Monthly Archives: November 2012

The Glacier Trips: Final Story, October 2012

Here it is – the final installment of my blog series about Yosemite’s glaciers.  Thank you for following and I hope you enjoyed the series!  If you’d like to read the first three posts to this story, click here.


Mt. Lyell and Lyell Glacier, from a USGS photo point, Lyell Canyon

October Glacier Trip

The first weekend in October found me again, hiking the long trail from Tuolumne Meadows through the beautiful Lyell Canyon.  My destination – The fourth and final encounter of this year, with Yosemite’s remaining glaciers.  I decided to hike ahead of the survey team for this trip; partly to experience the hike solo, but also to have additional time to photograph places along the trail I had been wanting to connect with—and had spotted on previous trips.  It was a beautiful day!  I stopped several times for photographic opportunities.  Below, I think, exemplifies early fall in Yosemite’s high country.

Old logs, Lyell Canyon looking north

Lyell Glacier and Peak, Lyell fork of the Tuolumne River, Lyell Canyon

I met up with the team later in the afternoon and we headed for our previous campsite during the September survey.  Volunteering for this trip was Greg Stock’s wife Sarah Stock, Brian Whitehead, Matt Holly, Jessica Thompson, Jen Jackson, and Dustin Garrison.  Arriving to camp before dinner gave us plenty of time to set up camp, eat, and watch one of the Sierra’s finest light shows!

Firey Sunset above the Kuna Crest, Yosemite high country

This trip was simply to get one more velocity measurement from the stakes in both glaciers, then take the stakes out and complete the four-year study.  We headed for the Maclure glacier first.  Freezing night temperatures helped keep the stakes in place, which made for easy measuring and removal (except for two stakes frozen in the ice).  Again, the weather was very good, so working during the day was a pleasure and sleeping at night was very restful.

For this trip, I could only work until noon on the first day.  This was because I had also been monitoring the development of the fall leaf color progress on the eastside and thought it might peak during this same weekend; thus, the plan was that I would leave the glacier trip a day early.  Greg and I connected after the weekend and he informed me that measurements on the Lyell Glacier were equally easy as on the Maclure.

If you read my previous blog, you will remember that I have initial findings from the survey that Greg Stock said would be appropriate for me to share and publish here.  Here they are!  First – the good news.  A recent correspondence with Greg revealed current velocity measurements of the Maclure Glacier:  “The Maclure Glacier moves about 22 feet per year, with somewhat faster motion in the summer than in the winter.  Our August-October measurements were indeed very similar to Muir’s, with about one inch per day of movement.”  Greg added that he and geologist Bob Anderson (the other part of the study team on the survey) are puzzled by the movement because the glacier is 60% smaller than the 1872 Muir study “with about 120 feet of vertical ice loss”.  The glacier is still moving and during our July trip, a few of us heard and felt the glacier’s bass-like creaking and popping sounds that seemed to indicate that movement was occurring underneath our feet – somewhat unsettling sounds when on the glacier!

By contrast, the data collected from the Lyell Glacier tells a very different story.  From July – October, Greg’s velocity measurements showed that the Lyell had no movement…at all!  Even with the Lyell’s larger surface area, making it visually the largest glacier in the park (and one of the largest in the Sierra), the data suggests dramatic change.  I’ll remind you once again that in order for a glacier to be called such, it needs movement.  It must have enough mass to keep that movement going and continued formation of ice to maintain the previous two.    The recent survey’s numbers were also gathered during a season in which a Sierra glaciers’ movement would be the greatest – during the summer months (as Greg stated above).

All the Lyell’s information puts Yosemite National Park’s first appointed geologist to the task of what to call the large ice structure below the northern slopes of the highest peak in the park.  As I write this, Greg is writing his report on the four-year glacier study, no doubt checking over the stats once more and finalizing his conclusions.  Computer models will be created to help interpret the data more easily to park service officials and the public.  “One thing is for sure”, Greg points out during one of the survey trips, “The news that’s revealed from this will be big!”  Greg has the report’s tentative finish date sometime in early 2013.

Panorama, Western Lobe of the Lyell Glacier, July 2012.  There are four people, just above the end of the right-entering talus field and below a single boulder, for scale.  Click on photo for larger version.

