Continuing
the journey: Utah |
Robert
Leverett |
Apr
12, 2007 08:54 PDT |
ENTS,
This is a continuation of the account of
Monica's and my trip from
Massachusetts last summer to the Rocky Mountain west and return.
A
number of you have said that you enjoy the trip descriptions and
that
you would like to see them continued (I stopped at my
daughter’s home
in Utah). I bow to your wishes and thank you for your interest.
I thank
the rest of you for your indulgence.
START OF THE RETURN:
Monica and I left South Weber, Utah on a rainy morning, heading
southeast toward Moab. The day promised to be overcast and
showery.
South Weber is an extension of Ogden, Utah and is located on the
upslope
of the Wasatch Front. My daughter’s house sets at about 4,600
feet above
sea level. From my daughter’s front picture window, one can
look
directly up to summits that exceed 9,000 feet in altitude,
nearly a
vertical mile above her home an so close as to almost reach out
an
touch. It was and still would be an inspiring place to live were
it not
for the suffocating development that threatens to strangle the
entire
western front of the Wasatch. It is no different than any other
urban-suburban population is doing, just that magnificent views
are
being wiped out, one by one – presumably why people chose
building lots
to start with.
Of course, I am always sad to have to say goodbye to my daughter
Celeste
and her husband Dale, but the time had come for Monica and me to
begin
our return trip to Massachusetts. The first day's destination
was
Durango, CO. about 8 or 9 hours via the route we planned.
Getting on to
I15 south, Monica and I were wary of hitting morning rush-hour
traffic,
and although the worst part of the rush had subsided, a surprise
awaited
us. Shortly after getting onto I15, we were caught in a
torrential
downpour that brought traffic on a still congested interstate
first to a
crawl, then to a stop, then back to a crawl, and so on. We crept
along
paralyzingly slow as I constantly muttered under my breath about
the
abominable messes we humans create in search of security,
convenience,
and comfort. The rain came down in sheets. Hey, wasn’t this
supposed to
be desert? We later learned that the weather system we drove
through had
spawned several small tornados and we had been perilously close
to one.
Passing much to near to a tornado has happened a half dozen
times to me
on my westward journeys. I have actually been in two tornados in
my life
and don't care to be in a third. I fortunately escaped injury
both
times, but that is another story. Both events were over before I
knew
what had happened so they don’t qualify me for weathering the
kinds of
experiences that Lee Frelich relishes and actually seeks.
Passing through Salt Lake City, we continued southward toward
drier
weather and reached interstate speed. The long line of the
Wasatch range
of the Rockies loomed to the east. Following the Wasatch along
its
north-south axis is something I always look forward to on trips
to Utah.
But I mostly see the northern end of the range, so this
experience was
to provide an extra treat. When we started, visibility at South
Weber
had been okay, but just south of there, things went swiftly to
hell in a
hand basket. The rain struck while we were well north of Salt
Lake City
and the view toward the mountains became non-existent. However,
I was
able to study the contours of my windshield and learned to
appreciate
the artistic patterns of very large raindrops splashing on my
windshield. Large trucks create their own art. It is a little
like
trying to enjoy art while under extreme duress. But, south of
Salt Lake
City, we could, once again, glimpse what is called the Wasatch
Front.
Perhaps, a few words about the Wasatch Range are appropriate at
this
point.
The Wasatch is one of the many ranges of the Rocky Mountain
system that
stretches from well up into Canada to Mexico. The main uplifts
of the
Rockies supposedly occurred around 65 million years ago, but
geological
activity has occurred up until as recently as 5 million years
ago and a
few of the ranges are still growing according to the latest
research.
The Wasatch Range is one of the younger ranges of the Rockies.
Most
visitors neither know this fact nor care, I dare say. Their
interest in
the Wasatch lies along recreational lines, skiing in particular.
Skiing
is what the Wasatch Range is famous for. However, the Wasatch
Range is
not some remote destination for the rich. The Wasatch form the
scenic
backdrop for Salt Lake City and tall buildings in the Mormon
Mecca have
unparalleled views of the peaks near Alta, Utah. The same can be
said
all along the Wasatch Front.
The Wasatch Range starts near the Idaho border and continues for
160
miles southward. The origin of the name of the range is
contested. Here
is one of the more colorful origins taken from Wikipedia that I
convey
without comment.
“"The Utes told me what the word 'Wasatch' means. They
said that one
time many Indians lived there between Heber and Provo. One day
the men
were out hunting when a big blizzard came up and they lost one
of the
hunters. When they found him he was dead and his penis was
frozen stiff.
They therefore called the place Wuhu' Seai Frozen Penis. Francis
McKinley, a Ute Indian Chief, tells the same story." [2]
The range reaches its highest elevation in its southern part, in
the
peak of Mount Nebo, a 11,928-foot high complex of three peaks.
