Excerpt from The Climatic Changes of Later Geological Times: A Discussion Based on Observations Made in the Cordilleras of North America
The Continental Masses have, with the Lapse of Geological time, been growing larger, 205. Reference to the Maps of Delesse, 206. Manner in which Detri tal Materials accumulate, 207. How the Continents have been built up, 207, 208. A Gain of Land the Necessary Result, 208. Permanence of the Ocean inferred from its great depth, 209. Stability Of the Continents a necessary couse quenco, 207. Mean Elevation of the Land Masses of the Globe, 209. Persist ence of Areas of Elevation and Depression first enunciated by Dana, 200. Geo logical Growth Of North America, 211 of Asia, 211. Foster and W'hitney, quoted, 211. - Evidence of the Stability of the Oceanic Areas derived from the Character of the Sea Bottom, 214-216. Investigations of Agassiz, 214. Views of A. Geikie and W. B. Carpenter, 215. Summary of the Evidence, 216. - Inquiry whether the Increase of the Continental Masses is Sumcient Cause for the Desiccation proved to have taken place, 216 - 219. Probable Effects on precipitation of Changes, in the form of the Land Masses, 217. Higher temperature suggested as a cause of former Greater Precipitation, 218.
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Paperback. Condition: New. Print on Demand. This book delves into the dramatic changes in climate that have occurred throughout the Earth's history, focusing on the glacial and post -glacial eras. The author, a prominent geologist of his time, challenges traditional assumptions about the role of glaciers in shaping the Earth's surface. Drawing upon his extensive fieldwork in the Cordilleras of North America, the author argues that glaciers are less powerful erosive forces than previously believed and that much of the geological work attributed to them is actually the result of water action. He further examines the cyclical nature of climate change, meticulously detailing evidence of past periods of intense precipitation, ice expansion, and subsequent desiccation. The book's insights extend beyond the Cordilleras, exploring similar patterns of climate change across continents, from the Himalayas to the Scandinavian Range, and ultimately challenging prevalent theories about the causes and consequences of the so -called "glacial epoch." Through detailed analysis of geological evidence and rigorous examination of prevailing scientific views, the author presents a compelling argument for a more nuanced understanding of the complex relationship between climate, geological processes, and the evolution of the Earth's landscapes. This book is a reproduction of an important historical work, digitally reconstructed using state-of-the-art technology to preserve the original format. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in the book. print-on-demand item. Seller Inventory # 9781330668320_0
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