Sceilg Mhichil is a steep, rocky glacial landform known as what?

Sceilg Mhichil, also known as Skellig Michael, is categorized as a crag. This term refers to a steep, rugged rock face or a prominent, rocky hill, typically formed through processes related to erosion and glaciation. The dramatic cliffs and rocky outcrops of Sceilg Mhichil are a testament to its formation and geological history, characterized by steep inclines that define the landscape.

In contrast, a cirque is a bowl-shaped depression carved by glacial activity, often found at the head of a valley, while a moraine is an accumulation of earth and rock that has been transported and deposited by a glacier. An esker is a long, winding ridge formed by sediment deposition in a glacial environment, often made up of sand and gravel. Each of these terms refers to specific landforms resulting from glacial and geological processes, but the defining characteristics of Sceilg Mhichil align most directly with the concept of a crag.