Presentations
Location:
    Deschutes Brewery Tap Room (upstairs) at 1044 NW Bond Street , Bend, Oregon
               
General Agenda:

     5:30 PM Join us for food & beverages
     7:00 PM Presentation


2019

Tuesday, January 22
Anita Grunder, Oregon State University
The High Lava Plains of Oregon: Volcanic and Tectonic Connection between Yellowstone and the Cascades

The High Lava Plains is an enigmatic province between the hot-spot related Steens Basalts and the subduction-related Cascades. Dr. Grunder will explore the implications of the westward age progression of rhyolites and the effect of protracted magmatism on the composition of the volcanic rocks and the crust.

Links to two videos from Anita's presentation:

Cenozoic Volcanism in the Pacific Northwest - 55 million years to present

Magma evolution in an extentional setting—High Lava Plains



Tuesday, February 26
Josh Roering, University of Oregon
Mountains, Earthquakes, and Landslides: Using Lasers to Peer Behind Cascadia's Green Veil

Tuesday, March 26
Allan Lerner, University of Oregon
Summary of the 2018 Eruption of Kilauea Volcano, Hawaii

Tuesday, April 23

Jeff Templeton, Western Oregon University
Newberry Volcano: Evaluating the Influence of Cascadia Subduction and the High Lava Plains on Magmatism at a Geologic Crossroads in Central Oregon

Tuesday, May 28
Hal Wershow, Central Oregon Community College
Holocene Glacial and Paleoclimate Reconstructions in the North Cascades, Washington

Tuesday, September 24
William Lingley, 
Energy Resources of Coastal Washington

Tuesday, October 22
Jim O'Connor, U.S. Geological Survey
The Other Flood: Ice-age Bonneville Flood on the Snake River

Tuesday, November 26
Title: TBA

Past Presentations

Fall 2018 Series


   
Tuesday September 25

Assembling the Northwest: a roadside view of Oregon and Washington geology

Marli Miller, University of Oregon


With its spectacular mountain ranges, lush valleys and tumbling rivers, the Northwest landscape attracts nature lovers and travelers from around the world. But the rain-soaked coast range, snow-covered volcanoes and expansive high desert didn't appear overnight. They formed through a variety of geologic processes over millions of years. UO geologist and photographer Marli Miller will outline the geology of Oregon and Washington as seen along our federal and state highways. Beginning with the plate tectonic setting of the Pacific Northwest, she will describe the process of continental growth that forms the underlying but diverse "basement" of the region and is readily visible in the Coast Range, North Cascades, Okanogan, Klamath, and Blue Mountains. Following that, a photographic "roadtrip" up I-84 and Washington State Highway 14 in the Columbia Gorge will illustrate many of the younger features that make our landscape so unique.

Tuesday October 23

The Crooked River Caldera

Jason McClaughry, Oregon Department of Geology and Mineral Industries - Baker City Field Office

The Crooked River caldera is a 26-mile long, 17-mile wide volcanic depression formed through a series of super-volcanic eruptions between 29.7 and 27.5 million years ago. Eruptions from the Crooked River caldera deposited massive volumes (>140 cubic miles) of tuff and rhyolitic lavas, dikes, and domes. All of these volcanic features are now well exposed in the rock walls of Smith Rock State Park. Current research suggests that the Crooked River caldera records some of the oldest caldera-forming eruptions related to the passage of the Yellowstone volcanic hotspot from the coast of the Pacific Northwest to the modern Yellowstone caldera in Wyoming during the past 50 million years. Jason’s talk will focus on regional tectonic models and geochemistry linking the Crooked River caldera to the Yellowstone volcanic hotspot.




Tuesday November 27

Groundwater hydrology and groundwater-dependent ecosystems of central Oregon

Marshall Gannett, Research Hydrologist Emeritus

                                     U.S Geological Survey 

Groundwater is critical for humans and ecosystems in central Oregon. The volcanic geology of the Deschutes and upper Klamath Basins is widely known to host substantial regional aquifer systems that store and transmit large volumes of groundwater that supports year-round flow to many streams. What is less well known is that there are smaller-scale local aquifer systems that exist in the region as well, and that there are unique groundwater-depend ecosystems associated with these different scales of groundwater flow. Marshall Gannett will describe the groundwater hydrology of central Oregon, focusing on the upper Deschutes Basin, and discuss recent research aimed at understanding groundwater-dependent ecosystems and the sensitivity to climate change.

Spring 2018 Series


Tuesday March 27

Geothermal Exploration at Newberry Volcano
Bart Wills, U.S. Forest Service 

Join the Central Oregon Geoscience Society and U.S. Forest Service geologist Bart Wills for a presentation on
the 40-­‐year geothermal history at Newberry Volcano. The presentation will introduce the geology of Newberry
and discuss the formation of Newberry National Volcanic Monument, the most recent geothermal projects
at Newberry, and some of the difficulties these projects have encountered in producing geothermal power.


Tuesday April 24

Mount Hood: Confessions of an interesting Boring volcano

Adam Kent, Oregon State University

Mount Hood is an active subduction zone volcano, and is the site of the most recent volcanic eruption in Oregon. The volcano is also deeply embedded in the social and recreational fabric of the state of Oregon, but despite the iconic profile details of the inner workings of Mount Hood have been quite poorly known. Adam Kent will present new research that sheds light on past and future volcanic activity at Mount Hood, with a focus on the clues that can be extracted from studying the erupted rocks themselves.


Tuesday May 22
 

Oblique subduction, rotating crustal blocks, and the active tectonics of the Pacific Northwest
Ray Wells, Research Geologist Emeritus, U.S. Geological Survey  


Oregon has been slowly rotating clockwise over geologic time. Coast Range basalt of the Siletz River Volcanics, about 50 million years in age, are rotated about 75°, whereas younger flows of the Columbia River Basalt (16-12 million years in age) exposed in the Coast Range are rotated about 20°. Rotations are largest along the coast and decrease inland. Northeast-directed subduction of the Juan de Fuca Plate beneath the continent drags the leading edge of Oregon northward, producing a clockwise shear in the continental plate. Ray Wells will present current understanding of active tectonics in the Pacific Northwest and the role that crustal rotation plays in the Cascade volcanoes and in shallow crustal faults in the Northwest urban corridor.                  

Visiting Scholar Program

The COGS Visiting Scholar Program is an open invitation to scientists who are visiting central Oregon and would like to present their research to the community. Although we try to schedule these programs in advance, many of these opportunities come up on short notice based on the travel schedules of visiting scholars. All Visiting Scholar presentations will be posted as early as possible on the COGS website, and will be announced via email. Stay informed on our Visiting Scholar Program by becoming a member of COGS, or by signing up for our email list.