Tag Archives: Nature

Oh My, Fungi!

There have been many times when I stooped during my meanders through the woods to look at fungi, often not considering that I was only seeing the fruiting body of a large underground network of “hyphae” – small root-like structures which interact with many species in woodlands. Most of the time I only contemplate the color, shape, or size of the mushroom, and move on without ever being able to identify the species. I believe that experience is the same for many others. However, as I stood on the deck at the Folk School in Fairbanks, Alaska and watched a band of kids ranging from age 7-12 roam through the woods with mycologist Christin Anderson, I was excited to learn of the species they brought in!

I was astounded by the diversity of mushrooms brought forth – in a short time they had collected over 10 genus, and many more species. Functionally, the collection of mushrooms ranged from parasitic, to decomposing; one species even grew on decomposing mushrooms! We observed the variety of color and size of each by touching and looking as Christin explained that it is not possible to absorb the toxin of any mushroom through the skin, although most people believe that you can. It was certainly news to my ears! On top of that, I didn’t know the hallucinogenic compounds in mushrooms are the not same ones that can kill you; poisons and hallucinogens are separate things.

I think mushroom identification is the hardest part of being a mycologist, and is simply overwhelming for those of who are not mycologists. However, with Christin at the helm of at least identifying each of the mushrooms to genus, I was excited to look up information each. Here’s just a little of what I learned about the diversity of the world of mushrooms.  As a result of my research, I am in awe of the functionality that mushrooms play in Alaskan ecosystems.

Below are a images of the mushrooms collected. If you are receiving this post via email, you may have to visit the post to see them, since there are too many to be sent in the email.

 

Literature and websites:

http://ncbi.nlm.nih.gov

http://www.shroomery.org/

en.wikipedia.org

http://www.mushroomexpert.com/

http://mushroom-collecting.com/

http://www.wildmanstevebrill.com/

http://www.backyardnature.net/

Michelot, D., & Melendez-Howell, L. M. (2003). Amanita muscaria: chemistry, biology, toxicology, and ethnomycology. Mycological research, 107(02), 131-146.

2016 Alaskan Calendar is Now for Sale!

Hello Everyone,

I am very, very, very  excited to write inform you of the release of my 2016 calendar! The content features some of the best imagery on this website, plus a few things that have never seen the “light of day”. The calendar is entitled “Seasonal Moods of Alaska” with imagery for each month captured in that month. The calendar is 100% designed by me including feature images, transparent images, windows, and text tying the imagery to the season. A huge thanks to my family and fiance for helping to proof the calendar! I believe the final product is a work of art mingled with science.

If you want to see it, clicking on the cover image or link link will bring you to the sales site that I created.  Otherwise, keep reading for some more information 🙂

2016 Seasons and Moods of Alaska Cover

https://ianajohnson.com/customproducts/

The calendar is printed on 9.5×13 paper and spiral bound leaving ample of room to write in your schedule. Of course it has a hole for hanging if that is all you want to do with it! With imagery from throughout Alaska, the calendar is a great memento of your trip to Alaska, for a friend who has been here, or to bring inspiration for your future trip here!

This calendar is being printed by my local shop in Perham, Minnesota. Your consideration and support also helping the local economy in Perham.

2016 Calendar Final 9halfx138
Each month has a premier image. This image from Mendenhall glacier showcases the high resolution imagery within the calendar.
2016 Calendar Final 9halfx1323
Every month has a transparent image behind the grid, and small windows with images from that month. Writing in the lower right panel ties together fuses the imagery and writing together.

The calendar will be available for pre-order through October 15th. At that time I will begin shipping orders. You can help me out a huge amount by spreading the word about this calendar or through a purchase! Thanks you so much in advance for your support in this project!

