Impact cratering begins with contact and compression, in which a shock rapidly heats and compresses target and impactor. During excavation, material moves outward and upward, producing a transient cavity and ejecta. Modification then involves gravitational collapse, wall slumping, fallback and, for large structures, rebound and central features. The stages overlap in time; crater size and morphology depend on gravity, impact conditions and target strength, not just the projectile's geometric hole size.
Ancestors (11)
- 2
- S29
- 2016
- Past exam of the short options paper shared by Prelims and Parts A and B of the physics course of the University of Oxford
- Short options paper shared by Prelims and Parts A and B of the physics course of the University of Oxford
- Physics course of the University of Oxford
- Undergraduate course of the University of Oxford
- Course of the University of Oxford
- University of Oxford
- List of universities
- Home
Discussion (0)
New discussionThere are no discussions about this article yet.
Articles by others on the same topic (0)
There are currently no matching articles.