The twice - daily lurches and icequakes are thought to arise from
ocean tides lifting the ice so that it can slide over the sticky spot, relieving mechanical strain that has built up on the glacier since the last high tide.
The ice stretches over these sticking points twice per day as the
tide lifts up and sets down the Ross Ice Shelf, a 1,100 - foot - thick slab of ice the size of Spain that hangs over the
ocean several hundred miles away.