Glaciers offer the potential to reconstruct past climate over timescales from decades to
millennia. They are found on nearly every continent, and at the Last Glacial Maximum …

Holocene glacial chronostratigraphies in glaciated valleys spread throughout the Himalayan-
Tibetan orogen, including the Himalaya, Tibet, Pamir, and Tian Shan, are developed using a …

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 …

Geochronological dating of glacial landforms, such as terminal and lateral moraines, is
useful for determining the extent and timing of past glaciation and for reconstructing the …

Detailed mapping and geochronological investigations of edifice-forming materials
reconstruct the growth history of Tongariro volcano, New Zealand, and subdivide the edifice …

Numerical glacier models applied to moraine chronologies provide an opportunity to
quantify past climate change. Here we apply a two-dimensional coupled mass balance–ice …

Mountain glacier records offer important constraints on the timing and magnitude of climate
variability during the last glacial cycle. Existing moraine chronologies from the central …

Glacial landscapes preserve records of past climate change. Investigating the glacier–
climate system over the Late Quaternary provides information about past climate change …