Formation of { 110) and {211} type facets in rare-earth aluminium garnet crystals grown along different crystallographic directions is analyzed and it is shown that D/2R pmameter (where D is the crystal diameter and R is the curvature radius of spherical growth interface) may be used t o characterize the number of originating facets and their configuration in crystals. m e B m rpaHaTax, BbIpaLueaeam BRom paanusmax KpucTaJmorpa@usecwix HanpaB-neHEiP.OnHcaum mCna o6paay1o~xc~z rpaHeB u ux KoH@IIIypamm B KpUcTannax secKoP nosepxHocTn paagena $as).A~a r n a q y e~c~l 06pa30BaHHe rpaHeP THna (110) €I (211) B peflK03eMeJIbHO-anioMU-HCIIOJIbaOBaH IIapaMeTp 012 R (me D-JItraMeTp KpUCTaJIna, R-paunyc KpHBll3HH C$epU-