Convergent boundaries form strong earthquakes, as well as volcanic mountains or islands, when the sinking oceanic plate melts. A single tectonic plate can have multiple types of plate boundaries with the other plates that surround it. As these plates move past one another, the two plates interact and can create cracks or faults within the surrounding area. This is known as a transform plate boundary. A transform boundary is a place where two of the Earth’s tectonic plates move past one another. Using the diagram of figures, select the names of the plate boundaries that match the figures going left to right. This movement is felt as an earthquake. A transform boundary (or conservative boundary) is where two of the tectonic plates slide alongside each other. This causes intense earthquakes, the formation of thin linear valleys, and split river beds. ... What causes magnetic stripes on the seafloor, such as those shown here? Transform boundary. But rather than sliding smoothly, the plates build up tension then release the tension with a burst of movement. Another large-scale feature is a hotspot, where a plate rides over a rising plume of hot mantle, creating a line of volcanoes on top of the plate. Sometimes Earth's magnetic field points north and sometimes it points south. When this happens, the scraping of the two plates causes earthquakes. Beside above, what are the effects of Transform boundaries? Earthquakes at Transform Plate Boundaries Discusses the large, shallow focus earthquakes at transform plate boundaries with particular emphasis on the San Andreas Fault Zone. When forces are parallel but moving in opposite directions, the stress is called shear. Plate Tectonics in New Zealand Linear valleys, small ponds, stream beds split in half, deep trenches, and scarps and ridges often mark the location of a transform boundary. Transform boundaries are where two of these plates are sliding alongside each other. A transform boundary is a fault zone with two plates that are horizontally sliding past each other. Transform plate boundaries are where plates slide laterally past one another, producing shallow earthquakes but little or no volcanic activity. Shear stress is the most common stress at transform plate boundaries. A transform boundary (or conservative boundary) is where two of the tectonic plates slide alongside each other. As the plates rub against each other, huge stresses can cause portions of the rock to break, resulting in earthquakes. A well-known transform plate boundary is the San Andreas Fault, which is responsible for many of California’s earthquakes. Transform boundaries represent the borders found in the fractured pieces of the Earth’s crust where one tectonic plate slides past another to create an earthquake fault zone. A transform plate boundary occurs when two plates slide past each other, horizontally. When this happens, the scraping of the two plates causes earthquakes. 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