From Alaska to Antarctica and Several Places In Between!

It’s been quite some time since I’ve blogged about my on-goings.  Since climbing Denali in May of 2016 with Kristin, Blaine, and Patrick, I’ve taught a field geology-geophysics course for UMaine in New Hampshire and Vermont which included several lake surveys with radar by canoe; moved to Seattle for 1-2 years to work with an amazing group of scientists at the University of Washington Department of Earth and Space Sciences; had many fishing, climbing, and other outdoor weekend adventures in Olympic National Park, Mt Rainier National Park, and the Cascades; been to two weddings (one of which I performed the ceremony of for my best friend, Jacob, and his amazing wife Jesse!); returned to the Eastern Alaska Range in September for a short two day field season of GPS measurements; been to Antarctica conducting research on two different projects I’m involved in; and climbed in New Hampshire for a few days of relaxation after my winter field work.  Now I’m back in Seattle preparing for my next field season in Eastern Alaska with the UMaine and Dartmouth crew.

I missed Thanksgiving, Christmas, and New Years away from my wonderful family.  We have very sadly lost some friends and family in the world recently.  But, I also have some wonderful memories from the past nine months.  Instead of a long blog today, I thought a bunch of photos/videos that reflect where I’ve traveled, outdoor adventures I’ve pursued, the friends I’ve spent time with, and some science I’ve completed, would be more fun for people to look at.  Enjoy!

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Relaxing with Kinley in the hammock after a spring and early summer full of field work!

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Getting ready to conduct a radar survey of lake bottom stratigraphy with my long time mentor, Steve Arcone, and a student from UMaine. Perfect day to be on the water!

 

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Steve doing what he is the master of (GPR)! Tom and I getting ready to paddle.

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A radar profile collected across a lake in New Hampshire showing water depth, layered sediments, and bedrock or till under the sediments. The sediments re probably made up of fine grained sands and silts deposited since the last glaciers retreated in this area over 12000 years ago.

 

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Jeep loaded down with clothes, bicycle, books, and outdoor gear, ready for the move from New Hampshire to Seattle!

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Some of my best friends that we were able to visit during our cross country road trip! Jacob (left), Kristin, and Jesse (right).

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Kristin and I were also able to visit her best friend, Abbey, for an evening during the road trip!

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Kinley (right) has a long lost brother, Abbey’s puppy (on the left)!

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Kristin’s prior office mate from Dartmouth, Lee, just happened to be in Bozeman, Montana when we were driving across country! Found a beautiful hike to spend an afternoon with her. This was also a great excuse to get Kinley out to stretch her legs!

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Arrived in Seattle, ready to roll. BUT, work doesn’t mean I can’t get out and play in the mountains on the weekend! Here, my good friend Brad tops out on a climb we completed in the Cascades. Brad and I have been on five field research seasons together so far and have another planned this spring!

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Friends from Maine! Scott Higgins, Tom and Dave Cassidy paid me a visit in Seattle to climb some in the Cascades. Too bad the weather was not great but we still had fun.

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Well… when its raining we find something else to do…. Like go check out Leavenworth during Octoberfest!

 

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Climbing at Washington Pass with some Juneau Icefield Research Program friends: Scott and Isabel!

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Washington Pass is a pretty amazing area!

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Classic granite on an amazing fall day in the Cascades!

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Ok…. so I have actually done LOTS of work this year as well… in fact, about 6 months of time away from home on field work. This is a map of McMurdo Ice Shelf in Antarctica. Last year we collected about 1300 km of radar in the grid on this map to look and the internal structure of the shelf. The next several photos are figures from the radar data we collected that I have finally processed.

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This radar profile was collected from the sea ice onto McMurdo Ice Shelf. You can see lots of cool internal features but too much to explain fully here. feel free to email me though if you have questions about the profile!

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Another cool radar profile with TON’s of cool glacier-ocean-ice flow features occurring here.

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And another….. this profile crossed the convergence of two glaciers basically! Pretty cool to see where the ice mass from one glacier ends and the ice mass of another glacier begins!

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Fractures in the bottom of the ice shelf show up as these hyperbolas.

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Another profile taken across the transition from sea ice onto the ice shelf. Only this profile shows a bunch of folds in the ice from land that the ice is obliquely running into.

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a to a’ on this photo (courtesy of Ben Roth) shows about where the last radar profile was collected. You can also see the folds on the surface as the ice shelf moves towards the open ocean but also pins up against hut Point Peninsula (which causes the ice to fold).

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Ht Point Peninsula is an interesting location. This is where vehicles from McMurdo and Scott Base access McMurdo Ice Shelf where the runways are located for transporting people to and from the ice. The folding at this location is worrisome to the folks in charge of McMurdo operations so we are studying the neighboring hillside to see 1) how much ice is there and 2) how fast that ice is moving down hill. We are doing this to determine if we may be able to put a road on the hillside that accesses the ice shelf further up-glacier and bypasses the major folding of the ice shelf in this area. This figure shows ice depths on the hill side and ice flow velocities measured using very high precision GPS survey instruments.

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I am also modeling the ice flow on the hillside. This is a block model of the hill based on ice thicknesses determined by radar and surface topography determined from a high resolution digital elevation model. The basics: my numerical model matches observations pretty well. BUT lots more to add to the model!

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Collecting GPS information for ice flow velocities (shown a couple photos back) on the Hut Point hillside.

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Colleagues helping me collect radar ice thickness measurements on the Hut Point Hillside. Thanks John, Trevor, and Perry! (notice we are roped up to keep us safe from any potential crevasses buried under the snowpack). Also notice Mount Erebus and Castle Rock in the background, two iconic features of Ross Island.

