Sept. 20-22, 2019: Mt. Rainier Field Trip
Professor Emeritus Pat Pringle of Centralia College and colleagues led a 3-day trip to the Mount Rainer area to see the geology of this fantastic mountain and its geologic and environmental effects on the surrounding region. Participants provided their own transportation and lodging (in Ashford and Packwood); we provided field trip log, a published guidebooks, experts on specific aspects of the geology and geomorphology, and a chance to see one of Washington’s three active volcanoes.
The trip started at 11 am Friday at Mud Mountain Dam Park south of Enumclaw. We made a CCW circumnavigation of Mt. Rainer and ended up on the northeast side on Sunday afternoon, east of Enumclaw. Rain and socked in that day, but good wx for the first two days. Many of the stops were roadside, but we took several 1-2 mile hikes with 300-500 feet of elevation change. A good time was had by all, and a true value at $50 each.

For more info, you can download the preliminary field trip route and schedule by clicking here. In addition, Pat published a guide to this area that will serve as a more comprehensive resource. Pdfs of the various chapters of the Roadside Geology of Mount Rainier National Park and vicinity, Information Circular 107 (IC-107) as well as pdfs of other publications can be downloaded via links in the Washington Geological Survey’s online catalog.

Field Trip June 22, 2019: Geology of Hurricane Ridge and the Olympic Mountains; Jim Aldrich—Leader
This trip was road-based with a bit of walking on the road, but nothing strenuous. We meet at the National Park Visitors Center (3002 Mt Angeles Rd, Port Angeles) at 9 am, when it opened. We’ll formed carpools to minimize the number of cars (5) at roadside stops. From there, we’ll traveled up to Hurricane Ridge, visited a number of roadcuts to see the Crescent basalt. Lunch was had on the deck of the Hurricane Ridge Visitors Center. From there, we drovee to see geologic features along Hurricane Ridge and overview the evolving landscape of this region.
We saw how tectonic forces of uplift driven by the subduction zone are balanced by the erosive forces of precipitation (Mt. Olympus gets 260″ annually).
group on a second walking tour of Seattle Building Stone. We saw all types of rock used in Seattle’s historic buildings and will learn about the geology and history of the stone and its use. This is a very popular walking tour and has been recently updated from his previous walks. More information about this tour can be found on
The date of the field trip was Saturday, May 11. The trip filled and we had wonderful weather, here are a few pictures and some words about our