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Our comparison of magnetic susceptibility with the lithology reveals that the high values of magnetic susceptibility are in the strata of sand and silt in the interglacial periods, whereas they are low in the strata of silty clay in the glacial periods.
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The upper part of this sequence, which was 10- to 13-m thick, was characterized by a set of acoustically transparent layers, and the lower part consisted of well-stratified strata suggestive of thin alternations of sand and mud.
The world in a grain of sand.
Consider a heap of sand.
Processes of sand remobilization, injection, and extrusion are complex and depend on many interrelated factors including: fluid(s) properties (e.g. pressure, volume, composition), parent unit and host-strata characteristics (e.g. depositional architecture, grain size and distribution, clay-size fraction, thickness, permeability) and burial depth at the time of injection.
Density of sand.
Porosity of sand.
Weight of sand.
Speaking of sand niggers.
Castles Made of Sand.
Several beaches lost 15-20 feet of sand.
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