Why are regions where convection currents diverge more suitable for building geothermal power stations?

Regions where convection currents diverge typically have thinner crust, making it easier for magma to rise closer to the surface and produce geothermal energy. This allows for easier access to hot water or steam reservoirs for generating electricity in geothermal power stations. Additionally, the heat transfer from the mantle to the crust is more efficient in these regions, making them more suitable for geothermal energy production.