. The Quarterly journal of the Geological Society of London. closed betweenlines of fault. In a case of ordinary unconformity or overlap subjected to denu-dation, discordant patches of the Murree beds might be expected tooccur resting on the older rocks; but these have not been met with,any detached portions which have been found being apparently let inamong the older rocks by faults, rather than folded into Under all these circumstances it is difficult to recognize inthis and the Simla region the same relations among formations orgroups, several of which may be fairly consider
. The Quarterly journal of the Geological Society of London. closed betweenlines of fault. In a case of ordinary unconformity or overlap subjected to denu-dation, discordant patches of the Murree beds might be expected tooccur resting on the older rocks; but these have not been met with,any detached portions which have been found being apparently let inamong the older rocks by faults, rather than folded into Under all these circumstances it is difficult to recognize inthis and the Simla region the same relations among formations orgroups, several of which may be fairly considered identical and in PHYSICAL GEOLOGY OF THE UPPER PUNJAB. 73 the same orographical position. Even in the Simla area a fault-likecharacter is attributed to the abnormal junction; and had we herethe transgressive overlap of different portions of the Tertiary serieson to the hill-rocks, it might be easier to assimilate the features ofthe two areas and to admit for this district Mr. Medlicotts viewthat the junction-line is not one of fault but of (50 S 3 | <D ID a a
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Keywords: ., bookcentury1800, bookdecade1840, bookidquarte, booksubjectgeology
