PASTURE SEED MIXTURE FOR HIGH RAINFALL DISTRICTS

1937 ◽  
pp. 71-78
Author(s):  
A. Stuart
Keyword(s):  
West Coast ◽  
The South ◽  
The West ◽  
High Rainfall ◽  
The North ◽  
Seed Mixture ◽  
Rainfall Map

In dealing with this subject it is essential to define the high rainfall districts, and on, perusing a rainfall map it was found, contrary to expectations, that the greater part of the North Island, as represented by the Auckland Province and Taranaki, has a rainfall of over 50 inches per annum. In the same category falls the West Coast of the South Island and all of Stewart Island.

scholarly journals Psychiatry in Nigeria

2003 ◽  
Vol 1 (2) ◽  
pp. 10-12 ◽  
Author(s):  
Oye Gureje
Keyword(s):  
West Coast ◽  
Federal System ◽  
The South ◽  
Central State ◽  
The West ◽  
Traditional Religions ◽  
The North ◽  
The People ◽  
State And Local

Nigeria is a huge country. It covers an area of 924 000 km2 on the west coast of Africa. It has a population of about 110 million, which means that every one in six Africans is a Nigerian. It is a country of diverse ethnicity, with over 200 spoken languages, even though three of those are spoken by about 60% of the population. Administratively, it is divided into 36 states and operates a federal system of government, with constitutional responsibilities allocated to the various tiers of government – central, state and local. There are two main religions, Islam (predominantly in the north) and Christianity (predominantly in the south). However, a large proportion of the people still practise traditional religions exclusively or in addition to either Islam or Christianity.

The phonemes of New Zealand English

1966 ◽  
Vol 11 (2) ◽  
pp. 79-82 ◽  
Author(s):  
L. G. Kelly
Keyword(s):  
New Zealand ◽  
West Coast ◽  
Industrial Revolution ◽  
Gold Rush ◽  
The South ◽  
The West ◽  
Social Differences ◽  
Free Church ◽  
The North ◽  
English Society

The New Zealand accent belongs to the British group of English accents. There are three main divisions: General New Zealand, which is spoken in most parts of the country, and the accents of Otago, in the south of the South Island, and on the West Coast of the South Island. The three divisions follow the original pattern of settlement. In the North Island, settlement was directed by the New Zealand Company, which founded Auckland and Wellington in 1840; other settlements followed in the late 1840s. In the South, the Anglican Church founded Christchurch and Nelson in the early 1850s. These settlements had the common aim of reproducing English society as it existed in the south of England and drew most of their settlers from persons dispossessed by the Industrial Revolution. The difficulties of life in early New Zealand effectively levelled out social differences, with important effects on the language. Otago was founded in 1848 by the Scottish Free Church. The West Coast was not settled until the Gold Rush of the 1860s attracted miners from the goldfields of Victoria and California. Since that time there has been considerable immigration from the British Isles, at first a mere trickle from Europe and then a flood of Central European refugees after the Second World War. In general the willingness of the average New Zealander to travel for reasons of work or promotion has prevented the growth of regional accents; but the West Coast and Otago tend to keep to themselves, isolated by rough country and their own sense of community.

Geological Interpretation of Airborne Magnetometer Observations from Nelson to Waikato River, New Zealand

1959 ◽  
Vol 96 (2) ◽  
pp. 118-124 ◽  
Author(s):  
H. W. Wellman
Keyword(s):  
New Zealand ◽  
West Coast ◽  
Axial Plane ◽  
Igneous Rocks ◽  
The South ◽  
The West ◽  
Geological Interpretation ◽  
The North ◽  
Cook Strait ◽  
Waikato River

AbstractA map is presented showing a series of airborne magnetometer profiles from the north end of the South Island of New Zealand to the mouth of Waikato River. The two southern profiles are related to the exposed Upper Palaeozoic igneous rocks which are considered to extend north across Cook Strait and along the west coast of the North Island to cause the anomalies in the northern profiles. The North Island profiles are considered to reflect the Kawhia Syncline and a major anticline to the east. The eastward displacement of the magnetic low relative to the synclinal axis at the surface is considered due to the eastward dip of the axial plane of the syncline.

