Difference between revisions of "Geography of Azazia"

Revision as of 02:14, 18 February 2006

The United Kingdom of Azazia, Juristan, Kingsland, and the Indian Islands, or UK, consists of several various islands and archipelagos scattered amongst the Pacific and Indian Oceans, with the bulk of the UK’s landmass residing in the north central Pacific Ocean on the Azazian Archipelago. The home country of Juristan rests within the Sea of Japan while Kingsland is located on the continent of Irathria and the Indian Islands consist of the Andaman and Nicobar Islands in the eastern Indian Ocean.

Physical Geography

The United Kingdom sports a widely-varied geography, owing to its numerous scattered locations across the globe from the Azazian Sea (alternatively called the Sea of Azazia) to the New Brittany Range, the island of New Australia, and the islands of Juristan and of the Verdant Archipelago. Despite the prevalence of islands in UK geography many were carved by diverse processes from volcanic eruptions to tectonic movements to glaciation and the rise of sea-levels.

Geology of the United Kingdom

The Home Islands formed from the collision of two continental tectonic plates the Azazian Plate and the Belden Plate, where the Azazian Plate broke away from Laurasia and shot across the Pacific rapidly until slamming into the Belden Plate, which had similarly violently torn itself free from the western end of Laurasia until the two collided in the north central Pacific.

The impact of the two plates, of which the Azazian is by far the larger, has led to the subduction of the Belden Plate underneath that of the Azazian, resulting in the New Brittany Mountain Range. Subduction has largely ceased and the Azazian and Belden Plates have merged into the Azazian-Belden Plate.

Both the Azazian and Belden Plates had consisted of lowlands except in the north and west, where subduction of the Pacific Plate underneath the Azazian Plate created the Ashley Mountains, named after Edward Ashley, an English navigator who charted the western islands.

During the last period of glaciation a massive glacier extended across most of the central Azazian continent, consisting of the merged plates. And as the glaciers retreated they carved a deep channel between the New Brittany Mountains, the Brittany Strait – which now separates the geologically linked New Brittany and Oceania mountain ranges. The weight of the glacier also depressed the central lowlands, and upon the glacier’s retreat and melting, the land gave way to the sea and numerous channels opened and flooded the depressed centre of the continent and creating the Sea of Azazia.

To the west, the subduction zone of the Pacific into the Azazian allowed for a firm western boundary of the Sea of Azazia, largely in numerous mountainous islands, which are accordingly volcanic in nature and still growing. The eastern boundary of the inland sea is formed by the eroded and sunken remnants of the northern reaches of the New Brittany Range and the piedmont on the now largely absorbed and/or sunken Belden Plate, which accounts for the comparatively low islands of Paxnova, Rimbaldt, and Torvey.

Mountains and Hills

The largest mountain range consists of the various portions of the Ashley Range, which has several important gaps that have become the channels separating New Australia from Arista and Arista from Nova Russka. These mountains are geologically young and the subduction process is still active, which results in several active volcanoes although there have been no serious eruptions since pre-colonial times.

The highest range, however, is the New Brittany Range, in conjunction with the Oceania Range – although the Oceania is the smaller and shorter of the two. Mount James is the highest mountain in the New Brittany Range as well as the Home Islands, ascending to a height of 7,921 meters on the northwest coast of New Britain. Mount Archibald is the second highest peak in the UK and is also located within the New Brittany Range just to the west of Imperium, soaring 7,782 meters high.

Because of the disparate nature of the UK, there are other mountains of notable height within the kingdom including Mount Burke in the Royal Crown Colony of Port Nelson, which peaks at 4,602 meters. For the most part, however, the geography of the mountains and hills on the various islands largely includes rolling hills, the remnants of mountains eroded during the last period of glaciation and from the submergence of mountains under the sea as the sea level rose at the end of the same period of glaciation.

Rivers, Lakes, and Inland Seas

Owing in large part to the small area of each island in the United Kingdom, there are no mega-river systems in the Home Islands. The largest is the River Tenka, which runs north for some 2,600 kilometers from the Bennington Mountains before emptying into the Azazian Sea, its mouth occupied on both sides by the city of Queensbury. Owing to their small size, Juristan, Kingsland, and the Indian Islands feature either rivers shorter than that of the Tenka or none at all.

However it should be noted that owing to the high mountain ranges, particularly in the southeast and northwest of the Home Islands, the Azazian Archipelago boasts a moderate number of small-length rivers that carry significant amounts of water from the mountains, which absorb large amounts of precipitation owing to the heavy rainfall. Among this class of river are rivers such as the Cerisa, Arista, and Cooley.

The UK also features a dearth of large lakes, although nearly two hundred small lakes can be found in the various mountains throughout the country. In the geologic past, however, the region of central lowlands now submerged as the Azazian Sea boasted numerous large lakes.

