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Hermann Karsten, pioneer of geologic mapping in northwestern South America

机译:南美洲西北部地质绘图先驱Hermann Karsten

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In the late 19th century, a regional map of NuevaGranada (present-day Colombia, Panama and parts of Venezuela and Ecuador)was published by German botanist and geologist Hermann Karsten (1817–1908).Karsten's work was incorporated by Agustín Codazzi (1793–1859), anItalian who emigrated to Venezuela and Colombia to serve as a governmentcartographer and geographer, in his popular Atlas geográfico ehistórico de la Republica de Colombia (1889). Geologic mapping and mostobservations provided in this 1889 atlas were taken from Karsten'sGéologie de l'ancienne Colombie bolivarienne: Vénézuela,Nouvelle-Grenade et Ecuador (1886), as cited by Manual Paz and/or FelipePérez, who edited this edition of the atlas. Karsten defined four epochsin Earth history: Primera – without life – primary crystallinerocks, Segunda – with only marine life – chiefly sedimentaryrocks, Tercera – with terrestrial quadrupeds and fresh water lifeforms life – chiefly sedimentary rocks, and Cuarta – mankindappears, includes diluvial (glacigenic) and post-diluvial terranes. He notedthat Colombia is composed of chiefly of Quaternary, Tertiary and Cretaceousplutonic, volcanic and sedimentary rocks, and that Earth's internal heat(calor central) accounted, by escape of inner gases, for volcanism,seismicity and uplift of mountains. Karsten's regional mapping andinterpretation thus constitutes the primary source and ultimate pioneeringgeologic research.
机译:19世纪末,德国植物学家和地质学家Hermann Karsten(1817-1908)出版了 NuevaGranada (今天的哥伦比亚,巴拿马以及委内瑞拉和厄瓜多尔的部分地区)的区域地图。由阿古斯丁·科达齐(AgustínCodazzi,1793年至1859年)合并而成,他是意大利人,曾移民到委内瑞拉和哥伦比亚担任政府制图师和地理学家,当时他的著作《哥伦比亚共和国历史地图集》(1889年)。这本1889年地图集提供的地质图和大多数观测资料取自Karsten'sGéologiede l'ancienne Colombie bolivarienne:Vénézuela,Nouvelle-Grenade et Ecuador (1886年),如Manual Paz和/或FelipePérez所引用编辑了此版本的地图集。卡斯滕(Karsten)定义了地球历史上的四个时代: Primera –没有生命–初级结晶岩 Segunda –仅具有海洋生物–主要是沉积岩, Tercera –陆地四足动物和淡水生物构成了生命-主要是沉积岩,而 Cuarta –人类则出现了,包括冲积(成冰川)和冲积后的地层。他指出,哥伦比亚主要由第四纪,第三纪和白垩纪的云母,火山岩和沉积岩组成,地球的内部热量(热量中心)是由内部气体逸出造成的,火山作用,地震作用和山。因此,Karsten的区域制图和解释构成了主要的地质资源和最终的开拓性地质研究。

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