What do you think?
Rate this book


368 pages, Kindle Edition
First published December 1, 2017

In nearly all rocks younger than the Archean, the most common sandstones are largely made of the durable mineral quartz, the most common mineral on the earth’s surface. This is because most other minerals (such as feldspars, which make up the bulk of most kinds of igneous rocks) are broken down quickly by chemical weathering. Quartz, on the other hand, is chemically inert (it’s just silicon dioxide, SiO2), plus it has no cleavages to break it into fragments, as feldspars do.
The final event was the collision of the African portion of Gondwana with the East Coast to crumple up the Appalachians in the Late Carboniferous (Pennsylvanian). This event also closed the predecessors of the Atlantic for good, and joined Laurentia or North America to the supercontinent of Pangea. The Appalachians were formed in this huge Himalayan-style collision over 300 millions of years ago and have been slowly eroding ever since.