|  | 
|  Dave, Chuck, Doris, and Yang at the Humphreys Peak Trailhead.
 |  
| 
At 8:15 AM on a cool, breezy Saturday morning with temperatures in the mid-
fifties, four Motorola Hiking Club members and guests – David Langford,
Chuck Parsons, Yang Wang, and his friend Doris Du from Allied Signal – met
at the Mt. Humphreys trailhead in the Kachina Peaks Wilderness Area to begin our
assault on Mt. Humphreys, at 12,633 feet the highest point in all of Arizona.
 
To even the most casual observer traveling this somewhat tortured landscape
north of the Flagstaff area, it must be readily apparent that something quite
dramatic, something on a very grand scale, must have occurred here in the far-
distant past.
This land for hundreds of square miles north and west of the present-day
Flagstaff area, encompassing most of the Coconino Plateau, was a seething
cauldron of volcanic activity that lasted from approximately 15 million years
ago to about 200,000 years ago, when the last great eruption occurred.
 
That mighty eruption, rivaling or even surpassing the Mt. St. Helens eruption of
1980, blasted away the upper 1,300 feet of what is now Mt. Humphreys (making its
original height almost 14,000 feet) in a cataclysmic explosion that rocked the
surrounding area for hundreds of square miles and blasted millions of tons of
hot ash and lava high into the atmosphere.
 |  
|  View looking west towards the vast San Francisco Volcanic Field.
 |  
| 
What we now call the San Francisco Peaks actually date back approximately 2.8
million years in time.
 
Exactly what happened next is still the subject of some debate among
today’s volcanologist and geologist.
Some of the experts go with the Mt. St. Helens theory – a violent sideward
explosion tore open an immense cavity on Humphrey’s northeast flank,
collapsing the peak, and creating the present-day Inner Basin.
A succession of glaciers then gradually ground down and smoothed out this great
basin, depositing a series of moraines across the open side of the basin as they
retreated.
This sculpturing by fire and ice created the awesome landscape we see before us
today.
 
Other experts support a second theory – that the central part of the
volcano erupted and then collapsed into its partially emptied magma chamber,
again creating today’s Inner Basin.
The end product, regardless of which theory is correct, is the present-day
stratovolcano known as Mt. Humphreys, composed of alternating layers of lava
flows and volcanic ash, accumulated over several million years of intermittent
eruptions.
(Just some food for thought here – the last known eruption in this area
occurred less than a thousand years ago, resulting in what we now call Sunset
Crater, northeast of Flagstaff.) One wonders – is it all really over?
 
Sorry for the digression, but I felt it was critical for a better understanding
and appreciation of what this area is all about.
Now back to the trail.
The Mt. Humphreys Trail, starting at 9,300 feet and ending 4.5 miles later at
the summit (the longest 4.5 miles on Earth), is deceptively easy at first,
carrying us for about a quarter mile over a relatively flat meadow into the edge
of the forest.
This now-colorful meadow was filled with alpine Iris swaying in the steady
breeze and a sparse covering of lush green ground cover.
The breeze was but a precursor of what would await us higher up on the trail.
This same meadow, wearing a thick cover of snow in the wintertime, serves in its
dual capacity as one of the Snowbowl’s lower ski slopes.
 
Entering a thick old-growth forest of aspen, Douglas and white fir, Englemann
spruce, and ponderosa pine, the trail now begins a gradual but steady climb up
the sloping side of Mt. Humphreys in a series of long switchbacks, so long in
fact that one is almost unaware they are even switchbacks at all in the
beginning.
It would be almost three very long miles before we would emerge from this forest
primeval.
 
At about 10,000 feet we encountered a massive rock slide, approximately 100 feet
wide and running for hundreds of feet down the mountainside – millions of
tons of rock literally forming a rock river, frozen in time.
This definitely would not have been a good place to be anywhere near, when that
earth-shaking event occurred, wiping out everything in its path as it smashed
its way downward to the bottom of the mountain.
Quite an impressive sight that would be repeated numerous times along this
awesome trail.
 |  
|  Two hikers view the scenery from the basalt rock slide area.
 |  
| 
It wasn’t too long before we saw our first patch of snow at about the
10,500-foot level, one of the few remaining remnants of last season’s
meager snowfall that survived only because of its deep-shade location.
In another week of two even these will vanish from the scene, as warmer
temperatures creep up the mountainside.
 
