Basal sliding
temp at base is above freezing=warm base glacier=moves downslope
internal deformation
ice crystals realign themselves into parallel layers and slide past eachother
striations
scratch marks caused by abrasion
chatter marks
discontinuous scratch marks caused by abrasion
roche motonnee
rock that has been plucked and made smooth by a glacier
eratics
huge boulders deposited on different bedrock
glacial budget
balance between accumulation and ablation. determines whether glacier is advancing or retreating. NOT THE VOLUME OF A GLACIER