1 00:00:10,614 --> 00:00:15,294 Speaker 1: You're listening to a Muma Mea podcast. Mumma Mea acknowledges 2 00:00:15,334 --> 00:00:18,174 Speaker 1: the traditional owners of land and waters that this podcast 3 00:00:18,214 --> 00:00:19,054 Speaker 1: is recorded on. 4 00:00:21,894 --> 00:00:22,094 Speaker 2: Hi. 5 00:00:22,214 --> 00:00:25,254 Speaker 1: I'm Claire Murphy. This is Mumma MIA's daily news podcast, 6 00:00:25,294 --> 00:00:28,534 Speaker 1: The Quickie. Between last week and this week, there have 7 00:00:28,574 --> 00:00:31,814 Speaker 1: been several major earthquakes across the country, with one in 8 00:00:31,814 --> 00:00:36,174 Speaker 1: particular raising questions about how much Australia's mining companies are 9 00:00:36,214 --> 00:00:40,534 Speaker 1: contributing to the increase in seismic activity. Today we'll speak 10 00:00:40,574 --> 00:00:43,134 Speaker 1: to an earthquake expert to find out whether humans are 11 00:00:43,134 --> 00:00:45,894 Speaker 1: making the ground a little more shaky. But before we do, 12 00:00:46,094 --> 00:00:48,894 Speaker 1: here's the latest from the Quikie newsroom. Wednesday, August twenty eight. 13 00:00:49,294 --> 00:00:52,414 Speaker 1: There are predictions that ticket sales for the Oasis reunion 14 00:00:52,494 --> 00:00:55,814 Speaker 1: tour next year could dwarf even Taylor Swift's EERU shows. 15 00:00:56,174 --> 00:01:00,494 Speaker 1: British music journalist and producer DJ Kevin McManus reminded ITV 16 00:01:00,894 --> 00:01:03,894 Speaker 1: that almost four percent of the entire population of the 17 00:01:03,974 --> 00:01:07,694 Speaker 1: UK tried to get tickets to Oasis to Nebworth shows 18 00:01:07,694 --> 00:01:11,014 Speaker 1: back in nineteen ninety six, nually selling two hundred and 19 00:01:11,014 --> 00:01:14,374 Speaker 1: fifty thousand. He says people still talk about those shows, 20 00:01:14,454 --> 00:01:17,334 Speaker 1: and this time around it could be even bigger. He's 21 00:01:17,374 --> 00:01:19,854 Speaker 1: also wondering if people will go just to see if 22 00:01:19,854 --> 00:01:22,054 Speaker 1: the brothers Liam and Noel will fall out before the 23 00:01:22,094 --> 00:01:24,974 Speaker 1: first show or the fifth. Oway says will perform a 24 00:01:25,014 --> 00:01:27,574 Speaker 1: series of live shows in the UK and Ireland next year. 25 00:01:27,854 --> 00:01:31,894 Speaker 1: Experts predicting with ticket sales, sponsorships, merch and film rights, 26 00:01:32,094 --> 00:01:35,014 Speaker 1: the brothers could make over four hundred million pounds, the 27 00:01:35,054 --> 00:01:39,374 Speaker 1: equivalent of nearly eight hundred million. Australian unions have slammed 28 00:01:39,374 --> 00:01:43,014 Speaker 1: the Fairwork Ombardsmen, saying threats to dock construction workers pay 29 00:01:43,054 --> 00:01:44,974 Speaker 1: for walking off the job to rally in support of 30 00:01:45,014 --> 00:01:49,774 Speaker 1: the CFMEU yesterday are baseless and misleading. Attorney General Mark 31 00:01:49,854 --> 00:01:54,014 Speaker 1: Drefers placed the CFMEU into administration last week after claims 32 00:01:54,014 --> 00:01:56,694 Speaker 1: they've been involved in corruption and bullying and had been 33 00:01:56,694 --> 00:02:00,934 Speaker 1: infiltrated by organized crime. Anger over the decision saw thousands 34 00:02:00,934 --> 00:02:04,294 Speaker 1: of workers attend rallies across the country despite threats from 35 00:02:04,334 --> 00:02:07,934 Speaker 1: the Fairwork Ombardsmen that unsanctioned industrial action could see them 36 00:02:07,974 --> 00:02:11,014 Speaker 1: docked four hours pay. The union say this was not 