Academic literature on the topic 'North straits salish'

This study presents five parallel, interwoven histories of evolving relations between humans and the rest of nature around the Strait of Georgia or North Salish Sea between the 1850s and the 1980s. Together they comprise a complex but coherent portrait of Canada’s most heavily populated coastal zone. Home to about 10% of Canada’s contemporary population, the region defined by this inland sea has been greatly influenced by its relations with the Strait, which is itself the focus of a number of escalating struggles between stakeholders. This study was motivated by a conviction that understanding this region and the sea at the centre of it, the struggles and their stakeholders, requires understanding of at least these five key elements of the Strait’s modern history. Drawing on a range of archival and secondary sources, the study depicts the Strait in relation to human movement, the Strait as a locus for colonial dispossession of indigenous people, the Strait as a multi-faceted resource mine, the Strait as a valuable waste dump and the Strait as a place for recreation / re-creation. Each of these five dimensions of the Strait’s history was most prominent at a different point in the overall period considered and constantly changing relations among the five narratives are an important focus of the analysis. The evolving roles of governance, science, cultural representation and conservationism / environmentalism are considered throughout. The only common element linking the five narratives, apart from the Strait itself, is a pervasive, well-founded fear of loss – fear of a dangerous sea or fear of losing access to the marine highway, fear of losing the Strait as indigenous patrimony or as a colonial entitlement, fear of losing its rich terrestrial and marine resources, fear of losing waste dumping privileges, fear of losing the Strait as recreational space. The study concludes with a brief consideration of the five narratives in the 21st century, their contemporary interactions and their links with the histories considered in this study.
Arts, Faculty of
Geography, Department of
Graduate

This thesis conducted the first acoustic analysis on Lekwungen (aka Songhees, Songish) (Central Salish). It studied the acoustic correlates of stress on vowels and the effects of consonantal coarticulatory effects on vowel quality. The goals of the thesis were to provide useful and usable materials and information to Lekwungen language revitalisation efforts and to provide an acoustic study of Lekwungen vowels to expand knowledge of Salishan languages and linguistics. Duration, mean pitch, and mean amplitude were measured on vowels in various stress environments. Findings showed that there is a three-way contrast between vowels in terms of duration and only a two-way contrast in terms of pitch and amplitude. F1, F2, and F3 were measured at vowel onset (5%), midpoint (50%), and offset (95%), as well as a mean (5%-95%), in CVC sequences for four vowels: /i/, /e/, /a/, and /ə/. Out of five places of articulation of consonants in Lekwungen (alveolar, palatal, labio-velar, uvular, glottal), uvular and glottal had the most persistent effects on F1, F2, and F3 of all vowels. Of the vowels, unstressed /ə/ was the most persistently affected by all consonants. Several effects on perception were also preliminarily documented, but future work is needed to see how persistence in acoustic effects is correlated with perception. This thesis provides information and useful tips to help learners and teachers in writing and perceiving Lekwungen and for learners learning Lekwungen pronunciation, as a part of language revitalisation efforts. It also contributes to the growing body of acoustic phonetic work on Salishan languages, especially on vowels.
Graduate
0290

The purpose of this thesis is to contribute to our understanding of how stress is assigned in SENCOTEN (a dialect of North Straits Salish). The stress system of the Salish languages has been traditionally thought of as being highly morpho-lexical. Montler (1986: 23) states that in SENCOTEN, roots and affixes are lexically specified for their stress properties. He claims that these roots and affixes are in a hierarchical relationship and compete with each other for stress assignment. However, in this thesis, I show that there is much less morpho-lexical stress in SENCOTEN than previously thought. The stress pattern of a high number of polymorphemic words, namely those that contain lexical suffixes, can be accounted for without resorting to a morphological hierarchy of stress. Instead, using an Optimality Theory analysis inspired by the work of Dyck (2004) and Kiyota (2003), I show that it is the weight distinction between full vowels and schwa that determines where stress will be assigned. In addition, I am able to show that metrical feet are grouped into trochees and that these trochaic feet are aligned to the right edge of the word.

The resultive and actual (imperfective) aspects in SENCOTEN, a dialect of North Straits Salish, have been previously considered to contain two separate actual and resultive morphemes (Montler 1986). In contrast, it is argued here that the SENOTEN resultive construction is a complex construction, built on an actual base by prefixation of stative [s-]. Both morphophonological evidence and morphosyntactic evidence for this claim are considered: resultives and actuals exhibit the same non-concatenative allomorphy, and they appear to be in complementary distribution with respect to argument structure. This thesis also considers the semantic aspectual properties of resultives, and suggests that the morphologically complex resultive is semantically compositional: it contains a [durative] feature contributed by the actual morpheme and a [static] feature contributed by the stative prefix.

The Persian Gulf connects to the Indian Ocean via the Strait of Hormuz. In this study, a three-dimensional hydrodynamic model (COHERENS) is employed in a fully prognostic mode to derive sound velocity profiles in the Persian Gulf, an evaporation-driven inverse estuary that is governed by import of surface water from the adjacent ocean and export of saline bottom gulf water through the Strait of Hormuz. During spring and summer, a cyclonic overturning circulation establishes along the full length of the Gulf. During autumn and winter, this circulation breaks up into mesoscale eddies, laterally stirring most of the Gulf’s surface waters. Output of the model shows that sound velocity in the Persian Gulf depends mainly on the temperature in the surface layer whereas the bottom layer as well as the southern part of the Gulf depends on temperature and salinity. Maximum sound velocity occurs during summer in the Persian Gulf which decreases gradually moving from Strait of Hormuz to the north western part of the Gulf. A gradual decrease in sound velocity profiles with depth was commonly observed almost at all stations in the Gulf. However, an exception occurred in Strait of Hormuz during winter. The results of the model are very close to previous observations.