Relive Important Archive Articles

A large number of important articles get buried over time as new articles are added to our website, so here’s a chance to review and relive some of our most important articles. We think you might enjoy reviewing these timeless features.

Hiking Drumheller Channels

Hiking Drumheller Channels Ice Age Floods National Geologic Trail There are scads of hiking trails all through Drumheller Channels National Natural Landmark. On a cloudy day in early June we took off on a couple of exploratory hikes that were simply amazing. We first proceeded south from the parking lot at Lower Goose Lake, running through late Spring wildflowers, eventually looking for one of Bruce Bjornstad’s geocaches. We wandered over hills and down into deeper valleys, always surrounded by the towering walls of basalt defining that section of Drumheller Channels. Along the way we found an area of apparent Kolk depressions with odd spires of basalt poking up out of the middle of a central mound. Soon we passed through a reedy area that bounded the southern edge of Lower Goose Lake. We continued on south to the edge of Black Lake where the geocache was supposed to be, but after 20 minutes with 4 of us looking in the area of the GPS coordinates, we finally decided the cache was no longer there and headed back. The hike was easy, very pleasant, and mercifully cool due to the cloudy morning. We then drove north across the O’Sullivan Dam, and back south through Columbia National Wildlife Refuge to the W. McManamon Road entrance to Crab Creek Marsh Unit #3 and the Basalt Columns at Drumheller Trailhead, the kickoff point to go to the top of “Nick’s Columns”. Nick Zentner’s videos about the columns are great, but the blooper where his rock hammer falls down between columns is priceless. We just had to see those columns for ourselves, and we weren’t disappointed. It’s interesting how only the columns along the edge are free standing, while those inboard are packed around with sediment. The little rain the area gets probably washed the sediment out of the spaces between the bordering columns. After walking around for a while we made our way back to the car and drove to the Drumheller Channels National Natural Landmark overlook for a final sweeping viewpoint. The entire area is huge and worth several days of exploring, but it’s also pretty easy to have a great time in just a few hours. This is a place you just have to experience. Quick Facts  Location: Adams County, Washington 99371

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Mammoth and Horse DNA Rewrite Ice Age Extinctions

New research reveals the ancient animals survived some 8,000 years later than previously thought Frozen soil samples collected around a decade ago are rewriting our understanding of iconic Ice Age animals like the woolly mammoth. The soil samples were pulled from Canada’s permafrost in the early 2010s, but no work on them had been published until recently. A new analysis of the DNA samples reveals that woolly mammoths, wild horses and steppe bison were around as recently as 5,000 years ago—some 8,000 years later than previously thought, according to a study published this week in Nature Communications. Scientists reconstructed the ancient ecosystem using radiocarbon dating of plant material trapped in the soil in combination with microscopic genomic sequences from animal species. Their results showed something unexpected: Large mammals like mammoths and horses were already on the decline before the climate warmed. The scientists found evidence of woolly mammoth and North American horse DNA as recently as 5,000 years ago, which means the animals held out until the mid-Holocene. Excerpted from the Smithsonian Magazine article by Corryn Wetzel

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Ice Age Floods’ Eye Candy

Check out Bruce Bjornstad’s Ice Age Floodscapes YouTube channel.  A growing library of surreal aerial video and pics of other-worldly megaflood features.These drone videos and images that can only be achieved and appreiciated from close range in the air give a unique perspective on large landscape features, such as: Gardena Cliffs Rhythmites, Streamlined Palouse Hills, Quincy Lakes Erratic, Moses Coulee, Castle Lake Cataract, Frenchman Coulee, Martin Falls Cataract, Reach Ice Age Floods’ Tours – 2017, Scabland Coulees, Williams Lake Cataract, The Great Blade, Lake Sacajawea Flood Bar, West Bar Giant Current Ripples, Devils Canyon Coulee, Missoula Flood Rhythmites, Ice-Rafted Erratics and Bergmounds, Wallula Gap, Dry Falls, Deep Lake Potholes, and Drumheller Channels

