What is a characteristic feature of valley glaciers as compared to continental glaciers?

Valley glaciers are characterized by their ability to carve sharp peaks and rugged features in mountainous areas. As they move down through valleys, typically formed by previous glaciation, they shape the landscape by eroding the surrounding rock, resulting in distinctive formations such as ridges and sharp peaks known as horn peaks. This sharp, jagged topography is one of the most recognizable features of valley glaciers.

In contrast, continental glaciers, which are much larger and cover vast land areas, tend to create more subdued and rounded landforms due to their sheer size and the way they flow over the landscape. These differences in scale and the effects on topography highlight the unique characteristic of valley glaciers in creating sharp, pointed mountain formations.