Papatūānuku: Layers and Movement
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Papatūānuku: Layers and Movement
Earth’s layered structure
Earth has three main compositional layers: the crust, mantle, and core. The core has a liquid outer part and a solid inner part. The crust is a thin, solid outer layer. Beneath it, the mantle is mostly solid rock that can slowly flow over long periods. The outer core is liquid metal, while the inner core is solid metal. Māori science terms used here: kirinuku (crust), koroka (mantle), matua o waho (outer core), matua o roto (inner core).
- A. Kirinuku (crust)
- B. Koroka (mantle)
- C. Matua o waho (outer core)
- D. Matua o roto (inner core)
- 4. Solid metal
- 3. Mostly solid rock that slowly flows
- 1. Liquid metal
- 2. Thin, solid outer layer
Plates in motion
The lithosphere consists of the crust and the rigid uppermost mantle. It is broken into tectonic plates. These plates move slowly over the softer, slowly flowing mantle beneath. At plate boundaries, plates may move apart, move towards each other, or slide past one another. These movements can cause earthquakes, volcanic activity and mountain building.
- Plate boundaries are places where Earth’s layers stop.
- Plate boundaries are where plates meet, and their interactions can cause earthquakes, volcanoes or mountain building.
- Every plate boundary produces a volcano.
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