The Megalithic Tomb of Pedra Branca, Portugal. Preliminary Report

1975 ◽  
Vol 41 ◽  
pp. 167-178 ◽  
Author(s):  
O. da Veiga Ferreira ◽  
G. Zbyszewski ◽  
M. Leitao ◽  
C. T. North ◽  
H. Reynolds de Sousa
Keyword(s):  
Atlantic Ocean ◽  
Sea Level ◽  
West Coast ◽  
Preliminary Report ◽  
Rough Terrain ◽  
The South ◽  
The West ◽  
The North ◽  
Small Streams ◽  
Local Construction

The megalithic tomb of Pedra Branca lies at Montum, on the west coast of Portugal about 140 kilometers south of Lisbon by road (fig. 1). The tomb is the first in Portugal to have yielded Beaker graves overlying earlier burials; prior to its discovery, no Beaker remains had ever been noted further south than Palmela, in the estuary of the Sado river, approximately 40 kilometers from Lisbon. The tomb is situated on the top of a small hillock 100 m above sea level, separated from the Atlantic Ocean by a fertile undulating plain about 5 km in width. The Lake of Melides lies to the north and, to the east, the hills of Grandola rise steeply to an altitude of 300 m; an expanse of rough terrain stretches to the south, ravined by various small streams which flow into the Lake of Santo André on the coast.When the tomb was discovered by surveyors of the Geological Services of Portugal, it was already very badly damaged; all the orthostats had been broken for use in local construction and part of the circular covering mound had already been ploughed under. The Services therefore, decided that a salvage campaign was called for, and a team made up of the authors, was invited to carry it out with funds granted by the Calouste Gulbenkian Foundation.

scholarly journals Abstract of Paper on the Frost of 1895 in Scotland

1902 ◽  
Vol 42 ◽  
pp. 532-534
Author(s):  
R. C. Mossman
Keyword(s):  
West Coast ◽  
The South ◽  
The West ◽  
North East ◽  
The North ◽  
Mean Temperature ◽  
The Mean

This great frost commenced on 28th December 1894 and terminated in its intense form on 20th February 1895, thus lasting 54 days. The greatest cold occurred from the 6th to the 20th of February. During this latter period pressure was higher in the north than in the south of Scotland, and the winds were consequently easterly or north-easterly, but light in force. Taking the two months, January and February, together, the mean temperature was more than 10° below the average at many inland places, but on the west coast it was only about 5° lower than usual. There are records of temperature in the north-east of Scotland, at either Inverness, Gordon Castle or Aberdeen for the last 132 years, and in all this time there was no winter with two such cold months as January and February 1895 at these places.

Chapter 6 Northern Nordaustlandet (and associated Islands Storoya, Kvitoya)

1997 ◽  
Vol 17 (1) ◽  
pp. 96-109 ◽  
Author(s):  
W. Brian Harland
Keyword(s):  
West Coast ◽  
Solid Rock ◽  
Major Part ◽  
The South ◽  
The West ◽  
Svalbard Archipelago ◽  
Ice Caps ◽  
Oxford University ◽  
The North ◽  
Pack Ice

