We have been really
enjoying our campsite here at Canyon Campground. It’s surrounded by lodge
pines, is private and has a very nice picnic area with fire pit. We have had a
lot of campfires and even cooked s’mores a couple of nights. For the uninitiated,
s’mores are 2 graham crackers with a half of a chocolate bar and a toasted
melted marshmallow sandwiched between them.
Yum..
Camping at Canyon Campground in Yellwostone |
The weather has been staying in the high 50s during the day and low to mid 30s at night so we are still in need of our heater. Thankfully, it is working fine.
Does anyone remember
using one of these? Did you ever see one out in the middle of the woods?
Haven’t seen one in so long, but we found it out in the middle of nowhere and
the only thing you can dial on it is 911 to the Park Ranger! Guess that’s good
because our cell phones don’t work very well here.
Today, Friday the 15th,
it is still rather cool, but Tim did his early morning run again to see if he
could repeat the wildlife extravaganza he had yesterday, but it was not to be.
No wildlife at all while he sat patiently and waited in the car. Not me… I
stayed bundled up in bed until the RV warmed up to the cozy 68 we set it for in
the morning. Much better than the 55 setting during the night.
We decided to do a
driving tour today with only a few short walks along the way. We traveled from
Canyon Village to Norris and took the detour road off of the Grand Loop to view
the Virginia Cascades. We also stopped
at Ice Lake for a 1 mile walk. At the trails’ end, we were inundated with
mosquitoes and beat a quick retreat to the car.
When we arrived at
the Norris Geyser Basin, it was about 11am and it was already very crowded. This
Basin is one of the hottest hydrothermal areas in Yellowstone. The literature
tells us that it has many hot springs and fumaroles with temperatures above the
boiling point (200 degrees F). They say that it is hard to imagine a setting
more volatile than Norris as it is part of one of the world’s largest active
volcanoes. Basically, the hydrothermal areas are fueled by magma which is
partially molten rock. The magma heats the water percolating down from the
surface and when superheated rises back to the surface. Depending on the makeup
of a particular area, it will cause a geyser, a hot spring, a fumarole (steam
vent) or a mud spot. The different
colors are caused by either sulphur (yellow), iron (dark brown, rust or red),
chlorophyll (emerald green), or algae (dark, blackish-green) and when the sun
hits them just right, they are brilliant.
We walked the
boardwalks and were indeed impressed by the beauty of the Geyser Basin beneath
the Gallatin Mountain Range.
Geyser Field |
A Fumarole |
Geyser Field in front of Gallatin Mountain Range |
We journeyed down
the Grand Loop which follows the rim of the caldera (the upper edge of the
original volcano in Yellowstone) towards Madison taking in the Gibbons River,
Meadows and then the Falls. We passed through Madison Junction and took the
Firehole Drive to see the Firehole Falls and River. The sheer force of the water going through
these canyons is impressive. At one time, this was all volcano and the canyons were
formed by molten lava.
Firehole Falls |
Gibbons Meadows |
Sunday 17 June 2012, Happy Father's Day, Daddy! I hope day is wonderful - Thanks for being such a wonderful father. I love you, Kristin
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