Gotowe bibliografie tematyczne / Indians of North America – Plateau region

Gotowa bibliografia na temat „Indians of North America – Plateau region”

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Data publikacji: 26 lipca 2024

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Artykuły w czasopismach na temat "Indians of North America – Plateau region"

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Nickens, Paul R. "Imagining the Multilayered Cultural Landscape: A Template from the Columbia Plateau of North America". Land 11, nr 10 (21.09.2022): 1613. http://dx.doi.org/10.3390/land11101613.

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Cultural landscapes encompass a diversity of manifestations of the interaction between humankind and the natural environment occurring in both space and time. In some instances where the human occupation of a specific area or region encompass a continuous and extended timeframe, successive cultural layers yield contrasting and disparate landscapes and heritage values. This “layering” of past cultural landscapes often leads to conflicting modern-day land, cultural resource management, and heritage value issues. A case study is presented from the Hanford Site in south-central Washington state, USA, where the natural landscape comprises prehistoric Native American, historic ethnographic, and historic period non-Indian evidence from over 10,000 years of occupation and use that clearly separate into several culturally and chronologically defined and overlapping cultural landscapes, which can be visualized as layered entities occurring on the same physical space.
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Kumar Pokharia, Anil, B. Sekar, Jagannath Pal i Alka Srivastava. "Possible Evidence of Pre-Columbian Transoceanic Voyages Based on Conventional LSC and AMS 14C Dating of Associated Charcoal and a Carbonized Seed of Custard Apple (Annona squamosa L.)". Radiocarbon 51, nr 3 (2009): 923–30. http://dx.doi.org/10.1017/s0033822200033993.

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An attempt was made to trace the antiquity of custard apple in India on the basis of accelerator mass spectrometry (AMS) and liquid scintillation counting (LSC) radiocarbon dates. Recently, seed remains of custard apple (Annona squamosa L.) in association with wood charcoals were encountered from the Neolithic archaeological site of Tokwa at the confluence of the Belan and Adwa rivers, Mirzapur District, in the Vidhyan Plateau region of north-central India. The wood charcoal sample was dated at the 14C laboratory of the Birbal Sahni Institute of Palaeobotany (BSIP), Lucknow, by conventional LSC 14C dating. The sample dated to 1740 cal BC (BS-2054). A seed sample of custard apple was dated by AMS at the Institute of Physics 14C laboratory, Bhubaneswar, India (3MV tandem Pelletron accelerator). Interestingly, the AMS date was given as 1520 cal BC (IOPAMS-10), showing a reasonable agreement with the LSC date carried out at BSIP. On botanical grounds, the custard apple is native to South America and the West Indies and was supposed to have been introduced in India by the Portuguese in the 16th century. The present 14C dates of the samples pushes back the antiquity of custard apple on Indian soil to the 2nd millennium BC, favoring a group of specialists proposing diverse arguments for Asian-American transoceanic contacts before the discovery of America by Columbus in AD 1492.
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Wang, Zhibiao, Renguang Wu, Anmin Duan i Xia Qu. "Influence of Eastern Tibetan Plateau Spring Snow Cover on North American Air Temperature and Its Interdecadal Change". Journal of Climate 33, nr 12 (15.06.2020): 5123–39. http://dx.doi.org/10.1175/jcli-d-19-0455.1.

