The first part of this article studies the collapses of point-vortices for the Euler equation in the plane and for surface quasi-geostrophic equations in the general setting of models. In these models the kernel of the Biot-Savart law is a power function of exponent . It is proved that, under a standard non-degeneracy hypothesis, the trajectories of the point-vortices have a H"older regularity up to, and including, the time of collapse. The H"older exponent obtained is and this exponent is proved to be optimal for all by exhibiting an example of a -vortex collapse. The same question is then addressed for the Euler point-vortex system in smooth bounded connected domains. It is proved that if a given point-vortex has an accumulation point in the interior of the domain as , then it converges towards this point and displays the same H"older continuity property. A partial result for point-vortices that collapse with the boundary is also established : we prove that their distance to the boundary is H"older regular.

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