A general discussion is given of climate variability over the last 150
0 years as interpreted from two ice cores from the Quelccaya ice cap,
Peru. The possible role of climatic variability in prehistory over thi
s period is discussed with emphases on (1) relationships between clima
te and the rise and decline of coastal and highland cultures, (2) the
possible causes of two major dust events recorded in the Quelccaya ice
cores around AD 920 and AD 600; and (3) implications of climatic vari
ation for the occupation and abandonment of the Gran Pajaten area. The
remarkable similarity between changes in highland and coastal culture
s and changes in accumulation as determined from the Quelccaya ice cor
es implies a strong connection between human activities and climate in
this region of the globe. Two ice cores drilled to bedrock from the 6
047 masl col of Huascaran in the Cordillera Blanca, Peru in 1993 offer
the potential of an annual to decadal climatic and environmental reco
rd which should allow the study of human-climate and human-environment
al relationships over 10,000+ years. The 1991 and 1993 evidence from t
he Quelccaya ice cap indicates that recent and rapid warming is curren
tly underway in the tropical Andes. Thus many of the unique glacier ar
chives are in imminent danger of being lost forever.