Monthly Presentations

The Central Oregon Geoscience Society holds regularly scheduled monthly presentations on the 4th Tuesday of each month, from September to November, and from January to May. All presentations are free and open to the public.


Please join us at:

Worthy Brewing (eastside location)

495 NE Bellevue Drive, Bend

In the Hop Mahal Room


5:30 pm social hour

7:00 pm presentation


COGS talk are free and open to the public -- all are welcome! Please join us for the social hour before the presentation.

Presentations are also live-streamed through Zoom. Please see the presentation details for Zoom registration links. Zoom presentations are recorded whenever possible, see the list of past presentations to watch recordings of past talks.



Visiting Scholar Presentations

Visiting Scholar presentations are scheduled during various times outside the regular monthly meeting schedule. Please check the schedule below for updates, or join the COGS email list for updates. To join the email list, go to the Join us page.



Upcoming Presentations

    • 24 Nov 2026
    • 5:30 PM
    • Online and in-person at Worthy Brewing


    Greater Siletzia and the Making of the Columbia Embayment, Northwest USA

    Ray Wells

    Research Geologist Emeritus, U.S. Geological Survey, Portland, OR

    Ray Wells has 50 years of field experience documenting the geologic structure and earthquake hazards of the Cascadia convergent margin in Oregon and Washington.


    We will look at the history of the Columbia Embayment (CE); the area of anomalous low topography that lies inboard of the Cascadia subduction zone and is enclosed by the oroclinal bend in the Mesozoic arc. We think that the accreted coastal basalt terrane of Siletzia extends eastward beneath the Columbia Basin, and that the timing of its emplacement overlaps with northward transport of far-travelled British Columbia terranes (“Baja BC”) and Laramide deformation of the US Cordillera. We propose a model that links the origin of the Kula Plate to the Laramide orogeny, its subsequent role in rifting of BC terranes out of the CE, about 400 km south of its present location, and contemporaneous emplacement of Siletzia. The model may help reduce the misfit between large paleomagnetic and smaller geologic estimates of BC terrane displacements.



    Please join us at:

    Worthy Brewing (eastside location)

    495 NE Bellevue Drive, Bend

    In the Hop Mahal Room


    5:30 pm social hour

    7:00 pm presentation


    COGS talk are free and open to the public -- all are welcome! Please join us for the social hour before the presentation.

    All presentations are also live-streamed through Zoom. There will be a registration link at the top of this page as we get closer to the date of this presentation.


    • 26 Jan 2027
    • 5:30 PM
    • Online and in-person at Worthy Brewing


    To Go Boldly Where Few Have Gone Before: Exploring the Seafloor of Planet Earth

    Michael J. Cheadle

    A Brit; BS & PhD from the UK, MS from the USA- Taught 10 years at University of Liverpool, UK and 24 years at the University of Wyoming.

    More than 70% of the Earth's seafloor remains unexplored and unmeasured by direct, bathymetric surveys; in fact we know more about the topography of the far side of the Moon and Mars than we do about~ 50% of the Earth’s surface. Consequently, seafloor exploration has led to spectacular geologic discoveries in recent times, with likely more exciting finds still to come. During this talk we’ll re-visit some of those discoveries: the largest offset (normal) faults in the world; hydrothermal vents and their exotic chemosynthetic lifeforms (analogs of the origin of life?); the competition between tectonics and magmatism at  mid-ocean ridges  and the nature of ocean crust itself-especially the poorly explored lower oceanic crust that lies below the ubiquitous basalt carapace in the Pacific.  The talk will also cover the basic principles that govern how mid-ocean ridges work, including the exhumation of vast tracts of the Earth’s mantle.

    Please join us at:

    Worthy Brewing (eastside location)

    495 NE Bellevue Drive, Bend

    In the Hop Mahal Room


    5:30 pm social hour

    7:00 pm presentation


    COGS talk are free and open to the public -- all are welcome! Please join us for the social hour before the presentation.

    All presentations are also live-streamed through Zoom. There will be a registration link at the top of this page as we get closer to the date of this presentation.


