LOG IN. UPLOAD PICTURES.
The Philippines has Zambo Mart to help propagate the Chavacano Language.
Difference between revisions of "Swaziland"
Line 18: | Line 18: | ||
:Male: (2009) 87.8% | :Male: (2009) 87.8% | ||
:Female: (2009) 86.2% | :Female: (2009) 86.2% | ||
'''GNI per capita (U.S.$)''' | '''GNI per capita (U.S.$)''' 2013) 3,060<br> | ||
1Controversial constitution became effective by royal decree on Feb. 8, 2006. | |||
2Includes 20 nonelective seats. | |||
3Includes 10 nonelective seats and 1 ex officio seat (the speaker, who may be designated from outside the House of Assembly). | |||
4Lozitha and Ludzidzini, royal residences close to Lobamba, have national symbolic significance. | |||
5The lilangeni is pegged to the South African rand at 1 to 1; the rand is accepted as legal tender within Swaziland. | |||
==About Swaziland== | ==About Swaziland== | ||
Line 27: | Line 38: | ||
The name Swazi is the Anglicized name of an early king and nation builder, Mswati II, who ruled from 1840 to 1868. The administrative centre is Mbabane, the former capital of the British colonial administration; the national capital is the seat of King Mswati III and his mother, the Ndlovukati, some 11 miles from Mbabane, at Phondvo in the vicinity of Lobamba, where the houses of parliament and other national institutions are situated. | The name Swazi is the Anglicized name of an early king and nation builder, Mswati II, who ruled from 1840 to 1868. The administrative centre is Mbabane, the former capital of the British colonial administration; the national capital is the seat of King Mswati III and his mother, the Ndlovukati, some 11 miles from Mbabane, at Phondvo in the vicinity of Lobamba, where the houses of parliament and other national institutions are situated. | ||
''' | ==Geography of Swaziland== | ||
'''The Land''' | |||
*Relief and soils | |||
A long and complex geologic history has created a landscape with a surprising variety of relief, climate, and soils for such a small country. There are four well-defined physiographic regions, extending longitudinally from north to south in roughly parallel belts. From west to east they are the Highveld, the Middleveld, the Lowveld, and the Lubombo (Lebombo) escarpment. Geologically, the oldest formations are in the west, and the youngest are in the east. | |||
The Highveld, covering about 30 percent of the country, is a complex of granites and more ancient metamorphosed quartzites, sandstones, and volcanics that has been eroded into a rugged mountain land. The average elevation is between 3,500 and 4,500 feet (1,100 and 1,400 metres); the highest points are the summit massifs of Bulembu (6,108 feet [1,862 metres]) and Ngwenya (5,997 feet [1,828 metres]) in the extreme west. Known to the Swazi as Inkangala (a cold, treeless place), the Highveld was the last part of the country to be settled. Its deeper-weathered red to yellow acid soils have developed on the gentler gradients and in river valleys. | |||
The Middleveld occupies about one-fourth of the country and has an average altitude of 2,000 to 2,500 feet. It is a region of rolling uplands and wide, well-watered valleys. It is mainly underlain by ancient granites and gneisses (metamorphosed granites), with dolerites and quartzites, which have weathered deeply to produce friable red and clay loams interspersed with shallower profiles of sands and sandy loams. To the Swazi it is known as Live (“The Country”) or Inkabave (“The Navel”) and is the heartland of the Swazi nation. | |||
The Lowveld, or Bushveld, covering nearly 40 percent of the country, is a generally undulating lowland with isolated knolls and ridges rising abruptly above the general level of 500 to 1,000 feet. In general, the soils reflect the transition from the acidic granites and sandstones of the western Lowveld to the more basic basalts and dolerites of the eastern part—i.e., from sandy loams in the west to red and black clays in the east, the latter being some of the most naturally fertile soils in the country. This region is called Lihlanze by the Swazi, meaning a warm place with trees—in its undisturbed state, the typical African savanna. | |||
The Lubombo escarpment and plateau covers about 5 percent of the country, consisting of a narrow strip of about 600 square miles. It rises abruptly from the Lowveld to an average altitude of 2,000 feet, with higher peaks (Siteki and Mananga) of about 2,500 feet in the north. It is deeply dissected by the gorges of three of the main rivers that traverse the country from west to east, the Umbuluzi, the Usutu, and the Ingwavuma. The plateau soils vary considerably, from shallow sands to deeper loams, depending on the composition of the volcanic lavas that form the bedrock. The Swazi have no specific name for this part of the country. | |||
*Drainage | |||
