The Quarterly journal of the Geological Society of London . f the Quaetzite-geavel to Geavelsor Local Oeigin. In the neighbourhood of Goring and Pangbourne the Quartzite-gravel is closely associated with deposits of a wholly differentcharacter and origin. On the western slopes of the Chilterns there is a spread of gravelconsisting almost wholly of flint, and mostly angular or subangular,which ranges from Little Stoke and Ipsden in a northerly directionto the neighbourhood of Watlington, as shown in the accompanyingsketch-map (PI. XXVIII). It occupies a plateau at a height ofabout 350 feet abov

GLIX-115-2AWG7MN

The Quarterly journal of the Geological Society of London . f the Quaetzite-geavel to Geavelsor Local Oeigin. In the neighbourhood of Goring and Pangbourne the Quartzite-gravel is closely associated with deposits of a wholly differentcharacter and origin. On the western slopes of the Chilterns there is a spread of gravelconsisting almost wholly of flint, and mostly angular or subangular,which ranges from Little Stoke and Ipsden in a northerly directionto the neighbourhood of Watlington, as shown in the accompanyingsketch-map (PI. XXVIII). It occupies a plateau at a height ofabout 350 feet abov
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The Quarterly journal of the Geological Society of London . f the Quaetzite-geavel to Geavelsor Local Oeigin. In the neighbourhood of Goring and Pangbourne the Quartzite-gravel is closely associated with deposits of a wholly differentcharacter and origin. On the western slopes of the Chilterns there is a spread of gravelconsisting almost wholly of flint, and mostly angular or subangular,which ranges from Little Stoke and Ipsden in a northerly directionto the neighbourhood of Watlington, as shown in the accompanyingsketch-map (PI. XXVIII). It occupies a plateau at a height ofabout 350 feet abov

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