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A blue horocycle in the Poincaré disk model and some red normals. The normals converge asymptotically to the upper central point.
Circles seen in a Apollonian gasket that are tangent to the external circle can be considered horocycles in a Poincare disk model
The order-3 apeirogonal tiling, {∞,3}, fills the hyperbolic plane with apeirogons whose vertices exist along horocyclic paths.

In hyperbolic geometry, a horocycle (Greek: ὅριον + κύκλος — border + circle) is a curve whose normal geodesics all converge asymptotically. (It is also called an oricycle or oricircle, and a limit circle.) It is the two-dimensional example of a horosphere (or orisphere).

A horocycle can also be described as the limit of the circles that share a tangent in a given point, as their radii go towards infinity. In ordinary euclidean geometry, such a "circle of infinite radius" would be a straight line, but in hyperbolic geometry it curves. From the convex side the horocycle is approximated by hypercycles whose distances go towards infinity.

In the Poincaré disk model of the hyperbolic plane, the horocycles are represented by circles tangent to the boundary circle. In the Poincaré half-plane model the horocycles are represented by circles tangent to the boundary line, and lines parallel to the boundary line. In the hyperboloid model they are represented by intersections of the hyperboloid with planes whose normal lies in the asymptotic cone.


If the metric is normalized to have Gaussian curvature −1, then the horocycle is a curve of geodesic curvature 1 at every point.

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