Southeast Asia Earthquake Tracker โ Live Earthquakes
By Paul Harrison | Founder & Publisher, Orbis Weather
Southeast Asia Earthquakes This Week: Friday, October 23, 2026
ยท @Paul
By Paul Harrison, Orbis Weather
It was a moderate week for earthquakes in Southeast Asia, with no quake reaching magnitude 5.5 and no tsunami. The strongest shaking came on Sunday, 18 October, at 16:00 WITA, off the north coast of Flores. BMKG first measured it at magnitude 5.3, later revised to 5.1; USGS put it at 5.2. It was felt at intensity IV to V in Manggarai and is part of the aftershock sequence of the magnitude 7.7 Flores earthquake of 15 August.
USGS also recorded a magnitude 5.2 quake off Northern Samar in the Philippines on Wednesday, 21 October, which PHIVOLCS measured at 4.8. Other felt quakes struck off Aceh, in the Banda Sea and beneath Bengkulu. BMKG ruled out a tsunami for every magnitude 5 event, and no damage or casualties were reported. This report is current to 05:58 WIB (Jakarta, Bangkok) and 06:58 WITA/PHT (Makassar, Manila, Singapore) on Friday, 23 October, which is 18:58 EDT on Thursday, 22 October.
Key facts
Item | Figure | Source |
|---|---|---|
Period covered | 00:00 UTC Fri 16 Oct to 22:58 UTC Thu 22 Oct 2026 | USGS query |
Quakes of magnitude 4.5+ | 17 (by USGS place name: 11 Indonesia, 4 Philippines, 2 Timor-Leste) | USGS |
Largest by USGS | M5.2 twice: off Flores (18 Oct) and off Northern Samar (21 Oct) | USGS |
Largest by BMKG | M5.4 off Aceh (20 Oct), revised to M5.1; Lebong M5.2 (22 Oct) unrevised | BMKG |
Largest in the Philippines | M5.1 off Baganga, Davao Oriental (16 Oct) | PHIVOLCS |
Strongest shaking | Intensity IVโV in Manggarai, Flores (18 Oct) | BMKG |
Tsunami | None; BMKG modelling showed no tsunami potential | BMKG |
Deaths or damage | None reported | BMKG, PHIVOLCS via news |
Latest felt quake | M5.2, Lebong, Bengkulu, 22 Oct, 17:57 WIB | BMKG |
This week’s earthquakes of magnitude 4.5 and above
USGS recorded 17 quakes of magnitude 4.5 or more in the search box; the 15 largest are listed, newest first.
Local date and time | USGS mag. | USGS location (area) | Depth |
|---|---|---|---|
Thu 22 Oct, 17:57 WIB | 4.9 | 85 km NNW of Curup, Indonesia (Lebong, Bengkulu) | 135 km |
Wed 21 Oct, 16:37 PHT | 5.2 | 68 km NE of Cabatuan, Philippines (sea off Northern Samar) | 10 km |
Wed 21 Oct, 16:44 WIT | 5.1 | 164 km NE of Lospalos, Timor Leste (Banda Sea, Maluku Barat Daya) | 123 km |
Tue 20 Oct, 23:29 WIB | 5.0 | 21 km SW of Meulaboh, Indonesia (off West Aceh) | 76 km |
Tue 20 Oct, 14:04 PHT | 4.6 | 7 km SE of San Julian, Philippines (Eastern Samar) | 10 km |
Mon 19 Oct, 20:06 WITA | 4.8 | 56 km N of Ruteng, Indonesia (sea north of Flores) | 10 km |
Mon 19 Oct, 18:10 WITA | 4.7 | 53 km NNE of Labuan Bajo, Indonesia (sea north of Flores) | 10 km |
Mon 19 Oct, 18:00 WIT | 4.7 | 163 km WNW of Tobelo, Indonesia (North Maluku waters) | 49 km |