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Ice Age Floods’ Features

This is an amazing compilation of extra ordinary photographs that have been expertly labeled to assist the viewer’s understanding of the evidence supporting the creation of the Channelled Scablands in Eastern Washington State, USA.  The photographs are panned and zoomed in and out on providing an overview and close-ups of flood evidence.  Music playing in the background helps the viewer focus on the information displayed in an unhurried manner.  The viewer can stop the screen at any time to give them more time to study the information displayed in great clarity.  For teaching, this methodology is suburb!  Much better than a regular film or static photos. YouTube slideshow prepared by Bruce Bjornstad, published Dec 8, 2012

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Glacial Lake Missoula – Inspired Classroom Videos

The Glacial Lake Missoula chapter has worked with Inspired Classroom LLC to produce a series of 9 short (3-7 minute) videos exploring different aspects of the Ice Age Floods in the Glacial Lake Missoula area. The entire set is posted to the Inspired Classroom LLC YouTube channel, including a full 31 minute version (below) that compiles the entire set. 

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Williams Lake Cataract Video

Williams Lake Cataract is an ancient, dry waterfall left behind along the Cheney-Palouse Scabland Tract in eastern Washington after Ice Age flooding recessionally ripped out underlying basalt to produce this massive cataract. Video produced by Bruce Bjornstad, Ice Age Floodscapes

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Smithsonian Article about the Ice Age Floods

Ice Age Floods Smithsonian Article Devastating Ice Age Floods That Occurred in the Pacific Northwest Fascinate ScientistsThe Scablands were formed by tremendous and rapid change, and may have something to teach us about geological processes on Marsby Riley Black – Science Correspondent – April 19, 2022 for Smithsonian Magazine The Earth seems to change slowly. Continents shift by about half an inch in a year. Sea levels rise by less than a quarter of an inch in the same amount of time. Mountains are constantly being eroded but, to us, seem to stand today just as they did yesterday and the day before. Our planet’s geological history often seems like one of slow, grinding change. But that’s hardly the whole story. Sometimes geological change comes startlingly, violently fast, leaving scars on the Earth’s surface. The Channeled Scablands of the Pacific Northwest, a landscape full of flat-topped plateaus that rise between steep-walled canyons, are among the vastly-altered landscapes that have caused researchers to rethink what they previously presumed. The geologic wounds are dramatic evidence that quick and catastrophic changes have played a significant role in shaping our planet. The Scablands, principally located in southeastern Washington state, bear the signs of an incredible Ice Age event. Between 14,000 and 18,200 years ago, huge glacial lakes on the boundaries of ice sheets burst from their natural dams and rushed over the landscape, scouring the hills and dropping massive stones as they went. Entire hills were washed away as the floodwaters dumped gravel, boulders and sediment in new places, almost like shaking a great geological Etch-a-Sketch. But this is a relatively new understanding, only broadly accepted since the 1970s. It took decades for geologists to construct even an outline of what the Scablands represent, a realization that proved to be a turning point for science. For if intense floods could carve such features once in Earth’s history, surely they could have changed landscapes at other times and in other places—even those as far away as the Martian surface. Geologists only began to pick up on the story of the Scablands a century ago. In the 1920s, naturalist J Harlen Bretz wrote several descriptive papers on the strange basins and odd channels of the area. Those channels had been created by moving water, but the way water had once flowed through the area seemed to make no sense. “The channels run uphill and downhill, they unite and they divide, they head on the back-slopes and cut through the summit,” Bretz wrote, “they could not be more erratically and impossibly designed.” The only reasonable conclusion, Bretz proposed, was that the Scablands were created by massive and short-lived floods. Bretz’s colleagues were not ready for such a conclusion. Ever since geology came into its own as a science in the 19th century, much of the field has been influenced by the concept of uniformitarianism—that the present is the key to the past. In a broad sense, that’s an excellent rule. The Earth is still changing, and many of those alterations—from erosion to volcanic eruptions—also occurred in the past. But some additional stipulations to the older formulation of the idea were unnecessarily taken as truth. One of them was that the Earth is changing at a slow, gradual rate and that quick, catastrophic change was impossible. Bretz’s idea for how the Scablands formed flew in the face of what many geologists accepted. Channels were carved over long periods of time by rivers, other geologists thought, not by sudden floods. To Bretz, the evidence was unmistakable. Among other things, the Scablands contained layers of gravel hundreds of feet high. Slow-moving streams couldn’t have left such vast accumulations. Pieces of gravel are larger and heavier than particles of sand or silt, requiring faster-moving water to pick up the gravel and transport it. Gravel deposits as tall as skyscrapers must have required an incredible amount of fast-flowing water. The pattern was consistent with the underlying geology of the area, as well. The rock beneath the massive flood deposits was relatively friable volcanic rock, easily broken and carved. The fragility of these rock layers allowed the floods to gouge out channels and canyons in a way that harder rocks would have been more resistant to. Yet the fact that Bretz couldn’t identify the source of the floodwaters caused many to dismiss his idea, and it wasn’t until evidence of similar events—such as Ice Age flood beds found in Montana—that other experts began to reconsider what Bretz had proposed. Eventually, by the 1970s, dismissive geologists changed their tune. Something catastrophic truly did transpire to create the Scablands. Not that the behavior or history of such floods are completely understood. “There are loads of outstanding questions and many people are thinking carefully about the Scablands,” says University of Washington geology PhD candidate Kelsay Stanton. Even though experts are confident that vast glacial lakes provided the water for the floods, the precise volumes of the repeated floods are unknown, and the timing of the dozens of outbursts has yet to be determined in detail. “The glacial outburst flooding of the Pacific Northwest is hardly a closed subject,” Stanton says. Part of what’s allowing geologists to keep going back to the Scablands is that the tools available to scientists have changed a great deal since Bretz’s time. “There are lots of geochronology and computer modeling methods now that weren’t available when Bretz and other early researchers were mapping the area,” says University of Massachusetts Amherst geology PhD candidate Karin Lehnigk. These repeated floods affected the ocean, she notes, with the influx of freshwater reducing the saltiness of the northern Pacific for years and altering the way colder, saltier water in deep ocean layers circulated. The floods affected more than the land they ran over, and have acted as models for how our modern glaciers might alter ocean circulation as they melt due to global warming. New, broad scale methodologies can offer some of these insights and these refined techniques have proved to be critical, as no one has ever

