2025-07-25 and 26 – QGS North Olympic Peninsula Field Trip

Eocene Bedrock Geology of the Northern Olympic Peninsula:  Arrival of the Siletzia Oceanic Terrane, Washington

 

WHEN:  July 25-26, 2025 (Friday and Saturday)

Quimper Geological Society (QGS) had an exciting two-day field trip on Friday, July 25, and Saturday, July 26, 2025, to the North Olympic Peninsula, led by led by Professor Erin Donaghy (University of Nevada, Las Vegas, sedimentologist and field geologist) with Carol Serdar Tepper (retired geologist, Washington Department of Ecology) and Jeff Tepper (Professor emeritus, University of Puget Sound) as co-leaders.

We looked at rocks related to docking of the Siletzia oceanic terrane, including volcanic and sedimentary units that formed while Siletzia was still offshore as well as, stratigraphic sequences that record both the pre-docking (Crescent and Aldwell Formations) and post-docking (Lyre, Hoko, and Makah Formations) history. At each stop we examined the rocks and discuss the field and lab techniques that were used to infer their paleo-environments and tectonic implications. The trip included some strenuous hiking/walking and several hours of driving each day, in places on paved but winding roads.

Logistical details for the trip are as follows:

  • The trip will begin both days at the Olympic National Park Visitor Center in Port Angeles, Washington, and will return there at the end of day one. More specifics will be provided once registration is finalized. Both days (Friday and Saturday) will begin at 8:30 AM (please DO NOT be late), end times may vary.
  • The group will be limited to 20 QGS members. (There will be additional geologists along to assist.) Spaces filled on a first-come, first reserved basis.
  • Participants should make their own arrangements for lodging in or near Port Angeles on Friday night (depending on your starting point on Friday (Day 1), you may also want to book both Thursday and Friday nights). Hotel availability can be tight during the summer, so booking early is recommended.
  • Participants should be in good physical health and comfortable walking several miles each day with some hikes being at ~6000 feet elevation.
  • Due to limited parking at some stops, carpooling is a must. We will coordinate this in advance as part of the registration process. Please offer your host driver money for gas and National Park fee (if applicable). If you are unable to carpool, please do not apply for registration.
  • Summer road construction along Highway 101 will increase your travel time, sometimes unexpectedly. Plan ahead.
  • The cost of the trip is $90, which includes box lunches both days and copy of the field guide.

TO BECOME REGISTERED:  1. Print the registration form; 2. Print all information completely; 3. Write a check (sorry, we are a small group) to:  JEFFERSON LAND TRUST; 4. Send registration form and check to the P.O. Box on the form.

About the leaders

Erin Donaghy, geology professor at the University of Nevada, Las Vegas is a sedimentologist who studies the evolution of sedimentary basins that form along active convergent margins. Her field work focuses on the west coast of North America, in particular the exotic terranes in western Alaska and the north Olympic Peninsula, Washington.

 

 

Carol Serdar Tepper, a licensed geologist, has spent her entire life on the Puget Sound playing with rocks. She began her career as a science teacher. She subsequently worked for Washington State mapping landslides and regulating surface mining, timber harvest impacts, and water-quality compliance. She is currently the leader and advisor for the Quimper Geologic Society.

 

 

Dr. Jeffrey TepperJeff Tepper, Professor emeritus at the University of Puget Sound, taught courses in mineralogy, petrology, and geochemistry before retiring in 2021. His research focuses on the magmatic and tectonic history of the Pacific Northwest and on environmental chemistry of water and sediment of local lakes.

2025-04-12 Dan Muhs – Tectonic Uplift in the Pacific Northwest

The Lecture
Subduction-related late Quaternary tectonic uplift and sea-level change in the Pacific NW and around the Pacific Rim

This was a Zoom-only lecture.

Quimper Geological Society welcomed Dan Muhs, an emeritus USGS geologist. He provided marine terraces as evidence of tectonic uplift along the Pacific Ocean plate.

