The Village Where The Land Became ‘Swiss Cheese’
It happened suddenly and without warning. Where there should have been the emerging first shoots of potato seedlings behind the orchard in Nikola Borojevic’s spacious garden, there was now huge hole. Measuring 30m (98ft) wide and 15m (49ft) deep, it quickly filled with water. And it wasn’t the only one.
Within the space of a few weeks, dozens of similar holes had opened up around the village of Mecencani and neighbouring Borojovici in north-east Croatia. The one outside Borojevic’s home in Mecencani appeared on 5 January, just six days after a 6.4 magnitude earthquake struck the area around the nearby city of Petrinja. It was the strongest earthquake to have hit Croatia for more than four decades, killing seven people and destroying thousands of homes.
While landslides and sinkholes are known to be triggered by earthquakes, along with other strange geological phenomena such as liquefactions – where the solid ground begins to behave like a liquid – the sheer number of holes appearing around the two villages surprised and baffled experts. A month after the earthquake, there were almost 100 sinkholes spread over a 10 sq km (3.8 sq miles) area, with new ones opening every week.
The hole in Borojevic’s garden is now the largest in the area. When it first appeared it was 10m (33ft) wide, but started to grow almost immediately.
“My wife was in the house the whole morning, looking occasionally through the window,” says Borojevic. “Around 2pm she noticed something strange in the garden. We went outside and there was this huge hole in our orchard.” Over the following three months, the hole tripled in size.
But the Borojevics were lucky. Other sinkholes in the area opened up just a few metres from the doorsteps of people’s homes and one appeared beneath a house, prompting officials to consider evacuating both villages. Others appeared in the surrounding woods and agricultural fields, where one of them, according to some local rumours, almost swallowed the local farmer and his tractor.
The unusually large number of sinkholes in one spot has drawn the attention of local and foreign geologists, keen to understand how the earthquake may have triggered the ground collapses.
“Nobody expected the appearance of so many sinkholes,” says seismologist Josip Stipcevic from the Department of geophysics at the Faculty of Science in Zagreb.
Croatia sits on a highly seismically active area, where the small Adriatic plate is colliding with the Eurasian tectonic plate, causing a number of active faults, explains Stipcevic. Before the earthquake on 29 December 2020, the country had experienced nine others with a magnitude over 6 since the beginning of the 20th Century. The last major earthquake to have occurred on the Pokupsko-Petrinja fault – along which the most recent one occurred – was in 1909.
The 1909 earthquake occurred only 23km north west from the epicentre of the one that shook at the end of 2020. That too attracted the attention of leading seismologists at the time. The famous Croatian geophysicist Andrija Mohorovicic studied seismographs from the 1909 Pokupsko earthquake and concluded that seismic waves travel with different speeds as they pass through different layers of the Earth. His insight led to the discovery of a boundary that separates Earth’s crust from its mantle, known today as the Mohorovicic discontinuity, or simply the Moho.
Today, researchers are studying the same area in the hope of understanding how the earthquake led to so many holes suddenly appearing.
Sinkholes are not the most common consequence of powerful seismic shocks but they do occur, especially in the areas with hidden underground cavities. After the devastating earthquake near the Italian city L’Aquila in 2009, two sinkholes immediately opened on roads in the old part of the city. Experts at the time suspected that a previous excavation of vertical trenches for a sewage conduit weakened the conglomerate roof of the underground cave, contributing to the collapse.
“The real anomaly in Croatia’s case is a very high number of sinkholes with significant dimension,” says Italian geologist Antonio Santo at University of Naples Federico II.
The deep and wide holes endangering the two Croatian villages are known as cover-collapse sinkholes. They usually appear in areas where the underground rock has been hollowed out to form cavities and caves by water and is covered with a thick layer of soil, sand or alluvium, and most importantly, clay.
Over time, the water slowly washes surface material from its deeper layers into the cavernous underground. If there was only sandy soil, this process could be eventually spotted on the surface. But the presence of clay makes this surface material more sturdy and consistent, so after a while, a void is formed in the soil from below, but is almost undetectable above ground. As the surface layer became structurally weaker, it eventually collapsed into the void below.
Usually this process happens over a long period of time, but can be accelerated by intensive rainfall, flooding or even human activity like mining or aggressive groundwater pumping.
After analysing data collected from the area around Mecencani and Borojovici, Croatian geologists concluded that the strange events resulted from a complex combination of several different factors.
