Work on The Principles of Geology is “interrupted,” and Charles Lyell investigates the nature and formation of loess deposits

Pub Date : 2020-03-01 DOI:10.1016/j.endeavour.2020.100718
Ian Smalley
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Abstract

Charles Lyell's life work, the influential textbook and philosophical treatise The Principles of Geology, helped to shape the Victorian age. There were few diversions from the central task of the Principles of Geology in the course of the twelve editions. Perhaps the most significant and notable was the discovery and investigation of loess; a silty sediment, often of considerable thickness, and widely distributed in the Rhine valley. He made a significant contribution to loess studies and, with his father-in-law, Leonard Horner, explored the loess regions of the Rhine Valley. The loess period lasted roughly from 1830 to 1836, and he established the first paradigm theory for the formation of loess deposits from deposition in a lake or perhaps from slow-moving water. This held sway until displaced by the aeolian theory of F. von Richthofen.

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《地质学原理》的研究工作被“中断”了,查尔斯·莱尔研究了黄土沉积物的性质和形成
查尔斯·莱尔的毕生著作——颇具影响力的教科书和哲学专著《地质学原理》,帮助塑造了维多利亚时代。在12个版本的过程中,很少有偏离《地质学原理》中心任务的地方。也许最重要和最值得注意的是黄土的发现和调查;一种粉质沉积物,通常相当厚,广泛分布于莱茵河流域。他对黄土研究做出了重大贡献,并与他的岳父伦纳德·霍纳(Leonard Horner)一起探索了莱茵河流域的黄土地区。黄土期大致从1830年持续到1836年,他建立了第一个范例理论,说明黄土沉积物是由湖泊沉积或缓慢流动的水形成的。这种理论一直占据主导地位,直到被f·冯·里希特霍芬的风成理论所取代。
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