Large-scale landslides in Salazie, La Réunion
Major landslides in Salazie
Geoscience for a sustainable Earth
Five million years ago, Réunion was born in the Indian Ocean from a submarine volcano. 100,000 years ago, the land was approximately like it is today, with the Piton des Neiges, as its highest point. When the Piton des Neiges was formed, huge landslides, linked to the action of erosion, created the three calderas of Cilaos, Mafate and Salazie. The geological formations created by the calderas underwent new landslides, some with heavy consequences. In certain spots, these are clearly visible. BRGM, the French geological survey, is a benchmark body in the use of Earth Sciences to manage surface and subsurface resources and risks. You will see that BRGM scientists have been studying these landslides for many years to assess the risks for the population. To better understand, let's join Katiana on site.
I am in the Salazie caldera, just below Hell-Bourg. We can clearly see what a landslide is. The land 150 m below was on my level several centuries ago. It slid down towards the Mât river, behind the cane fields. And it's still going on today. Further off, the land has crinkled, making the hills we see over there. The problem is that in some places there are many inhabitants.
Indeed, Katiana, the speed of the land movement depends on the sector. The Salazie caldera is one most monitored by the BRGM due to the many unstable areas identified. Grand-Îlet's inhabitants know well the effects of this massive landslide.
Hello Mr. Nourry. How are you?
What's happening here? It's scary!
Erosion made the crack, due to water underneath. The water flows underneath and goes down to the river below.
The crack has been here since 2000.
Is it still moving?
Yes. It moves every year. It goes down 5 to 6 cm a year.
Have you always known Grand-Ilet with ground movement?
Ground movement, yes.
For 27 years.
As a child too?
Mr. Nourry, we're behind your greenhouse. What happened here?
The land was sloping like this, but this hole wasn't here. There was no hole at all. It was flat.
It came with Hurricane Hyacinth?
And you're not afraid to live here? You don't fear a landslide?
When it rains too hard, I am afraid. Seeing what happened here, we're obviously afraid.
Voice, what's going on with Mr. Nourry's house and other houses here?
The phenomenon in this part of Grand-Îlet is a landslide. One of the biggest ever recorded. The entire sector is descending at various speeds, depending on the land. Look. The left-handed rampart is static as are the old lava flows at the base of the caldera. Above, the land is sliding. This layer is about 100 m thick and is moving steadily towards the river.
I'm at the foot of the landslide. Look up there, above us, there's a layer of boulders and gravel. Below, where I'm standing, due to pressure and slow rock movement, friction has turned the rock into clay. This is what scientists call the soap layer, because it helps the land to slide.
Under the landslide, the rocks and gravel gradually turn to clay. This clay also encourages landslide.
This is nothing new. In 1980, Hurricane Hyacinthe poured 3.5 m of water in 3 days into the Salazie caldera. The soil was saturated. On this road to Grand-Îlet, the ground slid towards the slopes and huts were buried.
Since the 1980 damage from Hurricane Hyacinthe, studies of the calderas' subsoil, and specifically that of Salazie, were undertaken. Since 2003, as part of the MvTerre project, the BRGM coordinates and runs most of the landslide research with financial support from Europe, the State, the region and the department. Since this date, pioneering results are regularly published.
BRGM scientists have put sensors at strategic spots, to get precise measurements and monitor the calderas' movements. In fact, Romain is at work right now.
What different sensors do you use?
This is a GPS, to record movements in real time. We've set up 10 of them at Salazie. On some houses, we've measured 10 m of movement since 2003.
These aren't the only tools you use.
No, I'll show you our other measuring techniques. This isn't an instrument, but a marker, for measurements. 150 geodetic markers are deployed on the calderas, which we measure every 6 months by GPS to calculate movement around these markers.
Why such measurements?
They help us identify areas that are moving and areas that aren't.
Studying the Grand-Îlet landslide shows that it's always moving. Different areas of Îlet move at different speeds. Speed increases from the top of the landslide to the bottom. At the front, the land moves from 30 to 55 cm a year. In the central, inhabited part, it moves from 15 to 30 cm a year. Speeds get slower towards the back of the landslide. The worst damage occurs where these different compartments meet. The landslide can't stop at the rampart facing it, because the river carries materials away. The landslide thus advances without obstacle. Below Hell-Bourg, on the other side of Salazie, the movement is even faster and some houses have moved by over 10 m in 10 years. This aerial shot shows the position of the roads and, in yellow, the houses 10 years ago. Everything has moved 10 m northwards.
