Quelccaya Ice Cap
Ice Cap·Peru·South America·Tropical Highlands
The Quelccaya Ice Cap, also known as Quenamari Ice Cap, is the second-largest glaciated area in the tropics, located in Peru's Andes mountains. It is a crucial source of meltwater for regional rivers and a vital archive of past climate data, preserved in its ice cores.
Key Facts
- ›It is the second-largest glaciated area in the tropics, after Coropuna.
- ›The ice cap covers an area of 42.8 square kilometers with ice up to 200 meters thick.
- ›Ice cores from Quelccaya were the first recovered outside of polar regions and provide data on past climate states.
- ›It is an important source of water, flowing into the Inambari and Vilcanota Rivers.
- ›Quelccaya is shrinking due to human-caused climate change and may disappear in the 21st or 22nd century.
- ›Since 2020, it is part of the Área de Conservación Regional Ausangate.
Known For
- being the second-largest glaciated area in the tropics
- providing crucial ice core data for paleoclimate research
- its significant retreat due to climate change
Qori Kalis Glacier, Ice Cliffs Up To 50 Meters High, Ice Domes, Glacier Caves, Penitentes and Sastrugi On the Ice Surface
áRea De ConservacióN Regional Ausangate
About Quelccaya Ice Cap
The Quelccaya Ice Cap, also known by the name Quenamari Ice Cap, is recognized as the second-largest glaciated area situated within the tropics, surpassed only by Coropuna. This significant ice formation is located in the Cordillera Oriental section of the Andes mountains in southern Peru.
Geography and Size
The ice cap covers an extensive area of approximately 42.8 square kilometers, with ice depths reaching up to 200 meters. It is characterized by imposing ice cliffs surrounding it and is fed by several outlet glaciers, the most prominent of which is the Qori Kalis Glacier. The landscape around Quelccaya is diverse, featuring lakes, moraines, peat bogs, and wetlands, and it supports a rich variety of flora and fauna, including birds that nest directly on the ice.
Climate Archive and Water Source
Quelccaya holds immense scientific importance due to its role as a critical archive of past climate conditions. In 1983, researchers obtained ice cores from the central area of the ice cap, which were the first of their kind recovered outside of the polar regions. Analysis of these cores has provided detailed reconstructions of past climate states, including evidence of the Little Ice Age, periods of regional drought and significant wet spells, and past and recent El Niño events. Furthermore, the ice cap serves as a vital source of water, with its meltwater eventually flowing into the Inambari and Vilcanota Rivers, contributing to the regional water supply.
Historical Extent and Current State
Historically, the Quelccaya Ice Cap was considerably larger, merging with neighboring glaciers during the Pleistocene epoch and experiencing a secondary expansion during periods of climate anomaly. Following a period of shrinkage at the beginning of the Holocene, a neoglacial expansion occurred around 5,000 years ago. After reaching a highstand during the Little Ice Age, Quelccaya has been experiencing a significant retreat, largely attributed to human-caused climate change. This retreat has led to the emergence of new terrain occupied by life and lakes, some of which pose flood risks if they breach. Climate projections suggest that without substantial climate change mitigation efforts, Quelccaya could vanish within the 21st or 22nd century.
Accessibility and Designation
The Quelccaya Ice Cap is situated in a remote area. The nearest road is approximately 40 kilometers away, and reaching the ice cap from there can take up to three days using pack animals. Despite its remoteness, it is recognized for its ecological and scientific value and, since 2020, has been part of the Área de Conservación Regional Ausangate, a protected area.
Source: Wikipedia ↗
Frequently Asked Questions
Where is the Quelccaya Ice Cap located?
The Quelccaya Ice Cap is located in the tropical highlands of southern Peru, within the Cordillera Oriental section of the Andes mountains.
What is the significance of the ice cores from Quelccaya?
Ice cores obtained from Quelccaya have provided invaluable data for reconstructing past climate conditions, including evidence of the Little Ice Age, regional droughts, wet periods, and El Niño events. These were also the first ice cores recovered outside of the polar regions.
What is the current state of the Quelccaya Ice Cap?
The Quelccaya Ice Cap has been shrinking due to human-caused climate change. Climate models predict its potential disappearance during the 21st or 22nd century if drastic mitigation measures are not taken.
What is the size of the Quelccaya Ice Cap?
The ice cap covers an area of approximately 42.8 square kilometers and can be up to 200 meters thick. It extends up to 17 kilometers from north to south and between 3 and 5 kilometers from east to west.
What kind of climate does Quelccaya experience?
The climate is characterized by high precipitation, primarily in austral summer, and relatively stable temperatures throughout the year, though global warming is causing summit temperatures to occasionally rise above freezing.
Is Quelccaya Ice Cap accessible to the public?
The ice cap lies in a remote area, with the closest road still 40 kilometers away. Reaching it can take up to three days with pack animals, indicating limited accessibility.
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