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== Geography == | == Geography == | ||
At approximately 1,055,828 square kilometres (407,657 square miles), Nuvania is the third largest country in [[Asteria Inferior]]. It is home to a number of topographical features and ecoregions that have had a significant impact on the people that live there. | |||
Northern Nuvania is composed of the ''[[Kustveld]]'', a wide alluvial {{wpl|floodplain}} that extends from the northern slopes of the [[Grootreeks]]. The ''Kustveld'' is divided between the immediate {{wpl|littoral}} and seasonal floodplains, the drier but still humid ''insulaire kust'' and the foothills of the Grootreeks. The seasonal floodplains are known in Nuvania as the ''vloedlande'' and are a series of seasonal {{wpl|riparian wetlands}} and along the immediate coast, {{wpl|salt water}} {{wpl|swamps}}. These areas were once more extensive, but have since been drained to create {{wpl|farmland}} and {{wql|urban areas}}, or have been modified to grow crops such as {{wpl|rice}}. The alluvial nature of the soils make the ''Kustveld'' one of the most fertile areas in Nuvania for {{wpl|pastures}} and crop growing, and the flat nature of the terrain make it suitable for the construction of large urban areas, making the ''Kustveld'' the most densely populated part of Nuvania. This has resulted in substantial losses of forest in the region, in addition to riparian and coastal wetlands. | |||
The ''[[Droëveld]]'' dominates central Nuvania, stretching from the border with [[Vilcasuamanas]] in the east to the coast on the far northern [[Sublustrian Sea]] in the west. It is one of the most sparsely populated areas in Nuvania. Much of the terrain is rolling or largely flat, with dry and {{wpl|seasonal streams}}, and lakes interspersed among eroded {{wpl|gullies}} known as ''grootkraake'' which flood during heavy rains. Within the ''Droëveld'' are multiple different zones, although the largest itself is called ''Droëveld'', meaning "dry field". ''Droëveld'' is typically flat or rolling terrain with {{wpl|grass}} cover and {{wpl|cacti}}, shrubs as principal cover, although {{wpl|trees}} used to the difficult climate are also found. The soil is a mixture of ancient {{wpl|alluvial}} {{wpl|sands}] and {{wpl|clay}}, which is easily eroded. While parts resemble a {{wpl|desert}}, the ''droëveld'' is not considered a true desert but instead a {{wpl|tropical dry forest}}. The flatter parts of the ''droëveld'' are simply referred to as the ''veld''. The area is rich in {{wpl|iron ore}}, with virtually all of Nuvania's iron ore mines located in this region. | |||
''[[Bushveld]]'' is found along the south facing slopes of the ''Grootreeks'' and typically consists of {{wpl|dry forests}} and {{wpl|bushland}} along the foothills and principal ranges themselves. Here the terrain mostly consists of rugged, often inaccessible terrain with deep {{wpl|valleys}}, and steep mountain slopes. This area has greater vegetation cover owing to its altitude, as it collects the {{wpl|precipitation}} from coastal weather systems during the short {{wpl|wet season}}, in addition to numerous {{wpl|fresh water springs}}. The ''bushveld'' is more prevalent towards the western coast, and largely does not exist towards the border with [[Vilcasuamanas]]. | |||
The ''[[Westveld]]'' is a name given to the area of flat lands between the coast and the ''droëveld'' which principally exists in [[Steynland]]. This area marks the transition between the rolling terrain of the ''droëveld'' and the low coastal plains. The ''westveld'' is especially known for the {[wpl|red soils}} rich in {{wpl|iron ores}} and {{wpl|oxides}}, as well as the comparatively little {{wpl|vegetation}} cover aside from certain species of {{wpl|palms}}. It is the smallest of the ''veld'' regions in Nuvania, and aside from the {{wpl|vegetation}}, has little defining features. | |||
Nuvania shares the [[Van Horn Strait]] with [[Vlissingemond]], and much of its western coast immediately faces the eastern coast of Vlissingemond. Known in Nuvania as the ''[[West Kust]]'', this area stretches from southwestern [[Kaap]] province through [[Steynland]], [[Arania]], and northwestern [[Suid Arania]]. It is predominantly flat and either sandy or alluvial in nature as the {{wpl|rivers}} that cross the central veld region empty into the [[Van Horn Strait]]. Like the ''westveld'', there is very little to define it from other parts of the coast aside from the relative {{wpl|aridity}}. However, the ''West Kust'' has significant deposits of {{wpl|phosphates}} which are economically important to local communities. The southern coast that faces the [[Sublustrian Sea]] proper shares much of the same features, but lacks the phosphate deposits. | |||