The
northern end of the Wasatch is the province of 9,000-foot
summits, but
nothing is lost in their scenic appeal because the entire
western front
of the Wasatch is a giant fault block, an upward thrust that
juts
abruptly above the surrounding desert. Going north, at some
point the
name changes from Wasatch to Bear River Mountains, which reach
elevations to 9,980 feet. Elevations at the western base of the
Wasatch,
which is bone-dry desert, are between 4,200 and 4,600 feet. From
there
it is a quick trip through 4,000 to 7,000 vertical feet of
terrain to
the rocky summits. There are few foothills in the Wasatch Front
and that
gives them the appearance of great height, yet also a closeness
that
confuses the senses about their altitudes. It is like being
close to a
smaller hill and looking up at a steep angle to the top or
farther away
from a larger hill and still looking up at the same angle. That
is the
norm for us, but in the case of the Wasatch, you look up steeply
from a
close distance to reap the dramatic effect of height and
closeness. The
Wasatch remind us of quick uplifts associated with other western
mountain ranges, notably the eastern thrust of Wyoming's
world-famous
Grand Tetons. But with the competition from the Tetons duly
noted, the
Wasatch front is an imposing site and is what residents of Salt
Lake
City, Ogden, Provo, Brigham City, and a few other towns wake up
to each
morning. The sudden change from the flat land to the west to the
precipitous Wasatch Front is more dramatic than what eastern
Colorado
residents see as they approach the higher Front Range of the
Colorado
Rockies from the eastern prairies. There are many other fine
mountain
ranges in Utah exhibiting sudden vertical uplifts. In fact, it
is hard
to find places in Utah that isn't extreme terrain either from a
topographical or climatic standpoint. But the Wasatch are extra
special
mountains and they do harbor a treasure for the athletic-minded.
Some of
the Wasatch slopes receive as much as 500 inches of snow
annually and
the powder skiing is often considered to be the best anywhere.
But we
were visiting the mountains in the middle of summer and residual
snowfields were skimpy. However, snow is actually a subordinate
feature.
It is the dizzying rock faces of the Wasatch that capture the
attention,
especially in summer, and often the stark contrasts in rock
color can
create unforgettable mountain-scapes. Of course, Utah is famous
for the
dazzling colors of its rock formations and vies with Arizona for
the
distinction of being our most colorful state.
After leaving the rain zone, and continuing southward, I found
my gaze
constantly shifting from road to mountain and back. I never tire
of
gazing at the contours of mountains. To me they are not just
large lumps
on the horizon. Each peak is an individual with a story, at
least
geologic, and deserves to be known and experienced. The overall
contours
and vegetative cover give each mountain range a uniqueness that
endears
it to mountain lovers. Approached from the west, the desert
suddenly
meets unforgiving rock and what was the complete domain of sand
becomes
ruled by impervious rock, unforgiving surfaces that challenge
the
elements millennia after millennia. To the delight of visitors
yearning
for an up close experience, the Wasatch Front is cut by many
precipitous
canyons that have the look and feel of unsurpassed ruggedness,
but
strangely accessible. One gets ruggedness in an up close and
personal
way, often leading to accidents and death. Narrow roads
penetrate many
of the canyons and trips up the canyons allows one to constantly
stare
up at the faces of 500 to 1,000-foot rock walls. The views are
simply
unforgettable.
If all this mountain babble from the creator of the ENTS List
comes as a
surprise, I should point out that I am first a mountain and
canyon
person, followed closely by forest, ocean and lakes. I am then a
prairie
and desert person. Lakes and/or rivers serve as enhancers within
mountain, canyon, forest, prairie, and desert landscapes. But
there
isn't much to emotionally separate the best of these types of
landscapes
for me, excepting for my mood at the moment. Perhaps the desert
trails
the others a bit, especially the featureless deserts. Deserts
such as
the Bighorn Basin in Wyoming are generally uninteresting to me
except as
they form the foreground for magnificent mountain ranges on
their
eastern and western borders, the Big Horns and Absorakas. But
not to
defame the desert-scape, the Sonoran Desert is another matter.
Ginat
saquaros rule and the spring blooms are breathtaking. For the
most part,
the above landscape categories overlap in their appeal to me and
when I
can combine two or more of the categories, which is usually the
case, it
is pure ecstasy. In Utah, I get lots of mountains, a little
forest, and
lots of desert. Rivers become the enhancers. The lakes are
generally
human-engineered reservoirs. They don’t count. The exception
is the
Great Salt Lake, a natural body of water, which is so
individualistic
that it is its own thing. Its 1,700-square mile surface makes it
the
largest lake in the West, but it is only 35 feet deep at its
deepest. It
is 3 to 5 times saltier than the ocean. It is a strange place
with
strange fauna and flora – well worth seeing.
As Monica and I passed through a notch in the Wasatch Range, we
began
to see more juniper as that plant became the dominant desert
vegetative
cover. The landscape assumed a more typical southwestern look
and feel.
I should point out that in contrast to the Salt Lake City
corridor, the
country south of Provo is truly wild. Population is virtually
non-existent once out of the Salt Lake City zone. One can travel
for
miles on back roads and never see another human. It is
blisteringly hot
in the summer and can turn surprisingly cold in the winter. Some
of
Utah’s mountains have recorded temperatures far below zero,
with a –69
degrees below zero F. at Peters Sink in the Bear River Range
near the
Idaho border.
