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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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  • Myanmar-Burma-Buddhism29.jpg
  • Myanmar-Burma-children21.jpg
  • Myanmar-Burma-Buddhism31.jpg
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  • Myanmar-Burma-children31.jpg
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  • Myanmar-Burma-children27.jpg
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  • Myanmar-Burma-Buddhism30.jpg
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  • I had read about this small mammal, which is actually a member of the racoon family and not a cat, and it didn’t disappoint. They have obviously become habituated to the procession of kayakers that camp on the island, and on one particular beach. One of them crept into our camp even when we were awake and cooking on a campfire, and came very close to us; I could hear the sound of it clattering around with our cooking pots.
    Kayaking- Gulf-of-California39.jpg
  • I became very familiar with this small local ferry because I usually used it to get to one of the small native communities like Kake, Angoon and Hoonah, from where I started my kayaking trips that often ended up at Tenakee Springs, where I boarded it to return back to Petersburg. It became like a trusted old friend that I enjoyed seeing cruising past my various campsites, and looked forward to being reunited with at the end of my arduous trips, and then relaxing in relative comfort on my way home to Petersburg.<br />
MV LeConte is a feeder vessel for the Alaska Marine Highway System, built in Sturgeon Bay, Wisconsin in 1973 and commissioned in 1974 by Alaska's ferry system. LeConte is the older sister ship to M/V Aurora, and both serve as feeder vessels that pick up passengers in small communities such as Hoonah and take them to larger regional communities (this process is colloquially known as the "milk run").<br />
In the case of the LeConte, it primarily serves in the northern portion of the Alaskan Panhandle in between Sitka and Juneau, but it also occasionally ventures all through Southeast Alaska as well, LeConte and the M/V Aurora are the only AMHS vessels able to serve the communities of Angoon, Pelican, Tenakee Springs, and two of the three vessels (the M/V Taku also is able to access these ports) to serve Hoonah and Kake. This quality is due because of these vessels' small sizes thus making them both vital assets for the ferry system and the residents of these rural villages.
    Alaska-Ferry97.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation17.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation12.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation18.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation15.jpg
  • The McBride tidewater Glacier, Glacier Bay national Park and Preserve, Southeast Alaska, USA.<br />
<br />
The Glacier Bay Basin is a myriad combination of tidewater glaciers, snow-capped mountain ranges, ocean coastlines, deep fjords, and freshwater rivers and lakes that provide widely varying land and seascapes, and hosts a mosaic of plant communities, and a great variety of marine and terrestrial wildlife. It has many branches, inlets, lagoons, islands, and channels that hold prospects for scientific exploration and a visual treat for the visitor.<br />
Glacier Bay, the body of water, covers an area 1.375 square miles (3,560 km2) of glaciers and accounts for 27% of the park area. It was a large single glacier of solid ice until early 18th century. It started retreating and evolved over the centuries into the largest protected water area park in the world. It was formerly known as the Grand Pacific Glacier about 4,000 feet (1200 m) thick and about 20 miles (32 km) in width, which has since then, over the last more than 200 years retreated by 65 miles (105 kms) to the head of the bay at Tarr Inlet, and in this process left separate 20 other glaciers, including this one, in its trail.<br />
Glaciers are very dynamic entities and there are seven “active” tidewater glaciers in Glacier bay, which are advancing into the sea and thus calve off large chunks of ice that fall into the sea with a thunderous noise, raising large waves.
    ice-5.tif
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation19.jpg
  • The Glacier Bay Basin is a myriad combination of tidewater glaciers, snow-capped mountain ranges, ocean coastlines, deep fjords, and freshwater rivers and lakes that provide widely varying land and seascapes, and hosts a mosaic of plant communities, and a great variety of marine and terrestrial wildlife. It has many branches, inlets, lagoons, islands, and channels that hold prospects for scientific exploration and a visual treat for the visitor.<br />
Glacier Bay, the body of water, covers an area 1.375 square miles (3,560 km2) of glaciers and accounts for 27% of the park area. It was a large single glacier of solid ice until early 18th century. It started retreating and evolved over the centuries into the largest protected water area park in the world. It was formerly known as the Grand Pacific Glacier about 4,000 feet (1200 m) thick and about 20 miles (32 km) in width, which has since then, over the last more than 200 years retreated by 65 miles (105 kms) to the head of the bay at Tarr Inlet, and in this process left separate 20 other glaciers, including this one, in its trail.<br />
Glaciers are very dynamic entities and there are seven “active” tidewater glaciers in Glacier bay, which are advancing into the sea and thus calve off large chunks of ice that fall into the sea with a thunderous noise, raising large waves.
    Southeast-Alaska-glaciation1.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation16.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation13.jpg
  • Blue icebergs develop from older, deep glaciers which have undergone tremendous pressure experienced for hundreds of years. The process releases and eliminates air that was originally caught in the ice by falling snow. Therefore, icebergs that have been formed from older glaciers have little internal air or reflective surfaces. When long wavelength light (i.e. red) from the sun hits the iceberg, it is absorbed, rather than reflected. The light transmitted or refracted through the ice returns as blue or blue-green. Older glaciers also reflect incident light preferentially at the short wavelength end of the spectrum (i.e. blue) due to Rayleigh scattering, much in the same way that makes the sky blue.
    Southeast-Alaska-glaciation14.jpg