Swaziland is one of the best-watered countries in southern Africa. Major perennial rivers, which have their sources in South Africa, flow through the country to the Indian Ocean. They are the Lomati, the Komati, the Umbuluzi, and the Usutu. The Usutu has the largest catchment in the country, with three main tributaries, the Usushwana, the Ngwempisi, and the Mkhondvo. In the south the Ingwavuma rises in western Swaziland and also cuts through the Lubombo. | |||
*Climate | |||
The climate is in general subtropical, but it is strongly influenced by the country’s position on the eastern side of southern Africa, which exposes it to moist maritime tropical air coming off the Indian Ocean for much of the year. The cessation of maritime airflow in winter months because of intensified continental winds produces a high degree of climatic variability. The climate is also subject to steep temperature and precipitation gradients from west to east because of the fall in altitude of about 4,000 feet over a distance of about 50 miles. | |||
Average maximum and minimum monthly temperatures are 72° F (22° C) and 52° F (11° C) in the Highveld and 84° F (29° C) and 59° F (15° C) in the Lowveld. The Middleveld occupies an intermediate position in these gradations. | |||
Swaziland falls within the summer rainfall region of the subcontinent, where about 80 percent of the precipitation falls during the summer months of October to March, usually in the form of thunderstorms and frontal rains. Average annual rainfall in the Highveld is about 55 inches (1,400 millimetres), in the Middleveld 34 inches, in the Lowveld about 22 inches, and on the Lubombo about 35 inches. However, variability in the annual totals is great, and figures have fluctuated dramatically from year to year. In the Middleveld, where the bulk of the population lives, the average has varied from a high of 63 inches to a low of 13 inches within a period of a few years. These extreme fluctuations appear to relate to wetter and drier than average quasi-cyclic fluctuations of from 8 to 11 years, which have been identified in the rainfall records. | |||
*Plant and animal life | |||
The natural vegetation includes forest—confined mostly to the Highveld and the windward slopes of the Lubombo escarpment—savanna, and grassland. Factors such as soil composition and moisture produce a variety of vegetation subtypes. There are both wet and dry forests, various densities of savanna, and several grassland types, which range from sweet to sour based on their palatability when mature and dry. Altogether it is a rich flora, with ferns and flowering plants alone accounting for more than 2,600 species. Some have a very limited distribution and are found only in or around Swaziland. | |||
The natural fauna has been severely depleted in recent years because of habitat destruction caused by the spread of the human population, and representative species such as antelope (impala, reedbuck, duiker, waterbuck, wildebeest, and kudu), hippopotamus, rhinoceros, elephant, giraffe, and zebra are found largely in protected reserves. However, smaller mammals—such as the baboon, monkey, jackal, and mongoose—may still be encountered, and several types of snake have a wide distribution. Crocodiles are also common in Lowveld rivers. Birdlife is abundant in each habitat and comprises both resident and migrant (breeding and nonbreeding) populations. The migrants come from central and North Africa and from farther afield (northern Europe and eastern Asia in the case of storks, swallows, and hawks). Distinctive among the more common birds are barbets, weavers, the various hornbills, the lilac-breasted roller, and the purple-crested loerie. | |||
*Settlement patterns | |||
Traditionally, the Swazi lived in family homesteads (imithi) dispersed throughout the countryside. The only larger settlements were the homesteads of royalty and chiefs. This pattern has been modified since the late 19th century by the exposure of the rural Swazi to the money economy. Nucleated settlements grew up at important administrative and trading centres under British colonial rule from 1903, but the process of urbanization accelerated only after World War II, when the establishment of major agricultural, mining, and industrial operations acted as magnets for job seekers and created sizable company towns such as Mhlume, Simunye, Big Bend, and Mhlambanyatsi. The largest are the administrative capital of Mbabane and the commercial and industrial centre of Manzini. Some 30 percent of the population is urban, and this figure is expected to increase because the urban growth rate exceeds the growth rate of the population as a whole. | |||
The rural population lives within a communal land tenure system administered by the traditional chiefs. A typical homestead includes the main hut of the headman (umnumzane); the huts of his mother, wife (or wives), and children; the kitchen and storerooms; and the cattle enclosure (isibaya) in front and facing east. Cattle are more than draft animals and a source of milk; they constitute a store of wealth for use on social and ceremonial occasions (e.g., lobola, or bride-price). | |||