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I finished my first Antarctic project on time… so, with some evenings of down time, I was able to take a rec trip to see some of the other local sights. Here is an iceberg frozen into the sea ice.

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Scotts Hut at Cape Evans which was used by part of Sir Robert Falcon Scott’s team between 1911 and 1913. Pretty amazing history here and well worth researching yourselves. Recommended reads include: Scotts Journals which chronicle his attempt to reach the pole, right up to his death at the very end; and “Endurance: Skackletons Incredible Voyage” which chronicles Shackletons attempt to reach the pole but getting stuck in pack ice instead!

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Just some cool wooden crates by Scotts Hut!

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Zoom of a little guy wandering around on the sea ice while we were on our way back from Cape Evans! Amazing little guy!

 A video of Mr. Penguin paralleling the road.  We didn’t want to disturb him with the vehicle so we stopped, and let him walk on by as he was travelling to who knows where!

A video taken from Observation Hill which is situated in between Scott Base and McMurdo Station.  In the video you can see Mount Erebus, Castle Rock, McMurdo Station, the sea ice, the ice shelf-sea ice transition, the Royal Society Range across the sea ice which is located in the dry valleys, White and Black Island, and the McMurdo Ice Shelf.  Amazing day up there with colleagues, Ryan, Zoe, and Fegy!

A video panning around while surveying the Hut Point Hillside looking towards the significant folds of ice at the ice shelf sea ice transition.

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On to the next project! Ohio Range, or what we called the “No-Fly-O” Range because it is a notoriously difficult place to reach. About 300 miles from South Pole in a region where weather converges from the East Antarctic Plateau and storms coming from the coast across West Antarctica. BUT, our pilots and NSF support folks did an amazing job this year and we got out to our study site quickly! The arrows are velocities measured using GPS stakes installed last year and remeasured this year.

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A really cool radar profile showing bedrock below ice, as well as ice rich till and contacts between firn and blue ice…. yep… lots going on so I will avoid describing all the details… just take if from me that this profile is really cool!

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During this project I officially started working with repeat images taken at different angles to build high resolution digital elevation models. The technique is known as Structure from Motion (look it up online!). This is one outcrop that I created a high resolution digital elevation model of.

papa_north  If you click on this PDF to the left titled papa_north and enable all functionality on it, you should be able to rotate the photo within the PDF to different orientations and actually see the Digital Elevation Model  I created using Structure from Motion techniques on about 100 photos I took of the outcrop from different angles.

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Melt only 300 miles from South Pole! Wow!!!!

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The team at the Ohio Range: Jen, Sujoy, Grant, myself, and Zach.

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Grant and I in front of the very first rock core collected under glacier ice. Sujoy and Zac will use this rock core with some specific chemical methods to determine the last time it was exposed to sun (i.e. no ice cover). We collected 5 rock samples like this from under the ice. Results from this project will help constrain estimates of glacier change over time.

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Grant holding a really nice (53 cm long) rock core that he was able to successfully drill for our team!

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Drilling Setup to collect the first rock core under ice!

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Testing my Ice Radar system with Jen to measure ice thicknesses in the Ohio Range. (Photo: Jen Erxleben)

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Christmas in the Ohio Range! Jen was amazing! She sketched each of these stockings and had surprises for each of us! And…. pay no attention to the tee-shirt I am wearing! (Photo: Jen Erxleben)

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Pancakes for breakfast! (Photo: Jen Erxleben)

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Sujoy holding a really cool piece of core. We drilled into the rock across a relatively steep face (40 degrees or so). This core has ice on the top right side and rock on the bottom left.

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Amazing place to do radar. Beautiful golden granite surrounding us! (Photo: Jen Erxleben)

Pretty common to be windy in the Ohio Range!

Jen Erxleben took this hilarious timelapse video of me trying to walk gracefully, without crampons or ice creepers, on the heavily scalloped blue ice….

img_0206Amazing panorama of the Ohio Range with me tinkering on the radar system. 2000′ high and several miles wide, the Ohio Range is a significant mass of golden granite! What an amazing place and a wonderful Antarctic Field Season! (Photo: Jen Erxleben)

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Back to New Hampshire after a successful Antarctic Field Season. A couple days off for ice climbing was a great idea! Repentence in North Conway, NH

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Well… the crux was a little too thin and delaminated for me to be psyched about climbing it, but the first pitch was a blast as always!

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Dr. Bromley enjoying the ice!

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Dr. Bromley and I discussing proposal ideas over a “day off” ice climbing!

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Fafnir on Cannon Cliff… what an amazing place!

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Fun to catch up with past University of Maine student and friend, Brian O’Leary, for a day of climbing at Cannon Cliff!

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Mr. Ben Winn, Engineer extraordinaire, Computer Science wizard, and “off the couch” mutant climber…. Always fun to get out with him!

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Well…. Bring on the next winter adventure!

A Denali Recap!

Sorry for the delay in an end of season summary but it was quite a whirl wind once we summited Denali, returned to Talkeetna, and traveled back to our respective home states.  The main take home points from the season include:

  • Blaine and Kristin were able to install a USGS survey marker at Windy Corner (13,500 fasl) for long term monitoring of tectonic movements in the Alaska Range. Just as importantly, Blaine was able to record GPS information over the marker with our GPS base station for over 5 days which will be a great first year dataset for comparison to measurements in the following years.

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    Blaine with the newly established USGS survey Marker at Windy Corner.

