1. Subglacial Eruption: Lava erupts under a glacier or ice sheet.
2. Rapid Cooling: The lava comes into contact with ice and meltwater, cooling quickly and shattering into small fragments.
3. Accumulation: These glassy fragments build up around the vent and are eventually compacted into layers of tuff.
4. Erosion and Exposure: After the glacier melts, the hardened layers are exposed, forming steep ridges, cones, or flat-topped mountains called table mountains (e.g., Herdubreid).

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