Misri Banda Ordovician Quartzite
Khyber–Nowshera Belt · also Misri Banda trace-fossil locality
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
The geology here
The stratigraphic units exposed at this site — every geological fact above traces to their cited sources.
Quantitative assessment
Scored with the Brilha (2016) method — each value 0–400. Desk-based first pass; the full score matrix ships with the open dataset.
Nearby geosites
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