  • Patrick was able to collect snow samples at Kahiltna Basecamp (7,600 fsal), Kahiltna Pass (10,200 fasl), Camp 14 (14,200 fasl), and High Camp (17,300 fasl) for comparison to the snow chemistry at the ice core drill site our collaborative team drilled at Mount Hunter (13,000 fasl) in 2013. This information will help us understand atmospheric chemistry as a function of elevation in the Alaska Range which is important for interpreting our ice core record we recently acquired.
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Patrick digging a snow pit to collect snow samples from for comparison to the Mount Hunter ice core collected in 2013.

  • We were able to collect ground-penetrating radar ice thickness measurements from the summit of Denali! This was the final challenging science endeavor of the season and included carrying the radar and GPS equipment to the summit as a team.  Kudos especially to our young and very strong Patrick who carried both a car battery and the GPR control unit while the GPS gear, cables and radar antenna was split between Kristin and I.
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    Kristin and I collecting GPR data at the summit of Denali

    Did I say car battery? Well… that’s not entirely correct.  It was ONLY an 18-amp hour 14-pound battery that Patrick carried, along with the 10 pound GPR control unit. (I say ONLY, jokingly).  Normally 60 extra pounds of gear spread between three people would not be a big deal, but the reality is, carrying that extra weight of science gear to the summit of the highest point in North America, along with the technical climbing and safety gear we needed to carry, is no small feat for a mere mortal research team.  We were happy to try it, but the extra effort beyond what climbing teams were expending to reach the summit, was certainly enough of a workout for all of us.  BUT, I digress and am jumping ahead of myself here.  Let me tell the entire story from Camp 14 to the summit and back…

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    Friends at basecamp!  (L to R) Dom Winski, Jimmy Voorhis (guiding on the mountain but prior MS student at Dartmouth), Patrick, myself, and Kristin

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    About 1/2 way to Camp 1 (which is at 7800 fasl).  Only 12500 feet in elevation gain to go for the summit of Denali (background)!

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    Patrick cooking up a hearty dinner in our camp 11 snow cave!

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Lounging in the Camp 11 snow cave while I wait for snow to melt for water!

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Looking up Squirrel Hill from the top of Motorcycle Hill on one of our acclimatization and cache days to Camp 14.

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Kristin moving up Squirrel Hill with Peters Dome (back right) and Peters Glacier (below right).

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Me at the top of Motorcycle Hill (12000 fasl) towing the radar gear and solar power panel with a duffel full of food under the panel.  We left the panel at Windy Corner with the GPS base station, thankfully!

On the same day that Blaine and Kristin installed the USGS survey marker at Windy Corner, Patrick and I shuttled a huge amount of science gear, food, and supplies to 14,200 fasl from the 11,000 fasl camp.  Kristin and Blaine joined us at Camp 14 with some extra supplies after they finished the survey marker installation.  We returned to Camp 11 for the evening, and on the following day, moved the rest of our gear, camp, and ourselves to Camp 14.

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The duffel of food and a couple containers of fuel!

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The team at a possible cache site above windy corner and below Camp 14.  We cached our gear at Camp 14 to cut a day out of our travel efforts so we could relax and rest a little more!

Once our entire team arrived at Camp 14, we settled in and started shuttling gear to higher cache sites the following day; first from Camp 14 to 16,400 fasl and a second beautiful day hike from Camp 14 to high camp at 17,300 fasl.  These two shuttle days helped us stage all our gear for a summit attempt and to acclimatize properly at higher elevations.  We then had some relaxing rest days at Camp 14 because of poor weather and also because we needed to trouble-shoot a few technical difficulties.  The cold temperatures were a little rough on some of the GPS cables, but after troubleshooting the cable issues (with assistance from the great park climbing rangers) we were able to get our GPS and GPR equipment all working properly.  We then installed the GPS base station over the USGS survey marker at Windy Corner with a 20-pound solar power panel, that we also hand carried up to the corner from base camp.  We hoped to record at least 48 hours of GPS data over the new survey marker as a first year of data for comparison to future years.

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Evening view from Camp 14!  Mount Foraker (right) Hunter (left) and the moon…. BEAUTIFUL!

During our stormy weather at Camp 14 (which was relatively mild), Camp 17 received sustained 80 mph winds over the course of one day and up to 50-60 mph winds during the other storm days.  We were happy that we decided to wait out the storm at lower elevation once we heard that news!  After three days of rest at Camp 14 due to the weather and equipment issues, we had a great weather opening to climb towards high camp.

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Climbing past Washburn’s Thumb about 16800 fasl on the West Buttress of Denali.  Coolest part of the climb we all agree!

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Patrick (left) and Kristin (right) on the awesome ridge between Camp 14 and Camp 17!

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Another amazing ridge view!

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And another!

One of the comical decisions of the trip was regarding our tent decision for high camp.  During the climb to Camp 14, we had used two The North Face VE-25 tents for sleeping quarters and a Hilleberg as a cook tent: plenty of room for four people.  BUT, to save weight and account for the added scientific gear weight, we decided to cut down on tents and bring only a single VE-25 tent for the four of us to sleep in.  Needless to say, the tent was plenty warm due to the crammed bodies packed inside the tent at high camp!

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Four of us squeezed in our VE-25 Tent at High camp! We were definitely warm enough!  (photo: Blaine Horner)

We had a few more days of poor weather at high camp while waiting for a summit bid.  In fact, we were not optimistic after two days of poor weather reports, unfortunately.  However, one thing about mountains is that the weather reports change almost as often as the weather.  After three days of waiting at high camp (with only one book to read between the four of us… Blaine wouldn’t read to us from it either!), we finally had a good weather report (or at least reasonable report) for the morning.

