The Piura's Weakest
After the rainy season, we find two 12-year-old surveys suggesting where prevention and rebuilding have to start.
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Nelson Peñaherrera C
Colán, Peru, amid the invasion of El Niño Current what ignited heavy rains across Peruvian Northern last Austral Summer.
Foto: © Arturo Peñaherrera.
Piura, Peru - Heavy rains fallen mainly last February and March left
desolation and critics. In one hand, thousand of liters of water and
sediment razed croplands, spoiled roads and flooded towns. In the other
hand, the people started to accuse their authorities and officials of
not surely anticipating to the event by preventive works and actions.
Rainy season that Piura Region lived was caused by an unexpected
warm-up of Pacific Ocean due to El Niño Equatorial Current entry
bringing warm water on. Southern Pacific Anticyclone simply
collapsed instead of pulling cold water frrom Humboldt Current,
stopped blowing Antarctic wind, becoming the sea more transparent,
less salty and especially hotter. This accellerated evaporation,
covered the sky with cumulus-nimbus clouds, produced heavy rains with
strong wind and electric activity.
Rains and rivers' overloads flooded the lowest places, mainly in Piura
Valley, those became to affect Piura City, the rregional capital.
There's not and explanation yet about why it was hard to forecast some
Those effects are not new and already had been warned in 2009 by
a survey from Peru's Geological, Mining and Metallurgical National
Institute (Ingemet in Spanish) , what made a large field assignment
across the regional territory explaining its geology, risk zones,
recommending prevention and mitigation actions.
Some years before, in 2005, Regional Government of Piura made a
Disaster Prevention Plan for a 5-year term, that analyzed
potential risks in the same territory based on historical antecedents,
detailing policies and activities addressed to avoid total and partial
damages to the people, the infrastructure and the economic activities.
Last May 8th, Peruvian Government launched a 3-year program called
Rebuilding with Changes, that pretends to replace the operativity of
whole Peruvian Northern. Although it was reported there are
already works projects for inmediate execution, nobody clearly reveals
where to start.
In our hand, we have combined the information by Ingemet survey,
Regional Government of Piura's plan and the FACTORTIERRA.NET coverage
to set a first place list that could give the initial priority.
More than 1,3 million inhabitants, equivalent to 70% of regional
population, could be benefit. They live in 48 of the 65 districts
Carrasquillo, Upper Piura Valley, March 23rd. This is the place
where Piura River releases of Andean Range and goes across the Peru's
widest coast strip.
Photo by Miguel Chávez, distributed by FACTORTIERRA.NET
1,- Piura Valley
It will be very diffficult to specify what part is the most vulnerable
because all seem to be. since many Andean rivers join to form Piura
River, the problems begin for approximately 949000 people living
along the valley, those around 2 for every 3 are Piura Metro Area
inhabitants, the regional capital city.
The speed powered by the Andean slope, the valley narrowness, the
amount of water after a heavy rainy season produce floods capable
to destroy cropfields, towns and bridges. Salitral's and Carrasquillo's
were rebuilt less than two decades ago, and they had to bear even being
under very fast thousands liters of water ttemporarily.
As the river releases of Andean Range, already in coastal flats,
continue to receive massive water flows, especially from creeks between
Chulucanas and Tambogrande cities, increasing it too much that
threatens Piura Metro Area, as happened on March 27th. Then, it floods
Lower Piura Valley until leading in Sechura Desert.
According to Ingemet, the most critical point is Piura-Huancabamba
Road, that is blocked by Seco and Serrán Rivers once they get
overloaded by summmer rains. In both cases, it was recommended to clean
the courses, rebuilding and maintenance of badens.
The unforested slopes can produce slides, for what house building and cropping in torrent flows were advised to avoid.
For the course in lowlands, it was recommended to build river defenses
for sslowing down the erosion, especially when passing amid Piura and
Going down the flow, it was warned the maintenance and reinforcement of
containment dams and river defenses to avoid flooding croplands in
Catacaos and Cura Mori Districts, Sechura City inclusive, where the
river leads once it filled Ramón Grande and Ñapique Lakes in Sechura
The good news for lowlands is the river has not changetd its course since 19th century ending, but nothing is still said.