    • 23 Feb 2027
    • 5:30 PM
    • Online and in-person at Worthy Brewing


    Jen McLeod

    Assistant Professor, Oregon State University, Eugene OR

    Please join us at:

    Worthy Brewing (eastside location)

    495 NE Bellevue Drive, Bend

    In the Hop Mahal Room


    5:30 pm social hour

    7:00 pm presentation


    COGS talk are free and open to the public -- all are welcome! Please join us for the social hour before the presentation.

    All presentations are also live-streamed through Zoom. There will be a registration link at the top of this page as we get closer to the date of this presentation.


    • 23 Mar 2027
    • 5:30 PM
    • Online and in-person at Worthy Brewing


    Drama Llamas and Mantle Mystery

    John Boyd

    Instilled with wanderlust and thirst for adventure from a young age, John was born and raised in one of the flattest places on the planet with the highest relief in the county being only about 10 m difference from its lowest point. From as early as the age of 6, he dreamed of expeditions to the Andes and some 20 odd years later, while working on his Masters of Geology at the University of Wyoming, that dream finally became a reality. Graduating in 2010, he moved to Alaska to work in the petroleum fields where he worked for a handful of years before moving on to other endeavors such as using geophysical surveys to investigate long-lived plutonic systems, teaching continuing education courses of the geology underfoot in the Bitterroot valley and surrounding areas of Montana, and most recently LiDAR processing for a mapping company that primarily produces high-definition 3D maps for the autonomous and semi-autonomous vehicle industry.  In his free time, he continues to tell stories and look at interesting rocks and geologic features, while planning adventures with his wife and teenage daughter in the playground that is the Pacific Northwest.

    Mysteries teach us that if one wants to understand what has happened, one needs to find a record of it. Just as in those mysteries, the record one finds is often a series of clues one must use to reconstruct the event rather than a complete record of it. In geology, if one wishes to understand what occurred during a particular orogen, one needs to go to the associated basins where those records or clues are stored. The sedimentary basins of the Altiplano-Puna Plateau in South America contain the record of retro-arc foreland basin evolution during the Cenozoic. The deformation of these basins is characterized by high angle reverse faults and thrusts deforming crystalline basement and sedimentary covers. While the mechanisms responsible for deformation within the region are not fully understood in detail, the relative abundance of intercalated tuffs within these basins and those within the bounding Eastern Cordillera enables the timing and pattern of deformation across the orogen to be constrained. As one of the largest intermontane basins within the Altiplano-Puna plateau, the Arizaro Basin is well suited to investigations of basin deformation in response to lithospheric processes. Here we present some of the data gathered to test a few of the models that have been used to explain the patterns of deformation, such as the taper of the orogenic wedge and lithospheric foundering or drips, as well as some of the adventures encountered in the pursuit of these clues. Finally, a brief overview of some of the recent work that has been published since the initial thesis that provides a bit of vindication and a current understanding of the processes responsible for the clues left behind.


    Please join us at:

    Worthy Brewing (eastside location)

    495 NE Bellevue Drive, Bend

    In the Hop Mahal Room


    5:30 pm social hour

    7:00 pm presentation


    COGS talk are free and open to the public -- all are welcome! Please join us for the social hour before the presentation.

    All presentations are also live-streamed through Zoom. There will be a registration link at the top of this page as we get closer to the date of this presentation.


    • 27 Apr 2027
    • 5:30 PM
    • Online and in-person at Worthy Brewing



    Please join us at:

    Worthy Brewing (eastside location)

    495 NE Bellevue Drive, Bend

    In the Hop Mahal Room


    5:30 pm social hour

    7:00 pm presentation


    COGS talk are free and open to the public -- all are welcome! Please join us for the social hour before the presentation.

    All presentations are also live-streamed through Zoom. There will be a registration link at the top of this page as we get closer to the date of this presentation.