Looking for drinking water?
No, we're sampling groundwater. This is from the subsoil. We want to understand how the landslide works. This device is a piezometer. This borehole, 100 m deep, monitors groundwater in the landslide. Here, the groundwater level is about 30 m down. Following it helps us understand water's role in the landslide and its underground flow.
So, water has a role in landslides? I thought it was just the slope and the soap layer.
Grand-Îlet inhabitants know very well, when it rains here, the landslide accelerates.
Can you show me how it works?
This pile of sand is the Grand-Îlet landslide, the glass is its substratum, the landslide's base. We can see that in this state, the landslide is very slow. We can't see it move.
So, this is the dry season.
Yes, it's the dry season. In the rainy season, we see that the slide accelerates. The landslide is speeding up.
It's clear that water plays a major role. We even see cracks. There are many more in the fastest zone, at the bottom.
The upper zone, where the landslide is slower, has less deformation.
The main triggers in Grand-Îlet are gravity, which stays constant, and groundwater level. The most recent studies show that groundwater-level variations affected the speed of the landslide. When the level rises, there's less friction at the base, so there's more movement. Rain accelerates movement. In the rainy season, the landslide accelerates. In the dry season, it slows down but keeps moving, because the table stays high enough, even with no rain. As the locals know, in the rainy season, new cracks appear in houses and in the roads.
Bertrand, you run MvTerre project. Why is BRGM's research interesting?
This phenomenon is globally unique in its size. The entire village, of several square kilometres, is sliding, 100 m thick, towards the gully. This means the ground is always moving.
That's hardly reassuring. Is it dangerous for people?
One of our project's goals is to reassure the population by studying the landslide. In this context, we've shown that it doesn't surge. It moves regularly, with acceleration phases but no sudden surges.
But, are there risks?
There can be. Notably mudslides. This means that today, thanks to these studies, you understand landslides very well. We understand them better, thanks to our modelling and monitoring. We've identified the role of rain and of groundwater and the connection between them and landslides.
Thank you, Bertrand.
Voice, have you understood why the BRGM's studies are important here? To understand landslides.
Yes, Katiana. They are also important because they help us find ways to slow landslides down. If a solution were needed to slow down Salazie's landslides, these studies show that we should also act to control groundwater.
The Salazie, Cilaos and Mafate cirques on La Réunion were formed by erosion in the wake of gigantic ground movements, and the land has continued to slip ever since.
The two landslips at Salazie, in inhabited terrain, were exceptional in the scale and the factors that triggered them. Downstream from Hell-Bourg, no less than 300 to 350 million m3 of soil have been shifting in the last ten years.
The disruption is considerable, especially for buildings and road infrastructure, with major consequences for the economy. There is no major risk of runaway ground movements, except very locally, but the situation has claimed a dozen victims in the last forty years.
Detecting, monitoring and modelling ground movements
Improving detection, understanding, monitoring and modelling of large-scale land movements: this was the aim of the MvTerre 2 project conducted by the BRGM in La Réunion from 2010 to 2013, in partnership with the European Union (ERDF), the DEAL, the La Réunion regional authority and the La Réunion geoscience laboratory.
This project was the follow-up to the MvTerre research project (2002-2008), which established the fundamental principles governing large-scale land movements, created geological maps of La Réunion’s three main cirques, identified past land movement events and tested satellite methods.
The MvTerre 2 project focused in particular on the Salazie cirque, installing different types of equipment to monitor land movements (10 permanent GPS points and 150 geodetic markers) simultaneously with water circulation (monitoring of 3 piezometers and 7 springs or rivers). The project also used geophysical investigation techniques and remote sensing.
350.00millions m3 for the two very large land slips at Salazie
1000.00inhabitants on the two Salazie land slips
150.00geodetic survey points across the three cirques
Understanding and modelling land movements
To develop a better understanding of these land movements and determine the risks for the population, the BRGM’s researchers worked in particular on:
- Links between geology, relief, hydrology, hydrogeology and large-scale land movements,
- modelling the behaviour of land movements.