Autumnal Aurora

I jumped when my alarm went off at 11:30 PM, and I looked at my surroundings to remind myself where I was. The sleeping bag wrapped around me and my reclined seat reinforced I was in my truck as my blurry eyes brought the steering wheel in focus. My memories flooded back to me; I arrived 30 minutes ago, and with no aurora in sight had set an alarm and took a nap. I was expectant that a G2 storm forecast was going to pay out, and as I peered out of trucks window it seemed I was in luck. The aurora was starting to show a band high in the sky. I turned the ignition, and drove down the road to find the “perfect”, golden tree – my goal for the night was to fuse autumn colors and the aurora together.

I stood on the road with my head craned up, watching a beautiful, green aurora band overhead. This aurora was  Mr. Jekyll which soon morphed into Mr. Hyde – albeit a beautiful version of him.  I was not ready for the full force of the aurora as it transformed the sky into a green and pink blanket of shimmering, dancing lights so different than what I had been looking at minutes earlier.  The energy that rolled overhead, I learned later, was the result of a monstrous, KP7 event, that pushed the aurora into Washington and the Midwest.  I was so overwhelmed by the aurora that I expressed myself by simultaneously singing, praying, and taking pictures by myself under the vast display of lights. For those who know me, you might guess that I was also grinning broadly from ear-to-ear. My smile would not have disappointed you!

For parts of the night, my only focus was to capture the overhead aurora corona to the best of my ability. The last time I successfully captured the corona was in Denali National Park last year. I couldn’t be more happy to show you this gallery of images from last night  – there were many more taken! The gallery is chronological, and hopefully gives a sense of the scale of the aurora and how quickly it built. These images are taken at 9mm, and hence have a ~120 degree field of view!

I am continuing to boost my online portfolio, so please stop by if you have a moment! A selection of these images has been added to my Fine Arts America Photo Gallery for purchase. Thank-you for your consideration!

Fine Arts America Photo Gallery

Matanuska Glacier Peril

I arrived back at the car from after a couple of hours hiking around on Matanuska Glacier, and my clothes were still wet. Although the day on the glacier had been beauty-filled and grand, I had learned a steep lesson on glacier safety.

We reached Matanuska Glacier just as the sun was starting to come out again. During the drive up the Matanuska Valley the sun illuminated the mountains that rose high on each side, and the Matanuska river lay below us along the curvy, Glenn Highway. As we stood in the parking lot we could see a 4 mile-wide swath of ice at the front of the glacier called the terminal moraine. From there the glacier stretched back over 26 miles into the mountains! We walked down the safest path of firm glacial silt and ice, which was marked by orange cones. In a few more minutes we stepped onto the full glacier.

Hindsight is always 20/20, which is why I now realize that stepping away from the orange cones which marked the “safe trail” was more risky than I previously thought. In a quest for images I moved through the ice hills of the glacier looking for pools of water to shoot reflection shots from. I walked through ankle deep, sticky mud towards higher ground where the glacier had deposited a gravel pile. From there I stepped to the edge of some flowing water, stuck out my toe to test the depth of the water, and immediately slipped off the ice edge and into the water. I never hit bottom!! The flowing water had cut a deep, deep pool which I now found myself in up to my shoulders. During the fall I was fortunate to have turned myself around quickly, so I put my elbows up on the edge of the glacier and pulled myself back out. In the fall my camera and tripod fell into a pile of glacial silt, and fortunately not into water with me. The incident lasted only a few seconds before I was back on solid ground and moving quickly away from that deep pool. I stripped off my wet shirt for warmth, used it to begin cleaning my camera, and shook a bit as the adrenaline set in.

What is particularly annoying (to me) and perturbing about the situation, is that I was not doing any unnecessarily risky. In fact, when I slipped in I was testing the water before stepping in. So, I’m now asking you to learn from me – test unknown and murky pools with a long stick, rather than a short toe!

Aside from a scrape with death, our day at Matanuska Glacier was remarkable. The gallery and images below details the gigantic ice face as well as the tiny details of the glacier.

