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Erfurt | |
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Country | |
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Population | 0 |
Erfurt ( AIR-furt, AIR-foort; German pronunciation: [ˈɛʁfʊʁt] (listen)) is the capital and largest city in the state of Thuringia, central Germany. It is located in the southern part of the Thuringian Basin, within the wide valley of the Gera river. It is located 100 km (62 mi) south-west of Leipzig, 300 km (186 mi) south-west of Berlin, 400 km (249 mi) north of Munich and 250 km (155 mi) north-east of Frankfurt. Together with a string of neighbouring cities Gotha, Weimar, Jena and others, Erfurt forms the central metropolitan corridor of Thuringia called Thüringer Städtekette (German "Thuringian city chain") with over 500,000 inhabitants.
Erfurt's old town is one of the best preserved medieval city centres in Germany. Tourist attractions include the Krämerbrücke (Merchants' bridge), the Old Synagogue, the ensemble of Erfurt Cathedral and Severikirche (St Severus's Church) and Petersberg Citadel, one of the largest and best preserved town fortresses in Europe. The city's economy is based on agriculture, horticulture and microelectronics. Its central location has led to it becoming a logistics hub for Germany and central Europe. Erfurt hosts the second-largest trade fair in eastern Germany (after Leipzig) as well as the public television children's channel KiKa.
Boulder | |
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State | Utah |
Country | United States of America |
Capital | |
Population | 0 |
Postcode | 84716 |
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.