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Travel Pictures - ALASKA & YUKON - 1994 |
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All images © Ron Miller |
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I traveled to the 49th state during August of 1994, arriving in Juneau on Alaska's mountainous southeast coast. From the capital city I boarded one of the many ferries on the "Alaska Marine Highway" to travel to Skagway through Alaska's archipelago. At this historic, gold rush town I joined two other travelers to hike the infamous Chilkoot Trail, reaching Canada on foot. I then ventured north to Dawson City in Yukon and eventually to Inuvik in the Northwest Territories. From Inuvik I returned to Alaska and visited Fairbanks, Denali National Park, Anchorage, and the spectacular Kenai Peninsula. |
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The lovely Valerie, a Canadian traveler, posing high above Alaska's capital
on the Gastineau Channel. The fjords |
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An August climb up an Alaskan snowfield to the highest point on Douglas Island - near Juneau, Alaska |
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A very festive atmosphere on board an Alaskan ferry. The "Alaska Marine
Highway System" transports passengers through the inside passage from Bellingham, Washington all the way to Skagway, Alaska. The ruggedly beautiful landscape of Alaska's archipelago makes the boat trip seem more like a sightseeing adventure - near Skagway, Alaska |
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My hiking partners (Doug and Valerie) packing supplies for the famed Chilkoot trail
(the haze is due to forest fires) - Skagway, Alaska |
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Striking out on the historic path of
the gold rush - Chilkoot Trail; near Skagway, Alaska |
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The Chilkoot Pass can be seen at
the top center of the photo. During the 1898 to 1900 gold rush, tens of
thousands of prospectors crossed the 3,550-foot pass on their way to Dawson City. A strictly enforced law required all prospectors entering Canada to bring enough food supplies to last them a year. This regulation meant that every miner had to haul almost 900 kg (a ton) of food over the border - an endeavor requiring multiple trips and close to three months - Chilkoot Trail, Alaska |
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Lakeside campsite on the Canadian side of the Chilkoot trail (again, the
haze is due to forest fires) - British Columbia, Canada |
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This innocuous-looking set of rapids meant disaster for many prospectors
traveling downriver during the gold rush. The rafts were difficult to maneuver since they were burdened with thousands of pounds of supplies to survive the harsh winters - Yukon River, southern Yukon |
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Although these old buildings have
survived the harsh elements for a hundred years since the
gold rush, they must still withstand the seasonal shifting due to the underlying permafrost - Dawson City, Yukon |
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I am outfitted appropriately to
combat mosquitoes and all other
unwanted, biting, and harassing insects - Dawson City, Yukon |
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Doug's Ford Explorer is departing the village of Arctic Red River, an "alcohol-free" town on
the remote Dempster Highway. The Dempster Highway is a 457-mile gravel road connecting Dawson City in the Yukon with Inuvik in the Northwest Territories. The road consists of a massive gravel pad ranging in thickness from 4 feet to 8 feet to prevent the road from sinking (during summer) into the underlying permafrost. The pad acts like a blanket to help keep the underlying permafrost frozen through the summer. The highway follows the route of an old dog sled trail and is named after Royal Canadian Mounted Police Inspector William Dempster who, as a young constable, frequently ran the route by dog sled - Yukon, Canada |
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Vista of the Ogilvie Mountains along the Dempster Highway with the jagged,
granite peak of Tombstone Mountain in the distance - Yukon, Canada |
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While driving the gravel road we met this group of cyclists, one of whom
just pedaled up from South America! - Dempster Highway; Yukon, Canada |
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Can you find the honey-colored grizzly bear and her cub near the center of
the picture? - Denali N.P., Alaska |
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In this stream that passes through the capital city, the salmon must
negotiate an unbelievable gauntlet of fishermen - Anchorage, Alaska |
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Vista of the massive Harding ice field where the frozen ocean "flows" into the Exit Glacier.
The ice field, including it's glaciers, covers more than 1,100 square miles which makes it the largest ice field entirely within the U.S. - Kenai Peninsula, Alaska |
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The terminus of the Exit Glacier. The deep blue color of glacial ice is due
to the fact that ice acts as a filter and absorbs first the longer
wavelengths of light (red, orange, yellow) which leaves only the shorter wavelengths (blue,
indigo, violet) and results in the blue color. On the surface of the glacier, the entire spectrum of light is reflected and the ice appears as white. However, several feet into the ice, only the shorter wavelengths penetrate and the ice appears as blue. The absence of air bubbles (the air has been squeezed out) also aids in the intensity of the blue color because more light is allowed to penetrate. Do you remember the order of the light spectrum? Here is a guide - (Roy G. Biv) - red, orange, yellow, green, blue, indigo, and violet - Kenai Peninsula, Alaska |
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Spawning salmon on the Kenai Peninsula - near Ninilchik, Alaska |
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All images © Ron Miller For authorized use of these photos, please contact Ron Miller at TheHappyCannibal@gmail.com |