A simplified model of plane isothermal steady ice flow in the land-based pa
rt, the shelf and the ice-sheet-ice-shelf transition zone of a glacier whic
h interacts with the sea is constructed using Glen's flow law and perturbat
ion methods. Boundary conditions on the joining line are obtained for the l
and-based part of the glacier. The dynamics of the ice-divide domain of the
glacier is analysed for the case of axially symmetric, steady, isothermal
ice flow. (C) 2001 Elsevier Science Ltd, All rights reserved.