Nuvania's dominant geographic feature is the [[Grootreeks]], a series of ranges stretching from [[Vilcasuamanas]] into northern Nuvania. The Grootreeks form part of an ancient {{wpl|rift system}} that separated the [[Asterias]] millions of years ago, with {{wpl|rift faulting}} and {{wpl|continental drift}} still occurring. Because of the nature of the Grootreeks, much of the {{wpl|soil}} and {{wpl|rock higher}} up is volcanic in nature, and {{wpl|seismic activity}} is still present in the mountain chain, although few large {{wpl|earthquakes}} are recorded. {{wpl|Geothermal activity}} takes place on both the northern and southern sides of the mountain range, the most famous being the [[Duiwelsbad Hot Springs]] near [[Meyershof]]. Because of the tectonic nature of the origin of these mountains, the Grootreeks are rich in numerous {{wpl|minerals}}, including {{wpl|precious metals}} such as {{wpl|gold}}, {{wpl|silver}}, and {{wpl|platinum}}, with the latter being found most abundantly in the southern ranges. The Grootreeks are home to numerous mountain peaks over 4,000 metres in height despite being outside of the primary crustal uplift. The tallest mountain in Nuvania is [[Mount de Wet]] at 4,507 metres (14,786 feet) in height, located in the Central Range of the Grootreeks. | |||
A spur from the same mountain range can be found in southern Nuvania, close to the frontier with x. These are known as the [[Kleine Grootreeks]]. These mountains are unusual in that they were formed in a similar manner to the Grootreeks, but are much older, and therefore are more eroded and weathered. Scientists have {{wpl|Radio carbon dating|dated}} the rocks at over two billion years old, and consider the Kleine Grootreeks to have been a part of an ancient rift system which could have been involved in the creation of both [[Asteria Inferior]] and [[Asteria Superior]]. These mountains contain a number of minerals, but are less mineral rich than the Grootreeks themselves. [[Rondetop]] is the tallest mountain in the Kleine Grootreeks at 2,251 metres (7,385 feet) in height. | |||
Most river courses in Nuvania are {{wpl|seasonal}} or {{wpl|dry}}, especially in the central ''veld'' region. In the north, there is ample rainfall where permanent rivers and streams flow. The longest river in this region is the [[Bruin River|Bruin]] at 328 kilometres long. The longest river in Nuvania is the [[Krige River]] at 862 kilometres. | |||
=== Climate === | === Climate === | ||
Revision as of 09:56, 1 September 2019
Nuvanian Free State Nuwanse Vrystaat | |
|---|---|
 Flag | |
| Motto: "Ons land, ons vryheid"(Asteriaans) "Our Land, Our Freedom" | |
| Anthem: Die Stem van Nuwanië The Call of Nuvania | |
 | |
| Capital and largest city | Pietersburg |
| Official languages | Asteriaans |
| Demonym(s) | Nuvanian |
| Government | Parliamentary republic |
| Walter Kronje | |
| Robert Marten | |
| Establishment | |
| 12 October 1673 | |
| 20 July 1720 | |
| 20 February 1819 | |
| 1 September 1886 | |
| Area | |
• Total | 1,055,828 km2 (407,657 sq mi) |
• Water (%) | 0.8 |
| Population | |
• July 2019 estimate | 48,177,598 |
• 2015 census | 47,448,333 |
• Density | 44.9/km2 (116.3/sq mi) |
| GDP (PPP) | July 2019 estimate |
• Total | $1.37 trillion |
• Per capita | $28,895 |
| GDP (nominal) | July 2019 estimate |
• Total | $530.33 billion |
• Per capita | $11,177 |
| HDI | 0. low |
| Currency | Goudë (₲) (NUG) |
| Time zone | Nuvanian Standard Time |
| Driving side | left |
| Calling code | 500 |
| Internet TLD | .nu |
Nuvania (Nuvanian: Nuwanië), officially the Nuvanian Free State (Nuwanse Vrystaat) is a sovereign state located in western Asteria Inferior. It is bordered to the west by Vlissingemond, to the northeast by Vilcasumanas, and to the east by Alforja, with coasts on the Vehmens Ocean and the Arucian Sea. With 47.4 million inhabitants, Nuvania is the second most populous country in Asteria Inferior.
Etymology
Geography
At approximately 1,055,828 square kilometres (407,657 square miles), Nuvania is the third largest country in Asteria Inferior. It is home to a number of topographical features and ecoregions that have had a significant impact on the people that live there.
