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The caldera contains two major lava dome complexes, the Haroharo vent alignment in the north and Tarawera vent alignment in the south. These two vent alignments are associated with current subsidence in the last 20 years of about 1.5 cm/year (0.59 in/year) which is assumed to be because of mainly cooling and contraction of previous magma melt. [6]
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The tubes were produced by a small vent at the southern end of the northern segment of the field, [84] extending 2.5 miles (4.0 km) from its base to the south and then the west. [85] They originated from the uppermost lava flow from a series of eruptions that ran into a valley on the western slope of the Portland Hills. [ 86 ]
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