Junction of granite and limestone
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Junction of granite and limestone
Fig 88 from Principles of Geology, being an attempt to explain the former changes of the Earths surface. Vol. 3 1832-33 by Charles Lyell (1797-1875)
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1797 1875 Boundary Diagram Geological Geology Granite Igneous Intrusion Intrusive Intrusive Rock Junction Limestone Lyell Section Sedimentary Sedimentary Rock Sir Charles Lyell Principles Of Geology Sir Charles
EDITORS COMMENTS
Fig. 88: A Geological Section through the Junction of Granite and Limestone - An Illustration of the Intrusive Processes Described in Sir Charles Lyell's 'Principles of Geology' (Vol. 3, 1832-33) This geological diagram, Fig. 88 from Sir Charles Lyell's seminal work 'Principles of Geology' (Vol. 3, 1832-33), offers a fascinating glimpse into the intricacies of Earth's geological past. The image illustrates the junction of granite and limestone, a boundary that bears testament to the dynamic and ever-changing nature of our planet's surface. Sir Charles Lyell (1797-1875), a pioneering Victorian geologist, meticulously documented the geological features of his time, providing the foundation for modern geological thought. In this diagram, Lyell highlights the intrusive nature of granite, a type of igneous rock, as it forces its way up through the existing sedimentary layers, such as the limestone, resulting in a striking juxtaposition of rock types. The intrusive process, as depicted in the diagram, is a testament to the powerful geological forces at play during the 19th century. The granite, originating from molten magma deep within the Earth, cools and solidifies as it rises, eventually forming a solid mass. As it intrudes into the surrounding sedimentary rock, it causes the limestone to deform and fracture, creating a complex geological section. This diagram is a visual representation of the cross-sectional view of the geological formation, offering valuable insights into the intricate relationships between different rock types and the geological processes that shaped our planet. The intricate details and precise labeling in this diagram reflect the meticulousness and rigor of Sir Charles Lyell's scientific approach, making it an essential contribution to the field of geology in the 19th century.
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