Interior Plains Region Might Vary
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Key Terms and Concepts for Exploring Nîhiyaw Tâpisinowin the Cree Worldview
Key Terms and Concepts for Exploring Nîhiyaw Tâpisinowin the Cree Worldview by Art Napoleon A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF ARTS in the Faculty of Humanities, Department of Linguistics and Faculty of Education, Indigenous Education Art Napoleon, 2014 University of Victoria All rights reserved. This thesis may not be reproduced in whole or in part, by photocopy or other means, without the permission of the author. ii Supervisory Committee Key Terms and Concepts for Exploring Nîhiyaw Tâpisinowin the Cree Worldview by Art Napoleon Supervisory Committee Dr. Leslie Saxon, Department of Linguistics Supervisor Dr. Peter Jacob, Department of Linguistics Departmental Member iii ABstract Supervisory Committee Dr. Leslie Saxon, Department of Linguistics Supervisor Dr. Peter Jacob, Department of Linguistics Departmental MemBer Through a review of literature and a qualitative inquiry of Cree language practitioners and knowledge keepers, this study explores traditional concepts related to Cree worldview specifically through the lens of nîhiyawîwin, the Cree language. Avoiding standard dictionary approaches to translations, it provides inside views and perspectives to provide broader translations of key terms related to Cree values and principles, Cree philosophy, Cree cosmology, Cree spirituality, and Cree ceremonialism. It argues the importance of providing connotative, denotative, implied meanings and etymology of key terms to broaden the understanding of nîhiyaw tâpisinowin and the need -
East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 Lrrs N and S
East and Central Farming and Forest Region and Atlantic Basin Diversified Farming Region: 12 LRRs N and S Brad D. Lee and John M. Kabrick 12.1 Introduction snowfall occurs annually in the Ozark Highlands, the Springfield Plateau, and the St. Francois Knobs and Basins The central, unglaciated US east of the Great Plains to the MLRAs. In the southern half of the region, snowfall is Atlantic coast corresponds to the area covered by LRR N uncommon. (East and Central Farming and Forest Region) and S (Atlantic Basin Diversified Farming Region). These regions roughly correspond to the Interior Highlands, Interior Plains, 12.2.2 Physiography Appalachian Highlands, and the Northern Coastal Plains. The topography of this region ranges from broad, gently rolling plains to steep mountains. In the northern portion of 12.2 The Interior Highlands this region, much of the Springfield Plateau and the Ozark Highlands is a dissected plateau that includes gently rolling The Interior Highlands occur within the western portion of plains to steeply sloping hills with narrow valleys. Karst LRR N and includes seven MLRAs including the Ozark topography is common and the region has numerous sink- Highlands (116A), the Springfield Plateau (116B), the St. holes, caves, dry stream valleys, and springs. The region also Francois Knobs and Basins (116C), the Boston Mountains includes many scenic spring-fed rivers and streams con- (117), Arkansas Valley and Ridges (118A and 118B), and taining clear, cold water (Fig. 12.2). The elevation ranges the Ouachita Mountains (119). This region comprises from 90 m in the southeastern side of the region and rises to 176,000 km2 in southern Missouri, northern and western over 520 m on the Springfield Plateau in the western portion Arkansas, and eastern Oklahoma (Fig. -
Physical Geography of the United States and Canada: a Land of Contrasts S
Chapter 5 Guided Notes _________________________________________________________________________________________ NAME Physical Geography of the United States and Canada: A Land of Contrasts s North America’s vast and varied landscape and abundant resources have attracted immigrants and shaped the development of the United States and Canada. Section 1: Landforms and Resources The United States and Canada have vast lands and abundant resources. These two countries share many of the same landforms. Landscape Influenced Development U.S., Canada: former British colonies, most people speak English Strong economic and political ties with one another Vast Lands Canada second largest country in the world by area; U.S. third Together they cover one-eighth of the earth’s land surface Abundant Resources Landmass and natural resources attract immigrants to both countries U.S. and Canada have developed into global economic powers Many and Varied Landforms All major landforms are found in U.S. and Canada; The two countries share mountain chains and interior plains The Appalachian Highlands Appalachian Mountains run 1,600 miles from Newfoundland to Alabama; More than 400 million years old o include Green and Catskill mountains in the north; Blue Ridge and Great Smoky mountains in the south Erosion has created gentle slopes, peaks from 1,200–2,400 feet The Appalachian Trail is a scenic hiking path along the chain The Interior Lowlands Great Plains extend from Missouri River to Rocky Mountains; Interior Plains extend from Appalachians -
Lesson Plans
