Research Results For 'Pacific'

ALEUTIAN LOW

The Aleutian low is a sub-arctic belt of low pressure that stretches across the North Pacific and is centred over the Aleutian Islands. It is separated by an area of relatively high pressure over the North Pole from a similar North Atlantic low pressure belt centred over Iceland. The Aleutian lows are most intense during mid- winter.
Research Aleutian Low

CANADIAN PACIFIC RAILWAY

The Canadian Pacific Railway is a line of railway which traverses British North America from the St Lawrence to the Pacific. One of the conditions upon which the province of British Columbia in 1871 entered the Dominion of Canada was the construction of such a railway. Since that time more than one act had been passed empowering different companies to go on with the work. Eventually, however, it was completed, according to arrangement with the Canadian government, by a syndicate of London, Paris, and American capitalists, being opened for general traffic in June, 1886. Commencing at Montreal, the line goes on to Ottawa, thence round the north of the Great Lakes to Port Arthur at the head of Lake Superior, and thence to Winnipeg, Manitoba, thence to Stephen in the Rocky Mountains, then across British Columbia to Vancouver on the Pacific. Vancouver, now a thriving city, owes its existence to this railway. The line was of great importance not only as a means of communication between Europe and Eastern Asia and Australasia, but also as a military highway binding together the great masses of the British Empire during the late 19th century.
Research Canadian Pacific Railway

COLONY

A colony is a settlement formed in one country by the inhabitants of another. Colonies may either be formed in dependence on the mother country or in independence. In the latter case the name of colony is retained only in a historical sense. Properly, perhaps, the term should be limited to a settlement which carries on a direct cultivation of the soil, as in the former British colonies of Canada and Australia in contrast to the former in Hindustan or Malta which were the mere superposition on the natives of a ruling race which took little or no part in the general industry of the country.

The motives which lead to the formation of colonies, and the manner of their formation, are various. Sometimes the ambition of extending territory and the desire of increasing wealth have been the chief impulses in colonization; but colonies became a necessity for the redundant population of European states in the 19th century.

Among ancient nations the principal promoters of colonization were the Phoenicians, the Greeks, and the Romans; the greatest colonizers in modern times have been the English and the Spaniards, next to whom may be reckoned the Portuguese, the Dutch, and the French. The Germans during the 19th century contributed largely to the tide of emigration, particularly in the direction of America;
but did little directly as colonizers.

The Phoenician colonies were partly caused by political dissensions and redundant population, but were chiefly commercial, serving as entrepots and ports of repair for Phoenician commerce along the coasts of Africa and Spain, in the latter of which they numbered, according to Strabo, more than two hundred. But it was in Africa that the most famous arose, Carthage, the greatest colonizing state of the ancient world.

The Greek colonies, which were widely spread in Asia Minor and the islands of the Mediterranean, the coasts of Macedonia and Thrace, in South Italy and Sicily, were commonly independent, and frequently soon surpassed the mother states in power and importance.

The colonies of Rome were chiefly military, and while the empire lasted were all in strict subordination to the central government. As the Roman power declined the remains of them amalgamated with the peoples among whom they were placed, thus forming in countries where they were sufficiently strong what are known as the Latin races, with languages (Spanish, Portuguese, French, and Italian) which are merely modifications of the old Roman tongue.

Before America and the way by sea to the East Indies were discovered, the only colonies belonging to European states were those of the Genoese, Pisans, and Venetians in the Levant and the Black Sea, flourishing establishments on which the mercantile greatness of Italy in those days was largely built.

The Portuguese were the first great colonizers among modern states. In 1419 they discovered Madeira, the Azores, and the Cape Verde Islands; the Congo and the Cape of Good Hope followed; and before the century was out Vasco de Gama had landed at Calicut on the Malabar coast of India. The first Portuguese colonies were garrisons along the coasts where they traded: Mozambique and Sofala on the east coast of Africa, Ormuz and Muscat in the Persian Gulf, Goa and Damao on the west coast of India. Colonies were established in Sri Lanka in 1505, in the Moluccas in 1510. Brazil was discovered in 1499, and this magnificent possession fell to Portugal, and was colonized about 1530. Bad government at home and the subjection of the country to Spain caused the loss of most of the Portuguese colonies.