    • 25 May 2027
    • 5:30 PM
    • Online and in-person at Worthy Brewing



    Please join us at:

    Worthy Brewing (eastside location)

    495 NE Bellevue Drive, Bend

    In the Hop Mahal Room


    5:30 pm social hour

    7:00 pm presentation


    COGS talk are free and open to the public -- all are welcome! Please join us for the social hour before the presentation.

    All presentations are also live-streamed through Zoom. There will be a registration link at the top of this page as we get closer to the date of this presentation.


Past Presentations

27 Oct 2026 Corridor of Cataclysm -- mapping the perilous geologic journey of the Owyhee River
22 Sep 2026 Does Volcanic Ash Fertilize The Globe?
13 Jun 2026 COGS Picnic Social - 2026
26 May 2026 Axial Seamount: The Hidden Active Volcano in the Pacific Northwest
28 Apr 2026 Let's talk about Mount Jefferson
24 Mar 2026 City of Bend Water Sources, Water Management, and Water Futures
24 Feb 2026 Illuminating a Deforming Landscape: Mapping and Analyzing Fault Scarps with Lidar Across Oregon
27 Jan 2026 The wax and wane of volcanism over 3.5 m.y. in the Goat Rocks Wilderness area, Washington Cascade Range
25 Nov 2025 Whales and Earthquakes, A Uniquely Oregon Story
28 Oct 2025 Ocean drilling: Realizing the foundation of ocean lithosphere and the mantle
23 Sep 2025 A common fate to all silicic eruptions?
20 Jun 2025 COGS Picnic Social - 2025
27 May 2025 Geologic carbon storage possibilities in the Pacific Northwest
22 Apr 2025 Cascadia Earthquakes and Other Disasters: Are We Ready?
25 Mar 2025 Interdisciplinary volcanology: Combining geochronology and geophysics at the Three Sisters volcanic complex
25 Feb 2025 How forests grow their own pot: Quantifying the role of trees as wind-wiggling, tap-dancing, and crowbar-wielding architects and builders
28 Jan 2025 Eruptive History of Three Fingered Jack, a Mafic Composite Cone in the Central High Cascades of Oregon
26 Nov 2024 The Changing Skyline: Photo Documentation of 100 Years of Landscape Change in the Central Oregon Cascade Range
22 Oct 2024 Cascade Volcanoes: Past, Present, and Preparing for the Future
24 Sep 2024 Was the 1700 Cascadia earthquake one or many ruptures?
10 Jul 2024 On Basaltic Andesites: The Dominant Lava Type of the Central Oregon High Cascades
9 Jun 2024 COGS Picnic Social
28 May 2024 From the Last Glacial Maximum to Present: New Chronologies for Oregon’s Cascade Ice Cap and Glaciers
23 Apr 2024 Extensional Evolution of the Horse Range, Eastern Nevada
26 Mar 2024 Sediment-Hosted Lithium Deposits at McDermitt Caldera: Oregon’s Critical Mineral Capital
27 Feb 2024 How, Why and Where Earth Melts
23 Jan 2024 Onset and impacts of the c.7700 ybp eruption of Mount Mazama, Oregon
28 Nov 2023 Hydrology of High-Desert Springs in Eastern Oregon
24 Oct 2023 Sunstones: The Good, The Bad, & The Ugly (in other words, the complex petrogenesis of our state gemstone)
26 Sep 2023 Live Tour of the JOIDES Resolution
23 May 2023 Looking down to look ahead: How Oregon’s fossil rodents can help us understand the impacts of past and future climate change
25 Apr 2023 In the Shadow of Volcanoes
28 Mar 2023 The Most Recent Earthquake on the Mount Hood Fault Zone, Oregon: Implications for cascading earthquake, landslide, & flood multi-hazards in the Columbia River Gorge
28 Feb 2023 Ancient Soils of Earth and Mars
24 Jan 2023 The ancient magnetic field: Clues hidden in lava flows from around the world
22 Nov 2022 The development of the science of geology and the growth of the railroad industry: How geology played a significant role in railroads of the Pacific Northwest
