The announcement of Zealandia as Earth’s eighth continent six years ago captivated the world’s attention. This vast landmass, submerged beneath the Pacific Ocean, challenges our understanding of Earth’s geological history and offers a fascinating glimpse into the dynamic forces that shape our planet.
A Continent Lost and Found
Zealandia’s existence remained hidden for centuries, concealed beneath kilometres of water. Its discovery involved piecing together geological and bathymetric data, revealing a continuous stretch of continental crust distinct from the surrounding oceanic crust.
Size and Location
Zealandia is an immense landmass, estimated to cover a staggering 4.9 million square kilometres – larger than the Indian subcontinent! It stretches an impressive 4,300 kilometres, lying southeast of Australia.
A Submerged Giant
While Zealandia qualifies as a continent, it is predominantly submerged beneath the Pacific Ocean. The majority of its landmass lies 1–2 kilometres below the water’s surface, making exploration a challenging endeavour.
A Journey Through Time
Zealandia’s story begins approximately 83 million years ago when it broke away from the supercontinent Gondwana. This separation marked the beginning of Zealandia’s long journey to its current location.
Unlocking Zealandia’s Secrets
Understanding Zealandia’s geological makeup is crucial to deciphering its history and its role in Earth’s evolution. The continent boasts a thick and diverse crust, providing valuable insights into the planet’s dynamic processes.
Exploration Challenges
Exploring Zealandia presents significant logistical hurdles. Its underwater location necessitates specialised equipment and techniques. Moreover, accessing the critical layers for study requires drilling 500 metres beneath the seabed, adding further complexity to research efforts.
A Key Piece of Earth’s Puzzle
Zealandia holds immense scientific value, offering a unique window into the movement of landmasses throughout Earth’s history. Studying this submerged continent can shed light on plate tectonics, continental drift, and the formation of ocean basins, enhancing our understanding of our planet’s evolution.
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