Beryl is shaped like a six-sided prism. Beryl is part of the
O isometric crystal system
monoclinic crystal system
O hexagonal crystal system
O triclinic crystal system

sediment layers stop spreading when they reach a barrier or they run out of sedimentary material. lateral spreading is the movement of gently to steeply sloping, saturated soil deposits caused by earthquake-induced liquefaction. i hope this . : )

i believe this is