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AbstractPrevious studies revealed the influence of the autumn–winter Tibetan Plateau snow cover on atmospheric circulation and climate in the North American region. The present study documents the relationship between the eastern Tibetan Plateau snow cover and the North American air temperature in spring and the associated physical processes using satellite-based snow cover, reanalysis atmospheric and surface variables, observation-based surface air temperature (SAT), and sea surface temperature (SST). A stable relationship is identified between the eastern Tibetan Plateau snow cover and the North American SAT in spring before the mid-2000s. Positive snow-cover anomalies over the eastern Tibetan Plateau induce cooling in the local atmospheric column. The atmospheric cooling stimulates a large-scale atmospheric wave pattern at the upper level that extends northeastward from the eastern Tibetan Plateau via northeast Asia and the North Pacific to North America. An anomalous high forms over North America, accompanied by anomalous descent. In the northwestern part, the horizontal advection by anomalous southerly winds along the west flank of anomalous anticyclone induces SAT increase. In the central part, the enhanced surface sensible heat flux following anomalous descent-induced downward shortwave radiation increase leads to SAT increase. The relationship between the eastern Tibetan Plateau snow cover and the North American SAT is weakened after the mid-2000s. The weakened relationship is attributed to an intensified impact of tropical central Pacific SST anomalies on the North American SAT variations through a Pacific–North America-like atmospheric circulation pattern, which overcomes the influence of the Tibetan Plateau snow-cover anomalies.
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ZHAO, XIN, DANDAN FENG, YUNTAO LI i HAOYU LIU. "Diversity and distribution of the superfamily Grylloidea (Orthoptera: Ensifera: Gryllidea) in the Nearctic region". Zootaxa 5040, nr 2 (21.09.2021): 283–88. http://dx.doi.org/10.11646/zootaxa.5040.2.7.

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Based on the geographic distribution database of the Orthoptera Species File, the diversity and distribution of the superfamily Grylloidea in the Nearctic region was studied using the statistics and Sorensen dissimilarity coefficient. A total of 164 species or subspecies belonging to 4 families, 9 subfamilies and 27 genera were recorded from this region; among which Gryllidae (93, 56.70%), followed by Trigonidiidae (44, 26.83%), Mogoplistidae (25, 15.24%), and Phalangopsidae (2, 1.22%). The diversity exhibits an asymmetric distribution pattern, with the southeastern coastal plain, the Interior Plateau and Piedmont of the United States was the most abundant. At the same time, the regional similarity of species distribution was analyzed, and the Nearctic was divided into four subregions: Boreal & Arctic zone of North America, Eastern temperate North America, Northeast temperate North America, and Southern North America & western temperate North America.
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Ames, Kenneth M., Kristen A. Fuld i Sara Davis. "Dart and Arrow Points on the Columbia Plateau of Western North America". American Antiquity 75, nr 2 (kwiecień 2010): 287–325. http://dx.doi.org/10.7183/0002-7316.75.2.287.

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The timing of the bow and arrow's introduction, spread, and replacement of the atlatl is an important research question in North American prehistory. Although regional archaeologists have not focused on the issue, it is generally thought that the bow and arrow were introduced on the Columbia Plateau ca. 2,300 years ago and completely replaced the atlatl by 1000 B.P. We apply two sets of discriminate functions and four threshold values to three large projectile point samples from the Columbia Plateau and a control sample from the Western Great Basin. Our results indicate that the atlatl was used on the Plateau by ca. 10,800 B.P. While the bow and arrow may have been present by 8500 B.P., they were ubiquitous in the region by 4400 B.P. Atlatl use appears to have increased for a while after 3000 B.P. At the same time, metric differences between dart and arrow points strengthened. Darts became rare after 1500 B.P. but seem to have been in use in small numbers at least until contact.
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Foster II, H. Thomas, i Arthur D. Cohen. "Palynological Evidence of the Effects of the Deerskin Trade on Forest Fires during the Eighteenth Century in Southeastern North America". American Antiquity 72, nr 1 (styczeń 2007): 35–51. http://dx.doi.org/10.2307/40035297.

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Three palynological cores from the coastal plain of Georgia and Alabama were analyzed for paleobotanical remains. Results show that the Indians of southeastern North America increased forest fires used in hunting as a response to the demand for deer hides during the early eighteenth century. Palynological data are consistent with known anthropogenic changes in the region. Charcoal abundance increased significantly between A.D. 1715 and 1770, which is the period of the most intensive hunting by the Indians. This study shows that forest fires from hunting had a significant and measurable effect on the evolution of the biophysical environment.
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Gamble, Lynn H. "Archaeological Evidence for the Origin of the Plank Canoe in North America". American Antiquity 67, nr 2 (kwiecień 2002): 301–15. http://dx.doi.org/10.2307/2694568.