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WA-DNR Website Features Phenomenal LIDAR Images

Washington State Geological Survey is collecting, analyzing, and publicly distributing detailed information about our state’s geology using the best available technology – LIDAR – an acronym for Light Detection And Ranging. The main focus of this new push for LIDAR collection is to map landslides, but there are innumerable additional benefits and applications of this data both inside and outside of the field of geology. A number of amazingly beautiful and revealing images are featured on the WA-DNR Flickr website, along with a trove of information about the technology and it’s applications. LIDAR is a surveying method that measures very precise distance to a target by illuminating that target with a pulsed laser light and measuring the reflected pulses with a sensor. Differences in laser return times and wavelengths can then be used to make digital representations of the target. LIDAR is expensive, but it can easily remove vegetation/grass/trees as it uses an emitting source and interferometry criteria to find the “last echo return” that is assumed as the ground, even in very dense scenarios (forests, corn fields, etc). LIDAR uses ultraviolet, visible, or near infrared light to image objects. It can target a wide range of materials, including non-metallic objects, rocks, rain, chemical compounds, aerosols, clouds and even single molecules. LIDAR is widely used for many different applications. Some (but by no means all) of those uses include: Geology and Hazards, Forestry, Graphics, Navigation, Meteorology and Fir,e Land-use planning, Archaeology and Agriculture. In geology, bare earth models allow closer study of geomorphology, which is the study of the origin of the topography of the earth. Floods, faults, landslides, erosion, and glaciers leave their mark on the landscape, and while these marks can be hidden by dense vegetation, they can’t hide from LIDAR. LIDAR can be used in the field of archaeology to find things hidden by the forest canopy. Large features that would be indistinguishable on the ground are readily apparent in a LIDAR survey, leading archaeologists to sites they might not have otherwise found. For example, intensity returns can be used to detect features just below the surface that affect plant growth.

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