25 Oct 2022 The Rock Bottom of Antarctica’s Food Chain
27 Sep 2022 Paleoseismic investigations of Quaternary active faults in the forearc and backarc of the central Pacific Northwest
22 Sep 2022 Evidence of humans in North America during the Last Glacial Maximum
28 Jun 2022 Volcanoes! Travelogue and Science of Two Volcanic Arcs
24 May 2022 Encountering the Unexpected in Pacific Northwest Geology
26 Apr 2022 When Magmas Meet High-Tech Metals: What Can the Mountain Pass Rare Earth Element Deposit Bring to the Future?
22 Mar 2022 Newberry Volcano Geothermal Projects, Past and Future
22 Feb 2022 From maar craters to cinder cones: Understanding Oregon's small, but most common, volcanoes
25 Jan 2022 Wildfire and Debris Flows
23 Nov 2021 Tectonic evolution of the Cascadia margin in southwest Oregon during the past 55 million years
26 Oct 2021 Evaluation of slip history and Holocene activity on faults in the Strawberry Mountains
28 Sep 2021 Timing and controls on growth of the Oregon Basin and Range Province
25 May 2021 I Date Rocks: A Geochronology Love Story
27 Apr 2021 Water in the Deschutes Basin: 2020 Hindsight – What Happened?
23 Mar 2021 The fragmented death of the Farallon Plate
23 Feb 2021 Our Vanishing Glaciers, Part II
26 Jan 2021 The Next Great Cascadia Earthquake - How did we get here?
24 Nov 2020 What lies under recently active Cascades volcanoes?
27 Oct 2020 Mapping the Magmatic Pathways Beneath Volcanoes from Newberry, Oregon to Santorini, Greece
22 Sep 2020 Red Rocks from Earth to Mars
25 Jun 2020 Extinction: Using catastrophic events to construct the geologic timeline
26 May 2020 The history and science of glacier change in the western US and a peek into their future
28 Apr 2020 Volcanoes in Our Backyard: Understanding and Mitigating Volcano Hazards in Central Oregon
24 Mar 2020 I Date Rocks: A Geochronology Love Story
25 Feb 2020 Mountains, Earthquakes, and Landslides: Using Lasers to Peer Behind Cascadia's Green Veil
28 Jan 2020 Three Newly Discovered Fault Systems in Oregon
26 Nov 2019 Oregon's Checkered Past
22 Oct 2019 The Other Flood: Ice-age Bonneville Flood on the Snake River
24 Sep 2019 Tectonic History of the Coos Bay Basin and its Relationship to Pacific Northwest ‘Siletzia’ Tectonics
10 Aug 2019 Newberry Volcano: A sleeping giant with two bubbling lakes
28 May 2019 Holocene Glacial and Paleoclimate Reconstructions in the North Cascades, Washington
23 Apr 2019 A new look at “old” tuffs from Newberry Volcano: Evidence for dynamic magmatic processes at a geologic crossroads in central Oregon
26 Mar 2019 Kīlauea's 2018 Fissure Eruption – Chronology, Processes, and Impacts of Kilauea's Largest Eruption in 200 Years
26 Feb 2019 Mountains, Earthquakes, and Landslides: Using Lasers to Peer Behind Cascadia's Green Veil
22 Jan 2019 The High Lava Plains of Oregon: Volcanic and Tectonic Connection between Yellowstone and the Cascades
27 Nov 2018 Groundwater hydrology and groundwater-dependent ecosystems of central Oregon
23 Oct 2018 The Crooked River Caldera
25 Sep 2018 Assembling the Northwest: A roadside view of Oregon and Washington geology
16 Jul 2018 Oregon's volcanoes: What have we learned from global advances in volcanology over the past decade?
22 May 2018 Oblique subduction, rotating crustal blocks, and the active tectonics of the Pacific Northwest
24 Apr 2018 Mount Hood: Confessions of an interesting Boring volcano
27 Mar 2018 Geothermal Exploration at Newberry Volcano

Central Oregon Geoscience Society

Email: COGeoSoc@gmail.com
P.O. Box 2154,  Bend, Oregon 97709

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