In mid-August, Becca and I dropped our kayaks into the Willamette River just north of Corvallis for an afternoon paddle to Albany. The river was filled with canoeist, kayaks, rafts, and inner tubes of various makes, colors and conditions. The river was lazy and slow and our kayaks occasionally scrapped river bottom gravels because of the low flows. I remember on February 8th, 1996 when the waterfront of Corvallis was a sea of umbrellas as citizens excitedly watched the river spill over its banks and flood the eastside. Greater Willamette River floods in 1964 and 1943 discharged far more water. A massive flood in 1861, during Corvallis’s early history, covered over 320,000 acres and washed away many emerging communities. The dams that block the McKenzie, Middle Fork of the Willamette and Santiam Rivers have done the work intended by the army engineers who constructed them so we will not likely experience a flood like 1861. However, I cannot but think the river a few tricks up its sleeve and may again surprise us with its power.
The Pleistocene floods that ravaged the Pacific Northwest were likely some of the most dramatic hydrologic events in earth’s history. Huge glaciers blocked canyons of the Clark Fork River in Idaho and created an enormous 3000 sq mile lake referred to as Lake Missoula. As the glaciers periodically receded the giant lake emptied in massive floods that inundated vast stretches of the Pacific Northwest. The waters surged through the Columbia Gorge transforming the landscape and depositing gravel and giant Pleistocene granite boulders from Montana and Idaho on the low hills and valley floors in the Willamette Basin. The Willamette Valley became a lake, 100 miles long, 60 miles wide and hundreds of feet deep. Geologists suspect that the floods occurred dozens of times over a period of 6,000 years during the Pleistocene with the last event perhaps 13,000 years ago. Another lake, Lake Bonneville, in the present day site of the Great Salt Lake, may have created another massive flood 14,000 years ago that ripped through Hells Canyon and into the Columbia Gorge. The Bonneville and Missoula floods left massive deposits of sediment on the valley floors of the Willamette Basin. There is evidence that humans resided in the Pacific Northwest during the latter periods of the giant floods and perhaps fished and encamped along the lake shores formed by the flood waters.
Bob Duncan, a geologist and geophysicist from Oregon State University, led a tour of Bald Hill Farm this July. Bob grasps the nature of events that span millions of years including the evolution of ocean basins, and the formation of ocean crusts and coastal mountain ranges. While most of us focus our imaginations on our next meals or weekend hikes, Bob’s imagination must roam across geologic epochs. The descriptions of his research and publications includes many wonderful words that I love to say such as “petrogensis” (dealing with the origins of rock particularly igneous rocks), “ophiolite” (serpentine, pillow lava, and chert rock typical of the upper mantel of the earth’s oceanic crust), “mafic” (rock that is rich in magnesium and iron), and “celadonites” (another rock type in the mica group that forms massive prismatic crystallites or clay aggregates), but had to look up to gain some basic understanding of their meanings. The tour provided a brief glimpse of the underlayments of the land that we walk on and, for the most part, take for granted.
The geomorphology of the Willamette Basin and our community shaped the natural history of the ecoregion and is deeply intertwined with eruptions of huge shield volcanos in the Cascades between 17 and 6 million years ago that flooded the valley with basalt, and the ice sheets that covered and etched the valley floor and hillsides for thousands of years. Bob also mentioned that until fairly recently many geologists assumed that the Pacific Northwest was reasonably secure from massive earthquakes similar to the latest one in Japan, but now the data clearly suggests that Washington and Oregon will likely experience a massive 9.0 or greater earthquake perhaps within the next 50 years. This super quake may last for up to 4 minutes and create tsunamis that inundate our coastal communities.
We take for granted that our grand structures such as dams and skyscrapers are incomparable monuments, but compared with the landforms shaped by lava flows, historic floods, and ice sheets, they are inconsequential.