The city of Chemnitz in Saxony (Germany) building its new economic profile
The city of Chemnitz in Saxony (Germany) building its new economic profile
复制标题
萨克森州开姆尼茨市（德国）正在打造新的经济形象
作者：
Andreas Bochmann;A. Dresler;W. Tietze
切姆尼茨，从1953年到1990年被称为卡尔马克思施塔特，位于萨克森的中心，是该地区的行政所在地，同名。该地区包括中部和西部Erzgebirge（矿石山）以及Vogtland。截至1995年，该市人口为C。271，000人，面积约12，871公顷。切姆尼茨位于厄尔士山脉的北方山脚，与中欧黄土带南部接壤。切姆尼茨位于海拔约300-450米处，一直延伸到厄尔士山脉盆地的东部边界，二叠纪火山贝加尔山（428米）从这里升起。几个世纪以来，来自前火山的斑状岩石已被证明是一种极好的建筑材料。在世纪城市的领土扩张期间，在切姆尼茨东北部的希尔伯斯多夫发现了一个令人印象深刻的”石化森林”，在那里从深红色壤土中出土了硅化的树干，可追溯到公元前。2.9亿年。这种独特的配置显然具有博物馆的品质。古植物学家Johann Traugott Sterzel（1841-1914）是第一个描述这种地质奇观的人。
Chemnitz, known from 1953 until 1990 as Karl Marx Stadt, is located in the center of Saxony and is the district's administrative seat bearing the same name. The district encompasses the middle and western Erzgebirge (Ore Mountain) as well as the Vogtland. As of 1995, the city has a population of c. 271,000 within an area of approximately 12,871 hectares. Chemnitz is situated at the northern foot of the Erzgebirge, bordering on the south of the mid-European loessial soil belt. Chemnitz lies approximately 300-450 meters above sea level and extends to the eastern border of the Erzgebirge basin, from which ascends the Permian volcano, the Beutenberg (428 meters). Over the centuries the porphyritic rock from the former volcano has proven to be an excellent building material. During the city's territorial expansion in the 19th century an impressive" petrified forest" was discovered in Hilbersdorf just northeast of Chemnitz where silicified tree trunks were unearthed from the deep red loam dating back c. 290 million years. This unique configuration is clearly of museum quality. The paleobotanist Johann Traugott Sterzel (1841-1914) was the first to describe this geological wonder.