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An Ancient Spirit Revealed at the Cane Creek Anticline Overlook
One of the best day trips out of Moab, Utah that I know is to the Anticline Overlook at Hatch Point, south of town in San Juan County. To get there; take U.S. Highway 191 South thirty-three miles to the Needles/Anticline Overlook Road
turnoff. According to my DeLorme Utah Atlas, the Needles/Anticline
Overlook Road becomes the Anticline Overlook Road and as you approach
your destination, it becomes the Hatch Point Road. Google Maps simply
calls it the Needles Overlook Road, but if you follow their road names,
you will detour on to a misidentified portion of County Road 133.
After you pass the Needles Overlook turnoff, things change. From that
point on, the road is graveled and Google gets it right, calling it the
Hatch Point Road. Most GPS units will get you to the Anticline
Overlook without any detours.
While
conducting research for this article, we found disagreement on the
proper name for the Anticline Outlook. Since there are two Creeks in
the area with similar names (Cane Creek and Kane Creek),
many websites tend to confuse the two. The proper name for the
anticline itself is the “Cane Creek Anticline”. Ironically, when you
stand at the Cane Creek Anticline Overlook on Hatch Point, the creek
that is directly below you is Kane Creek. If you take a few steps back
from the precipice and look across the Colorado River toward the center
of the collapsed anticline, the unseen Cane Creek descends at a place called Potash. For simplicity, I shall call our destination the shorter, “Anticline Overlook”.
The Anticline Overlook is located in the BLM controlled Canyon Rims Recreation Area,
which spans most of the area between Moab and Monticello, to the
south. Located just off the road, several miles from the overlook,
there is the BLM Hatch Point Campground, with nine campsites. If you
camp there, be sure to plan well, as it is almost sixty miles and
several hours travel time to Moab. Only six miles in from U.S. Highway
191, the Wind Whistle Campground has fifteen campsites and easier RV
access.
All
of the websites I checked indicate that the graveled road to the
Anticline Overlook is well graded and properly maintained. Although
that may be true, there is a tendency to get overconfident while
speeding along that road. I use the word “speeding”, because many
visitors ignore the speed limits and rocket down the road at full
speed. On one visit, I was guilty of speeding and found my rental car
drifting on top of the gravel as if it were ice. Luckily, the car had a
warning light that came on when traction was lost.
Thinking that I could avoid mishaps so far from town, on my next visit, I
stayed much closer to the posted speed limit. What I did not count on
was oncoming traffic. Just after a small SUV passed me going the other
way, I heard a loud crack as a rock hit my windshield. Over the next
few minutes, the resulting star-shaped crack propagated like a snake
slithering across the glass. The speeding SUV driver never knew what he
or she had done.
Although
the Needles Overlook is closer to the highway and is accessible on a
paved road, I prefer taking the longer route and visiting the Anticline
Overlook. With fewer visitors willing to risk traveling fifteen miles
on a gravel road, you might find yourself alone at one of the grandest
vistas in all of the Southwest. At the same moment that you stand
alone, listening only to the breeze, thousands of people might be at
the South Rim of the Grand Canyon,
downstream in Arizona. The Grand Canyon is deeper and wider, but to
me, the view at the Anticline Overlook is every bit as awe-inspiring.
At Hatch Point, the Anticline Overlook is at 5700 feet elevation. Hurrah Pass,
directly below is at 4780 feet. Potash, along the far bank of the
Colorado River is at 4025 feet. In other words, from the overlook to
the river is about 1700 vertical feet. For perspective, the new 1
World Trade Center building in New York City will top out at 1776 feet.
Make no mistake about it; at the Anticline Outlook, you are way up
there. The good news is that you are standing on a sturdy mesa, with
desert plants and weathered rocks all around.
Unless you hang your head over the rail and look straight down, there
is little of the vertigo producing effect of standing on top of a high
building. Sturdy steel pipe-rails help add to your feeling of security.
