The Long Half of the Train Ride
We found a nice ¼ mile path through
the woods which led to the canyon rim and the Barrancos Rim Hotel. The lobby
and bar of the hotel actually is built out over the canyon rim. We bought a
coke and marveled at the scenery as we quenched our thirst. What an awesome
sight. It was gorgeous. Wow, it was a long
way down to the bottom! The canyon is mountainous with deep gorges and lots
of vegetation.
I told my friend, “I am a bit
disappointed, as my perception was that you could see the canyon all the way on
the train and you can’t.”
“Actually until now we’ve seen very
little of the canyon. But this is
beautiful! There’s no way a camera can capture this. I’m going to use my panoramic,
but I still don’t think it will do the canyon justice.”
We headed for a path leading down
into the canyon. Our destination was some Tarahumara Indian caves. It was a
fairly easy hike, but we were about 7335-feet above sea level and the air was a
little thin. The Tarahumara are known to be great runners.
Geologically speaking the Barrancas
are young. They started to take shape 90 million years ago. Between 40-80 million years ago major
mountain ranges were forming along the entire west coast of North and South
America because of plate tectonics. Millions of years of erosion shaped the
volcanic plateaus into spectacular canyons. Finally the granites that had not
seen the light of day for 90 million years began to reach the surface.
For the past
5 million years the Sea of Cortez has been widening with each shift of the land.
Earthquakes rock the southwest coast of North America along the San Andreas
Fault System quite frequently. The Barrancas continue to deepen as the volcanic
tuff that makes the canyons walls slowly erode to the sea.
The Barrancas are amazing natural
geological wonders of Mexico. They are the result of volcanic eruptions
thousands of times greater than the 1980 eruption of Mt. St. Helens in the
United States. The rocks are igneous unlike the sedimentary rocks of the Grand
Canyon. And they are younger, a mere 25 million years compared to the several
hundred million year old rocks of the Grand Canyon. The Barrancas are actually seven
canyons with the deepest being nearly 1000 meters deeper than the deepest part
of the Grand Canyon. Each is an awesome work of nature!
Before dinner we indulged in drinking
margaritas and enjoying the quiet and beautiful scenery of this place in the
middle of nowhere. The few trucks moving around left a lot of dust behind them,
as the area is very dry.
The train was not due until 1:30 PM
the next day. After breakfast we again
walked over to the rim to watch some pretty basic Indian dancing and some of
their games. Later we took a short, dusty bus ride/tour seeing another hotel, a
school, a church, and a spectacular overlook. Then we continued on to
Diversardo where an observation deck offered a spectacular view of Arroyo Ojo
de la Barranca where it is 4135’ down to the Rio Urique. The narrow
ridge/plateau in this part of the canyon does not lend itself to much
development. There is a small airstrip on top of the mesa. The scenery was gorgeous in this untamed
and rural area.
There was a lot of confusion when
boarding the train for the last half of the trip to Chihuahua, but I had the
paid tickets in my pocket so we boarded and figured we straighten out any
problems after the train was on its way. This conductor spoke a lot less
English but there were no problems.
We descended through pine forest. At El Lazo (knot) Bridge the
train crosses over its own track to form a complete loop. The loop is necessary
to start losing altitude. Los Ojitos at 8071’ is the highest point above sea
level.
Creel ,founded in 1907and at 7735’, is the heart of the Tarahumara homeland and
gateway to Sierra Tarahumara.
Once again the loud speaker came on
and we made out, “The steepest grade of track is from Bocoyna to Sanchez. It is
a 2.5% grade. Bocoyna, at 7585’, was founded in 1702 by missionaries. The name means pine
forest in Tarahumara. The twin tower church in town is well known. East of
the train the mesas rise from 8250-8910’.”
We also learned San Juancito at 8000’
was established in 1906 with the coming of the railroad. We could see a large
sawmill. It is a main lumber center and is one of the coldest parts of the
state of Chihuahua.
Terrero was a village of white
plaster adobe buildings. It is a ranching and horse breeding area. Slowly the
pine trees gave way to cottonwoods, then juniper and oaks. Again the loud
speaker informed us, “Franciscan missionaries established Santa Isabela in
1668.”
And the final message was, “Palomas
is a village with rock quarries. The tuff-like rock is called cantera. Many of
the buildings in Chihuahua are made of this stone. From here on to Chihuahua is
agricultural land as it is a very fertile valley. Mennonites from Canada have
cultivated the area for over 40 years. You will see many apple and peach
trees.”
It was a rather long uninteresting
ride and when we finally reached Chihuahua at 9:30PM we both were ready to
disembark.