Nordaustlandet is the second largest island in the Svalbard archipelago. It has been generally inaccessible by ship because of polar pack ice except for the west coast, or in exceptional summers. Exploration has therefore been limited. The major part of the interior is covered by two large ice caps: Vestfonna and (the large) Austfonna which forms all of the southern coastline in the eastern part of the island. Pre-Devonian, mostly Precambrian outcrops of solid rock extend along the northern and northwestern seaboard. Wahlen-bergfjorden divides the west coast with post-Devonian rocks cropping out to the south of it. These have already been referred to in Chapter 5 so that the main object in this chapter is to outline what is known of the older rocks. Because of the ice caps covering the major part of the island, exposures, especially in the north and east, are often isolated on promontories along the highly indented coastline (Fig. 6.1).After the early visit by Parry in 1828 research was largely by Swedish geologists with A.E. Nordenskiold's sledge journeys in 1861, 1866, 1869 and 1873.A Swedish initiative led to the Russo-Swedish Arc of Meridian Survey along both sides of Hinlopenstretet. During the period 1899 to 1902 (De Geer 1923; Nathorst 1910) and later the Swedish-Norwegian expedition based at Sveanor in Murchisonfjorden (Kulling 1932) resulted in a thorough study of the Hecla Hoek rocks (Kulling 1934).Alongside this were a series of multidisciplinary expeditions from Oxford University in 1924, 1935-36 and 1951. Sandford accompanied the

US and Russian policies and strategies in the Middle East: Iraq and Syria as a model

2019 ◽  
pp. 220
Author(s):  
Esraa Aladdin Noori ◽  
Nasser Zain AlAbidine Ahmed
Keyword(s):  
Middle East ◽  
East Asia ◽  
Balance Of Power ◽  
Western World ◽  
International Conflicts ◽  
The South ◽  
The West ◽  
The North ◽  
East Region ◽  
Middle East Region

The Russian-American relations have undergone many stages of conflict and competition over cooperation that have left their mark on the international balance of power in the Middle East. The Iraqi and Syrian crises are a detailed development in the Middle East region. The Middle East region has allowed some regional and international conflicts to intensify, with the expansion of the geopolitical circle, which, if applied strategically to the Middle East region, covers the area between Afghanistan and East Asia, From the north to the Maghreb to the west and to the Sudan and the Greater Sahara to the south, its strategic importance will seem clear. It is the main lifeline of the Western world.

scholarly journals Gitksan

2016 ◽  
Vol 46 (3) ◽  
pp. 367-378 ◽  
Author(s):  
Jason Brown ◽  
Henry Davis ◽  
Michael Schwan ◽  
Barbara Sennott
Keyword(s):  
British Columbia ◽  
The South ◽  
The West ◽  
The North

Gitksan (git) is an Interior Tsimshianic language spoken in northwestern British Columbia, Canada. It is closely related to Nisga'a, and more distantly related to Coast Tsimshian and Southern Tsimshian. The specific dialect of Gitksan presented here is what can be called Eastern Gitksan, spoken in the villages of Kispiox (Ansbayaxw), Glen Vowell (Sigit'ox), and Hazelton (Git-an'maaxs), which contrasts with the Western dialects, spoken in the villages of Kitwanga (Gitwingax), Gitanyow (Git-anyaaw), and Kitseguecla (Gijigyukwhla). The primary phonological differences between the dialects are a lexical shift in vowels and the presence of stop lenition in the Eastern dialects. While there exists a dialect continuum, the primary cultural and political distinction drawn is between Eastern and Western Gitksan. For reference, Gitksan is bordered on the west by Nisga'a, in the south by Coast Tsimshian and Witsuwit'en, in the east by Dakelh and Sekani, and in the north by Tahltan (the latter four of these being Athabaskan languages).

scholarly journals ROME AT SEA: THE BEGINNINGS OF ROMAN NAVAL POWER

2017 ◽  
Vol 64 (1) ◽  
pp. 14-26 ◽  
Author(s):  
W. V. Harris
Keyword(s):  
West Coast ◽  
Asia Minor ◽  
North Coast ◽  
The West ◽  
Naval Power ◽  
The North

Between the Battle of Mylae in 260 bc (when Rome defeated Carthage off the north coast of Sicily) and the Battle of Myonnesus in 190 (when Rome defeated the Seleucid navy off the west coast of Asia Minor), the Romans established naval domination over the whole Mediterranean. Scholars generally believe, for quite good reasons, that this process of naval aggrandisement began abruptly, the Romans having previously taken no interest in the sea. That, after all, is what Polybius quite clearly says.

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