Striations in this piece of ice caught Kass' eye, and the lighting sealed the deal. I love this image of a glacial ice cube.
Striations in this piece of ice caught Kassie’s eye, and the lighting sealed the deal. I love this image of a glacial ice cube.
The face of the glacier was carved in interesting ways. This up-close shot looks at the melting ice on its surface.
The face of the glacier was carved in interesting ways. This up-close shot looks at the melting ice on its surface.
These large rocks melted rapidly, providing a brilliant blue window into the glacier.
These large rocks melted rapidly, providing a brilliant blue window into the glacier.
This panoramic image looks back at the glacier, and down the headwaters of the Matanuska River.
This panoramic image looks back at the glacier, and down the headwaters of the Matanuska River.
Semipalmated Plover
A semipalmated plover feeds in the glacial till and among the ice cubes of the Matanuska Glacier.
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The end of a happy day at Matanuska Glacier!

Watching a Glacier Die

Drop a few ice cubes in your drink before you start reading this, and consider the question : how many licks does it take to get to the center of a Tootsie Pop? Now, while you are thinking about that illusive answer, consider how many days it takes to melt a glacier. Just how fast does it happen? My several trips to Castner Glacier over the last 15 months provide interesting evidence into this impossible to answer question. Let’s take a look!

April 2014

When I first visited Castner Glacier in April 2014 a monstrous, multi-chambered ice cave shook me to my core. The ice cathedral hung over my head an estimated 80 feet above. The walls and ceilings of it were composed of blue, transluscent layers of ice and closer inspection of the walls showed that the clarity of the ice provided a window deep into the glacier of the sediment suspended in it. A chimney was cut into its ceiling allowing light to illuminate the icy floor of the glacier.  It was awe inspiring!

Castner Glacier Face April 2014
This was the glacial face (moraine) as I found it during my April 2014 visit. Clear, blue ice was found in the face, and particularly in the caves.
Castner Ice Cave Cathedral
Once you walked through the ice caves, this cathedral was found on the other side. I guess, based on my height in this picture compared to the ceilings, that the cave was 80 feet tall!
Castner Glacier Chimney
This chimney was found in the ceiling perhaps 20-30 feet above the glacier floor in April 2014. It was very narrow at the top, but the bottom is much wider than this picture would suggest. The icicles at its base suggest that some melting was occurring in it.

This video was taken in April 2014 during a walkthrough of the ice cave and captures the scope of it. Instability of parts of the video was due to the slippery ice floor!

August 2014

The next time I visited the rainiest summer recorded in Fairbanks was coming to a close, and the rain had reshaped the ice in unimaginable ways. Water ran down the glacier in small rivulets and opened the chimney to a yawning mouth. It degraded the ceiling so extremely, that large chunks of the cavern had crashed down. If you stood close to the mouth of the cave many rocks fell dangerously from the ceiling as they melted from their icy tomb of thousands of years. The rapid melt had removed the beautiful transparency from the ice. It was now silty and gray.

Castner Glacier Collapse
When we returned in August 2014 we found the result of the constant rain over the summer. The chimney had melted so rapidly that the roof of the ice cave had collapsed.
Castner Glacier Ice Cave Backside
This image shows the degradation of the chimneys from the top and back of the glacier. Although I didn’t take an April 2014 photo for comparison, this image is especially revealing when compared to June 2015 (upcoming images)
Castner Ice Cave Scale
My parents stand next to the ice cave’s face for perspective. The large blocks that stood in front in April were now gone, and the top of the cave is much, much thinner than just three months earlier. 
Castner Ice Cave Front 2015
This image from the front of the caves shows a large section of ice which caved off the front. The scale and setting of this picture is similar to the April 2014 image of me standing in front of the broad ice cave.

The rapid melting that we witnessed inspired me to create a different type of video for Castner. This video documents the fall (August) stage of plant life around the glacier, and then documents the progression of drops of water from the glacier which eventually build into the silty and fast-flowing Castner Creek.

June 2015

When I visited the Castner Ice Cave in June 2015, it was just a shadow of its former self. Only a small arch of ice remained of the once huge cave. Castner Creek ran through the remnant of the ice cave, where previously it had run to the side. In just fifteen months, unquantifiable amounts of ice from the glacier had transformed into water, carrying with it many tons of silt to the broader river valley that Castner Creek flowed into. The glacier was rapidly changing, dying.

