebus |
Binomial name | |
Lycaena phoebus | |
Synonyms | |
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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.
Moroccan music varies greatly between geographic regions and social groups. It is influenced by musical styles including Arab, Berber, Andalusi, Mediterranean, Saharan, West African, and others.
Taounate is a town in northern Morocco, and is the capital of Tawnat Province. It is located at around 34°32′9″N4°38′24″W. The town had 37,616 inhabitants as of the 2014 Moroccan census.
Melitaea diamina, the false heath fritillary, is a butterfly of the family Nymphalidae.
Central Atlas Tamazight or Atlasic is a Berber language of the Afroasiatic language family spoken by 2.3 million in the Atlas Mountains of Central Morocco as well as by smaller emigrant communities in France and elsewhere.
Hipparchia fagi, the woodland grayling, is a butterfly of the family Nymphalidae.
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.
Morocco provides a refuge for a rich and diverse flora with about 4,200 taxa, of which 22% are endemic. The phytogeographic zones of Morocco comprise 8 zones: the Mediterranean zone, the Cedar zone (1000-2000m), the sub-Alpine zone (2,000-2,500m), the Alpine zone (2,500m+), the semi-desert scrub zone, the Reg, the sandy desert zone and the oases.
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 Province, central Morocco, 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=Uppermost Pliensbachian) 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 floodings.
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 Chaouia is an Moroccan tribal confederation made up of Arabised Berber tribes, and a historical region of Morocco. It is bounded by the Oum er-Rbi' River to its southwest, the Cherrate River to its northeast, the plain of Tadla to the southeast and the Atlantic Ocean to the northwest. The region covers a land area of nearly 14 000 km2.
The Azilal Formation is a geological unit in the Azilal and Ouarzazate provinces of the High Atlas mountains of Morocco. It covers the Latest Pliensbachian to early Aalenian stages of the Jurassic period. It is a terrestrial deposit that overlies marine dolomites of equivalent age to the Budoš Limestone of Montenegro or the Marne di Monte Serrone of Italy. Dinosaur remains, such as the sauropod Tazoudasaurus and the basal ceratosaur Berberosaurus are known from the unit, along with several undescribed genera.
Kretania martini, or Martin's blue, is a species of North African butterfly in the family Lycaenidae and the subfamily Polyommatinae.
The Battle of Moulouya took place in may 1692 at a ford on the Moulouya river in Morocco. It was fought between the armies of the Alaouite Sultan Moulay Ismail and those of the Dey of Algiers Hadj Chabane.
Igiliz is a medieval village located on the edge of the Sous valley in the Anti-Atlas mountains of Morocco. It is most known for being the birthplace of Ibn Tumart, founder of the Almohad caliphate. The village was known as place of pilgrimage by Ibn Tumart's followers during Almohad rule.
Hyponephele maroccana, the Moroccan meadow brown is a butterfly of the family Nymphalidae. It is endemic to Morocco
Cigaritis zohra, the Donzel's silverline, is a butterfly in the family Lycaenidae. It is found in Algeria and Morocco.
Cigaritis allardi, Allard's silverline, is a butterfly in the family Lycaenidae. It is found in Algeria and Morocco.