Weed, Tuber, and Maize Farming in the Americas

The American continent extends over 12,000 kilometres from Alaska to Cape Horn, and encompasses an enormous variety of environments from arctic to tropical. For the purposes of this discussion, such a huge variety has to be simplified into a few major geographical units within the three regions of N...

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Main Author: Barker, Graeme
Format: Book Part
Language:unknown
Published: Oxford University Press 2006
Subjects:
Online Access:http://dx.doi.org/10.1093/oso/9780199281091.003.0012
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spelling croxfordunivpr:10.1093/oso/9780199281091.003.0012 2023-05-15T15:16:53+02:00 Weed, Tuber, and Maize Farming in the Americas Barker, Graeme 2006 http://dx.doi.org/10.1093/oso/9780199281091.003.0012 unknown Oxford University Press The Agricultural Revolution in Prehistory book-chapter 2006 croxfordunivpr https://doi.org/10.1093/oso/9780199281091.003.0012 2022-08-05T10:27:59Z The American continent extends over 12,000 kilometres from Alaska to Cape Horn, and encompasses an enormous variety of environments from arctic to tropical. For the purposes of this discussion, such a huge variety has to be simplified into a few major geographical units within the three regions of North, Central, and South America (Fig. 7.1). Large tracts of Alaska and modern Canada north of the 58th parallel consist of tundra, which extends further south down the eastern coast of Labrador. To the south, boreal coniferous forests stretch eastwards from Lake Winnipeg and the Red River past the Great Lakes to the Atlantic, and westwards from the slopes of the Rockies to the Pacific. The vast prairies in between extend southwards through the central United States between the Mississippi valley and the Rockies, becoming less forested and more open as aridity increases further south. South of the Great Lakes the Appalachian mountains dominate the eastern United States, making a temperate landscape of parallel ranges and fertile valleys, with sub-tropical environments developing in the south-east. The two together are commonly referred to as the ‘eastern Woodlands’ in the archaeological literature. On the Pacific side are more mountain ranges such as the Sierra Nevada, separated from the Rockies by arid basins including the infamous Death Valley. These drylands extend southwards into the northern part of Central America, to what is now northern Mexico, a region of pronounced winter and summer seasonality in temperature, with dryland geology and geomorphology and xerophytic vegetation. The highlands of Central America, from Mexico to Nicaragua, are cool tropical environments with mixed deciduous and coniferous forests. The latter develop into oak-laurel-myrtle rainforest further south in Costa Rica and Panama. The lowlands on either side sustain a variety of tropical vegetation adapted to high temperatures and frost-free climates, including rainforest, deciduous woodland, savannah, and scrub. South America can be ... Book Part Arctic Tundra Alaska Oxford University Press (via Crossref) Arctic Canada Cape Horn ENVELOPE(-135.021,-135.021,61.583,61.583) Pacific
institution Open Polar
collection Oxford University Press (via Crossref)
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description The American continent extends over 12,000 kilometres from Alaska to Cape Horn, and encompasses an enormous variety of environments from arctic to tropical. For the purposes of this discussion, such a huge variety has to be simplified into a few major geographical units within the three regions of North, Central, and South America (Fig. 7.1). Large tracts of Alaska and modern Canada north of the 58th parallel consist of tundra, which extends further south down the eastern coast of Labrador. To the south, boreal coniferous forests stretch eastwards from Lake Winnipeg and the Red River past the Great Lakes to the Atlantic, and westwards from the slopes of the Rockies to the Pacific. The vast prairies in between extend southwards through the central United States between the Mississippi valley and the Rockies, becoming less forested and more open as aridity increases further south. South of the Great Lakes the Appalachian mountains dominate the eastern United States, making a temperate landscape of parallel ranges and fertile valleys, with sub-tropical environments developing in the south-east. The two together are commonly referred to as the ‘eastern Woodlands’ in the archaeological literature. On the Pacific side are more mountain ranges such as the Sierra Nevada, separated from the Rockies by arid basins including the infamous Death Valley. These drylands extend southwards into the northern part of Central America, to what is now northern Mexico, a region of pronounced winter and summer seasonality in temperature, with dryland geology and geomorphology and xerophytic vegetation. The highlands of Central America, from Mexico to Nicaragua, are cool tropical environments with mixed deciduous and coniferous forests. The latter develop into oak-laurel-myrtle rainforest further south in Costa Rica and Panama. The lowlands on either side sustain a variety of tropical vegetation adapted to high temperatures and frost-free climates, including rainforest, deciduous woodland, savannah, and scrub. South America can be ...
format Book Part
author Barker, Graeme
spellingShingle Barker, Graeme
Weed, Tuber, and Maize Farming in the Americas
author_facet Barker, Graeme
author_sort Barker, Graeme
title Weed, Tuber, and Maize Farming in the Americas
title_short Weed, Tuber, and Maize Farming in the Americas
title_full Weed, Tuber, and Maize Farming in the Americas
title_fullStr Weed, Tuber, and Maize Farming in the Americas
title_full_unstemmed Weed, Tuber, and Maize Farming in the Americas
title_sort weed, tuber, and maize farming in the americas
publisher Oxford University Press
publishDate 2006
url http://dx.doi.org/10.1093/oso/9780199281091.003.0012
long_lat ENVELOPE(-135.021,-135.021,61.583,61.583)
geographic Arctic
Canada
Cape Horn
Pacific
geographic_facet Arctic
Canada
Cape Horn
Pacific
genre Arctic
Tundra
Alaska
genre_facet Arctic
Tundra
Alaska
op_source The Agricultural Revolution in Prehistory
op_doi https://doi.org/10.1093/oso/9780199281091.003.0012
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