Castner Ice Cave Back June 2015
This image of the Castner Ice Cave was shot in June 2015 from the back. The thin, collapsed chunk of ice in the foreground is all that remains of most of the ceiling of the cave.

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Castner Ice Cave Back Panorama
This image of the back of the Castner Ice Cave can be compared to the images taken in August 2014 and April 2014. The trailing edges of the large ice cathedral that I stood in can be seen in the back right. The arch of the glacier is thin, and a new chimney shows that it continues to degrade.
Castner Glacier Backside Panorama
The trailing edge of the ceiling on the right is all that is left of the ice cathedral from April 2014. Large piles of debris and silt have been deposited, and the floor where the cathedral was is much higher now.

The answer is two hundred fifty-two. At least that is what students at Purdue concluded to the center of a Tootsie Pop. But why does it matter that Alaska’s Castner Glacier and the state’s other glaciers are melting so rapidly? Alaska Dispatch News recently reported on a new study demonstrating that Alaskan Glaciers are losing 75 billion tons (75 gigatons) of ice each year, and that 94% of that loss is occurring on inland glaciers like Castner. This means that Alaskan glaciers will continue to contribute a significant amount to global sea level rise, especially in light of a warming climate. They end the article with a quote by study co-author O’Neel. “This is probably going to be a pretty tough year for a lot of the glaciers”, he stated. It appears he is right, and Castner’s included.

Go When The River Says Go

I was excited to head far into the Alaskan bush by river to help a friend open his cabin for the season. Almost a week of packing led up to the Wednesday we were supposed to leave.  However, when the middle day of the week arrived, high water reports from Fort Yukon and the Upper Porcupine River were ominous. Record snowfall in Old Crow, Yukon Territory, had swollen the giant river systems. They were far above travel-able levels, and over-flooded banks were pulling dangerous amounts of debris, ‘drift’, into the river. Our final destination was 220 river miles through the high water and drift of the Yukon and Porcupine Rivers, and the experienced judgement of Joe dictated that we would wait a few days before heading up to his cabin. Four days later the river had dropped to acceptable levels. It was go-time : the river was saying so!

Before I get into some of the stories of the trip. Come along on the trip with me by watching this video:

The notion of taking a boat far into the Alaskan bush is exciting! A long-time resident of the bush, Joe was anxious to open his cabin, and assess his estate because bears, humans, or weather can all impact an unoccupied cabin.  The boat-trip up river started in Circle, Alaska on a cloudy day. As we headed downstream in the Yukon River, we quickly entered the Yukon Flats National Wildlife Refuge. This expansive refuge is critical, critical habitat for breeding waterfowl and birds. In fact, the refuge hosts 150 species of breeding birds from 11 countries, 8 Canadian provinces and 43 of the 50 states. That’s remarkable diversity!

This is Delta, our wonderful river dog companion!
This is Delta, our wonderful river dog companion!

The Yukon Flats is aptly named. As we cruised along in the boat, the shores were a steady patchwork of riparian habitat consisting of willows, birch, and spruces. There was no perceptable climb in elevation. The fast, high water of the river kept progress slow, and Captain Joe was constantly vigilant for pieces of drift. Three foot-long sticks and entire trees were coming down the river at the rate of several or more pieces per minute. Hitting a small branch may result in a dented prop, but a large stump could have ended the trip. By the time we reached Curtis Slough to stop for the night, the intense driving had drained Joe (and rightfully so!). Overall we made it about 135 river miles from Circle.

