Final answer:
Water trapped in glaciers is an exception to water moving slowly. Underground aquifers and deep ocean currents represent examples of slow water movement.
Explanation:
Water trapped in glaciers would NOT be an example of water moving slowly. Glaciers flow more slowly at the bottom compared to the top due to less movement in the lower part. On the other hand, water in underground aquifers and deep ocean currents are examples of water moving slowly, with groundwater flowing at velocities of a few millimeters to centimeters per year and deep ocean currents moving at rates of kilometers per month.
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