Publication Date

8-2020

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Technical Report: UTEP-CS-20-89

Published in International Mathematical Forum, 2020, Vol. 15, No. 6, pp. 277-281.

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.

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