Since the Cane Creek Anticline is like a huge bubble of stone on the
surface of the Earth, from your vantage point you can see and almost
feel the Earth’s curvature. From the overlook, there is an unobstructed
view south to the Abajo (Blue) Mountains. On a clear day, you will see
the Henry Mountains
farther south. Looking southwest across the Colorado River, you will
see Dead Horse Point State Park. Directly to the west, are the brightly
colored settling ponds at Potash. Looking upstream beyond Potash, the
backside of the Moab Rim hides your view of Moab. The Portal,
which is the natural river-cut through the Moab Rim looks like a small
notch in such a large landscape. Over the top of the Moab Rim, you will
get a glimpse of the Big Bend area along the Colorado Riverway. On the horizon to the north, you will see the Book Cliffs, beyond Crescent Junction.
After taking in the view, see if you can find the Ancient Spirit
of the Anticline. Near the farthest and highest spot at Hatch Point, he
reclines beneath a protective rock ledge. With eyes that
simultaneously look east and west, he rests there, and watches as the
Colorado River slowly washes away untold volumes of land below him. When
he first stopped to rest there, the anticline was whole, blocking the
eroded views that I just described. After waiting with great patience
for eons to pass, he appears to smile as he looks out on one of the
best views in the world.
After skirting the Moab Pile, Potash Road then flows in close proximity to the Colorado River, hugging its right bank for most of the seventeen-miles to the place called Potash. There,
at pavement's end, Intrepid Potash-Moab, LLC operates its “Cane Creek
Plant”. Although a rocky road continues on, Utah Route 279, the Potash
Road ends there.
The fact that Kane Creek
(with a “K”) enters the Colorado River upstream from the plant and on
the opposite bank made us wonder if the plant was misnamed. Further
research indicated that raw potash deposits are contained within a
geological structure known as the “Cane Creek Anticline”, which is part of the broader Paradox Basin. Thus, the plant name reflects its geological underpinnings, not a fanciful geographical location adjacent to Kane Creek.
Watch the Video, "Potash Utah, USA"
For a number of miles
between Moab and Potash, the canyon accommodates both the river and two
wide banks. Thick stands of tamarisk trees lined each bank, often
blocking our view of the river. After its excursion through a deep
road-cut and tunnel near Corona Arch, the Union Pacific Railroad’s
Potash spur line joins Potash Road for the second half of the run to
Potash. In the 1960’s the Denver & Rio Grande Railroad built the
line to service the then-new potash mine. Reflecting its support for the
mining industry, the State of Utah provided access to the mine by
constructing State Route 279. Although now used mainly for recreational
purposes, the route
is still the only paved access road to Potash. The rail line and the
highway opened in the early 1960s, just in time for the first shipments
of processed calcium carbonate, commonly known as potash.
While driving along the
riverbank, we saw rock spires, buttes and many distant views. Often
showing barely a ripple on its surface, the river here runs fifty or
sixty feet deep in its bedrock channel. In William Faulkner’s novel, “As
I Lay Dying”, Darl says, “Before us the thick dark current runs”.
Before us, the thick dark Colorado River ran like a solid mass. Looking
tame within its banks, an undercurrent produced its silent power. On the way to Potash, we had no way of knowing that the river would soon enter the dramatic Colorado River Gorge. Looking up at the escalating height of the canyon walls brought back our premonition about the Perfect Flood.
Our vision of the future included a flood so large that it spanned from
one canyon wall to the other. Its immense volume swept away everything
in its path, including any sign of man or road.
At one time, there were
plans to continue the paved highway to the top of the high mesa, near
Dead Horse Point State Park. Because of the difficult terrain along that
former cattle path, Utah abandoned the route-extension in the 1970s. In
the late 1970s, the longer and less arduous State Route 313 became the primary route from Moab to Dead Horse Point and Canyonlands National Park.
The Cane Creek Potash plant
operates on a grand scale, including sprawling settling ponds, a
processing plant and loading facilities for both rail cars and trucks.
As we approached the plant, its mid-century-modern industrial
architecture dominated the tranquil riverside setting. More than fifty
years old, the facilities still served their intended purpose. As we
traveled past the plant that afternoon, we neither saw nor heard another
human. With nothing moving at the area, Potash had the feel of a 1950’s
ghost town.
