If you’ve lived in Laramie long, you know why we’re here: 150 years ago, the Union Pacific passed through the Laramie Valley during construction of the nation’s first transcontinental railroad.

But that’s only part of the story. The full explanation begins much earlier, back when a fortuitous combination of mountain-building and erosion created an easy route over the Laramie Mountains — the Gangplank.

One hundred million years ago, much of Wyoming was underwater, covered by the Western Interior Seaway, which split the continent from north to south. But it was not to last. Thirty million years later the land began to rise, forcing the sea to retreat. This was when the Laramie Mountains were born, part of a long and widespread episode of mountain-building that created most of the Rockies.

For the next 10 million-15 million years, the Laramie Mountains rose, while at the same time erosion wore them down. Such is the fate of mountains — as soon as uplift starts, erosion sets in. As much as 20,000 feet of material is thought to have been removed from the crest of the range. Streams and wind carried down the debris, depositing it on the flanks and eventually burying the Laramie Mountains in their own rubble.

It’s hard to imagine such huge changes: a sea disappearing, mountains rising, mountains worn down and buried. But at the scale of geologic time, the Earth’s surface is dynamic, always changing. This we know, though we can’t always explain why. Many mysteries remain … for example, today’s Laramie Mountains.

Ten million years ago, when the range was mostly buried beneath a thick covering of sedimentary rocks, the east flank was a broad gently-sloping plain. That’s not the case today (think Sybille Canyon); obviously, something happened. We know erosion resumed, but why? Perhaps the entire region was uplifted, invigorating streams. Maybe climate change brought greater precipitation. Whatever the reason, the sedimentary cover was removed during what geologists call the Great Exhumation. The Laramie Mountains were disinterred … almost.

Because of a serendipitous evolution of topography, the Great Exhumation left intact a gently- sloping wedge of sedimentary rocks in the southeast part of the range. Several million years later, on Sept. 21, 1865, General Grenville M. Dodge, soon-to-be chief engineer of UP at the time, scrambled up the ridge south of Crow Creek and found himself on this wedge. He was ecstatic. Here was an easy route up the Laramie Mountains, later christened “the Gangplank.”

Just two years later, on the evening of Oct. 12, 1867, UP tracklayers entered today’s Wyoming. They barely paused at Cheyenne, pushed west up the Gangplank, wound down into the Laramie Valley, and in early May 1868, reached Laramie City. Eager new residents had just thrown up buildings, joining the substantial UP shops started months before and the pioneers who were here before the trains arrived. Then, the tracklayers raced west, laying some 350 miles of track and establishing numerous “instant towns” before leaving Wyoming early in 1869.

The Gangplank is most striking at its western tip where the younger sedimentary rocks meet the ancient Sherman Granite. Only a few hundred feet separate the drainages of Crow and Lone Tree Creeks, and, though imperceptible to us, these streams are hard at work. Every year, they erode a bit more rock and soil, sending it down to the North Platte River, the Missouri, and eventually the Gulf of Mexico. In other words, the Gangplank won’t be here forever. You might want to take a look at it while you still can.

From Laramie, follow Interstate 80 east to the Summit and the Sherman Granite, which forms the crest of the range. This is ancient rock — formed from magma 1.7 billion years ago. It was exposed much later during uplift of the Laramie Mountains. Interstate 80 stays on Sherman Granite past Blair, Vedauwoo, Tree-in-the-Rock and Buford. Here, the terrain is relatively flat, and it’s tempting to think this is the Gangplank. But road cuts and occasional blobs of granite show otherwise.

Continue past Remount Road (Exit 339) and Harriman Road (Exit 342, large quarry). Just a short distance further, before the Wyoming Department of Transportation sand/salt storage structure, is the transition to the Gangplank. But don’t slow down — I-80 traffic is too heavy and fast for gawking. Instead, continue about 3 miles to Exit 345; drive to the truck parking area on the Gangplank.

At the east end of the parking area is a sign illustrating the Gangplank rising from the Great Plains onto the Laramie Mountains. The text makes more sense when you realize the sign originally stood at the west end of the Gangplank (you’ll be there soon). The slope next to the parking area reveals some of the sedimentary rocks that covered the range 10 million years ago, before the Great Exhumation.

After mastering the diagram on the sign, find the westbound frontage road at the opposite end of the parking area. Set your trip meter to zero and drive the Gangplank. At 2.0 miles, just past Mile Marker 2 (green) and near the top of the hill, you will leave the 10-million-year-old sedimentary rocks and return to the ancient Sherman Granite. Here, at the tip of the Gangplank, you can straddle more than a billion years of Earth history.

From the hilltop, the view east toward Cheyenne gives a good feel for how narrow this end of the Gangplank is. The north side (left) drops steeply down to the South Fork of Crow Creek. Lone Tree Creek is off to the south (not visible here). In the distance, the Gangplank widens and merges with the Great Plains in Nebraska.

More points of interest on the Gangplank, and additional driving tours of railroads past and present, are included in Railroads of Albany County — Tracking the Past. This free brochure is available at the Laramie Area Visitor Center and the Historic Railroad Depot. A scanned version is available at: www.laramiedepot.org/about/railroadsofalbanycounty/tabid/76/default.aspx

Editor’s note: This is one in a series written for the Albany County Museum Coalition that promotes interest in local cultural and natural history. Hollis Marriott came to Wyoming in 1977 to work at Devils Tower National Monument, fell in love with the wildness of the state, and stayed. She received a master’s degree in botany from UW in 1985. Now retired, she indulges her passions for botany and geology, and blogs about both at In the Company of Plants and Rocks (www.plantsandrocks.blogspot.com).

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