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Looking up at the Autobahn which traverses up to the low point in the skyline, left of center.  Wind and clouds at the summit on this day;  We waited another day to climb to the summit.  It was less windy (but still windy), snowing and more clouds unfortunately!

On June 23, we woke to relatively calm conditions at high camp, but cloudy conditions up high.  Hoping it would clear up and deciding this was our weather chance to make the summit, we headed up the hill, first tackling the Autobahn, a well-known and treacherous portion of the route on a steep and icy slope that gains almost 1,500 feet of elevation from high camp to Denali Pass.  Patrick and Blaine started out in front of Kristin and I, two rope teams in teams of two.  We all reached Denali Pass relatively quickly but here is where the day became more interesting.  Upon our arrival at Denali Pass, we found another team who had attempted to summit the day before.  It turns out they had an accident that evening prior and one of their team members suffered a potential head injury.  Following some discussion, the decision was made for Blaine to help these two stranded climbers down to high camp while I led Kristin and Patrick upward for our summit attempt.  Blaine passed along his extra science gear to Patrick (which is how Patrick ended up with two heavy pieces of equipment) and we slowly started working our way up the hill in the fresh snowfall, wind, and in and out of the passing clouds.

We also passed another large guided party at Denali pass making our team the first roped team of the day to push forward towards the summit.  Three solo climbers (no ropes) bounced in front of us, which we were quite happy with because they helped blaze a trail forward in the fresh powder snow which is exhausting to break trail in at over 18,000 feet!  Our climb to the summit was slow, steady, and honestly relatively uneventful (which is a good thing!).  We consistently checked on each other for warmth, comfort, and pace.  Our slow and steady pace found us on the summit ridge within a few hours of departing Denali Pass.  Unfortunately, the weather never really cleared up on the summit ridge.  For those of you who live in the northeast U.S.A., it was basically like a good cloudy day in the Presidential Range of the White Mountains in New Hampshire: windy, cold, snowy, but all were manageable with a slow pace and focus on our health and comfort through the entire day.  We reached the summit about 10 minutes before any other guided parties or roped teams reached it.  At the summit we didn’t waste much time checking out the scenery because we really couldn’t see any!  Kristin likens the view to the inside of a snowball. We were all pretty exhausted from the equipment haul as well, so we just set to work on our goal: to measure ice thickness with radar.  Kristin, Patrick, and I combined the radar equipment into my pack, linked all the cables and batteries together, AND VOILA!!! The radar turned on, the GPS synced with the radar, and we were in business. This is not to say that we expected the system NOT to work, it’s only that in all of our collective experiences working in the field, it’s usually never easy, works right the first time, or something goes wrong!  We were pretty psyched to get the system up and running on the first try.  Unfortunately, the one thing that DID go wrong during our time on the summit is the arrival of other summit teams as soon as we got the radar system up and running. This meant that we had a limited amount of time or access to the summit because others surrounded the summit upon their successive arrivals.  We completed three radar transects while near the summit: one from below and up to the summit marker, a second from the summit marker down slope, and a third that started down slope of the summit and traversed up and over the summit down a short portion of the West Buttress route.  After 20-30 minutes we finished our survey work, snapped some photos of us at the summit, and were ready to head down.  We were all tired and ready to make it back to camp but had several hours of slow downhill traverses to reach our comfortable sleeping bags.

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Myself, Kristin, and Patrick at the summit of Denali.  Not much of a view today unfortunately!

 

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Collecting radar data at the exact summit of Denali!

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Setting up the GPR at the summit of Denali!

We returned to high camp around 9:30 pm after summiting, about 13 hours from start to finish: not a HUGE day by mountain standards but long enough to look forward to a good night’s rest. We made several rounds of water on the MSR stove, had a ramen and mashed potato dinner, and were curled into bed by midnight. The following morning, we were packing by 9:30 am, ready to make a long 14-mile, (10,000 foot elevation change) push back to base camp.  We had another beautiful but climber-packed traverse from high camp down to Camp 14, arriving there around 3 pm.  This traverse section of the route is our collective favorite part of the West Buttress climb due to the steepness of the ridge and amazing scenery.  At Camp 14 we decided to take a mini-break to let temperatures cool down.  We dug up our cache of gear, and spent a few hours lounging around in the sun.  At 7 pm we started down the hill hoping to make it to Camp 11 within 3 hours.  It was beautiful to Windy Corner, but at the top of Squirrel Hill we were met by white out and snowy conditions which persisted the rest of the way to Camp 1.  But, temperatures were comfortable and we were all feeling pretty good.  Kristin and I left Camp 14 first with Patrick and Blaine following about an hour behind.  They traveled on skis making their descent more speedy and efficient than ours (our skis were cached at Camp 11). With the time differential, we all arrived at Camp 11 within 10 minutes of each other.

At Camp 11, we dug up our last buried cache, ate some smoked salmon and other snacks, and Blaine linked up with a friend who was kind enough to melt us some more water to save us time.  Blaine and Patrick again relaxed for a little longer while Kristin and I started slowly down the hill in the whiteout, traveling wand to wand with hopes of reaching camp 1 in another 3-4 hours.  Travel conditions were fairly atrocious on this leg of the route, unfortunately.  With a thin crust of ice over water-saturated snow caused by warm temperatures, whiteout and snowy conditions making for poor visibility, and our tired selves, Kristin and I decided skiing was not a safe option.  Unfortunately, with the skis off, the poor snow conditions caused us to post-hole slowly down the hill (post-holing means sinking into the snow up to our thighs upon every step).  Despite sinking into the snowpack, we decided the personal control and ability to keep our rope tight between us while traveling on this potentially crevasse ridden region of the route, was more important than traveling faster (as in on skis).  The talented skiers on our team (Blaine and Patrick!) were able to negotiate the route on skis, but skiing skill DEFINITELY played a role in their rapid successful descent!

