An earthquake measuring 8.0 struck Santiago Chile on 3 March 1985, and ended up killing 177 people and injuring about 2,575 others. This earthquake was being felt between the northern Antofagasta Region and the southern Los Lagos Region. It was felt with a maximum intensity of VIII on the Mercalli intensity scale. Damage and effects The quake left 177 people dead, 2,575 injured, 85,358 houses damaged or destroyed and about a million people homeless. Many landslides were registered too, pavement breaks with the destruction of the Pan-American Highway in several points, broken-down bridges and considerable damage in affected town's infrastructure, with a long interruption on basic services. The damage was valued in more than 1 billion US dollars. Reports by local residents in the coastal area from Matanzas to several kilometers north of Algarrobo indicated unusually low tides for a period of 3 to 5 days following the earthquake. After this, the tides reportedly returned to normal. This suggests that there was earthquake-related uplift along parts of the coast which was recovered in 3 to 5 days after the earthquake. Near Algarrobo, an estimate of the change is about 20 cm uplift. Tectonic setting Chile lies on the boundary between the Nazca Plate of the South Pacific continental plate. This results in Chile being one of the most seismically active regions in the world. On average, a magnitude 8 earthquake or greater occurs in the region about once every 25 years. Meaning that there is an expectation that a similar earthquake will happen in Chile in the future every 25 years. The main shock was actually made up of at least two shocks, with the initial motion beginning at approximately 11:00 PM followed by a greater event soon after. The magnitudes of the first and second shocks were calculated to be 5.2 and 6.9 respectively. The calculated proportion of energy released as aftershocks vs the main shock was relatively high, most likely due to the 7.2 aftershock on 9 April. Scientific understanding The earthquake was seen as particularly powerful, garnering the attention of the United States. They sent a team of geologists to study its effects because the overall information that could be gained from studying the earthquake could give better understandings overall of these powerful earthquakes. This earthquake in particular was considered extremely important in the understanding of earthquakes as "it was very significant as a geophysical event and