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An unstressed glass is optically isotropic, so it does not split incident light into differently phased in-plane components; it remains dark between crossed polars. A natural explanation of the colored regions after heating is devitrification: anisotropic crystallites have nucleated in the glass. Edges and surfaces provide heterogeneous nucleation sites, making their greater concentration there plausible.

Each approximately uniform crystallite can give a nearly uniform interference colour. Regions with similar thickness and effective birefringence have similar retardation and therefore similar spectral colour, while differing azimuths multiply the intensity by ${\sin }^2(2\alpha )$ and change brightness. Identical hue does not prove identical three-dimensional crystallographic orientation.

Stress-induced birefringence is a possible alternative in a heat-treated glass. The observations alone do not uniquely prove crystallinity; rotating-stage extinction, morphology or diffraction could distinguish the explanations. The crystallite interpretation is the straightforward phase-transformation explanation, without inventing a composition or heat-treatment schedule.

glass accommodates a chemically diverse waste inventory without requiring every constituent to fit one specific crystal site. A borosilicate network can incorporate many constituents while producing a dense monolithic waste form. An established melt-and-pour approach permits remote processing and a reproducible package geometry; suitable formulations combine useful waste loading with low aqueous release rates. The absence of crystalline grain boundaries also removes one possible preferential path, although cracks or other heterogeneity can still occur.

The flexibility has limits. Some constituents have limited solubility or can separate into undesired phases, and increasing waste loading can impair processability or durability. Melting can release volatile constituents that require capture and generate secondary wastes. Cooling stresses may crack the product and enlarge its accessible surface; devitrification or phase separation can change chemical durability. Heat and radiation can change density, bonding or microstructure even though the starting glass is already noncrystalline.

Most importantly, glass is an immobilisation medium, not an assertion of zero reaction with water. Durability depends on composition, temperature, solution chemistry and the evolution of alteration products. A low initial leach rate does not alone demonstrate long-term behaviour, and an amorphous structure does not make the material inert. Container and repository barriers complement rather than duplicate the glass's role. A suitable choice therefore balances processing, composition tolerance, radiation response and aqueous durability instead of maximising only one property.