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Pakistan Stratigraphy
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Cenozoic • Neogene formation GSP memoir

Vihowa Formation

Miocene

Sulaiman Basin

Part of Vihowa Group

Neogene in the time scale →

Cited in 6 sources Last reviewed Aug 10, 2026

Unit summary
Rank
formation
Status
Published
Age
Cenozoic · Neogene · late Early–Middle MioceneMiocene
Named by
Hemphill and Kidwai (1973)
Type locality
Vihowa Road, Sulaiman Range31.0667°N, 70.2667°E
Thickness
~700 m (type section, Vihowa Road)
Lithology
Grey and brown sandstone with subordinate red to brownish-red sandy siltstone; mudstone-rich in the lower part.
Synonyms
Not recorded

The lowest of the Sulaiman 'Siwalik' river deposits, full of Lower Siwalik mammal fossils, laid down as the foreland rivers got going ~17 million years ago.

Introduced by Hemphill and Kidwai (1973), type section at Vihowa Rud, the Vihowa Formation is red-to-maroon shale with grey-white calcareous sandstone and conglomerate plus silica sands, about 400–700 m thick. Its lower contact with the Chitarwata Formation and upper contact with the Litra Formation are disconformable. It is rich in continental vertebrates (Hemphill & Kidwai, 1973).

Fossils

Contacts

In the Sulaiman Fold Belt column
SandstoneFossils recordedConformable

Band colour = period; texture = dominant rock type. Lines between bands mark the contact type. 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
Sulaiman Basin
Region
Not recorded
Depositional environment
fluvial, continental
Coordinates
31.0667°N, 70.2667°E

Correlation

Not recorded. Compare this unit against other basins on the correlation panel →

Economic significance

Oligocene-Miocene coal showings; part of the uranium- and silica-sand-bearing Vihowa Group.

Remarks

The lower unit of the Siwalik-equivalent molasse (Vihowa Group) of the Sulaiman Range, equivalent to the Kamlial–Chinji formations of the Potwar; its fluvial channel-floodplain deposits and Lower Siwalik mammal fauna record establishment of the Himalayan foreland river system by about 17 Ma.

Sources (6)

Reviewer confidence: high

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: Appears in a single-author Geological Survey of Pakistan memoir (Malkani & Mahmood 2017), not cross-confirmed against the Shah lexicon. The Stratigraphic Committee of Pakistan is largely inactive, so documented provenance — not formal ratification — is the available signal.

Cite this unit
APA

Qudsi, L. (2026). Vihowa Formation. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991

BibTeX
@misc{stratigraphypk_vihowaformation,
  author    = {Qudsi, Lareb},
  title     = {{Vihowa 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/vihowa-formation (accessed August 30, 2026).

To cite the unit's original definition instead, see: Hemphill and Kidwai (1973).

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