Sumidero Canyon (Spanish: Cañón del Sumidero) is a deep natural canyon
located just north of the city of Chiapa de Corzo in the state of Chiapas, in
southern Mexico. The canyon's creation began around the same time as the Grand
Canyon in the U.S. state of Arizona, by a crack in the area's crust and
subsequent erosion by the Grijalva River, which still runs through it.
Sumidero Canyon has vertical walls which reach as high as 1,000 m (3,300 ft),
with the river turning up to 90 degrees during the 13 km (8 mi) length of the
narrow passage.
The canyon is surrounded by the Sumidero Canyon National Park, a federally
protected natural area of Mexico which extends for 21,789 hectares (53,840
acres) over four municipalities of the state of Chiapas. Most of the
vegetation in the park is low- to medium-height deciduous rainforest, with
small areas of mixed pine-oak forest and grassland. The canyon contains
endangered and threatened species such as the Central American river turtle
and the American crocodile, which can be seen on the riverbanks.
Map of the Sumidero Canyon route.
At the Sumidero Canyon pier there is a map with the route that the boats
take. The points of interest along the route are also marked on the map.
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The Embarcadero Cahuare Cañon del Sumidero.
Our river trip departs from the
Embarcadero Cahuare Cañon del Sumidero which is 10km (6 mi) from
the center of Tuxtla Gutiérrez, Chiapas, Mexico.
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Boarding.
This is the boat that will take us up the river.
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Crossing under the bridge.
The first event is to go under the Dr. Belisario Domínguez bridge on
road 190 that connects Tuxtla Gutiérrez to San Cristobal de las Casas.
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Advancing up the river.
Grijalva River, formerly known as Tabasco River, (Spanish:
Río Grijalva, known locally also as Río Grande de Chiapas,
Río Grande and Mezcalapa River) is a 480 km (300 mi) long
river.
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It is named after Juan de Grijalva who visited the area in 1518.
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A crocodile.
Immediately to our right we see a crocodile on the riverbank.
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Heading to the Canyon.
The river rises from Río Grande de Chiapas in southeastern Chiapas and
flows from Chiapas to the state of Tabasco through the Sumidero Canyon
into the Bay of Campeche.
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The great egret.
The great egret (Ardea alba), also known as the common egret,
large egret, or (in the Old World) great white egret or great white
heron is a large, widely distributed egret. The four subspecies are
found in Asia, Africa, the Americas, and southern Europe.
- Recently it is also spreading to more northern areas of Europe.
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Distributed across most of the tropical and warmer temperate regions
of the world, it builds tree nests in colonies close to water.
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An iguana on the tree trunk.
The iguana is a genus of herbivorous lizards that are native to tropical
areas of Mexico, Central America, South America, and the Caribbean.
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Iguanas have historically featured in the culinary traditions of
Mexico and Central America. Iguana meat is also consumed in parts of
the United States and Puerto Rico.
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Also, the eggs of iguana are consumed in some parts of Latin America,
such as Nicaragua and Colombia.
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Tourists enjoy the trip.
The scenery of the canyon has become a major tourist attraction for the
state, with developments for eco tourism and extreme sports. The
navigable part of the Grijalva River is mostly used to ferry visitors
into the canyon area.
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Most of the visitors are Mexicans. Weekends are busiest with local and
regional visitors to bike, swim, hike, camp and picnic.
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Approaching the highest part of the Canyon.
The highest part of the Canyon is a few kilometers north of the
Embarcadero.
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Another crocodile.
Another crocodile among the foliage rests on a rock on the edge of the
river.
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Arriving at the highest part of the Canyon.
The canyon proper is deep and narrow, characterized by vertical walls.
As the gap changes direction as much as 90 degrees in places, it
separates the Meseta de las Animas mesa in the west from the Meseta de
Ixtapa mesa in the east. The width of the canyon varies from 1 to 2
kilometres (3,300 to 6,600 ft). Most of the canyon's walls are between
200 and 700 metres (660 and 2,300 ft) high, reaching 1,000 metres (3,300
ft) at their highest point.
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These walls expose a long process of disturbance in the Earth's crust
with layers of limestone from the Upper Mesozoic, which contain
fossils of marine creatures.
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During the Mesocretac Period, there was an elevation of ocean floor
which formed much of the mountains of the area.
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A spider monkey.
Resting on a tree trunk (left) we can see a spider monkey.
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Geoffroy's spider monkey (Ateles geoffroyi), also known as the
black-handed spider monkey or the Central American spider monkey, is a
species of spider monkey, a type of New World monkey, from Central
America, parts of Mexico and possibly a small portion of Colombia.
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It is one of the largest New World monkeys, often weighing as much as
9 kg (20 lb). Its arms are significantly longer than its legs, and its
prehensile tail can support the entire weight of the monkey and is
used as an extra limb. Its hands have only a vestigial thumb, but
long, strong, hook-like fingers. These adaptations allow the monkey to
move by swinging by its arms beneath the tree branches.
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Geoffroy's spider monkey lives in fission–fusion societies that
contain between 20 and 42 members. Its diet consists primarily of ripe
fruit and it requires large tracts of forest to survive. As a result
of habitat loss, hunting and capture for the pet trade, it is
considered to be endangered by the International Union for
Conservation of Nature.
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The walls of the Canyon.
The walls of the canyon contain numerous small caves, rock formations
and other notable features.
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The best known of the area's caves is the Cave of Colors (Cueva de Colores). This cave gets its name from the filtration of magnesium,
potassium and other minerals which form colors on the walls,
especially shades of pink. It contains an image of the Virgin of
Guadalupe inside usually surrounded by fresh flowers and burning
candles left by visitors.
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The Cave of Silence (Cueva de Silencio) is so named because of
a lack of echo or any other kind of resonance in its interior.
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In another small cave, there is a stalactite called the Seahorse (Caballito de Mar) after its shape.
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Towards the most famous waterfall.
Once past the highest part of the canyon, we continue north towards the
most famous waterfall. In this section, the river is in the shape of an
S that prevents the view forwards or backwards.
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The interior of the canyon has thirty rapids, five waterfalls, three
beaches, two freshwater springs and a cofferdam three meters wide.
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A pelican.
A pelican rests on the branch of a tree.
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Pelicans (genus Pelecanus) are a genus of large water birds
that make up the family Pelecanidae. They are characterized by
a long beak and a large throat pouch used for catching prey and
draining water from the scooped-up contents before swallowing.
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They have predominantly pale plumage, except for the brown and
Peruvian pelicans.
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Christmas Tree waterfall.
Of the various seasonal waterfalls, the best known is the Christmas Tree
(Árbol de Navidad). The “branches” of the Árbol are made
by deposits from the waterfall which have been covered in moss.
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During the rainy season, when the waterfall is active, the water and
the light change the colors of the “branches” and make the formation
stand out.
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Returning to the starting point.
Having reached the furthest point of our river circuit, we return back
to the starting point.
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Another crocodile.
Another crocodile basking on a rock on the river bank.
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Another spider monkey.
Another spider monkey resting on a tree trunk.
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Chiapa de Corzo mural.
On the wall of the Embarcadero is this mural that represents a Parachico
dancer in front of the church in Chiapa de Corzo.
- On the far right you can see the La Pila fountain.
- On the far left you can see the Clock Tower.
- Both from Chiapa de Corzo.
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See also
Source
Location