Friday, 28 October 2016

Asteroid 2016 UQ36 passes the Earth.

Asteroid 2016 UQ36 passed by the Earth at a distance of 396 900 km (1.03 times the average distance between the Earth and the Moon, 0.27% of the average distance between the Earth and the Sun), at about 10.20 pm GMT on Monday 24 October 2016. It has not been possible to determine the size of this object, though given the closeness at which it passed the Earth, this inability implies it must be fairly small.

The calculated orbit of 2016 UQ36. Minor Planet Center.

2016 UQ36 was discovered on 26 October 2016 (two days after its closest approach to the Earth) by the University of Arizona's Mt. Lemmon Survey at the Steward Observatory on Mount Lemmon in the Catalina Mountains north of Tucson. The designation 2016 UQ36 implies that the asteroid was the 916th object (object Q36) discovered in the second half of October 2016 (period 2016 U).

2016 UQ36 is calculated to have a 851 day orbital period and an elliptical orbit tilted at an angle of 4.70° to the plain of the Solar System that takes it from 0.88 AU from the Sun (i.e. 88% of the average distance at which the Earth orbits the Sun) to 2.66 AU from the Sun (i.e. 266% of the average distance at which the Earth orbits the Sun, almost twice the distance at which the planet Mars orbits the Sun). It is therefore classed as an Apollo Group Asteroid (an asteroid that is on average further from the Sun than the Earth, but which does get closer).

See also...

 http://sciencythoughts.blogspot.co.uk/2016/10/asteroid-2016-to11-passes-earth.htmlhttp://sciencythoughts.blogspot.co.uk/2016/10/asteroid-2016-ud-passes-earth.html
http://sciencythoughts.blogspot.co.uk/2016/10/asteroid-462959-2011-du-passes-earth.htmlhttp://sciencythoughts.blogspot.co.uk/2016/10/asteroid-2016-th-passes-earth.html
http://sciencythoughts.blogspot.co.uk/2016/10/asteroid-2016-td-passes-earth.htmlhttp://sciencythoughts.blogspot.co.uk/2016/10/fireball-over-eastern-great-lakes-region.html
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Gorilla beringei graueri: Grauer's Gorilla declared to be Critically Endangered.

Eastern Gorillas, Gorilla beringei, are considered to belong to two subspecies, the Mountain Gorilla, Gorilla beringei beringei, and the Grauer's Gorilla or Eastern Lwland Gorilla, Gorilla beringei graueri. The Mountain Gorilla is considered to be Critically Endangered under the terms of the International Union for the Conservation of Nature's Red List of Threatened Species, and have been subject to extensive conservation measures and regular monitoring since the 1970s, with the effect that their population is currently thought to be slowly increasing. The Graurer's Gorilla, in contrast, is currently classified as Endangered under the terms of the International Union for the Conservation of Nature's Red List of Threatened Species, but no organized survey of the population of this species has been carried out since the 1990s, largely due to political instability and conflict in the east of the Democratic Republic of Congo where the majority of these Gorillas are found.

In a paper published in the journal PLoS One on 19 October 2016, Andrew Plumptre of the Wildlife Conservation Society and the Conservation Science Group at Cambridge University, Stuart Nixon of the North of England Zoological Society at Chester Zoo, Deo Kujirakwinja, also of the Wildlife Conservation Society, Ghislain Vieilledent of Forêts et Sociétés at L'organisme français de recherche agronomique et de coopération internationale pour le développement durable des régions tropicales et méditerranéennes, Rob Critchlow of the Department of Biology at the University of York, Elizabeth Williamson of the Faculty of Natural Sciences at the University of Stirling, Radar Nishuli of the Institut Congolais pour la Conservation de la Nature, Andrew Kirkby, again of the Wildlife Conservation Society, and Jefferson Hall of the Smithsonian TropicalResearch Institute, present the results of a new survey of the population of the Grauer's Gorilla, and discuss the implications of these results for the conservation status of this species.

A Grauer's Gorilla or Eastern Lwland Gorilla, Gorilla beringei graueri. Karl Ammann/WWF.

