Earth's Interior Cools Unevenly Across Hemispheres

Scientists find Pacific Ocean side cools faster than continental side, affecting tectonics and volcanism.

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Earth's Interior Cools Unevenly Across Hemispheres

Scientists find Pacific Ocean side cools faster than continental side, affecting tectonics and volcanism.

In brief

Scientists find Pacific Ocean side cools faster than continental side, affecting tectonics and volcanism. Earth's interior cools unevenly, with the Pacific Ocean hemisphere losing heat faster than continents, influencing long-term geological activity. Originally reported by Moneycontrol.

New Research Reveals

Scientists report Earth's interior cools unevenly across hemispheres, with the Pacific Ocean side losing heat faster.

Pacific Ocean Hemisphere

The Pacific Ocean hemisphere cools more quickly than continents, influencing tectonics and volcanic activity over millions of years.

Oceanic Crust Thinner

Oceanic Crust Thinner

Oceanic crust is thinner, allowing more heat to escape into the oceans, while continental crust is thicker and slows heat loss.

Scientists' Method

Scientists discovered the cooling pattern using mantle temperature data and geological modeling to understand mantle circulation.

Long-Term Effects

This uneven cooling shapes mantle circulation and plate tectonic behavior over geological timescales.

The main idea

Earth's interior cools unevenly, with the Pacific Ocean hemisphere losing heat faster than continents, influencing long-term geological activity.

Read the original on Moneycontrol

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