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Advanced maritime technology associated with long-distance exchange and intensified resource acquisition has been linked to the development of stratification and greater sociopolitical complexity in the Pacific Rim region. One such example is the emergence of hereditary chiefs among the Chumash Indians of southern California. Plank boats owned by an elite group of wealthy individuals and chiefs were an integral part of an elaborate economic system that was based on maritime exchange. An artifact assemblage associated with the construction, maintenance, and use of this watercraft was identified and analyzed. It included wooden planks, asphaltum plugs, asphaltum caulking, and chipped stone drills. Radiocarbon dates and other relative-dating techniques provide strong evidence that the plank canoe originated at least 1,300 years ago in southern California. This represents the earliest use of this type of watercraft in North America and probably in the New World. The timing of this innovation provides evidence that sociopolitical complexity developed in the region at least 500 years earlier than previously proposed.
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Liu, Shizuo, Qigang Wu, Steven R. Schroeder, Yonghong Yao, Yang Zhang, Tongwen Wu, Lei Wang i Haibo Hu. "Near-Global Atmospheric Responses to Observed Springtime Tibetan Plateau Snow Anomalies". Journal of Climate 33, nr 5 (1.03.2020): 1691–706. http://dx.doi.org/10.1175/jcli-d-19-0229.1.

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AbstractPrevious studies show that there are substantial influences of winter–spring Tibetan Plateau (TP) snow anomalies on the Asian summer monsoon and that autumn–winter TP heavy snow can lead to persisting hemispheric Pacific–North America-like responses. This study further investigates global atmospheric responses to realistic extensive spring TP snow anomalies using observations and ensemble transient model integrations. Model ensemble simulations are forced by satellite-derived observed March–May TP snow cover extent and snow water equivalent in years with heavy or light TP snow. Heavy spring TP snow causes simultaneous significant local surface cooling and precipitation decreases over and near the TP snow anomaly. Distant responses include weaker surface cooling over most Asian areas surrounding the TP, a weaker drying band extending east and northeast into the North Pacific Ocean, and increased precipitation in a region surrounding this drying band. Also, there is tropospheric cooling from the TP into the North Pacific and over most of North America and the North Atlantic Ocean. The TP snow anomaly induces a negative North Pacific Oscillation/western Pacific–like teleconnection response throughout the troposphere and stratosphere. Atmospheric responses also include significantly increased Pacific trade winds, a strengthened intertropical convergence zone over the equatorial Pacific Ocean, and an enhanced local Hadley circulation. This result suggests a near-global impact of the TP snow anomaly in nearly all seasons.
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Jin, L., Y. Peng, F. Chen i A. Ganopolski. "Modeling sensitivity study of the possible impact of snow and glaciers developing over Tibetan Plateau on Holocene African-Asian summer monsoon climate". Climate of the Past Discussions 4, nr 6 (11.12.2008): 1265–87. http://dx.doi.org/10.5194/cpd-4-1265-2008.