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As you move along the river there are cabins dotted along the way. Some of them, such as this one provide permanent shelter year around for bush dwellers. Others are seasonal or may just provide shelter for passing travelers.
Schuman House
An old cabin at “Schuman House”

We pulled into a small log cabin along the banks Curtis Slough, hoping to spend the night. The traditional landing was underwater, but I jumped ashore with the bow rope and headed to tie off to a nearby tree. I glanced at the cabin, and immediately saw that the plywood door had been torn in half; peeled back like the lid of a sardine can. “Hey Joe”, I stated, “A bear broke into the cabin, by tearing the door off”. “Ok, does it look fresh?”, he questioned. I assessed the raw wood in the torn door from 25 feet away and responded, “yup, sure does!”. By that time Joe had climbed up with Delta, our dog companion. Delta moved towards the cabin and sniffed the door; her demeanor immediately told us that it was a very fresh break in, and then I heard a can rattle from inside. The bear was still in the cabin! In two flicks of a lamb’s tail we were in the boat and headed across river to camp on a more desirable (bear free) gravel bar. Joe, knowing the owner of the cabin, made a satellite phone call to inform them of the situation. Remarkably, this bear encounter was the only one of the whole trip!

The next morning we continued up the Porcupine River, and moved out of the Yukon Flats and into the Arctic National Wildlife Refuge. The Arctic NWR is the largest piece of land in the refuge system, and home of the Porcupine Caribou Herd. No longer in the flats, we saw a mountain on the horizon! More significantly, that mountain was the beginning of the rocky ramparts which would line the river for the rest of our trip. The tall and colorful ramparts and bluffs of the Porcupine Rive were a welcome contrast to the Yukon Flats! As we moved through the landscape, the smile of enjoyment could not have been erased from my face by the spray of a skunk. The area was absolutely stunning; on a small scale, I was reminded of the Grand Canyon. Red, orange, and black rock walls rose high above the water. The bluffs held countless caves and spires shaped by wind, ice, and snow. The refuge of the high cliffs provided important nesting habitat. As we passed we noticed nests of golden eagles, ravens, and a peregrine falcon protected on all sides by the vertical rock faces.

Two hundred and twenty-two miles upriver we passed the final bluff across from Joe’s cabin. The boat swung around towards the opposite bank and soon I tied it off onshore. Already I felt connected to this beautiful region, and was excited to spend the next five days exploring it. The next chapter of cabin life to come soon!

Oh, and as one last, unrelated note the blog turned two on May 28th. Thank-you ALL for your continuing support. Your feedback, comments, and enjoyment of the material here is much appreciated!

Highlights of an Alaskan Bird-a-thon

The Alaska Songbird Institute has a goal for people during their second annual “Bird-a-thon” : find as many birds as you can within 24 hours in Alaska. We, team MRI (Madi, Ross, and Ian), decided to take the task seriously! We started our 24 hour window at 8:00 PM by birding a range of Fairbanks hot-spots. From there we headed south along the Richardson highway with the goal of making it Paxson to bird the Denali Highway – a 134 mile stretch of wetland potholes and alpine tundra chock-ful of birds.

May 15th was the first day the Denali Highway was officially open, and much of the Denali Highway’s tundra was still covered in snow due to 3000′ elevation gain. Because of the low-productivity of snow-covered areas, we targeted melt areas and ponds. There were many, many species of birds. Some of them, such as red-throated loons were still passing through to breed on lakes further north over the Brooks Range, using the Denali Highway region as a “stopover” until the ponds further north were ice free. But, the site was not a stopover for most. Many of the birds were there to make a nest and raise young in the 24 hour light. The tundra is the summer home of many species which are found in vastly different habitats during the winter. For instance, the long-tailed jaeger is an ocean bird. During the summer they nest in the tundra and eat berries and small rodents. Quite a change from the fish they traditionally consume! Wilson’s warbler migrate to South America, and arctic terns migrate to Antarctica (the longest animal migration). In fact, the Alaskan tundra is so unique and special that birds from six of the seven continents can be found on it. For those that see the tundra frozen in the winter, it is easy to forget the tundra is a highly valuable and necessary ecosystem!

Aside from the birds, the scenery of the Denali Highway is never ending! The melting ponds and flowing rivers created a patchwork of light and dark across the land. To the north, the horizon was ragged like torn cloth with the mountains of the Alaska Range. In the twilight at 2:00 AM (because it no longer gets fully dark here), the Alaskan Range stabbed through the colors of the sunset and on bluebird days like the one we had its snow covered peaks starkly contrasted the thawing tundra and blue sky.

