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Duncan Murrell - A Whale of a Time

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Duncan Murrell - A Whale of a Time

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  • My friend and I came across this “stagnating” glacier in Glacier Bay and because it was stagnating there were ice caves that had opened up beneath it. A stagnating glacier is a glacier that is neither advancing nor retreating, but melting in situ, in totality. It was amazing being able to walk beneath a glacier although somewhat precarions because stones were being dropped from the ice as it melted. The colour of the ice with the light shining through it from above was extraordinary; it was definitely one of the most “other-wordly” places that I have ever been to. If you looked closely into the ice you could see and hear all of the tiny capillaries of melt water that were gradually draining the life from the glacier. I wondered how long it had been “alive” for?<br />
Geologists believe that Glacier Bay existed during a minimum of four glacial periods ending with the Little Ice Age, which has a 4,000 years old record, as the latest period. All glaciers in the park today are said to be remnants of this glacial period.
    Southeast-Alaska-glaciation11.jpg
  • My friend and I came across this “stagnating” glacier in Glacier Bay and because it was stagnating there were ice caves that had opened up beneath it. A stagnating glacier is a glacier that is neither advancing nor retreating, but melting in situ, in totality. It was amazing being able to walk beneath a glacier although somewhat precarions because stones were being dropped from the ice as it melted. The colour of the ice with the light shining through it from above was extraordinary; it was definitely one of the most “other-wordly” places that I have ever been to. If you looked closely into the ice you could see and hear all of the tiny capillaries of melt water that were gradually draining the life from the glacier. I wondered how long it had been “alive” for?<br />
Geologists believe that Glacier Bay existed during a minimum of four glacial periods ending with the Little Ice Age, which has a 4,000 years old record, as the latest period. All glaciers in the park today are said to be remnants of this glacial period.
    Southeast-Alaska-glaciation9.jpg
  • My friend and I came across this “stagnating” glacier in Glacier Bay and because it was stagnating there were ice caves that had opened up beneath it. A stagnating glacier is a glacier that is neither advancing nor retreating, but melting in situ, in totality. It was amazing being able to walk beneath a glacier although somewhat precarions because stones were being dropped from the ice as it melted. The colour of the ice with the light shining through it from above was extraordinary; it was definitely one of the most “other-wordly” places that I have ever been to. If you looked closely into the ice you could see and hear all of the tiny capillaries of melt water that were gradually draining the life from the glacier. I wondered how long it had been “alive” for?Geologists believe that Glacier Bay existed during a minimum of four glacial periods ending with the Little Ice Age, which has a 4,000 years old record, as the latest period. All glaciers in the park today are said to be remnants of this glacial period.
    Alaska-ice5.jpg
  • My friend and I came across this “stagnating” glacier in Glacier Bay and because it was stagnating there were ice caves that had opened up beneath it. A stagnating glacier is a glacier that is neither advancing nor retreating, but melting in situ, in totality. It was amazing being able to walk beneath a glacier although somewhat precarions because stones were being dropped from the ice as it melted. The colour of the ice with the light shining through it from above was extraordinary; it was definitely one of the most “other-wordly” places that I have ever been to. If you looked closely into the ice you could see and hear all of the tiny capillaries of melt water that were gradually draining the life from the glacier. I wondered how long it had been “alive” for?<br />
Geologists believe that Glacier Bay existed during a minimum of four glacial periods ending with the Little Ice Age, which has a 4,000 years old record, as the latest period. All glaciers in the park today are said to be remnants of this glacial period.
    Southeast-Alaska-glaciation8.jpg
  • My friend standing under a stagnating glacier at Wolf Point, Glacier Bay National Park and Preserve, Southeast Alaska, USA.<br />
<br />
My friend and I came across this “stagnating” glacier in Glacier Bay and because it was stagnating there were ice caves that had opened up beneath it. A stagnating glacier is a glacier that is neither advancing nor retreating, but melting in situ, in totality. It was amazing being able to walk beneath a glacier although somewhat precarions because stones were being dropped from the ice as it melted. The colour of the ice with the light shining through it from above was extraordinary; it was definitely one of the most “other-wordly” places that I have ever been to. If you looked closely into the ice you could see and hear all of the tiny capillaries of melt water that were gradually draining the life from the glacier. I wondered how long it had been “alive” for?<br />
Geologists believe that Glacier Bay existed during a minimum of four glacial periods ending with the Little Ice Age, which has a 4,000 years old record, as the latest period. All glaciers in the park today are said to be remnants of this glacial period.
    ice.tif
  • Anthropomorphic iceberg, LeConte Inlet, Southeast Alaska, USA<br />
.<br />
Ice calving off from the tidewater glaciers of Southeast Alaska can assume just about any shape or form, that gradually metamorphoses as they melt. This was one of the most anthropomorphic icebergs that I ever came across washed up on the shore of the Le Conte inlet where the Le Conte Glacier is situated, the southernmost tidewater glacier in North America.
