Imagine a world where pigeon-sized dragonflies soar above spiders with half-meter-long legs, where 2-meter-long millipedes slither and 20-kilogram scorpions hunt. About 300 million years ago, such surreal creatures thrived; today, rocks hint at how these and other creatures in the deep past lived. These clues allow geologist and writer John Dvorak to vividly re-create ancient landscapes in How the Mountains Grew: A New Geological History of North America.
Far from a dusty tome plodding through plate tectonics, the book teems with life as Dvorak establishes inextricable links between geology and biology. Take the oversize dragonflies and millipedes now preserved as fossils. Rocks of a similar age hold evidence of a rise in atmospheric oxygen that helps explain how these animals grew so large.
The book zigzags from place to place on a chronological, continental-scale field trip. To avoid dizzying readers, Dvorak revisits certain sites that preserve multiple threads of geologic history. For instance, at Mount Rushmore in South Dakota’s Black Hills, he describes how, about 2 billion years ago, molten rock rose and lodged itself into sedimentary rocks deposited on the seafloor of bygone oceans. Today, presidents’ faces stare out from this now-solidified magma, those ancient oceanic sediments sitting just below the visage of George Washington. The book later returns to glimpse younger seas that came and went, depositing sediments now replete with fossils. All these rocks, Dvorak explains, whisper stories of how this particular mountain grew.
Far from a dusty tome plodding through plate tectonics, the book teems with life as Dvorak establishes inextricable links between geology and biology. Take the oversize dragonflies and millipedes now preserved as fossils. Rocks of a similar age hold evidence of a rise in atmospheric oxygen that helps explain how these animals grew so large.
The book zigzags from place to place on a chronological, continental-scale field trip. To avoid dizzying readers, Dvorak revisits certain sites that preserve multiple threads of geologic history. For instance, at Mount Rushmore in South Dakota’s Black Hills, he describes how, about 2 billion years ago, molten rock rose and lodged itself into sedimentary rocks deposited on the seafloor of bygone oceans. Today, presidents’ faces stare out from this now-solidified magma, those ancient oceanic sediments sitting just below the visage of George Washington. The book later returns to glimpse younger seas that came and went, depositing sediments now replete with fossils. All these rocks, Dvorak explains, whisper stories of how this particular mountain grew.