The 3 cirques in the Piton des Neiges range (Salazie, Cilaos and Mafate) were studied, using particularly elaborate instrumentation in the Salazie cirque, which has over 1000 inhabitants and where two major land movements have occurred.
At Grand-Ilet, surface and groundwater circulation was also monitored to understand the role of hydrogeology in land movements.
Two kinds of monitoring equipment were developed:
- for land movements (10 permanent GPS sensors and a network of 150 geodetic survey points across the three cirques),
- for water circulation (quantitative and physico-chemical monitoring of 3 piezometers and 7 springs or rivers).
Other more closely targeted surveys were also made: geophysical (electrical panels), in-situ shearing tests and remote sensing of land movements.
Raising local awareness of land movement risks
Activities to raise local awareness of land movement risks were also conducted, for two main purposes:
- to ensure knowledge appropriation by people living in risk-prone areas,
- to ensure awareness of the risks raised by land movements.
These activities included:
- talks at the Salazie secondary school (Taboo and Pictionary games adapted to natural risks),
- public meetings,
- production of a film, brochures and posters, and information panels on the sites.
Developing know-how for export to other regions in the world
Although the large-scale land movements in La Réunion offer an outstanding terrain on which to develop a research programme on these geological risks,
the idea is also to develop know-how that can be “exported” to other regions across the world.
One of the main lessons from these studies was the crucial role of hydrogeology. Although erosion is a factor, groundwater movements are the driving force of these landslides.
- Notice des cartes géologiques des cirques du Piton des Neiges (Ile de La Réunion, France)
- Carte géologique des cirques du Massif du Piton des Neiges à 1/25000
- Nouvelles datations K-Ar et 14C dans le massif du Piton des Neiges
- Rapport sur l'évolution paléoclimatologique de l'ile de La Réunion et des régions environnantes
- Evolution paléoclimatologique de l'ile de La Réunion - repérage des séquences sédimentaires remarquables dans les cirques - étude de faisabilité de datations par luminescence
- Inventaire des mouvements de terrain historiques à La Réunion
- Etude du glissement de terrain de grande ampleur de Cap Sylvestre, Cirque de Cilaos
- Etude du glissement de terrain de grande ampleur de Mathurin, Cirque de Salazie
- Analyse des modes d'effondrement en masse sur plusieurs sites de La Réunion
- Implantation d'un référentiel géodésique dans les cirques -présentation du réseau
- Synthèse des résultats du suivi géodésique réalisé dans les cirques du Massif du Piton des Neiges
- Potentiel de l'interférométrie-radar en matière de détection et de suivi des mouvements de grande ampleur -étude de faisabilité à partir d'images Radarsat
- Utilisation de techniques de télédétection (interférométrie radar et corrélation d'images optiques) pour la détection de glissements de terrain sur l'ile de La Réunion
- Etude du glissement de terrain de grande ampleur de Grand Ilet, Cirque de Salazie
- Suivi des glissements de Hell-Bourg et de Grand Ilet par les stations GPS permanentes
- Etude du glissement de terrain de grande ampleur d’Hell-Bourg, Cirque de Salazie
- Auscultation des remparts de La Réunion -moyens à mettre en oeuvre
- Suivi des déformations des remparts de La Réunion - présentation des dispositifs du Maïdo et de Mahavel
- Typologie des éboulements rocheux et des modes de rupture associés -étude bibliographique applications au contexte de l'ile de La Réunion
- Analyse de la fracturation et suivi des mouvements des remparts du Maïdo et de Mahavel par dispositif extensométrique
- Etat des lieux du suivi des réseaux géodésiques dans les cirques de la Réunion. Rapport final
- Elaboration des dispositifs de suivis hydrologique, hydrogéologique et hydrochimique du plateau de Grand Ilet (Salazie)
- Suivi des réseaux géodésiques dans les cirques de La Réunion
- Diffusion des connaissances acquises sur les mouvements de terrain de grande ampleur de Salazie et suivi des réseaux d’observation MvTerre-2 – Rapport d’activité
- Investigations géophysiques du glissement de terrain de Grand-Ilet