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Hitchman's More Great Photo Locations in North America CATHEDRAL GORGE
The
canyon walls surrounding this gorge are soft, bentonite clay that settled
to the bottom of an ancient lake bed about a million years ago. This
sediment formed a layer that was about 1400 feet thick. Surrounding
mountain ranges have since risen and faulted causing the lake to drain
down Rainbow Canyon to the south and into the Colorado River. Weather
patterns have changed greatly in the past million years. Today the
southwest has much less rain than it once did. Infrequent cloudbursts send
flash floods scouring down Meadow Valley Wash eroding the soft silt and
clay of Cathedral Gorge into a wonderland of columns and spires. Today,
all the silt washed down Cathedral Gorge flows into Lake Mead. The gorge was used as a garbage dump by local ranchers back in the 1860s. It began to be appreciated by newcomers who were reminded of European cathedrals and named it Cathedral Gorge in the 1890s. Ladders were built to allow visitors to climb through the maze of spires. During the 1920s, the area was used as a picnic grounds and as a backdrop for Shakespearean plays. The gorge became a state park in 1935.
There
is a new Visitor Center just off Highway 93 where you can stop for a free
trail map and ask any questions you might have about the park. You can
watch a short audio-visual presentation with information about Cathedral
Gorge. This is also a good place to get information about the other photo
possibilities in eastern Nevada. Check out the nearby Beaver Dam State
Park, the Ward Charcoal Ovens, and the Pahranagat National Wildlife
Refuge. For more information, call the Visitor Center at (775) 728-4460. The
road into the gorge is paved most of the way to the trailheads. You
won’t need a 4x4 here. Soon after passing the only fork in the road (a
left turn takes you into the campgrounds), you will begin to see patterns
of eroded canyon walls on the right side of the road. You can easily fill
most of a day in this park and never walk more than a few hundred feet
from your car. There
is a $3 free for day use, which you can pay using envelopes provided in
the parking areas at a few of the trailheads.
Stop and park where the pavement ends. Signs mark the location of several
“caves” along the right side of the road at that point. These are very
narrow “slot” canyons that lead back into the face of the cliffs. Some
are covered with slabs of stone and layers of sandstone creating natural
bridges and giving the impression of caves. Several of these caves extend
more than a hundred feet into the canyon walls with branching side
canyons. About
a mile farther north, at the end of the unpaved stretch of road, there is
a covered picnic area, several barbecue pits, and some restrooms. There
are also some impressive, free-standing formations (photo below) on the
edge of this parking area. At the north end of this parking area, the
“Juniper Draw Trail,” a four-mile loop, begins. Mostly level, this
trail makes a large loop around the perimeter of the gorge, along the base
of the formations. This trail can be muddy after a rain. You may not feel
like walking all the way around the loop, but you shouldn’t miss the
first formation of spires, about a half-mile up the gorge. A
short distance north of the parking lot, there’s a fork in the trail
where a half-mile side trail to the right leads up to the top of Miller
Point. More about that overlook in a moment. Bear left at the fork in the
trail and, in a few hundred feet, you’ll reach one of the more
impressive formations along the trail (photo on page 6). There are several
levels with many more spires rising behind this formation. They are
accessible via an unofficial trail leading up to some even better
viewpoints. To prevent more erosion, visitors are asked to stay on the
official trails. On
my recent trip back to Cathedral Gorge, the sky was filled with dramatic
cloud formations. A late spring snowstorm had passed through eastern
Nevada the week before and more rain was forecast for the next day. Great
clouds raced across the sky. I used a red filter for most of the exposures
I made on black-and-white film. I made vertical and horizontal
compositions each time I set up my tripod. A warming/polarizer was ideal
for exposing color film in Cathedral Gorge. It darkened the blue sky,
emphasizing the clouds and warming up the mostly gray canyon walls. In
the late afternoon, strong winds began to blow dust up the canyon. I
wrapped a plastic bag around the camera attached to the tripod over my
shoulder. At the far northern end of the gorge, the trail loops around the
base of the formations and heads south again, along the western side of
the gorge. I especially appreciated the lack of information signs along
the trail naming all the formations. Those things always get in a
photographer’s way. The trail circles around the far side of a large,
free-standing formation in the center of the gorge and finally reaches the
edge of the campground. Carry plenty of film, there are good compositions
all the way around the trail and the light will probably keep changing as
clouds drift over. From the campground at the end of the trail, it’s
only a short walk over to your car in the parking lot near the picnic
area. The
soft, sandy soil in the gorge is constantly eroding away and supports no
cactus and only a few wildflowers and some native plants. There are some
shade trees around the campgrounds where there are 22 campsites with
restrooms and hot showers operating from April through November. The
weather in this part of the Southwest can be brutal with heavy winter
snows and sub-zero temperatures–too cold for cactus. Summer days often
reach well over 100˚F. with thundershowers being common in August and
September. Don’t
miss the side road out to Millers Point, located about two miles north of
the main entrance to Cathedral Gorge on Highway 93. Park and walk out to
the viewpoint for a great view of two side canyons. At the end of the
overlook, you can follow the trail down into the gorge. There are several
wooden ladders and stairways on the way down. This trail leads about a
half mile south where it joins the loop trail near the parking area inside
the gorge. There
are very few services available in the nearby town of Panaca. The highway
passes by the old section of town. The town of Pioche, about ten miles
north of Cathedral Gorge, is a fascinating relic of a hillside mining
town. I have enjoyed many hours photographing its old buildings and
rusting remains. You’ll find a few restaurants and lodgings in Pioche.
But my favorite motel is located about fifteen miles south of Cathedral
Gorge in the railroad town of Caliente, Nevada. The Shady Motel is located
across the tracks from the old (restored) railroad station right in the
middle of Caliente. The Shady Motel is clean and quiet (until a freight
train passes through town in the middle of the night). Call (775) 726-3106
for a reservation and ask for one of their new rooms. I’ve tried several
restaurants in Caliente, Panaca, and Pioche, but can’t recommend any.
Please let me know if you find a good restaurant in this part of Nevada. If you are planning a photo exploration of the best remote locations in the Nevada desert, read my Photograph America Newsletter #58 - “Nevada Back Roads.” If you plan to visit Nevada’s Great Basin National Park, read my Photograph America Newsletter #48 - “Great Basin National Park.” More reasons to subscribe to the most detailed bimonthly photo/travel available. For more information check out: http://www.apogeephoto.com/800get_foto.html Previous Great Locations: Up
the Hudson River
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