A sharp ridge separating cirques is known as a "horn" or "arete." It forms as glacial erosion carves out steep valleys on either side, leaving a narrow, rugged ridge between the two cirques. This topographical feature is often characterized by its jagged peaks and steep slopes, making it a prominent feature in alpine landscapes. Horns and aretes are common in mountainous areas where glaciers have significantly shaped the terrain.
Sharp narrow ridge separating two glacial troughs (U-shaped valleys), or corries.
These sharp ridges are called aretes and form when glacial erosion carves out valleys on either side of the ridge. As glaciers move down the valleys, they erode the rock on both sides, sharpening the ridge. Aretes are a common feature in glaciated regions like the Alps or Himalayas.
watershed
arete
These sharp ridges are called arêtes, which form where glaciers erode and carve away the rock on either side of the divide between two glaciers. Over time, the erosive action of the ice sculpts a sharp ridge between the glacial valleys. A classic example of these features can be found in mountainous regions such as the European Alps.
The answer is ARETE
ArêteA sharp, narrow mountain ridge or spur, produced by glaciation, is known as an Arête.range
A bony ridge separating two surfaces is called an interosseous crest, which serves as an attachment point for muscles or ligaments and provides structural support between bones. It helps maintain stability and alignment in the joint.
An arête is typically formed when two glaciers erode parallel U-shaped valleys. The arête is a thin, sharp ridge of rock that is separating the two valleys.
An arête is a thin ridge of rock that is left separating the two valleys.
To fill the gap of separating plates.
To fill the gap of separating plates.