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Paleozoic • Permian In GSP lexicon

Warchha Sandstone

Early Permian (Artinskian)

Part of Nilawahan Group

Permian in the time scale →

Cited in 9 sources Last reviewed Jul 30, 2026

Unit summary
Rank
Not recorded
Status
Published
Age
Paleozoic · Permian · CisuralianEarly Permian (Artinskian)
Named by
Not recorded
Type locality
Warcha, Salt Range32.6628°N, 72.6939°E
Thickness
30 m (eastern Salt Range) to 155 m (western Salt Range)
Lithology
Sandstone, shale with speckled appearance
Synonyms
Speckled Sandstone; Warchha Group (part); Warcha Formation

A Permian red-bed sandstone deposited by high-sinuosity meandering rivers with broad floodplains; its speckled sandstone is a distinctive marker in the Nilawahan Group.

Named after Warcha in Salt Range. Post-glacial marine transgressive sequence. Speckled sandstone is distinctive marker horizon. Dandot Formation is a junior synonym. Part of the Nilawahan Group.

Fossils

Contacts

In the Salt Range column
SandstoneMixedFossils 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
Not recorded
Region
Not recorded
Depositional environment
fluvial, coastal, estuarine
Coordinates
32.6628°N, 72.6939°E

Correlation

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

Economic significance

The arkosic 'speckled sandstone' hosts sub-economic sedimentary copper, lead and tin shows northeast of Mianwali and north of Nilawahan Gorge — copper as chalcopyrite and malachite, tin as stannite, cassiterite and native tin — and carries local poor-quality coal seams. Preliminary trench sampling (~300 samples in 15 trenches; Gilani 1981) was not encouraging and base-metal potential is rated low.

Remarks

A fluvial sandstone deposited by meandering, avulsion-prone rivers on the northern margin of Gondwana; detailed facies-architecture and provenance studies make it one of the best-documented Permian fluvial successions of the Salt Range.

Sources (8)

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: 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
APA

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

BibTeX
@misc{stratigraphypk_warchaformation,
  author    = {Qudsi, Lareb},
  title     = {{Warchha Sandstone} --- 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/warcha-formation (accessed August 30, 2026).

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