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Resting at Camp 14 after the summit and decent from Camp 17

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View during our rest at Camp 14!

After a strenuous descent to Camp 1 arriving around 3 am, Kristin and I decided to set up camp for a few hours to get some rest.  We had been on the go since 10 am the prior morning with a few stops at each camp.  A little rest prior to completing the last 5.5-mile ski to basecamp would do us well!  During the rest stop, I brewed some more hot water, enough for a couple glasses of hot apple cider, and then we rested for a few hours.  I laid awake, listening to teams slowly trudge by us over the next couple hours.  It’s a common occurrence for teams to “death march” from the summit back to base camp over 24-48 hours- a continuous push without setting up a camp and sleeping.  Most of the teams that summited with us on June 23 were trying to do just that, each resting at various locations along the descent.  After three hours, Kristin and I were ready to go again.  After 30 minutes, we were packed up and had our skis on for the final trek back to basecamp.  We arrived into basecamp after a relatively uneventful ski, around 10:20 am, over 24 hours since we departed high camp the day before and less than 40 hours from our successful summit of Denali.  After a relaxing hour wait at basecamp we were on a flight back to town with Talkeetna Air Taxi.

Upon arriving in town, a shower, full pizza and calzone, ice cream, and relaxing on the town green was all in order.  Great end to a successful field season.  In a few months time (once we process data), we will distribute results of our field effort so folks can learn more about the science we accomplished this year.  Overall, a fantastic team, a fantastic effort, great support from TAT, the park service, Compass Data, USGS, and a very enjoyable field season!  Enjoy the many photos!

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Drying equipment and gear out back at Talkeetna Air Taxi in Talkeetna….  my pants no longer stay up after loosing about 14 pounds over this last 2 months on Denali and by Mount Logan!

 

Heading to the Mountain!

Hi all,

Quick note to let folks know that we will be heading to the mountain today, WE THINK!  We are having breakfast at our favorite morning food stop, the Talkeetna Roadhouse, and then heading back to TAT for check in.  Weather is looking pretty nice in Talkeetna but my phone radar app shows some clouds over the mountains.  Time will tell what our friends at base camp call in for a weather report.  Fingers crossed!

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The Talkeetna Roadhouse! If you visit this place, they have amazing Sourdough Pancakes with lots of blueberries and blackberries!    

Remember to follow along on my homepage at https://alpinesciences.net/ where my Twitter updates will display while we are in the field!  I am using my Delorme In Reach to send short updates to my Twitter, Facebook, and website pages simultaneously.  Each message I send will link to a map showing exactly where we are located on the West Buttress climbing route so we hope you follow along!  With a little bit of luck, patience, and perseverance, the next large BLOG I post will be back in Town Talkeetna after a successful field season! Cheers!

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Reminder of the route we will be climbing and primary locations we will be studying enroute up Denali, starting in a few short hours!

A DAY “OFF” IN TALKEETNA

We arrived safe and sound in Talkeetna, Alaska around 9:30 pm on Saturday evening.  We popped over to Talkeetna Air Taxi (TAT) to check on some missing shipped gear that we need for our field work (TAT was closed by the time we arrived), snagged a hotel room at the Swiss Alaska Inn, and then bounced downtown to visit some climbing friends at the local evening hangout, Fairview Inn.  Blaine was able to meet up with colleagues he hadn’t seen in a couple years and we talked with them about current climbing route conditions, considering they just came off Denali.

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Kristin and I at TAT, Saturday evening

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Amazing Plane! The Otter…

On Sunday morning we ate breakfast at the Inn and checked in with TAT. They helped us locate three of our missing bags which just arrived yesterday in Talkeetna.  We are still missing two bags but they are the less important of the five total bags so it seems our project is now officially a go!  We talked for a bit with the great folks of TAT (including owner of TAT, friend, and long-time supporter of science research in Denali, Paul Roderick).

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Blaine (center) and Brian Wright (USGS-left) looking skeptical as I explain ground-penetrating radar for use in measuring snow and ice thicknesses.  Seriously, it works guys!

We then bounced over to the DNP Ranger Station for our briefing with park rangers.  Every climber that goes onto Denali needs to fill out climbing permit paperwork in advance of their climb (which we had). Upon arrival, every group meets with a ranger to discuss their climbing objectives and some other pertinent details.  For example, we let the rangers know the color of our tents, our emergency communication capabilities (we have a Delorme In-Reach and a satellite phone), our planned route, and proposed start/end dates for our time on the mountain.  The rangers also summarize current route conditions and any policies which are pertinent to our climb.

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Lots of climbers this year but not a very high success rate!  Usually its a 50% success rate, not 35%!

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That’s a big foot!

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The marker we are installing at Windy Corner

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A comparison of markers on display at the ranger station. Note the center marker and the sticker in the upper right hand corner.  Blaine and team from last year surveyed the Denali summit at 20,310 feet above sea level, 10 feet lower than previously thought.  Now everyone has to change the elevation listed on all their Denali-related memorabilia!

