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Pakistan Stratigraphy
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Cenozoic • Neogene formation GSP memoir

Manchar Formation

Miocene-Pliocene

Kirthar Basin

Neogene in the time scale →

Cited in 6 sources Last reviewed Jul 31, 2026

Unit summary
Rank
formation
Status
Published
Age
Cenozoic · Neogene · Miocene-PlioceneMiocene-Pliocene
Named by
Blanford (1876)
Type locality
Manchhar (Manchar) Lake area, Sindh26.4230°N, 67.6730°E
Thickness
1000-2000 m
Lithology
Sandstone, clay, conglomerate (continental)
Synonyms
Manchar Group; Manchhar Formation; Manchhar Series

The Sindh version of the Siwalik molasse - Miocene-Pliocene river sandstones and clays around Manchhar Lake that carry the same kinds of mammal fossils as the Potwar Siwaliks.

Continental molasse in lower Indus basin. Equivalent to Siwalik Group. Contains mammal fossils.

Fossils

Contacts

In the Sindh Province column
SandstoneShale / mudFossils recordedContact not recorded

Band colour = period; texture = dominant rock type. Lines between bands mark the contact type; dotted = no contact recorded in the sources (not a claim of conformity). 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
Kirthar Basin
Region
Not recorded
Depositional environment
fluvial, continental
Coordinates
26.4230°N, 67.6730°E

Correlation

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

Economic significance

Not recorded

Remarks

The Miocene-Pliocene continental molasse of the lower Indus Basin, originally named the 'Manchhar Series' by Blanford (1876) after Manchhar Lake; it is the Sindh equivalent of the Siwalik Group. Poorly consolidated, fine- to medium-grained sandstone, clay and conglomerate overlie the marine Gaj Formation and yield Siwalik-type mammal fossils.

Research notes (2)

Field-by-field findings drawn from the cited literature. Every statement is traced to a registered source — follow a citation for the full reference.

Name & nomenclature (1)

  • Merged duplicate unit "Manchar Group" (manchar-group) into this record. Sources, provinces and any missing fields were carried over; the old name is retained as a synonym.

    Malkani, M.S. & Mahmood, Z. (2017)

Age & correlation (1)

  • Brohi et al. (2009): the Manchar Formation (Upper Miocene; book/paper spelling 'Manchar') caps the marine Tertiary section on the Surjan Anticline (Thano Bula Khan), overlying the Gaj Formation and underlying the Pleistocene Dada Conglomerate. Consistent with the curated Mio–Pliocene age.

    Brohi, I.A., Bablani, S.A. & Solangi, S.H. (2009)

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.

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Cite this unit
APA

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

BibTeX
@misc{stratigraphypk_mancharformation,
  author    = {Qudsi, Lareb},
  title     = {{Manchar 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/manchar-formation (accessed October 29, 2026).

To cite the unit's original definition instead, see: Blanford (1876).

    Saved on this device only.