Tag Archives: video

Virtual Cranes

“When we hear his call we hear no mere bird. We hear the trumpet in the orchestra of evolution. He is the symbol of our untamable past, of that incredible sweep of millennia which underlies and conditions the daily affairs of birds and men.” –Aldo Leopold – Marshland Elegy, A Sand County Almanac.

The sandhill cranes of Wisconsin

I’m slow to embracing the virtual world, but now that winter has arrived in the North, and plenty of time on my hands, but without the inclination to travel anywhere, I’ve done some virtual exploring.

In the spring, the Platte River in Nebraska is the place to be, to see the siege of sandhill cranes flying through to eat and rest before heading further north. In the autumn, however, the Wisconsin River near Baraboo, WI is a major stopover for this ancient breed of birds.

The Aldo Leopold Foundation usually offers tours and blinds for crane viewing and photography in the fall, but 2020 is not the year for those types of activities. Instead, they offered a virtual visit to the Wisconsin River and the over 10,000 cranes that are camping out along its banks. I joined one of these visits this week, and found it incredibly informative, and well produced. Still, no virtual visit compares to seeing the sandhill crane in person, or hearing and feeling that prehistoric bugle as it flows through you from across the terrain and the eons.

Luckily, next spring, I won’t have to go beyond my deck to experience them again.

The above video is one done previously by the International Crane Foundation and the Aldo Leopold Foundation.


SS Arthur M. Anderson

The Arthur M. Anderson

The freighter, Arthur M. Anderson, had been trailing the Edmund Fitzgerald during the fateful, November storm, that sank the Big Fitz in 1975. The Anderson reported the missing ship to the U.S. Coast Guard, and had made the safety of Whitefish Bay in the early morning hours of November 11, 1975. The Anderson then joined other ships, and reversed coarse back into the storm, to look for survivors.

After making the post on the Edmund Fitzgerald last week, I received a tip from Ogdensburg, New York along the Saint Lawrence Seaway, that the Anderson was back on Lake Superior on the 45th Anniversary of the sinking of the Fitz. In fact, it had passed the location of the wreck of the Fitzgerald early on the tenth, and came into the Duluth Harbor that evening.

Arthur M. Anderson coming through Duluth Harbor 10 November 2020; Photo credit: Duluth Harbor Cam

I was simply amazed that the Anderson was crossing the same waters on the 45th Anniversary.

The Arthur Anderson travels comes into Duluth under the iconic lift bridge, gives salute to the Edmund Fitzgerald

The above video is 9 minutes long, the Anderson appears at the 3:50 mark. The Master Salute to the Fitzgerald would have been something to experience in person along the canal.


Alaska Jökulhlaup

A large glacial dam gave way in Southeast Alaska this summer. Known by its Icelandic term: jökulhlaup, the power of this sudden release of pent up water can be incredibly destructive.

The terminus of Lituya Glacier; Photo credit: NPS/J. Capra

Desolation Lake, which sits above the Lituya Glacier in Desolation Valley, collects meltwater from both the Desolation and Fairweather Glaciers. That meltwater is normally blocked by the Lituya Glacier, forming the roughly four square mile lake.

The water level suddenly dropped 200 feet.

A commercial fisherman, Jim Moore, along with his two grandsons, tried to enter Lituya Bay to fish for Chinooks in August. They should have been riding the tide into the bay, but the unusually muddy water was moving outward, and it was filled with trees and other debris. The bay was also filled with small icebergs. Moore managed to bring some of the ancient ice onboard for his coolers, then left the bay, instead of fighting the dangerous current.

Lituya Glacier terminus and delta; Satellite image credit: USGS

It is one of the largest jökulhlaups known to have occurred in Alaska. The water found a path under the Lituya Glacier, causing a rush that would have rivaled the hourly discharge of the Amazon River. It would have lasted for several days.*

Lituya Bay has a history. In 1958, an earthquake triggered a landslide that started one of the largest known tsunamis at over 1700 feet.

*NPS Geologist, Michael Loso


Moose joins soccer match in Homer

A moose jumped a fence to join in on a pick up soccer match in Homer, Alaska. The moose appears to be a bit of a ball hog, but I was disappointed when the other players chose not to pass the ball back to the moose. I wouldn’t have been able to resist.

Another view, complete with commentary

Welcome to Alaska, Gunner.


After the Ice: Our Food

Part I:

The Arctic Research Consortium of the United States has put together a series of videos entitled After the Ice. The videos highlight the changes and the dangers to Alaska’s remote communities, that have relied on the sea ice for their livelihood and sense of community. The first video, which runs approximately 7-1/2 minutes, shows the extent that residents of remote Alaska rely on the sea ice for their source of food.

Much of Alaska, including many in communities like Fairbanks, live a subsistence lifestyle, relying on the land to provide sustenance. It’s a good series, on a population that few Outside even know exist.

Our garden is dying, is a line that cuts to ones heart.


Newtok Power

The village of Newtok, Alaska

Some regular readers may remember that I was out in the village of Newtok in February. I truly enjoyed my time there, and have great memories of the area, but especially the people.

Newtok is currently in the middle of a move. The village is under siege from the very water that gives it life. Due to the warming of the Arctic, ground is giving way, and Newtok is getting it from every direction. On one hand, the river is laying claim to huge chunks of land, taking homes with the shoreline. On the other hand, the ground is giving way to the melting permafrost, and water is filling in the gaps. In February, approximately one third of the population had moved across the river to the new location of Mertarvik, but it is going to be a long and complicated process.

Newtok made the news again this past week, when word made it around Alaska, that the generator that powers the village broke down, leaving the residents without power for an entire month. A month. In an age when most of us think about power very briefly, when we flip a switch or pay the electric bill, it’s good to remember that not everyone lives in such a situation.


