Pacanesia: Difference between revisions
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{{ | {{NONCANON}}{{Infobox country | ||
{{Infobox country | |||
| conventional_long_name = State of Pacanesia and Anesia | | conventional_long_name = State of Pacanesia and Anesia | ||
| common_name = Pacanesia | | common_name = Pacanesia | ||
Line 19: | Line 18: | ||
| ethnic_groups_year = 2005 | | ethnic_groups_year = 2005 | ||
| religion = {{ublist |item_style=white-space:nowrap; | | religion = {{ublist |item_style=white-space:nowrap; | ||
| | |47.3% Irreligion | ||
| | |22.8% Islam | ||
| | |10.3% Christianity | ||
| | |7.3% Judaism | ||
|12.6% other or undeclared}} | |||
| demonym = Pacanese | | demonym = Pacanese | ||
| government_type = Federal hereditary dictatorship ''under foreign control'' | | government_type = Federal hereditary dictatorship ''under foreign control'' | ||
Line 42: | Line 42: | ||
| percent_water = 1% | | percent_water = 1% | ||
| population_estimate = 980,000 | | population_estimate = 980,000 | ||
| population_census = | | population_census = 4,648,000 | ||
| population_estimate_year = 2023 | | population_estimate_year = 2023 | ||
| population_census_year = 2005 | | population_census_year = 2005 | ||
| GDP_PPP = $ | | population_density_km2 = 514.79 | ||
| GDP_PPP_year = | | GDP_PPP = $278.3 billion | ||
| GDP_nominal = $ | | GDP_PPP_year = 2005 | ||
| GDP_nominal = $278.3 billion | |||
| GDP_nominal_year = 2023 | | GDP_nominal_year = 2023 | ||
| Gini = 29.1 | | Gini = 29.1 | ||
| Gini_change = increase | | Gini_change = increase | ||
| HDI = 0. | | HDI = 0.728 | ||
| HDI_year = 2023 | | HDI_year = 2023 | ||
| HDI_change = increase | | HDI_change = increase | ||
| currency | | currency = {{ublist| kuata (—2010) | [[Riamese hull]] (2010—)}} | ||
| currency_code | | currency_code = RMH | ||
| utc_offset = +6 | | utc_offset = +6 | ||
| date_format = dd/mm/yyyy | | date_format = dd/mm/yyyy | ||
Line 64: | Line 65: | ||
| englishmotto = 'My Country o' My Country!' | | englishmotto = 'My Country o' My Country!' | ||
| capital_exile = Kahalie | | capital_exile = Kahalie | ||
| religion_year = 2005 | |||
}} | }} | ||
'''Pacanesia''', officially the '''State of Pacanesia and Anesia''' (Pacanese: ''Taheya o Pakaw e te Anaw'se'') is an an archipelagic nation located in the southern fringes of the Kaldaz Ocean. The nation is made up of 20 islands in 2 archipelagos, 12 in Pacanesia and 8 in Anesia. According to the World Assembly, as of 2023, Pacanesia has an estimated population of approximately 980,000. In contrast, the pre-war census conducted in 2005 reported a population of | '''Pacanesia''', officially the '''State of Pacanesia and Anesia''' (Pacanese: ''Taheya o Pakaw e te Anaw'se'') is an an archipelagic nation located in the southern fringes of the Kaldaz Ocean. The nation is made up of 20 islands in 2 archipelagos, 12 in Pacanesia and 8 in Anesia. According to the World Assembly, as of 2023, Pacanesia has an estimated population of approximately 980,000. In contrast, the pre-war census conducted in 2005 reported a population of 3,548,000 inhabitants. The capital and largest city is Jenni-Bahar, home to over 500,000 people—over 50% of the entire country's population. The de facto capital-in-exile is Kahalie, which used to be the largest city at over 700,000 before the civil war in 2005. | ||
Of the 2005 population, 51% identified as ethnically White, while | Of the 2005 population, 51% identified as ethnically White, while 21.3% identified as ethnically Pacanese. 27.1% are grouped into the "Ultramaro and multiracial" category, which is primarily made up of Anáhuacese, Arab and Mixed people. The rest of the census group categorized as "other", 0.6% of the population. | ||
Pacanesia's history spans two millenias, marked by the arrival of settlers via Pohnpenesia. Under various rulers, including kingdoms and tribedoms, it became a part of the Kaldaic Empire in the 13th century. Post-colonization in the late 16th century transformed the archipelago into the Kingdom of Pacanay in 1785. The 20th century witnessed Riamo's invasion, leading to Pacanesia becoming a Mandate of the Empire. Independence was achieved in 1930. In 2005, democratic mismanagement and dictatorship triggered a civil war. Riamo and Pohnpenesia invaded in 2010, establishing the Joint Territory of Pacanesia and exiling the government. The Civil War has plunged the nation into chronic poverty and conflict, displacing over