Tectonic Plates of Rathnir

Rathnir consists of 30 tectonic plates. This is a massive amount of tectonic plates compared to other planets. This huge number of tectonic plates have let to Rathnir having some strange and dangerous but never the less beautiful landscape, with massive mountains and biomes, making the world of Rathnir truly unique in the eyes of many.

Pre-Historic Data
Rathnir consists of thirty tectonic plates as previously mentioned. These tectonic plates have been shifting for billions of years, forming the beautiful landscape that Rathnir consists of today. Many of these plates vary in size, this was due to the splitting of some of them, also leading to a form of underground 'bordergore'. This has caused numerous volcanic eruptions and the formation of huge areas of tightly packed large mountains. It has caused tons of earthquakes, and the amount of tectonic plates have generally been an issue for the early humans, but as Rathnir now finds itself within the prolonged Modern Period in its territorial evolution the people of Rathnir has not seen much to these previously common earthquakes and volcanic eruptions.

The natural disasters that happen today, that is directly caused by tectonic movements are only small scale, and the people of the regions where its most common has grown accustomed to it. The large scale effects that the tectonic plates has had on Rathnir should not be overshadowed in anyway shape or form. As it shaped and formed Rathnir.

The Plates

 * Hafinia Major: Hafinia Major is a large plate that stretches from central Ummarnu to South Central Syltör. It is one of the main reasons that the Phagosian sea was developed in the way it was.
 * Hafinia Minor: Hafinia Minor is a break-away plate from Hafinia Major. It covers a majority of the mesa and is one of the sole reasons why the mesa looks as it does, forming massive mountains through large scale earthquakes early in it's history. This also caused it to break away from Hafinia Major
 * Auroran Plate: The Auroran Plate is quite small. It is one of the key elements that formed the mountainous areas around Fornost.