LESSON PLANS THE NORTH WEST MOUNTED POLICE: RECRUITMENT Recommended grades: 6 -12 Time required: 45 minute class lessons Materials: Images (Choice of students), Formatting paper (11X17 - cardstock or firm paper) Pencils, Markers, Computer fonts, Glue, Map of Canada - 1873 INTRODUCTION When the North West Mounted Police were formed in 1873, the objective of the force was to bring law and order to the Canadian west. As a new force, they needed to recruit young, healthy, hardworking men who were willing to endure hard conditions and follow strict protocol. To do this, the Canadian Government sent out Recruitment and Propaganda posters to try and gain interest in this newly founded force. OBJECTIVES At the end of this lesson, students will be able to: Understand the general history of the North West Mounted Police and why they were formed. Recognize why the NWMP were so important in the formation and protection of the Canadian west and what their role in bringing the nation together was. How recruitment was organized and the role it played in the creation of the force. IMAGES Please have students choose and print images from this section Map Showing NWMP Outposts and Patrols [detail] 1886 Collection of Glenbow Library, G3471-F82-1886-C212 The railway reached the western provinces by 1885, and thousands of newcomers moved in to farm and ranch. A new system of patrols and small outposts was put in place so the NWMP could stay in close touch with these newcomers. Two or three Police were stationed at each small post (red flag on map), and they did daily patrols on horseback (marked in white) throughout the region. -
Landforms and Resources
Name _____________________________ Class _________________ Date __________________ Physical Geography of the United States and Canada Section 1 Landforms and Resources Terms and Names Appalachian Mountains major mountain chain in the eastern United States and Canada Great Plains largely treeless area in the interior lowlands Canadian Shield rocky, flat area that surrounds Hudson Bay Rocky Mountains mountain chain in the western United States and Canada Continental Divide line of the highest points in the Rockies that marks the separation between rivers flowing to the east and to the west Great Lakes five large lakes found in the central United States and Canada Mackenzie River Canada’s longest river Before You Read In the last chapter, you read about human geography–the way humans in general relate to their environment. In this section, you will learn about the physical features and resources of the United States and Canada. As You Read Use a graphic organizer to take notes about the landforms and resources of the United States and Canada. LANDSCAPE INFLUENCED The United States and Canada are rich DEVELOPMENT (Page 117) in natural resources. They have much How vast are these countries? fertile soil and water and many forests and The United States and Canada occupy the minerals. This geographic richness has central and northern four-fifths of the attracted immigrants from around the continent of North America. Culturally, the world for centuries. region is known as Anglo America. This is 1. What binds Canada and the United because both countries were colonies of States together? Great Britain at one time and because most of _______________________________ the people speak English. -
Three Cranes Tavern (1629-1775) Charlestown, Massachsuetts
David Teniers “Tavern Scene” 1658 An Archaeological Reevaluation of the Great House/ Three Cranes Tavern (1629-1775) Charlestown, Massachsuetts By Craig S. Chartier Plymouth Archaeological Rediscovery Project May 2016 Citizens of the Commonwealth were given a rare opportunity to witness the investigation of part of Boston's earliest colonial past during the city's "Big Dig"/ Central Artery Project in 1985, when the Massachusetts Bay Colony's "Great House" was explored prior to the site's destruction (all of the background information presented here, on both the history of the property and the excavations, is based on Gallagher et al 1994). The Great House, located in City Square in Charlestown, was built in 1629 before Boston was even settled. It was to serve as the first residence of Governor Winthrop and the other prominent members of the company and as the colony's meetinghouse. It is believed to have been erected by a party of 100 men from Salem, who had been sent with orders to build it, lay out streets, and survey the two acre lots to be assigned to settlers. Work was begun in June 1629 and was expected to be completed by the time of the arrival of Winthrop's fleet of 11 ships in the summer of the following year. Archaeologists assumed that it was to have been a formal, professionally designed structure symbolizing the hierarchical nature of the new settlement and serving as a link between the old and new worlds. Unfortunately, soon after the fleet's arrival, a great mortality swept the colony, which the settlers attributed to the brackish drinking water in the new settlement. -
"In These Perilous Times": Plague and Plague Policies in Early Modem Denmark