Considering we are one of over 1000 climbers who are registered to climb the West Buttress of Denali this year, the rangers provided a detailed summary of:

  • Where their rangers are located on-route right now;
  • Where and how we can cache gear and equipment along the route, that we don’t need for the entire climb;
  • Where we can dump human waste on the mountain;
  • What is required for all climbers to have when traveling to higher camps on Denali;
  • Recent weather events such as snowfall or wind that significantly influence the safety or condition of the route (i.e. avalanche hazards, wind slabs, icy route conditions, etc.).

Ironically, probably one of the most commonly asked question by non-climbers is about how we manage human waste in the field (i.e. how and where do you go the bathroom? What do you do with the human waste?).  SO, I’ll give you a little run-down here as it relates to the West Buttress climbing route.  The park staffs a seasonal ranger station (tent) at base camp (7,600 fasl) where you fly into the West Buttress and a second at 14,200 fasl.  Pit latrines have been established at both sites where climbers can go pee in a hole. However, climbers also use a lightweight and portable 10” diameter capped-PVC tube called a “clean mountain can” (CMC) to sit on like a 5-gallon bucket, for #2!  The park provides biodegradable bags to line each CMC which you fill to the brim before you pull the bag out and tie it off like a trash bag.  Certain crevasses (large cracks in the glacier ice) on the Kahiltna are approved dumping grounds for climbers to toss their biodegradable bags of human waste into, with the idea that over time it is biodegrade.  This said, the most conscientious and environmentally friendly climbers try to minimize leaving their waste on the mountain so they also have the option of transporting it out via plane at the end of their season.  High on the mountain where the slopes are mostly ice due to high winds scouring the glacier, all waste is required to be carried down the mountain to lower elevations.  It’s a pretty extensive and impressive leave-no-trace strategy considering climbers often stay on the mountain for 18-20 days per group.  Lots of research has actually gone into the current waste management plan.  For example, here is a link to a peer-reviewed paper by colleagues about waste management on the Kahiltna!

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Clean Mountain Cans, ready to be used!

Another cool fact: Rangers patrol from base camp all the way to the summit and back to help answer climber questions, make sure climbers are following waste management (and other) regulations, and to be available in the event of an emergency which needs immediate attention (for example climbers who may have injuries from a fall, cold related injuries or illnesses such as frostbite or hypothermia, or high altitude illnesses).  Rangers on Denali are the backbone of the park and the climbing rangers are also a wealth of knowledge.  While at the ranger station, we bumped into a long-time ranger, now friend, and supporter of our science efforts, ranger Joe Reichert.  It’s always good to see the familiar faces in Talkeetna but Joe is one of those that has a tendency to stand out for both Blaine and I.  He is always positive, always has a smile on his face, and is ALWAYS psyched to chat about climbing, science, the park, or anything outdoors.  In reality, all of the rangers at Denali are similar to Joe in this manner so it’s always fun working alongside of them on the mountain.

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Joe Reichert with Kristin, myself and Blaine (left to right) in the Talkeetna Ranger Station

 After our ranger visit, we returned to TAT to organize and weigh all our gear which will be flown onto the mountain.  TAT (and any flight service provider for that matter) needs to know exact weights of everything so it’s a standard process to weigh every little piece of equipment.  With the organization and weighing of our gear out of the way, now we play the waiting game!

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Kristin weighing my skis and ski poles

Poor weather (snow and low clouds) has base camp socked in right now and it’s a down-pour in Talkeetna so it’s a no-fly day.  Will killed the rest of the day by eating pizza for lunch at Mountain High Pies (where we also ran into a friend and long-time pilot, Tony who showed us a cool video he recorded of sub-glacial melt water flowing out from under the vegetation-covered tongue of nearby Ruth Glacier), ice-cream at Nagley’s General Store, checking out various local artist shops, and walking down to the Susitna River.

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Nagley’s General store with a few other businesses.  Perhaps food at the West Rib may be in order today.  Check out their “Sewards Folly” burger.  4 pounds of meat in one burger!

At the Susitna, we realized that flying onto the glacier may be delayed for a few days, BUT, overall, it was a nice relaxing day yesterday to catch up on rest after the long travel day to arrive in Talkeetna.

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Where is the mountain?!  View last night across the Susitna River towards Denali… Maybe weather will improve tomorrow!

It’s raining this morning but that means breakfast at the Roadhouse.  They have amazing food in a comfortable family style atmosphere… Amazing black and blue (blueberries and blackberries) sourdough pancakes! Blaine, Kristin, and I just finished eating so now we wait and see what today brings!

RESEARCH ON DENALI: ‘THE GREAT ONE’

Yesterday, Kristin and I set off on a new exciting research adventure back to my old stomping grounds: Denali National Park and Preserve (DNP), Alaska.  2015 was the first in eight years that I had not returned to the wonderful town of Talkeetna, the hub of access to glaciers and mountains in DNP.  Talkeetna is one of my favorite towns in the country and for several years it turned into a summer home base for me.  Amazing people, wonderful businesses, caring community, all within walking distance of each other and a backdrop of the Alaska Mountain Range. Who could ask for more in an Alaska town?!

the highest mountain in DNP also happens to be the highest in North America at 20310 feet above sea level.  This peak was formerly known by U.S. citizens as Mount McKinley but its name was recently reverted back to one originally provided by natives of the area: “Denali” or “The Great One.”  It seems fitting that a place which is still wild, remote, and rugged by anyone’s classification, bears its original name.  Denali creates a trifecta view with two other large peaks in the area: Foraker (17,400 feet above sea level) and Hunter (14,573 feet above sea level). Native stories tell of Denali being the Father, Foraker being the mother, and Hunter being the child.  These three peaks create the ultimate backdrop to the town of Talkeetna when viewed across nearby Susitna River.