As one crosses Utah from any direction, one becomes conscious of
a
rugged land crisscrossed by many small ranges of mountains
jutting
boldly up, with features known only to local residents. Once out
of an
interstate corridor, one can feel very small in the vastness of
Utah.
Geologically, most of Utah lies in what is called the Great
Basin or the
Basin and Range Province. The Wasatch Range of the Rockies on
the east
is the dividing line in northern and central Utah between the
province
of the Rockies to the east and the Great Basin to the west. More
specifically, the Basin is a geological phenomena lying between
the
Rockies and Sierra Nevada that has no outlets for the
precipitation that
falls within the confines of the Basin. The altitudes are high
throughout most of the state. Utah averages 6,100 feet above sea
level,
ranking behind Colorado and Wyoming as our highest state in
terms of
average altitude.
Although most of Utah has colorful rock formations, it is the
southern
third of Utah that is the high color zone. The five national
parks,
wholly in Utah and in the southern half the Beehive state can
even claim
a little bit of the Grand Canyon NP. Sandstone cliffs of every
hue from
deep red to blinding white greet the visitor. This is the
country of red
rock canyons and rock arches that are routinely captured by
photographers. Central and southern Utah is also the province of
isolated mountain ranges, some of historical prominence. One
southern
range stands out, the La Sal Mountains. These mountains were a
prominent
landmark on the Old Spanish Trail from Santa Fe to Los Angeles.
The La
Sals rise boldly east of Moab, Utah. The range boasts at least
12 peaks
over 12, 000 feet altitude, culminating in Mount Peale at
12,721. The La
Sals are considered to be part of the southern Rocky Mountain
province.
They appear at great distance as a dark blue line with a crest
of white.
As one approaches the La Sals, the dark green conifer cover of
the
slopes up to the timberline is striking. The timberline is
probably
around 11,500 feet or more at the latitude. The conifers give
the
mountains a somewhat gentle, friendly appearance. Yet, the range
also
stands in bold relief. It rises a full 7,500 to 8,500 feet above
the
land around Moab. This elevation change gives the La Sal
Mountains
greater relief than even the sharper slopes of the western
Wasatch. The
origin of the La Sals is tied to volcanic activity between 25
and 28
million years ago, similar to what one encounters in parts of
Colorado’s
better-known San Juan Mountains to the east.
The town
of Moab had exploded with growth since Monica last saw
it, sprawling and generating the usual zone of human ugliness so
common
when people exploit the natural beautify of the landscape with
little
thought toward what they are creating. I always have mixed
feelings when
visiting a place like Moab. Most of the people around Moab are
dirt poor
and they have as much right to a better life as anyone, but
creating
ugliness from sublime beauty of a timeless landscape is not a
virtue.
Would I like Moab more if all the architecture were pleasing and
fit
better into the landscape? Yes, of course. People who create
architectural beauty that blends with the land are to be
commended. It
doesn’t have to be expensive – better that it isn’t, but
whatever the
financial investment, it doesn’t have to be an eyesore and
that is what
much of Moab has become. Urmph1 I’ll climb down from my
preaching rock
and move on.
Leaving Moab and the red rock formations, we angled southeast
toward
the Colorado border through lonely, but deliciously scenic
country. I
felt strangely at home as we passed by smaller rock formations,
crossed
long sloping ridges, viewed distant horizons, and bypassed
unnamed
mountains. I can’t explain the feeling I got. The smaller rock
formations were captivating, - not overpowering as the great red
cliffs
had been. Their smaller cousins seemed accessible to visitation
without
fear of exposure. There were easy paths to lookouts. The appeal
of the
rocks was heightened by the blend of big sky, distant mountains,
and a
desert-scape, dotted with juniper, some appearing to be of great
age.
Crossing into Colorado, Monica and I gradually observed a change
in the
landscape. Volcanic hills and spires appeared on the horizon
with shapes
that made them ideal landmarks, but also of great spiritual
value. This
area of Colorado is rich in Spanish-Mexican history and was, at
one
time, part of Mexico. We bypassed Mesa Verde NP and the
Escalante Ruins
NM. This is Anasasi country. Much of the land we passed through
in the
Colorado portion is part of the reservation system owned by the
Ute
Indians, who were the first western tribe to acquire and master
horses.
The country has a lonely, out of the way feel, but one that
resonates
with me quite well. It is a land of long mesas and isolated
volcanic
extrusions of transfixing shapes. Farther eastward the land
gives way to
the commanding presence of Colorado’s mighty San Juan range.
We did not
stop at Mese Verde. Time was not our ally and we were anxious to
get to
Durango to visit dear friends of Monica’s, a husband-wife
combination of
retired professors from Smith College. That is an interesting
story, but
I’ll save Durango and the San Juan Mountains for the next
episode.
Bob
Robert T. Leverett
Cofounder, Eastern Native Tree Society
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