The velocity of unstable large ice masses from hanging glaciers increases as a power-law function of time prior to failure. This characteristic acceleration presents a finite-time singularity at the theoretical time of failure and can be used to forecast the time of glacier collapse. However. the non-linearity of the power-law function makes the prediction difficult. https://countryscenesaddleryandpetsuppliers.shop/product-category/english-saddles/