What generally characterizes a convergent boundary between two continental plates?

A convergent boundary between two continental plates is primarily characterized by the formation of large mountain ranges. When two continental plates collide, the crust experiences intense pressure and is forced upward, resulting in significant geological features such as mountain ranges. This process is driven by the movement and interaction of tectonic plates, and it leads to the accumulation of sediment and the folding and faulting of existing rock layers.

The creation of large mountain ranges reflects the immense forces at work as the plates push against each other. Notable examples of mountain ranges formed by this process include the Himalayas, which were created by the collision of the Indian Plate and the Eurasian Plate.

While other geological features can arise from tectonic activities, such as ocean basins or rift valleys, they are not typically associated with the direct collision of two continental plates. Instead, those features generally occur in different tectonic settings.