Lloyd Stoess will present a free lecture with information showing how the Columbia, Palouse, and Yakima Rivers all had course changes during the last glacial period of the Ice Age. All three were changed by different forces. One was temporary and the other two were permanent. This lecture is in partnership with the Mid-Columbia Libraries Connell branch.
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Join us for a weekend of lectures and sight seeing in Ritzville, Washington! There is a small block of rooms set aside at an event rate through the Best Western Bronco Inn (509) 659-5000, ask for the Ice Age Floods Tour rate when you reserve your rooms. $170* field trip fee– Registering as a non-Ice Age Floods Institute Member $150* field trip fee– Registering as a Ice Age Floods Institute Member. If joining now or renewing as an IAFI member, also include your IAFI Membership Application with your field trip registration, fees and liability release form. Please write one check to IAFIPF for registration and a separate check to IAFI for membership fee. $145* field trip fee – Registering as a Palouse Falls Chapter Ice Age Floods Institute Member (thank you for your support!) *FIELD TRIP FEE covers: 1) outstanding and knowledgeable field trip leaders, 2) a very detailed and well-illustrated Field Trip Guidebook, 3) delicious lunch, snacks, and drinks, 4) comfortable deluxe chartered bus with microphone system for lectures while in route, and 5) delicious Mexican banquet! -Friday evening: Dinner is on-your-own-adventure. Check-in located in the lobby of the Bronco Inn between 7 and 8 p.m., as well as after the FREE pre-trip lecture at 8:00p by Lloyd Stoess on the topic "Following the Course of the Columbia River" in the Bronco Inn meeting room. -Saturday: Check-in located in the lobby of the Bronco Inn between 7:15 and 7:45 a.m. FIELD TRIP LEADERS: Lloyd Stoess, Palouse Falls Chapter President and Dr. Eugene Kiver, Professor Emeritus Eastern Washington University. DESCRIPTION OF FIELD TRIP: This bus tour will revolve around Saddle Mountain with stops including Lind Coulee, Drumheller Channels, Corfu Landslide Complex, Corfu ghost town, Smyrna Bench, Vantage interbed exposure, Beverly Bar, Sentinel Gap, McCoy Canyon Landslide, Priest Rapids Bar, Saddle Mountain summit, Othello Channels, multiple exposures of the Ringold Formation, Collier Coulee, and the Staircase Rapids. ITEMS TO BRING WITH YOU: Binoculars, camera, sunglasses, and clothing for variable weather conditions. Snacks, drinks, and lunch provided. -Saturday evening: FREE post-trip lecture at by Gene Kiver on the topic "Bonneville Flood and the Snake River" in the Bronco Inn meeting room. Cancellation refunds will be made only if field trip registrar, Jacqui Hair, receives notice no later than September 22 and vacancies can be filled from a stand-by list. Registration and liability form are both available for download at this link. |
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This event is open to the public, but only IAFI Cheney-Spokane members can vote during the member meeting. It will be held at the beautiful new Doris Morrison Learning Center at 1330 S. Henry Road. Exit the freeway south on Barker Road, turn left at the roundabout at Sprague Road, then right at the three-way junction on Henry Road. Member meeting: 2:00-3:00 PM Dr. Kiver's lecture will begin around 3 PM, after the member meeting. It is open to the public (see title and blurb below). Note: At present, we have three openings on our chapter board. Our board meets the third Tuesday of each month from 3-5 PM at the Wren-Pierson Building in Cheney. Interested? Members with expertise in accounting or K-12 education or medical experience or any other expertise that would aid our chapter's mission should send a very brief vita to Dr. Linda McCollum, President, IAFI Cheney-Spokane Chapter, lmccollum@ewu.edu Dr. Eugene Kiver Lecture: GLACIERS AND MISSOULA FLOODS IN NORTHEASTERN WASHINGTON Immense quantities of Glacial Lake Missoula floodwater roared through not only the Rathdrum/Spokane floodway but also through the rugged mountain topography of the Northern Rockies in northeastern Washington. Here floods ripped across non-basaltic glaciated rocks and through the Little Spokane River drainage into the Channeled Scabland south of the present course of the Spokane River. This alternate route is often overlooked. The Pend Oreille River course north of Newport has been reversed and now flows north into Canada. Glacial suppression of the crust is the suspected culprit. Over a mile of ice buried the Pend Oreille River valley near Canada during the late Wisconsin ice advance allowing water to flow north and cut deep canyons along the river course. |