Alkaline rocks having the alkalis over Al ratio in excess of 1, and containing a suite of complex alkali titano-, niobo- and zirconosilicates (e.g. eudialyte).
Vertical columnar jointing forms as a result of cooling, particularly of lava. The joint systems associated with cooling are typically polygonal in nature due to the cooling introducing stresses that are isotropic in the plane of the layer. A good example of columnar jointing can be see at Giant's Causeway in Ireland.
An eruption occurring through long, open crack in the ground. They commonly form flood basalts which are repeated flows on low viscosity lava and can cover large areas.
Incompatible relative to mantle minerals; those elements with large ionic radii such as Nb, Zr, U, Th, K, Na, Li, Be, REE, that preferentially go into the melt rather than remain in residual minerals.