I
had identified Grapevine Gulch Trail as being a relatively short
hike, 2.7 miles one way, trail that could easily be hiked by the
Skyliners as a 5.4-mile round trip hike. The trail is located in
Grapevine Gulch on the Prescott Valley side of Mingus Mountain and
the best way to reach the trail from Cottonwood would be to drive
south across Mingus Mountain on Hwy 89A and then follow Powerline
road, a dirt road, along the foot of the mountain to Grapevine Well
which marks the trailhead.
It
was a sunny day when Lila Wright, Karl Sink and the author set out
early in the morning of 18 February 2015 to explore the trail.
Although there were only the three of us and we could have ridden in
one vehicle we chose to take two because the dirt road we would
follow was unfamiliar to us. The two vehicles were a 4-wheel drive
pickup and a rear-wheel drive pickup. This would enable us to
determine whether 4-wheel drive was necessary and also provide a
measure of safety in the event of a breakdown in a remote area.
From
the Cottonwood Safeway parking lot it was 21.3 miles across the
mountain to the turnoff onto Forest Road 643 (Powerline Road). The
first 0.9 miles of FR 643, to the junction with FR 151, was heavily
traveled and maintained in excellent condition. However, from that
point on, the going became pretty rough in places as the road wound
its way over and around hills and across deep washes while generally
following the power line. I was happy to be driving a 4-wheeler. On
the other hand, Karl managed to follow all the way with his
rear-wheel drive vehicle. In the final analysis, a 4-wheel drive
vehicle is highly desirable and a high-clearance vehicle is a
necessity.
After
another 4.8 miles, 6.1 miles from Hwy 89A and a short distance after
FR 643 turned sharply east, we came to an intersection with FR 9002V.
Forest Road 643 turned right and continued south at this point, but
we continued straight ahead on FR 9002V until it turned left and
headed north. This is the Grapevine Gulch Trailhead, but we drove
straight ahead for another 0.1 mile to park at Grapevine Well.
The
map (right) shows the route (see
dark yellow track) we took along Powerline Road (FR 643) and FR 9002V
to Grapevine gulch Trailhead.
The
map insert (left) details the area
from the FR 643/9002V junction to the trailhead and also shows
Grapevine Well.
As
noted, we actually drove another 0.1 mile past what we took to be the
official Grapevine Gulch Trailhead. There, just short of the well,
we came to a gated fence (below)
and parked outside the gate to start our hike.
On
the other side of the fence the trail follows an old road, see the
faint track just to the left of the sign, that leads up the slope and
follows along the hillside before returning to the bottom of the
gulch. After crossing the fence, we paused for a few minutes to look
around at Grapevine Well and its associated windmill and water tank.
Lila and Karl at Grapevine Well
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The
roughest and steepest part of the trail was the short section of old
road that climbed up the hillside, but it was a short stretch of the
trail. When we reached the high point on the hill, just before
dipping back to the bottom of the gulch, we could see large rock
outcroppings near the streambed below; this was undoubtedly the
reason that the road builders had chosen the hillside in that area.
On the other hand, a cow trail did follow along the bottom of the
gulch and we could have followed that instead of the old roadbed.
In any case we were soon
enough back in the bottom of the gulch, following the remains of the
old road as it wound its way back and forth across the streambed. At
the time of our hike the streambed was bone dry for most of the way,
so we had no problem crossing it. A section of the streambed, about
0.9 miles from the trailhead, with the old road shown running along
its left bank is shown below.
Grapevine Gulch dry streambed with trail (old road) shown at left
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About 1.4 miles from the
trailhead we came to the remains of an old mine. The only reference
I could find to a mine at this location identified it as a “Cobalt
shaft; Cobalt prospect; Walker prospect [?])1”
The
source also indicates that it is a narrow (knife edge to 14 inches
wide), 15-foot vein deposit of partly oxidized, altered gabbro
(intrusive igneous rocks) containing relics of sulfide, possibly
cobaltiferous arsenopyrite.
Although
all we saw was the tailings pile alongside the streambed, the source
said the workings included “a
28 foot long opencut leading to an 18 foot long adit (horizontal
or nearly horizontal entrance to a mine).
A 20 foot winze (minor
connection between two levels in an underground mine) was
sunk at the portal2”.
Cement
Spring is located near the old prospect mine. I had seen the name on
the map and wondered how it got its name. One look at the spring
(right) answered that question.
Someone, probably the miners, had dug the spring out and reinforced
the walls with rocks cemented together. It was now more a shallow
well than a spring. Although no water entered the streambed at this
point, there was water in the spring.
From
Cement Spring, the Forest Service map indicated that the trail
continued for another 1.2 miles and ended at Trap Spring. When we
arrived there, we did find a mere trickle of water in the streambed
as shown in the below photograph. Contrary to the map, the trail
continued on past the spring and, as it appeared to be well used and
easy to hike, we decided to continue on up the gulch.
A trickle of water in the stream; trail continuing up the gulch (right)
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About
0.2 miles above Trap Spring a trail branched off to the right,
leading up a side wash to the northeast. We continued along the
trail in Grapevine Gulch, heading directly north, for another 0.5
miles before deciding to turn back. The trail was still clear and
easy to hike, sloping gently as it made its way up the gulch, and we
wondered who had extended it. I later determined that the extension
was the work of mountain bikers. The extension crosses the ridge
ahead, follows Ash Creek for a distance and then returns to Grapevine
Gulch Trail by way of the fork we had noted just above Trap Spring.
We
stopped along the way for a leisurely lunch but still found ourselves
approaching the end of our hike early in the afternoon. The below
photograph, looking across Prescott Valley from the mouth of the
gulch, was taken near the end of the hike. The Grapevine Well
Windmill is located just beyond the rock formation shown right of
center. Although the road looks good here, it is very rough ahead.
Looking across Prescott Valley; top of windmill visible above the rock formation
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After finishing the
hike, we decided that we would continue south on Powerline Road to
Hwy 169 for the return home. That idea didn't work because the road
is closed at a locked gate a short distance ahead. Finding ourselves
stymied in that plan, we decided that we would instead go west from
Powerline Road, following a road that we were sure would take us to
Fain Road. We would then follow Fain Road north to Hwy 89A.
Unfortunately, we soon came to another locked gate. This closure was
emphasized with a dead coyote hung on either side of the gate. We
weren't sure but
thought that might be a message for trespassers.
One of the coyotes is shown here (left).
We
gave up on all alternatives and returned home the way we had come.
After
uploading my GPS track, I measured the round trip hike as being 6.4
miles. The maximum elevation was 6132 feet and the total ascent was
891 feet.
Our
track is shown in red on the included map (next
page). The purple track is the bike trail that loops
across the ridge, down Ash Creek and then back across to rejoin
Grapevine Gulch Trail above Trap Spring.
1
Cobalt
shaft; Cobalt prospect; Walker prospect [?])
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