Northern Nuvania is composed of the Kustveld, a wide alluvial floodplain that extends from the northern slopes of the Grootreeks. The Kustveld is divided between the immediate littoral and seasonal floodplains, the drier but still humid insulaire kust and the foothills of the Grootreeks. The seasonal floodplains are known in Nuvania as the vloedlande and are a series of seasonal riparian wetlands and along the immediate coast, salt water swamps. These areas were once more extensive, but have since been drained to create farmland and Template:Wql, or have been modified to grow crops such as rice. The alluvial nature of the soils make the Kustveld one of the most fertile areas in Nuvania for pastures and crop growing, and the flat nature of the terrain make it suitable for the construction of large urban areas, making the Kustveld the most densely populated part of Nuvania. This has resulted in substantial losses of forest in the region, in addition to riparian and coastal wetlands.
The Droëveld dominates central Nuvania, stretching from the border with Vilcasuamanas in the east to the coast on the far northern Sublustrian Sea in the west. It is one of the most sparsely populated areas in Nuvania. Much of the terrain is rolling or largely flat, with dry and seasonal streams, and lakes interspersed among eroded gullies known as grootkraake which flood during heavy rains. Within the Droëveld are multiple different zones, although the largest itself is called Droëveld, meaning "dry field". Droëveld is typically flat or rolling terrain with grass cover and cacti, shrubs as principal cover, although trees used to the difficult climate are also found. The soil is a mixture of ancient alluvial [[Wikipedia:sands}] and clay, which is easily eroded. While parts resemble a desert, the droëveld is not considered a true desert but instead a tropical dry forest. The flatter parts of the droëveld are simply referred to as the veld. The area is rich in iron ore, with virtually all of Nuvania's iron ore mines located in this region.
Bushveld is found along the south facing slopes of the Grootreeks and typically consists of dry forests and bushland along the foothills and principal ranges themselves. Here the terrain mostly consists of rugged, often inaccessible terrain with deep valleys, and steep mountain slopes. This area has greater vegetation cover owing to its altitude, as it collects the precipitation from coastal weather systems during the short wet season, in addition to numerous fresh water springs. The bushveld is more prevalent towards the western coast, and largely does not exist towards the border with Vilcasuamanas.
The Westveld is a name given to the area of flat lands between the coast and the droëveld which principally exists in Steynland. This area marks the transition between the rolling terrain of the droëveld and the low coastal plains. The westveld is especially known for the {[wpl|red soils]] rich in iron ores and oxides, as well as the comparatively little vegetation cover aside from certain species of palms. It is the smallest of the veld regions in Nuvania, and aside from the vegetation, has little defining features.
Nuvania shares the Van Horn Strait with Vlissingemond, and much of its western coast immediately faces the eastern coast of Vlissingemond. Known in Nuvania as the West Kust, this area stretches from southwestern Kaap province through Steynland, Arania, and northwestern Suid Arania. It is predominantly flat and either sandy or alluvial in nature as the rivers that cross the central veld region empty into the Van Horn Strait. Like the westveld, there is very little to define it from other parts of the coast aside from the relative aridity. However, the West Kust has significant deposits of phosphates which are economically important to local communities. The southern coast that faces the Sublustrian Sea proper shares much of the same features, but lacks the phosphate deposits.
Nuvania's dominant geographic feature is the Grootreeks, a series of ranges stretching from Vilcasuamanas into northern Nuvania. The Grootreeks form part of an ancient rift system that separated the Asterias millions of years ago, with rift faulting and continental drift still occurring. Because of the nature of the Grootreeks, much of the soil and rock higher up is volcanic in nature, and seismic activity is still present in the mountain chain, although few large earthquakes are recorded. Geothermal activity takes place on both the northern and southern sides of the mountain range, the most famous being the Duiwelsbad Hot Springs near Meyershof. Because of the tectonic nature of the origin of these mountains, the Grootreeks are rich in numerous minerals, including precious metals such as gold, silver, and platinum, with the latter being found most abundantly in the southern ranges. The Grootreeks are home to numerous mountain peaks over 4,000 metres in height despite being outside of the primary crustal uplift. The tallest mountain in Nuvania is Mount de Wet at 4,507 metres (14,786 feet) in height, located in the Central Range of the Grootreeks.
A spur from the same mountain range can be found in southern Nuvania, close to the frontier with x. These are known as the Kleine Grootreeks. These mountains are unusual in that they were formed in a similar manner to the Grootreeks, but are much older, and therefore are more eroded and weathered. Scientists have dated the rocks at over two billion years old, and consider the Kleine Grootreeks to have been a part of an ancient rift system which could have been involved in the creation of both Asteria Inferior and Asteria Superior. These mountains contain a number of minerals, but are less mineral rich than the Grootreeks themselves. Rondetop is the tallest mountain in the Kleine Grootreeks at 2,251 metres (7,385 feet) in height.
Most river courses in Nuvania are seasonal or dry, especially in the central veld region. In the north, there is ample rainfall where permanent rivers and streams flow. The longest river in this region is the Bruin at 328 kilometres long. The longest river in Nuvania is the Krige River at 862 kilometres.