Authors:
Historic Era: Era 6: The Development of the Industrial United States (1870-1900)
Historic Theme:
Subject:
April 2000 | Volume 51, Issue 2
Authors:
Historic Era: Era 6: The Development of the Industrial United States (1870-1900)
Historic Theme:
Subject:
April 2000 | Volume 51, Issue 2
They moved our house to mine the earth it sat upon. They didn’t move just our house, but the entire town of Climax, Colorado. By the end of 1962, more than 205 homes had come down the 13-mile stretch of Highway 91 to the town of Leadville. Moving back to Leadville returned my father to his roots; he is the third generation of Fitzsimmonses to live there, and I am part of the fourth. Fitzsimmonses have been in Leadville since it was a bustling and refined mining town—or at least as refined as a mining town could be.
More than a century after its fame, Leadville reveals through exuberant storefronts and tall mine headframes the spirit of the people who built it. Follow Highway 91 south roughly twenty-five miles from Interstate 70 and the Copper Mountain Ski Resort, and you will meet Leadville, full of superb scenery and history. About halfway there, you’ll pass the Climax Molybdenum Mine. Here at the top of Fremont Pass was once a town, with post office, ski area, bowling alley, shopping center, schools, and movie theater. Climax, named after a narrow-gauge railroad station that first occupied the site, is now but a shadow of the immense center it once was, just as Leadville is an echo of the extraordinary city of its past.
Set in the upper Arkansas River Valley in nearly the middle of Colorado, Leadville has a robust elevation of 10,200 feet, making it the highest incorporated city in the United States. On each side regal mountain ranges offer constantly changing views. To the east stands the Mosquito Range; to the west, the Sawatch, home to the two highest peaks in the state. Mount Elbert measures 14,433 feet and Mount Massive, 14,421.
Leadville’s story, as with all mining towns, begins with geology. The mineralization around the city, created by rich hydrothermal solutions seeping into local geologic faults, is diverse—ranging from gold and silver to zinc and iron. More noticeable to the traveler than the geology, though, is Leadville’s weather. Winter comes in to stay by mid-October, but only after the explosion of aspen color and wildlife activity that is autumn; by the time May puts an end to the season, more than two hundred inches of snow will have fallen on Leadville. Yet we rarely endure more than four days without seeing the sun, and usually the snow-covered mountains accentuate an azure sky.
When gold was discovered in 1858 along the banks of Cherry Creek, near modern-day Denver, hopeful souls thronged to Colorado, seeking to repeat the California rush of 1849. In April of 1860, near the end of a long winter, Abe Lee and his companions crossed the snowy Mosquito Range, entering into the upper Arkansas River Valley, and prospected in the gulches upstream. It was Lee who discovered gold at the top of the Arkansas River