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Abstract. The impacts of various scenarios of snow and glaciers developing over the Tibetan Plateau on climate change in Afro-Asian monsoon region and other regions during the Holocene (9 kyr BP–0 kyr BP) are studied by using the coupled climate model of intermediate complexity, CLIMBER-2. The simulations show that the imposed snow and glaciers over the Tibetan Plateau in the mid-Holocene induce global summer temperature decreases, especially in the northern parts of Europe, Asia, and North America. At the same time, with the imposed snow and glaciers, summer precipitation decreases strongly in North Africa and South Asia as well as northeastern China, while it increases in Southeast Asia and the Mediterranean. For the whole period of Holocene (9 kyr BP–0 kyr BP), the response of vegetation cover to the imposed snow and glaciers cover over the Tibetan Plateau is not synchronous in South Asia and in North Africa, showing an earlier and a more rapid decrease in vegetation cover in North Africa from 9 to 6 kyr BP while it has only minor influence on that in South Asia until 5 kyr BP. Imposed gradually increased snow and glacier cover over the Tibetan Plateau causes temperature increases in South Asia and it decreases in North Africa and Southeast Asia during 6 kyr BP to 0 kyr BP. The precipitation decreases rapidly in North Africa and South Asia while it decreases slowly or unchanged during 6 kyr BP to 0 kyr BP with imposed snow and glacier cover over the Tibetan Plateau. The different scenarios of snow and glacier developing over the Tibetan Plateau would result in differences in variation of temperature, precipitation and vegetation cover in North Africa, South Asia and Southeast Asia. The model results show that the response of climate change in African-Asian monsoon region to snow and glacier cover over the Tibetan Plateau is in the way that the snow and glaciers amplify the effect of vegetation feedback and, hence, further amplify orbital forcing.
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Shagapova, G. R. "Ethno-cultural contacts of ancestors of the Khanty and Mansi peoples based on the materials of game culture". Bulletin of Ugric studies 10, nr 4 (2020): 748–58. http://dx.doi.org/10.30624/2220-4156-2020-10-4-748-758.

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Introduction: game culture of the Khanty end Mansi peoples has been developed over a long period of time, and it reveals different game plots, analogies of which we can find only in the Far East, Amur region, North-East of Russia and in North America. This allows us to determine the directions of the oldest contacts of migrations and cultural borrowings. Objective: to reveal common game plots in the culture of the Ob Ugrians and the peoples of the Far East and the North- East of Russia with following determination of the time and place of their emergence. Research materials: game plots published in works on the game culture of the Ob Ugrians, the peoples of the Far East, the Amur region, the North-East of Russia, and the Indians of North America. Results and novelty of the research: two games «The Snow Snake» and «Get Into the Ring With A Spear» were revealed, which linked the game cultures of Western Siberia, the Far East, the Amur region and North America, as well as at least three original stories: games with a large number of stones, various types of jumping, and jumping over sledges (narty) of the Khanty and Mansi peoples, which found analogies with the games of the peoples of the Far East and the North-East of Russia. The same type of rules, similar game equipment, and the male character of the games are observed. The author comes to the conclusion that the considered games originate from the oldest male rituals that came to America with Paleolithic migrants and have been preserved in the format of games. The games of the Eskimos, Chukchi, Koryaks and peoples of the Amur region, as well as the Ob Ugrians, indicate the existence of a common cultural space at a later time, but not earlier than the Paleolithic. Subsequently, the unity was destroyed: tribes and cultures migrated to the North-West (the ancestors of the Khanty and Mansi), to the North-East (the ancestors of the Chukchi, Koryaks, Evenks, etc.), and to the East (the ancestors of the peoples of the Amur region and the Far East). The novelty of the work lies in the fact that the game culture of the mentioned ethnic groups in a comparative aspect has not previously been the subject of scientific research.
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Rozprawy doktorskie na temat "Indians of North America – Plateau region"

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HENDERSON, ERIC BRUCE. "WEALTH, STATUS AND CHANGE AMONG THE KAIBETO PLATEAU NAVAJO (ARIZONA)". Diss., The University of Arizona, 1985. http://hdl.handle.net/10150/187979.

