The Ring of Fire is a horseshoe-shaped area in the Pacific Ocean known for its high seismic and volcanic activity.
Earthquakes and volcanoes are common in this region due to the presence of multiple tectonic plates.
Tectonic plates are large pieces of the Earth’s crust that float on the semi-fluid mantle below, causing them to move and collide.
When these plates move against each other, they create tension that can result in earthquakes.
The Ring of Fire is home to 75% of the world’s active volcanoes, making it one of the most geologically active regions on Earth.
Volcanoes in this area can erupt explosively, spewing ash, lava, and gases into the air.
In addition to earthquakes and volcanoes, the Ring of Fire is also prone to tsunamis, which are large ocean waves triggered by underwater earthquakes.
Despite the risks associated with living in the Ring of Fire, many communities in this area have adapted to the constant threat of natural disasters.
Scientists continue to study the Ring of Fire in order to better understand and mitigate the potential impacts of earthquakes and volcanic eruptions in the region.