Being the 2012 glacier survey’s regular photographer was exceptional!  Not only did I get to travel to one of the most beautiful places in the park, but the opportunity helped to augment my photography skills.  This was the first time I had the chance to document an event, in addition to creating artful photographs.  As seen from my website’s portfolio – there are no humans in my photographs.  It was great to test this new territory.  I learned a lot and perhaps this is only the beginning.  I am also eternally grateful to Greg Stock for allowing me the chance to be a part of this historic survey.  Not only have I gotten to know him better, but I got to meet many volunteers who, like me, share a fascination of glacial geology and wanted to know first-hand what is going on with Yosemite’s glaciers.  Meeting Colorado University, Boulder’s Bob Anderson was equally great, as he had much additional glacial information and enthusiasm to share.

It is also important to note that this isn’t the only recent study of Yosemite’s glaciers.  Hassan Basajic studied many of the Sierra Nevada glaciers and wrote an impressive report on his findings, which you can read here. Of considerable interest for me was Hassan’s use of comparing old photos of the glaciers with his new ones taken in the exact location of the old photos to show visual evidence of the glaciers’ retreats.

I can’t speak for all who participated, but I can say that this experience not only informed me of the current conditions of these ice formations, but it has helped me see the direct effects of climate change in my back yard.  For me, climate change is now more real than ever.  Learning the truth about these glaciers is emotional.  I feel a profound sadness for the loss of these incredible moving bodies of ice.  For now, I can say, “At least the Maclure is still moving”.  But, for how much longer?  Perhaps I can take comfort in the fact that the Sierra glaciers have been growing and retreating, disappearing and reappearing throughout the range’s history.  Maybe, thousands of years from now, the very spot I write this blog from in Yosemite Village will once again be under meters of ice, experiencing the day-to-day ablation of yet another glacial period; erasing any signs of The Ansel Adams Gallery, the scoured Ahwahneechee acorn grinding stones, and possibly even the vertical walls of Half Dome and El Capitan.

The future remains to be seen.

For now though, I have witnessed first-hand and documented through my camera, another diminishing ecosystem caused by our present-day, human-caused, warming planet.  How will this affect all the species, including us, who rely on this resource?  Maybe I should be happy for experiencing these glaciers while they are still here; believe me – I am! Yet, as I look to the future and ponder the National Park Service’s Mission Statement, “… to conserve the scenery and the natural (my emphasis) and historic objects and the wild life therein and to provide for the enjoyment of the same in such manner and by such means as will leave them unimpaired for the enjoyment of future generations.”, I am left with an emptiness that the coming generations will experience a Yosemite impaired; a Yosemite without glaciers. A Yosemite wilderness not mismanaged by its faithful and evolving National Park Service, but by forces much larger than itself—forces that are collective and know no boundaries.

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The Glacier Trips: September 2013

My Apologies for not getting these stories out sooner!  I had an incredibly busy October and time got away from me to write.  With that, enjoy the remaining glacier blog posts!

September Glacier Trip

Park Geologist Greg Stock uploading temperature data to his small laptop.  This gauge has been out in the field since the beginning of the glacier study in 2008.

September’s glacier trip found me on the ice with a team of six volunteers, Colorado University,  Boulder geology professor Robert Anderson (the other institution involved with the glacier study), and of course, Yosemite National Park geologist Greg Stock.  The goals this month:  Record the position of glacier stakes since August and begin the removal of equipment from the area, as the study’s end is the first week of October.  In addition, stream and temperature gauge data was downloaded, as part of a water discharge study, and then the equipment was removed, per Leave No Trace wilderness principles.  The biggest piece of equipment removed was the meteorological station (MET station for short), which has recorded weather data in the region since the early days of the glacier study nearly 4 years ago.  After the final data was collected onto Greg’s laptop, the MET station was dismantled, divided up amongst the volunteers, carried down to base camp and eventually out of the back-country.

Volunteers Brina Mocsny and Scott Borden help dismantle the meteorological station with Colorado University, Boulder professor Bob Anderson (pictured with light cap).

Cooler September temperatures slowed glacial ablation enough to hold six of seven stakes in their positions, making measurements far easier than August.  Still, we had to drill the holes deeper to ensure they would be intact to measure on our final October trip.  While on the Lyell glacier, I wanted to make sure to photograph a marker on a rock face – a ‘K’ – which marked where the glacier’s surface was during a 1933 survey .  I was very interested in knowing the elevation difference between the ‘K’ and the current glacier surface, now below it.  Professor Anderson loaned me his lazer rangefinding device to get this distance.  I walked over to a spot (see below photo), found a piece of exposed ice at the end of the glacier, got down at ice level, and shot the lazer right at the ‘K’.  40 vertical meters came back (approx. 130 feet).