Mórrope, Peru, about 100 miles to the south of Piura City.
Pan-American Highway was very damaged by the combined action of many
rivers, almost dry, those lead in Sechura Desert to create La Niña Lake.
Photo provided by Kevin Saucedo.
2.- Paita and Talara Coastal Plateaus
Speaking in geological terms, what Piura knows as 'shore cord' was sea
floor several millenia ago. In mid-Cenozoic, that floor started to
elevate progressively creating a kind of an almost flat table emerging.
Today is a big part of Piura's Northern Coast surface, only interrupted
by the Paleozoic's Coast Range (formed by Amotape Mounts, Silla de
Paita and Illescas Mount).
The flat is known as 'tablazo' in spanish or 'coastal plateau' and it's
still elevating, what produces a rare landscape - a half-a-mile strip
almost sea level that suddenly jumps up about 65 to 100 feet. It begins
in Máncora at the north, ends in Gobernador Point at the middle of
Piura's shore. Itps only interrupted by dozen creeks leading in the
sea, Chira River Delta and Sechura Desert.
Talara, Paita cities and their beaches circuits have been settled just
between waves line and the elevation beginning, especially Cabo Blanco
and Colán. In consequence every time it rains extraordinarily, creeks
activate and cracks created in the plateaus slopes also form little
streams leading into the sea. Although coastal plateau's soil is
basically sediment compounded with runded little stones, it's necessary
more wather than usual for the material slices down not considering the
Paita and Talara historic downtowns are located precissely in those
zones at sea level, and despite some creeks are canalized, theyalready
were destroyed by the water and the mud - during the last 34 years,
those low zones have been damaged by those agents precissely.
In Talara Province, many paths and roads connecting the beaches go
through the base of the plateaus, exposing them before the same type of
damage. Ingemet has recommended containing nets and walls in some
segments of slopes and badens with wide shewers in streams courses,
those have to be checked out constantly to avoid their blocking by
sediment and trash.
If whoever living on the plateau flat tops thinks to be save, could be
mistaken. Because the torrents and slides creeks begin on the
high part, facilities and uptowns in weak compactation terrains could
sucumb as happened toa seafood processing plant in Paita and Sudamérica
Neighborhood in Talara.
The recommendation is monitoring constantly and relocation in mid
term, especially in those places where erosion and the plateau
elevation process have destroyed waste water pipelines, which
flow are contributing to carve the slope.
Another critical sssegment is former Amotape-Negritos Road that runs in
paralell to drinking water pipeline to Talara Province what could break
and cut the flow off. Also the crude oil pipelines pumped up from
the underground in El Alto, Restín and Los Órganos could be
About 259000 people live from Máncora to Gobernador Point.
Lower Chira Valley seen where it begins near Marcavelica, in
front of Sullana City, Peru. An upcoming storm is also visible on this
shot taken last March 31st.
Photo by Corey Godley, distributed by FACTORTIERRA.NET
3.- Lower Chira Valley
Although Chira River load is the double than Piura River, its neighbor,
its erosive process is not acuted so much despite it has got to dig a
big long ditch in the coastal plateau on its medium and lower course.
Controlled since 1976 in Poechos Dam, an average summer for Chira River
ever means a 1500 to 2000 cubic meters per second load, according to
Chira-Piura Special Project official record this year. However
beginning April 1998, it became 7000 cubic meters per second, 75% more
than Piura River maximum historical load.
Because of gravity, the valley's most vulnerable zone is is its lower
course between Sullana and Paita Provinces borderline and its lead into
the Pacific Ocean. About 41000 people live straight there.
According to Ingemet, the Lower Chira Valley is prone to floods because
it's very flat. Overloads can also block the traffic between the two
banks as happened in 1998 when destroyed Simón Rodríguez Bridge, close
to a plant that pumps drinking water for Paita and Talara cities.
For the moment, rims have to be reinforced to avoid the erosion, and
people have to be alert every time there is an official evacuation
announcement. At least, the plateau is so close to get save.
Huancabamba Valley erosive problems could be
accelerated after the fires in 2016-ending razed a big part of cloudy
Photo by El regional de Piura / file.
