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The basalt has a porosity of between 8 and 9 percent. Most of the basalt units are migmatitic with a layered fabric that reflects an original type of igneous activity. In some places, additional basalts appear as dark felsic rocks (Figure 3). It is obvious that the lava composition is extremely variable because of heterogeneous igneous activity. The basalt is composed of plagioclase, pyroxene, olivine, magnetite, ilmenite, and plagioclase-phenocrysts. The occurrence of shocked quartz indicates that the rock was formed from plutonic igneous activity. Olivine is up to 75 percent of the total volume of the lava, and the concentration of pyroxene does not exceed 12 percent.
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