Columbia Plateau Indian Place Names: What Can They Teach Us?
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Computational Challenges for Polysynthetic Languages
Computational Modeling of Polysynthetic Languages Judith L. Klavans, Ph.D. US Army Research Laboratory 2800 Powder Mill Road Adelphi, Maryland 20783 [email protected] [email protected] Abstract Given advances in computational linguistic analysis of complex languages using Machine Learning as well as standard Finite State Transducers, coupled with recent efforts in language revitalization, the time was right to organize a first workshop to bring together experts in language technology and linguists on the one hand with language practitioners and revitalization experts on the other. This one-day meeting provides a promising forum to discuss new research on polysynthetic languages in combination with the needs of linguistic communities where such languages are written and spoken. Finally, this overview article summarizes the papers to be presented, along with goals and purpose. Motivation Polysynthetic languages are characterized by words that are composed of multiple morphemes, often to the extent that one long word can express the meaning contained in a multi-word sentence in lan- guage like English. To illustrate, consider the following example from Inuktitut, one of the official languages of the Territory of Nunavut in Canada. The morpheme -tusaa- (shown in boldface below) is the root, and all the other morphemes are synthetically combined with it in one unit.1 (1) tusaa-tsia-runna-nngit-tu-alu-u-junga hear-well-be.able-NEG-DOER-very-BE-PART.1.S ‘I can't hear very well.’ Kabardian (Circassian), from the Northwest Caucasus, also shows this phenomenon, with the root -še- shown in boldface below: (2) wə-q’ə-d-ej-z-γe-še-ž’e-f-a-te-q’əm 2SG.OBJ-DIR-LOC-3SG.OBJ-1SG.SUBJ-CAUS-lead-COMPL-POTENTIAL-PAST-PRF-NEG ‘I would not let you bring him right back here.’ Polysynthetic languages are spoken all over the globe and are richly represented among Native North and South American families. -
Linguistics 203 - Languages of the World Language Study Guide
Linguistics 203 - Languages of the World Language Study Guide This exam may consist of anything discussed on or after October 20. Be sure to check out the slides on the class webpage for this date onward, as well as the syntax/morphology language notes. This guide discusses the aspects of specific languages we looked at, and you will want to look at the notes of specific languages in the ‘language notes: syntax/morphology’ section of the webpage for examples and basic explanations. This guide does not discuss the linguistic topics we discussed in a more general sense (i.e. where we didn’t focus on a specific language), but you are expected to understand these area as well. On the webpage, these areas are found in the ‘lecture notes/slides’ section. As you study, keep in mind that there are a number of ways I might pose a question to test your knowledge. If you understand the concept, you should be able to answer any of them. These include: Definitional If a language is considered an ergative-absolutive language, what does this mean? Contrastive (definitional) Explain how an ergative-absolutive language differs from a nominative- accusative language. Identificational (which may include a definitional question as well...) Looking at the example below, identify whether language A is an ergative- absolutive language or a nominative accusative language. How do you know? (example) Contrastive (identificational) Below are examples from two different languages. In terms of case marking, how is language A different from language B? (ex. of ergative-absolutive language) (ex. of nominative-accusative language) True / False question T F Basque is an ergative-absolutive language. -
What Are the Limits of Polysynthesis?