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This study focuses on the wealth stratification system of the Navajo of the Kaibeto Plateau. The Kaibeto Plateau was settled by the Navajo in the mid-nineteenth century. By the 1930s they had developed an economically and socially stratified society rooted in a livestock economy and influenced by institutions of the surrounding society. In the years since livestock activities have been severely constrained by the federal government: Holdings have been radically decreased and pastoralism has ceased to be the main source of income and subsistence. These changes are described and analyzed. Wealth stratification is conceived of as a phenomenon to be explained and one which has implications for the study of social change. In the 1930s a handful of families owned most of the livestock in the region. These families were, uniformly, descendants of the wealthier and more prominent early settlers. Even after federal programs destroyed the economic advantage these wealthy families possessed, the children of the relatively wealthy have, at least until recent years, continued to prosper (relative to their poorer neighbors) in various ways. They have, on average, higher levels of educational attainment and better occupational profiles. The different responses of individuals at different levels in the social hierarchy have effected the composition of the rural population. More descendants of the wealthy have moved away and/or married individuals from distant communities. Social structures which functioned in the livestock economy to integrate families in the region have disintegrated. The chapter has emerged as an important social and political unit. Although the wealthy families seemed to have dominated chapter politics initially, recent elections indicate a declining influence. The historical facts reported here indicate the importance of social variability in the study of social change. It is argued that the Navajo were never a socially homogeneous group. Thus institutional pressures and shifting government policies have not affected all families in the same manner. Such findings have implications not only for the way in which anthropologists theorize about tribal people and social change, but also have implications for those responsible government officials who seek to formulate solutions to perceived problems on contemporary American Indian reservations.
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Harmon, Alexandra. "A different kind of Indians : negotiating the meanings of "Indian" and "tribe" in the Puget Sound region, 1820s-1970s /". Thesis, Connect to this title online; UW restricted, 1995. http://hdl.handle.net/1773/10446.

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Fierst, John Timothy. "The struggle to defend Indian authority in the Ohio Valley-Great Lakes region, 1763-1794". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2001. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/MQ57540.pdf.

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Atwell, Ricky Gilmer. "Subsistence variability on the Columbia Plateau". PDXScholar, 1989. https://pdxscholar.library.pdx.edu/open_access_etds/4048.

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Long-term human dietary change is a poorly understood aspect of Columbia Plateau prehistory. Faunal assemblages from thirty-four archaeological sites on the Plateau are organized into fifteen aggregate assemblages that are defined spatially and temporally. These assemblages are examined in terms of a focal-diffuse model using ecological measures of diversity, richness and evenness. Variability and patterning in the prehistoric subsistence record is indicated. Major trends in human diet and shifts in subsistence economies are documented and the relationship between subsistence and some initial semi-sedentary adaptations on the Plateau is clarified.
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Elixhauser, Sophie. "Nammeq : personal autonomy and everyday communication in the Ammassalik Region, East Greenland". Thesis, University of Aberdeen, 2011. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=166166.

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Tegtmeier, Kristen Anne. "Bleeding borders : the intersection of gender, race, and region in territorial Kansas /". Digital version accessible at:, 2000. http://wwwlib.umi.com/cr/utexas/main.

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Archibald, Samantha L., i University of Lethbridge Faculty of Arts and Science. "Contested heritage : an analysis of the discourse on The spirit sings". Thesis, Lethbridge, Alta. : University of Lethbridge, Faculty of Arts and Science , 1995, 1995. http://hdl.handle.net/10133/27.

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This thesis contributes to the knowledge of museology, anthropology and Native American studies. It is an analysis of the discourse that surrounded The Spirit Sings: Artistic Traditions of Canada's First Peoples, an exhibition prepared by the Glenbow in Calgary as the 'flagship' of the Olympic Arts Festival in 1988. After the Lubicon Indians of Northern Alberta called for a boycott of The Spirit Sings, in attempt to draw critical attention to their long outstanding lands claim, a large and heated debate ensued involving several disciplines, particularly anthropology and museology. Much of this debate took place in the print media, therefore a large body of material remains to be reviewed and studied. The intent of this thesis is to illustrate that the issue of museological representation of First Nations was one of the most central themes discussed in the discourse, but to argue that the major players dealt with this issue on only the most concrete level and therefore largely neglected to recognize that the issue of First Nation's representation was not just a concern over museum interpretation but more importantly an issue of the contested authenticity of national and cultural claims.
vi, 335 p. ; 29 cm.
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Douglas, Anne. "The significance of James Bay Cree cultural values and practices in school committee policy-making : a documentary study". Thesis, McGill University, 1989. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=59542.

