17 datasets found

For the Valles Calchaquíes region, Northwestern Argentina, we derived rock glacier surface velocities (in unit m/a) from multi-temporal aerial and satellite imagery using a...

For the Valles Calchaquíes region, Northwestern Argentina, we derived rock glacier surface velocities (in unit m/a) from multi-temporal aerial and satellite imagery using a...

The glacier on Illimani in the eastern Bolivian Altiplano is one of the few in the mid- to low-latitudes giving access to ice covering the entire Holocene. The impurity and...

The glacier on Nevado Illimani in the eastern Bolivian Altiplano is one of the few in the mid- to low-latitudes giving access to ice covering the entire Holocene. The impurity...

These data represent pollen counts from sediment and moss polster samples collected in 2015 along an altitudinal gradient in the Ecuadorian Andes. Moss polsters are collected...

The highly-elevated and flat Altiplano in Peru is a remarkable landscape feature in such metastable geomorphologic context. However, the northern edge of the Peruvian Altiplano,...

The product provides modeled mean annual ground temperatures (MAGT) at the top of the permafrost for Andes, New Zealand and East African Plateau at 1 km spatial resolution....

Soil temperature (°C) was collected in the uppermost levels of the active layer of El Candidato rock glacier, from 2022 to 2022. El Candidato is an active rock glacier placed in...

Soil temperature (°C) was collected in the uppermost levels of the active layer of El Candidato rock glacier, from 2022 to 2022. El Candidato is an active rock glacier placed in...

Glaciers in the Andes are among the fastest shrinking and largest contributors to sea level rise in the world. They also represent crucial water resources in many tropical and...

The new climate dataset BASD-CMIP6-PE for Peru and Ecuador based on the bias-adjusted and statistically downscaled CMIP6 projections of 10 GCMs addresses the need for reliable...

RAIN4PE is a novel daily gridded precipitation dataset obtained by merging multi-source precipitation data (satellite-based Climate Hazards Group InfraRed Precipitation, CHIRP...

Tourmaline-cemented magmatic-hydrothermal breccias are a major host to sulphide mineralization in the supergiant Río Blanco–Los Bronces (RB–LB) porphyry Cu-Mo district in...

The Central Andes (~21°S) is a subduction-type orogeny formed in the last ~50 Ma from the subduction of the Nazca oceanic plate beneath the South American continental plate....

The southern Central Andes (SCA, 29°S-39°S) are characterized by the subduction of the oceanic Nazca Plate beneath the continental South American Plate. One striking feature of...

The Central Andean orogen formed as a result of the subduction of the oceanic Nazca plate beneath the continental South-American plate. In the southern segment of the Central...

The Central Andean orogeny is caused by the subduction of the Nazca oceanic plate beneath the South-American continental plate. In Particular, the Southern Central Andes (SCA,...