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  • October 2025

  • Sat 18
    Williams Lake Cataract

    🗺️ Cheney-Spokane Chapter Fall Field Trip

    October 18, 2025 @ 9:00 am - 3:00 pm PDT

    Saturday, October 18, 9:00 AM – approx. 3:00 PM No cost • Car caravan format • BYO food & drinks After a summer of record heat, haze, and delay, cooler weather has finally arrived—and so has our rescheduled fall field trip! Join us on Saturday, October 18, just one week after our annual membership meeting, for a full-day exploration of the northern Cheney-Palouse scabland tract. This year’s trip will spotlight the landscape that first led J Harlen Bretz to propose a massive outwash flood beneath an ice cap—before he reluctantly considered Thomas Pardee’s theory of glacial Lake Missoula as the water source. We’ll trace their steps and interpretations across key sites, guided by: Dr. Linda B. McCollum, Professor Emeritus at EWU and current chapter president Glenn Cruickshank, who has meticulously mapped Bretz’s and Pardee’s field notes using Google Earth 🧭 Trip Overview We’ll meet at 9:00 AM at the Cheney-Spokane Chapter parking lot (1st Street & Cheney Plaza Road, south end of Cheney) for a quick briefing. From there, we’ll caravan to: Turnbull Wildlife Refuge HQ – hike and discussion of scabland channels Williams Lake Cataract – second only to Dry Falls in scale Amber Lake – loess island and classic scabland topography Lunch break in Cheney – bring your own food and drinks Fish Lake (Cheney-Spokane Road) – scour pools and rock blade formations Marshall – glacial outwash delta and broad flood channel features We expect to wrap up around 3:00 PM. All stops have ample parking, so there’s no limit on vehicles—everyone’s welcome! 📝 What to Bring Your own food and drinks A signed liability form (click on the red button below to download and print one that you can bring to the event) Curiosity, good shoes, and maybe a camera! This is a great chance to revisit foundational flood geology with fresh eyes and expert insight. We hope to see you there!  