First, although the coastal part of Croatia belongs to the world-famous Dinaric karst, home to thousands of deep limestone caves and hundreds endemic cave-species, underground limestone formations also stretch inland beneath central Croatia. The limestone that forms cavernous rock in this boundary area between the Dinaric karst and Pannonian basin was deposited in the Miocene period when this area was underwater and connected to what is now the Mediterranean sea.
“While Dinaric karst is mostly from the Cretaceous and Jurassic period, the karst that we find here is younger and even more porous and hollow,” says Josip Terzic, a hydrogeologist from the Croatian Geological Survey. “It is limited to a few small zones around here and close to the city of Zagreb.”
When the Pannonian basin became disconnected from the Mediterranean due to the shifting landmasses some 11 million years ago, it became a massive lake. Rivers slowly filled it with silt, sand and gravel to form the present-day vast lowlands. Consequently, around 10-15m of soil, stones and clay lay on top of the porous rock beneath the villages of Mecencani and Borojevici.
The danger, though, was hard to detect. Some sporadic sinkholes appeared before, but according to locals, very rarely.
“It is obvious that earthquakes accelerated some already on-going processes,” says Terzic. In fact, the first discovered sinkhole started to open after a magnitude 5 foreshock struck the area the day before the larger one. As the stronger earthquake and the accompanying aftershocks shook the area, it caused the ground to shift by more than 30cm (12 inches). This displacement destabilised the precarious situation.
“The earthquakes caused massive dynamic stress to these lands and locations that were already in borderline balance suddenly collapsed,” says Terzic.
His colleague, Bruno Tomljenovic, a geophysicist at Zagreb University believes that the earthquakes disrupted the movement of water underground, sending it shooting upwards towards the surface, and moving from areas of high pressure to lower pressure. This increased hydrodynamics in underground passages accelerated collapsing of surface material, explains Tomljenovic.
“Also, there is a chance that a few collapsed sinkholes caused additional changes in hydrodynamics, with water searching for new passages and possibly causing more sinkholes,” says Tomljenovic. An unusually large number of shocks also may have contributed to so many collapses at the same time, says geologist George Veni, director of The National Cave and Karst Research Institute in New Mexico, an area also know for sinkhole problems, often caused by activities connected to industrial wells. Human influence also increases the rate at which cover-collapse sinkholes form, warns Veni.
One recent report from scientists at the University of Zagreb warns that irrigation systems built in the Mecencani and Borojevici area probably accelerated the karstification process.
For the time being scientists don’t have enough data to analyse the connection between the strength and number of earthquakes with the appearance of sinkholes.
“The situation in Croatia can be considered as warning of what can happen in countries with earthquakes and areas that are prone to cover-collapse sinkholes,” says Veni.
But predicting where sinkholes like this may open up is far from easy, says geologist Mario Parise an experts on hazards in karst environments at the University Aldo Moro in Bari, Italy.
“We can so far just rely on the historical data and documents to know areas that are most susceptible to this type of processes,” he says. Although some sinkhole hazard models have been proposed in the last decade, “developing a warning system for sinkholes is a field where much work needs to be done”, he adds.
For Tomljenovic, one of the lessons from the Croatian sinkholes is the need for more intensive seismic microzonation in order to detect areas within the populated areas that are especially vulnerable to dangerous earthquake consequences. He and his colleagues are attempting to do this using electrical resistivity tomography and seismic refraction surveying in the Mecencani and Borojevici area, in the hope of identifying locations that are safe from sinkholes and those that are still prone to them.
But the danger of new sinkholes appearing over the coming year is still on many residents’ minds. Changes to the water table through the year, combined with further aftershocks as the fault settles, could lead to more collapses, according to Stipcevic.
In the meantime, the massive hole filled with water still stands in Borojevic’s garden and has even become a local tourist attraction. Six months after the earthquake, efforts to fill in the sinkholes should begin soon.
“It’s also a tricky business,” says geotechnician Davor Ljubicic who is coordinating geotechnical working group at the civil protection crisis unit. “Very near these two villages is the communal water supply source Pašino vrelo as well as a number of private wells. So, you must be really careful to choose material for covering sinkholes.”
Using cement or the wrong material to fill in the sinkholes could pollute local drinking water sources, so engineers are instead hoping to plug them with large boulders and then backfill the rest with smaller stones and gravel, says Mario Bacic, a civil engineer at the University of Zagreb.
It isn’t going to be cheap. Filling the hole in Borojevic’s could cost an estimated 200,000 EURO (£172,000).
“I could turn it into a fishpond,” jokes Borojevic.
Written By Vedrana Simicevic