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The fragmentation of the magmatic foam is violent and causes the bubble clasts to collide against the conduit wall and with each other resulting in finely dispersed fragments (Cashman et al. According to Hallet, large rocks, or clasts, commonly freeze up through the soil. In hand specimen, leached, oxidized, and sheared San Diego breccia consists of cobble to boulder sized, sub-rounded aphanite clasts in a dark gray, amorphous silica matrix. |
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