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The similar, but offset, increases in equilibrium temperatures for medial and distal layers 1 and 2 are consistent with both layers being deposited from the same flow.

However, any proximal deposits left by the later, hotter material must have been subsequently eroded, or be so thin that our collection failed to sample them.

Additional palaeomagnetic data collected by us and others from pumice clasts show comparable temperature variations, but these temperature estimates are shown here to be due to a chemical remanence and unreliable for accurate temperature estimates.

Cooler temperatures in proximal parts of the ignimbrite are consistent with admixture of 20% cold lithic clasts at source and interaction with the pre-eruption Lake Taupo.

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