In 1979, Seiya Uyeda and Hiroo Kanamori introduced a tectonic model with two end members of a subduction-boundary continuum: the “Chilean” type (shallow dip of the subducting plate, great thrust events, compression, and uplift of the overriding plate) and the “Mariana” type (steep dip of the subducting plate, no great thrust events, tension, and little or no uplift). The concept has been used to explain variable rates of Quaternary uplift around the Pacific Rim, and the paper has been cited over a thousand times since its publication in the Journal of Geophysical Research.  We now have a sufficient number of dated late Quaternary marine terraces from around the Pacific Rim to test the veracity of this model. In this presentation, well-dated emergent shorelines of the Pacific Rim was explored, from South America, North America, the Aleutians, Japan, and the Marianas.

About the Speaker

Dan Muhs is an emeritus scientist with the U.S. Geological Survey. He earned B.A. and M.S. degrees from the University of Illinois and a Ph.D. from the University of Colorado. He was a research geologist with the USGS from 1985 until his retirement in 2022.  Despite his retirement, Dan remains an active researcher, lecturer, and writer.

Dan’s interests are in the fields of coastal and eolian geomorphology, Quaternary stratigraphy, soil genesis, and paleoclimatology. Most of his work has been in the US (Alaska, western US, and Great Plains), but he has also worked in Canada, Mexico, Caribbean, Spain, and western Pacific. Over the course of his career he has authored more than 150 scientific papers on a diverse range of subjects focused on the Quaternary period, including the origins and history of loess and dune fields, paleozoogeography of marine fossil invertebrates, tests of glacial isostatic adjustment models, and sea-level histories and tectonic uplift rates deduced from emergent marine terraces. Dan has received numerous awards and recognition, including the Geological Society of America Kirk Bryan Award.

2025-05-03 Leigh Tucker and Marquis Richardson

Where are the Olympic Coast garnet sands coming from and how did they get there?

Washington State contains multiple beaches where garnet bearing sands are present, including the outer coast and within Puget Sound. The source of these garnets is unclear. To better understand where these garnets come from, we look inside them to investigate inclusion minerals. When garnets form in metamorphic environments, they can trap other minerals from their surroundings. These trapped minerals can give us pressure and temperature constraints to narrow down the source of the garnet. We can then compare results between garnet samples and their potential sources to their current locations. This information improves our understanding of how glaciers and rivers transported sediment during the last glaciation of the region. Our study also furthers a new technique of using garnet inclusions as tracers of where sediments originated.

About the Speakers

Leigh Tucker is a post-baccalaureate student at the University of Washington working towards a Bachelor of Science in Geology. Her undergraduate honors research extended the work started by Marquis Richardson, comparing sands from the Puget Sound and the Olympic Coast to determine if the garnets came from the same source. She recently interned with the USGS Earthquake Science Center on the development of an automated earthquake rupture mapping tool using machine learning and unmanned aerial vehicles. Leigh plans to pursue a graduate degree in volcanology after completing her BS in June 2025. When she isn’t studying, you can find Leigh baking, hiking, or reading to her granddaughter.

Marquis Richardson graduated from the University of Washington with a BS in Earth and Space Sciences: Geoscience. During his time there he investigated index mineral inclusions in garnet sands from Ruby and Rialto Beaches on the Olympic Coast (Washington). After graduation he hiked the Pacific Crest Trail and worked as a staff geologist for a geotechnical consulting firm before moving to restoration ecology work. He will be hiking the Continental Divide Trail over the summer of 2025 with plans to pursue graduate school after he returns.

POST Lecture emails:

5/3/2025 (PM) Carrie Carpenter from Whidbey Island wrote an email asking about sand on the beach close to where she lives:  “i live on whidbey…East Point in Saratoga Passage… garnet sands?”

Yes, these too are garnet sands…