Publication Date
8-2020
Abstract
It has been empirically observed that the average shape of natural fragmentation results -- such as natural rock fragments -- is a distorted cube (known as cuboid). Recently, a complex explanation was provides for this empirical fact. In this paper, we propose a simple geometry-based physical explanation for the ubiquity of cuboid fragments.
Comments
Technical Report: UTEP-CS-20-89
Published in International Mathematical Forum, 2020, Vol. 15, No. 6, pp. 277-281.