Along with the birds, there was plenty of mammals to see. By the end of the trip we watched well over 20 moose and probably 30 caribou. Arctic ground squirrels fed along the roadsides, and frolicked across the snow. The young animals of spring are out and about, and we enjoyed watching a red fox kit chew on some grass outside of its den after we returned to Fairbanks.

Alaska Range Caribou
A herd of caribou navigate around a pond with the expanse of the tundra behind them.
Moose
A mother moose and her yearly calf browse on new growth of willow.
Velvet Bulls
Two bull caribou lounge about in velvet antlers.
Fox Kit
This fox kit was a joy to watch. You can tell by the smooth walls of this den that they have spent quite a bit time going in and out.

So, bringing it back to where it all started, why go birding for 24 hours straight? It seems that it might be a bit crazy (for instance getting about 3-4 hours of sleep). To understand that, you simply have to understand what I believe birding is. Birding is a chance to observe the natural environment either individually or with friends. An opportunity to go birding with a two great friends (we rock, MRI!) in a place as remote and diverse as Interior Alaska is a moment to relax and learn something new (essentially a guarantee); it should not be passed up. Even if observing wildlife is not for you, my definition of “birding” can be modified to fit almost any hobby. Don’t pass up opportunities to learn and be with good friends. After 24 hours, we identified 68 species of birds; a pretty remarkable list and I cannot wait until next year’s Bird-a-thon!

Bird list
Here’s the list of observed species during team MRI bird-a-thon. 68 species in 24 hours! Ironically we did not turn up a black-capped chickadee – very ironic considering they are a classic species of Alaska.

A Wood Frog, Blog

Visually and sonically the pond was alive. Golden light of a pre-evening sun poured over the pond, and where the light fell on the far bank the sound of spring in Alaska, a loud wood frog (Rana sylvatica) chorus, echoed in the birches. Wood frogs are the only species of amphibian found in Interior Alaska, because let’s face it : there are not many species that can withstand -40 degree temperatures! In the winter, wood frogs burrow into the soil under leaves or woody debris and concentrate glucose in their blood as anti-freeze. However, the glucose only provides some relief. In the cold months with little sun, their heart stops beating, eyes freeze, blood freezes, and brain activity stops. By almost any definition the frogs would be declared dead, but when spring temperatures arrive the frogs thaw out from the inside-out (instead of the outside-in, scientists have no idea how), resume life, and jump into local ponds for reproduction. It was that yearly event that I stood in the middle of with my camera.

I waded into the ~55 degree water, and through the old vegetation of the pond. Crossing the 60 foot wide pond to where the frogs called, resulted in water mid-way up my thighs and soaked my pants. I draped a camouflage cloth over me and waited like a giant, brown heron (or maybe the swamp monster) for the frogs to start singing. When they did it started as a single croak which seemed to say “all clear”. Within no time the life of breeding wood frogs unfolded all around me. Only a few feet away, each frog that called swelled up pockets of skin along their cheeks and side, and sent a rippling well of water out from its body. I think that communication occurs both by sound and by the small waves of water, although that is just an observation. Many of the male frogs chased females while rapidly swelling their air sacs, calling, and sprinting towards females. Often their approaches seemed to be rejected. I watched as many males swam up rapidly to a female and attempt to mount, but were thwarted by an elusive mate. Often in denser vegetation, groups of frogs boiled in the water as a constant struggle to maintain a female ensued. As I watched the frogs many mosquitoes fed on their exposed heads. After seeing that, I hypothesize that frogs are an important early food source for mosquitoes. I stood for 90 minutes while my legs turned into cold stumps, and finally decided that I couldn’t take the cold water much longer. However, my 90 minutes in the water was worth it! The short video below captures just some of this behavior. Be sure to watch them call in slow motion. Enjoy!

