The most accurate interpretation of how changes in the rate of plate tectonics might impact the geological features of a coastal region over millions of years is:
1) Increased plate tectonic activity would lead to more frequent volcanic eruptions and the formation of new landmasses, altering the coastal landscape.
Increased plate tectonic activity, such as a higher rate of subduction or the emergence of new mid-ocean ridges, can lead to volcanic activity and the creation of new landforms. This can significantly reshape coastal regions, create new islands, and alter shorelines through processes like uplift and subsidence.
Conversely, a decrease in plate tectonic activity can also affect coastal regions by slowing down geological processes that create new land or modify existing landforms. It's important to note that while erosion might occur over time, it is generally a slower process influenced by other factors rather than an immediate response to decreased tectonic activity.
The other options (2, 3, and 4) downplay the connections between tectonic activity and coastal geology, whereas option 1 accurately reflects the dynamic relationship between tectonic processes and coastal features.