What is Far from plate boundaries still active?

Regions far from tectonic plate boundaries can still exhibit geological activity due to processes such as mantle plumes and intraplate stress. Hotspots, like those that form the Hawaiian Islands, arise from localized areas of high heat flow in the Earth's mantle, leading to volcanic activity. Additionally, intraplate earthquakes can occur as a result of ancient faults reactivating or due to stresses transmitted through the crust. These phenomena demonstrate that geological processes can remain active even in the absence of direct plate boundary interactions.