Medical History, 2003, 47: 413-450 "In These Perilous Times": Plague and Plague Policies in Early Modem Denmark PETER CHRISTENSEN* Plague has long since disappeared from Denmark. Why it did so remains a puzzle and is one of the themes of this article. More recently, and almost as puzzling, plague has also disappeared from Danish historiography. In the works of eighteenth-century historians the Black Death was described in considerable, if often imaginative, detail and the recurring plague outbreaks were mentioned regularly.' By the late nineteenth century this was no longer the case. The terrible mortality still guaranteed the Black Death a few lines in the history books, but there was practically no discussion ofthe causes nor ofthe possible short or long-term consequences. The rest ofthe plague cycle was almost completely ignored with the exception of the well-documented, but also isolated, 1711 outbreak in Copenhagen.2 The reason for this revision must be sought in the rise ofmodem historical scholarship in Denmark in the late nineteenth century. As in other countries, history had until then been the preserve of so-called antiquarians who had uncritically paraphrased chronicles and annals, sources which modem critical examination has proved to be biased, inaccurate and unreli- able. Now an emerging group of professional, academic historians, most of them mediev- alists incidentally, argued that henceforward the study of history should be based on solid, objective archival materials such as parish registers, laws, estate accounts, cadastral surveys, minutes, etc. Unfortunately, the sources relevant to the Black Death were sparse * Dr Peter Christensen, Department of History, ' For example, P F Suhm, Historie afDanmark, 14 University of Copenhagen, Njalsgade 102-2300 vols, Copenhagen, 1782-1828, vol. -
Refusing to Hyphenate: Doukhobor Autobiographical Discourse
REFUSING TO HYPHENATE: DOUKHOBOR AUTOBIOGRAPHICAL DISCOURSE By JULIE RAK, M.A. A Thesis Submitted to the School ofGraduate Studies in Partial Fulfilment ofthe Requirements for the Degree Doctorate McMaster University © Copyright by Julie Rak, June 1998 DOCTORATE (1998) (English) McMaster University Hamilton, Ontario TITLE: Refusing to Hyphenate: Doukhobor Autobiographical Discourse AUTHOR: Julie Rak, B.A. (McMaster University), M.A. (Carleton University) SUPERVISOR: Professor Lorraine M. York NUMBER OF PAGES: vi,256 (ii) Abstract My thesis, Refusing to Hyphenate: Doukhobor Autobiographical Discourse brings together recent theories ofautobiography with a consideration ofalternative autobiographical writing and speaking made by a Russian-speaking migrant group, the Doukhobors ofCanada. The situation ofthe Doukhobors is ideal for a consideration of alternate autobiographical forms, since Doukhobors have fallen outside liberal democratic discourses ofCanadian nationalism, land use and religion ever since their arrival in Canada in 1899. They have turned to alternate strategies to retell their own histories against the grain ofthe sensationalist image ofDoukhobors propagated by government commissions and by the Canadian media. My study is the first to recover archived autobiographical material by Doukhobors for analysis. It also breaks new ground by linking new developments in autobiography theory with other developments in diaspora theory, orality and literacy and theories ofperformativity, as well as criticism that takes issues about identity and its relationship to power into account. When they had to partially assimilate by the 1950s, some Doukhobors made autobiographical writings, translations and recordings that included interviews, older autobiographical accounts and oral histories about their identity as a migratory, persecuted people who resist State control. Others recorded their protests against the British Columbian government from the 1930s to the 1960s in collective prison diaries and legal documents. -
Archaeology in Alberta 1978
ARCHAEOLOGY IN ALBERTA, 1978 Compiled by J.M. Hillerud Archaeological Survey of Alberta Occasional Paper No. 14 ~~.... Prepared by: Published by: Archaeological Survey Alberta Culture of Alberta Historical Resources Division OCCASIONAL PAPERS Papers for publication in this series of monographs are produced by or for the four branches of the Historical Resources Division of Alberta Culture: the Provincial Archives of Alberta, the Provincial Museum of Alberta, the Historic Sites Service and the Archaeological Survey of Alberta. Those persons or institutions interested in particular subject sub-series may obtain publication lists from the appropriate branches, and may purchase copies of the publications from the following address: Alberta Culture The Bookshop Provincial Museum of Alberta 12845 - 102 Avenue Edmonton, Alberta T5N OM6 Phone (403) 452-2150 Objectives These Occasional Papers are designed to permit the rapid dissemination of information resulting from Historical Resources' programmes. They are intended primarily for interested specialists, rather than as popular publications for general readers. In the interests of making information available quickly to these specialists, normal production procedures have been abbreviated. i ABSTRACT In 1978, the Archaeological Survey of Alberta initiated and adminis tered a number of archaeological field and laboratory investigations dealing with a variety of archaeological problems in Alberta. The ma jority of these investigations were supported by Alberta Culture. Summary reports on 21 of these projects are presented herein. An additional four "shorter contributions" present syntheses of data, and the conclusions derived from them, on selected subjects of archaeo logical interest. The reports included in this volume emphasize those investigations which have produced new contributions to the body of archaeological knowledge in the province and progress reports of con tinuing programmes of investigations. -
