subduction zones
Subduction zones are regions where one tectonic plate moves under another and sinks into the Earth's mantle. This process occurs at converging boundaries, often where an oceanic plate meets a continental plate. As the sinking plate descends, it can cause geological activity such as earthquakes and volcanic eruptions. Subduction zones are crucial for recycling Earth's materials and play a significant role in shaping landscapes. They also create deep ocean trenches and mountain ranges, highlighting the dynamic nature of our planet's surface.
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Subduction zones are areas where one tectonic plate sinks beneath another into the Earth's mantle. This process occurs at convergent boundaries, often leading to the formation of deep ocean trenches and volcanic arcs. As the subducting plate descends, it can cause intense geological activity, including earthquakes and volcanic eruptions. These zones are crucial to the Earth’s geology, recycling materials and shaping landscapes over millions of years. Regions such as the Pacific Ring of Fire are well-known for their subduction zones, showcasing the dynamic nature of our planet.