Soon after the Portuguese the Spaniards commenced the work of colonization. In 1492 Columbus, on board of a Spanish vessel, discovered the island of San Salvador. Haiti, or San Domingo, Porto Rico, Jamaica, and Cuba were soon colonized, and before the middle of the 16th century Mexico, Ecuador, Venezuela, New Granada (Colombia), Peru, and Chili were subdued, and Spain took the first rank amongst the colonizing powers of Europe. But the Spaniards never really attempted to develop the industrial resources of the subject countries. The pursuit of mining for gold or silver occupied the colonists almost exclusively, and the enslaved natives were driven to work themselves to death in the mines. Cities were founded, at first along the coasts, for the sake of commerce and as military posts; afterwards also in the interior, in particular in the vicinity of the mines, as Vera Cruz, Cumana, Porto Bello, Carthagena, Valencia, Caracas; Acapuico and Panama, on the coast of the Pacific; Lima, Goncepcion, and Buenos Aires. The colonial intercourse with Spain was confined to the single port of Seville, afterwards to that of Cadiz, from which two squadrons started annually - the galleons, about twelve in number, for Porto Bello; and the fleet, of fifteen large vessels, for Vera Cruz. When the power of Spain declined, the colonies declared their independence, and thus were formed the republics of Mexico, Venezuela, Colombia, Ecuador, Peru, Bolivia, Chili, etc. Cuba, Porto Rico, and the Philippine Islands passed to the United States in 1898; the Caroline Islands, etc, were sold to Germany in 1899; and by 1900 hardly any colony remained to Spain.

The hate of Philip II, who prohibited Dutch vessels from the port of Lisbon, forced the Dutch to import directly from India or lose the large carrying trade they had acquired. Several companies were soon formed, and in 1602 they were united into one, the Dutch East India Company, with a monopoly of the East India trade and sovereign powers over all conquests and colonies in India. The Dutch now rapidly deprived the Portuguese of nearly all their East Indian territories, settled a colony at the Cape of Good Hope in 1650, established a West India Company, made extensive conquests in Brazil between 1623 and 1660, which were soon lost, and more permanent ones on some of-the smaller West India Islands, as San Eustatia, Curacoa, Saba, etc. The growing power of the British and the loss of Holland's independence during the Napoleonic wars were heavy blows to the colonial power of the nation. But the Dutch still possesed numerous colonies in the East Indies at the start of the 20th century, among which the more important were Java, Sumatra, Dutch Borneo, the Molucca Islands, and part of New Guinea, also several small islands in the West Indies, and Surinam.

No colonizing power of Europe had a career of such uniform prosperity as Great Britain. The English attempts at colonization began nearly at the same time with the Dutch. After many fruitless attempts to find a north-east or north-west passage to the East Indies, English vessels found their way round the Cape of Good Hope to the East Indies in 1591. The East India Company was established in 1600. English commerce with India, however, was not at first important, and they possessed only single factories on the continent up until the beginning of the 18th century. The ruin of the Mogul Empire in India after the death of Aurengzebe in 1707 afforded the opportunity for the growth of British power, as the British and French were compelled to interfere in the contentions of the native princes and governors. The French appeared at first to maintain the superiority; but the British in turn got the upper hand, and the victory of Clive at Plassey in 1756 laid the foundation of an exclusive British sovereignty in India. By the middle of the next century the British territory embraced, with the exception of a few dependent states, nearly the whole of India, and this vast territory was still under the government of the East India Company - a mercantile company, controlled indeed by parliament, but exercising many of the most important functions of an independent sovereignty. On the suppression of the Indian mutiny in 1857-1858 the government of India was transferred to the crown by act of parliament in 1858.