Climbing ever higher, at about the 11,000 foot level we begin to notice the
trees gradually thinning in numbers and shrinking in height, becoming more bent
and twisted in appearance due to the punishing effects of the relentless winds
howling up this mountainside.
From just a little above 11,000 feet to the tree line at 11,400 feet, one of the
few trees that can survive this harsh and unforgiving environment is the Bristlecone
pine, the oldest living thing on Earth.
Living Bristlecone pines in the Sierra Nevada range of California have been
dated at 4,000 years old, mere saplings at the time the pyramids were being
erected.
 
The trail is now becoming more and more rocky, traversing several more
rockslides along the way (actually several of the switchbacks meet the same long
rockslide we encountered earlier).
We have now seen the first of several huge avalanche tracks streaking their way
down the mountainside, evidence of the force of millions of tons of snow and
rubble roaring down the mountain’s slopes, bulldozing down everything in
their path and leaving a cleared out swath of total destruction in their wake.
 
This unbelievable and sometimes awful power of nature is evident almost
everywhere along this long, winding trail to the summit.
 
Beyond 11,400 feet the familiar tree line, or what’s left of it, slowly
begins to disappear altogether, and the only tundra found in Arizona gradually
starts to emerge in its place.
 
However, the hardy little Bristlecone pine still hangs on tenaciously in ever-
dwindling numbers and only very reluctantly will relinquish its final foothold
on these mountain slopes, finally giving way completely to the tundra somewhere
above the saddle at 11,800 feet.
The tundra, with its small and twisted ground-hugging shrubs and numerous tiny
wildflowers, including the rare San Francisco Groundsel, will soon become almost
the only thing that can survive in this now extremely harsh and punishing
environment.
It is really amazing the number of colorful wildflowers that seem to be thriving
in this area.
Due to the very fragile nature of this environment, all camping is prohibited
beyond this point, according to a posted trail sign marking the 11,400-foot
level.
 
Rounding a bend in the trail we see Mt. Agassiz looming ahead in the distance,
its upper peak piercing the clear blue sky at 12,400 feet, second only to that
of our destination – the still unseen Mt. Humphreys.
We are becoming acutely aware that the trail seems to be getting a bit steeper
at this point and the footing a bit more treacherous as well, with a lot of
loose rock now covering much of the path.
The switchbacks are also getting shorter and tighter, as the trail slowly winds
and claws its way up the slope toward the long, rocky ridgeline that connects
Mt. Humphreys with Mt. Agassiz.
 
Finally, after struggling through several more ever-steeper and tighter
switchbacks, we emerge – at 11,800 feet – onto the ridgeline,
commonly known as the saddle, where we catch our first glimpse of the majestic
Mt. Humphreys, still looming in the distance another 870 feet higher and a
little over a mile away.
Sloping away directly in front of us is the breathtaking Inner Basin, an immense
green and rocky valley forged from a cauldron of fire and ice 200,000 years ago
and surrounded by the towering San Francisco Peaks.
 |  
|  Remnants of last winter’s snowfall still remain in the Inner Basin.
 |  
| 
To the west of the saddle, stretching endlessly toward the horizon, is the vast
Coconino Plateau and the San Francisco Volcanic Field, a smoldering and churning
hot-bed of volcanic activity dating back fifteen million years, that was the
primary force in shaping this landscape we see spread out before us today.
 
After struggling through too many switchbacks to count over a course of almost
3.5 miles and an elevation gain of 2,500 feet, in air growing thinner with each
foot of elevation gain, you now feel drained, wasted, almost totally exhausted.
Virtually every muscle, every tendon, and every fiber in the lower half of your
body – not to mention your entire respiratory system – is begging,
pleading, imploring you to do the sensible thing and turn back now, while you
still have the remaining strength in your body to make the return trip back to
the trailhead.
It’s a long walk back through that forest primeval, even from here.
 
A good number of sensible people do exactly that, including one of our own
party, Doris Du.
She had not complained (at least to me) of any soreness or extreme fatigue to
this point, but simply (and sensibly) decided she had gone far enough and would
wait at the saddle for the rest of us to return from the summit.
Hot Rod Dave Langford, meanwhile, had long since pulled ahead of the rest of our
small group and was no doubt enjoying the view from the summit by now, wondering
what in the world happened to Yang, Doris, and myself.
Most of the die-hards, including Yang and myself, are drawn on inexorably by the
mysterious and powerful force of the mountain, challenging us to test our limits
even further – pushing us to the very edge of our bodies’ physical
endurance envelope.
 
