Latest news with #InternationalSeismologicalCentre
Yahoo
24-04-2025
- Science
- Yahoo
Scientists Spotted Signs of a Hidden Structure Inside Earth's Core
While most of us take the ground beneath our feet for granted, written within its complex layers, like the pages of a book, is Earth's history. Our history. Research shows there are little-known chapters in that history, deep within Earth's past. In fact, Earth's inner core appears to have another even more inner core within it. "Traditionally we've been taught the Earth has four main layers: the crust, the mantle, the outer core and the inner core," Australian National University geophysicist Joanne Stephenson explained in 2021. Our knowledge of what lies beneath Earth's crust has been inferred mostly from what volcanoes have divulged and what seismic waves have whispered. From these indirect observations, scientists have calculated that the scorchingly hot inner core, with temperatures surpassing 5,000 degrees Celsius (9,000 Fahrenheit), makes up only 1 percent of Earth's total volume. But a few years ago, Stephenson and colleagues found evidence Earth's inner core may actually have two distinct layers. "It's very exciting – and might mean we have to re-write the textbooks!" Stephenson explained at the time. The team used a search algorithm to trawl through and match thousands of models of the inner core with observed data across many decades about how long seismic waves take to travel through Earth, gathered by the International Seismological Centre. Differences in seismic wave paths through layers of Earth. (Stephenson et al., Journal of Geophysical Research: Solid Earth, 2021) So what's down there? The team looked at some models of the inner core's anisotropy – how differences in the make-up of its material alters the properties of seismic waves – and found some were more likely than others. While some models suggest the material of the inner core channels seismic waves faster parallel to the equator, others indicate the mix of materials allows for faster waves more parallel to Earth's rotational axis. Even then, there are arguments about the exact degree of difference at certain angles. The study here didn't show much variation with depth in the inner core, but it did find there was a change in the slow direction to a 54-degree angle, with the faster direction of waves running parallel to the axis. "We found evidence that may indicate a change in the structure of iron, which suggests perhaps two separate cooling events in Earth's history," Stephenson said. "The details of this big event are still a bit of a mystery, but we've added another piece of the puzzle when it comes to our knowledge of the Earth's inner core." These findings may explain why some experimental evidence has been inconsistent with our current models of Earth's structure. The presence of an innermost layer has been suspected before, with hints that iron crystals that compose the inner core have different structural alignments. "We are limited by the distribution of global earthquakes and receivers, especially at polar antipodes," the team writes in their paper, explaining the missing data decreases the certainty of their conclusions. But their conclusions align with other studies on the anisotropy of the innermost inner core. Future research may fill in some of these data gaps and allow scientists to corroborate or contradict their findings, and hopefully translate more stories written within this early layer of Earth's history. This research was published in the Journal of Geophysical Research. An earlier version of this article was published in March 2021. 'Bone Collector' Caterpillar Wears Dead Bugs to Steal Prey From Spiders 113 Million-Year-Old 'Hell Ant' Discovery Is Oldest Ever Found Most Bees Nest in The Ground. Offering Rocks And Gravel Is a Simple Way to Help Them Thrive.
Times of Oman
28-03-2025
- Climate
- Times of Oman
Six earthquakes in a day rock Myanmar
As per the NCS, the latest earthquake occurred at a depth of 10km, making it susceptible to aftershocks. "EQ of M: 4.3, On: 28/03/2025 15:25:39 IST, Lat: 19.43 N, Long: 95.47 E, Depth: 10 Km, Location: Myanmar," NCS stated in a post on X. Another earthquake of 4.4 magnitude on the Richter Scale occurred at a shallow depth of 10km. "EQ of M: 4.4, On: 28/03/2025 14:48:32 IST, Lat: 23.35 N, Long: 95.31 E, Depth: 10 Km, Location: Myanmar," NCS said in a post on X. Another earthquake of magnitude 4.9 occurred at a depth of 30km. "EQ of M: 4.9, On: 28/03/2025 13:07:03 IST, Lat: 22.55 N, Long: 95.34 E, Depth: 30 Km, Location: Myanmar." NCS reported that an earthquake of magnitude 5.0 occurred in the region as a result of the aftershock of previous earthquakes. "EQ of M: 5.0, On: 28/03/2025 12:57:53 IST, Lat: 22.97 N, Long: 95.56 E, Depth: 10 Km, Location: Myanmar," NCS stated. An earthquake of magnitude 7.0 occurred in the region at 12 pm, at a depth of 10km, as per NCS. "EQ of M: 7.0, On: 28/03/2025 12:02:07 IST, Lat: 21.41 N, Long: 95.43 E, Depth: 10 Km, Location: Myanmar," NCS stated on X. Prior to this, a powerful earthquake of 7.2 magnitude rocked the region. "EQ of M: 7.2, On: 28/03/2025 11:50:52 IST, Lat: 21.93 N, Long: 96.07 E, Depth: 10 Km, Location: Myanmar," as per NCS. Shallow earthquakes like these are more dangerous than deeper ones due to their greater energy release closer to the Earth's surface, causing stronger ground shaking and increased damage to structures and casualties, compared to deeper earthquakes, which lose energy as they travel to the surface. Although Myanmar is an earthquake-prone country, an official national seismic hazard map has not been proposed. Due to the collision between the Eurasian and Indo-Australian plates, Myanmar has a high seismic hazard level. According to the earthquake parameters summarized by the International Seismological Centre, around 140 events with magnitude greater than or equal to 3.0 have taken place in Myanmar and its vicinity every year from 1990 to it is evident that Myanmar is vulnerable to hazards from moderate and large magnitude earthquakes, including tsunami hazards along its long coastline. The Sagaing Fault elevates the seismic hazard for Sagaing, Mandalay, Bago, and Yangon, which together represent 46 per cent of the population of Myanmar. Although Yangon is relatively far from the fault trace, it still suffers from significant risk due to its dense population. For instance, in 1903, an intensive earthquake with magnitude 7.0 that occurred in Bago also struck Yangon.
