Читать книгу The Rheology Handbook - Thomas Mezger - Страница 97

In the Ice Age (which, for example, came to an end in Northern Germany around 14,000 years ago), the shear force of glaciers moved loose layers of soil masses and pieces of solid rock, e. g. boulders, weighing several tons. The so-called “solifluction” of the partially thawed permafrost soil resulted in plastic deformation of the landscape.