Looking at the village from the air in the summer, it’s an entirely different world than when I was there in February. The contrast is stunning, so I thought I’d share a few more “winter” pictures of my time in Newtok.

Newtok on my flight in.

Walking the village of Newtok; Camera: Widelux

Newtok arrival

Brooks Falls Bear Cam

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Click to link below to visit the Katmai “Bear Cam”, from explore.org:

 

https://explore.org/livecams/brown-bears/brown-bear-salmon-cam-brooks-falls

 

 


The Return to Mount Kennedy

Connecting Generations through ice & snow:

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After the assassination of John F. Kennedy, the people of Canada wanted to honor the slain president.  In November 1964, the Canadian government, following the suggestion of famed mountaineer, photographer and cartographer, Bradford Washburn, elected to name an unclimbed peak in the St Elias Mountain Range, Mount Kennedy.

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RFK on Mount Kennedy

The mountain lies 145 miles from Whitehorse, YT, within Kluane National Park, and less than 10 miles from the Alaska panhandle.  Mount Kennedy forms a triangle with Mount Alverstone and Mount Hubbard.  At the time of the dedication, the mountain was the tallest (13,944 ft) unclimbed peak in the St Elias range.

National Geographic put together a team to make the first ascent of Mount Kennedy in 1965.  The team was led by Jim Whittaker, who had been the first American to climb Mount Everest, and was made up of mostly experienced mountaineers.  Also making the climb: Bobby Kennedy, to honor his fallen brother.

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Jim Whittaker & Robert Kennedy on the summit

On 24 March 1965, the climbers made for the summit.  This was Kennedy’s first taste of mountaineering.  To add to the tension, RFK was no fan of heights.  The other climbers insisted that politics was far more dangerous than climbing mountains, which would prove prophetic.

Crossing the Cathedral Glacier, Kennedy fell into a crevasse.  Luckily, it was a narrow one, and he only went in to the waist, and quickly scrambled out.  The final run to the summit is the most risky, as the climber has to traverse a narrow ledge with a sheer one thousand foot drop.

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Photos credit: Whitehorse Star

Jim Whittaker and Bobby Kennedy would become good friends on the climb, a friendship that would last until Kennedy’s death.  Whittaker would name one of his sons after the U.S. Senator.

50 Years Later:

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The Whittaker Brothers

Fifty years after the original ascent of Mount Kennedy, the two sons of Jim Whittaker wanted to honor their father and his friend Robert Kennedy.  They decided to climb the mountain themselves.

Leif Whittaker is an experienced climber like his father, but Bobby Whittaker had more experience in Seattle’s Grunge Scene than summiting mountains.  Christopher Kennedy, the son of RFK,  would join the Whittakers on the expedition.

Return to Mount Kennedy is the documentary about the two ascents.  The footage from the original climb is pretty impressive to see.

I saw a screening of the documentary prior to the Coronavirus outbreak.  It was put on by REI, the outdoors store, which had Jim Whittaker as its early CEO.

The documentary is available on several streaming platforms.  The original National Geographic story can be found in the July 1965 edition of the magazine.

Trailer: Return to Mount Kennedy


The sound of moving water

Welcome back


The thaw has finally come to the north.  Running water, which has not been visible for several months now, can be found at every turn.  The change of seasons, so dramatic towards the ends of the earth, is an adventure to experience every year.

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The melt is slowly crossing The Pond

The transition season in Alaska’s Interior is a quick one, as a friend recently reminded me.  As I wrote earlier, it has been years since I experienced the spring thaw in its entirety.  I’m enjoying break up, even though boots are often required to experience the melt, close up and personal.

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Creamers Field

The snow is all gone out at Creamers Field, the local waterfowl sanctuary.  The field was loaded with geese, ducks, a few sandhill cranes, and more trumpeter swans than I usually see out there.  The swans arrived early, and are taking advantage of the retired dairy farm.  I took the Leica out there, so we will eventually see if anything will come out of those pictures.  The swans were putting on a show that day, so hopefully I captured something on film worth sharing.


Dall Sheep

Alaska’s Big Five; Chapter Five:

 

Dall Sheep, Ovis Dalli dalli, can be found throughout Alaska’s mountain ranges.  Dall Sheep prefer relatively dry country, their territory is the open alpine ridges, mountain meadows and steep slopes.  They like to keep an extremely rugged “escape terrain” close at hand, and are not often found below tree line.

The rams are known for their massive curling horns.  The ewes have shorter, more slender and less curved horns.  The males live in groups and seldom interact with the females until breeding season, which is in December.

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Lambs are born in late May to early June.  Ewes usually reach breeding age at 3-4, and have one lamb each year after that.  The lambs are most vulnerable during their first 30-45 days of life, and mortality rate is high during this time.  Wolves, black & brown bears and golden eagles are the main predators.

Dall sheep horns grow steadily from early spring to late fall, but tend to slow, if not stop growing altogether, during the winter months.  This leaves growth rings on the horns called annuli.  These growth rings can help identify the age of Dall Sheep. In the wild, 12 years of age is considered old for a Dall Sheep, but rams have been identified as high as 16, and ewes up to 19 years of age.  A Dall Sheep ram can weigh up to 300 pounds, with the ewes being about half that weight.

Between 1990 – 2010, Dall Sheep numbers had dropped by 21%, from 56,740 to 45,010.  Numbers started increasing up until 2013, when a later than average snowfall put a damper on recovery efforts.  Dry, heavy snow loads appear to have little effect on sheep population, but the heavy, wet snowfalls, with a frozen crust can make foraging and travel difficult.  Freezing rain has also become more prevalent.  All of these factors contribute to more avalanches, which have become a significant cause of death for Dall Sheep in the state.

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