Brina helps give human scale to 79 years of glacial retreat.

So, between 1933 and 2012, the Lyell glacier lost around 130 vertical feet of ice from my position.  To put this in perspective, imagine you were walking on the Lyell glacier in 1933.  You would be 130 feet above my head, more or less, a massive ice sheet between you and me!  It’s not there anymore.  In 79 years, all that ice has melted away.  With 2012 California and national temperatures breaking records for more consecutive highs each year, these conditions seem to point towards more melting.

The most important analysis, however, will be the data collected from the stakes off both the Lyell and Maclure glaciers.  Reading my first blog post from this project, you will remember that in order for a glacier to be considered such, it needs to have enough mass to move.  If it’s not moving, it would be considered more of an ice field than a glacier.

A conversation with Greg revealed even more interesting glacier facts.  The Sierra glaciers have oscillated in behavior throughout the mountain range’s lifetime.  Glaciers have grown and retreated several times.  Greg even mentioned that at one point, glaciers were completely absent from the range.  He emphasized that these oscillations have had thousands of years of regularity between them.  By contrast, this last retreat to present time took only 150 years of time – extremely out of the norm and notably beginning the same time as the Industrial Revolution (roughly 1850); the time when burning fossil fuels and releasing C02 into the atmosphere began in earnest by humans.    “The last 150 years”, Greg points out, “is very much out of [geological] regularity of past Sierra glacial retreats.”

The team walks through a shallow col, while Maclure Peak and glacier tower behind them. Left to right: Taryn Mead, Scott Borden, Bob Anderson, Jonathan Byers

Having finished this trip’s work on the Lyell, the team hiked to the Maclure region the next day for measurements and some clean-up of old stakes, left behind from previous glacier studies, dating as far back as the 1970’s.  Similar stake conditions to the Lyell made for easy lazer rangefinder measuring and re-drilling of the stake holes.  This day found me walking alongside professor Robert (Bob) Anderson, using an ice auger to make the stake holes deeper and holding a prism above the stakes for Greg to get distance measurements from his lazer rangefinding station at the base of the glacier.

Professor Bob Anderson holds a prism to capture the lazer rangefinding beam and send it back to Greg Stock at a fixed position below.

Bob was a pleasure to work with and listen to!  He has previous experience working with glaciers at Glacier National Park and told the group stories about being underneath glaciers, setting up monitoring equipment.  He also worked on Colorado glaciers and had just returned from Alaska studying glaciers there before our trip.  He was grateful for my camera knowledge – especially when I turned on the Highlight indicator in his Nikon camera.  In Bob’s spare time, he enjoys photography and still employs his 4X5 medium format film camera to capture images.

Professor Bob Anderson expounding geologic processes, while park geologist Greg Stock and volunteer Scott Borden listen.

Speaking of being underneath glaciers…After the team was finished with our Maclure Glacier work, Greg took us to one of the Maclure’s amazing wonders – its ice caves!  We entered two at the toe of the glacier and a whole different world revealed itself!  We were on newly scraped rock, covered with glacial flour, while the bottom of the glacier was the roof of the cave.  This world stayed at a constant temperature around 32 degrees Fahrenheit, allowing for all sorts of ice forms to be present.  The pictures below show a few of the things seen there.  Going into the Maclure ice caves was not only a highlight of this trip, but a highlight of all my trips to the glaciers this year!

A naturally occurring ice sculpture in one of the ice caves underneath the Maclure Glacier.

Looking out the mouth of a Maclure Glacier ice cave.

One last note:  Weather on this trip, while cooler and with more wind, was much more pleasant than the August trip (Read my blog post on the August Glacier Trip to see what happened then).  Clouds formed, but rain never fell.  Also, Shauna loaned me her two-person tent, which when pitched correctly, had no problems with the stiff winds we had and allowed me lots of room to keep my gear dry in case of rain.

With each glacier trip, I have gained more respect for Greg and Bob and the information that they are retrieving for their study.  I believe this knowledge will have a significant impact not only on the health of Yosemite’s remaining glaciers, but bring additional and unique awareness to the larger impacts of human-caused climate change.  Stay tuned for part two of this blog on October’s final glacier trip and for future posts when Greg’s final report is done!  The next post will also have initial findings from the survey – the first public writing of the results from your’s truly.  Historic!!

Looking out to the Kuna Crest, with an un-named lake in the foreground. The team camped at this lake!

Sun setting behind peak, near Mt. Maclure

Glorious Sierra sunset over the Kuna Crest.

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