half the population, causing over 350,000 casualties, mostly civilians, and decimating the economy. | Pacanesia's history spans two millenias, marked by the arrival of settlers via Pohnpenesia. Under various rulers, including kingdoms and tribedoms, it became a part of the Kaldaic Empire in the 13th century. Post-colonization in the late 16th century transformed the archipelago into the Kingdom of Pacanay in 1785. The 20th century witnessed Riamo's invasion, leading to Pacanesia becoming a Mandate of the Empire. Independence was achieved in 1930. In 2005, democratic mismanagement and dictatorship triggered a civil war. Riamo and Pohnpenesia invaded in 2010, establishing the Joint Territory of Pacanesia and exiling the government. The Civil War has plunged the nation into chronic poverty and conflict, displacing over half the population, causing over 350,000 casualties, mostly civilians, and decimating the economy. | ||
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{{WIP}} | {{WIP}} | ||
== Geography == | == Geography == | ||
Pacanesia comprises an archipelagic territory encompassing 20 islands, distributed across two primary archipelagoes in the Kaldaz Ocean: Pacanesia in the north and Anesia in the south. Twelve islands are situated within the Pacanese Archipelago, while eight are part of Anesia. Pacanon stands as the largest island, while Um Agaba holds the distinction of being the smallest. Positioned as one of the southernmost territories | Pacanesia comprises an archipelagic territory encompassing 20 islands, distributed across two primary archipelagoes in the Kaldaz Ocean: Pacanesia in the north and Anesia in the south. Twelve islands are situated within the Pacanese Archipelago, while eight are part of Anesia. Pacanon stands as the largest island, while Um Agaba holds the distinction of being the smallest. Positioned as one of the southernmost territories in the world, Pacanesia maintains an average latitude exceeding -70°. | ||
Due to tectonic activity, Pacanesia's topology is diverse. The Pacanese Islands, especially Pacanon, have extremely rugged and craggy terrain, with valleys and mountain peaks situated throughout. The highest peak is Mt. Susulu, a volcano in the Antipácano Range in Pacanon, reaching a height of 3,456 meters. In Anesia, most islands maintain a relatively flat landscape, due to low tectonic pressure compared to the Pacanese archipelago. The Gran Pantana, situated between the islands of Pacanon and Magali'i, constitutes an expansive region characterized by marshland and swampland. It represents the lowest elevations within the nation and experiences recurrent flooding during the summer season. | Due to tectonic activity, Pacanesia's topology is diverse. The Pacanese Islands, especially Pacanon, have extremely rugged and craggy terrain, with valleys and mountain peaks situated throughout. The highest peak is Mt. Susulu, a volcano in the Antipácano Range in Pacanon, reaching a height of 3,456 meters. In Anesia, most islands maintain a relatively flat landscape, due to low tectonic pressure compared to the Pacanese archipelago. The Gran Pantana, situated between the islands of Pacanon and Magali'i, constitutes an expansive region characterized by marshland and swampland. It represents the lowest elevations within the nation and experiences recurrent flooding during the summer season. | ||
[[File:Gran Pantana.jpeg|200px|thumb|left|the Gran Pantana marshes.]] | [[File:Gran Pantana.jpeg|200px|thumb|left|the Gran Pantana marshes.]] | ||
Unlike Pohnpenesia, where volcanic activity contributed significantly to island formation, all of Pacanesia's islands were shaped through tectonic drift, with minimal volcanic influence aside from Pacanon. There are virtually no | Unlike Pohnpenesia, where volcanic activity contributed significantly to island formation, all of Pacanesia's islands were shaped through tectonic drift, with minimal volcanic influence aside from Pacanon. There are virtually no large bodies of water in the archipelago with the exception of the Kahalie Delta, emptying into the Totoni Pott. However, small crater lakes (''potts'') are not uncommon, particularly in Anesia, while the primary watercourses consist mainly of the Arroya Friya river extending from Kahalie to Atas Bandaw; with several tributaries. Several waterfalls are also present, notably on the island of Hemolele. | ||