Mon 19 Oct, 17:45 WITA | 4.9 | 54 km NE of Labuan Bajo, Indonesia (sea north of Flores) | 10 km |
Sun 18 Oct, 16:00 WITA | 5.2 | 55 km NNW of Ruteng, Indonesia (sea north of Flores) | 10 km |
Sat 17 Oct, 20:46 WITA | 4.6 | 70 km W of Tambolaka, Indonesia (sea west of Sumba) | 69 km |
Sat 17 Oct, 18:07 UTC+9 | 4.6 | 51 km N of Pante Makasar, Timor Leste (sea north of Oecusse) | 91 km |
Sat 17 Oct, 15:20 WITA | 4.5 | 59 km NNW of Ruteng, Indonesia (sea north of Flores) | 10 km |
Fri 16 Oct, 20:18 PHT | 4.7 | 10 km SE of Lamitan, Philippines (Davao Occidental) | 10 km |
Fri 16 Oct, 17:13 PHT | 4.9 | 31 km ENE of Kinablangan, Philippines (off Davao Oriental) | 74 km |
Not shown: two magnitude 4.5 events, in the Banda Sea (Mon 19 Oct, 15:15 WIT) and 142 km SSW of Abepura, Papua (Tue 20 Oct, 22:27 WIT). Source: USGS query, run at 22:58 UTC on 22 October. Times are local: WIB is UTC+7, WITA and PHT are UTC+8, WIT and Timor-Leste time are UTC+9.
The week’s notable quakes
Flores Sea, East Nusa Tenggara (18โ19 October). BMKG recorded a magnitude 5.3 quake at 16:00 WITA on Sunday, 18 October, 10 km deep. Its press release revised this to magnitude 5.1, at sea 53 km northwest of Ruteng, Manggarai. BMKG called it a shallow thrust-fault quake caused by the Flores Back-arc Thrust. Its felt list shows intensity IVโV in Manggarai and III in West Manggarai; its shaking model gave IV at Macang Pacar and Reok. BMKG said that, as of 18 October, 22,097 aftershocks of the 15 August magnitude 7.7 Flores earthquake had been recorded, the largest magnitude 6.2. Three more felt quakes followed on 19 October, of magnitude 4.8, 4.7 and 4.5 by BMKG, felt weakly (intensity IโII) in Manggarai. USGS measured the 18 October quake at 5.2.
Off Northern Samar, Philippines (21 October). PHIVOLCS located a magnitude 4.8 quake at 4:37 p.m. PHT, 108 km N 41ยฐ E of Mapanas. Its catalogue lists a depth of 57 km, while news reports citing PHIVOLCS gave 31 km. EFE reported that PHIVOLCS first estimated magnitude 5.0. Intensity I was felt in Gamay, and PHIVOLCS expected no damage or aftershocks. USGS measured magnitude 5.2 at 10 km depth.
Off West Aceh, Sumatra (20 October). BMKG first reported magnitude 5.4 at 23:29 WIB, 74 km deep, then updated it to magnitude 5.1 at 56 km, 55 km southwest of Meulaboh. BMKG attributed it to subduction, with thrust faulting. It was felt at intensity IIIโIV in West Aceh, Southwest Aceh and Nagan Raya, and IIโIII in Banda Aceh. BMKG had detected no aftershocks by 23:50 WIB. USGS gave magnitude 5.0 at 76 km.
Lebong, Bengkulu (22 October). BMKG recorded magnitude 5.2 at 17:57 WIB, updated to 113 km deep, on land 13 km northwest of Lebong. BMKG described an intermediate-depth, strike-slip quake from deformation inside the sinking plate (“intra-slab”). Residents reported intensity III in Bengkulu city, Arga Makmur and Curup. USGS measured magnitude 4.9 at 135 km.
