This study considers the problem of simultaneous propagation of multiple closely spaced hydraulic fractures in homogeneous rocks, under the limited entry condition that ensures uniform flux distribution between the fractures. In particular, the sensitivity of the results to fracture propagation regimes is investigated. There are four primary regimes of hydraulic fracture propagation that are related to interactions between two dissipation mechanisms, related to fluid viscosity and rock toughness, and a fluid storage mechanism (fracturing fluid leak-off), which can occur either inside the fracture or inside the formation. It is shown that the fracture behavior varies dramatically with respect to the fracture propagation regime. In particular, fractures that propagate in the viscosity dominated regime exhibit weak stress shadow interactions, grow predominantly radially, and develop nearly identical fracture geometries. In contrast, fractures that propagate in the toughness regime exhibit strong stress shadow interactions, grow as individual segments avoiding others that are propagating simultaneously, and develop geometrical structures resembling petals in a flower, where the overall geometry is radially uniform, but the individual fractures form non-overlapping segments of the total surface area. Results are presented for the case of Newtonian fluids with and without stress anisotropy, power-law fluids, and consider the case of fracture toughness anisotropy. Finally, the effect of fracture spacing on fracture geometry is investigated for different fracture regimes.