The discoveries of the Cabots, following soon after the voyages of Columbus, gave the English crown a claim to North America, which, though allowed to lie dormant for nearly a century, was never relinquished, and which, in the reign of Elizabeth I, led to colonization on a large scale. Walter Raleigh's settlement on Roanoke Island (North Carolina) in 1585 failed to become permanent, but in 1607 the colonists sent out by the London Company to Chesapeake Bay founded Jamestown, on the James River, in Virginia. The next great settlement was that of the Pilgrim Fathers, who landed on the 21st of December 1620, in Massachusetts Bay. The colonization of New Hampshire, Maine, New Jersey, Connecticut and Rhode Island, soon followed. In the State of New York and the Hudson River Territory the British found the Dutch already in possession; but in 1664 they seized the colony of New Amsterdam by force, changing its name to New York in honour of James, Duke of York. Pennsylvania was founded by William Penn, and colonized with Quakers in 1682; Maryland in 1631 by a party from Virginia; Carolina in 1670 and Georgia in 1732 by colonies from England.

Colonies were early established in the West India Islands, including Barbados, half of St. Christopher's in 1625, and soon after many smaller islands. Newfoundland was taken possession of in 1583, colonized in 1621 and 1633. Canada was surrendered to Britain at the Peace of Paris in 1763. In 1764 began the disputes between Britain and its North American colonies, which terminated with the acknowledgment of the independence of the United States, Canada remaining a British dependency.

Australia was discovered in the beginning of the 17th century. The first Australasian settlements of Britain were penal colonies. New South Wales, discovered in 1770, was established as a penal colony in 1788; Tasmania (Van Diemen's Land), discovered by Tasman in 1642, followed in 1803; West Australia, also first used as a penal settlement, became a free colony in 1829; Victoria was colonized in 1835, and made an independent colony in 1851; South Australia was settled in 1836. In 1851 the discovery of gold in Victoria gave a great impetus to the Australian Colonies. Queensland was made a separate colony from N.ew South Wales in 1859. New Zealand, discovered by Tasman in 1642, began to be used for whale-fishery about 1790, was settled in 1839, and made a colony in 1840. In 1874 the Fiji Islands, and in 1884 part of New Guinea, were annexed as crown colonies. In South Africa Cape Colony, first settled by the Dutch in 1652, finally became a British colony in 1815. Natal followed in 1843. Later annexations were Bechuanaland in 1885, Zululand in 1887, Rhodesia (now Zimbabwe) in 1888-89, and the Orange River Colony and Transvaal in 1900. In Western Africa were the colonies of the Gold Coast, Gambia, and Sierra Leone - ancient possessions of the British crown; with Lagos and Nigeria acquired in 1885 and after. Other possessions were British East Africa (Kenya), with Uganda and Somaliland. Gibraltar was acquired in 1704, Malta in 1800.

According to their government relations with the crown the colonies were arranged under three heads: (1.) Crown colonies, in which the crown had the entire control of legislation, while the administration was carried on by public officers under the control of the home government. (2.) Colonies possessing representative institutions but not responsible government, in which the crown had no more than a veto on legislation, but the home government retained the control of public officers. (3.) Colonies possessing representative institutions and responsible government, in which the crown had only a veto on legislation, and the home government had no control over any officer except the governor. All colonies were, however, disabled from such acts of independent sovereignty as the initiative in war, alliances, and diplomacy generally.

France was somewhat late in establishing colonies. Between 1627 and 1636 the West Indian islands of St Christopher's, Guadeloupe, and Martinique were colonized by private persons. Champlain was the pioneer of the French in the exploration of the North American continent, and founded Quebec in 1608. Colbert purchased several West India islands, as Martinique, Guadeloupe, St Lucia, etc, and sent out colonists in 1664 to Cayenne. In 1670 the East India Company formed by Colbert founded Pondicherry, which became the capital of extensive possessions in the East Indies. At the beginning of the 18th century France had extensive settlements in Canada, Nova Scotia, and Newfoundland, the most flourishing of the West India islands, and she seemed to have a prosperous career before her in India. Ere long, however, the rival interests of British and French colonists brought about a conflict which terminated in the loss of Canada and other North American possessions, as well as many of the West India Islands, while the dominion of India passed into the hands of the British.

During the 19th century Germany made an effort to take rank as a colonial power, and acquired in Africa the territories of Damaraland, Great Nama Land, etc, on the south-west coast, north of Cape Colony; the Cameroons District; a large portion of territory formerly claimed by the Sultan of Zanzibar, extending inland to Victoria Nyanza, etc; also in the Pacific a portion of New Guinea, then subsequently called Kaiser Wilhelm's Land, the Bismarck Archipelago, Marshall Islands, etc.

