Click on any image for a larger view
Molas Pass |
Ouray
Waking to a cool clear morning, we head back into Durango for
gas for the next part of our journey. We
stop at a farmer’s market for ‘Palisades’ peaches. We happened across these a few years ago and
are hooked. We also find plums, crenshaw melons, and coffee; we are set to go.
The ride to Silverton turns into an adventure, first heavy rain, then
sleet, enough to accumulate on the road.
The weather changes between rain and clear for the next 30 minutes
before finally clearing, giving us dry pavement. The road winds up and over mountain passes,
dropping into valleys. Passing Silverton,
the mountains take on hues of gold, copper and cream.
Red Mountain |
Yankee Girl Mine |
Approach to Ouray |
Part of the Cascade Falls |
Waiting for winter |
Ouray Pool/Hot Springs |
Beginning of our Jeep trip |
View of Yankee Boy Basin |
James tells us late spring is a great time to come, with the
mountainside awash in spring wildflowers.
Each year spring appears at a different time in the mountains, it
depends on when the previous winter’s snowpack disappears, letting people in,
this year, it was July. The roads back
in this area are repurposed mining roads.
We can’t imagine trekking back here, to mine in the 1800’s; using mules
to haul wagons, working at these elevations, somewhere over 12,000’, above the
tree line, in the middle of winter. People
were tougher back then; I can’t see me doing that. At each of our destinations we are surrounded
by different mountains; Mount Sneffels,
Teapot, and Cirque, are the only ones I can remember.
View from Silver Basin |
Silver Basin |
Tarn in Silver Basin |
Our return is slow, the ride up was
a fun E-ticket Disney ride, the ride down is a more adventurous. I always get this bad feeling when the hood
of the truck blocks the view of the road, especially when we are going
downhill, on uneven, twisty mountain ‘roads’.
James handles it without flinching, his eyes glued to the break in the
trees knowing that the road is below.
I’m so glad I am not driving. On
our return we make several quick stops for photo ops, before arriving back in
town. We say our goodbyes to James,
promising ourselves we have to come back to see this area at the peak of
wildflower season.
Black Canyon of the Gunnison
After lunch we head off to Black Canyon of the Gunnison National Park. But first, we make a stop at Mouse’s Chocolates & Coffee for hot chocolate. Nicida has a lavender hot chocolate, I have a Mexican hot chocolate. Mine is spicy, the spiciest hot chocolate I’ve ever had. It takes several sips before I decide like it and would order it again. Our drive to Black Canyon is only 50 miles. Once we leave Ouray the land transforms into an open plain with ranching and farming replacing the high reaching mountains. At Montrose, we turn east, a few miles further we make the turn into the park, climbing almost 2,000’ above the open mesa.
Gunnison River in the Black Canyon |
Schist, Gneiss and Pegmatite layers |
We see the bedrock of the earth, metamorphic rock, from the
Precambrian Era, approximately 1.8 billion years old. Schist and gneiss, two forms of metamorphic
rock, were formed by pressure on volcanic rock. 1.4 – 1.7 billion
years ago magma squeezed into cracks in the schist and gneiss, minerals grew
from the magma as it cooled, forming pegmatite, igneous rock. This is the lighter colored stripes in the darker schist and gneiss. The Gunnison Uplift pushed this metamorphic/igneous
rock up, which was then buried by more volcanic activity. Then, what we now call the Gunnison River,
started flowing, cutting a path through the volcanic rock and into the
metamorphic rock forming the Canyon. All
this activity occurred over the past tens of millions of years. I skipped probably 99% of the details of how
this all occurred, I’ll leave that for you to dig into.
At each, we see small snippets of the river, but we always hear the rushing river. The pegmatite looks like abstract brush strokes of white colored paint on the darker schist and gneiss. The stokes appear different from each overlook. We are anywhere from 1,800’ to 2,000’ feet above the river. Geologists estimate the river erodes the rock at an average of 1” every 100 years. Tomorrow, the north rim.
The next day we start our trip home. Before leaving the park, we detour to the
East Portal, upstream from the canyon.
We descend 2,000’ feet to see the river at eye level. It is calm and quiet, with a strong, fast
current. A tunnel was dug upstream from
here to provide water to the farms on the mesa outside of the canyon. It took 4 years, from 1905 to 1909, to dig the
11’ x 12’ x 6-mile-long tunnel. We
follow the five-mile-long road mules used pulling wagons from the top to the
bottom of the canyon. We are informed
that the Interstate system builds the roads to a grade of not more than
6%. This road has a maximum grade of
16%.Gunnison River
Return
Exiting the park, we drive along the Gunnison Valley. The river itself is far from the road, until
we come to the Blue Mesa Reservoir, the largest lake within Colorado, stretching
for miles. Passing the reservoir, outside
the town of Gunnison we see a smaller, upstream, version of the Gunnison River. We stop for lunch enjoying the warm weather
and sunshine. Stopping in the visitor
center, we find another volunteer, this time she is excited to tell us the
wonders of the Gunnison area. Inquiring
further we find out that this area receives an average of 180” of snow annually. Up on the mountain, the average is 300”,
great for long season playing in the snow; XC-skiing, snow shoeing, and fat
tire biking. Leaving town, we find the
last farmer set on the side of the highway selling Palisades peaches, stopping
we stock up on the delicious fruit. The
land east of town becomes arid. As the
road starts up the foothills to Monarch Pass, trees reappear. There is anywhere from 20 – 40% tree loss due
to the dry conditions this area has been experiencing over the past
decade and bark beetle infestation. We crest Monarch Pass at 11,311’,
the tree line, starting the long downward drive to Salida, CO. Past Salida, we drive parallel to the Arkansas River,
used by many for float trips and fly fishing.
We find a campground on the river enjoying listening to the gurgling
water flow behind the camper. It’s a
very comfortable 70° and sunny as we have dinner.Fall color
Waking to a nice cool day we have breakfast before starting
our three-day drive back home. Following
the Arkansas river, we notice all of the rafting companies are closed, the water
in the river seems low, we see rocks protruding above the water level in many
spots, making rafting or kayaking more of a challenge. We turn west again, climbing up to 8,000’
seeing a string of 13,000’ and 14,000’ mountains, many of them with a light
coating of fresh snow. Once we join I-25
we are on the same road we took up to CO.
Some of the wildflowers seem to have come back to life, with the rain
that passed through the area while we were on our trip. We decide to stop in Dalhart, TX for the
night. Descending to 4,000’ we are back
hotter weather – 90°. Our drive the next day
seems to drag. We make it to Snyder, TX,
staying in a hotel for the night. We are
at a lower elevation, and a higher temperature - 95°. Our final day on the road passes uneventful, the
temperatures have cooled from 100°+ when we left, to 90’s today, with the same
90’s forecast for the next several days.Impending storm
After emptying the camper, doing laundry, and going out for dinner,
I spot my next project… Cleaning the mass
of insects from the front of the truck and camper.
It was a good trip.
Thank you for stopping by.
Mark
Very beautiful photos, Mark!
ReplyDeleteColorado is a special place to see. We missed peak fall color by a week or two, but it was still beautiful.
ReplyDelete