Geographical consensus posits that Pacanesia's islands form part of a submerged mass of continental crust known as 'Caldacia.' This geological formation extends from the Pacanese Archipelago to the Boscettian Islands in Pohnpenesia, primarily concentrated within Pacanesia. Elevation maps substantiate this perspective. The prevailing theory suggests that Caldacia, along with most of the Pohnpenesian Island Group (PIG), diverged from the Meredonnean continent over 90 million years ago. Anesia's flat terrain and low topography is attributed to the absence of significant tectonic thrust, due to the archipelago's separation from the continent with minimal collision. the Tel Aleya | Geographical consensus posits that Pacanesia's islands form part of a submerged mass of continental crust known as 'Caldacia.' This geological formation extends from the Pacanese Archipelago to the Boscettian Islands in Pohnpenesia, primarily concentrated within Pacanesia. Elevation maps substantiate this perspective. The prevailing theory suggests that Caldacia, along with most of the Pohnpenesian Island Group (PIG), diverged from the Meredonnean continent over 90 million years ago. Anesia's flat terrain compared to Pacanesia, and it's low topography, is attributed to the absence of significant tectonic thrust, due to the archipelago's separation from the continent with minimal collision. the Tel Aleya Mountain located in Haunderria, the largest island in the Anesian Group, stands as the highest point in Anesia, with an elevation of around 232 meters at the maximum. | ||
[[File:Mount Susulu.jpeg|200px|thumb|left|Mount. Susulu towering over suburbs near Kahalie.]] | |||
=== Climate === | |||
Due to it's extreme southern latitude, Pacanesia is one of the most coldest countries on the planet. The climate zones are mainly split into the 2 archipelagoes of Pacanesia and Anesia. The Pacanese Archipelago, especially Pacanon, has an average summer high of around 10-12 °C, while Anesia's summer temperatures are only between 4-6 °C on average. Most of Pacanon maintains relatively moderated temperatures due to Kaldaic trade winds from Pohnpenesia. Anesia's low topography makes it susceptible to extreme temperature swings throughout the year, especially coastal cities. |
Latest revision as of 13:34, 13 April 2024
This text is non-canon because it was either retconned, the lore was changed, or the countries listed in this article no longer exist. Please comment on this article's talk page to share your input, comments and questions. Note: Linking this article might complicate your own worldbuilding. |
State of Pacanesia and Anesia Taheya o Pakaw e te Anaw'se (Pacanese) | |
---|---|
Motto: Na Taheya o' Na Taheya 'My Country o' My Country!' | |
Anthem: "Prevail in the Seas" | |
Capital and largest city | Jenni-Bahar |
Capital-in-exile | Kahalie |
Official languages |
|
Regionalized language |
|
Ethnic groups (2005) |
|
Religion (2005) |
|
Demonym(s) | Pacanese |
Government | Federal hereditary dictatorship under foreign control |
• President | Tariqua Abadul |
Legislature | General Kiuva |
Legally administrated by Pohnpenesia and Riamo as a joint territory, local government in exile since 2010. | |
• Kingdom of Pacanay | 1785 |
• Riamese mandate | 1905 |
• Independence | 1930 |
• Pacanese civil war begins | 2005 |
• Invasion of Pacanesia and Riamo-Pohnpenesian control | 2010- |
Area | |
• Total | 9,029 km2 (3,486 sq mi) |
• Water (%) | 1% |
Population | |
• 2023 estimate | 980,000 |
• 2005 census | 4,648,000 |
• Density | 514.79/km2 (1,333.3/sq mi) |
GDP (PPP) | 2005 estimate |
• Total | $278.3 billion |
GDP (nominal) | 2023 estimate |
• Total | $278.3 billion |
Gini | 29.1 low |
HDI (2023) | 0.728 high |
Time zone | UTC+6 |
Date format | dd/mm/yyyy |
Driving side | right |
Calling code | +451 |
Internet TLD | .pc |
Pacanesia, officially the State of Pacanesia and Anesia (Pacanese: Taheya o Pakaw e te Anaw'se) is an an archipelagic nation located in the southern fringes of the Kaldaz Ocean. The nation is made up of 20 islands in 2 archipelagos, 12 in Pacanesia and 8 in Anesia. According to the World Assembly, as of 2023, Pacanesia has an estimated population of approximately 980,000. In contrast, the pre-war census conducted in 2005 reported a population of 3,548,000 inhabitants. The capital and largest city is Jenni-Bahar, home to over 500,000 people—over 50% of the entire country's population. The de facto capital-in-exile is Kahalie, which used to be the largest city at over 700,000 before the civil war in 2005.
