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We show that the recipe for computing the expansions 𝜃ℓ and 𝜃n of outgoing and ingoing null geodesics normal to a surface admits a covariance group with nonconstant scalar κ(x), corresponding to the mapping 𝜃ℓ→κ𝜃ℓ, 𝜃n→κ−1𝜃n. Under this mapping, the product 𝜃ℓ𝜃n is invariant, and thus the marginal surface computed from the vanishing of 𝜃ℓ, which is used to define the apparent horizon, is invariant. This covariance group naturally appears in comparing the expansions computed with different choices of coordinate system.