The only previous attempt at surveying the population of the Graur's Gorrila took place in 1994-95, when conservationists surveyed the population in the Kahuzi-Biega National Park, thought to be home to about 86% of the species' population, coming up with a figure of 16 900 individuals, on top of which it is thought there were a further 1000-2000 individuals in the Tayna-Usala region. Since this time the civil war in Rwanda in 1994 led to hundreds of thousands of refugees to flee into eastern Democratic Republic of Congo, destabilizing the area and helping to trigger the Congolese civil war of 1996-2003 which killed an estimated five million people, and destroyed much of what little infrastructure existed in the east of the country. This situation was further exasperated by refugees and militia groups fleeing conflicts in South Sudan and Uganda, and by military incursions by several neighbouring countries seeking access to the area's rich reserves of gold and coltan minerals.

This has led to a situation where much of the east of the Democratic Republic of Congo was in the hands of a variety of militia groups, many of which also control mining encampments, and are at least in part dependent on bushmeat (hunted game) for sustenance. Gorillas are often considered a valuable target by bushmeat hunters, as their large size means they provide a large amount of meat for a single kill, and their ground-dwelling habit makes them easier to track than the semi-arborial Chimpanzees. Against this background the Congolese parks authorities have struggled to re-assert their authority in the region, with more than 150 rangers from the Institut Congolais pour la Conservation de la Nature having been killed in action over the past 20 years.

 The funeral of an ICCN Ranger killed in the line of duty. Virunga National Park/Fallen Rangers Fund.

Plumptre et al. collected data from foot surveys made by park ranger and community ecogaurds (who operate on community run reserves) between 2011 and 2015. They were able to collect data from the Itebero-Lulingu and Nzovu sectors of the Kahuzi-Biega National Park, which were surveyed in 1994-95, plus the Kasese sector of the Kahuzi-Biega National Park, the Concession Forestière Communautaire des Banisamasi and the Tayna and Kisimba-Ikobo reserves, which were not.

From this data they were able to produce estimates of the population of Grauer's Gorillas in each of these areas, with the largest surviving population found in the Itebero-Lulingu sector of the Kahuzi-Biega National Park, where there are now an estimated 655 remaining Grauer's Gorillas, compared to an estimated 5635 in 1994-95. This was followed by the Tayna and Kisimba-Ikobo reserves (not surveyed in 1994-95) with an estimated combined population of 541 Gorillas. After this came the Nzovu sector of the Kahuzi-Biega National Park, with an estimated 258 Gorillas, compared to an estimated 1188 in 1994-95, then the Kasese sector of the Kahuzi-Biega National Park with an estimated 183 Gorillas and the Concession Forestière Communautaire des Banisamasi, with an estimated 24 Gorillas.

Map of the probability of presence for Grauer's gorilla. Occupancy probability was mapped using three covariables (tree cover, altitude and distance to recent deforestation) and a spatial autocorrelation (left panel). The probability threshold maximising the TSS was 0.35. This threshold was used to derive a gorilla distribution range (upper right panel) for which presence probabilities were greater than this value (grey = less than 0.35). Plumptre et al. (2016).

This gives a total estimated figure of 1661 surviving Grauer's Gorrillas in 2011-15, compared to the figure of 17 900-18 900 for 1994-95. This implies that the Grauer's Gorilla has lost 86.6% of its population in the Itebero-Lulingu and Nzovu sectors of the Kahuzi-Biega National Park in the two decades from 1995 to 2015. Gorillas can live for about 40 years, but a generation is generally taken as being about 20 years, which means that this loss has occurred in a single generation. One of the International Union for the Conservation of Nature's criteria for being included on the Red List of Threatened Species under the category Critically Endangered is the loss 80% or more of a species population within three generations. As the Grauer's Gorilla is known to have lost more than 80 of its population in a single generation across much of its range, and is likely to have declined by a similar amount in the other, previously unsurveyed areas, Plumptre et al. recommend that this species be included on the Red List as Critically Endangered.

See also...
 
http://sciencythoughts.blogspot.co.uk/2016/03/landslide-at-kamoto-copper-mine-kills.html
http://sciencythoughts.blogspot.co.uk/2015/03/terrestrial-behaviour-in-borneo.html 

http://sciencythoughts.blogspot.co.uk/2015/12/tantalum-mining-in-twenty-first-century.html
http://sciencythoughts.blogspot.co.uk/2014/11/crop-raiding-behaviour-by-chimpanzees.html
http://sciencythoughts.blogspot.co.uk/2014/12/amnesty-international-report-implicates.html



 
 
 
 
 
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Thursday, 27 October 2016

Landslide kills seven in Antioquia Province, Colombia.

