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Statement 1: The flow of deep layer current is opposite to the surface layer current in the oceans Statement 2: The deeper water is deflected by the Coriolis EffectStatement 3: Deeper layers of water move more slowly than the surface layers

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Statement 1: The flow of deep layer current is opposite to the surface layer current in the oceans <br>Statement 2: The deeper water is deflected by the Coriolis Effect<br>Statement 3: Deeper layers of water move more slowly than the surface layers






 
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