As noted, the Azazian Sea is the pre-eminent natural body of water that has shaped the development of the Home Islands. Before the prior ice age a large river flowed from the New Brittany/Oceania Range northwards along what is now the undersea Beckett Channel, a deep cut in the seabed. The Azazia River drained the whole of the interior continent, with rivers such as the Tenka acting as small tributaries that drained more specific highland areas. With the coming ice age, however, the vast interior was consumed by ice which depressed the land below sea level and so as the ice age ended the glacier retreated and melted, its grooves and channels exposing the inland to the Pacific, which quickly flooded the continent with the Beckett Channel or the Azazia River now running as a deep and navigable passage through the Brittany Straits to its former mouth just north of Port Hamptonshire and Westport.

Artificial Waterways

Because of the large numbers of small rivers and streams and the large inland sea that connects each island to the next the UK has seen no real need for massive canal systems to be constructed. Most waterways traversing the land are to be found on New Australia, the largest island in the UK and even then most waterways are used for the purpose of irrigation.

Coastline

Islands

Climate

(For more information see the Climate of Azazia)

Although varied in geography and disparate in nature the UK typically experiences temperate climates with warm temperatures and moderate precipitation.

For the Home Islands, the most important mechanisms for the climate and temperature are the warm Pacific currents, specifically the Northern Equatorial Current and the North Pacific Current, and the prevailing winds that emanate from the Pacific anticyclone, providing cool, dry air to much of the archipelago.

Precipitation usually falls most regularly during the winter months, as the decreasing temperatures shift the anticyclone further north, allowing low pressure systems to advance across the archipelago. With most of these weather systems originating in the west or the south, areas fronting the sea and backed by mountains, specifically areas on the western coasts of Arista, Nova Russka, and San Isabel. The whole western plains of New Australia also experience moderate amounts of rainfall in addition to the southern coast, with areas near the Oceania Range, such as Breningrad and Philadelphia receiving significant amounts of precipitation due to the amplification caused by the orthographic effect.

Human Geography

International Boundaries

The Azazian Archipelago, alternatively styled as the Home Islands for their historical importance and primacy in the development of the UK, has no land borders with any foreign power, as do the Indian Islands; however, the home country of Juristan is located on the northeastern quadrant of an island of several powers and so the United Kingdom technically shares a land border with the nations of Neo-Soviet Russia, Slaytanicca, Lachenburg, and Red Tide2. At this moment, the UK does not share any land border with foreign governments in Kingsland.

With respects to the colonies and territories, the UK shares a land border with several other nations – most prominently in Sarnia, where the UK borders the nations of Sarzonia and a territory of the Kingdom of Geletia. The Royal Crown Dependency of Victoria was granted to the United Kingdom in the aftermath of the Lindimese Civil War, resulting in the transfer of a small area of Lindimese soil around an undeveloped deep water harbour where the UK has constructed a dependency. Because of its status of sovereign UK territory, the United Kingdom can also be considered as having a land border with Lindim.

Lastly the UK shares several borders of close maritime proximity, borders consisting of rivers of small channels that separate UK territory from those of other sovereign states. The Royal Crown Colony of Port Elizabeth is situated within the western islands of the Jipangunesian Archipelago, and with several islands within sight from the beaches of UK territory it can be said that the UK shares a close proximity border with Jipangunesia. The Verdant Archipelago Union also at one time shared such a boundary with the UK until its populace voted to enter into a Commonwealth with the United Kingdom, and in recognizing the reigning monarch of the UK as head of state the border is no longer considered an international border.

National Sovereignty

Local Government

Demographics

Economic Geography

(For more information see Economic Geography of Azazia)

Primary Sector

The UK’s primary sector has largely shifted to the peripheral territories, the colonies and dependencies. As environmental concerns have arisen regarding pollution and contamination of the land, sea, and air the old mines in the Home Islands are no longer profitable to operate. Instead of reinvesting in new mines in the Home Islands, mining companies are investing in new mines in more plentiful lodes in colonies such as Sarnia, New Corcyra, and New Atlantis.

Secondary Sector

In a similar fashion to the decline of the primary industries within the UK, the secondary sectors has also begun to shrink in the Home Islands and Juristan (never having gained a stronghold in the Indian Islands and remaining of some importance in Kingsland.) The remaining centers of manufacturing are to be found in the areas around Breningrad, Regal, Merskov, Archangel, Etar, Azaz, Caliz, and Hamm-on-Sea. All but the first lay upon the western islands, and all are nevertheless witnessing a decline in the importance of their manufacturing.

Tertiary Sector

With the decline of the secondary sector in the eastern islands, various communities shifted their economic focus to the development of the tertiary sectors of the economy. Of the most critical importance is Philadelphia, the primary financial capital of the UK. The city of Imperium hosts a great number of financial services as well, as do the cities of Breningrad, Portsmouth, and Artega. However, other cities provide important regional functions, including the cities of Queensbury, Port Hamptonshire, Westport, and numerous cities throughout the colonies.

Quaternary Sector

Lastly, the quaternary sector has begun to rise to new importance, again particularly in the wealthier eastern regions of the UK’s Home Islands, although to a certain degree also in the gateway cities of Juristan and Kingsland. Important centers are again the Golden Triange of Philadelphia, Breningrad, Portsmouth, and Artega. In Juristan the important city is that of Providence while Kingsland boasts the cities of Charlotte and Port Melbourne.

Natural Resources

Environment