  • November 2025

  • Sat 1

    Field Trip East of Coulee City, WA – Updated

    November 1, 2025 @ 10:00 am - 5:00 pm PDT

    Karl Lillquist will lead "East of Coulee City" field trip on the day after Halloween. We will meet at the Coulee City Campground at 10am.  Stops will include: 1) Coulee monocline; 2) Hartline Basin expansion bar; 3) top of Hartline Hill; 4) mid-slope Hartline Hill; and 5) Hartline Basin scablands. Quick description:  Topics will center around Ice Age flooding associated with Glacial Lake Missoula in the area east of Coulee City.  Trip will begin on the peninsula on the north end of Coulee City Community Park.    Detailed schedule and the topics to be covered:  10:00  Stop 1—Coulee City Community Park—Topics: Bedrock & structural geology; weather & climate; General patterns of Glacial Lake Missoula floods and the Okanogan Lobe of the Cordilleran Icesheet; Banks Lake.    10:45  Depart 11:00  Stop 2—Coulee Monocline —Topics:  Monoclines & homoclines; Age of Coulee Monocline and its relationship to Ice Age floods & Hartline Basin; Historical orchards, highways & railroads. 11:45  Depart 12:00  Stop 3—Hartline Basin Expansion Bar—Topics: Bretz in the Hartline Basin; Expansion bars; Soils atop expansion bar. 12:45  Depart 1:00     Stop 4—Top of “Hartline Hill”—Topics: Maximum flood limit; Loess-based soil characteristics, origins & age; Water erosion & loess; 1:45     Depart 2:00     Stop 5—Mid-slope on “Hartline Hill”—Topics: Unnamed canyon & fan; Possible floodwaters over “Hartline Hill”. 2:45     Depart 3:00     Stop 6—Hartline Basin Scablands—Topics: Scablands & Bretz;  Floods, erosion & scablands; Giant pendant bars;  Other possible floodwater sources in Hartline Basin 4:00     Depart for home Logistics: This trip is free and open to the public.  There is no need to register. After Stop 1, we will drive on a mix of paved and good quality gravel roads.  Passenger cars should be fine on these roads. I encourage you to consider carpooling.  This will reduce the time it takes to get us all together at each stop plus will reduce our carbon footprint.    We will take short walks at Stops 2, 3 and 6.  By short, I mean 0.25 mi or less at each stop.  There will be a bit of somewhat steep, uneven terrain at each of the stops.  We will also need to cross a barbed wire fence at Stops 2 and 6. No restroom or picnic facilities are available along our field trip route after Stop 1.  Therefore, you will need to use the great outdoors if you need to go.  Plan on eating lunch/snacks on the road or at the stops.  There will not be a formal lunch stop. Dogs and kids are fine to bring as long as they are well-behaved. Dress for the weather.  November weather here can be sunny and mild to rainy, windy & chilly.  Our first two stops will be especially exposed to a possible north wind.  A field guide is posted on my CWU website at https://www.cwu.edu/academics/geography/_documents/karl-lillquist.php.  Scroll down the page to “Field Guides”.  You will find it under “East of Coulee City”.  Feel free to download and bring it on the field trip in digital format or print it out. The Ellensburg Chapter of the Ice Age Floods Institute will also provide ~40 hard copies of the field guide for the trip.  There is no cost for the field guides.  However, if you are not a member of the Ellensburg Chapter, please consider making a donation to the chapter to help cover the costs of the field guides (each cost ~$15/each).  Field Trip Liability Form Please print and fill out the attached field trip liability release form, and give it to one of the Ellensburg Chapter IAFI officers at the field trip.  We will also have hardcopies of the liability release form if you need them.  Thank you! Questions? Email me at lillquis@cwu.edu or leave a phone message at 509 963-1184.  Emails are best as I only check that phone a couple of times each week.  A heads up: I may be away from phone  & email between 29 October to 1 November.    I hope to see you Saturday 1 November! Karl L.

    Free
  • Tue 4

    EVOLUTION OF THE COLUMBIA RIVER SYSTEM

    November 4, 2025 @ 6:30 pm - 8:00 pm PST
    The Reach Museum 1943 Columbia Park Trl , WA, Richland, WA, United States

    We have always assumed that the Columbia River and its tributaries have been the same for many millions of years. The Earth is constantly fooling us like that.  In reality most river systems are dynamic, and the Columbia River is no exception. We will explore how it has changed over the past 16 million years.  We’ll see how in earlier times locations such as like Yakima, Prosser and Benton City would have been on the Columbia River, while the Tri-Cities would have been left high and dry. The Columbia River system is one of the great river systems of North America, draining much of the Pacific Northwest, as well as parts of the western United States and British Columbia. The river system has had a long and complex history, slowly evolving over the past 17MY The Columbia River and its tributaries have been shaped by flood basalt volcanism, Cascade volcanism, regional tectonism, and finally outburst floods from Glacial Lake Missoula. The most complex part of river development has been in the northern part, the Columbia Basin, where the Columbia River and its tributaries were controlled by a subsiding Columbia Basin with subtle anticlinal ridges and synclinal valleys superimposed on a flood basalt landscape. After negotiating this landscape, the course to the Pacific Ocean led through the Cascade Range via the Columbia Trans-Arc Lowland, an ancient crustal weakness zone that separates Washington and Oregon. The peak of flood basalt volcanism obliterated the river paths, but as flood basalt volcanism waned, the rivers were able to establish courses within the growing fold belt. As the folds grew larger, the major pathways of the rivers moved toward the center of the Columbia Basin where subsidence was greatest. The finishing touches to the river system, however, were added during the Pleistocene by the Missoula floods, which caused local repositioning of river channels.

