The most recent maximum in global ice volume occurred around 23,000 to 19,000 years
ago, during Marine Isotope Stage 2 (MIS 2;∼ 29-14 ka) according to benthic δ 18 O and sea …

Proxy records from across the Southern Hemisphere show significant local to regional scale
variability in climatic and environmental conditions during late Marine Isotope Stage 3 and …

ABSTRACT Ruapehu (150 km3 cone, 150 km3 ring-plain) and Tongariro (90 km3 cone, 60
km3 ring-plain) are iconic stratovolcanoes, formed since∼ 230 and∼ 350 ka, respectively …

Ruapehu is an active~ 150 km 3 andesite-dacite composite volcano located at the southern
end of the Taupo Volcanic Zone, New Zealand. The growth of the present-day edifice has …

This paper constitutes a review of the last (Otiran) glaciation in New Zealand, spanning
marine isotope stages (MIS) 4-2. We highlight the nature of glaciation, which is …

Reconstructions of former ice masses from glacial geomorphology help to constrain the
nature and timing of glaciation in relation to climatic forcing. This paper presents a new …

Combining 3‐D inversion of high‐resolution aeromagnetic data with airborne hyperspectral
imaging creates a new method to map buried structure and hydrothermal alteration, applied …

Late Cenozoic convergence between the Australian and Pacific Plates has led to extensive
crustal deformation and exhumation in New Zealand. Over the past five decades, the …

Accurate volcanic hazard assessments rely on a detailed understanding of the timing of past
eruptions. While radiometric methods like 40 Ar/39 Ar or K/Ar are by far the most …

Heinrich events are characterized by worldwide climate modifications. Over the Altiplano
endorheic basin (high tropical Andes), the second half of Heinrich Stadial 1 (HS1a) was …