Seven people are known to have died and it is feared that more people may be buried, following a landslide in Antioquia Province, Colombia, on the morning of Wednesday 26 October 2016. The andslide hit a four lane highway about 12 km to the north of the provincial capitol, Mendalin, covering about 200 m of road and burying a number of vehicles. The incident is reported to have happened following a period of heavy rain. Landslides are a common problem after severe weather events, as excess pore water pressure can overcome cohesion in soil and sediments, allowing them to flow like liquids. Approximately 90% of all landslides are caused by heavy rainfall.

The scene of the 26 October 2016 Antioquia landslide. AFP.

Antioquia is a mountainous province with several distanct climate zones. The Medallin area is considered to gave a monsoon climate, with a to peaks in rainfall in May and October. Two hot wet seasons per year is normal on the equator, where the Sun is highest in the sky around the equinoxes and lowest at the solstices, as opposed to the situation at higher latitudes, where the Sun is highest at one solstice and lowest at the other.

Monsoons are tropical sea breezes triggered by heating of the land during the warmer part of the year. Both the land and sea are warmed by the Sun, but the land has a lower ability to absorb heat, radiating it back so that the air above landmasses becomes significantly warmer than that over the sea, causing the air above the land to rise and drawing in water from over the sea; since this has also been warmed it carries a high evaporated water content, and brings with it heavy rainfall. In the tropical dry season the situation is reversed, as the air over the land cools more rapidly with the seasons, leading to warmer air over the sea, and thus breezes moving from the shore to the sea (where air is rising more rapidly) and a drying of the climate.

 Diagrammatic representation of wind and rainfall patterns in a tropical monsoon climate. Geosciences/University of Arizona.

See also...

http://sciencythoughts.blogspot.co.uk/2015/07/eruptions-on-nevado-del-ruiz.htmlhttp://sciencythoughts.blogspot.co.uk/2015/10/magnitude-54-earthquake-in-santander.html
http://sciencythoughts.blogspot.co.uk/2015/05/fifteen-missing-after-inrush-at.htmlhttp://sciencythoughts.blogspot.co.uk/2015/05/landslide-kills-at-least-78-people-in.html  
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
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Wednesday, 26 October 2016

Central Italy shaken by pair of Earthquakes.

The United States Geological Survey recorded two significant Earthquakes in Central Italy on Wednesday 26 October 2016. The first had a Magnitude of 5.5 and occurred 7 km to the southwest of the town of Visso in Macerata Province at a depth of 10 km at about 7.10 pm local time (about 5.10 pm GMT), while the second had a Magnitude of 6.1 km and occurred 2 km to the north of the town, again at a depth of 10 km, slightly before 7.20 pm local time (slightly before 5.20 pm GMT). There are no reports of any injuries following these events, but minor damage has been reported across a wide area, as well as power cuts and one instance of a road being closed by a small landslide. People have reported feeling the event across Central and Northern Italy, as well as in parts of Slovenia and Croatia.

The approximate location of the first 26 October 2016 Visso Earthquake. Google.

The approximate location of the second 26 October 2016 Visso Earthquake. Google.

Italy is in an unusual tectonic setting, with the west of the country lying on the Eurasian Plate, but the east of the country lying on the Adriatic Plate, a microplate which broke away from North Africa some time in the past and which is now wedged into the southern margin of Europe, underlying eastern Italy, the Adriatic Sea and the west of the Balkan Peninsula. This, combined with the northward movement of the African Plate into Italy from the south, leads to uplift in the Apennine Mountains that run the length of the country, and makes Italy extremely prone to Earthquakes. 

Outline map showing the approximate positions of the Eurasian (EU), Adriatic (AD) and African (AF) Plates. Di Bucci & Mazzuli (2003).

Historically Italy has suffered a number of devastating Earthquakes that lead to large numbers of casualties, though in recent decades the country has made serious attempts to prevent this, with better warning systems and tighter building regulations, though the large number of historic buildings in Italy, which cannot easily be replaced (and any attempt to do so would be unlikely to succeed due to their high cultural value), meaning that the country is unlikely to be completely risk free any time soon.

