Final answer:
The statement that ocean-ocean collision forms large Himalayan-scale mountain belts is false. The Himalayas formed from the collision of two continental plates, not oceanic plates. This process involves the deformation of the Earth's crust due to enormous pressure and force resulting in the creation of the mountain belt and associated suture zones.
Step-by-step explanation:
It is false to say that ocean-ocean collision tends to form large Himalayan-scale mountain belts. The formation of mountain ranges like the Himalayas typically involves the collision of two continental plates rather than oceanic plates. This major geologic process is known as continent-continent convergence, where the immense pressure and force exerted by the converging continental masses result in the earth buckling and folding. The resulting deformation pushes rocks upward as well as dragging some of them deep below the surface, thus creating high elevation regions like the Himalayas or the Alps.
The formation of the Himalayas specifically can be traced back to the convergence of the Indian tectonic plate pushing northward into the Eurasian plate, creating the mountain range and the high-altitude Tibetan Plateau. Besides mountain formation, these areas can exhibit associated geologic features such as suture zones where ophiolites are present, indicating the past presence of an ocean basin between the two converging continents.