scholarly journals Conditions for the spread of the Peyote cult in North America

1975 ◽  
Vol 7 ◽  
pp. 70-83
Author(s):  
Åke Hultkrantz
Keyword(s):  
Nineteenth Century ◽  
North America ◽  
American Indian ◽  
Rio Grande ◽  
Religious Movement ◽  
The North ◽  
North American Indian ◽  
Native North America ◽  
Modern Form ◽  
New Facilities

As is well known large parts of native North America with the Prairies and Plains in the middle of the continent as the centre of diffusion have constituted, since the end of the last century, the scene of a nativistic Indian movement, the so-called peyote cult. The peyote cult—or, as it should have been called, the peyote religion — is named after its central cultic action, the consumption (by eating, drinking or smoking) of the spineless cactus peyote (Lophophora williamsii). This cactus that may be found growing wild along the Rio Grande and in the country south of this river contains several alkaloids, among them the morphine-like, hallucinogeneous mescaline. In pre-Columbian days peyote was used in connection with certain public ceremonies among the Indians of Mexico, for instance, at the annual thanksgiving ceremonies. In its modern form the peyote ritual constitutes a religious complex of its own, considered to promote health, happiness and welfare among its adepts. The two major questions are: what were the conditions for the diffusion of the peyote cult? What particular factors accounted for the spread of the cult to just those areas that were mentioned above, and for its obstruction in other areas?  The change in the North American Indian situation at the end of the nineteenth century supplied new facilities for religious innovations and for the introduction of a foreign religious movement, the peyote cult.

scholarly journals The Timeless African and the Versatile Indian in Seventeenth-Century Travelogues

2005 ◽  
Vol 14 (1) ◽  
pp. 23-44
Author(s):  
Michel Duquet
Keyword(s):  
Seventeenth Century ◽  
North America ◽  
American Indian ◽  
West Coast ◽  
Tropical Environment ◽  
The West ◽  
The North ◽  
Native Populations ◽  
French And English ◽  
North American Indian

Abstract The seventeenth century saw the early stages of significant trading on the west coast of Africa as well as the establishment of permanent settlements in North America by Dutch, French and English explorers, merchants, colonists and missionaries in a period marked by the imperial contest that had been set in motion on the heels of the discovery of America in 1492. The travelers who wrote about their voyages overseas described at length the natives they encountered on the two continents. The images of the North American Indian and of the African that emerged from these travel accounts were essentially the same whether they be of Dutch, French or English origin. The main characteristic in the descriptions of African native populations was its permanent condemnation while representations of the Indian were imbued with sentiments ranging from compassion, censure and admiration. The root causes for this dichotomy were the inhospitable and deadly (to Europeans) tropical environment of Africa’s West Coast and the growing knowledge of local societies that Europeans acquired in North America. The analysis of the contrasting images of natives on both sides of the Atlantic and the context within which they were produced are the focus of the paper.

A 200-Year Perspective of Climate Variability and the Response of White Spruce in Interior Alaska

2003 ◽  
Author(s):  
Glenn Patrick Juday ◽  
Valerie Barber
Keyword(s):  
Nineteenth Century ◽  
North America ◽  
Climate Variability ◽  
Tree Ring ◽  
Tree Growth ◽  
White Spruce ◽  
Boreal Region ◽  
The North ◽  
Interior Alaska ◽  
Summer Temperatures

The two most important life functions that organisms carry out to persist in the environment are reproduction and growth. In this chapter we examine the role of climate and climate variability as controlling factors in the growth of one of the most important and productive of the North American boreal forest tree species, white spruce (Picea glauca [Moench] Voss). Because the relationship between climate and tree growth is so close, tree-ring properties have been used successfully for many years as a proxy to reconstruct past climates. Our recent reconstruction of nineteenth- century summer temperatures at Fairbanks based on white spruce tree-ring characteristics (Barber et al. in press) reveals a fundamental pattern of quasi-decadal climate variability. The values in this reconstruction of nineteenth-century Fairbanks summer temperatures are surprisingly warm compared to values in much of the published paleoclimatic literature for boreal North America. In this chapter we compare our temperature reconstructions with ring-width records in northern and south-central Alaska to see whether tree-growth signals in the nineteenth century in those regions are consistent with tree-ring characteristics in and near Bonanza Creek (BNZ) LTER (25 km southwest of Fairbanks) that suggest warm temperatures during the mid-nineteenth century. We also present a conceptual model of key limiting events in white spruce reproduction and compare it to a 39-year record of seed fall at BNZ. Finally, we derive a radial growth pattern index from white spruce at nine stands across Interior Alaska that matches recent major seed crop events in the BNZ monitoring period, and we identify dates after 1800 when major seed crops of white spruce, which are infrequent, may have been produced. The boreal region is characterized by a broad zone of forest with a continuous distribution across Eurasia and North America, amounting to about 17% of the earth’s land surface area (Bonan et al. 1992). The boreal region is often conceived of as a zone of relatively homogenous climate, but in fact a surprising diversity of climates are present. During the long days of summer, continental interior locations under persistent high-pressure systems experience hot weather that can promote extensive forest fires frequently exceeding 100 kilohectares (K ha). Summer daily maximum temperatures are cooled to a considerable degree in maritime portions of the boreal region affected by air masses that originate over the North Atlantic, North Pacific, or Arctic Oceans.

Edmund S. Curtis and the North American Indian, Incorporated

1999 ◽  
Vol 23 (1) ◽  
pp. 74
Author(s):  
Edward J. Gallagher ◽  
Mick Gidley
Keyword(s):  
American Indian ◽  
North American ◽  
The North ◽  
North American Indian
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