Vidiakot Formation
Ordovician
Karakoram-Hindukush Basin · Central Karakoram Batholith
Part of Baroghil Group
Ordovician in the time scale →Cited in 6 sources Last reviewed Jul 31, 2026
- Rank
- formation
- Status
- Published
- Age
- Paleozoic · Ordovician · Early OrdovicianOrdovician
- Named by
- Quintavalle et al. (2000)
- Type locality
- Type section along the Vidiakot ridge (Baroghil side), Axial Unit; named after the Vidiakot ridge, crops out between the Paur Gol and Chilmarabad.
- Thickness
- 400–500 m
- Lithology
- Fine-grained slate and siltstone with fine sandstone intercalations.
- Synonyms
- Not recorded
Early Ordovician slates and siltstones of the western Karakoram.
Vidiakot formation consists of fine grained slates and siltstone with fine sandstone intercalations. Its age Lower Ordovician.
Fossils
Not recorded
Contacts
Band colour = period; texture = dominant rock type. Lines between bands mark the contact type (wavy = unconformity inferred from a missing period). True scale makes height ∝ recorded thickness; hatched = thickness not recorded. Ages approximate, for ordering.
This unit (highlighted) within its province column; faded ends continue above and below. Line style marks the contact type.
Distribution & setting
- Basin
- Karakoram-Hindukush Basin
- Region
- Central Karakoram Batholith
- Depositional environment
- marine, outer shelf
- Coordinates
- Not recorded
Correlation
Not recorded. Compare this unit against other basins on the correlation panel →
Economic significance
Not recorded
Remarks
A Lower Ordovician fine-clastic unit of the lower Paleozoic succession of the western Karakoram-Hindukush.
Sources (7)
- Malkani, M.S. & Mahmood, Z. (2017). Stratigraphy of Pakistan. Geological Survey of Pakistan, Memoir Vol. 24.
- Gaetani, M. and others (1996). Reconnaissance geology in Upper Chitral, Baroghil and Karambar districts (northern Karakorum, Pakistan). Geologische Rundschau, 85, 683-704.
- Zanchi, A. & Gaetani, M. (2011). The geology of the Karakoram range, Pakistan: the new 1:100,000 geological map of Central-Western Karakoram. Italian Journal of Geosciences, 130(2), 161-262.
- Shah, S.M.I. (2009). Stratigraphy of Pakistan. Geological Survey of Pakistan, Memoir Vol. 22.
- Talent, J.A., Gaetani, M., Mawson, R., Molloy, P.D. & Conaghan, P.J. (1999). Early Ordovician and Devonian conodonts from the Western Karakoram and Hindu Kush, northernmost Pakistan. Rivista Italiana di Paleontologia e Stratigrafia, 105(2), 201-226.
- Gaetani, M., Le Fort, P., Tanoli, S., Angiolini, L., Nicora, A., Sciunnach, D. & Khan, A. (1996). Reconnaissance geology in Upper Chitral, Baroghil and Karambar districts (northern Karakorum, Pakistan). Geologische Rundschau, 85, 683-704.
- Kazmi, A.H. & Abbasi, I.A. (2008). Stratigraphy and Historical Geology of Pakistan. Department & National Centre of Excellence in Geology, University of Peshawar, Peshawar. 524 pp. ISBN 978-969-9119.
Reviewer confidence: medium
Every fact on this page is source-cited. This entry is part of the peer-archived Pakistan Stratigraphy Dataset (doi.org/10.5281/zenodo.21363991, CC‑BY‑4.0).
Lexicon status: Name attested in the Shah (1977/2009) Geological Survey of Pakistan compilation — the national stratigraphic lexicon. This records where the name is documented; it is not an endorsement of the unit’s definition, age or figures.
Cite this unit
Qudsi, L. (2026). Vidiakot Formation. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991
@misc{stratigraphypk_vidiakotformation,
author = {Qudsi, Lareb},
title = {{Vidiakot Formation} --- Pakistan Stratigraphy Dataset},
year = {2026},
publisher = {Zenodo},
doi = {10.5281/zenodo.21363991},
url = {https://doi.org/10.5281/zenodo.21363991}
} Archived dataset: doi.org/10.5281/zenodo.21363991 (CC‑BY‑4.0) · Direct link to this entry: https://stratigraphy.pk/formation/vidiakot-formation (accessed August 30, 2026).
To cite the unit's original definition instead, see: Quintavalle et al. (2000).
Related units
Referenced in other successions
Overlain by Vandanil Formation
Saved on this device only.