Wrangell-St.
Elias National Park and Preserve is huge. But there is really only one road
deep into it, and we’re staying at the end of that road. The Wrangell Mountains are
volcanic in origin and Mt. Wrangell is still considered an active volcano. The
tectonic plates in the area are operating in a manner that is actually pushing
the mountain ranges higher. Many of the highest mountains in the U.S. are
located within this national park.
The park also
contains the majority of glacial ice in the State of Alaska. Two of those
glaciers are right outside our lodge. The larger of the two, Kennicott Glacier,
flows right through the town of Kennicott and down to McCarthy. Most of what
we can see from Kennicott is the terminal moraine zone. When we pulled into
town yesterday, there were vast undulating fields of gravel that looked like
tailings from a mining operation. In fact, this is part of the glacier and the
gravel is covering the ice at depths from a few inches to several feet. As you
move north up toward the mountains, the ice begins to show.
Our hike
today took us two miles from town to the Root Glacier. Once on the glacier, we
hiked another mile or so before returning to town.
Karen was
full of excitement at the start of our hike.
The
excitement began to build as we approached the toe of the glacier.
With our
crampons in place, we began our ascent toward a higher understanding of the icy
realm.
In the
distance, we could see the Staircase Icefall, which our guide told us is the
second largest icefall in the world.
We crossed
many ice rivers as we made our way up the glacier.
At our
crampon orientation, our guide told me, “grasshopper, you must trust your
crampons, for they will keep you firmly rooted.”
We lunched
next to a pristine glacial pond.
And, even
drank from its waters.
Then, it was
time to begin the return trek.
At times, the
landscape became disorienting.
But, we made
it off the glacier.
When Karen’s
knees got sore, a fellow hiker (a massage therapist/nurse from Holland)
provided some on-trail acupressure as a palliative measure. After nearly six
hours of hiking, Karen was ready to call it a day.
Once back at
the lodge, you could see way up toward the top of the Kennicott Glacier. With
the sun, came the mosquitoes. If you look closely at the photo below, you can
see where one of those pesky insects photo-bombed my shot (left side halfway
up).
Later that
afternoon, I took a two mile ‘cool-down’ walk around the mine buildings to see
what the area looked like when it wasn’t raining (as it was yesterday). After a
filet mignon dinner at the lodge, we retired for the evening.
Lupine lined the trail.
Next: Valdez
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