The traditional pattern of homestead life is strictly seasonal. With the onset of the rains in spring (August or September), women plant gardens along the riverbanks; later, when the heavy rains come in summer (October to February), with help from the men, they plow or hoe to sow corn (maize) and sorghum (a millet) in larger fields. At this time all able women and children abandon their homesteads for the fields, and the men also join in the planting and weeding. The summer months are, on the whole, the hungry months, unless supplemented by remittances from working members of the family. Autumn to early winter (March to May) is the harvest; by July the last of the corn and sorghum has been dried and brought in. Activity then moves to the homesteads, where women and men thresh the grain, the best of which is stored and the remainder consumed at once. Winter is a time for relaxation, hunting, entertaining, and visiting. To some extent this traditional round has been disrupted by population pressure on land, by increased drift to the towns, by the absence of men working in the cities, and by the use of hired tractors for plowing, but the basic pattern is still recognizable. | |||
The traditional centres of Swazi life are the royal villages of the ngwenyama (the king) at Ludzidzini and of the ndlovukazi (the queen mother) at Phondvo, both of which are in the “royal heart” of the country and not far from the old royal capital of Lobamba. | |||
==Demography of Swaziland== | |||
==Economy of Swaziland== | |||
==Government and Society of Swaziland== | |||
==Culture Life of Swaziland== | |||
==History of Swaziland== | |||
==Disclaimer== | ==Disclaimer== | ||
{{disclaimer countries}} | {{disclaimer countries}} |
Revision as of 05:01, 20 March 2015
Official name Umbuso weSwatini (Swati); Kingdom of Swaziland (English)
Form of government monarchy1 with two legislative houses (Senate [302]; House of Assembly [663])
Head of state and government King: Mswati III, assisted by Prime Minister: Barnabas Sibusiso Dlamini
Capitals Mbabane (administrative and judicial); Lobamba (legislative)4
Official languages Swati (Swazi); English
Official religion none
Monetary unit lilangeni5 (plural emalangeni [E])
Population (2013 est.) 1,237,000COLLAPSE
Total area (sq mi) 6,704
Total area (sq km) 17,364
Urban-rural population
- Urban: (2010) 21.3%
- Rural: (2010) 78.7%
Life expectancy at birth
- Male: (2012) 49.8 years
- Female: (2012) 49.1 years
Literacy: percentage of population age 15 and over literate
- Male: (2009) 87.8%
- Female: (2009) 86.2%
GNI per capita (U.S.$) 2013) 3,060
1Controversial constitution became effective by royal decree on Feb. 8, 2006.
2Includes 20 nonelective seats.
3Includes 10 nonelective seats and 1 ex officio seat (the speaker, who may be designated from outside the House of Assembly).
4Lozitha and Ludzidzini, royal residences close to Lobamba, have national symbolic significance.
5The lilangeni is pegged to the South African rand at 1 to 1; the rand is accepted as legal tender within Swaziland.
About Swaziland
The Swiss Confederation was founded in 1291 as a defensive alliance among three cantons. In succeeding years, other localities joined the original three. The Swiss Confederation secured its independence from the Holy Roman Empire in 1499. A constitution of 1848, subsequently modified in 1874, replaced the confederation with a centralized federal government. Switzerland's sovereignty and neutrality have long been honored by the major European powers, and the country was not involved in either of the two world wars. The political and economic integration of Europe over the past half century, as well as Switzerland's role in many UN and international organizations, has strengthened Switzerland's ties with its neighbors. However, the country did not officially become a UN member until 2002. Switzerland remains active in many UN and international organizations but retains a strong commitment to neutrality.
Swaziland, officially Kingdom of Swaziland, Swazi Umbuso Weswatini, landlocked country in the eastern flank of South Africa, where it adjoins Mozambique. It extends about 110 miles (175 kilometres) from north to south and about 80 miles from west to east at its largest dimensions.
The name Swazi is the Anglicized name of an early king and nation builder, Mswati II, who ruled from 1840 to 1868. The administrative centre is Mbabane, the former capital of the British colonial administration; the national capital is the seat of King Mswati III and his mother, the Ndlovukati, some 11 miles from Mbabane, at Phondvo in the vicinity of Lobamba, where the houses of parliament and other national institutions are situated.
