. The Quarterly journal of the Geological Society of London. of the surface section from toBurdole, length 1100yards (see Fig. 22 ). The sequence of 2, 3, i and 5 is proved upon theescarZmt ■ that of 1 andl on the dip slope. XI. is, to a certain extent, constructive: the sequence of 1, 2 and 3is lined on the east side of Malum; that of 5 and 6 on the west side; tin- exact relation of No. 4 to the Upper andLou; r Groups is »> guile dear. XII. is a vertical rendering of the surface section across the Hambleton massive,lenath s m (see ); 4 and 5 vary greatly within short distan
. The Quarterly journal of the Geological Society of London. of the surface section from toBurdole, length 1100yards (see Fig. 22 ). The sequence of 2, 3, i and 5 is proved upon theescarZmt ■ that of 1 andl on the dip slope. XI. is, to a certain extent, constructive: the sequence of 1, 2 and 3is lined on the east side of Malum; that of 5 and 6 on the west side; tin- exact relation of No. 4 to the Upper andLou; r Groups is »> guile dear. XII. is a vertical rendering of the surface section across the Hambleton massive,lenath s m (see ); 4 and 5 vary greatly within short distances; the thickness of 5 is a presumed averagealma Ot actual line of section; northwards it is 50 ft. thick, and southwards it has thinned out. XIII. gives the,1. r I. out of the series as shoivn in a transverse valley about the centre of tlie Tabular Chain: the lower part ofl\^eTthiThTOStler,-here only i ft. thick. XIV Another transverse valley, 5 m. from the coait theI M?adle Calcareous Grit PerlxpS °U *fL ** **; * 3 Quart ;: [ MSuft ■ it* i: . PI XY\T.
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Keywords: ., bookcentury1800, bookdecade1840, bookidquarte, booksubjectgeology
