In this paper, we study a nonlocal degenerate parabolic equation of order α+2 for α∈(0,2). The equation is a generalization of the one arising in the modeling of hydraulic fractures studied by Imbert and Mellet in 2011. Using the same approach, we prove the existence of solutions for this equation for 0<α<2 and for nonnegative initial data satisfying appropriate assumptions. The main difference is the compactness results due to different Sobolev embeddings. Furthermore, for α>1, we construct a nonnegative solution for nonnegative initial data under weaker assumptions.