Hydrogeology and Paleohydrology of Ancient Machu Picchu
Abstract The study of the ancient Inca water supply of Machu Picchu was performed by the authors under an archaeological permit issued by the Peruvian Government in 1994. The study included an evaluation of the hydrogeology of the ancient spring water supply situated on the north slope of the mounta...
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crwiley:10.1111/j.1745-6584.1997.tb00131.x 2023-12-03T10:24:11+01:00 Hydrogeology and Paleohydrology of Ancient Machu Picchu Wright, Kenneth R. Witt, Gary D. Zegarra, Alfredo Valencia 1997 http://dx.doi.org/10.1111/j.1745-6584.1997.tb00131.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1745-6584.1997.tb00131.x http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1745-6584.1997.tb00131.x/fullpdf en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Groundwater volume 35, issue 4, page 660-666 ISSN 0017-467X 1745-6584 Computers in Earth Sciences Water Science and Technology journal-article 1997 crwiley https://doi.org/10.1111/j.1745-6584.1997.tb00131.x 2023-11-09T14:05:57Z Abstract The study of the ancient Inca water supply of Machu Picchu was performed by the authors under an archaeological permit issued by the Peruvian Government in 1994. The study included an evaluation of the hydrogeology of the ancient spring water supply situated on the north slope of the mountain of Machu Picchu and its relationship to the Machu Picchu fault. Based on field measurements, the yield of the primary spring has a seasonal variation of between 25 and 125 liters per minute. This flow adequately provided the domestic water requirements of up to 1000 inhabitants of the mountain top royal retreat of the Inca ruler Pachacuti, occupied primarily between 1450 and 1540 AD. The permanent population between visits of the Inca ruler was about 300. Final abandonment occurred in 1572 AD. The estimated geologic catchment area related to the Machu Picchu fault is roughly 50 percent greater than the topographic basin area. A 749 meter‐long canal delivered the spring flow to the center of the community to serve a total of 16 water supply fountains. A theory that a water shortage caused Machu Picchu to be abandoned proved to be unsubstantiated based on a study of the Quelccaya Ice Cap corings data that demonstrated that the last decade of the occupation was wetter than the previous eight decades. The builders of Machu Picchu developed a community domestic water supply using the spring and a hydraulic infrastructure in an effective and efficient manner. They utilized a gravity flow canal sized to carry the spring flow with a suitable safety factor against overtopping. Article in Journal/Newspaper Ice cap Wiley Online Library (via Crossref) Inca ENVELOPE(-59.194,-59.194,-62.308,-62.308) Groundwater 35 4 660 666 |
institution |
Open Polar |
collection |
Wiley Online Library (via Crossref) |
op_collection_id |
crwiley |
language |
English |
topic |
Computers in Earth Sciences Water Science and Technology |
spellingShingle |
Computers in Earth Sciences Water Science and Technology Wright, Kenneth R. Witt, Gary D. Zegarra, Alfredo Valencia Hydrogeology and Paleohydrology of Ancient Machu Picchu |
topic_facet |
Computers in Earth Sciences Water Science and Technology |
description |
Abstract The study of the ancient Inca water supply of Machu Picchu was performed by the authors under an archaeological permit issued by the Peruvian Government in 1994. The study included an evaluation of the hydrogeology of the ancient spring water supply situated on the north slope of the mountain of Machu Picchu and its relationship to the Machu Picchu fault. Based on field measurements, the yield of the primary spring has a seasonal variation of between 25 and 125 liters per minute. This flow adequately provided the domestic water requirements of up to 1000 inhabitants of the mountain top royal retreat of the Inca ruler Pachacuti, occupied primarily between 1450 and 1540 AD. The permanent population between visits of the Inca ruler was about 300. Final abandonment occurred in 1572 AD. The estimated geologic catchment area related to the Machu Picchu fault is roughly 50 percent greater than the topographic basin area. A 749 meter‐long canal delivered the spring flow to the center of the community to serve a total of 16 water supply fountains. A theory that a water shortage caused Machu Picchu to be abandoned proved to be unsubstantiated based on a study of the Quelccaya Ice Cap corings data that demonstrated that the last decade of the occupation was wetter than the previous eight decades. The builders of Machu Picchu developed a community domestic water supply using the spring and a hydraulic infrastructure in an effective and efficient manner. They utilized a gravity flow canal sized to carry the spring flow with a suitable safety factor against overtopping. |
format |
Article in Journal/Newspaper |
author |
Wright, Kenneth R. Witt, Gary D. Zegarra, Alfredo Valencia |
author_facet |
Wright, Kenneth R. Witt, Gary D. Zegarra, Alfredo Valencia |
author_sort |
Wright, Kenneth R. |
title |
Hydrogeology and Paleohydrology of Ancient Machu Picchu |
title_short |
Hydrogeology and Paleohydrology of Ancient Machu Picchu |
title_full |
Hydrogeology and Paleohydrology of Ancient Machu Picchu |
title_fullStr |
Hydrogeology and Paleohydrology of Ancient Machu Picchu |
title_full_unstemmed |
Hydrogeology and Paleohydrology of Ancient Machu Picchu |
title_sort |
hydrogeology and paleohydrology of ancient machu picchu |
publisher |
Wiley |
publishDate |
1997 |
url |
http://dx.doi.org/10.1111/j.1745-6584.1997.tb00131.x https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1745-6584.1997.tb00131.x http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1745-6584.1997.tb00131.x/fullpdf |
long_lat |
ENVELOPE(-59.194,-59.194,-62.308,-62.308) |
geographic |
Inca |
geographic_facet |
Inca |
genre |
Ice cap |
genre_facet |
Ice cap |
op_source |
Groundwater volume 35, issue 4, page 660-666 ISSN 0017-467X 1745-6584 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1111/j.1745-6584.1997.tb00131.x |
container_title |
Groundwater |
container_volume |
35 |
container_issue |
4 |
container_start_page |
660 |
op_container_end_page |
666 |
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1784272527157100544 |