International Symposium on Polysynthesis in the World's Languages February 20-21, 2014 NINJAL, Tokyo What are the limits of Polysynthesis? Michael Fortescue, Marianne Mithun, and Nicholas Evans Of the various labels for morphological types currently in use by typologists ‘polysynthesis’ has proved to be the most difficult to pin down. For some it just represents an extreme on the dimension of synthesis (one of Sapir’s two major typological axes) while for others it is an independent category or parameter with far- reaching morphosyntactic ramifications. A recent characterization (Evans & Sasse 2002: 3f.) is the following: ‘Essentially, then, a prototypical polysynthetic language is one in which it is possible, in a single word, to use processes of morphological composition to encode information about both the predicate and all its arguments, for all major clause types [....] to a level of specificity, allowing this word to serve alone as a free-standing utterance without reliance on context.’ If the nub of polysynthesis is the packing of a lot of material into single verb forms that would be expressed as independent words in less synthetic languages, what exactly is the nature of and limitations on this ‘material’? The present paper investigates the limits – both upwards and downwards – of what the term is generally understood to cover. Reference Evans, N. & H.-J. Sasse (eds.). (2002). Problems of Polysynthesis. Berlin: Akademie Verlag. 1 2014-01-08 International Symposium on Polysynthesis in the World's Languages February 20-21, 2014 NINJAL, Tokyo Polysynthesis in Ainu Anna Bugaeva (National Institute for Japanese Language and Linguistics) Ainu is a typical polysynthetic language in the sense that a single complex verb can express what takes a whole sentence in most other languages. -
Flood Basalts and Glacier Floods—Roadside Geology
u 0 by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 WASHINGTON STATE DEPARTMENTOF Natural Resources Jennifer M. Belcher - Commissioner of Public Lands Kaleen Cottingham - Supervisor FLOOD BASALTS AND GLACIER FLOODS: Roadside Geology of Parts of Walla Walla, Franklin, and Columbia Counties, Washington by Robert J. Carson and Kevin R. Pogue WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Information Circular 90 January 1996 Kaleen Cottingham - Supervisor Division of Geology and Earth Resources WASHINGTON DEPARTMENT OF NATURAL RESOURCES Jennifer M. Belcher-Commissio11er of Public Lands Kaleeo Cottingham-Supervisor DMSION OF GEOLOGY AND EARTH RESOURCES Raymond Lasmanis-State Geologist J. Eric Schuster-Assistant State Geologist William S. Lingley, Jr.-Assistant State Geologist This report is available from: Publications Washington Department of Natural Resources Division of Geology and Earth Resources P.O. Box 47007 Olympia, WA 98504-7007 Price $ 3.24 Tax (WA residents only) ~ Total $ 3.50 Mail orders must be prepaid: please add $1.00 to each order for postage and handling. Make checks payable to the Department of Natural Resources. Front Cover: Palouse Falls (56 m high) in the canyon of the Palouse River. Printed oo recycled paper Printed io the United States of America Contents 1 General geology of southeastern Washington 1 Magnetic polarity 2 Geologic time 2 Columbia River Basalt Group 2 Tectonic features 5 Quaternary sedimentation 6 Road log 7 Further reading 7 Acknowledgments 8 Part 1 - Walla Walla to Palouse Falls (69.0 miles) 21 Part 2 - Palouse Falls to Lower Monumental Dam (27.0 miles) 26 Part 3 - Lower Monumental Dam to Ice Harbor Dam (38.7 miles) 33 Part 4 - Ice Harbor Dam to Wallula Gap (26.7 mi les) 38 Part 5 - Wallula Gap to Walla Walla (42.0 miles) 44 References cited ILLUSTRATIONS I Figure 1. -
Syllable Structure in Umatilla Sahaptin* Tymoteusz Alan Chrzanowski
Syllable Structure in Umatilla Sahaptin* Tymoteusz Alan Chrzanowski A thesis submitted in partial fulfillment of the requirements for the degree of Bachelor of Arts in Linguistics Swarthmore College December 2018 Abstract Umatilla Sahaptin is a Shaptian language spoken in North-Eastern Oregon by the Umatilla tribe. While it has some documentation, such as a dictionary and sketch grammar, there are still acknowledged gaps in the literature. The purpose of this thesis is to fill one of those gaps with a description of syllable structure. To do this I compare data gathered from speakers of Umatilla with published accounts of sylla ble structure in the mutually intelligible sister language Yakima. After establishing what is meant by syllable structure and what is known about Yakima, I discuss the data I gathered. Using word list and sentence elicitations, stories, poems, and songs I conclude that Umatilla syllable structure is very similar to Yakima's, with some differences, namely in maximal margins, minimal words, and licensing of sonority sequence defying clusters. 