. Bulletin of the British Museum (Natural History), Geology. AND JURASSIC AMMONITES FROM WEST PAKISTAN 303 Kala Chitta the outcrops take a north easterly swing and are exposed in Hazara Ranges (Margala and Murree Hills) lying between Abbottabad and Islamabad. These northerly placed Mesozoic out-crops are separated by a belt of Tertiary and Quarternary deposits from the southern outcrops of Western Salt Range and Trans Indus Ranges (Surghar, Maidan and Khisor Ranges including Shaikh Budin Hills). In the eastern and north-eastern limits the Mesozoic rocks of northern areas are separated from tha
. Bulletin of the British Museum (Natural History), Geology. AND JURASSIC AMMONITES FROM WEST PAKISTAN 303 Kala Chitta the outcrops take a north easterly swing and are exposed in Hazara Ranges (Margala and Murree Hills) lying between Abbottabad and Islamabad. These northerly placed Mesozoic out-crops are separated by a belt of Tertiary and Quarternary deposits from the southern outcrops of Western Salt Range and Trans Indus Ranges (Surghar, Maidan and Khisor Ranges including Shaikh Budin Hills). In the eastern and north-eastern limits the Mesozoic rocks of northern areas are separated from that of Himalaya (Spiti) by a belt of Tertiary and Quarternary , u s S R INDEX 77A AREA INVESTIGATED 1. HAZARA 2 KALACHITTA 3. NlZAMPUR 4. KOHAT 5 TRANS INDUS SALT RANGE 6 SHAIKH BUDIN HILLS 0 100 1 1 34°T. ABBOTTABAD^ yPESHAWAR J °&1 4 Kohol l_yoCompbellpur s/2>° ° 3T E2 "RAWALPINDI c 1 Kolobogh «.". Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original British Museum (Natural History). London : BM(NH)
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