Kawagarh Fm
Type Locality and Naming
Holotype section: Kawagarh Hills, north of Kalachitta Range (KcR). Author: A. Day (AOC, unpublished report). Reference section: None.
Lithology and Thickness
Clayey limestone. The formation in its type locality and adjoining areas of northern Kalachitta Range (KcR), Nizampur and eastern Kohat consists of dark marl, calcareous shale and nodular / argillaceous limestone. In eastern Kohat (Kohat Pass section) dolomitic limestone beds occur in the lower part while further west in Samana Range, Darsamand and Khadimak sections, the formation is typically a lithographic to sublithographic, grey and light grey limestone with subordinate marl and shale. The formation is divisible in western Kohat into two members: (1) an upper Tsukail Tsuk Limestone, which mainly consists of a grey sub-lithographic, thick, bedded to massive, escarpment forming limestone, and (2) A lower Chalor Silli member, which consists of light grey, olive grey, lithographic to sub-lithographic, thin- to medium-bedded limestone with subordinate calcareous shale and marl intercalations in the lower part. In southern Hazara area, the lithology is similar to western Kohat; however, in upper part a Nara Sandstone member, which consists of grey, brownish grey to dark grey, thick-bedded calcareous sandstone with some minor limestone interbeds is recognized. In northern Hazara (Kathwal-Kalapani section), the sandstone member is not developed and the Kawagarh Fm consists of grey, olive grey, light grey sublithographic limestone with subordinate marl and calcareous shale.
Thickness: 40-200+ m. In the type section, its thickness ranges from 40-70 m. In western Kohat, the thickness varies from 110 m (Samna Range) to 120 m (Darsamand section). In eastern Kohat, it varies from 70 m (Taudi Mela section) to 90 m (Mazari Tang section). In Hazara, the thickness varies from 45 m in the south (Changla Gali) to over 200 m (Chanali section). It is 70 m in Kathwal section.
Relationships and Distribution
Lower contact
Disconformably underlain by Lumshiwal Fm
Upper contact
Disconformably overlain by Hangu Fm (Paleocene).
Regional extent
This formation is developed only in Kohat, northern Kalachitta Range (KcR), Nizampur and Hazara (Kohat-Margala Province (Ko-MP)). The formation is NOT developed in southern KcR, the SR and TrIR where the Tertiary rocks directly overlie Lumshiwal Fm or older rocks.
GeoJSON
Fossils
The formation contains Globotruncana lapperenti, G. vaporate, G. concavata carinata, G. vapora - calcarata, Heterohelix reussi, H. globocarinate, H. globolusa etc.
Age
Depositional setting
Additional Information