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Audhild Bay is not the only place on northern Ellesmere Island with enigmatic volcanics.   Phillips Inlet and Yelverton Bay both contain huge exposures of relatively undescribed and unstudied rock.   On an exceptionally clear day, John, Pete, and Matt P., ran a fly camp to these areas to collect samples.
 
 

With their choked sediment loads and constantly shifting channels, braided rivers, like this one, are often indicative of tectonically active or glaciated regions.
The north shore of Phillips Inlet, and its precipitous cliffs of sedimentary and volcanic strata.   Without any real sense of scale in the Arctic, it is difficult to gauge the size of and distance to objects captured in photographs.   We felt very small when we flew into Phillips Inlet.
Another view of outcrops at Phillips Inlet.   There was plenty of intriguing rock on the ground in the form of talus, but no readily accessible outcrops from which to collect meaningful samples.
The mountains just north of Phillips Inlet, marking the western edge of the Ellesmerian icesheet.
Yelverton Bay, from the southwest.   A deep and impressive fiord.
We found an accessible outcrop at Hansen Point.   Here John and Pete extract a set of cores they drilled.
A suncompass, the device we use to orient each core.   If you look closely, you can see six other cores we drilled from this dike.
This is the view we enjoyed from above Hansen Point: The air was clear and cool, the sky very blue, and glaciers stretched out into Arctic Ocean in front of us.   Several hundred kilometers across the ocean was Siberia's north shore.