37 00:02:11,214 --> 00:02:14,494 Speaker 1: industrial action and to call it so is misleading, saying 38 00:02:14,534 --> 00:02:17,134 Speaker 1: they were uniting to protest what they believe is an 39 00:02:17,134 --> 00:02:21,374 Speaker 1: attack on basic workers' rights and procedural fairness. The Israeli 40 00:02:21,454 --> 00:02:24,334 Speaker 1: Defense Force has managed to rescue another hostage in a 41 00:02:24,374 --> 00:02:27,734 Speaker 1: complex operation, more than ten months after he was captured 42 00:02:27,774 --> 00:02:30,654 Speaker 1: in the October seven attack. Fifty two year old kade 43 00:02:30,694 --> 00:02:33,414 Speaker 1: Fahan al Khadi, a member of the Bedouin community in 44 00:02:33,494 --> 00:02:36,814 Speaker 1: southern Israel, was rescued from a tunnel in southern Gaza. 45 00:02:37,094 --> 00:02:39,854 Speaker 1: The details of how he was located and extracted have 46 00:02:39,974 --> 00:02:43,374 Speaker 1: not been shared, authorities saying it could compromise the security 47 00:02:43,374 --> 00:02:46,734 Speaker 1: of both the remaining hostages and the IDF. Israeli Prime 48 00:02:46,734 --> 00:02:49,574 Speaker 1: Mister Benjamin Ettanya, who says they will continue to bring 49 00:02:49,614 --> 00:02:54,414 Speaker 1: hostages home through both negotiations and rescue operations, saying both 50 00:02:54,454 --> 00:02:57,134 Speaker 1: require Israel to have a military presence in the field 51 00:02:57,454 --> 00:03:01,694 Speaker 1: and unceasing military pressure on Hamas. Prince Harry has announced 52 00:03:01,694 --> 00:03:04,534 Speaker 1: his next royal not royal visit, heading to New York 53 00:03:04,574 --> 00:03:07,494 Speaker 1: next month. Harry will be doing this trip solo, Megan 54 00:03:07,574 --> 00:03:09,854 Speaker 1: staying home with the kids while he visit. It's the 55 00:03:09,854 --> 00:03:12,614 Speaker 1: City that Never sleeps during the UN General Assembly, High 56 00:03:12,694 --> 00:03:15,534 Speaker 1: Level Week and Climate Week. While he's there, Harry is 57 00:03:15,614 --> 00:03:18,654 Speaker 1: set to advance a number of his patronages while attending 58 00:03:18,694 --> 00:03:22,534 Speaker 1: several engagements with African Parks, the Halo Trust, the Diana 59 00:03:22,574 --> 00:03:25,614 Speaker 1: Award and Travelist. He'll also be furthering the work of 60 00:03:25,654 --> 00:03:28,814 Speaker 1: the Archwell Foundation, which recently launched an initiative to help 61 00:03:28,854 --> 00:03:32,374 Speaker 1: parents deal with online bullying. Harry's travel plans come as 62 00:03:32,374 --> 00:03:34,694 Speaker 1: a new theory has emerged as to why his father, 63 00:03:34,774 --> 00:03:38,054 Speaker 1: King Charles, is trying to move his disgraced brother Andrew 64 00:03:38,094 --> 00:03:40,654 Speaker 1: out of the Royal Lodge. Richard Eden from The Daily 65 00:03:40,694 --> 00:03:43,294 Speaker 1: Mail says he believes it's a potential future home for 66 00:03:43,374 --> 00:03:47,454 Speaker 1: Queen Camilla should she outlive him. The theory also casting 67 00:03:47,454 --> 00:03:50,454 Speaker 1: into doubt the King's current health situation as to why 68 00:03:50,494 --> 00:03:53,694 Speaker 1: he's making these moves with such urgency. That's What's happening 69 00:03:53,734 --> 00:03:55,694 Speaker 1: around the world today. Next, we find out if digging 70 00:03:55,774 --> 00:03:58,254 Speaker 1: up Cole might just be making the Hunter Valley in 71 00:03:58,334 --> 00:04:14,574 Speaker 1: New South Wales earthquake central. If you drive away from 72 00:04:14,614 --> 00:04:17,894 Speaker 1: Sydney Northwest to the Hunter Valley, you are