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An exterior misaligned planet exerts an orbit-averaged secular torque on each belt orbit. In the hierarchical limit $a_d\ll a$, its leading quadrupole approximation drives nodal precession about the planet's orbital angular-momentum axis at a rate of orderup to a coefficient of order unity. Because this rate varies across a radially extended belt, differential nodal precession winds an initially flat belt into a warp and eventually a vertically thick, phase-mixed structure. Collisions can damp the free inclinations and make material approach a forced or Laplace plane; at sufficiently large mutual inclination, coupled eccentricity-inclination evolution such as the Kozai–Lidov mechanism may also become important.