In this article, we will explore in detail the topic of 1968 Sulawesi earthquake, a topic that has captured the attention of academics, experts, and hobbyists alike. With an in-depth approach, we will analyze the different facets related to 1968 Sulawesi earthquake, from its origin to its impact on today's society. Throughout these pages, we will examine the different perspectives and opinions regarding 1968 Sulawesi earthquake, as well as its evolution over time. Through exhaustive research and the collection of relevant data, we will delve into the ins and outs of 1968 Sulawesi earthquake with the aim of providing our readers with a complete and enriching insight into this topic.
UTC time | 1968-08-14 22:14:23 |
---|---|
ISC event | 818025 |
USGS-ANSS | ComCat |
Local date | August 15, 1968 |
Local time | 06:14:23 |
Magnitude | 7.4 ML 7.2 Mw(USGS) |
Depth | 17 km (11 mi)[1] |
Epicenter | 0°04′N 119°41′E / 0.06°N 119.69°E[1] |
Fault | Palu-Koro fault |
Areas affected | Indonesia |
Max. intensity | MMI IX (Violent) |
Casualties | 213 killed |
The 1968 Sulawesi earthquake struck Indonesia on August 14. It had a Richter magnitude of 7.4, spawned a large tsunami, and killed roughly 200 people.
The earthquake had a Richter magnitude of 7.4. It created a tsunami with wave heights of 8 m (26 ft) to 10 m (33 ft), which soon traveled onto Sulawesi. The most extensive waves reached 300 m (980 ft) inland, destroying 700 homes and killing around 200 people.[2]
The earthquake ruptured along Palu-Koro fault[3] in Manimbaja Bay. It caused subsidence that decreased elevations by as much as 2 m (6 ft 7 in) to 3 m (9.8 ft) along the coast. It also appeared to uplift at least one of the Togian Islands.[2]
The earthquake was near the Celebes Sea; it sank the island of Tuguan.[4]
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