Banda Sea, Maluku (21 October). BMKG first measured magnitude 5.1 at 16:44 WIT, then revised it to 4.9 at 90 km, 58 km northeast of Maluku Barat Daya. It called the quake an intermediate-depth, oblique-thrust subduction event, felt at intensity III on Moa and Lakor islands. USGS gave magnitude 5.1 at 123 km.
PHIVOLCS also listed a magnitude 5.1 quake 73 km N 59ยฐ E of Baganga, Davao Oriental, at 5:13 p.m. PHT on 16 October (USGS: 4.9). USGS recorded nothing of magnitude 4.0 or more in the Andaman Sea, Thailand, Malaysia, Singapore, Brunei, Cambodia or Laos. On the mainland, it listed a magnitude 4.4 quake 33 km southeast of Sฦกn La, Vietnam (06:59 ICT, UTC+7, on 19 October), and a magnitude 4.4 at 21:08 UTC on 17 October, described as 66 km WSW of Nuofu, China. Timor-Leste had only offshore events, listed in the table above.
Damage, casualties and tsunami status
No deaths, injuries or building damage were reported this week. For the West Aceh quake, Journalist Independent reported on 21 October that there was “no verified information yet” on casualties or damage. For the Northern Samar quake, EFE reported on 21 October that PHIVOLCS ruled out damage. BMKG’s tsunami modelling showed no tsunami potential for any of its four magnitude 5 events, and no tsunami warning was issued.
Why Southeast Asia has so many earthquakes
This week’s quakes trace the region’s plate boundaries. Off Sumatra, the Indo-Australian plate sinks beneath the Eurasian plate along the Sunda megathrust, which runs about 5,500 km from Myanmar to near Australia; BMKG linked the Aceh quake to this subduction. Beneath Bengkulu and the Banda Sea, quakes occurred inside the sinking plate itself, at intermediate depth. North of Flores, BMKG tied the quakes to the Flores Back-arc Thrust, the fault behind the 15 August earthquake. East of the Philippines lies the Philippine Trench, about 1,320 km long. USGS classes quakes 0โ70 km deep as shallow, 70โ300 km as intermediate and 300โ700 km as deep.
What to watch
- Flores aftershocks: the sequence from the 15 August earthquake remains active, with five felt quakes north of Flores this week alone.
- Aftershocks elsewhere: BMKG advised residents to be wary of possible aftershocks after the Lebong quake and to avoid cracked buildings.
- Volcanic earthquakes: PHIVOLCS logged 5โ9 volcanic earthquakes a day at Kanlaon and 4โ14 a day at Mayon, both at Alert Level 2, according to the Smithsonian weekly report for 15โ21 October.
- Context: USGS recorded two quakes of magnitude 5.5 or more in the region in the previous four weeks: 5.9 near Tambolaka, Sumba (4 October) and 5.5 near Burias, Philippines (8 October).
- Official channels: BMKG (bmkg.go.id, warning.bmkg.go.id) in Indonesia and PHIVOLCS in the Philippines issue the official alerts. No agency can predict earthquakes.
About this article
This article summarises agency data and news reports; it is not an official warning. The week runs from 00:00 UTC on Friday, 16 October, to the USGS query at 22:58 UTC on Thursday, 22 October, within 12ยฐSโ29ยฐN and 91ยฐEโ142ยฐE. Agencies use different stations and methods, so their magnitudes and depths differ. BMKG publishes automatic figures within minutes and revises them in a press release; this week it lowered three of its four magnitude 5 readings.
Term | Meaning |
|---|---|
Magnitude | The size of a quake. Each whole number means about 32 times more energy released (USGS). |
Intensity (MMI) | How strongly shaking is felt at a place, in Roman numerals; it varies with distance. III is felt indoors like a passing truck. |
Epicentre | The point on the surface directly above where the quake starts. |
Aftershock | A smaller quake that follows a larger one in the same area. |
Subduction | One tectonic plate sinking beneath another, as along the Sunda megathrust. |
Frequently asked questions
What was the strongest earthquake in Southeast Asia this week? USGS measured two quakes at magnitude 5.2: off Flores on 18 October and off Northern Samar on 21 October. BMKG’s highest first reading was 5.4 off West Aceh, later revised to 5.1.