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“The Great One” (Denali) viewed from Middle Hunter Peak on the flanks of Mount Hunter (photo by Karl Kreutz, 2013)

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Mount Foraker from the summit of the Middle Peak on Mount Hunter in 2013.  Note the snow covered valley on the right side of this photo is the ice divide that we collected two surface to bedrock ice cores from in 2013.  You can see some ski tracks in the photo where we collected ground penetrating radar ice depth measurements.

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The big three: Mount Foraker on the left, Mount Hunter in the middle, and Denali on the right in the back.  Just in the sun near the shadow of Hunter you can see a dark area in the snow.  That was the ice core drill site in 2013.

The first reported successful ascent of Denali was in 1913 by a group up the Muldrow and Harper Glaciers located on the North side of Denali.  In 1951 Bradford Washburn and his team forged their way up the Kahiltna Glacier to the summit of Denali.  Today, more than 1000 climbers per year attempt to climb Denali via the West Buttress along the Kahiltna Glacier, the same route that Washburn’s team climbed over 70 years ago.  Approximately 50% of those climbers are successful with the remaining climbers being turned around prior to reaching the summit due to a number of reasons.  Climbing the West Buttress is an enormous endeavor: 13,000 feet of elevation gain along 18 miles of crevasse-covered glaciers, steep, and icy slopes over the course of 2-3 weeks in sub-arctic conditions can challenge the most proficient climbers.  Add 50-100 pounds of extra research gear on top of what climbers typically bring with them, and our team has our work cut out for us.

The mountain is big, hazards are real, weather and temperatures can be extreme, and climbing at elevation is just down-right exhausting, challenging, and even dangerous due to potential altitude related illnesses.  SO, in front of our primary research goals for this season that I list below, we have a fourth goal which is ultimately the most important so I list it first:

Our goals this year are to:

1) Maintain the health, safety, and well-being of our team.

2) Install a USGS survey marker on bedrock at or near 14,000 feet above sea level which will be used for repeat elevation surveys of Denali over the next several years to estimate tectonic uplift rates;

3) Measure the ice thickness on the summit of Denali at 20,310 feet above sea level, using Ground-Penetrating Radar;

4) Collect snow samples along an elevation transect (some snow at high elevation and some at lower elevation) on the mountain to compare their chemistry.

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Proposed climbing route and research sites for this years effort on Denali 

My colleagues and I have written lots about our prior research efforts in DNP on previous BLOG’s so if you are interested you can bone up here.  We also have several papers published on the Kahiltna Glacier and other regions within DNP that are listed here.  This year’s research effort is funded by two primary sources:

The first source is from the U.S. Geological Survey to our team leader, Blaine Horner, who works for Compass Data Inc.  Their funding is provided to install the USGS monument and radar survey the summit of Denali.  The second source of funding is from Dartmouth College to continue the snow chemistry research and other associated projects as part of our long term ice core research effort within DNP.  The teams for each project decided to team up in effort to minimize impact on the mountain (i.e. fewer climbers) and also to combine resources.  As always, a hearty thank you goes out to the many individuals working for the park, air service providers, and within the town of Talkeetna who continue to make our research a possibility.  The summit team for this project includes Blaine Horner, Kristin Schild, Patrick Saylor and myself.  Bio’s for Blaine and Kristin are below. Bio’s for Patrick and I can be found in our Eclipse research (prior blog posts).

Blaine Horner: Blaine is an account executive for CompassData Inc. and he pieced the proposal together to install the GPS monument and collect radar data at the summit of Denali.  Blaine has a pretty extensive outdoor history which includes ski patrolling, surveying, and search and rescue as a ranger for Denali National Park.  In 2015 his team successfully resurveyed the summit elevation of Denali which had not been completed in recent time.  Prior elevations were listed as 20,320 feet above sea level but Blaine’s more recent survey with current technology revealed an elevation of 20,310 feet, 10 feet lower than previously thought.  Find more about Blaine’s 2015 effort here. Thanks for the initiative in pursuing this great project and for the invite Blaine!

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Kristin Schild: Kristin is in the final year of her PhD at Dartmouth College within the Earth Sciences Department.  Her research focuses on understanding subglacial water controls on tidewater outlet glaciers in Greenland and Svalbard.  She has participated in over a twenty field seasons in places including Svalbard, Greenland, Alaska, and Antarctica and it’s probably her favorite part of the job.  She has also spent a ton of time working with ground-penetrating radar, GPS, meteorological stations, and oceanography instrumentation as well as using remote sensing data from satellites to study glaciers, oceans, and landforms.  In her spare time Kristin is also on the New England K9 Search and Rescue Team with our Coonhound, Kinley and she volunteers as a diving instructor for Dartmouth and local 8-12th grade students in the Upper Valley of New Hampshire.  Oh yeah, in all her free time she ALSO is a substitute science teacher for Indian River Middle School in Canaan, NH!  She is a busy woman so we are psyched to have her along!

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Kristin (second from the right) in one of her many elements with some of the students she teaches science to at Indian River Middle School!

Patrick Saylor: Just a photo for Patrick considering he already has a bio a couple posts back!

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Seth Campbell:  Not much reason to have a bio of me here so, also just a photo!