Witness accounts of Earthquakes can help geologists to understand these events, and the structures that cause them. The international non-profit organisation Earthquake Report is interested in hearing from people who may have felt this event; if you felt these quakes then you can report it to Earthquake Report here.
See also...

http://sciencythoughts.blogspot.co.uk/2016/08/italian-earthquake-kills-at-least-120.htmlhttp://sciencythoughts.blogspot.co.uk/2016/05/dozens-of-cars-swallowed-by-sinkhole-in.html

 
http://sciencythoughts.blogspot.co.uk/2014/11/at-least-four-killed-by-landslides-in.htmlhttp://sciencythoughts.blogspot.co.uk/2014/08/four-dead-in-italian-flash-flood.html

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Monday, 24 October 2016

Understanding the ancestry of the European Bison.

The European Bison, or Wisent (Bison bonasus), is one of a very small number of megafaunal (large) animal species to have survived from the Pleistocene in northern temperate latitudes. However the origin of the European Bison is less clear than it would immediately seem, as the earliest known fossil specimens date only from the Early Holocene (i.e. less than 11 700 years ago), prior to which Europe was inhabited by a different Bison species, the Steppe Bison (Bison priscus), which ranged from Britain in the east across Europe, Asia and Beringia (the landmass between Alaska and the Russian Far East which was exposed during the Pleistocene glaciations when the sea level was lower) and into western Canada. The Steppe Bison is considered to be the ancestor of the American Bison (Bison bison), but its relationship to the modern European Bison is less clear, as the European Bison, while clearly related to the American Bison, is genetically more closely related to Cattle (Bos spp.). This could potentially be due to recent hybridization between the species, the European Bison having gone through a number of population bottlenecks as it came into conflict with Humans and domestic animals, with the population having fallen to just twelve individuals in the 1920s, but hybrids between Bison and Cattle are usually infertile, making this a somewhat doubtful hypothesis.

In a paper published in the journal Nature Communications on 18 October 2016, a team of scientists led by Julien Soubrier of the Australian Centre for Ancient DNA at the University of Adelaide describe the results of a new study of the ancestry of the European Bison, which takes into account both archaeological and genetic evidence.

Soubrier et al. sequenced DNA from 64 Bison specimens from Late Pleistocene sites (from before 50 000 years ago to about 14 000 years ago) across Europe. 38 of these specimens, from the Caucasus, Urals, North Sea, France and Italy, were found to belong to a previously unknown Bison lineage, identified as Clade X (in biology a clade is a group of organisms with a common ancestor; a clade includes all the organisms descended from that ancestor and no organisms not descended from that ancestor). Based upon the relationship between Clade X and the European Bison, the two species shared a last common ancestor about 120 000 years ago (during the Eemian Interglacial), however like the European Bison, including Ancient European Bison used in this study (and unlike the American Bison) members of Clade X appear to derive about 10% of their DNA from a Cattle (Bos sp.) ancestor.

This discovery is interesting as it rules out the possibility of recent hybridization between Modern Cattle and European Bison, instead suggesting that the species came about as the result of a hybridization between ancient Steppe Bison and the Aurochs (Bos primigenius), a large Pleistocene animal thought to have been ancestral to modern Domestic Cattle. Further examination of the Bison samples in the study revealed that they all derived their mitochodrial DNA (mtDNA) from a Bos ancestor, but none of them any Y-chromosome DNA, This implies that both the European Bison and Clade X came about as a result of a hybridization between male Steppe Bison and female Aurochs, not implausible given that in all known Bovid species males tend to capture harems of females which they defend aggressively against other males, and that while the Aurochs were big animals, Steppe Bison were even larger. However whether or not the European Bison and Clade X arose from a single hybridization event, a cluster of such events or completely unrelated events could not be determined.

Soubrier et al. further observe that two distinct morphologies of Bison are recorded in European Pleistocene cave art. A total of 820 depictions of Bison are known from European cave art (21 % of all known animal depictions from the Pleistocene of Europe), and all of these fall into two morphotypes (shapes). The first is a long-horned animal with robust forequaters and a distinct hump, that appears in art dating from before the Last Glacial Maximum, roughly between 22 000 and 18 000 years ago. The second form is a more slender animal with small, recurved, horns and a small hump, which appears in Magdalenian art, roughly between 17 000 and 12 000 years ago. These differences have previously been regarded the expression of different artistic styles, however Soubrier et al. reject this hypothesis. Two different Bison morphologies (a robust form and a slender form) have also been noted from bones dredged from beneath the North Sea).

