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Mouxy
Mouxy (; frp, Meûssi) is a commune in the Savoie department in the Auvergne-Rhône-Alpes region in south-eastern France. Geography Dominated by Mount Revard, the Town of Mouxy is located on the heights above Aix-les-Bains, to which it is adjacent. It is part of the urban area of Chambéry. It is also part of the agglomeration community of Grand Lac. The important nearby towns of Annecy to the north, and Chambéry to the south, are located at distances as the crow flies of and 12.5 km ¾ miles respectively. Neighboring towns Mouxy is bordered by four municipalities: Pugny-Chatenod on the north, Drumettaz-Clarafond on the south, Aix-les-Bains on the east, and Les Déserts on the west. Many localities make up the collective community such as Chenoz, Montecovie, La Croix Balmont, Le Crêt, Le Faubourg, Le Biollay, and Le Mentens. The town is 628 hectares .28 km2, 2.425 sq. mi.in area; the elevations range over almost 1200 meters 940 feet from . The lowest poin ...
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Aix-les-Bains
Aix-les-Bains (, ; frp, Èx-los-Bens; la, Aquae Gratianae), locally simply Aix, is a commune in the southeastern French department of Savoie.Commune d'Aix-les-Bains (73008)
INSEE
Situated on the shore of the largest natural lake of glacial origin in France, the , this is a major ; it has the largest freshwater

Communauté D'agglomération Grand Lac
Communauté d'agglomération Grand Lac is the ''communauté d'agglomération'', an intercommunal structure, centred on the town of Aix-les-Bains. It is located in the Savoie department, in the Auvergne-Rhône-Alpes region, southeastern France. Created in 2017, its seat is in Aix-les-Bains.CA Grand Lac (N° SIREN : 200068674)
BANATIC. Retrieved 18 November 2022.
The name ''Grand Lac'' refers to the . Its area is 300.0 km2. Its population was 76,759 in 2019, of which 30,463 in Aix-les-Bains proper.
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Communes Of France
The () is a level of administrative division in the French Republic. French are analogous to civil townships and incorporated municipalities in the United States and Canada, ' in Germany, ' in Italy, or ' in Spain. The United Kingdom's equivalent are civil parishes, although some areas, particularly urban areas, are unparished. are based on historical geographic communities or villages and are vested with significant powers to manage the populations and land of the geographic area covered. The are the fourth-level administrative divisions of France. vary widely in size and area, from large sprawling cities with millions of inhabitants like Paris, to small hamlets with only a handful of inhabitants. typically are based on pre-existing villages and facilitate local governance. All have names, but not all named geographic areas or groups of people residing together are ( or ), the difference residing in the lack of administrative powers. Except for the municipal arrondi ...
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Saint-Pierre-de-Curtille
Saint-Pierre-de-Curtille is a commune in the Savoie department in the Auvergne-Rhône-Alpes region in south-eastern France. It is situated near the northwestern shore of Lac du Bourget. Heritage sites It is home to a prehistoric pile-dwelling (or stilt house) settlement that is part of the Prehistoric Pile dwellings around the Alps UNESCO World Heritage Site. These dwellings, now submerged in the Lac du Bourget, date from the 4th millennium BCE. The Hautecombe Abbey, situated on the lake shore, has been a classified monument since 1875. See also *Communes of the Savoie department The following is a list of the 273 communes of the Savoie department of France. The communes cooperate in the following intercommunalities (as of 2020):
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Geological
Geology () is a branch of natural science concerned with Earth and other astronomical objects, the features or rocks of which it is composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology, and so is treated as one major aspect of integrated Earth system science and planetary science. Geology describes the structure of the Earth on and beneath its surface, and the processes that have shaped that structure. It also provides tools to determine the relative and absolute ages of rocks found in a given location, and also to describe the histories of those rocks. By combining these tools, geologists are able to chronicle the geological history of the Earth as a whole, and also to demonstrate the age of the Earth. Geology provides the primary evidence for plate tectonics, the evolutionary history of life, and the Earth's past climates. Geologists broadly study the properties and processes of Ear ...
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Neolithic
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egypt in th ...
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Hydrotherapy
Hydrotherapy, formerly called hydropathy and also called water cure, is a branch of alternative medicine (particularly naturopathy), occupational therapy, and physiotherapy, that involves the use of water for pain relief and treatment. The term encompasses a broad range of approaches and therapeutic methods that take advantage of the physical properties of water, such as temperature and pressure, to stimulate blood circulation, and treat the symptoms of certain diseases. Various therapies used in the present-day hydrotherapy employ water jets, underwater massage and mineral baths (e.g. balneotherapy, Iodine-Grine therapy, Kneipp treatments, Scotch hose, Swiss shower, thalassotherapy) or whirlpool bath, hot Roman bath, hot tub, Jacuzzi, and cold plunge. Uses Water therapy may be restricted to use as aquatic therapy, a form of physical therapy, and as a cleansing agent. However, it is also used as a medium for delivery of heat and cold to the body, which has long been the b ...
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Lake Bourget
Lac du Bourget (; English Lake Bourget), also locally known as Lac Gris (; en, Grey Lake) or Lac d'Aix (), is a lake at the southernmost end of the Jura Mountains in the department of Savoie, France. It is the deepest lake located entirely within France, and either the largest or second largest after Lac de Grand-Lieu depending on season. The largest town on its shore is Aix-les-Bains. Chambéry, the capital of Savoie, lies about 10 km south of the lake. The lake is mainly fed by the river Leysse (and other small rivers), and it drains towards the river Rhône through the Canal de Savières, an artificial channel. It is a Ramsar site. The extinct bezoule was found only in this lake. The lake was formed during the last period of global glaciation in the Alps (Würm glaciation) during the Pleistocene epoch. It has a surface area of . The long and narrow north-south axis of the lake extends 18 km in length, and ranges between 1.6 km and 3.5 km in width. The ...
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Marl
Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part of the cliffs of Dover, and the Channel Tunnel follows these marl layers between France and the United Kingdom. Marl is also a common sediment in post-glacial lakes, such as the marl ponds of the northeastern United States. Marl has been used as a soil conditioner and neutralizing agent for acid soil and in the manufacture of cement. Description Marl or marlstone is a carbonate-rich mud or mudstone which contains variable amounts of clays and silt. The term was originally loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions. These typically contain 35–65% clay and 65–35% carbonate. The te ...
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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 ...
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Urgonian Limestone Formation
The Urgonian Limestone is a geologic formation in France. It preserves fossils dating back to the Cretaceous period. Some parts of the limestone have undergone metamorphism to produce ductile folds next to faults. See also * List of fossiliferous stratigraphic units in France See also * Lists of fossiliferous stratigraphic units in Europe These lists of fossiliferous stratigraphic units in Europe enumerate the rock layers which preserve the fossilized remains of ancient life in Europe by the modern countries wher ... References External links * Geologic formations of France Jurassic France Limestone formations {{Cretaceous-stub ...
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Alluvium
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Alluvium is also sometimes called alluvial deposit. Alluvium is typically geologically young and is not consolidated into solid rock. Sediments deposited underwater, in seas, estuaries, lakes, or ponds, are not described as alluvium. Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations. Definitions The present consensus is that "alluvium" refers to loose sediments of all types deposited by running water in floodplains or in alluvial fans or related landforms. However, the meaning of the term has varied considerably since it was first defined in the French dictionary of Antoine Furetière, posthumously published in 1690. Drawing upon concepts from Roman law, Furetière defined ''alluvion'' (the F ...
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