Interfaces in rocks, especially grain boundaries in olivine dominated rocks, have been subject to about 40 years of studies. The grain boundary structure to property relation is fundamental to understand the diverging properties of polycrystalline samples compared to those of single crystals. The number of direct structural observations is small, i.e. in range of 100 micrographs, and the number of measurements of properties directly linked to structural observations is even smaller. Bulk aggregate properties, such as seismic attenuation and electrical conductivity are sensitive to grain size, and seem to show influences by grain boundary character distributions. We review previous studies on grain boundary structure and composition and plausible relations to bulk properties. Experimentally determined seismic properties and rheology of olivine are sensitive to grain boundary characteristics. The grain boundary geometry is described using five independent parameters, generally their structural width is ranges between 0.4-1.2 nm and