Produced by: Manoj Kumar
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Deep beneath the Indian subcontinent, tectonic shifts are slowly reshaping its foundation.
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A phenomenon called “delamination” is causing parts of the Indian tectonic plate to fragment.
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Seismic data from southern Tibet revealed cracks in the Indian plate at 100-km depths.
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Northeastern India near Bhutan shows notable tectonic movement along the subduction zone.
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These processes occur over millions of years, making them invisible on the Earth’s surface.
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The findings challenge prior assumptions about how continental plates collide and deform.
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The tectonic activity may explain the ongoing rise of the Himalayan mountain range.
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Understanding these shifts can improve predictions of seismic activity in the region.
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Despite the buzz, India is not physically breaking apart into separate landmasses.
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This natural process highlights the Earth’s slow, intricate tectonic evolution.
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