Cave painting example of steppe Bison-like and Wisent-like morphs. (a) Reproduction from Lascaux cave (France), from the Solutrean or early Magdalenian period (about 20 000 years ago). (b) Reproduction from the Pergouset cave (France), from the Magdalenian period (less than 17 000 years ago). Soubrier et al. (2016).

The oldest specimens with a European Bison genotype dated from before 55 000 years ago, while the oldest Clade X specimen dated from 23 000 years ago, and the youngest Steppe Bison from 19 000 years ago. However all known specimens from between 50 000 and 34 000 years ago are Steppe Bison. Environmental reconstructions and stable isotope studies of remains (which can reconstruct the environments in which ancient organisms live by studying the ratios of different carbon and nitrogen isotopes in their bones) suggest that the European Bison and Steppe Bison inhabited different environments, with the Steppe Bison dwelling in cold, tundra grasslands and the European Bison favouring a warmer, more mixed environment.

Based upon this Soubrier et al. suggest that there were two distinct Bison species present in Europe for much of the Late Pleistocene. The Steppe Bison favoured cold grassland environments and expanded its range during colder periods, disappearing at the end of the Pleistocene, probably due to a mixture of a loss of much of this environment and a rising Human population armed with better hunting tools. The European Bison arose from one or more hybridization events between the Steppe Bison and the Aurochs, but was able to persist as a ecologically separate entity due to a preference for a different environment, favouring warmer landscapes with mixed vegetation. This species has also been severely pressured by expanding Human populations, but was better able to cope with the changing climate and has persisted till modern times.

See also...

http://sciencythoughts.blogspot.co.uk/2016/01/ammotragus-lervia-diet-of-barbary-sheep.htmlAmmotragus lervia: The diet of the Barbary Sheep in the Bou Hedma Mountains of Tunisia.                                                         The Barbary Sheep (or Aoudad), Ammotragus lervia, is a wild Caprid found in North Africa, from the Mediterranean as far south as the Niger and Lake...
http://sciencythoughts.blogspot.co.uk/2014/07/a-highly-specialized-musk-ox-from-late.htmlA highly specialized Musk Ox from the Late Miocene of Gansu Province, China.              In 1932 Birger Bohlin, chief palaeontologist with the explorer Sven Hedin’s Sino-Swedish Scientific Expedition to Northwest China, discovered an...
http://sciencythoughts.blogspot.co.uk/2013/08/how-fencing-tibetan-prairies-is.htmlHow fencing the Tibetan prairies is effecting the endangered Przewalski’s Gazelle. The Przewalski’s Gazelle (Procapra przewalskii) is a species of high altitude adapted Antelope, which formerly ranged across much of northwestern China and Inner Mongolia. It is now restricted to a small area around Qinghai Lake on the Tibetan Plateau, with...
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Asteroid 2016 UD passes the Earth.

Asteroid 2016 UD passed by the Earth at a distance of 72 540 km (0.21 times the average distance between the Earth and the Moon, 0.05% of the average distance between the Earth and the Sun), slightly after 11.30 pm GMT on Monday 17 October 2016. There was no danger of the asteroid hitting us, though had it done so it would have presented no threat. 2016 UD has an estimated equivalent diameter of 9-28 m (i.e. it is estimated that a spherical object with the same volume would be 9-28 m in diameter), and an object of this size would be expected to explode in an airburst (an explosion caused by superheating from friction with the Earth's atmosphere, which is greater than that caused by simply falling, due to the orbital momentum of the asteroid) in the atmosphere between 32 and 20 km above the ground, with only fragmentary material reaching the Earth's surface. 

The calculated orbit of 2016 TO11. Minor Planet Center.

2016 UD was discovered on 19 October 2016 (two days after its closest approach to the Earth) by the University of Arizona's Mt. Lemmon Survey at the Steward Observatory on Mount Lemmon in the Catalina Mountains north of Tucson. The designation 2016 UD implies that the asteroid was the fourth object (object D) discovered in the second half of October 2016 (period 2016 U).

2016 UD has a 695 day orbital period and an elliptical orbit tilted at an angle of 10.3° to the plain of the Solar System that takes it from 0.51 AU from the Sun (i.e. 51% of the average distance at which the Earth orbits the Sun, between the orbits of Mercury and Venus) to 2.56 AU from the Sun (i.e. 256% of the average distance at which the Earth orbits the Sun, almost twice the distance at which the planet Mars orbits the Sun). It is therefore classed as an Apollo Group Asteroid (an asteroid that is on average further from the Sun than the Earth, but which does get closer). This means that 2016 UD has occasional close encounters with the Earth, with the next predicted for June 2174.

