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Examples
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The layer below is a partially fluid solid named the athenosphere, which ends at a depth of about 200 km.
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In some places, called subduction zones, one plate sinks beneath another plate and returns to the molten regions of the athenosphere.
Conservapedia - Recent changes [en] Batterylow 2009
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In some places, called subduction zones, one plate sinks beneath another plate and returns to the molten regions of the athenosphere.
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The layer below is a partially fluid solid named the athenosphere, which ends at a depth of about 200 km.
-
The layer below is a partially fluid solid named the athenosphere, which ends at a depth of about 200 km.
-
In some places, called subduction zones, one plate sinks beneath another plate and returns to the molten regions of the athenosphere.
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The layer below is a partially fluid solid named the athenosphere, which ends at a depth of about 200 km.
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