Aretes
Unwarped mountains typically have high peaks with sharp ridges.
Mountains have several features. They have steep sides and sharp ridges and peaks. They are rocky and barren, and usually have snow on them.
The sharp crack you hear from thunder when it is close it the electricity in the air.
Obsidian is a natural volcanic glass with potentially sharp fracture edges.
Aretes
Sharp narrow ridge separating two glacial troughs (U-shaped valleys), or corries.
terminal moraines--------------------------------------------------------------------------------------------------------They can be:Cirques, bowl-shaped depressions where glacial ice cuts back into the mountain walls.Horns, sharp, pyramid-like peaks that form when three or more alpine glaciers carve a mountain.Arête, a jagged ridges that form between two or more cirques that cut into the same mountain.Also U-shaped valleys and Hanging Valleys.
Many topographical features may be the result of glaciers. Lakes, sharp ridges on mountains, and glacial striations are some examples of these.
They are tall and they have sharp peaks and ridges.
Glacial Ice - APEX 2022
An arête is a thin ridge of rock which is formed when two glaciers erode parallel U-shaped valleys. The arête is a thin ridge of rock that is left separating the two valleys Arêtes can also form when two glacial cirques erode head wards towards one another, although frequently this results in a saddle-shaped pass, called a col. The edge is then sharpened by freeze-thaw weathering. Where three or more cirques meet, a pyramidal peak is created. - (a famous example is the 'Matterhorn'). Form the above it must be clear that arêtes are landforms found in mountainous terrains that have been subject to glaciation. They are therefore very common in the Alps.
Unwarped mountains typically have high peaks with sharp ridges.
Glacial horn
young
No, instead have jaggered ridges that are serrated and sharp on their upper and lower jaws.
Glacial horn