United States

The continental crust of the United States has hotter areas with high heat flow and colder areas with low heat flow.
The Appalachian Mountains and Sierras are thickened continental crust with low heat flow. In essence, tectonic compression that made the mountains and their mountain roots thickened the insulating blanket of continental crust, thus reducing surface heat flow. Florida is underlain by very old, cold lithosphere that was once part of Africa, and thus also has low heat flow.