We may understand this intellectually but not intuitively. Because planetary change takes place so slowly, we don't notice it and tend to think it's not happening. Nevertheless, most of the processes that have defined Earth's history, such as plate tectonics, seem to function as they always have. The lithospheric plates, for instance, continue to move at roughly the same rate they have over the last three billion years. At just centimeters per year, this movement is difficult to perceive, but it's nonetheless significant.
According to plate tectonics, the continental plates have in the past, and will again, come together to form supercontinents. For example, about 225 million years ago, all of the extant continents joined together to form a single landmass known as Pangaea, fitting together like the pieces of an enormous jigsaw puzzle. This supercontinent, one of many that have formed over the course of Earth's history, took tens of millions of years to come together through multiple collisions and tens of millions of more years to break apart through a process called rifting. Geologists believe that unitary supercontinents form about every 250 million years, which is roughly the same amount of time that it takes our solar system to complete a single orbit around the center of the galaxy. Some geologists have suspected a connection, but none has yet been demonstrated.
Could some past cataclysmic events on this planet have resulted from Earth's passing through a particularly dangerous region of space? That is certainly a possibility, and if so, such events will likely happen again-but not quickly. (The Bedside Baccalaureate, edited by David Rubel)