![]() Each of the three different boundary types can create their own unique fault type, and the movements of the plates occur at the fault location. At convergent boundaries, the tectonic plates collide with one another while at divergent boundaries the plates split apart from one another. Transform boundaries are distinct from two other types of boundaries: divergent boundaries and convergent boundaries. The messages are constantly coming and seismologists are fast learning to read them.” - Reginald Daly “Earthquakes traveling through the interior of the globe are like so many messengers sent out to explore a new land. Though Wilson was initially skeptical of the theory of plate tectonics his work became instrumental in our current understanding of it and he was also the first person to advance the theory of volcanic hotspots. Transform boundaries were hypothesized/conceived of by John Tuzo Wilson, a Canadian geophysicist, in 1965. ![]() Let’s take a deeper, more detailed look at transform boundaries and discover how the two plates interact with one another, as well as how transform boundaries differ from other types of geological boundaries. While this is the basic definition of a transform boundary, there’s more to them than that. As these plates move past one another, the two plates interact and can create cracks or faults within the surrounding area. ![]() A transform boundary is a place where two of the Earth’s tectonic plates move past one another.
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