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Will it Bang, Bubble, or Fizz? Shane Cronin – Massey University Anticipating the next eruption of Mt Taranaki.

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Presentation on theme: "Will it Bang, Bubble, or Fizz? Shane Cronin – Massey University Anticipating the next eruption of Mt Taranaki."— Presentation transcript:

1 Will it Bang, Bubble, or Fizz? Shane Cronin – Massey University Anticipating the next eruption of Mt Taranaki

2 Clue no: 1 – what’s at the top?

3 Rock-falls/avalanches <1 km runout Block-and-Ash Flows (BAF) Can be 15 km runout What happens when domes fall down? Photos: G. Lube

4 Merapi volcano – June 2006 Twin brother of Mt Taranaki Erupting sporadically since 1994 >150 deaths June 2006, 20,000 evacuated, 2 deaths “minor eruption” evidence of it may never be recorded in the geologic record Aster Image

5 >700 o C “block-and-ash flows” Photos – T. Wilson

6 Original Channel Fill >1 year later The aftermath – rain-generated lahars

7 How do we know this from Taranaki?

8 Blue-Rata Reserve Taranaki, 15 km from source Charcoal 3 m

9 Example Taranaki BAF 15 km runout 2200 m drop Image T.Platz

10 Clue no 2: Pumice

11 Burrell Lapilli – AD 1655

12 Explosive eruptions – “Plinian” Map: T. Platz

13 Other types and sizes of eruption?

14 Eruption styles a) Sub-Plinian b) Dome a b Mineral clues – iron oxides Images: M. Turner

15 Clue no 3: Pulses of magma “recharge” Feldspar textures Images: Platz, Turner

16 A repeating pattern of eruption episodes opening pumice eruption lava-flows and dome building Repose (  degassing) next episode Episode 1 Episode 3 Episode 2

17 Umutekai – New Plymouth Clue no 4: Detailed eruption histories

18 Overall time-smoothed eruption rates Image: M.Bebbington

19 Sub-Plinian Dome Splitting record into two types Image: M.Bebbington

20 Where are we in the cycle?

21 Conclusions – next eruption at Mt Taranaki We are in an unusually long (although not unprecedented) lull in activity The next eruption could take one of three possible general forms: 1.Large explosive pumice eruption (last one AD1655) – not likely 2.Small explosive pumice eruption 3.Lava dome eruption Both likely types of eruption will begin with collapses from the summit area – intrusion of magma (oversteepening, earthquakes), and vent clearing Both types of eruption could herald a period of more frequent eruptions to follow A lava-dome eruption could continue for many years/decades

22 High Low Hazard Zone 1:300yrs 1x10 6 m 3 Risk of inundation Anticipated hazards for the start of the “next one” Image: J.N. Procter


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