Curiously-arranged stones say it used to be much colder, and not that long ago.
Laramie winters are cold, with daily highs generally below freezing. Winds blow hard, often 30 to 40 mph, gusting to 50, 60, even 70. When arctic air masses visit, temps drop well below zero (F) and we post numbers and pictures on Facebook to show what we have to endure. But we shouldn't brag. Our local rocks and dirt tell us that Laramie weather could be much worse.
Twelve thousand years ago—a mere blink of a geologic eye—an ice sheet covered North America as far south as today’s central Montana, North Dakota, and eastern South Dakota. It never reached Wyoming, but we weren’t exempt from the bitter cold. Most of our basins contained permafrost, with only the uppermost soil melting in summer. When it refroze, expansion cracked the surface, year after year, creating networks of polygons. Now they’re buried under soil, except where fortuitously revealed by disturbance.
Relic frost polygons exposed during road construction at Crescent Junction, Wyoming (Mears 1987).
Frost wedges (polygons in cross-section) at the Rawlins city dump (Mears 1987; arrows added).
In the mountains, it was cold enough that snow survived summer melting. It accumulated, turned to ice, and began to flow, as glaciers. In the Medicine Bow Mountains west of Laramie, alpine glaciers merged into an ice cap across most of the crest, except for the highest part—the Snowy Range, a long steep-sided ridge of hard quartzite. Glaciers scratched and polished the rock only at the base; snow and ice didn’t accumulate above, at least not enough to form glaciers.The Snowy Range stood above the alpine ice cap (SH Knight 1990).
Field assistant cavorts on the gently-rolling crest of the Medicine Bows; Snowy Range behind.
Though unglaciated, the Snowy Range was not immune to cold. Frigid conditions left their mark in other ways, most obviously the abundant felsenmeer (rock seas)—massive accumulations of boulders created by water! Bit by bit, expansion with freezing shattered solid quartzite into huge jumbled piles of angular blocks.The trail to the summit of Medicine Bow Peak repeatedly crosses felsenmeer, fortunately via paths built by trail crews. The summit itself is a giant rockpile.My old pal Sparky takes a break en route to Medicine Bow Peak.
Final section of trail to the summit. See any patterns in the plants and rocks in the foreground?
Emmie summits Medicine Bow Peak, her first ascent.
Just before the final push to the summit, the trail crosses a saddle underlain by a basalt dike (older sources call it diorite). Basalt is softer than quartzite and weathers more easily, explaining the low area with soil. Short alpine plants form turf among lichen-covered rocks—a meadow of sorts.View of meadow from summit trail, in late August.
Meadow on basalt dike; older sources call it diorite.
Dike from below, near Sugarloaf trailhead.
From the right perspective, one sees that rocks in the little meadow are not randomly scattered. They outline polygonal patches of vegetation. Sound familiar? Yes, these are permafrost features—stone nets. Rocks and dirt were sorted, by annual freeze-thaw. Currently, active stone nets are common in Alaska, northern Canada, and other places with permafrost.Sorted rocks are covered in lichen, suggesting they haven’t moved in awhile.
Developed soil, vegetation, long plant roots, and lichen-covered rocks indicate these stone nets are no longer active. But that could change. If another glacial episode were to override our global warming, stone nets and frost wedges would grow again. And here in Laramie, it may not have to be all that much colder!Blizzards often close I-80, filling Laramie with trucks. Would life go on if glacial times returned?
• • •
Thirty-three years have passed since we lined up along a ditch to admire relic frost wedges, but the memory is still vivid. It was early October and snowing Laramie snow—horizontal with the wind. Doc Mears spoke of Pleistocene times 12,000 years ago, his strong baritone easily penetrating the howling wind, while we took notes as best we could with wet cold shivering hands. “I estimate the average annual temperature need drop just 10º C for a return to full periglacial conditions,” intoned Mears. None of us doubted it!
Dr. Brainerd “Nip” Mears, Jr. at Hanna Junction, 1970. Mears’s discovery of relic ice wedges was a major contribution to our understanding of Wyoming paleoenvironments. Photo by Wayne Sutherland.
Sources (in addition to links in post)Knight, SH. 1990. Illustrated geologic history of the Medicine Bow Mountains and adjacent areas, Wyoming. Geological Survey of Wyoming Memoir 4. PDFMears, B, Jr. 1962. Stone nets on Medicine Bow Peak, Wyoming. Short note, University of Wyoming Contributions to Geology (p. 48).Mears, B, Jr. 1987. Late Pleistocene periglacial wedge sites in Wyoming: an illustrated compendium. Geological Survey of Wyoming Memoir No. 3. PDFMears, B, Jr. 2001. Glacial records in the Medicine Bow Mountains and Sierra Madre of southern Wyoming and adjacent Colorado, with a traveler's guide to their sites. Geological Survey of Wyoming Publ. Info. Circ. No. 41. PDF