The iron-enriched basalt (IEB) waste form, developed at the Idaho National Engineering Laboratory a decade ago, was modified by adding sufficient TiO 2 and ZrO 2 to develop zirconolite (ZrCaTi 2 O 7 ) crystals in addition to those crystals that normally form in a cooling basalt. Zirconolite is an extremely leach-resistant mineral with a strong affinity for actinides. Zirconolite crystals containing uranium and thorium that have endured more than 2 billion years of natural processes have been found. On this basis, zirconolite is considered an ideal host crystal for transuranic elements in wastes.Zirconolite crystals were developed in laboratory melts of IEB which contained 5 wt % each of TiO 2 and ZrO 2 and were slow-cooled in the 1200-1000C range. Actinide surrogates were incorporated into zirconolite rather than precipitated in residual glass. Zirconolite crystals should stabilize and immobilize dilute transuranics (TRUs) found in heterogeneous low-level wastes as effectively as they do in the Synroc used for high-level wastes. Synroc requires hot-pressing equipment but zirconoiite may be precipitated from a cooling basaltic melt.