Activity 1 Flashcards
1
Q
You can divide planets and moons with a solid surface into two categories:
A
- Active surfaces
- Inactive surfaces
2
Q
“Active” planets
A
- Have relatively “young” surfaces.
- AKA surfaces that have been recently or are currently being modified by plate tectonics, volcanic activity, active weathering/erosion and the creation of new surface materials.
3
Q
How did geologist Grove K. Gilbert oppose the beliefs that craters were purely of volcanic origin?
A
- He observed that the floors of craters on the moon were generally below the level of the surrounding plains
4
Q
Debate of circular craters with the Impact hypothesis
A
- A problem that some noted regarding the impact hypothesis was the predominantly circular shapes of most craters
- Argued that only impacts striking the ground directly from overhead (at a 90° angle to the ground’s surface) should result in circular craters.
- Since most impacts occur at an angle to the ground surface, it was argued that most craters formed this way should be elliptical, not circular.
5
Q
Debate of circular craters with the Impact hypothesis - CONSIDERATION OF SPEED:
A
- Did not consider the speeds most impacting bodies travel—between 17 and 70 kilometres per second
- Before impact, the meteor possesses much kinetic energy. But upon impact, is converted into other forms, including heat.
- All matter is held together by binding energy, which physically holds the atoms and molecules together.
- If the energy produced during the impact exceeds the binding forces that hold the meteor together, it will explode in all directions, generating a spherical shockwave and heat and ultimately creating a circular crater.
- Throughout this process, most impacting bodies are vaporized and/or fragmented.
- Materials are ejected from the crater, but most fall back to cover the crater floor
6
Q
Simple Impact Craters
Crater Types and Features
A
- Most common
- Characterized by bowl-like shape with a raised outer rim.
- When a meteor strikes the surface, it creates a cavity with a circular, raised rim and a flat or slightly curved floor
- Rim height and diameter depend on the size and velocity of the impacting object.
- Floor - smooth with minor variations due to the ejection of material during the impact.
7
Q
Complex Impact Craters
Crater Types and Features
A
- Larger and more intricate in structure than simple craters
- Form when a significantly larger object strikes the surface with greater force, causing extensive surface deformation.
- Have a central peak or peaks surrounded by a ring or rings of elevated terraces (from rebound of material); terraces result from the collapse of the crater walls inward
8
Q
Materials Ejected from Craters
Crater Types and Features
A
- Additional common features are rays caused by ejected material (ejecta) exiting the crater during the impact
- **”Lobes” **of materials that are thought to form when ice in the subsurface melted during the impact, causing a slurry of materials to flow over the surface.
9
Q
Age Relationships - how can we tell which craters are older/younger?
A
- Cross-cutting relationships
10
Q
A