The Mean Value Theorem for Several Variables states that if a function is continuous on a closed and bounded region and differentiable on the interior of that region, then there exists at least one point within the region where the gradient of the function is parallel to the vector connecting the endpoints of a line segment joining two points in that region. This theorem extends the classic Mean Value Theorem from single-variable calculus to functions of multiple variables, emphasizing how changes in multiple dimensions relate to overall change in a function.
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