Was there a tsunami warning? No. BMKG’s modelling showed no tsunami potential for any of its magnitude 5 quakes, and none caused a tsunami.
Why do BMKG, PHIVOLCS and USGS give different magnitudes? Each agency uses its own stations and methods. BMKG also revises its first automatic figures; this week the Flores quake went from 5.3 to 5.1.
Are the Flores quakes still aftershocks of the August earthquake? BMKG placed the 18 October quake in the sequence of the 15 August magnitude 7.7 Flores earthquake. By 18 October it had counted 22,097 aftershocks.
Can these earthquakes be predicted? No. Agencies can describe where quakes are common and expect aftershocks after a large event, but cannot forecast the time or size of a specific quake.
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Official Sources
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๐ Southeast Asia Earthquake Tracker โ Live Earthquakes
Monitor earthquakes across Indonesia, the Philippines, Myanmar, Malaysia, Singapore, Thailand, Vietnam and surrounding areas with the Orbis Weather Southeast Asia Earthquake Tracker.
Southeast Asia lies within one of the most geologically active regions on Earth. Powerful tectonic forces surrounding Indonesia and the Philippines regularly produce earthquakes, volcanic activity and, in some circumstances, tsunamis.
The Orbis Weather tracker provides a regional view of significant earthquake activity, including recent M4.0+ earthquakes, stronger events and earthquakes carrying tsunami-related flags in the source data.
Earthquake parameters can be revised as seismic agencies analyze additional information, so always consult national authorities for official earthquake and tsunami warnings.
๐ Why Southeast Asia Has So Many Earthquakes
Southeast Asia sits near the boundaries of several major and smaller tectonic plates.
These enormous sections of Earth’s crust move slowly relative to one another.
Where plates collide, slide past each other or one plate descends beneath another, stress can accumulate in the Earth’s crust.
When that stress is suddenly released, an earthquake occurs.
Indonesia and the Philippines are particularly active because they lie along complicated plate boundaries associated with the broader Pacific Ring of Fire.
๐ฅ What Is the Pacific Ring of Fire?
The Pacific Ring of Fire is a vast zone of earthquakes and volcanoes surrounding much of the Pacific Ocean.
It extends through areas including New Zealand, Indonesia, the Philippines, Japan, Russia, Alaska and the western coasts of North and South America.
Many of the world’s active volcanoes and powerful earthquakes occur within this broad tectonic region.
Indonesia and the Philippines form important parts of this system.
๐ฎ๐ฉ Why Indonesia Has So Many Earthquakes
Indonesia is one of the most earthquake-prone countries in the world.
The country sits at the meeting point of several tectonic systems, including major subduction zones.
Along a subduction zone, one tectonic plate is forced beneath another.
These boundaries can produce powerful earthquakes when accumulated tectonic stress is suddenly released.
Indonesia’s geography โ thousands of islands spread across several active tectonic zones โ means earthquake activity can occur from Sumatra and Java through Sulawesi, the Banda Sea, Maluku and Papua.
๐ต๐ญ Earthquakes in the Philippines
The Philippines is also highly seismically active.
The country lies between major tectonic systems and contains numerous active faults and offshore trenches.
Earthquakes can occur beneath the islands or offshore.
Some offshore earthquakes may require tsunami evaluation depending on their magnitude, depth, location and fault movement.
As in Indonesia, earthquake risk varies considerably between different parts of the country.
๐ฒ๐ฒ Earthquakes in Myanmar
Myanmar has a different but still important tectonic setting.
One of its major geological features is the Sagaing Fault, a large strike-slip fault extending through much of the country.
