Next, we're heading down to the river, to the old station at the bottom of the gorge.
People living near the gorge knew about its coal long before anyone mined it on a large scale. It showed in the cliffs, and Native Americans and early settlers may have gathered some of it for their own use. But the big seams sat mostly untouched until 1873, when the Chesapeake and Ohio Railway finished its line through the gorge.
That railroad changed everything. Suddenly the seaports of the East were connected, through this gorge, to Cincinnati, Saint Louis and Chicago. Businessmen moved in fast and opened mines. The railroad became the gorge's highway, linking towns that could hardly be reached any other way. African Americans came up from the South, and thousands of European immigrants came looking for work and a better life. There were so many trains that people down here could read the morning paper from Richmond or Cincinnati on the day it was printed. In 1910, more than two hundred people a day passed through the new train station at Thurmond, upriver.
The mines were built high on the walls of the gorge, and chutes and conveyors carried the coal down to the tracks. By 1905, about seventy-five mines were working in the gorge, between there and Hawks Nest.
Two of the towns grew up at the bottom of this road, one on each bank: Fayette, and South Fayette across the river. Fayette began with a landowner named Martin Blume. He sold the railroad the right to build through his land, and as part of the deal, he and his descendants could ride the trains for free, for as long as they ran. That bargain lasted more than a century. By 1875, two years after the first train, his town already had a post office, a depot, a store and a saloon. The town also had a three-story store, and even a garage where people left their cars while they traveled by train.
In the late 1800s, this road was unpaved, carried traffic both ways and was never plowed in winter. Mudslides were a constant problem, and they still are.
All the while, water trickles down through these hillsides, through layers of shale, sandstone and coal, and into the creeks that feed the river. One old mine on this slope, the Ajax, is now a honeycomb of flooded tunnels. And the river below has a long way to go. It starts in the mountains near Blowing Rock, North Carolina, and flows north. Past this gorge, it joins the Gauley to form the Kanawha, which runs to the Ohio, then the Mississippi. A drop of water from a spring on this slope may end up in the Gulf of Mexico.