'I would like to thank my consultants, Thomas Morningowl and Mildred Quaemptes, since it was their time and knowledge that made this work possible at all. I would also like to thank the Confederated Tribes of the Umatilla, for the privilege of working with the tribe, specifically the Language Program, the Education Commission, and the Board of Trustees. In particular I would like to thank Modesta Minthorn, for her help and guidance through the process of securing per mission for my work and scheduling time to do it. I would also like to thank the Eugene M. -
Characterization of Ecoregions of Idaho
1 0 . C o l u m b i a P l a t e a u 1 3 . C e n t r a l B a s i n a n d R a n g e Ecoregion 10 is an arid grassland and sagebrush steppe that is surrounded by moister, predominantly forested, mountainous ecoregions. It is Ecoregion 13 is internally-drained and composed of north-trending, fault-block ranges and intervening, drier basins. It is vast and includes parts underlain by thick basalt. In the east, where precipitation is greater, deep loess soils have been extensively cultivated for wheat. of Nevada, Utah, California, and Idaho. In Idaho, sagebrush grassland, saltbush–greasewood, mountain brush, and woodland occur; forests are absent unlike in the cooler, wetter, more rugged Ecoregion 19. Grazing is widespread. Cropland is less common than in Ecoregions 12 and 80. Ecoregions of Idaho The unforested hills and plateaus of the Dissected Loess Uplands ecoregion are cut by the canyons of Ecoregion 10l and are disjunct. 10f Pure grasslands dominate lower elevations. Mountain brush grows on higher, moister sites. Grazing and farming have eliminated The arid Shadscale-Dominated Saline Basins ecoregion is nearly flat, internally-drained, and has light-colored alkaline soils that are Ecoregions denote areas of general similarity in ecosystems and in the type, quality, and America into 15 ecological regions. Level II divides the continent into 52 regions Literature Cited: much of the original plant cover. Nevertheless, Ecoregion 10f is not as suited to farming as Ecoregions 10h and 10j because it has thinner soils. -
Historical and Current Forest and Range Landscapes in the Interior
United States Department of Historical and Current Forest Agriculture Forest Service and Range Landscapes in the Pacific Northwest Research Station United States Interior Columbia River Basin Department of the Interior and Portions of the Klamath Bureau of Land Management General Technical and Great Basins Report PNW-GTR-458 September 1999 Part 1: Linking Vegetation Patterns and Landscape Vulnerability to Potential Insect and Pathogen Disturbances Authors PAUL F. HESSBURG is a research plant pathologist and R. BRION SALTER is a GIS analyst, Pacific Northwest Research Station, Forestry Sciences Laboratory, 1133 N. Western Avenue, Wenatchee, WA 98801; BRADLEY G. SMITH is a quantitative ecologist, Pacific Northwest Region, Deschutes National Forest, 1645 Highway 20 E., Bend, OR 97701; SCOTT D. KREITER is a GIS analyst, Wenatchee, WA; CRAIG A. MILLER is a geographer, Wenatchee, WA; CECILIA H. McNICOLL was a plant ecol- ogist, Intermountain Research Station, Fire Sciences Laboratory, and is currently at Pike and San Isabel National Forests, Leadville Ranger District, Leadville, CO 80461; and WENDEL J. HANN was the regional ecologist, Northern Region, Intermountain Fire Sciences Laboratory, and is currently the National Landscape Ecologist stationed at White River National Forest, Dillon Ranger District, Silverthorne, CO 80498. Historical and Current Forest and Range Landscapes in the Interior Columbia River Basin and Portions of the Klamath and Great Basins Part 1: Linking Vegetation Patterns and Landscape Vulnerability to Potential Insect and Pathogen Disturbances Paul F. Hessburg, Bradley G. Smith, Scott D. Kreiter, Craig A. Miller, R. Brion Salter, Cecilia H. McNicoll, and Wendel J. Hann Interior Columbia Basin Ecosystem Management Project: Scientific Assessment Thomas M. -
Final Environmental Impact Statement and Proposed Land-Use Plan Amendments for the Boardman to Hemingway Transmission Line Proje
