The town of Spruce Pine, North Carolina, doesn’t have a lot to say for itself. Its Web site, which features a photo of a flowering tree next to a rusty bridge, notes that the town is “conveniently located between Asheville and Boone.” According to the latest census data, it has 2,332 residents and a population density of 498.1 per square mile. A recent story in the local newspaper concerned the closing of the Hardee’s on Highway 19E; this followed an incident, back in May, when a fourteen-year-old boy who’d eaten a biscuit at the restaurant began to hallucinate and had to be taken to the hospital. Without Spruce Pine, though, the global economy might well unravel.
Spruce Pine’s planetary importance follows from an accident of geology. Some three hundred and eighty million years ago, during the late Devonian period, the continent of Africa was drifting toward what would eventually become eastern North America. The force of its movement pressed the floor of a Paleozoic sea deep into the earth’s mantle, where, in effect, it melted. Over the course of tens of millions of years, the molten rock cooled to form deposits of exceptionally pure mica and quartz, which were then pushed back up toward the surface. In the twentieth century, Spruce Pine’s mica was mined to make windows for coal-burning stoves and insulation for vacuum tubes. In the computer age, it’s the town’s quartz that’s critical.
Diese Geschichte stammt aus der October 30, 2023-Ausgabe von The New Yorker.
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Diese Geschichte stammt aus der October 30, 2023-Ausgabe von The New Yorker.
Starten Sie Ihre 7-tägige kostenlose Testversion von Magzter GOLD, um auf Tausende kuratierte Premium-Storys sowie über 8.000 Zeitschriften und Zeitungen zuzugreifen.
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