first greeted 73 00:04:18,014 --> 00:04:22,814 Speaker 1: by picturesque wine country, stunning valleys dotted with vineyards and 74 00:04:22,854 --> 00:04:26,134 Speaker 1: wedding receptions where tourists had to enjoy a weekend away, 75 00:04:27,334 --> 00:04:30,014 Speaker 1: but go just a little bit further west to the 76 00:04:30,014 --> 00:04:32,774 Speaker 1: town of Singleton and you'll start to catch glimpses from 77 00:04:32,774 --> 00:04:37,014 Speaker 1: the highway of colossal open cut coal mines. The tiny 78 00:04:37,134 --> 00:04:40,174 Speaker 1: vehicles on its fast slopes brought into perspective when one 79 00:04:40,174 --> 00:04:42,974 Speaker 1: crosses a bridge, even just the wheels of the trucks 80 00:04:43,134 --> 00:04:46,374 Speaker 1: much bigger than a human. One of these mines is 81 00:04:46,414 --> 00:04:50,654 Speaker 1: between two Hunter Valley towns, Musselbrook and Denman. Owned by BHP, 82 00:04:50,974 --> 00:04:55,054 Speaker 1: the Mount Arthur mine employs around two thousand people. It's 83 00:04:55,054 --> 00:04:57,734 Speaker 1: almost at the end of its life, operations expected to 84 00:04:57,774 --> 00:05:01,294 Speaker 1: wrap up in twenty thirty, but on Friday it became 85 00:05:01,374 --> 00:05:09,054 Speaker 1: the epicenter of a four point seven magnitude earthquake. The 86 00:05:09,054 --> 00:05:11,534 Speaker 1: map show the center of the quake located near the 87 00:05:11,574 --> 00:05:14,934 Speaker 1: middle of the pit, shaking nearby towns. Just after midday 88 00:05:14,934 --> 00:05:19,494 Speaker 1: on Friday, the rattle felt as far away as Sydney. 89 00:05:20,694 --> 00:05:23,294 Speaker 1: Since then, there have been many after shocks that have 90 00:05:23,374 --> 00:05:26,294 Speaker 1: continued through the weekend and into the start of this week. 91 00:05:27,614 --> 00:05:29,614 Speaker 1: The people who live and work in the region are 92 00:05:29,654 --> 00:05:32,454 Speaker 1: a little worried, especially after this quake brought down the 93 00:05:32,494 --> 00:05:36,494 Speaker 1: roofs of several local businesses. Damaged buildings, cracked windows and 94 00:05:36,574 --> 00:05:39,254 Speaker 1: caused the power to go out for several hours. But 95 00:05:39,334 --> 00:05:41,614 Speaker 1: they're also used to living with the sounds and feel 96 00:05:41,654 --> 00:05:43,174 Speaker 1: of living near mining activity. 97 00:05:43,774 --> 00:05:46,654 Speaker 2: Was that another after shock? Honestly, I can't tell if 98 00:05:46,694 --> 00:05:49,454 Speaker 2: it's mind blasts. Half the time I reckon there was 99 00:05:49,494 --> 00:05:52,814 Speaker 2: another tremor at about eleven felt it at Charlestown too. 100 00:05:53,134 --> 00:05:55,134 Speaker 2: That's at least sixteen since they started. 101 00:05:55,934 --> 00:05:59,054 Speaker 1: But with the location of the quake's epicenter, the arguments 102 00:05:59,094 --> 00:06:03,214 Speaker 1: began over where the mining can cause seismic activity. I 103 00:06:03,294 --> 00:06:05,814 Speaker 1: just wonder how many more artificial earthquakes are going to 104 00:06:05,814 --> 00:06:08,574 Speaker 1: be created from the Hunter Valley's finest mining industry. 105 00:06:08,894 --> 00:06:12,854 Speaker 2: What would you rather the odd rumble or thousands unemployed? 