B2H Final EIS and Proposed LUP Amendments Appendix H—Visual Resources Supporting Data Appendix H VISUAL RESOURCES SUPPORTING DATA This appendix includes the following: Appendix H1 – Visual Analysis Unit Descriptions - Visual Analysis Unit Descriptions Table - Change in Cultural Modification to the Scenic Quality Rating Units Appendix H2 – Contrast Rating Worksheets - Baker Field Office Visual Contrast Rating Worksheets* - Malheur Field Office Visual Contrast Rating Worksheets* - Owyhee Field Office Visual Contrast Rating Worksheets* - Additional Visual Contrast Rating Worksheets Appendix H3 – Photo Simulations - Photo Simulations from Visual Resource Report 1 - Additional Photo Simulations *NOTE: For the Final Environmental Impact Statement, additional route variations have been analyzed. As a result, certain routes analyzed for the Draft Environmental Impact Statement have been renamed. They are as follows: Proposed Action changed to Applicant’s Proposed Action Alternative Burnt River Alternative to Flagstaff A – Burnt River Alternative Flagstaff Hill to Flagstaff A Alternative Double Mountain Alternative to Variation S5-B2 H-1 This page intentionally left blank. B2H Final EIS and Proposed LUP Amendments Appendix H1—Visual Analysis Unit Descriptions Appendix H1 VISUAL ANALYSIS UNIT DESCRIPTIONS The Visual Analysis Unit (VAU) descriptions are provided in Table H1-1, which includes an overall description of each VAU within the B2H Project area for visual resources. The descriptions of the units include information about the landforms, topography, water, and vegetation within the units, as well as other features and information. The VAUs are identified by two digits, followed by three numbers, and a unit name. The two digits represent the BLM field office or resource area in which the unit is located (BR=Border Resource Area; CE=Central Oregon Resource Area; BA=Baker Resource Area; MA=Malheur Resource Area; OW=Owyhee Field Office; FR=Four Rivers Field Office). -
Summary of the Columbia Plateau Regional Aquifer-System Analysis, Washington, Oregon, and Idaho
SUMMARY OF THE COLUMBIA PLATEAU REGIONAL AQUIFER-SYSTEM ANALYSIS, WASHINGTON, OREGON, AND IDAHO PROFESSIONAL PAPER 1413-A USGS tience for a changing world Availability of Publications of the U.S. Geological Survey Order U.S. Geological Survey (USGS) publications from the Documents. Check or money order must be payable to the offices listed below. Detailed ordering instructions, along with Superintendent of Documents. Order by mail from prices of the last offerings, are given in the current-year issues of the catalog "New Publications of the U.S. Geological Superintendent of Documents Survey." Government Printing Office Washington, DC 20402 Books, Maps, and Other Publications Information Periodicals By Mail Many Information Periodicals products are available through Books, maps, and other publications are available by mail the systems or formats listed below: from Printed Products USGS Information Services Box 25286, Federal Center Printed copies of the Minerals Yearbook and the Mineral Com Denver, CO 80225 modity Summaries can be ordered from the Superintendent of Publications include Professional Papers, Bulletins, Water- Documents, Government Printing Office (address above). Supply Papers, Techniques of Water-Resources Investigations, Printed copies of Metal Industry Indicators and Mineral Indus Circulars, Fact Sheets, publications of general interest, single try Surveys can be ordered from the Center for Disease Control copies of permanent USGS catalogs, and topographic and and Prevention, National Institute for Occupational Safety and thematic maps. Health, Pittsburgh Research Center, P.O. Box 18070, Pitts burgh, PA 15236-0070. Over the Counter Mines FaxBack: Return fax service Books, maps, and other publications of the U.S. Geological Survey are available over the counter at the following USGS 1. -
Download the Full Report 2007 5.Pdf PDF 1.8 MB
The Northwest Power and Conservation Council’s Directory of Columbia River Basin Tribes Council Document Number: 2007-05 Table of Contents I. Introduction 1 II. Tribes and Tribal Confederations 5 The Burns Paiute Tribe 7 The Coeur d’Alene Tribe 9 The Confederated Salish and Kootenai Tribes of the Flathead Reservation 12 The Confederated Tribes and Bands of the Yakama Nation 15 The Confederated Tribes of the Colville Reservation 18 The Confederated Tribes of the Grand Ronde Community of Oregon 21 The Confederated Tribes of the Umatilla Indian Reservation 23 The Confederated Tribes of the Warm Springs Reservation of Oregon 25 The Kalispel Tribe of Indians 28 The Kootenai Tribe of Idaho 31 The Nez Perce Tribe 34 The Shoshone Bannock Tribes of the Fort Hall Reservation 37 The Shoshone-Paiute Tribes of the Duck Valley Reservation 40 