EARTHQUAKE

An earthquake is a movement of the earth, caused either by volcanic activity below the surface or by a large area of earth, weaker than that which surrounds it, slipping a little downwards.
Earthquakes need not be severe. In some parts of the Pacific they are a daily, and not especially frightening, occurrence.

The motion occurs in very different ways, having sometimes a perpendicular, sometimes a horizontal undulating, and sometimes a whirling motion. It also varies much in degrees of violence, from a shock which is hardly perceptible to one which bursts open chasms and changes the appearance of the ground itself. During these shocks sometimes smoke and flames, but more frequently stones and torrents of water are discharged.
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ETHICAL RELATIVISM

In philosophy, ethical relativism is the view that ethical judgements are true or false only relative to a particular context. So if I say that eating people is wrong, while you say it is right, we may both be speaking the truth. For cannibalism may be wrong in my context and right in yours. Relativists disagree about what the relevant context for us is. Some would say it is a particular cultural or historical setting, so cannibalism may be permissible among ' primitive' natives of a Pacific Island but not in a modern European city. Other relativists claim that the relevant context is that of a specific individual, so that cannibalism may be right for you and wrong for me simply because we are different people with different inclinations. But all relativists deny that there is any way of formulating moral claims that will make them true in all conceivable contexts. In this they depart for the common-sense view that we can reasonably make moral assessments of the behaviour of other people, even when they come from a
rather different social or historical context.
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GUANO

Guano (from the Peruvian huano meaning dung) is the partially decomposed and dry excrement of sea-birds. Since the 19th century it has been highly prized as a manure, and led to the claims and disputes of the many tiny islands and atolls in the Pacific Ocean (such as the Gilbert Islands, Line Islands etc) as the western countries sought to lay sole claim to the collection of the vast tons of guano deposited on these islands by their bird populations.

The name guano has also been extended to accumulations of a similar kind from land birds, and even from bats in caverns. Owing to the fact that rain washes such deposits away, great accumulations of guano exist principally in hot and dry tropical regions. The most important of all were the deposits on the Chincha Islands off the coast of Peru, which yielded a considerable revenue to the country, but were quite exhausted by 1900. From 1853 to 1872 about 8,000,000 tons were obtained from these islands. The guano which was found there was from 60 to 80 or 100 feet (as much as 30 meters) in thickness, and was entirely due to the droppings, accumulated for many ages, of the innumerable sea-birds which make these islands their resting-place and breeding-ground. Other deposits of less extent have from time to time been found, and Peru remained the chief source of supply, its deposits being worked under the Chilian government.

Guano varies extremely in composition, but it may be roughly divided into nitrogenous and phosphatic. The first of these contains about 21 per cent of ammonia. This is the case with the Peruvian variety, which contains almost all the inorganic matter required by a plant, and that in a highly available form, so that it is looked upon as one of the best of all fertilizing agents for different crops. Its use as a manure was known to the native Peruvians centuries ago, but no attention was paid to the accounts by modern travellers of its wonderful efficacy until Von Humboldt brought some to Europe and had it analysed. It began to be brought to Europe about 1846. It was used raw or in its natural state, but most of the phosphatic guanos (some of which hardly deserve the name of guano) required to be dissolved by sulphuric acid before using. There were also manures known fish guano, prepared from fish or fish refuse, flesh guano, blood guano, etcc. Large quantities of fish guano were made in the United States from the menhaden, the oil being first extracted.
Research Guano

KNIGHTS OF LABOR

The Knights of Labor was an early American trade union-like order founded in Philadelphia in 1869 by Uriah S Stevens and formally organized in 1871 for the protection of working people and the development of educated labour. It was secret until the name was made public in 1881. By that time nearly all trades were represented. It was governed by a national executive board and local assemblies which had power to order strikes and boycotts. The chief strike ordered was that on the Missouri Pacific system in 1886. It failed.
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MOUNTAINS

Mountains are often classified according to their mode of formation: Fold
mountains; Block mountains; Residual mountains; Volcanic mountains.

