1. The fossils are located on the bedding planes , and are randomly oriented. 2. Deep underground, this water then moves horizontally along bedding planes and fractures. 3. M�lange occurrences are associated with thrust faulted terranes in bedding planes . 4. The mudstone shows cleavage at an angle steeper than the bedding planes by 20? 5. Carboniferous Limestone has horizontal layers ( beds ) with bedding planes , and vertical joints. 6. Mudcracks are a common as well as wavy bedding planes . 7. It makes up the brunt of some bedding plane assemblages. 8. The ore boundaries are parallel to the bedding planes . 9. This realignment, known as schistosity, bears no relationship to the original horizontal bedding planes . 10. The footprints, which form tracks, occur in several levels on bedding planes of fine-grained sediments.
Mobile