Zealandia, often referred to as a submerged continent, primarily lies beneath the ocean’s surface, with around 93% of it underwater and only a small portion visible above sea level as New Zealand. Many people wonder if Zealandia could rise above the ocean due to geological processes.
In theory, Zealandia could emerge more prominently if certain geological activities were to occur. These might include tectonic uplift from seismic activities or other geological shifts that raise portions of the crust above current sea levels. However, such events are unpredictable and typically occur over geological timescales, often taking thousands or even millions of years.
Additionally, the rise of land can be influenced by factors such as melting ice caps, changes in sea levels, and environmental conditions. Yet, while there are possibilities in the distant future, for all practical purposes today, Zealandia will remain largely submerged as it has been for millions of years.
In conclusion, while Zealandia could technically rise, it is unlikely to occur in any immediate time frame, and any significant geological changes would take ages to manifest.