  • Sat 15

    Barker Canyon Giant Cave Arch Rockshelter Field Trip – Sat. Nov. 15th

    November 15, 2025 @ 9:30 am - 3:00 pm PST
    Dry Falls Visitor Center 35661 HWY 17 North, Coulee City, WA, United States

    Join Outing Coordinators Mark Amara, Geologist and Gene Wing of the Lower Grand Coulee Chapter on Saturday November 15th for a 3-mile hike to visit the Barker Canyon Giant Cave Arch Rock Shelter Ice Age Floods Feature in the Upper Grand Coulee   Date: Saturday November 15th, 2025 Start time: 9:30 am Meeting Place: We will meet at the Dry Falls Visitors Center parking lot at 35661 Hwy 17 North, Coulee City, 99115 and plan to leave at 9:30 AM sharp and drive to Barker Canyon DRIVING DIRECTIONS:        Please see the attached map or coordinates of the Rock Shelter are: 119.193029 degrees Latitude - 47.89900 degrees Longitude  Fees: A Discover Pass is required What to bring: Lunch, drinks, snacks, appropriate clothing and footwear, camera, etc.

  • Mon 17

    Puget Lobe Lecture: Jeff Tepper on the Initiation of the Cascade Arc

    November 17, 2025 @ 7:00 pm - 8:30 pm PST
    Bellevue College Building T Room 127 3000 Landerholm Cir SE, Bellevue, WA, United States

                    Dr. Jeff Tepper The Cascade volcanic chain, the world’s youngest continental arc, was “born” shortly after accretion of the  Siletzia oceanic terrane ~50 My ago.   That collision, which led to formation of the Olympics, terminated the  earlier subduction system and caused a portion of the subducting Farallon slab to break off.  When Cascade  magmatism began less than 5 My later, there was a new trench located outboard of Siletzia.  In this talk I will  present a new model, based on petrology, geochronology, plate motion reconstructions, and mantle tomography,  that explains how subduction was initiated so quickly and in a setting where the slab was young and hot and in  theory too buoyant to subduct.   

  • December 2025

  • Tue 9

    Foster Creek and Foster Coulee: Insights on Ice Age Floods, Glaciers, and Lakes on the Waterville Plateau, WA

    December 9, 2025 @ 7:00 pm - 8:30 pm PST
    Wenatchee Valley Museum and Cultural Center 127 S. Mission, Wenatchee, WA, United States

    The Wenatchee Valley Erratics Chapter of the Ice Age Floods Institute will meet Tuesday, December 9 at 7:00 PM, at the Wenatchee Valley Museum and Cultural Center, 127 S. Mission, Wenatchee. Or via Zoom link: https://us02web.zoom.us/j/81855547958  Meeting ID: 818 5554 7958 Karl Lillquist will give our final live, and Zoom, presentation for 2025. Karl is a physical geographer, who taught at Central Washington University until his retirement in summer of 2024. He will talk about “Foster Creek and Foster Coulee: Insights on Ice Age Floods, Glaciers, and Lakes on the Waterville Plateau, WA.” Please note! The Wenatchee Valley Erratics now has its own website: https://wverratics.org/ !

    Free
  • Wed 10

    Mystery of the Channeled Scablands and the Two Detectives who Solved it.

    December 10, 2025 @ 1:00 pm - 2:00 pm PST
    Pomeroy Senior Center 695 Main St., Pomeroy, WA, United States

        The unique landscape of the Channeled Scablands was a mystery that baffled the first geologists who visited them over 100 years ago. Finding clues, they unraveled the mystery that was unbelievable to their colleagues. After more than two decades of discovering more clues, the theory that enormous floods had carved the scabland was finally accepted by most of the scientific community.  Lloyd Stoess, President of the Palouse Falls Chapter, will take you on a journey following these two early detectives and the clues they found as well as what today's detectives and the modern tools they are using to better understand our incredible landscape.

    Free
  • January 2026

  • Mon 5

    Puget Lobe Lecture: The Bonneville flood- the other flood!