Geography of Swaziland
The Land
- Relief and soils
A long and complex geologic history has created a landscape with a surprising variety of relief, climate, and soils for such a small country. There are four well-defined physiographic regions, extending longitudinally from north to south in roughly parallel belts. From west to east they are the Highveld, the Middleveld, the Lowveld, and the Lubombo (Lebombo) escarpment. Geologically, the oldest formations are in the west, and the youngest are in the east.
The Highveld, covering about 30 percent of the country, is a complex of granites and more ancient metamorphosed quartzites, sandstones, and volcanics that has been eroded into a rugged mountain land. The average elevation is between 3,500 and 4,500 feet (1,100 and 1,400 metres); the highest points are the summit massifs of Bulembu (6,108 feet [1,862 metres]) and Ngwenya (5,997 feet [1,828 metres]) in the extreme west. Known to the Swazi as Inkangala (a cold, treeless place), the Highveld was the last part of the country to be settled. Its deeper-weathered red to yellow acid soils have developed on the gentler gradients and in river valleys.
The Middleveld occupies about one-fourth of the country and has an average altitude of 2,000 to 2,500 feet. It is a region of rolling uplands and wide, well-watered valleys. It is mainly underlain by ancient granites and gneisses (metamorphosed granites), with dolerites and quartzites, which have weathered deeply to produce friable red and clay loams interspersed with shallower profiles of sands and sandy loams. To the Swazi it is known as Live (“The Country”) or Inkabave (“The Navel”) and is the heartland of the Swazi nation.
The Lowveld, or Bushveld, covering nearly 40 percent of the country, is a generally undulating lowland with isolated knolls and ridges rising abruptly above the general level of 500 to 1,000 feet. In general, the soils reflect the transition from the acidic granites and sandstones of the western Lowveld to the more basic basalts and dolerites of the eastern part—i.e., from sandy loams in the west to red and black clays in the east, the latter being some of the most naturally fertile soils in the country. This region is called Lihlanze by the Swazi, meaning a warm place with trees—in its undisturbed state, the typical African savanna.
The Lubombo escarpment and plateau covers about 5 percent of the country, consisting of a narrow strip of about 600 square miles. It rises abruptly from the Lowveld to an average altitude of 2,000 feet, with higher peaks (Siteki and Mananga) of about 2,500 feet in the north. It is deeply dissected by the gorges of three of the main rivers that traverse the country from west to east, the Umbuluzi, the Usutu, and the Ingwavuma. The plateau soils vary considerably, from shallow sands to deeper loams, depending on the composition of the volcanic lavas that form the bedrock. The Swazi have no specific name for this part of the country.
- Drainage
Swaziland is one of the best-watered countries in southern Africa. Major perennial rivers, which have their sources in South Africa, flow through the country to the Indian Ocean. They are the Lomati, the Komati, the Umbuluzi, and the Usutu. The Usutu has the largest catchment in the country, with three main tributaries, the Usushwana, the Ngwempisi, and the Mkhondvo. In the south the Ingwavuma rises in western Swaziland and also cuts through the Lubombo.
- Climate
The climate is in general subtropical, but it is strongly influenced by the country’s position on the eastern side of southern Africa, which exposes it to moist maritime tropical air coming off the Indian Ocean for much of the year. The cessation of maritime airflow in winter months because of intensified continental winds produces a high degree of climatic variability. The climate is also subject to steep temperature and precipitation gradients from west to east because of the fall in altitude of about 4,000 feet over a distance of about 50 miles.
Average maximum and minimum monthly temperatures are 72° F (22° C) and 52° F (11° C) in the Highveld and 84° F (29° C) and 59° F (15° C) in the Lowveld. The Middleveld occupies an intermediate position in these gradations.
Swaziland falls within the summer rainfall region of the subcontinent, where about 80 percent of the precipitation falls during the summer months of October to March, usually in the form of thunderstorms and frontal rains. Average annual rainfall in the Highveld is about 55 inches (1,400 millimetres), in the Middleveld 34 inches, in the Lowveld about 22 inches, and on the Lubombo about 35 inches. However, variability in the annual totals is great, and figures have fluctuated dramatically from year to year. In the Middleveld, where the bulk of the population lives, the average has varied from a high of 63 inches to a low of 13 inches within a period of a few years. These extreme fluctuations appear to relate to wetter and drier than average quasi-cyclic fluctuations of from 8 to 11 years, which have been identified in the rainfall records.
