Deadwood lies at the northern tip of the Black Hills, where the land is ancient and rubbed smooth by time. The Black Hills are more rugged at their southern extremity, where bare granite forms pinnacles and spires.
It has long been a fact familiar to geologists, that, both on the east and west coasts of the central part of Scotland, there are lines of raised beaches, containing marine shells of the same species as those now inhabiting the neighbouring sea.
All geologic history is full of the beginning and the ends of species-of their first and last days; but it exhibits no genealogies of development.
The Ozarks are old and worn mountains from the geological past.
Most of the Amazon basin is as flat as a pancake and laced with extravagantly meandering waterways. One school of thought holds that more than 145 million years ago, when Africa and South America were joined, the Amazon's main stem was connected to the Niger River and actually flowed in the opposite direction, toward the Pacific Ocean.
I can only tell where I feel most at home, which is in the erosional landscape of the red rock desert of southern Utah, where the Colorado River cuts through sandstone and the geologic history of the Earth is exposed: our home in Castle Valley.
The traces of upheavals become more impressive when one moves a little higher, when one gets even closer to the foot of the great mountain ranges. There are still plenty of shell layers. We notice them, even thicker and more solid ones.
Western Australia is covered by granite, the largest single piece of Achaean rock that still lies on the surface of the, of, of the Earth, that's 2.5 to 2.9 billion years old. It's one of the most ancient and intact bits of the Earth's crust.