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This documentary study sought to determine the relevance of the James Bay Cree's cultural values and practices to their policy-making process as school committee members. The Cree's formal school system, for which they have full responsibility, is based on the values and practices of non-native society.
Using the historical method, both primary and secondary sources were searched for relevant information concerning Cree culture and its distinguishing characteristics. Evidence of a distinct egalitarian society, practicing consensus, reciprocity and communal land use was found. Sources also indicated the continuing existence and adaptability of Cree values and practices despite prolonged interaction with non-native society.
This thesis proposes that these cultural values and practices predispose the Cree to be effective school committee members. The study provides data for a possible future ethnographic study of Cree school committee participation. Further research could also focus on the policy-making process required of Cree school board members.
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Fish, Suzanne K. "Agriculture and society in arid lands a Hohokam case study /". Diss., The University of Arizona, 1993. http://etd.library.arizona.edu/etd/GetFileServlet?file=file:///data1/pdf/etd/azu_e9791_1993_589_sip1_w.pdf&type=application/pdf.

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Thesis (Ph. D.)--University of Arizona, 1993.
"In addition to chapters [leaves 20-57] unique to the dissertation, ten papers are included that were published during the period of doctoral enrollment"--Leaf 19. Includes bibliographical references.
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Hinshaw, Michael Lloyd. "Ethnohistoric study of culture retention and acculturation among the Great Lakes and Oklahoma Odawa". Virtual Press, 1996. http://liblink.bsu.edu/uhtbin/catkey/1020186.

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This study examines the history and culture of the Odawa people from their prehistory until the present time. This paper looks at a creation story of the Odawa to see how they perceived their own beginnings. Following this, there is an examination of the prehistory, protohistory and history of this people. The section on the history of this people is broken up into three major periods---French, British and American. In the course of this examination, it is discovered that they were originally part of the loosely structured Anishnaabeg (People), or the Ojibwa, Odawa and Potawatomi, which were made up of separate bands. They then coalesced into the Odawa, primarily under the influences of European contact. Finally, in the American period, they split into two main groupings---the Great Lakes and Oklahoma. This paper explores why the Oklahoma group ended up acculturated while the Great Lakes bands retained their culture.
Department of Anthropology
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Książki na temat "Indians of North America – Plateau region"

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Boulé, Mary Null. Plateau region: Yakama people. Vashon, WA: Merryant Publishers, 1997.

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Boulé, Mary Null. Plateau region: Nez Percé people. Vashon, WA: Merryant Publishers, 1998.

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Legacy on stone: Rock art of the Colorado plateau and four corners region. Boulder, Colo: Johnson Books, 1990.

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Cole, Sally J. Legacy on stone: Rock art of the Colorado Plateau and Four Corners Region. Boulder, Colo: Johnson Books, 2008.

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Cox, Beverly. Spirit of the Harvest: North American Indian Cooking. New York, NY: Stewart, Tabori & Chang, 1991.

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Ditchfield, Christin. Plateau Indians. Chicago, Ill: Heinemann Library, 2012.

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Ditchfield, Christin. Plateau Indians. Chicago, Ill: Heinemann Library, 2012.

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E, Walker Deward, Sturtevant William C i Smithsonian Institution, red. Plateau. Washington, D.C: Smithsonian Institution, 1998.

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Hetzler, Richard. The Mitsitam Cafe Cookbook: Recipes from the Smithsonian National Museum of the American Indian. Golden, CO: Fulcrum Publishing, 2010.

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Doherty, Craig A. Plateau Indians. New York: Chelsea House, 2007.

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Części książek na temat "Indians of North America – Plateau region"

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Kimber, Clarissa T., i Darrel McDonald. "Sacred and Profane Uses of the Cactus Lophophora Williamsii from the South Texas Peyote Gardens". W Dangerous Harvest. Oxford University Press, 2004. http://dx.doi.org/10.1093/oso/9780195143201.003.0013.