4.- Huancabamba Valley
One of the most beautiful landscapes of Piura Andes, produced by
vulcanism, glaciation and a rare geological anomaly that unallowed it
to elevate more than 12870 feet altitude (known as Huancabamba
Deflection), is also a mortal trap if caution is not taken.
Officially sourced in Shimbe Lake, perhaps the most famous in Huarinjas
Complex at 10560 feet altitude, Huancabamba River falls down free many
times until forming a very narrow valley, V-shaped, from 8250 feet
altitude in El Carmen de la Frontera District to 6600 feet altitude in
Sóndor District , then becoming Piura/Cajamarca borderline until
turn east in Porculla Pass (7260 feet altitude, in Huarmaca
District) creating a deep canyon where the entire Andean Range's major
depression is located.
About 52000 people live only in its medium course, if we add the whole
valley inside Piura Region territory it raises 91000 people.
Having a very steep surface, slides are common due to constant rains
over the summits known as jalcas [pronounce "halkas"] or Piurano moors, caused by the
violent shock of humidity from the Pacific and the Amazon Jungle. Even
when the terrain is basically clay, it is not any warrant if
deforestated for roads, paths, croplands and many towns like Sapalache,
Huancabamba, Sóndor or Sondorillo.
As a collateral effect already in the western side of the range,
mudslides caused by rains can affect Canchaque and San Miguel De El
Faique both located in Pacific slope. Crossing the range to the north
there is another place in Pacaipampa District where the torrent slided
down as much as a mile, Ingemet said. Coming back to Canchaque and next to Pusmalca
River, La Afiladera (The Edger in english) is famous for being the
detour to that town or San Miguel, and for its vertical clay-&-rock
vertical wall that has already blocked Piura-Huancabamba Road
Returning to Huancabamba Valley, if slides are not enough, enormous
carves across the terrain can collapse the slopes. Many are caused by
geological faults -the zone has a quake timeline- appearing one
after one along the river course. The most notable runs down along
Huáscar Street in Huancabamba City (6500 feet altitude), , opening wide
toward the river as a stream. The slipping has destroyed the
pavement and it's belief it continues umperceptible day after day.
The only to do is containing the slopes where creeks have to be crossed
and also disencouraging human settlements and agriculture on cracked
zones. In La Afiladera case, a containing net was recommended to set
Another threat for Huancabamba City, La Perla Neighborhood, its
lowest place to be exact, is the river itself. fed by a dozen of
creeks, it can raise its level and flood as it was happened previous
years ago. For the moment, river dams and walls are the best
defense means against the water, but if the people give up to
live in that zone, it would be better. Some were relocated where the
landing lane was projected (the neighborhood is called el Aterrizaje,
The Landing in Spanish), but it begun another debate: where
the relief is going to land in emergency case.
Sullana City's Canal Vía, last March 8th night. Its creators believe it's time to remake it.
Photo by María Chero, distributed by FACTORTIERRA.NET
More Critical Spots
According to Ingemet and Piura Regional Government papers, other places
where reabling and rebuilding are necessary: Sullana-Lancones Road
due to mudslides and creek raising, Las Lomas-sapillica Road because of
mudslides, Sullana-Ayabaca Road, and Ayabaca-espíndola Roadd especially
where the detour to Aypate Archeological Site starts.
Although it doesn't appear on the papers, Tambogrande-Chulucanas
Road is ever broken by the creeks leading into Piura River.
Nevertheless, phosphate extraction in sechura Desert is under threat every time it becomes La Niña Lake.
Piura's second largest metro area, Sullana, has the
adjacent blocks to Canal Vía as a main risk zone, that drives down Cieneguillo and Cola del
Alacrán Creeks to Chira River creating a cascade. After more than 30
years working, a project is being proposed to reinforce, even remake,
segments of the course now protected by cement slabs.
National and regional governments are not agree yet about the grand
total caused by Coastal El Niño event across Peruvian Northern, but
Macroconsult consulting firm calcullated it US$ 3,12 billion ending
March, almost meaning 6% of gross domestic product. Peru's
President Pedro Pablo Kuczynski says tere is enough money for facing it
- many people is skeptical about.
Will be possitive changes after the rebuilding for real?
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