Ekenta: Difference between revisions
mNo edit summary |
|||
| Line 2: | Line 2: | ||
== History == | == History == | ||
Ekenta has often been part of [[Ganuo]], with its importance to the country growing in recent centuries as the rapid spread and increased yields of [[Sugo|sugo]] have made the shorelines and shallow waters on its western edge more hospitable for large populations. In the current era, | Ekenta has often been part of [[Ganuo]], with its importance to the country growing in recent centuries as the rapid spread and increased yields of [[Sugo|sugo]] have made the shorelines and shallow waters on its western edge more hospitable for large populations. In the current era, the entire island is owned by Ganuo. | ||
== Geology == | == Geology == | ||
Ekenta entirely almost consists of continential rock with a few volcanic basalt intrusions, mainly in the northeast, and is moving westward with the [[Ganuoan Plate]] away from [[Amalthea]] at a slow pace of 3 millimeters per year. | Ekenta entirely almost consists of continential rock with a few volcanic basalt intrusions, mainly in the northeast, and is moving westward with the [[Ganuoan Plate]] away from [[Amalthea]] at a slow pace of 3 millimeters per year. | ||
Revision as of 14:20, 2 October 2020
Ekenta is the largest island in the world, and is one of the two main landmasses on the Ganuoan Plate. It has a large population supported by strong rains and fertile soil found in many small river valleys.
History
Ekenta has often been part of Ganuo, with its importance to the country growing in recent centuries as the rapid spread and increased yields of sugo have made the shorelines and shallow waters on its western edge more hospitable for large populations. In the current era, the entire island is owned by Ganuo.
Geology
Ekenta entirely almost consists of continential rock with a few volcanic basalt intrusions, mainly in the northeast, and is moving westward with the Ganuoan Plate away from Amalthea at a slow pace of 3 millimeters per year.