Operated as a deep mine at its inception, an August 1963 mine explosion killed eighteen miners. With its human toll placing it in the top five U.S. mining disasters
since 1940, the mine operators opted to change over to a water
injection process. The subsequent use of deep water injection required
conveying large amounts of scarce Colorado River water to the mines and
ponds, there to evaporate in the desert sunlight. With water
accomplishing all of the underground work, there are now both fewer
miners and a reduced threat to their lives. Mining engineers now pump
Colorado River water uphill to the mining sites, where they inject it
three thousand feet down and into the Cane Creek Anticline. Once inside,
the water loosens the raw calcium carbonate, creating a plastic flow,
which migrates back to the surface. Once the
minerals are at the surface, huge pipes conduct the brine to the
settling ponds below. For reasons of efficiency, gravity conducts the
minerals downward, in a series of steps that end at the processing plant
near the riverbank.
Intrepid Potash’s predecessors created the settling ponds in the late 1970s. Terraced
into anticline bench lands above the river, the settling ponds cover
hundreds of acres. Large enough to show as geographical features on our
Utah Atlas, the settling ponds created for us a striking blue and white
oasis in the desert. Because their location covers two sides of a bulge
on the Cane Creek Anticline, the ponds are visible from many locations
around the area. With the blue and white pools appearing in so many
photographs, taken from so many different angles, even some Moab locals
think that there are several different settling pond facilities in the
area.
Although we are not aware
of any declared seismic risks within the anticline, its geological
history suggests large-scale upheaval and subsidence. With that as
background, common sense tells us that the diminutive and elegant
earthworks at Potash might not survive even a moderate seismic event. In
our mind, we pictured continued injection of water into the Cane Creek
Anticline precipitating such a seismic event. If the resulting
earthquake were large enough, it could liquefy or slump the earthworks
at the settling ponds. If breached, highly concentrated brine could
cascade down-slope toward the Colorado River.
Apparently,
there is not a centralized website that covers issues regarding the
Potash entire settling pond system. Although we did find individual
pages that indicated the size and depth of some ponds, there was no way
for us to understand the overall size and scope of those operations. The
scant documentation provided by State of Utah web pages classifies
individual pools as “low risk”. Since there is no unified reporting
system regarding settling pond issues, we wondered if there have been
any recent inspections of the earthworks at Potash. If not, how can mine
operators and the state declare that individual parts of the system are
"low risk"?
With the decades-long drama taking place at the the Moab Pile, only a few miles upstream,
identification and remediation of other potential threats to the
Colorado River have taken a back seat. It would be a shame to save the
Colorado River from nuclear peril, only to witness an accident at
Potash. Collapse of the settling pond system could pollute the river
with untold amounts of potash, which is primarily used as crop
fertilizer. Although placing poor second to the danger of radiation
entering the Lower Colorado Basin, surely a large dose of industrial
strength fertilizer would not help water quality.
According to legal
documents available on the internet, Intrepid Potash uses both temporary
and permanent pipelines to conduct potash brine from their mining sites
to the settling ponds. A second set of pipes conducts the chemicals
from the ponds to the plant for processing. During our own drive past
the settling ponds, we saw evidence that raw potash slurry had recently
cascaded down a streambed and into the ponds. Although little was
growing along that streambed prior to its flooding, the heavy coating of
crystalized brine will prevent new plant growth there any time soon.
At the Moab Confluence Festival in October 2008, author and naturalist Craig Childs signed for us a copy of his classic book, "The Desert Cries".
The subtitle of Craig's book is, "A Season of Flash Floods in a Dry
Land". On the title page of our copy, Craig wrote, "Put your hand on the
ground. Feel for the flood. It is coming, always".
In December 2008, three
million gallons of toxic fly ash and water cascaded downstream from a
Tennessee Valley Authority (TVA) power plant. Once its retention pond
failed, there was no way to save the valley below. A river of toxic
chemical-sludge obliterated the local landscape, ruining it forever as a
place to live. If nothing else, the senseless destruction at the TVA
facility tells us that old, earth-dam retention ponds like the ones at
Potash require periodic, independent inspection and public disclosure of
their current risk.