Frogs in the spring have long been a part of my life. Growing up, my open window in the warming days would let their songs in. In the Midwest, higher frog species diversity adds a wider range of tenors and bass to the chorus. The small, 200 foot diameter “frog pond” just inside the woodline is a consistent producer of leopard frogs (bass), spring peepers (tenors), wood frogs, tree frogs (several species), and likely others. The frog pond was an important stomping ground for my brother and my nature education. Although I never got to observe the frogs very often because they were pretty elusive, we often collected eggs and tadpoles for rearing. So, finally after all these years, the opportunity to see these frogs in Alaska up close was a real treat!

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A quick selfie of frog photography.

Want to learn more? Check out this video highlighting some ongoing University of Alaska Fairbanks research!

By a Team of Seven Into Heaven

It seemed like a good omen that the clouded skies cleared to bluebird conditions as we pulled into the parking lot of Wickersham Dome. The unexpected blue skies cheered us on as we went about threading our ganglines, clipping on snowhooks, and packing our sleds. Eager and expectant dogs watched our progress, and when we began to hook them up their tug lines, they fed upon each others energy. Leaping, pulling, and baying they waited for me to pull my snowhook and quickrelease. When I did, the sled lurched over the hardpack of the parking lot, banked left onto the main trail, and we were on our way to Crowberry Cabin, 30 miles into White Mountains.

Sled dogs have a plethora of personalities. Jeff (friend and owner of Black Spruce Dog Sledding) let me know that Sooner, one of my dogs in lead only pulled well for “people he liked”, and I was conscious of that trait as we made our first stop. I walked up to the front of the team and gave Sooner a good pat on the head. “Keep it up, bud”, I stated. I’m not sure if my initial approaches made a difference or not, but Sooner and Stoic, the lead along with him, pulled great the entire trip with their heads down, and always with some tension on the tuglines. Behind the leads, Simon, an old veteran pulled well too. As a veteran dog he knew his roll in the team and worked hard. Sniffing the tip of Simon’s tail was Beaver and Scorch. Finally, taking “wheel”, Grizz and George were responsible for pulling hard. George can be a great worker, and out of my entire team he is my favorite. He loves to check out what’s going on, and since his position was closest to the sled, every time I opened the sled bag he craned his neck to get a look inside. Together they were my team of 7, and I was happy to be pulled by them!

Crowberry cabin sat on a facing to the west, and the peaks of the White Mountains surrounded us. The wooden cabin looked iconic for the Alaskan Wilderness. Throughout the Whites, these public use cabins serve as refuge for those who venture far. Trappers, hunters, mushers, or snow machiners make use of them. The full log construction of this cabin was wonderful, and when once we built a fire and warmed the inside, it was a truly incredible getaway. The four bunkbeds, dinner table, and camps stove, and lantern made it into a 5 star Alaskan Suite. However, admiration of the cabin was actually secondary to the task at hand. I walked along the gangline of the staked out dogs and tossed out beef snacks. We layed down straw for each of the pairs to keep them off the snow, and started heating up water for their main course – kibbles and meat. Building a fire, we enjoyed the sunset and fed the dogs their final meal.

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This was Jeff’s dog, and a notorious chewer. To prevent any damage to the gangline or necklines, this dog got his own bed of straw and post at a tree.
Our lookout.
Our lookout.
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A moody landscape over the White Mountains.
Curved black spruces in the white mountains
Curved black spruces in the white mountains
Crowberry Cabin
Crowberry Cabin
The sunset over the white mountains illuminating the edge of the snow-carrying front.
The sunset over the white mountains illuminating the edge of the snow-carrying front.

The next morning an inch of powdery snow had fallen over the night. My team was wide awake as I stepped outside for the first time, and George gave me a happy tail wag. I dusted the snow off my sled, packed my gear, harnessed my team and hit the trail. The dogs were just as eager to set out on the trail as the day before. The intermittent, light snow shaded the hills and made our ride home far different. The sprawling vistas of the White Mountains were gone, replaced by a moody gray. The next 4 hours breezed by, and before I knew it the Wickersham Dome parking lot was back under foot, ending an incredible experience and trip!