Of the 2005 population, 51% identified as ethnically White, while 21.3% identified as ethnically Pacanese. 27.1% are grouped into the "Ultramaro and multiracial" category, which is primarily made up of Anáhuacese, Arab and Mixed people. The rest of the census group categorized as "other", 0.6% of the population.
Pacanesia's history spans two millenias, marked by the arrival of settlers via Pohnpenesia. Under various rulers, including kingdoms and tribedoms, it became a part of the Kaldaic Empire in the 13th century. Post-colonization in the late 16th century transformed the archipelago into the Kingdom of Pacanay in 1785. The 20th century witnessed Riamo's invasion, leading to Pacanesia becoming a Mandate of the Empire. Independence was achieved in 1930. In 2005, democratic mismanagement and dictatorship triggered a civil war. Riamo and Pohnpenesia invaded in 2010, establishing the Joint Territory of Pacanesia and exiling the government. The Civil War has plunged the nation into chronic poverty and conflict, displacing over half the population, causing over 350,000 casualties, mostly civilians, and decimating the economy.
Etymology
The etymology of the term "Pacanesia" is a subject of debate, with several theories claimed regarding its origin. The first and most widely accepted theory among scholars suggests a derivation from the Proto-Kaldaic root "p¹-kʷ," denoting wood, referring to the abundant forests in the region. Another theory, proposed by the Kaldaz Archaeology Institute, contends that "Pacanesia" may have originated from a Korsannean term, "pakua," meaning frost.
History
This article is incomplete because it is pending further input from participants, or it is a work-in-progress by one author. Please comment on this article's talk page to share your input, comments and questions. Note: To contribute to this article, you may need to seek help from the author(s) of this page. |
Geography
Pacanesia comprises an archipelagic territory encompassing 20 islands, distributed across two primary archipelagoes in the Kaldaz Ocean: Pacanesia in the north and Anesia in the south. Twelve islands are situated within the Pacanese Archipelago, while eight are part of Anesia. Pacanon stands as the largest island, while Um Agaba holds the distinction of being the smallest. Positioned as one of the southernmost territories in the world, Pacanesia maintains an average latitude exceeding -70°.
Due to tectonic activity, Pacanesia's topology is diverse. The Pacanese Islands, especially Pacanon, have extremely rugged and craggy terrain, with valleys and mountain peaks situated throughout. The highest peak is Mt. Susulu, a volcano in the Antipácano Range in Pacanon, reaching a height of 3,456 meters. In Anesia, most islands maintain a relatively flat landscape, due to low tectonic pressure compared to the Pacanese archipelago. The Gran Pantana, situated between the islands of Pacanon and Magali'i, constitutes an expansive region characterized by marshland and swampland. It represents the lowest elevations within the nation and experiences recurrent flooding during the summer season.
Unlike Pohnpenesia, where volcanic activity contributed significantly to island formation, all of Pacanesia's islands were shaped through tectonic drift, with minimal volcanic influence aside from Pacanon. There are virtually no large bodies of water in the archipelago with the exception of the Kahalie Delta, emptying into the Totoni Pott. However, small crater lakes (potts) are not uncommon, particularly in Anesia, while the primary watercourses consist mainly of the Arroya Friya river extending from Kahalie to Atas Bandaw; with several tributaries. Several waterfalls are also present, notably on the island of Hemolele.
Geographical consensus posits that Pacanesia's islands form part of a submerged mass of continental crust known as 'Caldacia.' This geological formation extends from the Pacanese Archipelago to the Boscettian Islands in Pohnpenesia, primarily concentrated within Pacanesia. Elevation maps substantiate this perspective. The prevailing theory suggests that Caldacia, along with most of the Pohnpenesian Island Group (PIG), diverged from the Meredonnean continent over 90 million years ago. Anesia's flat terrain compared to Pacanesia, and it's low topography, is attributed to the absence of significant tectonic thrust, due to the archipelago's separation from the continent with minimal collision. the Tel Aleya Mountain located in Haunderria, the largest island in the Anesian Group, stands as the highest point in Anesia, with an elevation of around 232 meters at the maximum.
Climate
Due to it's extreme southern latitude, Pacanesia is one of the most coldest countries on the planet. The climate zones are mainly split into the 2 archipelagoes of Pacanesia and Anesia. The Pacanese Archipelago, especially Pacanon, has an average summer high of around 10-12 °C, while Anesia's summer temperatures are only between 4-6 °C on average. Most of Pacanon maintains relatively moderated temperatures due to Kaldaic trade winds from Pohnpenesia. Anesia's low topography makes it susceptible to extreme temperature swings throughout the year, especially coastal cities.