1961
DOI: 10.1061/taceat.0008148
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Underseepage and its Control: A Symposium: Investigation of Underseepage - Mississippi River Levees

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Cited by 9 publications
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“…The upper 40 m of sediments at our study area share the near-surface sedimentary facies common throughout the LMRV (Figure 3), which contains Holocene point bar channel deposits and associated abandoned channels [12,61]. Point bar sedimentary sequences are the product of the river's lateral accretion over time, developing highly vertical and horizontal heterogeneous soils in terms of grain size and composition [12,61].…”
Section: Geological and Geotechnical Setting Of The Study Areamentioning
confidence: 86%
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“…The upper 40 m of sediments at our study area share the near-surface sedimentary facies common throughout the LMRV (Figure 3), which contains Holocene point bar channel deposits and associated abandoned channels [12,61]. Point bar sedimentary sequences are the product of the river's lateral accretion over time, developing highly vertical and horizontal heterogeneous soils in terms of grain size and composition [12,61].…”
Section: Geological and Geotechnical Setting Of The Study Areamentioning
confidence: 86%
“…The upper 40 m of sediments at our study area share the near-surface sedimentary facies common throughout the LMRV (Figure 3), which contains Holocene point bar channel deposits and associated abandoned channels [12,61]. Point bar sedimentary sequences are the product of the river's lateral accretion over time, developing highly vertical and horizontal heterogeneous soils in terms of grain size and composition [12,61]. The upper 10-m section of Mississippi point bars is often composed of interbedded sands, silts, and clays with preservation of the original accretionary dip angle and represents the inclination of the inner bank of the river channel bend [62].…”
Section: Geological and Geotechnical Setting Of The Study Areamentioning
confidence: 89%
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