Overview
On 20 July 1859 an earthquake was recorded at Lonthor, one of the Banda Islands in eastern Indonesia, at 4.6 S, 129.9 E. The entry carries no magnitude, focal depth, or intensity rating, and no casualty or damage figures. The Banda group sits inside the Banda Arc, a tightly curved subduction system where the Australian plate meets a mosaic of small plates, producing both shallow and exceptionally deep earthquakes within a compact area. Lonthor, also called Banda Besar, was the centre of the Dutch nutmeg monopoly, and the colonial administration's presence is the reason a nineteenth-century felt report from so remote an island entered the record at all.
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About This Earthquake
1859 Indonesia, Lonthor Island: unknown magnitude earthquake, shallow crustal focus. No fatalities recorded. Indo-Australian subduction zone.
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Frequently Asked Questions
The largest earthquake ever recorded was the 1960 Valdivia earthquake in Chile, at magnitude 9.5. It generated a tsunami that traveled across the Pacific Ocean and caused damage as far away as Hawaii and Japan. The earthquake killed approximately 1,655 people and left 2 million homeless.
The deadliest earthquake in recorded history was the 1556 Shaanxi earthquake in China, estimated at magnitude 8.0-8.3, which killed approximately 830,000 people. Many casualties resulted from the collapse of yaodong (cave dwellings) carved into loess cliffs. The 2010 Haiti earthquake (M7.0, ~316,000 deaths) was the deadliest in modern times.
Pre-instrumental earthquake magnitudes are estimated from written accounts of damage, felt reports, geological evidence such as fault scarps and liquefaction features, and tsunami records. These methods provide approximate magnitudes with typical uncertainties of 0.3-0.5 magnitude units.
QuakeFYI's historical database covers earthquakes from approximately 2150 BC to the present, with over 5,700 significant events. Written records from ancient China, Greece, and the Middle East provide some of the earliest accounts. Instrumental recording began around 1900 with the first standardized seismographs.
An earthquake swarm is a sequence of many earthquakes occurring in a localized area over weeks to months without a clear mainshock. Unlike aftershock sequences where one large event is followed by smaller ones, swarms have no single dominant event. They are often associated with volcanic activity or fluid migration in the crust.