
The warning came twelve hours early, though nobody recognized it as one. On the afternoon of January 14, 2021, a magnitude 5.7 earthquake rattled Majene in West Sulawesi, triggering landslides, destroying two houses, and sending dozens of coastal residents fleeing to higher ground. Indonesia's meteorological agency, the BMKG, issued an advisory: the fault still held enough energy to produce something worse. Residents were urged to prepare. Then, at 2:28 AM on January 15, the main shock arrived -- a magnitude 6.2 rupture along the Mamuju-Majene Thrust Fault that shook the ground for five to seven seconds and changed the province overnight.
Sulawesi sits at one of the most tectonically complex intersections on Earth. The Australian, Pacific, Philippine, and Sunda plates converge here, grinding against one another and spawning a mosaic of smaller microplates that rotate, compress, and fracture the island's strange K-shaped landmass. The main active fault in western Central Sulawesi is the left-lateral Palu-Koro strike-slip fault, responsible for the devastating 2018 Palu earthquake and tsunami. But the 2021 event struck along a different structure entirely: the Mamuju-Majene Thrust Fault, an offshore reverse fault that slopes eastward beneath the coast at a steep 45-degree angle before flattening at depth. GPS data shows the Makassar block rotating counterclockwise, its northwestern margin pressing against the Sunda block across the Makassar Strait. The same fault had produced a destructive earthquake near Majene in 1969, killing at least 64 people. The geology here does not forget.
The mainshock struck at shallow depth with its epicenter in Majene Regency, about 32 kilometers south of Mamuju, the provincial capital. Shaking reached Modified Mercalli intensity VI -- Strong -- in both Majene and Mamuju, and was felt as far away as Makassar to the south and Palu to the north. Four of West Sulawesi's five regencies suffered damage. In Mamuju, the consequences were catastrophic. Half the city's structures were damaged or destroyed, according to regional government officials. The main hospital lost 50 percent of its building, forcing hundreds of patients to be treated outdoors. AirNav Indonesia's office at Tampa Padang Airport was severely damaged; the control tower cracked; air traffic operations were diverted to Makassar. The Mamuju penitentiary's perimeter fence collapsed. Telecommunications went dark. Power stations failed across the region.
Landslides triggered by the shaking cut the main road between Mamuju and Majene, isolating at least six villages. In Majene, nine people were buried under a slide; rescuers pulled eight out alive, but one person died. Three members of the same family perished when debris engulfed their house. Schools bore a staggering toll: initial reports counted 15 damaged or destroyed, a figure that eventually climbed to 103 across Mamuju, Majene, Mamasa, and even Polewali Mandar Regency, with 37 suffering heavy structural damage. At least 7,000 homes, 21 health facilities, a supermarket, a harbor, and public offices were damaged or destroyed. The preliminary cost of the damage exceeded 821 billion rupiah. By January 25, the confirmed death toll reached 105 people. Nearly 6,500 others were injured, including 426 with serious wounds. Close to 20,000 people were displaced from their homes.
The earthquake arrived during Indonesia's COVID-19 pandemic, compounding every aspect of the disaster. Packed evacuation camps raised fears of new infection clusters. West Sulawesi's planned mass vaccination program was postponed as healthcare resources were diverted to earthquake relief. The national disaster agency, BNPB, acknowledged that stocks of personal protective equipment had dwindled. President Joko Widodo ordered Minister of Social Affairs Tri Rismaharini to the disaster zone and declared a state of emergency. The Indonesian Air Force dispatched a Boeing 737; the Navy sent two ships, including a hospital vessel; and two navy battalions deployed to Mamuju and Majene. The state oil company Pertamina ensured fuel supplies held steady, sending mobile storage units and fuel trucks from Donggala Regency. The Indonesian Red Cross, led by former Vice President Jusuf Kalla, mobilized teams from Palu and Makassar. Yet complaints from evacuees mounted: aid arrived slowly, distribution was uneven, and some families reported receiving nothing for a full week.
Scientific analysis after the earthquake revealed something unsettling. The 2021 rupture was a partial break along the Makassar Strait thrust -- the fault did not release all of its accumulated strain. Seismologists noted that fewer aftershocks followed this event than typically accompany shallow crustal earthquakes in Indonesia, a pattern consistent with a large seismic moment released over a small rupture area in a short burst. The locked portion of the fault remains. West Sulawesi continues to grow, its economy driven by agriculture, cocoa, and palm oil, its population rebuilding on the same ground that shifted beneath them. Electricity was fully restored on February 5, nearly a month after the quake. The schools have been rebuilt or repaired. The fault line has not moved -- yet. In a region where four tectonic plates jostle for position, the question is never whether the ground will shake again, but when.
The earthquake epicenter lies at approximately 3.00S, 118.92E, in Majene Regency, West Sulawesi. From altitude, the western coast of Sulawesi is visible as a narrow strip between mountains and the Makassar Strait. The nearest airport is Tampa Padang Airport (WAFJ) in Mamuju, which was damaged in the earthquake but remained operational. Sultan Hasanuddin International Airport (WAAA) in Makassar lies approximately 200 km to the south. The mountainous terrain inland shows the complex geology of the region, with landslide scars potentially still visible on steep slopes.