106 00:06:15,014 --> 00:06:17,934 Speaker 1: The Mount Arthur mind quake wasn't the only major tremor 107 00:06:17,934 --> 00:06:21,934 Speaker 1: in Australia these past few days. Over in WA's wheat belts, 108 00:06:21,974 --> 00:06:25,014 Speaker 1: there have been several tremors this last week, the largest 109 00:06:25,094 --> 00:06:29,134 Speaker 1: of four point four magnitude registering in Wildcatchum and felt 110 00:06:29,214 --> 00:06:32,814 Speaker 1: up to two hundred kilometers away. Thirty minutes later, another 111 00:06:32,894 --> 00:06:36,094 Speaker 1: four point one magnitude quake struck the same area, with 112 00:06:36,214 --> 00:06:38,694 Speaker 1: locals told to expect the earth to continue to shake 113 00:06:38,734 --> 00:06:42,414 Speaker 1: for days, maybe even weeks to come. There was also 114 00:06:42,534 --> 00:06:45,974 Speaker 1: a three point zero magnitude earthquake in Victoria's Gippsland region 115 00:06:46,014 --> 00:06:48,694 Speaker 1: on Monday night around eight pm. The center of the 116 00:06:48,694 --> 00:06:51,854 Speaker 1: tremor was at Sandy Point, near Wilson's Promontory and felt 117 00:06:51,894 --> 00:06:55,294 Speaker 1: as far away as Foster Leon, Gather and Inverlock. Just 118 00:06:55,334 --> 00:06:58,214 Speaker 1: three weeks ago, there was a four point seven level 119 00:06:58,254 --> 00:07:01,974 Speaker 1: quake in Victoria's high country. So is this normal or 120 00:07:01,974 --> 00:07:04,534 Speaker 1: do we need to be concerned that Australia's ground it's 121 00:07:04,534 --> 00:07:10,174 Speaker 1: getting a little too shaky. Jonathan Griffin is a senior 122 00:07:10,214 --> 00:07:13,774 Speaker 1: seismologist at Geoscience Australia. Jonathan, just to start, can you 123 00:07:14,174 --> 00:07:16,774 Speaker 1: tell us just how many earthquakes we generally have each 124 00:07:16,854 --> 00:07:17,734 Speaker 1: year here in Australia. 125 00:07:18,214 --> 00:07:22,974 Speaker 2: Yeah, So across Australia we register about one hundred magnitude 126 00:07:23,014 --> 00:07:26,734 Speaker 2: three earthquakes every year, and we get about one or 127 00:07:26,774 --> 00:07:31,054 Speaker 2: two magnitude five earthquakes or greater every year, and we 128 00:07:31,054 --> 00:07:33,854 Speaker 2: get a magnitude six sort of every five to ten 129 00:07:33,974 --> 00:07:35,014 Speaker 2: years on average. 130 00:07:35,654 --> 00:07:39,454 Speaker 1: So those magnitude four point some things that we've experienced 131 00:07:39,494 --> 00:07:42,734 Speaker 1: the last week in Wa and in New South Wales. 132 00:07:43,054 --> 00:07:45,814 Speaker 1: How regularly would we have something like that, And they 133 00:07:45,894 --> 00:07:49,294 Speaker 1: generally in places where we don't register that much of 134 00:07:49,334 --> 00:07:51,494 Speaker 1: an issue because they're away from civilization. 135 00:07:52,254 --> 00:07:55,214 Speaker 2: Yeah, so, as you know, Australia is very sparsely populated. 136 00:07:55,414 --> 00:07:59,334 Speaker 2: Earthquakes can happen anywhere across the continent and therefore they 137 00:07:59,334 --> 00:08:02,174 Speaker 2: often occur where very few people are and maybe aren't 138 00:08:02,214 --> 00:08:04,534 Speaker 2: felt by a lot of people. Certainly, this has been 139 00:08:04,574 --> 00:08:07,614 Speaker 2: a more interesting week than average, with a couple of 140 00:08:07,654 --> 00:08:11,454 Speaker 2: fours over in wa will Cutcham and then the two 141 00:08:11,534 --> 00:08:14,374 Speaker 2: fours New Muscle Brook over the last few days as well. 142 00:08:14,454 --> 00:08:17,654 Speaker 2: So that's not what happens every week, and it's made 143 00:08:17,694 --> 00:08:20,814 Speaker 2: it interesting, certainly to have these two events happening either 144 00:08:20,854 --> 00:08:23,654 Speaker 2: side of the continent. But they're not connected. They're simply 145 00:08:23,694 --> 00:08:26,974 Speaker 2: too far away and the earthquakes aren't big enough or 146 00:08:26,974 --> 