Later it was removed from the series as unlike zeolites, bavenite loses the water stored in its crystal lattice in a way higher temperature, between 210 and 320 °C.

It can also appear in radial aggregates, meaning it has a center from which crystals radiate without producing a stellar form.

However, Canille managed to solve its structure thanks to Berry, who suggested direct Be ⇌ Al with electroneutrality.

[4] Bavenite is usually associated with beryl, phenakite, bertrandite, quartz, epidote, stibnite, albite, orthoclase, titanite, clinozoisite and tremolite.

Bavenite can also occur in the Alps, where it was created as a product of the hydrothermal weathering of beryllyium-bearing minerals (mostly beryl) through metamorphism.

In Spain, very high-quality specimens, relevant on a global scale, have been found in miarolitic cavities in the granite of several quarries in Cadalso de los Vidrios (Madrid).

In the quarries of La Cabrera (Madrid), it appears as cottony-looking aggregates formed by capillary crystals.