South Island High Country Evolution
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South Island High Country Evolution
🏔️ Phase 1: Gondwana Land and Ancient New Zealand (200-300 Million Years Ago)
Sediment from ancient Gondwanaland was deposited to depths of up to _____________ metres in the _____________ Basin. Under pressure, this became _____________ rock, and where heat and pressure were most intense, it metamorphosed into _____________.
⛰️ Phase 2: The Rangitata Orogeny (125-200 Million Years Ago)
🌋 Phase 3: Kaikoura Orogeny (25-10 Million Years Ago - Today)
The western side of the Alpine Fault moved _____________ relative to the eastern side at a rate of _____ to _____ cm per year. This resulted in approximately _____________ km of total displacement.
❄️ Phase 4: Erosion and Modern Landscape
🔄 Timeline Summary
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