With a grim new determination to reach our goal, we press onward into the ever-
increasing winds, now growing steadily stronger with every 100-foot gain in
altitude.
We had already experienced 25-30 MPH winds back at the saddle, where we left
Doris.
The mountain’s call to the summit is virtually irreversible at this point,
and lightning and thunder would be the only thing to turn us back now.
That was actually beginning to look more and more like a distinct possibility,
as billowing gray clouds sweeping in from the west were starting to increase in
numbers.
The thought of turning back now so close to our goal drove us on at an even
quicker pace, despite the altitude.
Extremely violent electrical storms can strike these peaks at almost any time,
and over the years a small number of unlucky hikers have been struck and killed
by lightning at or near the summit, with no cover whatsoever for protection.
It is highly advisable to turn back immediately at the first sound of thunder
and beat a quick retreat to lower ground.
 
Not too far above the saddle, Yang and I met Gloria Jiang from the hiking club.
She had started out with a friend about a half-hour behind us back at the
trailhead and was now on her way back down from the summit.
We were evidently talking to a seasoned mountain hiker here.
 
The remainder of the trail from here to the summit consists largely of rock
rubble, much of it loose volcanic talus, treacherous footing for the
unwary.
At this point we are essentially hiking on a gigantic cinder pile.
As we slowly wind our way up the ridge, carefully picking our way through the
loose rubble, the winds sweeping in from the west grow steadily stronger, making
it more difficult than ever to keep forging ahead.
 |  
|  Above Agassiz Saddle, hikers continue to push towards the summit.
 |  
| 
About a quarter mile in the distance we see what has to be Mt. Humphreys, a long
procession of hikers carefully picking their way up its steep southern exposure.
 |  
|  Now above 12,000 feet, the air is very thin and
 the risk of altitude sickness becomes very real.
 |  
| 
We soon join this procession and slowly pick our way to the top – only to
find we have been duped, like many an unwary hiker, by a false summit!
The mountain is seeking its revenge on us, mocking us to the very end, for the
true summit lies yet another quarter-mile and another 150 feet higher in the
distance.
 
At this point you must control yourself and suppress an urge to sit down and
cry, for true mountain men (and mountain women) obviously do not cry.
 
Gathering what remaining strength we can muster for this final assault of the
true summit, we navigate out onto the last ridge approach, where we encounter
ferocious and unrelenting 50-60 MPH winds roaring up the mountain’s
western flank and slamming into us broadside.
 |  
|  On the final approach to the summit.
 |  
| 
This horrendous wind is now so powerful it is quite a challenge to even maintain
an upright position, and most of us find ourselves desperately trying to
counter-balance and lean heavily into the wind to prevent getting body-slammed
into the rocks, or worse, being blown over the edge into the rock-filled Inner
Basin far below.
Not a good way to end the day at all.
 
At some point Yang had forged ahead of me, and as I was nearing the end of the
last ridge approach, Dave and I crossed paths as he was returning from the
summit.
Dave has been to the mountaintop! He whispered something about a fantastic view
and the terrible winds, and even being cold and tired (can’t imagine why),
as I casually nodded in agreement, wondering why in the world he was whispering
in this deafening wind.
The truth is he was actually screaming at the top of his lungs, but these
roaring winds literally tore the words right out of his mouth and flung them out
into space.
Soon I met Yang, also returning from the summit.
We too exchanged a few brief blown-away words, and I then pressed on alone,
determined now more than ever to reach the top of this mountain, despite being
bone-weary and walking on legs of rubber.
 
Pushing ahead into this unmerciful and unrelenting wind, I made the final
assault up the last steep slope to the top alone – only to find about
twenty-five other hikers already there, huddled together in the rock shelter and
hunkered down, trying to ride out these relentless summit winds.
 |  
|  Hikers resting on the summit of Mt. Humphreys.
 |  
|  The view from the top.
 |  
| 
After I finally catch my breath and start to take in the spectacular 360-degree
panoramic view of hundreds of square miles stretched out below us, it finally
starts to sink in.
We are actually standing on top of Arizona, the highest land point in the entire
state.
 
We are now 2.4 miles above sea level, or precisely 12,633 feet above San Diego
Bay.
 
Between the altitude, the elevation change, sore, aching muscles, and this
horrendous wind, it has been quite a struggle to make it to this, our final
destination.
Was it all worth it? On the way up, we certainly all had our doubts, growing
stronger as the journey wore on.
Considering that this experience – in this place and this time – and
this unparalleled view are to be found nowhere else on this Earth, I believe
that we can all safely say, yes, it was all more than worth it.
With that, we will close out yet another unique chapter on another unique
experience in this very unique and special place called Arizona.
 |  |