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Giant Impact Events
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A calculation of the canonical moon-forming impact event using
the smoothed particle hydrodynamics code GADGET2 (Marcus et
al. 2009). The first 24 hours after the proto-Earth is hit
by a Mars-size object. Colors denote the core and mantle
materials.
-
Merging of two ice-rock planets (Marcus et
al. 2010).
- Catastrophic disruption on an ice-rock planet (Marcus et
al. 2010).
- Hit-and-run between two ice-rock planets (Marcus et
al. 2010).
- Formation of the unusual dwarf planet Haumea (Leinhardt et
al. 2010).
Impact Cratering
- Formation of the Chicxulub impact basin (Senft and
Stewart 2009).
- Formation of the unusual central pit craters on Ganymede
(Senft and Stewart
2011).
- Formation of the South Pole-Aitken basin on the Moon (Stewart,
LPSC, 2011).

Tooting crater on Mars. A young 29-km diameter impact crater with a fluidized ejecta blanket.
Giant impacts are common at the end of planet formation. Image credit: Don Davis