The type area of the Ordovician Misri Banda Quartzite, whose cross-bedded quartzites carry abundant Cruziana rugosa and Skolithos trace fossils — among the clearest Lower Palaeozoic ichnofossil assemblages in the Peshawar basin.

• Type section of the Misri Banda Quartzite (Tremadoc–Llandeilo)
• Cruziana rugosa and Skolithos trace fossils
• Marks the Ordovician transgression over the Cambrian(?) Ambar Formation

This geosite is an editorial selection; the geological facts trace to the cited sources on the linked unit pages. Coordinates are indicative and not surveyed. ← All geosites · Suggest a correction