(2 Dec 2024) Grace Sherwood Winer is a geologist and explorer who has done extensive studies on the melting of glacial ice in the Arctic. She will present present her work on the islands of Svalbard and Iceland at our meeting on 06Jan2025 at 7:00pm at Bellevue College, Building B, Room 104. Note room change! This will be an In-person lecture and livecast via Zoom. Click on Zoom link: https://us02web.Zoom.us/j/82985244730 Bellevue College, Bldg B, Rm 104
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International Old Rock Day - January 7 Celebrate Old Rock Day on January 7 every year. It's a day to remember the Earth’s incredible history and to pay tribute to the amazing geologists who help us understand it. We’ve been dependent on rocks since we first walked the Earth, and today it’s no different, with rocks forming the foundation of our daily lives. History of "Old Rock Day"The study of rocks was first introduced by the Ancient Greek Theophrastus in his work, “Peri Lithon” (“On Stones”), and became the cornerstone of geology for other interested scientists. The study was advanced by Pliny the Elder, who recorded numerous minerals and metals in great detail, with a particular focus on their practical use. Although working without the tools we use today, Pliny was able to correctly identify the origin of amber as fossilized tree resin.It wasn’t until 1603 when the word ‘geology’ was used for the first time by Italian naturalist Ulisse Aldrovandi. It took a further 150 years for the first geological maps to be drawn by British geologist William Smith, whose work began the process of ordering rock layers by examining the fossils contained in them.Then, in 1785, James Hutton wrote and presented a paper to the Royal Society of Edinburgh called ‘Theory of the Earth’, which outlined his belief that the world was far older than previously thought. His breakthroughs make him widely considered the first modern geologist.In 1809 William Maclure produced the first geological map of the USA, a task he completed thanks to two painstaking years spent personally traversing the country. With the invention of radiometric dating in the early 20th century, scientists could finally provide an accurate figure for the age of the earth by tracing the radioactive impurities found in rocks. It helped scientists to see that the Earth is one very old rock indeed!Rocks have been essential for human development, which is why we celebrate Old Rock Day and the wonder of the geological world. Why We Love "Old Rock Day" Geology is coolStudying the natural world helps us protect, preserve, and predict it so that we can live in harmony with natureRocks are usefulFrom the sturdy bricks of our homes to the sidewalk beneath our feet, rocks are essential for human existenceRocks are preciousSome of the most coveted things in the world today — gold, diamonds, and other gemstones — are old rocks (minerals)Reprinted from National Today - Old Rock Day |
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J Harlan Bretz "It was a debacle," wrote J Harlan Bretz in 1923, that carved Washington's Channeled Scabland. This prescient finale today brings to mind debacles geologic, personal and periodic. The cataclysm in Bretz's "Spokane flood" initiated a famous controversy. Published arguments against great Scabland flood erupted in the 1920's and raged on into the 1940's--critics by various more conventional schemes calling for less water over more time. As Bretz had almost no published support, it seemed to many his personal debacle. Yet re-reading the early reports, and recently the summary field notes, I sense that by the extraordinary field evidence he had documented throughout the region, Bretz knew all along that his 'catastrophysm' would prevail. After J.T. Pardee showed in 1942 that huge glacial Lake Missoula had discharged abruptly. Bretz and colleagues in 1956 show with the old evidence--and with stark new evidence in giant current dunes adorning many gravel bars--that water from glacial Lake Missoula had indeed carved the 'Channelled Scabland'. With detailed geomorphic field evidence they skewer Bretz's critics--this in turn becoming their personal debacle. waittThe story takes a more gradualistic turn with discovery that Lake Missoula drained periodically. In his final Scablands paper in 1969, Bretz, by geomorphic evidence counts seven floods at most. But hardly a decade later, new stratigraphic evidence was showing that Lake Missoula released scores of giant floods during the last glaciation alone. These outbursts were both periodic and gigantic by degrees, truly colossal and coming decades apart when the damming Purcell Trench lobe was thick, but as the ice gradually thinned diminishing to coming only a decade or a few years apart, and at the end one year apart. This 'jokulhlaups' idea erupted new controversy, this one also lasting more than two decades. If it has simmered down lately, this argument is also being settled by field evidence. If Missoula floods were numerous and periodic during last-glacial marine-Isotope stage 2 (25-15 thousand years ago), what happened during seemingly equally deep glaciations of AR-isotope stages such as 6 and 12 (140-440 thousand years ago)? So far we know of no supporting field evidence--only scattered field sites that suggest one gigantic flood far back, perhaps a million years ago. It will be for today's young scientists to decipher this and other remaining enigmas. Thursday, January 16, 2025, In Person 6:45PM PST Tualatin Heritage Center, 8700 SW Sweek Drive, Tualatin, OR 97062 ALSO Simultaneous Live ZOOM from THC if you cannot attend the in-person THC meeting yourself. Click here for Zoom meeting, Meeting ID: 869 4651 3479 Passcode: 322382. |
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It’s that time of the year! Time to contemplate ice ages and glacial lakes. Time for the Glacial Lake Missoula Chapter of the Ice Age Floods Institute’s Cabin Fever Lecture! Warm up your curiosity about those iconic strandlines we can see from town with a lecture from renowned geologist James W. Sears. New “LiDAR ” mapping techniques may imply that the famous Lake Missoula strandlines on Mount Sentinel and Mount Jumbo record only one draining of the ice-age lake. The draining coincided with massive erosion at the bottom of the lake, but passive lowering of lake level at the top, marked by short-term strandlines cut a few inches into thin colluvial soil on the mountainsides. About the Instructor: Dr. James W. Sears received his PhD from Queen’s University, Canada, in 1979, and has taught at the University of Montana since 1982. This is a live event that will not be recorded or streamed. |
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