    Alaska-glaciation20.tif
  • Ice calving off from the tidewater glaciers of Southeast Alaska can assume just about any shape or form, that gradually metamorphoses as they melt. This was one of the most anthropomorphic icebergs that I ever came across washed up on the shore of the Le Conte inlet where the Le Conte Glacier is situated, the southernmost tidewater glacier in North America.
    Southeast-Alaska-glaciation20.jpg
  • Large fluted iceberg in Le Conte Inlet, Southeast Alaska, USA.<br />
<br />
I think that this was the only time that I ever saw a glacier that had melted like this, into very symmetrical fluted ridges. I haven’t found an explanation for this peculiar phenomenon.
    ice-3.tif
  • Bull moose (Alces alces andersoni), Adam’s Inlet, Glacier Bay National Park and Preserve, Southeast Alaska, USA.<br />
<br />
They originated in Asia and crossed into North America shortly before the Bering Land Bridge between Asia and America flooded about 11,000 years ago, and then dispersed throughout Beringia ( prehistoric Interior Alaska and northwest Canada). About 10,000 years ago an ice-free corridor opened up between the huge continental glaciers that covered Canada, allowing animals like moose, grizzly bears and bison to move south from Berangia to the Pacific Northwest into the continental United States.<br />
Moose subsequently evolved into four North American subspecies (and other sub-species found in Scandinavia and Russia). Alaska is home to the world’s largest, Alces alces gigas, as well as a smaller sub-species, Alces alces andersoni. Gigas, also known as Alaska moose or tundra moose, is found in Alaska, the Yukon and northwest British Columbia; andersoni, or anderson’s moose, is found in Southeast Alaska, the eastern Yukon, and central B.C east to Michigan.<br />
Impeded by mountain ranges, icefields and glaciers, moose did not colonize Southeast Alaska until the 20th century. They are far more recent arrivals than Sitka black-tailed deer and wolves, which moved up the coast from the south about 8,000 years ago as the glaciers melted and land was exposed. Moose from British Columbia accressed Southeast via the river corridors and arrived in the Taku River valley south of Juneau and the Stikine River basin near Petersburg about 1910.<br />
I had a memorable encounter with a large herd of moose in Adam’s Inlet in Glacier Bay in the middle of winter. I was standing on the mudflats at low tide and set up my tripod to photograph the moose on the shore. Gradually they started to walk towards me until eventually I was surrounded by at least 20 moose who were more curious about me than afraid; apparently their protected status in the National Park had made them not fear humans.
    wildlife-12.tif
  • They originated in Asia and crossed into North America shortly before the Bering Land Bridge between Asia and America flooded about 11,000 years ago, and then dispersed throughout Beringia ( prehistoric Interior Alaska and northwest Canada). About 10,000 years ago an ice-free corridor opened up between the huge continental glaciers that covered Canada, allowing animals like moose, grizzly bears and bison to move south from Berangia to the Pacific Northwest into the continental United States.<br />
Moose subsequently evolved into four North American subspecies (and other sub-species found in Scandinavia and Russia). Alaska is home to the world’s largest, Alces alces gigas, as well as a smaller sub-species, Alces alces andersoni. Gigas, also known as Alaska moose or tundra moose, is found in Alaska, the Yukon and northwest British Columbia; andersoni, or anderson’s moose, is found in Southeast Alaska, the eastern Yukon, and central B.C east to Michigan.<br />
Impeded by mountain ranges, icefields and glaciers, moose did not colonize Southeast Alaska until the 20th century. They are far more recent arrivals than Sitka black-tailed deer and wolves, which moved up the coast from the south about 8,000 years ago as the glaciers melted and land was exposed. Moose from British Columbia accressed Southeast via the river corridors and arrived in the Taku River valley south of Juneau and the Stikine River basin near Petersburg about 1910.<br />
I had a memorable encounter with a large herd of moose in Adam’s Inlet in Glacier Bay in the middle of winter. I was standing on the mudflats at low tide and set up my tripod to photograph the moose on the shore. Gradually they started to walk towards me until eventually I was surrounded by at least 20 moose who were more curious about me than afraid; apparently their protected status in the National Park had made them fearless of humans.
    Alaska-wildlife-moose1.jpg
  • I think that this was the only time that I ever saw a glacier that had melted like this into very symmetrical fluted ridges. I haven’t found an explanation for this peculiar phenomenon.
    Southeast-Alaska-glaciation7.jpg