Start here: Explorer · Ages 10 and upAnswer sheet for teachers
Answers: Iron meteorites and their hidden patterns
- A: An iron sulphideTroilite is an iron sulphide, often found as nodules in irons along with graphite.
- C: HexahedriteHexahedrites are low in nickel, nearly all kamacite, and often show Neumann lines.
- B: Melting let the dense metal sink inwardsWhen an asteroid melted, its heavy metal sank to the middle and formed a core.
- A: Gibeon, a fine octahedriteGibeon from Namibia is a fine octahedrite, and the giant Hoba meteorite is an ataxite.
- C: By the width of their kamacite bandsOctahedrites are called coarse, medium or fine according to how wide their kamacite bands are.
- False: the right answer is Kamacite is low in nickel and forms broad bandsLow-nickel kamacite makes the broad bands, edged by thin borders of nickel-rich taenite.
- True (We cannot sample Earth's core directly)We cannot sample Earth's core directly, so asteroid cores are the closest examples we can study.
- Shock (accept any answer with the same meaning)Neumann lines are fine parallel lines produced by shock, for example from impacts.
- Its bands follow the faces of an eight-sided shape (accept any answer with the same meaning)An octahedron has eight faces, and the bands in an octahedrite run parallel to them.
- Octahedrite (accept any answer with the same meaning)Octahedrites have roughly 6 to 13 per cent nickel and show a Widmanstätten pattern.
Task
Answers will vary. The task comes from the lesson: Look at pictures of an etched iron meteorite and try drawing the pattern. Notice how the bands cross at a few set angles. Can you find the thin bright borders of taenite?
Look for work that uses the key words correctly and gives a reason for each point.
Howardites · teacher copy: keep it separate from the pupil worksheets