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Pakistan Stratigraphy
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Mesozoic • Cretaceous formation GSP memoir

Khalkhal Formation

? Cretaceous

Karakoram-Hindukush Basin · Central Karakoram Batholith

Cretaceous in the time scale →

Cited in 4 sources Last reviewed Jul 30, 2026

Unit summary
Rank
formation
Status
Published
Age
Mesozoic · Cretaceous? Cretaceous
Named by
Desio (1963)
Type locality
Khalkhal glacier, a tributary of the Godwin-Austen (Baltoro) glacier35.8000°N, 76.4500°E
Thickness
about 800 m
Lithology
About 800 m of slaty calcareous sandstone, phyllite and conglomerate.
Synonyms
Not recorded

A thick (about 800 m) slaty metasedimentary unit of the Baltoro glacier region.

Named by Desio (1963) after the Khalkal Glacier, a tributary of the Godwin-Austen Glacier in the Baltoro basin, the Khalkal Formation is about 800 m of slaty calcareous sandstone, phyllite and conglomerate.

Fossils

Not recorded

Contacts

In the Karakoram column
IgneousLimestoneSandstoneFossils 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
Karakoram-Hindukush Basin
Region
Central Karakoram Batholith
Depositional environment
Not recorded
Coordinates
35.8000°N, 76.4500°E

Correlation

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

Economic significance

Not recorded

Remarks

A thick metasedimentary slate–sandstone–phyllite unit of the Baltoro region of the central Karakoram; its precise age is not established.

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.

Age & correlation (1)

  • Kazmi & Jan (1997): the Khalkhal Formation (the book's spelling; DB 'Khalkal' is a typo) is queried Cretaceous — shales, sandstones and conglomerates forming the highest (youngest) stratigraphic level of the Gasherbrum sedimentary sequence, in the sedimentary belt north of the Karakoram Batholith (Broad Peak area, where it is deformed to greenschist facies). This is a Karakoram/Gasherbrum unit — the DB regional tagging should be verified.

    Kazmi, A.H. & Jan, M.Q. (1997)

Thickness (1)

  • Baseline thickness '200m' is a migration artifact: it is the thickness of the K2 gneiss, whose description is concatenated into this record. The Khalkal Formation proper is about 800 m thick (Desio, 1963). Flag for Phase-6 cleanup.

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

Sources (3)

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). Khalkhal Formation. In Pakistan Stratigraphy Dataset [Data set]. Zenodo. https://doi.org/10.5281/zenodo.21363991

BibTeX
@misc{stratigraphypk_khalkalformation,
  author    = {Qudsi, Lareb},
  title     = {{Khalkhal 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/khalkal-formation (accessed October 29, 2026).

To cite the unit's original definition instead, see: Desio (1963).

    Saved on this device only.