A branching root cast from grasses that grew on the ashy lahars deposited along the ancestral Missouri River system. Plant roots growing in calcareous soils made holes that were filled with calcite after the organics rotted away. (Photo by Rob Thomas via Yellowstone Caldera Chronicles.)
Volcanism in the Yellowstone region has generated a lot of ash over the last several million years. Rivers, including the ancestral Missouri River, have played an important role in distributing this ash across the landscape of southwestern Montana.
When we think of the Yellowstone hotspot, we commonly think of the volcanic scars left behind as the North American Plate slowly passes southwest over a stationary source of heat. However, deposits in the margins of the hot spot track are some of the most useful in reconstructing how caldera eruptions work and how this hotspot produced the complex landscape we see today.
When the Yellowstone hotspot started to feed eruptions near the intersect of Nevada, Idaho and Oregon some 16.5 million years ago (about the same time as the eruptions of the Columbia River Basalts initiated), it thermally bulged and extended the brittle crust around it, influencing the shapes of mountain ranges and valleys. From about 16.5 to 4.5 million years ago, the basins captured rivers, some of which flowed to the northeast into southwest Montana. Preserved in these sedimentary deposits is a spectacular story of a tumultuous time in southwest Montana. Let’s explore it!
For millennia, people have undoubtedly recognized the bright white layers of ash exposed in the mountain ranges in southwest Montana. Unlike many other ash deposits, these did not fall from the sky, but were carried from Idaho by gigantic flows of water and ash that flowed off the Yellowstone thermal bulge and down the ancestral Missouri River drainage. The viscous flows, called lahars, accumulated in the northeast-trending valleys created during the emergence of the hotspot, burying the valley floors in up to 100 feet (30 meters) of ash and rock debris. It appears that the lahars came in pulses, because the ash beds contain tabular blocks of ash that were deposited, rapidly hardened, and were subsequently peeled up and transported downstream by another pulse of ash and water. It’s hard to determine the time interval between pulses, but it was likely no more than hours to days. After deposition, grasses grew on the ash, making soils with abundant casts of the roots.
The origin of the ash is easy to explain given the explosive, silica-rich magma t
As the North American plate moved Montana to the southwest and the hotspot settled in under the crust south of Rexburg, Idaho around 6.5 million years ago, a basalt lava flow erupted and flowed down a northeast-trending valley as far north as Dillon, Montana. That flow, known as the Timber Hill basalt, was close to the last deposit that made it into Montana from the hotspot, because around 4.5 million years ago, the thermally raised terrain in the region started to collapse, forming northwest-trending extensional valleys and mountains that blocked and diverted the ancestral Missouri River into a maze of new northwest-and-northeast-
Today we are confident that most of the extensional topography of southwest Montana formed during the last 16.5 million years, and that the active ranges are northwest-trending and formed during the last 4.5 million years. The faults that raise the northwest-trending mountains are active, as shown by the 1959 Hebgen Lake (Quake Lake) earthquake, the largest recorded earthquake in the Rocky Mountains. So, as you drive around southwest Montana, look for the bright white layers of ash exposed high in the mountain ranges and contemplate that they were once deposited in the ancestral Missouri River as it flowed off of the Yellowstone thermal bulge many millions of years ago!
Yellowstone Caldera Chronicles is a weekly column written by scientists and collaborators of the Yellowstone Volcano Observatory. This week’s contribution is from Robert Thomas, Professor of Geology in the Environmental Sciences Department, University of Montana Western.
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