El geólogo escocés Archibald Geikie defendió la teoría de la erosión de la superficie terrestre por acción fluvial, agentes de meteorización y hielo durante las edades de hielo repetidas, reemplazando la visión predominante de la escultura submarina. También investigó la actividad volcánica pasada, organizando cronológicamente las erupciones de Escocia y reconociendo discordancias significativas en sus antiguas capas de arenisca. Sus extensos escritos incluyeron textos fundamentales sobre geología, biografías de científicos colegas y exploraciones de paisajes geológicos e historia volcánica, consolidando su legado como una figura clave en las ciencias de la Tierra.
This volume offers a detailed exploration of Great Britain's ancient volcanoes, presenting insights from the original 1897 edition. It features high-quality reprints that maintain the integrity of the original text, providing a valuable resource for those interested in geology and the historical context of volcanic activity in the region. The work serves as a comprehensive reference for both enthusiasts and scholars studying the geological features of Great Britain.
Featuring a facsimile reprint of a scarce antiquarian work, this edition preserves the original's cultural significance despite potential imperfections like marks and flawed pages. It reflects a commitment to protecting and promoting literature by making historical texts accessible in high-quality modern formats. Readers can expect an authentic experience that honors the original while acknowledging its age.
This authoritative textbook provides a comprehensive overview of geology, covering everything from the structure of the Earth to the formation of rocks and minerals. With clear explanations and vivid illustrations, this is an essential resource for students and professionals alike.
A fascinating look at the geology of Scotland, as seen through the eyes of renowned geologist Archibald Geikie. The book focuses on a single boulder that Geikie discovered in the Scottish Highlands, which he used as a lens through which to view the region's complex geological history.
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