1994
DOI: 10.1016/0013-7952(94)90077-9
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The Netherlands without engineering geology: No lands

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“…Such deposits, along with younger soft Holocene clays, are particularly predisposed to settlement and compaction. Holocene sands deposited in tidal channels are very loosely packed and often exhibit porosities greater than 40%, consequently, such sands can be instable and prone to liquefaction (De Mulder, 1994). The Pleistocene deposits in the east are predominantly sandy soils that are glacial, fluvial and aeolian in origin.…”
Section: Geologymentioning
confidence: 99%
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“…Such deposits, along with younger soft Holocene clays, are particularly predisposed to settlement and compaction. Holocene sands deposited in tidal channels are very loosely packed and often exhibit porosities greater than 40%, consequently, such sands can be instable and prone to liquefaction (De Mulder, 1994). The Pleistocene deposits in the east are predominantly sandy soils that are glacial, fluvial and aeolian in origin.…”
Section: Geologymentioning
confidence: 99%
“…While generally flat, these deposits gently slope upwards to an elevation of 20 m above mean sea level in the east and south, although ice-pushed ridges can locally reach heights of 100 m (De Mulder, 1994;van der Meulen et al, 2013).…”
Section: Geologymentioning
confidence: 99%
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