Extending from northern California to southwestern British Columbia, is the Cascade Arc. Within the Canadian segment of the arc, there are seven volcanic centers, with the most recent eruption in B.C. being approximately 2,400 years ago. Despite having lava compositions that are unusual relative to the rest of the arc, there has not been much scientific research done in this area, mostly because of the remoteness of the volcanoes and their difficult access.
(see photos of the sampling expeditions: https://www.flickr.com/photos/cdbeard/sets/72157635274504449; https://www.flickr.com/photos/cdbeard/sets/72157636134686613)
Dominique recently began work in this field, using both archived and newly collected samples, and now has good coverage of these volcanoes. Results show geochemical differences with the southern part of the Cascades that can be related to the age of the subducting slab, decreasing by approximately 4 million years, which potentially led to reduced slab inputs or the change in the angle of the subduction (Mullen and Weis, 2013, 2015).
These results have been generating interest in the scientific community to the south of the border and Dominique has begun working on some of the US volcanoes of the High Cascades as well. The new isotopic results, especially for Pb, show very interesting relationships when compared with sediment data from the Cascadia (Carpentier et al., 2013, 2014) and Astoria basins and the local oceanic crust.
This information helps identification of different mantle domains and processes at the scale of 100 km.