- Plant and animal life
The natural vegetation includes forest—confined mostly to the Highveld and the windward slopes of the Lubombo escarpment—savanna, and grassland. Factors such as soil composition and moisture produce a variety of vegetation subtypes. There are both wet and dry forests, various densities of savanna, and several grassland types, which range from sweet to sour based on their palatability when mature and dry. Altogether it is a rich flora, with ferns and flowering plants alone accounting for more than 2,600 species. Some have a very limited distribution and are found only in or around Swaziland.
The natural fauna has been severely depleted in recent years because of habitat destruction caused by the spread of the human population, and representative species such as antelope (impala, reedbuck, duiker, waterbuck, wildebeest, and kudu), hippopotamus, rhinoceros, elephant, giraffe, and zebra are found largely in protected reserves. However, smaller mammals—such as the baboon, monkey, jackal, and mongoose—may still be encountered, and several types of snake have a wide distribution. Crocodiles are also common in Lowveld rivers. Birdlife is abundant in each habitat and comprises both resident and migrant (breeding and nonbreeding) populations. The migrants come from central and North Africa and from farther afield (northern Europe and eastern Asia in the case of storks, swallows, and hawks). Distinctive among the more common birds are barbets, weavers, the various hornbills, the lilac-breasted roller, and the purple-crested loerie.
- Settlement patterns
Traditionally, the Swazi lived in family homesteads (imithi) dispersed throughout the countryside. The only larger settlements were the homesteads of royalty and chiefs. This pattern has been modified since the late 19th century by the exposure of the rural Swazi to the money economy. Nucleated settlements grew up at important administrative and trading centres under British colonial rule from 1903, but the process of urbanization accelerated only after World War II, when the establishment of major agricultural, mining, and industrial operations acted as magnets for job seekers and created sizable company towns such as Mhlume, Simunye, Big Bend, and Mhlambanyatsi. The largest are the administrative capital of Mbabane and the commercial and industrial centre of Manzini. Some 30 percent of the population is urban, and this figure is expected to increase because the urban growth rate exceeds the growth rate of the population as a whole.
The rural population lives within a communal land tenure system administered by the traditional chiefs. A typical homestead includes the main hut of the headman (umnumzane); the huts of his mother, wife (or wives), and children; the kitchen and storerooms; and the cattle enclosure (isibaya) in front and facing east. Cattle are more than draft animals and a source of milk; they constitute a store of wealth for use on social and ceremonial occasions (e.g., lobola, or bride-price).
The traditional pattern of homestead life is strictly seasonal. With the onset of the rains in spring (August or September), women plant gardens along the riverbanks; later, when the heavy rains come in summer (October to February), with help from the men, they plow or hoe to sow corn (maize) and sorghum (a millet) in larger fields. At this time all able women and children abandon their homesteads for the fields, and the men also join in the planting and weeding. The summer months are, on the whole, the hungry months, unless supplemented by remittances from working members of the family. Autumn to early winter (March to May) is the harvest; by July the last of the corn and sorghum has been dried and brought in. Activity then moves to the homesteads, where women and men thresh the grain, the best of which is stored and the remainder consumed at once. Winter is a time for relaxation, hunting, entertaining, and visiting. To some extent this traditional round has been disrupted by population pressure on land, by increased drift to the towns, by the absence of men working in the cities, and by the use of hired tractors for plowing, but the basic pattern is still recognizable.
The traditional centres of Swazi life are the royal villages of the ngwenyama (the king) at Ludzidzini and of the ndlovukazi (the queen mother) at Phondvo, both of which are in the “royal heart” of the country and not far from the old royal capital of Lobamba.
Demography of Swaziland
Economy of Swaziland
Government and Society of Swaziland
Culture Life of Swaziland
History of Swaziland
Disclaimer
This is not the official site of this country. Most of the information in this site were taken from the U.S. Department of State, The Central Intelligence Agency, The United Nations, [1],[2], [3], [4], [5],[6], [7], [8], [9], [10], [11], [12], [13], [14],[15], [16], [17], [18], [19], [20], [21], [22], [23], [24],[25], [26], [27], [28], [29], [30],[31], [32], [33], [34], and the [35].
Other sources of information will be mentioned as they are posted.