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Peyote is one of the best-known plant sources for a psychedelic experience. This small cactus is also associated in the popular mind with North American Indians and Hippies. Although its ritual use is thought to be over 7,000 years old (Furst 1989, cited in Schaefer 1996: 141), its use by Indians of the Native American Church (NAC) is less than 100 years old. The peyote button is the essential ingredient in the ritual ceremony associated with NAC meetings and is referred to as “the medicine” by those who regard the button as a god-being and ingest it as a sacrament (Slotkin 1956: 29; Smith and Snake 1996: 80, 91, 105–6). Even more recently, non-Indians have formed churches (the Neo American Church) to follow the Peyote Way or Road (Trout 1999: 47). Secular uses of peyote are as medicine, especially for topical application to the skin on open wounds (Schultes 1940), for divination to discover something lost or when possible attacks of the enemy will occur; or for mind-altering experiences of a nonreligious nature, that is, for recreation. These nonritual (profane) uses have a long history, but peyote’s more significant sacred use in the United States, as measured by numbers of participants, has been in force for little more than 100 years. Various plants are called peyote in Mexico (Schultes 1938: 157), and their usage in the public and official literature of Texas and the United States has not been precise over the years (Morgan 1976: 12, La Barre 1975: 14–17). The major confusion over the common name among field anthropologists and government officials has been with the mescal bean, or Texas mountain laurel [Sophora secundiflora (Ort.) DC]. This hardy, small tree produces a hard, highly toxic, red seed, which has had a long history of ritual use by Amerinds (La Barre 1975: 15). The distribution of the mescal bean is on the southern edge of the Edwards Plateau, on the caliche cuestas in the Rio Grande Plains, and in the mountains of the Trans-Pecos. The native Americans of this region strung the beans into necklaces or bracelets, and a shaman might have passed down to another shaman some of these items as important paraphernalia.
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Pritzker, Barry M. "California". W A Native American Encyclopedia, 112–61. Oxford University PressNew York, NY, 2000. http://dx.doi.org/10.1093/oso/9780195138979.003.0002.

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Abstract California,” in the context of this chapter, corresponds approximately to the present state of California. It omits the southeastern deserts because the Indian cultures of those deserts are usually considered part of the Southwest. Nor does it cover the region east of the Sierra Nevada (Great Basin), the extreme northeast of the state (Plateau), or Baja California (Mexico). The region contains two great mountain ranges, the Coastal and the Sierra Nevada; two major rivers, the Sacramento and the San Joaquin, and many minor river systems; roughly 1,100 miles of coast; interior semidesert; and, at least before the nineteenth century, huge areas of grassland in the central valleys. Much of California’s climate may be categorized as Mediterranean, with the north, west, and highlands in general receiving more precipitation than the south, east, and lowlands.
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"Images from the Region of the Pueblo Indians of North America". W Images from the Region of the Pueblo Indians of North America, 1–54. Ithaca, NY: Cornell University Press, 2017. http://dx.doi.org/10.7591/9781501707704-003.

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Graham, Alan. "Late Cretaceous through Early Eocene North American Vegetational History: 70-50 Ma". W Late Cretaceous and Cenozoic History of North American Vegetation (North of Mexico). Oxford University Press, 1999. http://dx.doi.org/10.1093/oso/9780195113426.003.0008.