00:08:29,774 Speaker 2: close enough to interact with each other. We like to 147 00:08:30,014 --> 00:08:33,134 Speaker 2: draw conclusions that maybe they're linked, but certainly in this 148 00:08:33,214 --> 00:08:33,774 Speaker 2: case they're not. 149 00:08:34,534 --> 00:08:37,094 Speaker 1: Now we've spoken to you about this before, about the 150 00:08:37,134 --> 00:08:40,134 Speaker 1: fact that Australia the continent itself, doesn't really sit on 151 00:08:40,334 --> 00:08:43,054 Speaker 1: any of the major tectonic plates like some other countries do, 152 00:08:43,094 --> 00:08:45,374 Speaker 1: which is why we don't tend to get the very 153 00:08:45,414 --> 00:08:48,134 Speaker 1: big earthquakes, but we do still have fault lines that 154 00:08:48,214 --> 00:08:50,734 Speaker 1: run across the country, right, that's right. 155 00:08:50,894 --> 00:08:54,374 Speaker 2: Australia is a very ancient continent and while it's a 156 00:08:54,534 --> 00:08:57,814 Speaker 2: stable continental area in now so we occupy the interior 157 00:08:58,054 --> 00:09:01,534 Speaker 2: of a techonic plate, the Australia India Plate, and that 158 00:09:01,614 --> 00:09:05,494 Speaker 2: plate is moving north northeast at about seven centimeters a year. 159 00:09:05,614 --> 00:09:09,174 Speaker 2: As it does that, it's crashing into the Pacific Plade 160 00:09:09,254 --> 00:09:12,534 Speaker 2: to the north in pav New Guinea, Indonesia, to the 161 00:09:12,574 --> 00:09:15,934 Speaker 2: east in New Zealand. And it's at those plate boundaries 162 00:09:15,934 --> 00:09:20,174 Speaker 2: where most earthquakes occur and now largest earthquakes occur. But 163 00:09:20,374 --> 00:09:23,214 Speaker 2: despite that, the crashing into other plates at the boundary, 164 00:09:23,294 --> 00:09:27,174 Speaker 2: that causes stresses in the crust of Australia itself. So 165 00:09:27,214 --> 00:09:30,654 Speaker 2: our continent is being squeezed from the plate boundary and 166 00:09:30,694 --> 00:09:33,094 Speaker 2: we have old fault line. You know, in the past, 167 00:09:33,414 --> 00:09:36,214 Speaker 2: as the continent of Australia formed, you had more active 168 00:09:36,254 --> 00:09:39,454 Speaker 2: faults and these faults are still there. There's still weaknesses 169 00:09:39,494 --> 00:09:43,254 Speaker 2: in the crust and by squeezing the crust, those weaknesses 170 00:09:43,254 --> 00:09:45,654 Speaker 2: can fail and that's what causes an earthquake. 171 00:09:46,334 --> 00:09:48,774 Speaker 1: Well can we talk about whether man can actually have 172 00:09:48,814 --> 00:09:51,974 Speaker 1: an impact on when those faults fail, because obviously the 173 00:09:51,974 --> 00:09:56,334 Speaker 1: epicenter of the musclebrook Denman quake was basically in the 174 00:09:56,374 --> 00:09:58,934 Speaker 1: middle of a major coal mine, and a lot of 175 00:09:58,934 --> 00:10:02,574 Speaker 1: conversation has been happening about weather digging up that amount 176 00:10:02,574 --> 00:10:04,854 Speaker 1: of dirt from that one spot, which obviously sits on 177 00:10:04,894 --> 00:10:07,694 Speaker 1: a fault line, has an impact on whether it will 178 00:10:07,694 --> 00:10:10,054 Speaker 1: increase sizemic activity. Could that be the cakes? 179 00:10:10,734 --> 00:10:15,294 Speaker 2: So human activity can induce earthquakes. I was talking before 180 00:10:15,374 --> 00:10:18,574 Speaker 2: how the Australian continent is being stressed by these big 181 00:10:18,654 --> 00:10:21,974 Speaker 2: plate boundary forces. That's sort of the cause of the earthquakes. 