Climate and Time in Their Geological Relations
Published in the late 19th century, 'Climate and Time in Their Geological Relations' by James Croll examines the interplay between Earth's climate and geological phenomena, particularly focusing on glacial epochs and the distribution of life across different climatic zones. Croll presents a scientific analysis of secular climate changes, supported by established physical principles. This work is notable for its early contributions to climatology and geological time, influencing future studies in these fields.
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“In geology the effects to be explained have almost all occurred already, whereas in these other sciences effects actually taking place have to be explained.””
— James Croll
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<a href="https://lex-books.com/book/climate-and-time-in-their-geological-relations-b4f755ed-fca3-4a0c-bbd6-f618a1628ee0"><img src="https://lex-books.com/badges/read-on-lex.svg" alt="Read Climate and Time in Their Geological Relations by James Croll free on Lex" width="160" height="40"></a>[](https://lex-books.com/book/climate-and-time-in-their-geological-relations-b4f755ed-fca3-4a0c-bbd6-f618a1628ee0)[url=https://lex-books.com/book/climate-and-time-in-their-geological-relations-b4f755ed-fca3-4a0c-bbd6-f618a1628ee0][img]https://lex-books.com/badges/read-on-lex.svg[/img][/url]Read Climate and Time in Their Geological Relations by James Croll free on Lex: https://lex-books.com/book/climate-and-time-in-their-geological-relations-b4f755ed-fca3-4a0c-bbd6-f618a1628ee0Cite this book
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Croll, James. Climate and Time in Their Geological Relations. Lex, lex-books.com/book/climate-and-time-in-their-geological-relations-b4f755ed-fca3-4a0c-bbd6-f618a1628ee0.Croll, J. (n.d.). Climate and Time in Their Geological Relations. Lex. https://lex-books.com/book/climate-and-time-in-their-geological-relations-b4f755ed-fca3-4a0c-bbd6-f618a1628ee0Croll, James. Climate and Time in Their Geological Relations. Lex. https://lex-books.com/book/climate-and-time-in-their-geological-relations-b4f755ed-fca3-4a0c-bbd6-f618a1628ee0.
