A horizontal lift of from is a curve in projecting to , starting at , and tangent to the horizontal distribution of the connection. In a local frame write . Horizontality is the linear ordinary differential equation
whose initial-value theorem gives local existence and uniqueness; successive trivializations continue the lift.
A geodesic satisfies , and
for the geodesic with initial velocity . Since , the inverse function theorem makes a diffeomorphism near zero; its inverse gives normal coordinates. A geodesic sphere is inside such a normal neighborhood.
The Gauss lemma states
For the variation , let . The coordinate vector fields commute, so metric compatibility and constant geodesic speed give
Since , evaluation at proves the formula. In particular radial and spherical directions are orthogonal.
Solved by gpt-5.6-sol high.
Choose a normal ball on which is a diffeomorphism, and take smaller than half its radius. For , is a geodesic of length . If a competing curve remains in the normal ball, write it in polar form. The Gauss lemma makes radial and angular velocities orthogonal, so its speed is at least the absolute radial speed and its length is at least . A curve leaving the larger normal ball already accumulates more than in radial variation. Thus the radial geodesic minimizes length.
At , both and the geodesic sphere are hypersurfaces. If their tangent hyperplanes were distinct, they would be transverse. The transverse intersection theorem would then make a submanifold of dimension
For this has positive dimension near , contradicting that the intersection is the singleton . Therefore .
The conclusion fails in dimension two because a transverse intersection is zero-dimensional and may be isolated. In the Euclidean plane, let be the unit circle, , and let . Then , but is horizontal whereas is vertical.
Solved by gpt-5.6-sol high.

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