182 00:10:22,014 --> 00:10:26,814 Speaker 2: But we can then locally, through various human activities affect 183 00:10:26,854 --> 00:10:31,254 Speaker 2: that the stress field locally around so activities like mining 184 00:10:31,294 --> 00:10:34,134 Speaker 2: where you take a load of rock off the earth, 185 00:10:34,574 --> 00:10:37,774 Speaker 2: or other activities such as filling water reservoirs. You know, 186 00:10:37,854 --> 00:10:40,014 Speaker 2: you add a big load of water on top of 187 00:10:40,214 --> 00:10:43,214 Speaker 2: an area that didn't previously have it. That can locally 188 00:10:43,214 --> 00:10:46,934 Speaker 2: affect the stress field and it can induce earthquakes to happen. 189 00:10:47,134 --> 00:10:49,854 Speaker 2: And we've seen that around the world, both in terms 190 00:10:49,894 --> 00:10:54,134 Speaker 2: of mining, you know, water reservoirs, and also sometimes hydraulic fracking. 191 00:10:54,494 --> 00:10:57,414 Speaker 2: So there's all these mechanisms that I sort of known 192 00:10:57,454 --> 00:11:01,054 Speaker 2: to induce earthquakes. What's really difficult is when any particular 193 00:11:01,134 --> 00:11:04,294 Speaker 2: earthquake happens like this one, to actually say yes, it 194 00:11:04,374 --> 00:11:07,014 Speaker 2: was caused by mining or no it wasn't. To do that, 195 00:11:07,054 --> 00:11:10,854 Speaker 2: you sort of need really higher level monitoring, seismic monitoring, 196 00:11:11,054 --> 00:11:15,374 Speaker 2: lots of instruments closely around where these earthquakes occurred. Certainly 197 00:11:15,414 --> 00:11:17,734 Speaker 2: a GEOSUNS Australia where you run a national network that 198 00:11:17,814 --> 00:11:21,654 Speaker 2: just doesn't have the resolution to do that. So, you know, 199 00:11:21,734 --> 00:11:24,374 Speaker 2: while we can say that, you know, there's been plenty 200 00:11:24,414 --> 00:11:26,654 Speaker 2: of earthquakes over the years in the Hunter Valley, and 201 00:11:26,694 --> 00:11:29,134 Speaker 2: it's certainly possible that at least some of them have 202 00:11:29,214 --> 00:11:32,294 Speaker 2: been induced by mining, what we can't do is go 203 00:11:32,374 --> 00:11:34,814 Speaker 2: and point to any particular event like these ones that 204 00:11:34,894 --> 00:11:37,294 Speaker 2: happened over the weekend and yes, they definitely were due 205 00:11:37,334 --> 00:11:37,774 Speaker 2: to mining. 206 00:11:38,534 --> 00:11:40,494 Speaker 1: A lot of the conversation that's been happening around here too, 207 00:11:40,574 --> 00:11:44,054 Speaker 1: is that, in fact, there's no coincidence that mines end 208 00:11:44,134 --> 00:11:46,734 Speaker 1: up being quite near or even on top of fault lines, 209 00:11:46,774 --> 00:11:50,574 Speaker 1: because that seismic activity creates a lot of geological wondrous 210 00:11:50,574 --> 00:11:53,734 Speaker 1: things to happen, like coal seams or gold seams or 211 00:11:53,814 --> 00:11:57,014 Speaker 1: many other different things. So it's not a coincidence, and 212 00:11:57,094 --> 00:11:59,054 Speaker 1: that some minds will line up with fault lines. 213 00:11:58,894 --> 00:12:02,694 Speaker 2: Right, yes, exactly right. So the great example is Calgoley 214 00:12:02,734 --> 00:12:06,374 Speaker 2: over in Wa a mass evolved fault zone, and all 215 00:12:06,414 --> 00:12:09,534 Speaker 2: the gold mineralization has happened along that. The coal mine 216 00:12:09,814 --> 00:12:13,014 Speaker 2: in the Hunter Valley are less, you know, the coals 217 00:12:13,054 --> 00:12:15,414 Speaker 2: not formed by faulting in the same way, it's the 218 00:12:15,414 --> 00:12:19,454 Speaker 2: accumulation of plants essentially over long periods of time. But 219 00:12:19,534 --> 00:12:22,694 Speaker 2: certainly that's true that some of our major minds are 220 00:12:22,734 --> 00:12:25,254 Speaker 2: located on very old faults, and so you do have 221 00:12:25,374 --> 00:12:28,774 Speaker 2: the kind of potentially weaknesses there that can fail again. 