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Nine fine Trailblazers at Willow Lake. [photo by John]
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Back row, let to right: Joe, Susan, Eric, Doreen
Front row, left to right: John, Carl, Lin, Mimi, Dottie.
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At 7:00 AM under bright blue Arizona skies and a glaring sun, seven hikers from
the Arizona Trailblazers Hiking Club set out on the hour and a half drive north to
Prescott, a quaint small city of some 40,000 inhabitants.
In its past history, Prescott was twice designated as the state capital before the
latter was finally relocated to Phoenix.
Once we reached the trailhead at about 9:00 AM we were greeted by two additional
Trailblazers who welcomed our arrival with a surprising quick “champions”
breakfast on the run: a box of Krispy Cream donuts.
They were delicious and pumped up our carbohydrates for the 4.5 miles hike around
the lake.
By 9:15 we were on our way following the Red Trail that will “hug” and
circumvent Willow Lake, a man-made lake built in 1935.
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Willow lake and its trails.
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Aerial picture of Willow Lake and Watson Lake.
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A sign welcomes us.
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The lake was created by damming a narrow canyon in the rock formation that
surrounds it.
It is used as a reservoir but also as a recreational lake where you can fish,
canoe, kayak or sail. Though the current water level was low, the lake was still very
fine for all these activities.
You will see in several of the pictures the, once upon a time when we used to have
more rainfall, the high water markings, in other words, “bathtub rings”
on the rocks, some 15 to 20 feet above current water level.
The lake water surface area covers 400 acres.
The rock formation called “Granite Dells” around the lake is unusual.
One might as well feel being on some other planet.
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Water Makings. [photo by Joe]
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Dell Rock shapes. [photo by Joe]
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Dell Rocks. [photo by Lin]
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Willow Lake. [photo by Lin]
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Did I pique your interest about its formation? Here is what the geologists said:
The Granite Dells is a geological feature north of Prescott, Arizona.
The Dells consist of exposed bedrock and large boulders of granite that have eroded
into an unusual lumpy, rippled appearance. Geologically speaking: the
“Precambrian Dells” granite has been dated at 1.4 billion years old.
Its plutonic rock was intruded at a depth of around one or two miles.
These cover rocks have since been eroded away. Weathering along joints produced
the rounded boulders and other unusual rock formations that characterize the
Granite Dells. This process is called “spheroidal weathering”, and is
common in granitic terrains.
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More rock formations. [photos by John]
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Our hiking in Prescott’s “Granite Dells” was like getting lost in
a Stone Age labyrinth. The network of paths on the north shore of Willow Lake coiled
through hulking quartz-studded granite buttes squeezing in and out on the paths in
heaving accordion style. The rugged meandering loop trails moved seamlessly from
claustrophobically tight spaces to airy exposed promontories with unobstructed vista.
On these rocks the trail followed spray-painted white dots that serve as directional
beacons.
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| Photos by John: |

Trailblazers on the march.
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Starting trail.
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Trailblazers on the march.
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Odd looking boulders.
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A tight spot.
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Follow the leader.
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Are we lost already?
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This way.
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Don’t push those boulders!
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Oh, here is the next dot.
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Just follow those dots, folks.
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| Photos by Carl: |

Here we are.
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Onward marching Trailblazers.
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Eric leads.
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Climbing the slippery rock trail.
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Now Dottie leads the climb.
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Susan leads going down a narrow ledge.
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Lin leads us down the same ledge.
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A forlorn tree stands watch as more clouds roll in. [photos by Lin]
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From different points along the trail, we could see the low level and the high level
markings of the water line etched into the rocks.
Do you remember your children bath “tub rings” at home after they
had been playing in the mud?
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Bathtub rings. [photo by John]
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There were many photos opportunities and we did not skimp on clicking our
cameras’ shutters.
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Water puddles. [photos by Carl]
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Water everywhere. [photo by Carl]
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Let’s go ahead. [photo by Lin]
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Where there is water, there is life. [photo by John]
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Lin’s signature pose. [photo by John]
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Joe approaches the dam. [photo by John]
At its narrowest point in the Dell rock formation, a dam was built in a canyon thus
creating this manmade lake. We stood right beneath the dam and admired it.
The dam was built in 1935, which makes it now an 81 year old structure.
We felt safe standing below this 100 foot or taller wall, until Joe, one of our
hikers quipped hypothetically: “What would happen to us if the dam suddenly
burst open?”
Well, Joe, the flood of water gushing out at a high speed would
have carried us miles down the canyon. I can’t swim, Joe! With this morbid
thought we continued on our hike with the objective of reaching the end of the Dells
rock formation that bounds the northern shores of the lake.
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The dam, from lake water level. [photo by Lin]
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Panorama of the dam and the lake. [photo by Lin]
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Standing at the bottom of the canyon, we faced a 100 steps climb to reach the Dells
rocks above the lake water surface.
Once we reached the top, we continued our trek until we found a shady spot and
decided to stop and eat our snacks. “Rufus” a dog belonging to another
hiker who happened to pass by our rest stop, decided to take a plunge in the lake.
Certainly, the water was cold and not very clean.
“Rufus” didn’t seem to mind.
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1000 stairs: what goes up must come down. [photos by John]
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One step at a time. [photo by John]
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Let’s take a break. [photo by John]
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Two-tone rocks by the water. [photo by John]
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Onward and upward. [photo by John]
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Yes, I can get up there. [photo by John]
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Made it. [photo by John]
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Rufus. [photo by John]
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Lunch break. [photo by John]
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After our snack break, and contrary to past hikes around Willow Lake, this time
instead of completing the circumference trail around the lake, where the last two
miles run on a nondescript trail shared by dogs, joggers and bicyclers, and literally
is a stone throw away from the highway, we decided to come back via the Dells Red
rocks trail.
This allowed us to get a double whammy of rock hopping, negotiating narrow ridges
and slippery rock surfaces.
This made our return hike much more enjoyable and much more interesting and
exciting rock hopping experience.
We followed the “white dots” going out and coming back.
We gladly report that no one fell, slipped or twisted an ankle.
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We’re on top of the world. [photo by John]
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Climbing the golden staircase. [photo by John]
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Curious lines mark the granite boulders. [photo by John]
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Back to the trailhead. Trailblazers follow the white dotted lines. [photo by John]
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It’s this way, folks. [photo by John]
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We have another hill to climb. [photo by John]
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At the suggestion of Susan we took an inland trail, for part of our return hike, just
to change the scenery.
At one point, in a clearance along the trail, we came across a house.
We wondered who might be living there!
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Return hike through thickets. [photos by John]
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Woodsy trail. [photo by John]
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Squeezing between the rocks. [photo by John]
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Desert varnish. [photo by John]
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Trailblazers on the rocks. [photo by John]
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| Starting Time: | 9:15 | AM |
Finishing Time: | 1:00 | PM |
| Stopped Time: | 0:30 | hrs:min
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Duration: | 3:45 | hrs:min |
| Avg. Speed Overall: |
1.43 | mph |
Starting Elevation: |
5,151 | ft |
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