description Charles Lapworth Overview
Charles Lapworth was an English geologist who resolved the contentious Ordovician-Silurian boundary dispute in 1879 by defining the new Ordovician geological period. He achieved this by using graptolite fossils to establish detailed biostratigraphic zones in the Southern Uplands of Scotland. Lapworth's work laid the foundation for modern stratigraphic practices, demonstrating how fossil assemblages can be used to date and correlate rock layers.
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What is Charles Lapworth famous for in geology?
Charles Lapworth is best known for resolving the highly contentious Ordovician-Silurian boundary dispute in 1879. He achieved this by defining an entirely new geological period, the Ordovician, based on detailed fossil evidence.
How did Charles Lapworth discover the Ordovician period?
Lapworth extensively studied graptolite fossils in the Southern Uplands of Scotland. By mapping these fossils in distinct, overlapping biostratigraphic zones, he proved there was a distinct geological time period between the Cambrian and Silurian.
Where did Charles Lapworth conduct most of his geological work?
Much of Lapworth's foundational work was conducted in the rugged Southern Uplands of Scotland. He later became a prominent professor of geology at the University of Birmingham.
What award did Charles Lapworth receive for his geological work?
Lapworth received the prestigious Royal Medal from the Royal Society in 1891 for his groundbreaking research in paleontology. He was also awarded the Wollaston Medal by the Geological Society of London in 1899.
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