Around 180 AD, New Zealand experienced a catastrophic volcanic event known as the Hatepe eruption or Taupo eruption. This eruption holds significance as the world’s most massive volcanic eruption to occur within the past 5,000 years. The eruption spewed an estimated 100 cubic kilometers (24 cubic miles) of ash, rock, and pumice into the atmosphere, causing widespread devastation in the surrounding region and exerting a substantial influence on global climate patterns.
The far-reaching effects of the Hatepe eruption were remarkable. Ash particles from the eruption have been discovered as far away as Antarctica, highlighting the colossal scale of its impact. Furthermore, the eruption is believed to have induced a volcanic winter, characterized by a prolonged period of cooler temperatures and reduced sunlight, which endured for several years. This event is recognized as the most significant eruption ever recorded from a New Zealand volcano and ranks among the most violent eruptions witnessed on Earth within the past 5,000 years. Classified as a Volcanic Explosivity Index (VEI) 7 eruption, it expelled approximately 120 cubic kilometers of material, leaving an indelible mark on the planet’s geological history.