Laurentide Ice Sheet Retreat Around 8000 Years Ago Occurred Over Western Quebec (700-900 Meters/Year)
The retreat chronology of the Laurentide Ice Sheet during the last 10,000 years and implications for deglacial sea-level rise David Ullman University of Wisconsin-Madison, Department of Geoscience Author Profile Shortcut URL: https://serc.carleton.edu/59463 Location Continent: North America Country: Canada State/Province:Quebec, Labrador City/Town: UTM coordinates and datum: none Setting Climate Setting: Tectonic setting: Type: Chronology Show caption Show caption Show caption Description Much of the world's population is located along the coasts. In a world of changing climate, the rate of sea level rise will determine the ability of these communities to adapt to sea level rise. Perhaps the greatest uncertainty in sea level rise prediction has to do with amount of water melting off of Earth's major ice sheets. Recent decades have seen an accelerated loss of ice from Greenland and Antarctica. These bodies of ice may be prone to change more rapid than expected. Greenland and Antarctica contain enough frozen water, which, if melted could raise sea level by 70 m, but predictions on the rate at which this sea level rise could occur depend on scientists' understanding of the complex physics of ice flow (and on future climate scenarios). Paleoclimate researchers study past climates in hopes of developing a better understanding of our current and future climates. Similarly, understanding past ice sheets will aid in future prediction of ice sheet change. At the end of the Last Glacial Maximum, roughly 20,000 years ago, much of Earth in the northern hemisphere was covered in vast ice sheets. -
Soil Ecoregions in Latin America 5
Chapter 1 Soil EcoregionsSoil Ecoregions in Latin Latin America America Boris Volkoff Martial Bernoux INTRODUCTION Large soil units generally reflect bioclimatic environments (the concept of zonal soils). Soil maps thus represent summary documents that integrate all environmental factors involved. The characteristics of soils represent the environmental factors that control the dynamics of soil organic matter (SOM) and determine both their accumulation and degradation. Soil maps thus rep- resent a basis for quantitative studies on the accumulation processes of soil organic carbon (SOC) in soils in different spatial scales. From this point of view, however, and in particular if one is interested in general scales (large semicontinental regions), soil maps have several disadvantages. First, most soil maps take into account the intrinsic factors of the soils, thus the end results of the formation processes, rather than the processes themselves. These processes are the factors that are directly related to envi- ronmental conditions, whereas the characteristics of the soils can be inher- ited (paleosols and paleoalterations) and might no longer be in equilibrium with the present environment. Second, soils seldom are homogenous spatial entities. The soil cover is in reality a juxtaposition of several distinct soils that might differ to various degrees (from similar to highly contrasted), and might be either genetically linked or entirely disconnected. This spatial heterogeneity reflects the con- ditions in which the soils were formed and is expressed differently accord- ing to the substrates and the topography. The heterogeneity also depends on the duration of evolution of soils and the geomorphologic history, either re- gional or local, as well as on climatic gradients, which are particularly obvi- ous in mountain areas. -
Louisiana's Bousillage Tradition
Louisiana’s Bousillage Tradition: Investigation of Past Techniques for Future Practice FITCH MID-CAREER GRANT FINAL REPORT By: Laura Ewen Blokker Principal, Southeast Preservation [email protected] Heather A. Knight Adjunct Assistant Professor, Tulane School of Architecture [email protected] Contents Introduction ..................................................................................................................................... 1 Survey Work ................................................................................................................................... 2 Materials Analysis .......................................................................................................................... 9 Interviews ...................................................................................................................................... 17 Conclusions and Future Directions ............................................................................................... 23 Glossary ........................................................................................................................................ 25 On the cover: Clockwise from left, tacheron trampling Spanish moss into clay for bousillage at Green House by H. Knight; detail of bousillage in Estopinal House by L. Blokker; photomicrograph of Dumesnil House bousillage showing traces of decayed Spanish moss bark by J. Walsh. Introduction This report describes the work of the 2009 Fitch Mid-Career Grant funded project, “Louisiana‟s