See also...

http://sciencythoughts.blogspot.co.uk/2016/10/asteroid-2016-to11-passes-earth.htmlAsteroid 2016 TO11 passes the Earth.    Asteroid 2016 TO11 passed by the Earth at a distance of 895 500 km (2.33 times the average distance between the Earth and the Moon, 0.60% of the average distance between the Earth and the Sun), slightly after 7.00 pm GMT on Wednesday 12...
http://sciencythoughts.blogspot.co.uk/2016/10/asteroid-462959-2011-du-passes-earth.htmlAsteroid (462959) 2011 DU passes the Earth.                                                     Asteroid  (462959) 2011 DU passed by the Earth at a distance of 5 828 000 km (15.2 times the average distance between the Earth and the Moon, or 3.90%...
http://sciencythoughts.blogspot.co.uk/2016/10/asteroid-2016-th-passes-earth.htmlAsteroid 2016 TH passes the Earth.       Asteroid 2016 TH passed by the Earth at a distance of 128 300 km (0.34 times the average distance between the Earth and the Moon, 0.09% of the average distance between the Earth and the Sun), at about 4.30 pm...
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Sunday, 23 October 2016

Queensland miner killed in trench collapse.

A sixty-two-year-old miner has been found dead following a the collapse of an exploration trench at a mine in Opalton, Queensland, on Saturday 22 October 2016. Sid Cuddy was reported missing after a friend visited the site where he was operating at about 4.00 pm local time. The location is described as being extremely remote, being about 150 km southwest of Winton and about 300 km west of Longreach, and it took police and firefighters six hours to reach the site, and a further three hours to clear the trench and find Mr Cuddy's body.

Sid Cuddy (62), who died in a collapse at an exploration trench at an opal mine in Opalton, Queensland, on 22 October 2016. The Courier Mail.

Opal is an amorphous form of silica containing as much as 21% water, It is made up of tiny spheroids of crystalline silica some 150 to 300 nm in diameter, with random alignments to one another. Light passing through these crystaloids is refracted as by a prism, leading to the 'opalescent' sheen which gives the mineral its value. Opal is formed by water percolating through silica rocks, where it desolves some of the mineral forming a silica-rich solution. This can accumulate in any cracks or gaps in the rock, where if it reaches a high enough concentration it can precipitate out as opal.

Opal beds in Queensland are found largely in exposures of the Cretaceous Winton Formation, an iron rich sandstone laid down in a shallow inland sea (the Etomanga Sea) that covered parts of Queensland and central Australia during the Early Cretaceous. which extends from Hungerford on the New South Wakes border northwest to the area around Kynuna, a distance of over 1000 kilometres. The opal here is typically found in cracks in ironstone concretions (themselves formed by precipitation from water that has accumulated iron as it peculated through the feruginous sandstone), and is commonly called 'boulder opal'.

These fields have been worked since the 1870s, with the bulk of the mining done by small, artisanal miners who sink shallow trenches into the sandstone looking for opal-bearing boulders. The Opalton deposits were among the first opal fields discovered in Australia, and as well as still supporting a mining industry, are now a thriving tourist attraction.

Mr Cuddy is described as having been a highly experienced miner, always willing to help other less experienced prospectors. The cause of the collapse that killed him is as yet unknown.

See also...

http://sciencythoughts.blogspot.co.uk/2015/02/worker-killed-by-exploding-tyre-at.htmlWorker killed by exploding tyre at Queensland coal mine.                                                       A 21-year-old man has been killed and a second worker severely injured after a tyre on a truck exploded at the Dawson Coal Mine, an open pit mine near Moura in Queensland, Australia, at about...
http://sciencythoughts.blogspot.co.uk/2015/02/worker-killed-in-rockfall-at-south.htmlWorker killed in rockfall at South Australian copper mine.                                                   A worker has been killed in a rockfall at the BHP Billiton owned Olympic Dam Copper Mine in South Australia. Brian Partington, 47, was struck on the chest by falling rocks at about 6.00 am local time on Tuesday 10 February 2015. The cause of...
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