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Imagine a ball on the error
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surface with
velocity v.
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It
starts off by following the
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gradient,
but once it has
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velocity,
it no longer does
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steepest
descent.
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It
damps oscillations by
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combining
gradients with
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opposite
signs.
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It
builds up speed in
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directions
with a gentle but
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consistent
gradient.
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On an
inclined plane it
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reaches
a terminal velocity.
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