SUMMARY
The M5.7 Mid Indian Ridge earthquake occurred on November 3, 2014, at 08:48 UTC, with a P-wave arrival time of approximately 08:58 UTC and an S-wave arrival time of 09:07 UTC. The epicenter was located approximately 480 km southeast of Amsterdam Island, making it roughly equidistant from Western Australia, Antarctica, and Africa. This seismic event is classified as a respectable amplitude quake, indicating significant geological activity in the central Indian Ocean.
PREREQUISITES
- Understanding of seismic wave types (P-waves and S-waves)
- Familiarity with earthquake magnitude scales (e.g., Richter scale)
- Knowledge of global tectonic plate boundaries
- Geographical awareness of the Indian Ocean region
NEXT STEPS
- Research seismic wave propagation and its implications for earthquake detection
- Explore the geological features of the Mid Indian Ridge
- Study the impact of distance on earthquake intensity and perception
- Investigate historical seismic activity in the Indian Ocean region
USEFUL FOR
Seismologists, geologists, and anyone interested in understanding seismic events and their geographical contexts, particularly in the Indian Ocean region.