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Limoges | |
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State | |
Country | |
Capital | |
Population | 139150 |
Limoges (, also US: , French: [limɔʒ] (listen); Occitan: Lemòtges, locally Limòtges [liˈmɔdzes]) is a city and commune, the capital of the Haute-Vienne department and was the administrative capital of the former Limousin region in west-central France. Situated on the first western foothills of the Massif Central, Limoges is crossed by the Vienne River, of which it was originally the first ford crossing point.
The second most populated town in the New Aquitaine region after Bordeaux, a university town, an administrative centre and intermediate services with all the facilities of a regional metropolis, its has an urban area of 283,557 inhabitants in 2016, making it the sixth in South-West France and the 38th in the whole country.The inhabitants of the city are called the Limougeauds.
Founded around 10 BC under the name of Augustoritum, it became an important Gallo-Roman city. In the Middle Ages Limoges becomes a large city, strongly marked by the cultural influence of the Abbey of Saint-Martial, within the Duchy of Aquitaine, whose dukes are invested and crowned in this city. From the 12th century onwards, its enamels were exported throughout the Christian world. In 1765, during the industrial revolution, the discovery of a deposit of kaolin in the Saint-Yrieix-la-Perche region enabled the development of the Limoges porcelain industry, which would make Limoges world-famous.
Boulder | |
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State | Montana |
Country | United States of America |
Capital | |
Population | 1445 |
In geology, a boulder is a rock fragment with size greater than 256 millimetres (10.1 in) in diameter. Smaller pieces are called cobbles and pebbles. While a boulder may be small enough to move or roll manually, others are extremely massive.
In common usage, a boulder is too large for a person to move. Smaller boulders are usually just called rocks (American English) or stones (In British English a rock is larger than a boulder). The word boulder is short for boulder stone, from Middle English bulderston or Swedish bullersten.In places covered by ice sheets during Ice Ages, such as Scandinavia, northern North America, and Siberia, glacial erratics are common. Erratics are boulders picked up by ice sheets during their advance, and deposited when they melt.
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