Geologic field trip from Yellowstone Lake to Portland, Oregon at 30,000 feet
What a start to the new year! January 1, I flew home to Oregon with a north-facing window seat on a spectacularly clear day. So much incredible landscape! So much incredible geology! Here are nine photos I shot out the plane window, keyed to the geologic map below.
Photo 1. Absaroka Range, northern Wyoming and southern Montana. You can see that these mountains consist of layered rocks (see bottom of photo especially)–but they’re not sedimentary. They are basaltic to dacitic lava flows and pyroclastic rocks of the Absaroka Volcanic Field, erupted from about 53-43 million years ago. Much of the present topography is the result of glacial erosion during the Pleistocene.
Photo 2. Yellowstone Lake. As you can see on the map, Yellowstone Lake fills only a fraction of the caldera created by Yellowstone’s Lava Creek Eruption, 600,000 years ago. Since then, rhyolite lavas, shown in pink, filled in the caldera. Notice the oval-shaped bay at the end of the lake’s western arm. It’s called West Thumb, and is a younger caldera that erupted about 150,000 years ago. It’s a caldera within a caldera! It’s pretty big too– almost identical in size to Crater Lake in Oregon –but compared to the main caldera, it’s tiny.
Photo 3. Recent faulting of the Basin and Range Province. In this photo, the Pahsimeroi River flows northwestward to its confluence with the Salmon River, near the left side of the photo –and the Salmon continues flowing northward for about 100 miles before it turns westward and eventually joins the Snake River.
But what I think is so cool about this photo is that it so clearly shows the abrupt western edge of the Lemhi Range, which runs diagonally from the right (east) side of the photo to just above the center. The range literally rises right out of the ground. That abruptness is caused by faulting that takes place recently and frequently enough that erosion doesn’t keep up with it. The fault is a normal fault, caused by crustal extension. Notice the linear nature of the ranges to the northeast (upper right) –More normal faulting! This is a northern expression of the Basin and Range Province. Woohoo!
Photo 4. Mountains of the Idaho Batholith. Granitic rock of the Idaho Batholith underlies a huge area of Idaho, some 14,000 square miles of it. On the geologic map, it’s the big green area. The rock intruded as a series of plutons during the Late Cretaceous, from about 100 – 65 million years ago. Similar in age and composition to the Sierra Nevada Batholith, the Idaho Batholith was fed by magma created during subduction along the west coast of North America.
Photo 5. Hell’s Canyon. Not only does the north-flowing Snake River in Hell’s Canyon form the boundary between Idaho and Oregon (Yay, we made it to Oregon!), and not only is it the deepest canyon in the conterminous United States, but it’s also incredibly important from a geologic-history-of-western-North-America point-of-view.
Notice the flat areas above the canyon–they’re especially visible on the west (left) side, but you can also see them on the east. Those places are flat because they’re made of flat-lying basalt of the Columbia River Basalt Group. These basalts erupted mostly between 17-14.5 million years ago, but kept erupting off and on until about 6 million years ago –and they cover ALL of northern Oregon and ALL of southeastern Washington State. In fact, they flowed all the way to the Pacific Ocean.
Those basalt flows overlie rock of the Wallowa accreted terrane: mostly volcanic and sedimentary rock that formed in an island arc setting, far offshore from North America. It was added (accreted) to the North American continent during the Mesozoic –probably some 150 million years ago.
Photo 6. Wallowa Mountains, Oregon. Just west of Hell’s Canyon are the Wallowa Mountains, Oregon’s premier alpine country outside of the Cascades. Like Hell’s Canyon, the Wallowas contain the accreted Wallowa terrane overlain by Columbia River Basalt –but the Wallowas also host the Wallowa Batholith, a Jurassic-Cretaceous granitic “stitching pluton”. It’s called a stitching pluton because it intrudes across accreted terranes and “stitched” them together.
You can see a bunch of other things in this photo though. First off, the mountains end suddenly in a line: a recently active fault zone that has uplifted them more than 5000′ relative to the valley floor. Also, you can see how glaciers carved the landscape. Notice the deep U-shaped valleys, cirques, and knife-edged ridges called aretes. And see the lake in the upper right corner of the photo? It’s Wallowa Lake, dammed by a glacial moraine!