Climbing

5/24/2016

Well, yesterday was a big day!  Thanks to the Icefield Discovery pilot, Tom, we were able to get our entire team out of the field over a 24 hour period.  What a successful season! General stats are as follows:

  1. 81 meters of ice core drilled (one 64 m core and one 17 m core)
  2. 40+ km of ice-penetrating radar to measure ice thicknesses
  3. 40+ km of GPR to measure shallow horizons for recent snow accumulation studies
  4. 20 short-term ice flow velocity stakes measured
  5. Dozens of caramelo bars, snickers bars, and coffee crisp bars eaten
  6. About a 1 pound bottle of Sriracha Hot sauce consumed (mostly by Dom!)
  7. Some other crazy Habanero hot sauce consumed by Steve!
  8. A very healthy and happy smiling team coming out of the field!

I’ll write more about our experiences and research soon but, a video  (courtesy of Justin’s camera work) and photos (courtesy of Karl and myself) are worth a thousand words. Here are some teasers to start with.  Enjoy!

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5/7/2016

Today, we first want to give a big shout out to the awesome staff at Icefield Discovery who are helping us to successfully accomplish our research in Kluane National Park & Preserve. Sian is the camp manager (and has been our awesome main point of contact for this work). She is following in her fathers footsteps, running the show.  Lance is the do EVERYTHING, fix EVERYTHING, help ANYWHERE kind of person that every great program needs to be successful, not to mention he guides folks for the program.  Tom is the very happy, funny, and experienced pilot who will get us safely to and from our research site on the Icefield. Ashley and Emily have been cooking up a storm, and cleaning, and numerous other daily camp duties to make sure all the visitors have what they need while staying at the camp.  We are so thankful for their hospitality!

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Standing (L to R): Dan, Emily, Sian, Dorota, Justin, Patrick, Steve, and Dom; Sitting (L to R): Ashley, Bronwyn, Dov (the pup!), Lance, Seth, Karl, and Tom

Last night the camp manager for Icefield Discovery, Sian, told Karl and I that we would be either first or second up for flights this morning as our first attempt to reach the ice core site.  Good news considering our ice core equipment coming from UMaine via a shipment, which was delayed by over a week, arrived yesterday afternoon.  After the exciting news from Sian, our team tore into the ice core equipment to check that all the parts were in order.  Karl and I also prepped the first load of gear to go in with us.  We are limited to about 760 pounds of weight per flight which includes person weights which means that Karl and I had about ahmmmm….  lets say  400 pounds to play with and fit more gear onto the plane besides ourselves.

Our gear list included the following:

  1. Personal packs (with sleeping bags, clothes, pads to put under the bags in our tent, toiletries,)
  2. Tent and tent anchors: A Bibler Bombshelter (nice 3 person single walled mountaineering tent which would provide plenty of room for Karl and I plus our personal gear).
  3. Skis (for both of us)
  4. Food and Camping Equipment:  We went with a couple MSR XGK mountain stoves and an MSR cook kit.  Both are pretty light and packable.  for food, lots of rices, pastas, and other one pot meals that make for easy and quick cooking and an easy cleanup! breakfasts typically include oatmeals, some dried fruit, or cereals with powdered milk. Snacks during the day are pre-cooked sausage or sliced meats, cheese, gorp, candy bars (Caramelos are amazing and snickers bars are the old stand-by!)
  5. Technical gear: two of each of the following, harnesses, belay devices, pickets, ice screws, and ice axes; lots of carabiners, several prussiks, a climbing rope, and a few other fancy trinkets to keep us safe when travelling around on the glacier where huge cracks under the winter snowpack known as crevasses wait to try to swallow us up! (99.9999999999999% of the time the crevasses don’t swallow us whole – don’t worry mom we are being safe!) If you are not familiar with some of the climbing and glacier terminology we use (students following along with us in the classroom perhaps?) look online for photos and examples!
  6. Research Gear:  Karl and I decided to bring as much research gear as we could fit on the first flight.  We included some ice penetrating radar equipment which we use to measure snow and ice thicknesses on the icefield, and some GPS equipment which we use to measure how fast the ice is moving at the site we are studying.  We will explain about the GPR and GPS equipment on another post!

We maxed the plane out at 740 pounds so not bad for a guess weight on our first flight!  We hit the hay close to midnight and were up and running again by 6:30 am.  We loaded the plane up and received our safety briefing with pilot, Tom Bradley.  By 9:30 am we were in the air heading towards our study site.  One MINOR problem:  as we came around the bed in the valley we traveled up with the plane, we ran into a low lying cloud bank that blocked our passage into the mountains we were trying to reach.  We returned to camp with our tails between our legs but with hopes that it would improve through the day.  Weather reports suggested a high pressure system coming this way so we were initially pretty confident we would have another shot at it today.  By 11 am we anti-ed up to try again, only to be thwarted a second time due to clouds hanging over our little section of the ice field.

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Flight path from the GPS for our second flight towards our research site.  Although it was not a success due to clouds, we got some nice views!

As I sit at camp now, we are watching the cover the mountains and fill the access valley so it looks like we will have to wait for another attempt tomorrow.  BUT, we have acquired  have some photos and videos over the last few days so the delay provided a chance to provide a teaser of the season start, below.  Check them out!  Thanks Dan Dixon (for photos) and Justin Leavitt (for video) below!

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IMPORTANT NOTE:  So we are one day delayed?  SO WHAT!  Have I ever told you the story of our team making it all the way to Antarctica, sitting around for about 5-6 weeks, and then returning home, never making it to our study site because of bad weather?

Rule # 1: patience is important in this type of work!

Check out Icefield Discovery facebook link here and their webpage here.  Their parent non-profit organization, Kluane Lake Research Station operated by the University of Calgary can be found here.