1. Anticlinal structure which plunges in all directions.
2. (volcanic dome, tholoid) A mound of viscous lava, usually rhyolite in composition, which has grown and built up over a vent. The mound of solid lava is covered by coarse, angular blocks which form by chilling and brecciation of the growing dome’s surface. The blocks accumulate around the growing dome to produce a scree slope of crumble breccia. Domes can grow by repeated injection of magma into the dome body (endogenous dome) or by repeated eruption of small volumes of magma from the surface of the dome (exogenous dome).
3. (salt dome) A circular or elongate plug, 1–2 km in diameter but extending downwards for many kilometres, formed by the upward movement of buoyant and less dense evaporitic material (commonly halite) into denser overlying rocks. The diapiric movement (see diapir) may be initiated by tectonic thickening.
4. A special form of crystal development characterized by two roof-like faces symmetrical about a plane of symmetry. The faces are repeated once only about an axis of symmetry.