Figure 1From: Linear stability of plane Poiseuille flow in an infinite elastic medium and volcanic tremorsIllustration of our model. A plane fluid layer of a constant thickness, 2a, is sandwiched between two semi-infinite elastically deformable bodies. The fluid inside flows in one direction. Deformation of the elastic surrounding and the fluid motion can be generally represented by the superposition of symmetric and antisymmetric solutions.Back to article page