A recent job had me “installing” a phone booth outside a customer’s home. The booth is complete with working pay phone and light. I have not had many requests in the past to get one of these back in working order, but I do like to diversify.
Good things to keep in mind for a future install: A pay phone weighs 55 pounds, so shipping to Alaska is quite hefty; a phone booth, can, with difficulty, be moved by one person with an appliance dolly, but it also slides like a blunt bobsled on the fresh snow.
Possibly one of those only in Interior Alaska moments.
Snow! Finally, we received a nice dumping of snow.
I have 8-9″ of fresh snow outside my door.
I took the snowshoes out for a spin for the first time this season, which required breaking a new trail. The beavers seem to be content within their lodge and under the ice. Any remaining standing trees should be safe until spring thaw, but I’ll keep checking on them.
Otherwise, it was just a nice afternoon out in the woods, checking out the fresh tracks in the new snow. Which includes, for the first time in a few years, lynx tracks. I’ll have to get a trail cam or two out there.
This week is the 17 year anniversary of the 2002 Denali Earthquake. At a magnitude of 7.9, to date, it is the largest quake I have personally experienced.
On 23 October 2002, the Denali Fault released a magnitude 6.7 quake. That would be a foreshock of what was to come on November 3.
Highway Shift; Richardson Highway, circa 2002
After the 6.7, I remember the Alaska Earthquake Center saying that the Denali Fault was capable of producing an 8.0. Sure enough, the fault came very close.
I was at an intersection in my ’66 Chevy C-20. All of a sudden, the truck was lurching all over the place, and I found it hard to stay on the brake pedal. There were two university students in the next lane, the passenger rolled down his window and asked what the hell was happening. I said, “Earthquake”. He then promptly hit the driver on the arm and said, “I told you it was an earthquake”.
The light changed, I drove on, but had to stop at the next light. The earth was still shaking. An elderly couple had been walking on the sidewalk, and the wife fell to the concrete, the husband was struggling to stay upright by hugging a signpost. Then the shaking was over. I rolled down the other window, to see if the couple was all right. They were, and I headed home to see if there was any damage.
The quake had ruptured 205 miles of earth along three different, yet connected faults in Interior Alaska. It was the largest ever recorded in Alaska’s Interior. It was the largest inland quake North America had seen in almost 150 years.
Both the Parks & Richardson Highways saw major damage. The Trans-Alaska Pipeline moved sideways 18 feet, and rose 5 feet. The engineers had designed for the fault, and the pipeline behaved exactly as it was designed to behave. Although, it did come within two feet of its sideways movement limit.
The Denali Earthquake was felt as far away as Louisiana.
Previously, the largest earthquake Fairbanks had experienced was a magnitude 7.3 in 1937.
Halloween saw the fourth year in a row where Fairbanks officially had an inch of snowpack. Trick or Treat without bunny boots? The world is in chaos. By the end of the weekend, three inches of snow lay on top of our ice-coated roads.
Sunday morning saw the return of below zero to The Valley. Monday morning, my thermometer read -10F. It’s damn well about time. For those Outside, I’m sure excitement for below zero seems a bit mad, but Interior Alaska is built for below zero. For those who like to stay in the positive, the high temp made it to the mid-teens above.
This isn’t going to help with Alaska’s lack of sea ice. Utqiagvik, on the Arctic coast was above freezing, as was Nome.
But the Interior is at last making ice. For the moment, at least.
The Juneau Ice Field is located just north of Alaska’s capital city. The ice field covers 1500 square miles, more than a third larger than Rhode Island, and stretches from Alaska across the border into British Columbia. The ice field is home to over 40 large glaciers and more than 100 smaller glaciers. The Juneau Ice Field has been one of the most studied in the world, with the Juneau Ice Field Research Project being conducted annually since 1946.
Taku Glacier, as seen across the Taku River
One of the most talked about glaciers within the Juneau Ice Field has been Taku Glacier. It has been the last advancing glacier within the ice field. It’s “mass balance” has been in the positive; it has been gaining more snow during the coarse of a year than it has lost in melt.
Taku Glacier from the air
Taku is the thickest measured glacier in Alaska. It is considered a high elevation glacier, which has helped it maintain the title of an advancing glacier.
That designation has officially come to an end. With the increasingly warm temperatures that Alaska has been experiencing over the past decade plus, the Taku Glacier is now retreating.
When Taku has calved in the past, it has sent icebergs into the Juneau harbor. Massive calving events would not only send icebergs to Juneau, but also into the Inside Passage.
When Columbia Glacier in Prince William Sound started its retreat, sending icebergs into The Sound, the State of Alaska was forced to create an ice-watch program for oil tankers and cruise ships.