At the 2012 Northern Territory election, the Country Liberal Party (CLP) won 16 of 25 seats, to 8 for Labor and 1 Independent. During a chaotic term, 4 CLP and 1 Labor members defected to sit as Independents, so the pre-election parliamentary numbers were 12 CLP, 7 Labor and 6 Independents.
At yesterday’s NT election, the ABC is calling 15 of 25 seats for Labor, 1 for the CLP and 3 for Independents, with 6 in some doubt. The ABC’s prediction is 18 Labor, 3 CLP and 4 Independents. Even if Labor loses all doubtful seats, they would still have a clear majority.
Two of the doubtful seats – Blain and Nhulunbuy – are cases where the incorrect final two candidates were selected on election night. The electoral commission will need to redo the two candidate count in those seats. Former chief minister Terry Mills, who was deposed by Adam Giles in the last term, will need a strong flow of preferences from the CLP in Blain.
Giles himself is in trouble in his own seat of Braitling, trailing Labor by 21 votes on a swing of almost 20 points. Former Labor leader Delia Lawrie is likely to hold her seat of Karama as an Independent; she leads by 51.2-48.8.
Overall primary votes were 43.1% for Labor (up 6.6), 31.7% for the CLP (down 18.9), 3.5% for the new 1 Territory Party, 2.8% for the Greens (down 0.5) and 18.9% for all Others (up 9.3). The Others were mostly Independents. The Poll Bludger has a breakdown of the votes and seats for each region.
There are still some booths that have not yet been added to counts, particularly in remote seats. However, most electorates are reporting postal counts, so it is unlikely that the CLP’s position will improve post-election, in the way the Federal Coalition’s position improved. Counting will resume tomorrow morning.
At this election, the voting system was changed to optional preferential voting; previous NT elections used compulsory preferential voting. However, this change appears to have helped Labor. In Braitling, Labor trails by 10.4% on primary votes, but leads by 0.4% after preferences. It is likely that minor party voters who were hostile to the CLP put the CLP last, while those who were better disposed to the CLP followed the CLP’s advice, and just voted “1”.
At the March 2015 NSW election, the Coalition won 45.6% of the primary vote, with 34.1% for Labor and 10.3% for the Greens. The Coalition won the two party vote 54.3-45.7.
The first ReachTEL poll since the election, conducted Thursday night from a sample of 1610, has the Coalition and Labor tied at 50-50. Excluding the 8.1% undecided from the primary votes gives 42.9% for the Coalition (down 2.7 since the election), 38.0% for Labor (up 3.9) and 8.7% for the Greens (down 1.6).
Opposition leader Luke Foley led Premier Mike Baird 51-49 as better Premier, but ReachTEL’s forced choice better PM/Premier question removes the lean towards the incumbent that other polls exhibit. Despite the Coalition’s slump, voters approved of the ban on greyhound racing by a 51-31 margin.
Polls in most states are very scarce outside election campaigns. The last NSW poll by a credible pollster was the November-December 2015 Newspoll, which had the Coalition ahead by 56-44. This ReachTEL implies that the gloss has come off the Coalition since then.
The Appenines region of central Italy has been struck by a deadly earthquake, with a magnitude of 6.2. The quake, which had an epicentre roughly 10km southeast of Norcia, Italy, occurred just over seven years after the 2009 L’Aquila earthquake that killed more than 300 people only 90km away.
The latest earthquake occurred at 3:36 am local time. The number of fatalities is unknown at time of writing but already exceeds 30. Buildings have collapsed in nearby Amatrice and residents are reportedly trapped in rubble.
This earthquake is no surprise. Italy is prone to earthquakes; it sits above the boundary of the African and European plates. The oceanic crust of the African plate is subducting (sinking) under Italy, creating iconic natural features such as the volcano at Mount Vesuvius. These plates are converging at a rate of around 5mm each year.
Both the L’Aquila and Norcia earthquakes were located below the central Appenines, which form the mountainous spine of Italy.
The Earth’s crust under the Appenines of central and western Italy is extending; eastern central Italy is moving to the north east relative to Rome. As a result, this region experiences normal faulting: where one part of the earth subsides relative to another as the crust is stretched.
The fault systems in the central Appenines are short and structurally complex, so the earthquakes are not large by global standards, the largest almost invariably hover around magnitude 6.8 to 7.0. But because the quakes are shallow and structurally complex, and because many of the local towns and cities contain vulnerable buildings, strong shaking from these earthquakes has the potential to inflict major damage and loss of life in urban areas.
This region also seems to be particularly prone to earthquake clustering, whereby periods of relative quiet are interrupted by several strong earthquakes over weeks to decades.
Both Norcia and L’Aquila feature prominently at either end of a zone of large Appenine earthquakes. This zone has produced many strong earthquakes. The latest Norcia earthquake occurred only around 90km northwest of the L’Aquila earthquake and very close to the epicentre of the 1979 Norcia earthquake, which had a magnitude of 5.9.
But the area’s earthquake history can be traced back over seven centuries. During this period, this region has been hit by at least six earthquakes that have caused very strong to severe shaking. Amatrice, so badly damaged in the most recent quake, was severely damaged in 1639. A few decades later, in 1703, roughly 10,000 people were killed in Norcia, Montereale, L’Aquila and the surrounding Appenine region in three magnitude 6.2-6.7 earthquakes.
Parts of Norcia were subsequently built upon the surface rupture created in the 1703 earthquake. Another earthquake in 1997 killed 11 people.
In this most recent event, an estimated 13,000 people would have experienced severe ground shaking, probably lasting 10-20 seconds.
The estimated damage of this latest earthquake will almost inevitably exceed US$100 million, and may top US$1 billion. Amatrice appears to be among the populated areas that were most severely affected.
The region now faces a prolonged and energetic aftershock sequence; over the first 2.5 hours following the mainshock, at least four earthquakes of around magnitude 4.5 were recorded in the region by the US Geological Survey. More than 10,000 aftershocks were recorded following the L’Aquila earthquake in 2009.
We note that within the region, there is excellent and continuously improving scientific information about the hazard. But the knowledge of the hazard has not always translated well into measures that directly reduce economic loss and fatalities in earthquakes.
Following the L’Aquila earthquake, six scientists were convicted of manslaughter for failing to inform the public adequately of the earthquake risk. Although the charges were subsequently dropped, this marked a major development in the way blame is apportioned after large natural events, particularly with regard to effective hazard communication.
Numerous vulnerable buildings remain, and the recovery process is commonly plagued by long disruptions and inadequate government funding to recover rapidly. Both the 2009 L’Aquila earthquake and this most recent quake highlight just how important it is to translate hazard assessments into improving the resilience of infrastructure to strong shaking. The focus should remain on linking science, engineering and policy, this is often the biggest challenge globally.
Brendan Duffy, Lecturer in Applied Geoscience, University of Melbourne; Mark Quigley, Associate professor, University of Melbourne, and Mike Sandiford, Chair of Geology & Redmond Barry Distinguished Professor, University of Melbourne