In the photo above, you can see where one plate (eastern), is being forced underneath the other plate, which is also causing a slight rise in that plate.
Here at the main ridge located on my plate, the spreading is roughly 78 millimeters per year. Based on the information above, and also below, you can see that the spreading is
Looking at the above photo, you can see a range of earthquake sizes, although the depth of them are around the same area, which i between 0 and 70 km deep into the ocean, although there was one that was between 70 to 150 km deep, but was a low magnitude. With these earthquakes being so shallow, and in an area where the seafloor is young, it is thought for this to be forced spreading.
One thing that is specific to convergent boundaries are the chances to create volcanoes. As you can see in this picture, the way the volcanoes have come up works a pattern with the shape of the convergent boundary. There are a few other volcanoes located near the southern portion of the plate, but the most prominent ones are located near the ridge, along side the convergent boundary.