The Spokane Tribe of Indians 42 III. Canadian First Nations 45 Canadian Columbia River Tribes (First Nations) 46 IV. Tribal Associations 51 Canadian Columbia River Inter-Tribal Fisheries Commission 52 Columbia River Inter-Tribal Fish Commission 53 Upper Columbia United Tribes 55 Upper Snake River Tribes 56 The Northwest Power and Conservation Council’s Tribal Directory i ii The Northwest Power and Conservation Council’s Tribal Directory Introduction The Northwest Power and Conservation Council’s Tribal Directory 1 2 The Northwest Power and Conservation Council’s Tribal Directory Introduction The Council assembled this directory to enhance our understanding and appreciation of the Columbia River Basin tribes, including the First Nations in the Canadian portion of the basin. The directory provides brief descriptions and histories of the tribes and tribal confedera- tions, contact information, and information about tribal fi sh and wildlife projects funded through the Council’s program. -
Reconstructing Proto-Sahaptian Sounds
Reconstructing Proto-Sahaptian Sounds Noel Rude Confederated Tribes of the Umatilla Indian Reservation Sahaptin and the mutually unintelligible Nez Perce comprise the Sahaptian language family. This paper attempts to reconstruct the sound system of the parent language of that family. There is little dialect variation in the available data for Nez Perce, whereas Sahaptin divides into three definable dialect clusters: Columbia River (Umatilla, Tenino, Celilo, etc.); Northwest (Klickitat, Upper Cowlitz, Yakima, etc.); Northeast (Priest Rapids, Walla Walla, Palouse, etc.). Various features distinguish the dialects, e.g., long vowels derived from certain VCV sequences are more common in the Northern dialects and in Nez Perce, the Northeast dialects and Nez Perce are more likely to preserve the glottal stop, and the palatalization of *k is most extensive in the Columbia River dialects. The reconstructions proposed here are, as always, more or less tentative. Unless otherwise indicated the examples labeled Sahaptin (S) are from Umatilla.1 Figure 1. The Sahaptian language family Proto-Sahaptian Nez Perce Sahaptin Columbia River Northern Northwest Northeast 1 For the connection between Sahaptin and Nez Perce, see Aoki (1962), Rigsby (1965), Rigsby and Silverstein (1969), and Rude (1996, 2006). For the relationship with Plateau Penutian, see Aoki (1963), Rude (1987), and Pharis (2006). For a possible relationship within the broader Penutian macro-family, see DeLancey & Golla (1979) and Mithun (1999), also Rude (2000) for a possible connection with Uto-Aztecan. For Sahaptin grammars, see Jacobs (1931), Millstein (ca. 1990a), Rigsby and Rude (1996), Rude (2009), and for published NW Sahaptin texts, see Jacobs (1929, 1934, 1937). Beavert and Hargus (2010) provide a dictionary of Yakima Sahaptin, Millstein (ca. -
2008 Tribal Annual Report
Historical Perspective of the Confederated Tribes of Warm Springs Before settlements began throughout what is known today as the United States of America, Indigenous tribes spread across the North American continent like a sunset across an open front. In what is known today as the Columbia River Gorge (We’Mulx (Kiksht) N’Chi Wana (Ichishkin) Pabahuudu (Numu)), tribes of the Warm Springs Indian Reservation of Oregon developed societies beside the Columbia River, the Cascade Mountains, the John Day River, the Klamath Basin, and southern parts of Oregon and Idaho. From the beginning, our tribes were sustained on these bountiful lands blessed with abundant resources. In 1855, Indian Bands of the Columbia River Basin entered into, what the United States called, a peace treaty relinquishing approximately ten million acres of usual and accustomed lands used by the Indian Bands in the area who were then relocated to designated Indian Reservations located inland from their home in the Gorge. A small band of Paiutes later joined the tribes on the Warm Springs reservation in 1879 after being relocated from their southern Oregon homelands to the Yakima Reservation as prisoners of the Bannock War. Today, all three tribes reside on the reservations as family, friends, and an overall connected community. The Wasco bands on the Columbia River were the eastern-most group of Chinookan and Kiksht speaking Indians. Although they were principally fishermen, their frequent contact with other Indians throughout the region provided for abundant trade. Commerce was succeeded with Chinookan bands such as the Clackamas to the west and Sahaptin bands to the east such as the neighboring Warm Springs and Nez Perce.