Strike-slip faults occur where blocks of Earth’s crust move primarily horizontally past each other.
Significant earthquakes along active faults can cause intense ground shaking, particularly near populated areas.
๐ธ๐ฌ Can Singapore Experience Earthquakes?
Singapore has a much lower local earthquake hazard than Indonesia or the Philippines because it is not located directly on a major active plate boundary.
However, powerful earthquakes in Sumatra can sometimes produce noticeable shaking in Singapore.
Shaking may be particularly noticeable to occupants of taller buildings.
This does not mean Singapore has suddenly become the epicenter of an earthquake. Seismic waves from sufficiently powerful regional earthquakes can travel considerable distances.
๐ฒ๐พ Earthquakes and Malaysia
Much of Peninsular Malaysia has relatively low seismicity compared with neighboring Indonesia.
However, earthquakes in Sumatra can sometimes be felt across parts of Malaysia.
East Malaysia is closer to more active tectonic regions, and Sabah in particular has experienced damaging earthquakes.
Regional earthquake monitoring is therefore relevant even in countries that experience fewer major local earthquakes.
๐น๐ญ Earthquakes in Thailand
Thailand is not as seismically active as Indonesia, but earthquake hazards still exist.
Northern and western Thailand contain active faults, while powerful earthquakes in neighboring Myanmar can produce shaking across the border.
Earthquake risk should therefore not be considered zero simply because major events occur less frequently.
๐ป๐ณ Earthquakes in Vietnam
Vietnam generally experiences less earthquake activity than Indonesia or the Philippines, but earthquakes do occur.
Northern Vietnam and other areas contain active fault systems capable of producing seismic activity.
Offshore earthquakes elsewhere in the region may also be relevant when evaluating tsunami hazards.
๐ What Does Earthquake Magnitude Mean?
Magnitude measures the size of an earthquake at its source.
The scale is logarithmic rather than linear.
That means the difference between a magnitude 5 and magnitude 6 earthquake is much more substantial than the numbers might suggest.
Each whole-number increase represents approximately 32 times more energy release.
A magnitude 6 earthquake therefore releases roughly 32 times as much energy as a magnitude 5 earthquake.
Magnitude alone does not determine how destructive an earthquake will be.
๐ What Is an Earthquake Epicenter?
The earthquake begins underground at a location known as the hypocenter, or focus.
The epicenter is the point on Earth’s surface directly above that underground source.
Maps generally display the epicenter because it provides a convenient geographic location for the earthquake.
The strongest shaking does not necessarily occur exactly at that point.
Local geology, fault rupture direction, building construction and earthquake depth can all influence shaking.
โฌ๏ธ Why Earthquake Depth Matters
Earthquakes can occur at very different depths.
A shallow earthquake places the source of seismic energy closer to the surface and can therefore produce strong shaking near the epicenter.
Deeper earthquakes may be felt across larger areas but often produce less intense surface shaking near their epicenters than a similarly sized shallow event.
Southeast Asia experiences both shallow and very deep earthquakes because of its complex subduction zones.
โ ๏ธ What Does M4.0+ Mean on the Orbis Tracker?
The Orbis Weather regional tracker focuses primarily on earthquakes of magnitude 4.0 and above.
This helps prevent the map from becoming overwhelmed by the very large number of small earthquakes detected across such an active region.
Many M4-range earthquakes cause little or no damage.
The effects of any earthquake depend on magnitude, depth, distance from populated areas, local ground conditions and construction quality.
๐ด What Does an M6.0+ Earthquake Mean?
Magnitude 6 and larger earthquakes deserve increased attention because they have greater potential to produce damaging shaking.
That does not mean every M6 earthquake will cause a disaster.
A deep M6 earthquake far offshore may have relatively limited effects, while a shallow earthquake close to a densely populated city can be considerably more dangerous.
Location and depth always matter.
๐ Can Southeast Asian Earthquakes Cause Tsunamis?
Yes.