222 00:12:29,294 --> 00:12:32,294 Speaker 1: Now, in the case of the Wa quake near while 223 00:12:32,374 --> 00:12:34,294 Speaker 1: Catchum and the one in the Hunter Valley, or the 224 00:12:34,334 --> 00:12:36,814 Speaker 1: two big ones really in the Hunter Valley, there have 225 00:12:36,894 --> 00:12:39,894 Speaker 1: been maybe even dozens of after shocks now and it's 226 00:12:40,174 --> 00:12:43,414 Speaker 1: days and days later. How long do after shocks generally 227 00:12:43,454 --> 00:12:45,334 Speaker 1: tend to go for? Is there any period of time 228 00:12:45,374 --> 00:12:46,814 Speaker 1: that you can say, okay, now was sort of out 229 00:12:46,854 --> 00:12:47,494 Speaker 1: of that period? 230 00:12:48,294 --> 00:12:52,294 Speaker 2: So after shots over time they tend to get smaller 231 00:12:52,294 --> 00:12:56,414 Speaker 2: in magnitude and happen less frequently. What we do see 232 00:12:56,414 --> 00:12:59,254 Speaker 2: in Australia is that some of our aftershot sequences do 233 00:12:59,374 --> 00:13:02,494 Speaker 2: last for quite a long time. So some of your 234 00:13:02,534 --> 00:13:06,294 Speaker 2: listeners may remember our largest earthquake to occur since we've 235 00:13:06,294 --> 00:13:08,534 Speaker 2: been recording them, what was the main Stift six point 236 00:13:08,534 --> 00:13:11,694 Speaker 2: six tenant Creaker quake that happened in nineteen eighty eight. 237 00:13:11,854 --> 00:13:14,814 Speaker 2: Now we still get aftershocks from that event happening today 238 00:13:14,894 --> 00:13:17,014 Speaker 2: every now and then, not be a mainitude three or 239 00:13:17,054 --> 00:13:19,934 Speaker 2: something that pops off in the same location. So in 240 00:13:19,974 --> 00:13:22,294 Speaker 2: some areas they can last for a very long time. 241 00:13:22,454 --> 00:13:25,854 Speaker 2: They seem to decay off more quickly in Eastern Australia, 242 00:13:25,894 --> 00:13:29,054 Speaker 2: which is geologically a bit younger, but certainly if you're 243 00:13:29,054 --> 00:13:31,734 Speaker 2: listening to remember the wolds Point earthquake in Victoria and 244 00:13:31,814 --> 00:13:34,374 Speaker 2: in twenty twenty one that gave Melbourne a really good shake. 245 00:13:34,854 --> 00:13:38,534 Speaker 2: We're still seeing aftershocks from that event occasionally now as well. 246 00:13:38,614 --> 00:13:41,894 Speaker 2: So while most of them happen in the days and 247 00:13:41,934 --> 00:13:45,134 Speaker 2: weeks after the main shock, we can see those sequences 248 00:13:45,174 --> 00:13:46,134 Speaker 2: go on for quite some time. 249 00:13:47,054 --> 00:13:48,934 Speaker 1: Just finally, Jonathan, we don't want to scare anyone, but 250 00:13:49,414 --> 00:13:51,334 Speaker 1: is there any way to map out where we presume 251 00:13:51,414 --> 00:13:55,494 Speaker 1: or predict the next biggest earthquake might be depending on 252 00:13:55,574 --> 00:13:58,094 Speaker 1: what seismic activity has been happening in recent times. 