Measurements of the magnetoresistivity of graphite with a high degree of
control of the angle between the sample and magnetic field indicate that the
metal-insulator transition (MIT), shown to be induced by a magnetic field
applied perpendicular to the layers, does not appear in parallel field
orientation. Furthermore, we show that interlayer transport is coherent in less
ordered samples and high magnetic fields, whereas appears to be incoherent in
less disordered samples. Our results demonstrate the two-dimensionality of the
electron system in ideal graphite samples.Comment: 4 figures, details adde