Compression (Pushing the Clay Together)What happens: If you push both sides of the clay inward, mimicking a convergent plate boundary, the clay may buckle, fold, or rise.Water Reaction: The water will be displaced and may ripple outward as the clay shifts, similar to how real water behaves during tectonic movement that creates undersea ridges or trenches.Tension (Pulling the Clay Apart)What happens: If you pull the clay apart, mimicking divergent boundaries, cracks or rifts might form.Water Reaction: Water will fill the gaps created by the tension, just like how water fills rift valleys in tectonic settings. There might also be small ripples as the clay separates.Shearing (Sliding the Clay Side by Side)What happens: If you move the clay sideways in opposite directions, mimicking transform boundaries, friction may cause uneven motion, leading to movements.Water Reaction: The water may ripple or splash slightly due to the sudden sideways motion, simulating the small disturbances that can occur during earthquakes along transform faults.