When rocks are stressed, electronic charge carriers are activated which are defect electrons in the oxygen anion sublattice, O– in a matrix of O2–, known as positive holes. They have properties such as the ability to flow out of the stressed volume and spread into the surrounding unstressed rocks. The wave function associated with these charge carriers is highly delocalized, meaning that the spin density is distributed over hundreds of O2– neighbors. We conducted three sets of experiments to test the prediction that a specific quantum mechanical effect, the delocalization of the electronic wave functions associated with oxygen anions in the 1– valence state, has a measurable effect on fundamental properties of rocks. Normally the O– exist in the structure of rock‐forming minerals in the form of tightly bonded O–pairs, called peroxy defects. We set out to measure (i) the "softening" of rocks in which peroxy defects are activated, (ii) our capability to manipulate the distribution of the electronic charge carriers, called positive holes, that arise from the delocalized O– states, and (iii) the volume expansion predicted to accompany the break‐up of peroxy bonds and delocalization of the wave functions. We successfully demonstrated (i) and (ii), showing a "softening" of the rocks on the order of 10‐15%. We did not yet successfully demonstrate the volume increase effect. The mechanical properties of materials, including rocks, are influenced by many factors. Most prominent among those factors are defects on different scales. They range from point defects on the scale of atoms to linear defects within grains such as dislocations, 2‐dimensional defects along grain boundaries, and larger defects such as microfractures. The many forms of imperfections can be summed up as "damage". Damage is usually accumulative but can often be "repaired" through various annealing processes. In this project we have pursued a particular form of imperfections due to point defects in the oxygen sublattice of minerals, whereby oxygen anions have changed their valence from the usual 2– state to 1–. Under certain conditions point defects that consist of pairs of O– become activated. As the O––O– bond breaks up, there is strong evidence that the wave functions associated with the O– become delocalized over many neighboring oxygen anion position. As we show in this Report this quantum mechanical process of delocalization has a measurable effect on the mechanical properties of rocks: it makes rocks mechanically weaker and softer.