Rocky
Mountain National Park
While
at Granby, CO, we were close to the west entrance of Rocky Mountain National
Park, which is the third most popular National Parks. We were to be in Granby for a few days, so we
could take our time and split up time in the Park over a couple of days. Let’s get started!
Driving
through the Park was a beautiful sight!
You’ll see more great views as we travel through this part of the Park.
At
10, 120 feet in elevation, we looked out at the Never Summer Mountains. It’s the only volcanic range in Rocky
Mountain National Park. Below it lies
the Kawuneeche Valley, which is Arapahoe for “valley of the coyote”. The Valley was shaped by glaciers and the
Colorado River. The most recent glacier receded
about 14,000 years ago.
The
next sight we saw was Poudre Lake, right at the Continental Divide (10,759 feet
in elevation). As you can see f rom the
color of the grass, autumn is beginning to arrive up high in the Rockies. This view is lovely, but on the way back, we
saw another great sight from here (be patient!).
We’re
used to wide open driving, but up here at 11,600 (and higher) wide open takes
on an entirely new meaning!! I kept
thinking each view was the best, and then along came another one!
The
Gore Range is named for Sir St. George Gore, and Irish aristocrat, who came to
this area on a hunting expedition, led by Jim Bridger in 1854, who was
described as a mountain man. This range
is now a part of Eagles Nest Wilderness Area. The 133,000 acres that make up
the wilderness area is as wild today as it was when the area was discovered in
1854.
They
call this road Trail Ridge Road, and this image shows you why!! The scene is absolutely beautiful, and I love
the little lake down the way. But do you
see the blurred area at the bottom of the image? That’s the road edge, and we are just outside
the image. We are driving right along
the rim, and should we go off the road, it’s all downhill!
These
lava cliffs aren’t the site of a former active volcano. But it’s not.
These cliffs are the result of volcanic activity from long ago…. from
the Never Summer Mountains, which are quite a distance away. Those volcanoes erupted over 20 million years
ago, and the ash that floated from there, settled, and hardened.
I
love the feeling of space that this image creates. Things are very wide open in spaces along
this drive.
As we drove along the road, I took the upper
image, and wondered what the edge of the ground overlooked. The larger image is what the answer is to
that question! It’s Forest Canyon, and
at this point, we’re at the overlook area.
The Big Thompson River flows down the Forest Canyon as it has for
thousands of years. I couldn’t see the
river for the trees!! Several times over
the past 2 million years, glaciers have formed and moved down the river. Forest Canyon formed along an ancient fault
line. On the left side of the image
above, you can see Hayden Gorge, a U-shaped glacial valley. Interesting note – Poudre Lake, shown
earlier, is made up of water flowing from The Big Thompson River!
The short trail to get to see the actual Forest Canyon
Overlook crosses the tundra (Russian for “land of no trees”). This area is above the tree line and with
winds that often exceed 100 mph (although not today!), temperatures remain
below freezing for at least 5 months out of the year. Tundra plant communities take a long time to
mature, so people are asked to stay on the trail and off the tundra. Most people complied when we were there,
although there was a couple who apparently thought their need for a photo on
the tundra eclipsed caring for this ecosystem. There were areas with lots of
rocks that form a “patterned ground” (shown above) that is only found in Alpine
and Arctic regions. During the last Ice
Age, the pattern of freezing and thawing the topsoil caused the rock pattern to
emerge.
In
1982, when the Lawn Lake Dam was 79 years old, it burst and sent 29 million
gallons of water down the Roaring River, through Horseshoe Park and into Estes
Park. Three people lost their lives and
tons of boulders, tree, gravel and sand were swept downhill until they settled
into a fan shape, and the place became known as Alluvial Fan. This area was again pummeled during the
Colorado Flood of 2013, piling on more debris, and again changing the
landscape. This is Horseshoe Falls, that
runs through the damaged area. Amazing
how two such damaging events can result in such a picturesque little waterfall.
And
so, we started down Old Fall River Road.
This road was being used by tourists in their car caravans back in 1926,
so it’s been around quite a while! It’s
now a dirt one-way road, and we liked it because, relatively speaking, it
wasn’t that crowded. The day we traveled
down it, we felt like it was a bit of Grand Central Station, but like I said,
it was “relatively” quiet!! The image on
the left is the road at the beginning of the 9-mile (or is it 11? Depends on
the road sign!) road and the image on the left is of a crease in the mountain
that looked like a dry riverbed, and is, most likely, where the winter snow
melt flows down.
I
loved the spot of autumn colors in the trees.
The area was just starting to put on the fall color show – we were about
a week or so early for the full show.
This was kind of a rehearsal!!
Since
it was such a nice day, we opened the top of Jeep and enjoyed the overhead
views – both the mountains and the trees!
We enjoy doing that because it’s such a nice way to open up the views
and our enjoyment of the drive!
I’m
including this image of a mountain simply because I really liked the color shading! I would love to make a quilt with these
colors sometime!!
I
read and was told to expect to see a LOT of animals in Rocky Mountain National
Park. Well, I guess the animals didn’t
get that memo, because the only wildlife we saw was this moose, who was very
accommodating in terms of posing for the cameras!! In case you’re wondering, the collar the
moose is wearing is a method of tracking the moose.
Enjoy!!