Small-scale faults at high-angle from the primary bedding in the c. 2.8 Ga banded iron formation near Mount Magnet. The gap created during faulting is filled by basaltic lava flows. Photo ID 670
Small-scale faults at high-angle from the primary bedding in the c. 2.8 Ga banded iron formation near Mount Magnet. The gap created during faulting is filled by basaltic lava flows. Photo ID 670
Photograph: ivan zibra
Reference: Geological Survey of Western Australia. http://www.dmp.wa.gov.au/371.aspx