253 00:13:58,974 --> 00:14:02,974 Speaker 2: So we can't predict earthquakes. At Geoscience Australia we produce 254 00:14:03,054 --> 00:14:07,894 Speaker 2: the National Seismic Hazard Assessment, which is basically a model 255 00:14:07,894 --> 00:14:11,214 Speaker 2: of where we think earthquakes could happen in the future 256 00:14:11,654 --> 00:14:14,414 Speaker 2: and what the ground shaking from that would be. And 257 00:14:14,414 --> 00:14:16,894 Speaker 2: that's the kind of information that can then be used 258 00:14:16,894 --> 00:14:21,334 Speaker 2: to design buildings and other infrastructure to be resilient to 259 00:14:21,414 --> 00:14:23,614 Speaker 2: the level of shaking that we think we might see. 260 00:14:23,854 --> 00:14:26,414 Speaker 2: As I said, we can't predict earthquakes. We do know 261 00:14:26,814 --> 00:14:29,414 Speaker 2: that we get aftershot sequences, So where you have had 262 00:14:29,534 --> 00:14:32,974 Speaker 2: an earthquake, chances are you're going to get more earthquakes 263 00:14:32,974 --> 00:14:35,574 Speaker 2: happening over the next little while we'd expect more will 264 00:14:35,614 --> 00:14:37,774 Speaker 2: happen in a muscle brook and while catch them. After 265 00:14:37,814 --> 00:14:42,374 Speaker 2: these events, typically they get smaller over time, but occasionally 266 00:14:42,454 --> 00:14:47,894 Speaker 2: you get a bigger one occurring as well. 267 00:14:47,934 --> 00:14:50,454 Speaker 1: According to the Smart Traveler website, if you do find 268 00:14:50,454 --> 00:14:52,974 Speaker 1: yourself in the midst of an earthquake, the advice is 269 00:14:53,014 --> 00:14:54,934 Speaker 1: to drop down to the floor on your hands and knees, 270 00:14:55,174 --> 00:14:57,494 Speaker 1: cover your head and neck, or hop under something that 271 00:14:57,494 --> 00:14:59,894 Speaker 1: can shield you from falling debris, like a table, But 272 00:15:00,054 --> 00:15:03,254 Speaker 1: move around as little as possible. Stay calm, stay away 273 00:15:03,254 --> 00:15:08,174 Speaker 1: from windows, and stay inside until the shaking stops. Injuries 274 00:15:08,214 --> 00:15:10,294 Speaker 1: can happen if people move around too soon and the 275 00:15:10,294 --> 00:15:13,694 Speaker 1: shaking hasn't quite finished or things haven't stopped moving and falling. 276 00:15:14,654 --> 00:15:17,214 Speaker 1: Use stairs rather than an elevator when you do go 277 00:15:17,254 --> 00:15:20,214 Speaker 1: to leave the building, as earthquakes do tend to cut power. 278 00:15:20,814 --> 00:15:23,054 Speaker 1: If you're outside, you're told to lie on the ground 279 00:15:23,134 --> 00:15:25,254 Speaker 1: or drop to your hands and knees, cover your head 280 00:15:25,254 --> 00:15:27,894 Speaker 1: and neck, and stay away from buildings, power lines, or 281 00:15:27,934 --> 00:15:31,174 Speaker 1: street lights if you can. If you're driving, pull over 282 00:15:31,214 --> 00:15:34,374 Speaker 1: and avoid bridges or overpasses if possible. Stay in your 283 00:15:34,374 --> 00:15:37,054 Speaker 1: car with your seat belt on until the shaking stops. 284 00:15:37,494 --> 00:15:39,134 Speaker 1: If you are in your car and a power line 285 00:15:39,174 --> 00:15:42,214 Speaker 1: comes down, don't get out, wait till someone comes to help. 286 00:15:43,254 --> 00:15:46,374 Speaker 1: If you're driving somewhere mountainous, look out for falling rocks 287 00:15:46,494 --> 00:15:50,094 Speaker 1: or landslides. Now, lucky for us, we won't get the 288 00:15:50,254 --> 00:15:52,734 Speaker 1: big shakes like they do in places where the tectonic 289 00:15:52,774 --> 00:15:55,694 Speaker 1: plates meet, but it's better to be safe than sorry. 290 00:15:56,574 --> 00:15:58,814 Speaker 1: Thanks for taking some time to feed your mind today. 291 00:15:59,014 --> 00:16:01,654 Speaker 1: The quickie is produced by me Claire Murphy and our 292 00:16:01,694 --> 00:16:05,094 Speaker 1: senior producer Taylor Strato, with audio production by tomline 293 00:16:14,774 --> 00:16:17,134 Speaker 2: A Speci