High mountain chains such as the Himalayas, Andes, Alps, and Rockies are known as new fold mountain systems. The term 'fold' is a reference to the way in which such mountains have been formed. Throughout millions of years slow movements of the earth's crust have caused these
mountains to be raised. The movements which have resulted in mountain buildings were not, however, vertical uplifts. They were primarily horizontal movements, the effect of which was to cause the crust of the earth to 'wrinkle', in a similar way to which a tablecloth wrinkles if it is pushed along the table. The arched or upraised parts of the folds are known as anticlines and the troughs as synclines. These folds can vary greatly in size. Mountain building is undoubtedly due to some deep-seated cause. For a long period the most simple explanation was that folding was entirely due to the cooling and contraction of the earth, so that the crust, already cold and shrunken, had to wrinkle to fit itself to the still cooling and contracting 'core'. One of the objections advanced against this theory is that the amount of shrinking necessary to account for the Himalayas, Alps, etc., seems to be greater than the mere contraction of the earth would allow. While the theory of contraction cannot be completely rejected, serious consideration must be given to the more recent explanations of mountain building. For instance, Wegener suggests that mountain building may be due to the 'wrinkles' produced by the drifting of a continental mass, e.g. that the Alps were formed by the northward drift of the African continent towards the more stable blocks of Central Europe. As the African mass drifted slowly northward the zone between it and the European mass became narrower, and the land was raised into high ridges or folds. The raising of the Alps was accompanied by the formation of the deep trough which contains the Mediterranean Sea. The same hypothesis would account for the building of the Himalayas and the depression of the Indo-Gangetic trough by the northward drift of the Deccan mass.

During the physical history of the earth, mountain building appears to have proceeded more actively at some periods than others. Fold mountains are, therefore, not all of the same age. The newest group of fold mountains include the Himalayas, Alps, Rockies, and Andes. During an earlier period of folding (the Carboniferous) the Pennines, Appalachians, the Cape Ranges of South Africa, and the Dividing Range of Australia were uplifted. A still earlier period of folding accounted for the original mountains of Scotland and Norway, of which the present mountains are merely the worn down stumps. The older fold mountains, which have been subjected to the forces of denudation (such as the weather, rivers, glaciers, etc.) for long geological periods, are much lower and less rugged than the newer fold mountains. The term 'new fold' is applied to the mountain ranges which have been folded most recently, but they seem very old when their age in actual years is considered because they were uplifted many millions of years before historic time. Mountain building is a very long and slow process; and in the case of certain mountain chains, such as the Andes and the mountains of Japan, is probably still proceeding.

The new fold mountain systems of the world, except in such instances as the simple low folds of the Weald (South-east England), usually consist of high parallel ranges, the average height being well over 3000 metres. In the Himalayas' the highest peak rises to 8840 metres; in the Andes 7000 metres; in the Rockies 6000 metres; in the Alps to 4600 metres. Vast though these heights appear, the wrinkles of the earth's crust are only slight. The highest mountain in the world (Mount Everest) is about five miles high, so that on a globe of 40 cm, diameter it would protrude only 2.5 mm. Most of the active volcanoes are found in the neighbourhood of fold mountains, where the crust of the earth has been fractured during the process of folding. All around the Pacific Ocean there are many active and extinct volcanoes, as in New Zealand, the East Indies, Japan, and North, Central, and South America. Another belt of active volcanoes is associated with the fold mountains of the West Indies. The mountains of this type are characterised by ruggedness of relief in contrast to the smooth and rounded contours of mountain areas which have been subjected to weathering agents for long periods of time. This is obvious if pictures of the Alps and the Scottish Highlands are compared.

