1844
DOI: 10.1680/imotp.1844.24537
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On Railway Cuttings and Embankments; With an Account of Some Slips in the London Clay, on the Line of the London and Croydon Railway.

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Cited by 5 publications
(3 citation statements)
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“…Earlier Gregory (1844) describing the slip at New Cross Station on the London-Croydon railway noted that 'innumerable breaks or faults in this soil are found to be covered with crystals in minute flakes or spiculae between which the water would have a clear passage'.…”
Section: Eocenementioning
confidence: 99%
“…Earlier Gregory (1844) describing the slip at New Cross Station on the London-Croydon railway noted that 'innumerable breaks or faults in this soil are found to be covered with crystals in minute flakes or spiculae between which the water would have a clear passage'.…”
Section: Eocenementioning
confidence: 99%
“…As early as 1844, an engineer, Gregory and a geologist, Sir Henry Delabache observed the softening of fissures within the London clay and suggested that progressive softening might account for slips that occurred several years after construction [5]. Soon after, it was suggested that clay slopes along canals would eventually be reduced to inclinations similar to those exhibited in the natural terrain.…”
Section: Slopes and Overconsolidationmentioning
confidence: 99%
“…Since the first suggestions by Gregory and Delabeche that the strength of the London clay was being reduced by a softening of the clay material adjacent to fissures, several other researchers have alluded to this possible mechanism to account for the deterioration of strength in many clays [5].…”
Section: Slip Surface Ru = Wh/zmentioning
confidence: 99%