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Calanque De Port-Miou
The Calanque de Port-Miou is one of the three big Cassis calanques. It is very long and narrow, and thus was very suitable for establishing a marina. The name ''Port-Miou'' is an approximate transcription in French orthography of the Occitan ''Pòrt-Melhor'' (the "best port A port is a maritime facility comprising one or more wharves or loading areas, where ships load and discharge cargo and passengers. Although usually situated on a sea coast or estuary, ports can also be found far inland, such as Ham ...") which is locally pronuncied /pwɔʁ.mi.ju/. History Port-Miou was for a long time a seigniory in its own right, dependent on the Maison des Baux. On April 4, 1402, in Brantes, at the foot of Ventoux, in the presence of his wife Alix des Baux, Odon de Villars donated to his nephew Philippe de Lévis the fiefs of Brantes, Plaisians and their dependencies, the seigneuries of Saint-Marcel, Roquefort, Le Castellet, Cassis and Port-Miou, dependent on the barony o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calanques Port-Miou
A calanque (, "inlet"; co, calanca, plural ''calanche'' or ''calanchi''; oc, calanca, plural ''calancas'') is a narrow, steep-walled inlet that is developed in limestone, dolomite, or other carbonate strata and found along the Mediterranean coast. A calanque is a steep-sided valley formed within karstic regions either by fluvial erosion or the collapse of the roof of a cave that has been subsequently partially submerged by a rise in sea level.Bird, E.C.F., 2008, ''Coastal Geomorphology: An Introduction'', 2nd ed. John Wiley and Sons Ltd. West Sussex, England. Goudie, A., 2004, ''Encyclopedia of Geomorphology.'' Routledge. London, England. Monroe, W.H., 1970, ''A Glossary of Karst Terminology.'' Water-Supply Paper 1899-K. U.S. Geological Survey. Reston, Virginia. Characteristics Location The best known examples of this formation can be found in the Massif des Calanques (''Massís dei calancas'' in Occitan, the traditional local language) in the Bouches-du-Rhône departm ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cassis, Bouches-du-Rhône
Cassis (; Occitan: ''Cassís'') is a commune situated east of Marseille in the department of Bouches-du-Rhône in the Provence-Alpes-Côte d'Azur region, whose coastline is known in English as the French Riviera, in Southern France. In 2016, it had a population of 7,265. It is a popular tourist destination, famous for its cliffs (''falaises'') and the sheltered inlets called '' calanques''. The wines of Cassis are white and rosé, and not to be confused with crème de cassis, a specialty of Burgundy which takes its name from blackcurrants (''cassis''), not the commune. Geography The town is situated on the Mediterranean coast, about east of Marseille. Cap Canaille, , between Cassis and La Ciotat ("the ''civitas''") is one of the highest maritime bluffs in Europe, a sailor's landmark for millennia. It is east of Marseille and in the department of Bouches-du-Rhône. One of its main beaches, called "Bestouan", is made cooler by a karstic source. History The pres ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calanque
A calanque (, "inlet"; co, calanca, plural ''calanche'' or ''calanchi''; oc, calanca, plural ''calancas'') is a narrow, steep-walled inlet that is developed in limestone, dolomite, or other carbonate strata and found along the Mediterranean coast. A calanque is a steep-sided valley formed within karstic regions either by fluvial erosion or the collapse of the roof of a cave that has been subsequently partially submerged by a rise in sea level.Bird, E.C.F., 2008, ''Coastal Geomorphology: An Introduction'', 2nd ed. John Wiley and Sons Ltd. West Sussex, England. Goudie, A., 2004, ''Encyclopedia of Geomorphology.'' Routledge. London, England. Monroe, W.H., 1970, ''A Glossary of Karst Terminology.'' Water-Supply Paper 1899-K. U.S. Geological Survey. Reston, Virginia. Characteristics Location The best known examples of this formation can be found in the Massif des Calanques (''Massís dei calancas'' in Occitan, the traditional local language) in the Bouches-du-Rhône department o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marina
A marina (from Spanish , Portuguese and Italian : ''marina'', "coast" or "shore") is a dock or basin with moorings and supplies for yachts and small boats. A marina differs from a port in that a marina does not handle large passenger ships or cargo from freighters. The word ''marina'' may also refer to an inland wharf on a river or canal that is used exclusively by non-industrial pleasure craft such as canal narrowboats. Emplacement Marinas may be located along the banks of rivers connecting to lakes or seas and may be inland. They are also located on coastal harbors (natural or man made) or coastal lagoons, either as stand alone facilities or within a port complex. History In the 19th century, the few existing pleasure craft shared the same facilities as trading and fishing vessels. The marina appeared in the 20th century with the popularization of yachting. Facilities and services A marina may have refuelling, washing and repair facilities, marine and boat chandlers, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
French Orthography
French orthography encompasses the spelling and punctuation of the French language. It is based on a combination of phoneme, phonemic and historical principles. The spelling of words is largely based on the pronunciation of Old French c. 1100–1200 AD, and has stayed more or less the same since then, despite enormous changes to the pronunciation of the language in the intervening years. Even in the late 17th century, with the publication of the Dictionnaire de l'Académie française, first French dictionary by the Académie française, there were attempts to Reforms of French orthography, reform French orthography. This has resulted in a complicated relationship between spelling and sound, especially for vowels; a multitude of silent letters; and many homophones—e.g., ''/////'' (all pronounced ) and ''//'' (all pronounced ). This is conspicuous in verbs: ' (you speak), ' (I speak) and ' (they speak) all sound like . Later attempts to respell some words in accordance with their ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Occitan Language
Occitan (; oc, occitan, link=no ), also known as ''lenga d'òc'' (; french: langue d'oc) by its native speakers, and sometimes also referred to as ''Provençal'', is a Romance languages, Romance language spoken in Southern France, Monaco, Italy's Occitan Valleys, as well as Spain's Val d'Aran; collectively, these regions are sometimes referred to as Occitania, Occitània. It is also spoken in Calabria (Southern Italy) in a linguistic enclave of Cosenza area (mostly Guardia Piemontese). Some include Catalan language, Catalan in Occitan, as the Linguistic distance, distance between this language and some Occitan dialects (such as the Gascon language) is similar to the distance between different Occitan dialects. Catalan was considered a dialect of Occitan until the end of the 19th century and still today remains its closest relative. Occitan is an official language of Catalonia, where a subdialect of Gascon known as Aranese dialect, Aranese is spoken in the Val d'Aran. Since Sept ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Port
A port is a maritime facility comprising one or more wharves or loading areas, where ships load and discharge cargo and passengers. Although usually situated on a sea coast or estuary, ports can also be found far inland, such as Hamburg, Manchester and Duluth; these access the sea via rivers or canals. Because of their roles as ports of entry for immigrants as well as soldiers in wartime, many port cities have experienced dramatic multi-ethnic and multicultural changes throughout their histories. Ports are extremely important to the global economy; 70% of global merchandise trade by value passes through a port. For this reason, ports are also often densely populated settlements that provide the labor for processing and handling goods and related services for the ports. Today by far the greatest growth in port development is in Asia, the continent with some of the world's largest and busiest ports, such as Singapore and the Chinese ports of Shanghai and Ningbo-Zhou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Provence-Alpes-Côte D'Azur
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateau ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliffs Of Metropolitan France
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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