The opportunity to experience dog sledding for an overnight trip is the fulfillment of a life-long dream. I have literally wanted to drive my own team since reading about fictional characters “Lew and Charlie” in Fur Fish Game, stories by Jack London, or books like Jim Kjelgaard’s “Snow Dog”. Those stories have fueled my imagination and desire to visit open spaces since I was twelve. I have always been drawn to the mystery, adventure, and vastness of remote areas. The White Mountains are just one of the broad wilderness areas of Alaska, and the opportunity to experience it using the low-impact “Alaskan” method was truly a gift!

Jeff's team was a bit faster than mine, and I captured them here as we headed back home.
Lindsey’s team was a bit faster than mine, and I captured them here as we headed back home.
The crew. Jeff, KattiJo, and Lindsey. A great trip!
The crew. Jeff, KattiJo, and Lindsey. A great trip!

Into the Mouth of an Ice Beast

The receding glaciers in the Bays of Southeast Alaska are opening up barren landscapes and new lands for colonizing vegetation and birds like arctic terns. As we walked along Sitaantaagu (Tlingit : “The Glacier Behind the Town”), I felt connected to the misty, snow covered mountains, and rocky lake shore. It is renowned and spectacular country!

Mendenhall glacier is receding at up to 150 feet per year, and in 1900 the large quantities of melt water began forming Mendenhall Lake.  The lake is now home to salmon which have colonized glacial streams. Remarkably, it seems that colonization by salmon occurs in a decade or two. Much shorter that I ever suspected!  As we, a large group of wildlife biologists, walked along the shoreline of Mendenhall Lake and told stories of field seasons gone-by or hypothesized on natural processes, icebergs which had calved from the glacier drifted in the middle of the lake.Naturalist Bob Armstrong introduced me to a small, alpine wildflower called purple mountain saxifrage.  This early bloomer, he stated, is a critical resource of early emerging insects like the bumble bees.

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Purple saxifrage is one of the first spring flowers to bloom in the Juneau region.
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Purple saxifrage filled with the rains of Juneau.

The face of the Mendenhall Glacier got bigger, and bigger, and bigger as we approached. By the time I reached the front of the glacier it loomed in front of me for almost a half mile.  I walked up the river of melt-water in front of the glacier and  touched the edge of the the ice cave it had carved. I grinned a bit, threw myself over a three foot bolder guarding the cave and stepped inside into the mouth of the icebeast. I was awestruck. Curved, turquoise ice hung over my head like whipped meringue. The sound of the river reverberating in the small space was numbing, and was fed by each drop of water that fell from the ice into the river. Looking further up the cave, the color transitioned from turquoise to cerulean blue. As I walked further the surrounding area turned so blue, that I could have been scuba diving in an ocean.

The hardest part to capture in these pictures is the scale of the ice cave. It stretched back over 100 feet, and as I walked in the ceiling diminished from 7 feet, to 5 feet, and finally I was relegated to crawling on my hands and knees in the narrow space.

The way ‘out’ was graced by a set of rock ptarmigan. These birds, allowed me to get very close, and I framed up this shot with the face of the Mendenhall Glacier in the background. These ptarmigan won’t be white for much longer!

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A beautiful rock ptarmigan in front of Mendenhall Glacier
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A puffy rock ptarmigan!

Glacial recession in expansion in Alaska has occurred since the last glacial maximum. The Little Ice Age caused the expansion of Alaskan glaciers about 4,000 years ago, and recent recession has exposed what has been buried for nearly a millennium. These stumps were exposed by the receding Mendenhall glacier and were aged to nearly 1,500 years ago! “Deep time” can be hard to comprehend, and it amazing to think the Imperial Chinese Empire had been established for 800 years and that Medieval Europe was enforcing fiefdoms through rigid monarchies when these hemlock and sitka black spruce were buried!

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A large stump of a forest buried by ice ~1,500 years ago. It has been determined the forest was composed of hemlock and sitka black spruce.
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This stump field is degrading fast, but it’s likely more forests will be uncovered as the Mendenhall Glacier receeds even further.