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- W2100532005 abstract "Summary Although numerous glacial striae have been observed in upland areas where the glacial deposits are thin, relatively few records of their occurrence are known from the thickly drift-covered parts of eastern Durham, and those that have been described present no consistent pattern of ice movement. The study of samples from the Lower Till sheet of east Durham by both stone orientation analysis and stone count analysis indicates a general direction of ice movement from west-north-west to east-south-east. The results illustrate the value of using different and unrelated techniques in the solution of glacial problems." @default.
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- W2100532005 date "1971-04-01" @default.
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- W2100532005 title "STONE ORIENTATION AND STONE COUNT DATA FROM THE LOWER TILL SHEET, EASTERN DURHAM" @default.
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- W2100532005 doi "https://doi.org/10.1144/pygs.38.3.343" @default.
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