http://www.guardian.co.uk/world/2013/mar/04/what-causes-sinkholes-florida-man


What causes sinkholes?
It's the stuff of nightmares: last week, the ground opened up and swallowed a 
Florida man as he lay sleeping in his home. But why do these sinkholes occur 
and how widespread are they?

  a.. 
  a..  
  b.. 
    a.. Jon Henley 
    b.. The Guardian, Monday 4 March 2013 17.35 GMT 
    c.. Jump to comments (39) 

Link to video: Sinkhole house in Florida demolished 
Last week, in a quiet residential suburb east of Tampa, Florida, the Earth 
opened up and swallowed a man. Jeff Bush, 37, was tucked up in bed late on 
Thursday evening when his entire bedroom floor simply gave way with a deafening 
crash that his brother, in the room next door, later described as "like a truck 
hitting the house".

Jeremy Bush, 35, heard his brother's scream and rushed towards his bedroom. 
"Everything was gone," he told local television stations. "My brother's bed, my 
brother's dresser, my brother's TV. My brother was gone. All I could see was 
the top of his bed, so I jumped in and tried digging him out. I thought I could 
hear him screaming for me and hollering for me."

As the house's floor threatened to collapse further into a gaping hole more 
than 9m across and 15m deep, a sheriff's deputy who had arrived on the scene 
with the emergency services eventually pulled Jeremy to safety. Jeff remained 
trapped. "I couldn't get him out," Jeremy said. "I tried so hard. I tried 
everything I could. No one could do anything."

As Jeremy and four others, including a two-year-old child, were led away 
uninjured, rescue teams lowered a microphone and video camera into the hole, 
but it was soon apparent that Bush could not have survived. By Saturday, the 
search for his body had also been abandoned. "We just have not been able to 
locate Mr Bush, and so for that reason, the rescue effort is being 
discontinued," a local official, Mike Merrill, said. "At this point, it's 
really not possible to recover the body."

When the ground begins opening up beneath our feet and plunging unsuspecting 
mortals into the abyss, some may be tempted to reach for the Bible and start 
predicting the End of Times (and a quick online search reveals that several of 
the wackier sort of website have not hesitated to do just that). But biblical 
as the story sounds, the sinkhole – as the phenomenon is called – that caused 
Jeff Bush's death was not an act of God but of geology.

 A sinkhole in the centre of Guatemala City that swallowed a three-storey 
building in May 2010. Photograph: Luis Echeverria/AP Natural sinkholes – as 
opposed to manmade tunnel or cave collapses – occur when acidic rainwater seeps 
down through surface soil and sediment, eventually reaching a soluble bedrock 
such as sandstone, chalk, salt or gypsum, or (most commonly) a carbonate rock 
such as limestone beneath. In a process that can last hundreds, sometimes 
thousands of years, the water gradually dissolves small parts of the rock, 
enlarging its natural fissures and joints and creating cavities beneath.

As the process continues, the loose, unconsolidated soil and sand above is 
gradually washed into these cracks and voids. Depending on how thick and strong 
that top layer is (sand will not last long; clay can hold out for millennia), 
and how close to the surface the void beneath is, the land may be able to 
sustain its own weight – and that of whatever we build on top of it. But as the 
holes grow, there will come a day when the surface layer will simply give way.

"Once those caves start to collapse, the materials above will simply funnel 
in," says Dr Anthony Cooper, a principal geologist at the British Geological 
Survey, which maps the country for rock types susceptible to sinkholes and 
carries out surveys for developers, builders and individuals worried about the 
prospects of the land caving in beneath them. "It's just like an eggtimer, 
really. That's certainly what appears to have happened with this incident in 
Florida."

 Jeremy Bush, right, is consoled as he sits outside the home where a sinkhole 
swallowed his brother Jeffrey Bush. The house has since been demolished. 
Photograph: Chris O'Meara/AP In the language of geologists, the process that 
causes sinkholes is "the creation of a void which migrates towards the 
surface". In the language of the layman, when there's not enough solid stuff 
left underneath to support what is left of the loose stuff above, the whole lot 
collapses. The resulting depressions characterise what is known as a karst 
landscape, in which hundreds or even thousands of relatively small sinkholes 
form across an area that, seen from the air, can appear almost pock-marked.

Since around 10% of the world's surface is made up of karst topographies, 
sinkholes are far from uncommon. The entire state of Florida, as the Bush 
family unfortunately learned, is classed as karst landscape, and sinkholes are 
so common that insurers are obliged by law to offer cover to home owners who 
ask for it (insurance was compulsory until 2007, when many home owners dropped 
it because of the rising cost). "If you look at a satellite image of the state, 
or even just a map," says Cooper, "you'll see it's peppered with little 
circular lakes and lots and lots of sinkholes. A great many of them are 
visible, but many more are covered in. It's typical karst topography."

Elsewhere in the US, sinkholes are common in Texas, Alabama, Missouri, 
Kentucky, Tennessee and Pennsylvania. In Britain, the BGS says the 
carboniferous limestone of the Mendip Hills, the north of the South Wales 
coalfield, the Peak District, the Yorkshire Dales, the northern Pennines and 
the edges of the Lake District all host well-developed karst landscapes. 
Karstic features are also common in the UK on the chalk of south-east England, 
on salt in the centre and north-east of the country, and particularly on the 
gypsum that underlies parts of eastern and north-eastern England, especially 
around Ripon and Darlington, and in the Vale of Eden.

