Extensive Secondary Cratering From the InSight Sol 1034a Impact Event
P M Grindrod1, I J Daubar2, B Fernando3
1Natural History Museum London UK.
Summary
A seismic event on Mars, detected by NASA
Area of Science:
- Planetary Science
- Impact Cratering Studies
- Seismology
Background:
- Impact cratering is a fundamental process in Solar System history.
- Observing small-scale features like secondary craters is challenging due to image timing gaps.
- Seismic data offers precise timing for impact events.
Purpose of the Study:
- To investigate secondary cratering using a precisely timed seismic event.
- To analyze the characteristics of a new impact crater and its associated secondary events.
- To understand the formation and fading of secondary impact features.
Main Methods:
- Utilized seismic event data (S1034a) from NASA's InSight mission for precise impact timing.
- Analyzed orbital imagery of the new impact crater.
- Quantified secondary impact features (low albedo spots) and their distribution.
Main Results:
- Confirmed seismic event S1034a resulted from a new impact cratering event.
- A ~9m primary crater generated over 900 secondary impact events (low albedo spots) up to 7km away.
- Secondary impact ejecta velocities were estimated below 200 m/s.
- Low albedo spots fade within 200-300 days.
Conclusions:
- Seismic data provides a unique opportunity to study small-scale secondary cratering.
- Low albedo spots are significant indicators of secondary impact processes.
- Secondary impact features on Mars have a relatively short observable lifespan.
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