Mountains are effective climatic barriers, and the climates of regions on either side of a high mountain range are very different. For example, the coast lands of British Columbia have an equable climate and a heavy rainfall, while the lands to the east of the Rockies have an extreme climate and light rainfall. Again, the climate of the mountainous areas differs from that of the adjacent lowlands. The great mountain systems of the world are mainly important for their minerals, and, in the temperate zone, for their lumber. In the plateau regions of some mountain systems agriculture has been made possible by irrigation, and above the forests in temperate areas there are valuable alpine pastures. The swift streams of mountains are frequently sources of hydro-electric power, especially in countries which have no coal, such as Switzerland and Norway. In North America, the Western Cordillera provides gold, copper, lead, and silver, especially in the states of Nevada and Montana. The Andes provide tin and copper (Bolivia), gold and platinum
(Colombia), and silver (Peru). The Highlands of East Australia are important for copper and gold. The lumbering industry is specially important in British Columbia, Washington, and Oregon (soft woods), the Central American mountainous lands (hard woods), the Himalayan slopes (teak and sal), and the Scandinavian mountains (soft woods).

To provide food for the mining communities in inaccessible mountain areas, agriculture has been developed. There are numerous irrigation schemes in operation in most of the mountain states of the USA, e.g. at Salt Lake City in Utah. Similarly, the Andean states, e.g. Bolivia, grow small quantities of cereals in the plateau areas. Mountain pastures have been utilised most extensively for cattle rearing in Switzerland and Scandinavia. The vast central plateau of Asia is, owing to difficulty of access and climatic extremes, so isolated from other regions that very little development of any kind, on modern lines, has taken place. High mountain ranges are also barriers to communication, and so tend to separate peoples. Traffic across mountains is limited to the passes, which are often so high as to be snowbound in winter. Such ranges as the Alps, Andes, etc. can only be crossed with great difficulty or by expensive tunnelling.

It sometimes happens that movement of the earth's crust occurs along cracks or faults. Where such movement leaves a block of higher land standing between two areas of lower land, the highland is known as a 'Block Mountain' or horst. The Vosges and Black Forest Mountains are examples of such formations These mountains are usually very steep-sided, and often the summit levels are roughly the same.

When an area of highland remains standing above the general level after rivers and other natural agents have lowered the surface of the surrounding area, the name residual mountain is used. Sometimes such highlands are called 'mountains of denudation'. This term can usually be applied to the mountain ridges associated with 'dissected plateaux'. Included in this class are the mountain ridges of the Highlands of Scotland, the Sierras of Central Spain, and the Mesas and Buttes of the western plateau lands of the United States.

Mountains may be formed by volcanic material piled up around a crater, such mountains are popularly known as volcanoes.
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NORTHWEST BOUNDARY QUESTION

The Northwest Boundary Question was a historic territorial dispute in North America. The territory bounded north by latitude 54 degrees 40 minutes, east by the Rocky Mountains, south by latitude 42 degrees, and west by the Pacific Ocean has been claimed at various times and to various extents by Russia, Spain, Great Britain and the United States. The Russian claim, which rested mainly upon occupation by fur traders, was settled by a treaty made on January 11, 1825. Under this treaty the United States were to make no-settlements north of latitude 54 degrees 40 minutes and Russia none south of that latitude. England and Russia agreed upon the same terms.

The Spanish claims were confined south of latitude 42 degrees by the treaty which ceded Florida in 1819. Great Britain had little or no claim by discovery. The United States' claim rested upon the voyage of Gray up the Columbia River in 1792, and the explorations of Lewis and Clark through the Rocky Mountains and through the Oregon country in 1805-06, under the orders of Jefferson. By the treaty of October the 20th, 1818, the whole territory west of the Rocky Mountains was to be opened to both countries for ten years, and, in 1827, the joint occupation for an indefinite period was agreed upon. Later this produced dissatisfaction, and after considerable negotiation, Great Britain was induced in 1846 to accept latitude 49 degrees as the boundary from the Rocky Mountains to the channel between Vancouver's Island and the mainland.
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PACIFIC RAILROADS

The outbreak of the American Civil War and the feeling of necessity of a better connection with the Pacific coast, induced the American Government to make large grants in favour of the Central Pacific, Union Pacific and Kansas Pacific Railroads, by an act of July the 1st, 1862. Later, 47,000,000 acres were granted to the Northern Pacific. The Central Pacific and Union Pacific were completed in 1869. The construction and finance of the Union Pacific were managed by the Credit Mobilier and involved in legislative scandals. In 1878 the office of Commissioner of Railroads was instituted, to supervise the accounts of the Pacific railways.
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