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At the end of the Cretaceous the Appalachian Mountains had undergone 180 m.y. of erosion since their principal uplift in the Middle Pennsylvanian through the Late Permian (300-250 Ma), but they were higher and more rugged than at present and provided a somewhat more diverse vertically zoned array of habitats. In contrast, the Rocky Mountains were only ~1 km above sea level at 65 Ma; the Coast Ranges, Sierra Nevada, and Cascade Mountains would not attain substantial heights until late in the Tertiary. Computer models in the NM mode, which simulate conditions in western North America in the Late Cretaceous, show a nearly continuous westerly jet stream with relatively small amplitude between the troughs (lowpressure systems) and ridges (high-pressure systems). The present north-south seasonal meandering of the jet stream was also less. Thus, in the models precipitation and temperatures were more uniform throughout the year and there was less regional differentiation in climate. CO2 concentrations during the Cretaceous are estimated to have been 4-8 times to 10-12 times higher than at present. With a 2-5°C warming for each doubling of CO2, this provides part of the explanation for the higher MAT documented for the Late Cretaceous and Early Tertiary. High CO2 concentrations near the end of the Cretaceous may have been a holdover from earlier intense volcanism in the South Pacific that began to subside at ~ 100 Ma. The term epeirogeny refers to vertical motions of the Earth’s crust, and these movements affect the ocean floor, as well as the continents. There was a 50% increase in the production of ocean crust in the Middle Cretaceous compared to earlier times, as represented by the early Aptian Ontong Java Plateau, the Earth’s largest oceanic plateau, now submerged over 2 km off the Solomon Islands. A sense of the magnitude of this structure can be gained by comparing its volume with that of the surface-exposed Deccan Traps of India (66 Ma). The latter are ~1 km thick and have a volume of 1.5 x 106 km3. The Ontong Java Plateau is ~36 km thick and has a volume of 50 x 106 km3.
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Flick, Alex J., i Julia A. King. "“We Can Fly No Farther”". W The Archaeology of Removal in North America, 19–44. University Press of Florida, 2019. http://dx.doi.org/10.5744/florida/9780813056395.003.0002.

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Chapter 2 by Alex Flick and Julia King explores the relationship between memory, place, and the post-Contact dispossession of indigenous lands on Maryland’s western shore. Documentary, oral, and archaeological evidence reveal how the colonial dispossession of land and the accompanying displacement of Native people proceeded hand in hand with the removal and/or appropriation of the material signs of the indigenous past. Displaced people, however, resisted this erasure in the remaking of place. Those who left the region adopted new practices while retaining familiar ones including, in the case of the Maryland Indians, a persistence in hunting, wigwam, and canoe construction and in mortuary practices reminiscent of ossuary practices known in the homeland. Those who remained in the region maintained and perpetuated memories of culturally significant places through repeated acts of visitation and oral tradition.
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"Prefatory Note". W Images from the Region of the Pueblo Indians of North America, vii—x. Ithaca, NY: Cornell University Press, 2017. http://dx.doi.org/10.7591/9781501707704-001.

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"List of Illustrations". W Images from the Region of the Pueblo Indians of North America, xi—xiv. Ithaca, NY: Cornell University Press, 2017. http://dx.doi.org/10.7591/9781501707704-002.

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"Notes". W Images from the Region of the Pueblo Indians of North America. Ithaca, NY: Cornell University Press, 2017. http://dx.doi.org/10.7591/9781501707704-004.

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"Aby Warburg's Kreuzlingen Lecture: A Reading". W Images from the Region of the Pueblo Indians of North America, 59–109. Ithaca, NY: Cornell University Press, 2017. http://dx.doi.org/10.7591/9781501707704-005.

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"Notes". W Images from the Region of the Pueblo Indians of North America, 110–14. Ithaca, NY: Cornell University Press, 2017. http://dx.doi.org/10.7591/9781501707704-006.

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Streszczenia konferencji na temat "Indians of North America – Plateau region"

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Ruleman, Cal, Adam M. Hudson, Marc W. Caffee i Keith A. Brugger. "THE MIDDLE PLEISTOCENE UNCONFORMITY AND MIS 12-11 (~478-385 KA): GLACIOFLUVIAL PROCESSES OVERRIDE LATE MIOCENE-MIDDLE PLEISTOCENE (~6 MA-500 KA) TECTONO-MAGMATIC CAPTURE AND DEEP-CANYON INCISION, WESTERN GREAT PLAINS-SOUTHERN ROCKY MOUNTAINS-COLORADO PLATEAU REGION, NORTH AMERICA". W GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-339129.

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