Back from fieldwork so time to tweet about the boulder hunting. This is the central portion of the Ruby Range, SW Yukon. Follow thread for more info. #SFUglacialgeology#YukonGeologicalSurvey
We are dating deglaciation, both the Cordilleran Ice Sheet (CIS) and local alpine glaciers. These small cirques would have supported glaciers during the last glaciation (MIS 2). #SFUglacialgeology#YukonGeologicalSurvey
We use the accumulation of Terrestrial Cosmogenic Nuclides from glacially transported boulders to date deglaciation. Good boulder selection is crucial. These large boulders are from the CIS, most of these are saw worthy! #SFUglacialgeology#YukonGeologicalSurvey
Derek Cronmiller (MSc student) using a cut out saw to take a uniform sample in the upper 2.5-3 cm of a boulder. Some people just use chisels, but that is way more work! And does not always provide a uniform sample. #SFUglacialgeology#YukonGeologicalSurvey
We then use a chisel to get sample with uniform thickness. TCN dating is based on the accumulation of rare isotopes (10Be in this case) formed by bombardment by high energy cosmogenic particles. #SFUglacialgeology#YukonGeologicalSurvey
By measuring the amount of 10Be and knowing the production rate, when the boulders melted out of the glacier can be calculated. We sampled three boulders on this moraine in Albert creek that may predate the last glaciation and be MIS 4. #SFUglacialgeology#YukonGeologicalSurvey
This is the Late Wisconsinan (MIS 2) moraine in Albert Creek. Four boulders were sampled just inside this limit. We can compare this age to that of the CIS to understand forcing mechanisms. Derek's initial findings are local ice deglaciation later than the CIS #SFUglacialgeology
Experimenting with a Makita angle iron with a diamond blade on it. Worked well and is much lighter for hiking! But having enough batteries are an issue. #SFUglacialgeology#YukonGeologicalSurvey
The glacial history of Ruby Range is complex. These Tors (periglacial features) indicate a long period of weathering. These surfaces have likely not been glaciated, unless it was cold based ice. #SFUglacialgeology#YukonGeologicalSurvey
One of the finding of Derek’s thesis is that there are much larger areas of the uplands that have never been glaciated compared to previous studies. #SFUglacialgeology#YukonGeologicalSurvey
The boulder hunting team, from left to right, Jeff Bond (YGS), Dion Parker (TRK Helicopters), Derek Cronmiller (SFU). Was a fantastic day both weather wise and geologic! We took a record 10 samples! #SFUglacialgeology#YukonGeologicalSurvey
Got dropped off first thing and Dion had to go set out some other people. As it leaves you always wonder if it will come back. But he did! #SFUglacialgeology#YukonGeologicalSurvey
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On August 29 examined some active layer detachment slides Near Arch and Quill creeks, SW Yukon. Around 25-30 slides occured on August 17, the same time the Alaska Highway was blocked by debris flows. A thread of these. This is the slides near where we landed. 1/10
Landed on the deposition zone of one of the landslides and flew the drone. Helicopter indicated for scale. 2/10
This is part of Crey Ackerson’s MSc thesis supported by Kristy Kennedy from the Yukon Geological Survey. 3/10
Finally some pictures of the Koidern Landslide. Start with some aerial pictures and then some more details. Some really interesting mollards, and some have remobilized! It is a long thread as it was a really cool landslide! 1/10
Looks like several phases. Initial failure crossed the small valley and then turned the corner. Then remobilization with a more fluid flow down the valley, blocking the larger stream. Then a smaller failure from the headscarp, where we first landed the helicopter. 2/10
Margin of the slide with lots of mollards. Nice streaking of the bedrock. 3/10
Spent a beautiful Friday at Point Grey (aka Wreck Beach) looking at the stratigraphy. He we have two advance sub-units below the till. The lower is interstratified sand and silt with peats, with ages from 26-24 ka, the upper, cross stratified sand. 1/
These advance sediments are called Quadra Sands and some diatoms in the lower sub-unit sediments indicate marine incursion. The upper sands show tidal influence. With eustatic sea level at this time, indicates >100 m of isostatic depression! 2/
The accumulation of ~70 m of Quadra sands indicates significant accommodation space. The two sub-units are exposed all along the escarpment. 3/
Friday’s Seymour valley fieldtrip examined the stratigraphy of the thick valley fill. The base is 42-29 ka MIS 3 gravel, sand and peat, indicating warmest climate at the base and progressively cooler to the top. 1/9
The MIS 2 Fraser Glaciation, has two advance stades. These are advance glaciolacustrine sediments of the older Coquitlam Stade, a mix of laminated to finely bedded silt and sand and diamicton. 2/9
Indicates ice blocked the mouth of the Seymour valley, forming this lake. There is wood in these advance sediments, dating to around 21 ka. Implies there is a spruce-fir forest in the area as ice advanced. 3/9