. The Quarterly journal of the Geological Society of London . he bed below, and running downamongst the lumps. Worn flint-shaped lumps of hard marl, vertical fracture. Sandy, with perished shells in lajers. Clay, red and grey, in lanrinse. Very red sandy rock, sometimes blue and grey, with large bivalves, layers in sandy laminated brown sandy sandy stone, often red outside, ripple-marks on the top. Composed of perished shells, thin layers of limestone and a line of beef about the and yellow sand in layers. , thin-laminated, soft
. The Quarterly journal of the Geological Society of London . he bed below, and running downamongst the lumps. Worn flint-shaped lumps of hard marl, vertical fracture. Sandy, with perished shells in lajers. Clay, red and grey, in lanrinse. Very red sandy rock, sometimes blue and grey, with large bivalves, layers in sandy laminated brown sandy sandy stone, often red outside, ripple-marks on the top. Composed of perished shells, thin layers of limestone and a line of beef about the and yellow sand in layers. , thin-laminated, soft and yellow; impressions of Archceoniscus. Hard blue and brown marl, Archceoniscus, Cyprides, Cyclas, Ostrece, insects thin white limestone and red sand rock, occasional streaks of blue; oysters and impressions of large sandy limestone. Fig. 2.—Section of Parbeck-Becls in a Railway-cutting 1^ mile westof Dinton Station, Vale of Wardour. (Scale, -i- inch to 1 foot.) Surface. Wealden and Trail. o O Q a Flints, trail. Yellow and red sandy clays. Endogenites erosa. Hard marl, eroded surface. lining Beef. Chert.
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Keywords: ., bookcentury1800, bookdecade1840, bookidquarte, booksubjectgeology