Southeast Asia contains several tectonic zones capable of generating tsunamis.
However, not every large earthquake produces a tsunami.
A damaging tsunami generally requires substantial displacement of ocean water. Large, shallow earthquakes beneath or near the ocean are therefore of particular concern when they involve vertical seafloor movement.
Indonesia’s BMKG operates earthquake and tsunami-warning services and publishes tsunami-related earthquake information.
๐ What Does the Tsunami Flag Mean?
The Orbis tracker identifies USGS events carrying a tsunami flag.
This requires careful interpretation.
A tsunami flag does not mean a destructive tsunami is heading toward every coastline.
It indicates that the earthquake has tsunami-related significance within the source data.
The Orbis page already correctly warns readers that official tsunami warnings and local emergency instructions should be used for large or shallow offshore earthquakes.
Keep that warning exactly in spirit.
๐ Why Offshore Earthquake Location Matters
A powerful earthquake beneath land cannot directly displace a large body of seawater in the same way as an undersea earthquake.
For tsunami generation, the type of fault movement is also important.
A large undersea earthquake involving substantial vertical displacement of the seafloor can suddenly move the water above it.
That disturbance can generate tsunami waves traveling away from the source.
Scientists therefore examine much more than magnitude when assessing tsunami potential.
๐ The 2004 Indian Ocean Tsunami
Southeast Asia’s earthquake risk was tragically demonstrated by the December 2004 Sumatra-Andaman earthquake and Indian Ocean tsunami.
The enormous undersea earthquake off northern Sumatra generated a devastating tsunami affecting coastlines around the Indian Ocean.
The disaster fundamentally changed tsunami awareness and contributed to major improvements in regional warning and monitoring systems.
It also demonstrated why people living near tsunami-prone coastlines should understand natural warning signs and official evacuation procedures.
๐ Earthquakes and Volcanoes
Indonesia and the Philippines experience both frequent earthquakes and volcanic eruptions because the same broad tectonic processes contribute to both hazards.
However, an earthquake occurring near a volcano does not automatically mean the volcano is about to erupt.
Volcanologists examine many indicators when evaluating volcanic unrest, including earthquake patterns, ground deformation, volcanic gas emissions and changes in temperature.
For Indonesian volcanic activity, visitors can use the Orbis Weather Indonesia Volcano Tracker alongside this earthquake page.
๐ What Are Aftershocks?
Aftershocks are earthquakes occurring after a larger earthquake as the surrounding crust adjusts to the new distribution of stress.
Some aftershocks can be strong enough to cause additional damage.
They may continue for days, weeks, months or longer following a major earthquake.
The largest aftershocks are especially important when buildings have already been weakened by the initial earthquake.
๐ What Is an Earthquake Swarm?
An earthquake swarm is a sequence containing many earthquakes in a relatively small area without one event necessarily dominating the sequence as a clear mainshock.
Swarm activity can occur for different geological reasons.
An earthquake swarm by itself does not mean that a major earthquake or volcanic eruption is imminent.
Scientists analyze the location, depth, frequency and other characteristics of the earthquakes to understand what may be happening.
๐ Why Earthquake Magnitudes Sometimes Change
Initial earthquake information is often preliminary.
As additional seismic stations report data and scientists refine their analysis, the estimated magnitude, depth and exact epicenter can change.
Indonesia’s BMKG explicitly warns that earthquake parameters can change during the first minutes after an event before expert review.
That is normal and does not mean the earthquake itself changed after it occurred.
It means scientists obtained a better estimate.
๐๏ธ Why Some Earthquakes Cause More Damage Than Others
Magnitude is only one factor.
Damage can depend on:
Earthquake depth โ shallow earthquakes can create intense nearby shaking.
Distance โ communities closer to the rupture generally experience stronger shaking.
Ground conditions โ soft sediments can amplify seismic waves.