    January 5 @ 7:00 pm - 8:30 pm PST
    Bellevue College Building T Room 127 3000 Landerholm Cir SE, Bellevue, WA, United States

    The Bonneville Flood was one of the largest floods on Earth. First discovered by G.K. Gilbert in the 1870s during his inspection of the outlet at Red Rock Pass, Idaho, it was rediscovered in the 1950s by Harold Malde and coworkers, leading to mapping and assessment of spectacular flood features along Marsh Creek, Portneuf River, and Snake River for over 1100 kilometers between the outlet and Lewiston, Idaho. The cataclysmic flood - from the rapid 115-meter drop of pluvial Lake Bonneville from the Bonneville level to the Provo level - was nearly 200 meters deep in places and flowed at a maximum rate of about 1 million cubic meters per second — about 100 times greater than any historical Snake River flood. Along its route the Bonneville Flood carved canyons and cataract complexes and built massive boulder bars. These flood features have been a rich source for understanding megaflood processes. Yet it still offers much more with new and developing techniques for hydrodynamic modeling and landscape analysis.

  • Tue 6

    An Introduction to the Missoula Floods

    January 6 @ 6:30 pm - 8:00 pm PST
    Zoom Meeting

    Dr. Gary Ford, president of the Ice Age Floods Institute, will provide an introductory presentation of the Missoula Floods and reveal ho repeated, cataclysmic floods during the last Ice Age carved a dramatic landscape through much of the Pacific Northwest. Event: IAFI Lake Lewis January Member Meeting and Guest Lecture “An Introduction to the Missoula Floods” By Gary Ford Date: January 6, 2026 Time: Members Meeting: 6:30PM-7:00PM, Lecture: 7:00PM - 8:00PM (PST)   Join Zoom Meeting https://us06web.zoom.us/j/87852702318?pwd=Ye0a71u5MbQUtry9qp6u2qSw79dqIa.1 Meeting ID: 878 5270 2318 Passcode: 634508

  • March 2026

  • Sat 14

    Free STEAM Workshops for K–12 Educators – The Dalles, OR

    March 14 @ 9:00 am - 4:00 pm PDT
    Columbia Gorge Discovery Center 5000 Discovery Dr., The Dalles, OR, United States

    Every student in the Northwest should experience the incredible science story of the megafloods that shaped our landscape and history. To help bring this story to life, the Ice Age Floods Institute, Engaging Every Student, and our partners are excited to invite K–12 educators to free special training events. Thanks to support from the Avista Foundation, we are offering free hybrid workshops where you will gain access to valuable resources designed to inspire students to investigate their local environment. New Curriculum Resources Participants will explore a new Ice Age Floods Detectives phenomena-based curriculum with supporting presentations targeted to 4th grade, as well as hands-on investigations from the National Park Service's Investigating Ice Age Floods curriculum. Both explore the megafloods that shaped the Northwest and are adaptable for grades K–12 Free STEAM Workshops for K–12 Educators Details (In-person with options to join us via Zoom): Location: The Dalles, OR: Sat., Mar. 14, 2026 (register here: tinyurl.com/yxw9haet) Featuring: Engaging classroom and field-based activities, including exciting ways to model Floods phenomena Stories of the megafloods that transformed the Northwest 18,000–12,000 years ago at the end of the Last Glacial Period Up to 7 Washington STEM Clock Hours and/or PDUs for license renewal in Oregon and other states Schedule: All workshops 9:00 am–4:00 pm (or half day) 9:00–12:00 | Interactive workshop featuring new Ice Age Floods Discovery curriculum: targeted to grade 4 and adaptable for K–12 12–12:30 | Working lunch (provided) 12:30–3:30 | Interactive workshop featuring Investigating Ice Age Floods curriculum adaptable for grades K–12 3:00 or 3:30–4:00 | Nearby interpretive field studies with experts Cost: Free Ice Age Floods Institute mini-Grants available  To cover materials, transportation, STEM clock hour fee, etc. Learn more: iafi.org/k-12grants. Help Spread the Word: We encourage you to share this informative Ice Age Floods Workshops flyer with other educators to let them know about this opportunity!  For questions, comments, or ideas on where we might offer additional training, please contact Rick Reynolds, M.S.Ed., at rick@engagingeverystudent.com. Thanks for your interest and all you do to inspire our students to investigate our environment!  

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