"Gypsum is the most soluble of all," says Cooper. "If you were to place a block 
of gypsum the size of a transit van in a river, it would dissolve completely 
within about 18 months." Ripon in North Yorkshire, Cooper says, is very 
susceptible to sinkholes, the most famous – some 20m deep – dating back to 
1834. In 1997, four garages collapsed into a huge sinkhole that only just 
missed the front of a neighbouring house.

One of the more spectacular recent British sinkholes, a 7.5m-deep crater, 
opened up in 2010 beneath a patio in Grays, Essex. "It was like an earthquake. 
There was a rumbling and we both ran out to look and there just a couple of 
steps away there was this monstrous hole," the house owner, Ben Luck, said at 
the time. "It was there in a second. There wasn't a bit of dust, and there was 
no sign of the crazy paving – it had all disappeared in the hole." Structural 
engineers said the hole was caused after water penetrated chalk some 25m down, 
causing tonnes of soil above it to shift.

 This sinkhole appeared overnight in a house in Guatemala City in 2011. It was 
12.2m deep and 80cm in diameter. Photograph: Johan Ordonez/AFP Around the 
world, this process that produces sinkholes has created such striking natural 
features as the hills of Ireland's western coast, the caves of Slovenia and the 
pillars of Guilin in China. Where the underlying limestone layer is thick and 
rainfall heavy, vast underground caverns and subterranean rivers have produced 
sinkholes of dimensions that make what's happened in Florida or Essex look 
positively insignificant: the Xiaozhai tiankeng ("heavenly pit") in Chongqing, 
China, is 662m deep; the Dashiwei tiankeng in Guangxi 613m. Croatia has a 
530m-deep hole, with vertical walls, called the Red Lake, while Papua New 
Guinea has the Minyé sinkhole (510m deep) and Mexico the Sótano del Barro 
(410m) and Sótano de las Golondrinas (372m deep).

What finally triggers a collapse? The most common factor, Cooper says, is 
changing groundwater levels, or a sudden increase in surface water. During long 
periods of drought, groundwater levels will fall, meaning cavities that were 
once supported by the water they were filled with may become weaker (water 
pumping, for factories or farms, can have a similar effect). Conversely, a 
sudden heavy downfall can add dramatically to the weight of the surface layer 
of soil and clay, making it too heavy for the cave beneath to bear.


Link to video: Huge sinkhole in Guangzhou swallows buildings 
Sometimes the trigger can be man-made. In chalky West Sussex in 1985, a burst 
water main caused an alarming rash of small 1m- to 4m-wide sinkholes to appear 
in Fontwell. "There  was also a man who emptied his swimming pool out on to his 
garden, and was soon confronted with a large sinkhole under his house," Cooper 
says. "And in Florida, automatic frost sensors have set off sprays fed from 
boreholes and intended to stop strawberry crops from freezing – but the result 
was more than 100 small sinkholes."

So how can you detect a developing sinkhole – and can anything be done about it 
once you suspect the process may be under way? In Britain, Cooper says, the BGS 
maps the country to locate rock types that may be affected by sinkholes. It 
also keeps an up-to-date National Karst Database recording visible sinkholes, 
springs, soakaways and known building damage. Using all manner of modern 
technologies, "we cut an awful lot of data, from rock types to slope angles, 
covering materials and drainage, and basically zone the country into datasets 
that can be used by property developers, local councils, the construction 
industry, insurers and the like," he says.

At the most basic level, people in a sinkhole-prone zone are best advised 
simply to "look around them, at the adjacent land and buildings". Telltale 
signs may include sagging trees or fence posts, doors or windows that no longer 
close properly, and rainwater collecting in unlikely places. Some developing 
sinkholes can be filled in; Anthony Randazzo, a former University of Florida 
professor who has spent his career studying sinkholes, now runs a profitable 
company that does just that, injecting grout to fill cracks that develop 
underground and shore up the foundations of buildings. "It's like a dentist 
filling a cavity," he says.

But this is not always possible. The key is good drainage; you want to get 
water away from a vulnerable area. "Covering an opening up with concrete, or 
filling up a hole completely with solid concrete, may not necessarily help," 
warns Cooper. Sometimes, too, the hole may simply be too deep: 80m, perhaps, 
compared with the 12-15m height of a house. "On some occasions, we have had to 
point out to developers that a hole 20m deep and 30m wide is a lot bigger than 
a house," Cooper says. "That's a hell of a lot of concrete."

Despite the frequency of sinkholes, linked fatalities are rare. Randazzo says 
he can recall only two other people besides Bush who have died because of them 
in the US during the past 40 years. Even then, he says, in both cases the 
people concerned had been drilling boreholes (and thus interfering with 
groundwater levels). "Usually, you have some time," Randazzo, who has lectured 
on sinkholes at Oxford University, told USA Today. "These catastrophic 
sinkholes give you some warning over the course of hours. This latest incident 
is very unusual, and very tragic."

In the UK, Cooper says, no deaths attributable solely to naturally formed 
sinkholes (as opposed, say, to the collapse of disused mine chambers) have been 
recorded in recent times. But, he points out, since extremes of 
sinkhole-affecting weather – long periods of drought, for example, followed by 
spells of unusually heavy and persistent rain – are widely predicted to become 
more frequent as the Earth's climate changes, "we would certainly expect there 
to be more sinkholes in the future". It could be only a matter of time before 
Britain buries a Jeff Bush.


[Non-text portions of this message have been removed]

Kirim email ke