Building construction โ earthquake-resistant structures generally perform better.
Duration โ prolonged strong shaking can increase damage.
Population density โ the same earthquake can have dramatically different human consequences depending on where it occurs.
๐ข Why Tall Buildings Can Feel Distant Earthquakes
Long-period seismic waves from powerful earthquakes can travel great distances.
Tall buildings can respond more noticeably to these slower oscillations than small, rigid structures.
This helps explain why people in high-rise buildings in places such as Singapore or Kuala Lumpur may occasionally report swaying from a powerful distant earthquake.
Feeling an earthquake does not necessarily mean structural damage is occurring.
๐งญ Can Scientists Predict Earthquakes?
Scientists cannot currently predict the exact time, location and magnitude of a future earthquake with the precision needed to issue conventional short-term earthquake forecasts.
Seismologists can identify active faults, estimate long-term earthquake probabilities and rapidly detect earthquakes after they begin.
Earthquake early-warning systems can sometimes provide seconds of warning after an earthquake has started but before the strongest seismic waves reach locations farther away.
That is fundamentally different from predicting an earthquake days or weeks in advance.
๐ก๏ธ What Should You Do During an Earthquake?
Earthquake safety advice can vary somewhat by country and environment, so local emergency guidance should take priority.
In many situations, people indoors are advised to Drop, Cover and Hold On โ drop to the ground, take cover beneath sturdy furniture if available and hold on until shaking stops.
Stay away from windows and objects that could fall.
After strong shaking near a tsunami-prone coastline, immediately follow local tsunami evacuation instructions.
๐ฐ๏ธ How the Southeast Asia Earthquake Tracker Works
The Orbis Weather Southeast Asia Earthquake Tracker queries the USGS Earthquake Catalog for regional seismic activity.
The USGS catalog supports filtering earthquake information by magnitude, date, geographic region and depth.
Orbis organizes that information into a simplified Southeast Asia dashboard showing recent activity, stronger earthquakes and regional groupings.
Country groupings are approximate geographic classifications based on epicenter coordinates rather than official political or seismic-agency boundaries.
๐ก Official Earthquake Sources
The USGS provides the live event data used by the current Orbis browser widget.
For Indonesia, BMKG is an essential official regional source for earthquake and tsunami information.
National geological, meteorological and disaster-management agencies should always be consulted when a significant earthquake affects a particular country.
Official authorities โ not Orbis Weather โ determine local tsunami warnings, evacuation orders and emergency actions. BMKG’s tsunami service similarly states that national, state and local authorities are responsible for official threat and warning decisions.
๐ Monitor Earthquakes Across Southeast Asia
Southeast Asia’s complicated tectonic setting makes continuous earthquake monitoring valuable.
Indonesia and the Philippines experience particularly frequent seismic activity, while earthquakes in Myanmar, Malaysia, Thailand, Vietnam and neighboring areas can also pose local or regional hazards.
Use the Orbis Weather Southeast Asia Earthquake Tracker to monitor significant seismic activity, then consult official national authorities whenever a potentially damaging earthquake or tsunami threat develops.
For additional regional monitoring, explore the Orbis Weather Indonesia Volcano Tracker, Southeast Asia Natural Hazards, Singapore Weather & Natural Hazards and Daily Southeast Asia Weather & Natural Hazards Briefing.
โ ๏ธ Important Earthquake & Tsunami Disclaimer
The Orbis Weather Southeast Asia Earthquake Tracker is provided for general information, education and situational awareness.
Earthquake magnitudes, locations and depths may initially be preliminary and can be revised as additional seismic data becomes available.
A tsunami flag displayed by the tracker does not mean a tsunami has been confirmed or that a particular coastline will be affected.
For significant earthquakes, tsunami warnings, evacuation information and emergency instructions, consult the responsible national and local authorities.
Do not use Orbis Weather alone for earthquake or tsunami life-safety decisions