(at this point, the folks in the seats next to me wanted to throw me out of the airplane)
Photo 7. View of Washington High Cascades over The Dalles. That’s Mt. St. Helens on the left (west), Mt. Adams in the middle, and Mt. Rainier in the far distant right. Mt. Rainier is 90 miles away!
These volcanoes are dormant –which means that they’re …sleeping? And they can awaken at any time. I remember a college friend of mine wanted to climb Mt. St. Helens in 1979. It was dormant then, and nobody worried about it. Then in May, 1980 it erupted violently, blowing off its top 2000′. Both St. Helens and Mt. Rainier have erupted many times in the past several thousand years; Mt. Adams though, erupted only twice in that period.
Photo 8. Columbia Gorge, the Washington High Cascades, and the Bonneville Landslide. From left (west) to right, the volcanoes are Mt. St. Helens, Mt. Rainier, and Mt. Adams. You can see the Bonneville Landslide along the river on the right side of the photo, directly below the left base of Mt. Adams. It detached from the cliffs directly behind it about 1450 A.D. and slid right into the river –and it pushed the river about a mile to the south! Just downriver from the landslide, you can see the Bonneville Dam zig-zagging across the river.
The ridges at the bottom of the photo lead up to Mt. Hood, another dormant stratovolcano and Oregon’s highest peak. Apparently, the view out the south side of the plane was even more ridiculously cool.
Photo 9. Columbia River, just below Portland. Right near Portland, the Columbia River turns northward for about 40 miles before it heads west again out towards the Pacific–and it drops only 10 feet in elevation for the whole distance. The northward deflection of the river is probably the result of uplift of the Portland Hills, which likely began as long as 16 million years ago (they also deflect 16 million year old lava flows of the Columbia River Basalt). That town along the river in the background is St. Helens, Oregon.
See more geologic photos of Oregon by typing “Oregon” into the geology search engine on my website –or type “Oregon, aerial” if you want to see aerial shots! And if you’re suddenly really excited about Oregon geology, please check out the new edition of Roadside Geology of Oregon!
Great. What camera did you use and how did you process the images? I’ve never had much joy taking pictures out of plane windows.
I’m reminded of a remark by Darwin (forget the exact words and context – does anyone reading this know them?) about how much more pleasurable it is to observe nature on the basis of scientific understanding.
So the people sitting next to you should have been offering to buy you drinks in return for a commentary.
LikeLiked by 1 person
Thanks! I use a Canon 5D Mark II and shoot RAW –way too much of a camera for shooting out of plane windows (and too heavy to carry around) –any good dslr would make good aerial shots –if it’s clear.
I process the images in lightroom and then Adobe Photoshop. Lightroom allows me to crop easily, semi-locally adjust exposure, and bump up the “clarity” –which diminishes atmospheric things like haze. And then in Photoshop, I adjust levels and sharpen the image.
How true about observing nature when you can recognize some things and know enough to ask questions!
And my comment about them throwing me out the window was just silliness on my part. The guy in the middle seat was really interested –but I did worry some that my all-too-frequent audible exclamations, followed by multiple camera clicks, was annoying!
Good stuff, good research, well done, and thanks!
Incredible photos combined with maps that allow even the geologically challenged (me) to understand and get excited. Thanks so much Marli Miller. What a gift!
Date: Sun, 11 Jan 2015 15:10:17 +0000 To: email@example.com
Outstanding photos! Excellent commentary. Thanks.
Marli maybe you should do a Skyside Geology of North America for all those airline magazines.
LikeLiked by 1 person
Nice work. The moderate snow seems to improve the “3D” appearance of the photos. Thanks for sharing.
LikeLiked by 1 person
Pingback: Columbia River Basalt Group–outrageous! | geologictimepics
The zig-zagging directly below the Bonneville landslide is Bonneville Dam. The northernmost zig is the site of the newest bank of generators, damming a channel that was excavated for their placement. Cascade locks is further downstream.
I admire your work! Great redo of Roadside Geology!
LikeLiked by 1 person