Final answer:
Kama‘ehuakanaloa is expected to eventually become less active as it moves away from the Hawaii hotspot, while new islands could form to the southeast. Major Hawaiian volcanoes like Mauna Kea are now dormant but important for activities such as astronomy. The active hotspot means ongoing volcanic eruptions and the potential emergence of new islands in the Hawaiian chain.
Step-by-step explanation:
Based on what we have learned about plate tectonics and the Hawaiian hotspot, the volcano known as Kama‘ehuakanaloa, along with other Hawaiian volcanoes, will continue to evolve over time. As the Pacific Plate moves northwestward, Kama‘ehuakanaloa will likely become less active and eventually go dormant as it moves away from the stationary hot spot, much like what happened with the older islands in the chain, such as Kauai. Meanwhile, new volcanic islands could form southeast of the current Hawaiian Island chain, as the magma from the hot spot creates new volcanic material on the ocean floor.
Hawaii's biggest volcanoes have become iconic due to their massive size and cultural significance. For example, Mauna Kea is not only a dormant volcano but also a renowned location for astronomy, whereas Mount Kilauea is one of the most active volcanoes globally. The Hawaiian citizens are accustomed to living with volcanic hazards, such as lava flows, rather than explosive eruptions.
As the hotspot continues to be active, the same process that formed the Hawaiian Islands will lead to ongoing volcanic eruptions and the growth of the island chain, with new islands possibly emerging. This has implications for the region's geography and could pose different hazards to the natural environment and human activities in the future.