Pressured from all sides: the February 1913 surrender of the northeast corner of the Tsuu T'ina Nation

2004 ◽  
Vol 30 (1) ◽  
pp. 112-129 ◽  
Author(s):  
Patricia K. Wood
Keyword(s):  
2021 ◽  
Vol 135 (2) ◽  
pp. 186-191
Author(s):  
Paul M. Catling ◽  
Brenda Kostiuk ◽  
Jeffrey H. Skevington

Alaska Wild Rhubarb (Koenigia alaskana var. glabrescens; Polygonaceae) is a native Arctic, subarctic, and alpine plant of northwestern North America. Although the plant has some economic and ecological importance, its biology is poorly known. At 11 sites in the northeast corner of its range in Northwest Territories, we found that 87% of its floral visitors were flies, mostly Syrphidae, a diverse family known to be important pollinators. Insects visiting consecutive flowers on different plants and, thus, likely effecting pollination were also flies (78.6%) and also mostly Syrphidae (72.7%) followed by Hymenoptera (20%). Although syrphids were the dominant potential pollinators at most sites, there was some variation among sites. Our results provide quantitative support for pollinator diversity and the major role of Syrphidae in pollination of Alaska Wild Rhubarb. We suggest that pollination is not a limiting factor in this plant’s spread, nor its rare and local occurrence and restricted distribution, because the majority of its pollinators are widespread.


1922 ◽  
Vol 15 (1) ◽  
pp. 43-48

Foreword. The territory of the Lake Shore Division of the Illinois Teachers’ Association comprises some half dozen counties in the northeast corner of the state exclusive of the City of Chicago. A considerable portion of its population is suburban to the larger city and practically all of its business activities center there.


Author(s):  
M. Koehl ◽  
M. Fuchs ◽  
T. Nivola ◽  
J. Koch ◽  
L. Cartier ◽  
...  

Abstract. This paper is a review of the modelling of two edifices located in a city which developed on the vestiges of a Roman city during antiquity endowed in the 4th century with a military camp. The term castellum is used for the first structure. A second structure concerns the remains of a castle dismantled at the end of the 17th century, which was generally known only by an engraving in perspective made shortly before its demolition, and the cadastral matrix that had preserved the traces of its right-of-way. It is a Renaissance castle built in the 16th century by the Württemberg family in the northeast corner of the ruins of the castellum. The projects contain a first part of data analysis and interpretation based on available documents. Similar sites close in terms of architecture, geographical location and construction period were also visited to get inspiration from them and to be able to make proposals for restitution. Despite the lack of data available, the multidisciplinary aspect of these projects is very important. In fact, the experience of archaeologists and the monitoring of modelling throughout its progress is essential to work out models that are both justifiable, at the level of the proposals made and sufficiently complete to be able to be highlighted. Once the models validated, they are integrated in a virtual way into the contemporary urban environment, through an interactive virtual tour. This paper reviews the principles implemented during the modelling, the rendering and the valorisation of the models thru virtual tours and AR/VR implementation.


1958 ◽  
Vol 90 (10) ◽  
pp. 623-627 ◽  
Author(s):  
W. W. Judd

In the description of the Byron Bog (Judd, 1957a) it was pointed out that Redmond's Pond is situated in the northwest corner of the bog and that during 1956 a tent-trap was anchored in a small bay in the northeast corner of the pond to trap insects emerging as adults from the water. The position of the trap on the pond is shown in the map accompanying the description of the bog (Judd, 1957a) and the structure and use of the trap are also described by Judd (1957b). The trap was placed on the water on May 15, 1956 and remained there until November 8. It was about four feet from the edge of the pond in water about two feet deep. At this point the bottom of the pond was composed of a thick layer of loose, brown peat and the adjacent edge of the pond was occupied by a dense growth of leatherleaf, Chamaedaphne calyculata, growing in Sphagnum (Judd, 1957a). The branches of the bushes of leatherleaf extended out over the water of the small bay in which the trap floated. The only rooted plant growing in and around the trap was spatterdock, Nuphar advena. Floating in the water was a sparse growth of bladderwort, Utricularia vulgaris, and on the surface of the water there were a few scattered fronds of duckweed, Lemna minor, and water flax-seed, Spirodela polyrhiza.


1979 ◽  
Vol 29 ◽  
pp. 115-151 ◽  
Author(s):  
Irene J. Winter

It is a good maxim that all controversial archaeological issues should be reviewed regularly in the light of new material and/or changing perspectives; and certainly one of the most controversial issues in the history of the early first millennium B.C. in the Near East has been the dating of the reliefs and inscriptions built into the two Citadel Gates at Karatepe.The site itself, set on the west bank of the Ceyhan River in the northeast corner of Cilicia, sits on a natural hill just south of a spur of the foothills that mark the beginning of the juncture of the Taurus and Amanus mountain ranges (cf. Maps, Figs. 2, 3). It was first discovered and explored in 1946 by a Turkish team, headed by H. Th. Bossert, investigating ancient road systems of the “Neo-Hittite” period. Active field seasons were initiated at Karatepe, along with soundings at the neighbouring site of Domuztepe on the opposite bank of the Ceyhan, and were continued through the mid-1950s, since which time restoration has been in process at Karatepe under the direction of Professor Halet Çambel of Istanbul University.


2015 ◽  
Vol 53 (02) ◽  
pp. 53-0933-53-0933
Keyword(s):  

Author(s):  
James F. Osborne

This book presents a new model for the kingdoms that clustered around the northeast corner of the Mediterranean Sea during the Iron Age, ca. 1200–600 BCE. Rather than presenting them as an ancient version of the modern nation-state, characterized by homogenous ethnolinguistic communities like “the Aramaeans” or “the Luwians” living in neatly bounded territories, this book presents these polities as being fundamentally diverse and variable, distinguished by demographic fluidity and cultural mobility. This conclusion is reached via an examination of a host of evidentiary sources, including site plans, settlement patterns, visual arts, and historical sources. Together, these lines of evidence lead to the awareness that this time and place consisted of a complex fusion of cultural traditions that is nevertheless distinctly recognizable unto itself. This book thus proposes a new term to encapsulate that diversity: the Syro-Anatolian Culture Complex.


Antiquity ◽  
1932 ◽  
Vol 6 (24) ◽  
pp. 434-444
Author(s):  
C. S. Jarvis

In my recently published book I have advanced a theory as to the Wanderings of the Israelites and the loss of the Egyptian Host, which if not entirely original contains a considerable amount of fresh evidence based on ten years’ experience of the Peninsula. Like all theories that tend to upset old beliefs this has resulted in a considerable amount of criticism and comment. The assumption briefly is that the Israelites never went to southern Sinai as has been firmly believed for the last 1900 years, but remained for the whole of the period of the Wanderings in the comparatively small cultivable area in the northeast corner of Sinai where they could grow corn for making bread and find grazing for their flocks. This part of my theory is by no means new as the same views have been expounded already by several students of the Wanderings, and I have merely corroborated their opinion and brought forward new evidence and arguments to prove the theory by virtue of my long residence in the Peninsula and knowledge of the country and climate. The explanation I have given of the loss of the Egyptian Host, however, is a novel one, and so far as I know has never been published previously though Sir William Willcocks assumes that the disaster occurred in a lake in northern Sinai and not in the Red Sea; but the lake he selects is not the Bardawil as I maintain, and the incidents that caused the flooding were totally different from those I have suggested.


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