. Memoirs of the Geological Survey of India. Section across Sulphur-spring ravme at Lalci cu Wan^TihiJtrj T>. Jtfivrth-ci?*, of spring. Pig Section across DhaianBange atDliaran Laic . KHIRTHAR RANGE. 87 At Bando-ji-kabar, near the head of the Salari stream, Nari beds1Nari beds on higher come in uPon tne Khirthars of the higher range,Tan£es- . and extend thence to the southward, occupying the trough of a synclinal between two ridges of Khirthar general section is shown in the annexed sketch (PL III, fig. 1).The synclinal of Nari beds is continued across the head
. Memoirs of the Geological Survey of India. Section across Sulphur-spring ravme at Lalci cu Wan^TihiJtrj T>. Jtfivrth-ci?*, of spring. Pig Section across DhaianBange atDliaran Laic . KHIRTHAR RANGE. 87 At Bando-ji-kabar, near the head of the Salari stream, Nari beds1Nari beds on higher come in uPon tne Khirthars of the higher range,Tan£es- . and extend thence to the southward, occupying the trough of a synclinal between two ridges of Khirthar general section is shown in the annexed sketch (PL III, fig. 1).The synclinal of Nari beds is continued across the head-waters of theSalari and Maki streams to beyond Harar. It is much complicated andcut up by faults, the sharp synclinals and anticlinals being frequentlyaccompanied by fracture and slipping. Thus at the head of the Salarithe section is of this kind (PI. Ill, fig. £), or there may be a fault•east as well as west of the Nari synclinal. Between the Salari and Maki streams, and again south of the Maki stream, the ridge of Khirthar limestone to theKhirthar ridge. r,j , . east of the Nan synclinal has a precipitous scarp to the eastward, probably a fa
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Keywords: ., bookcentury1800, booksubjectgeology, booksubjectminesandmineralr
