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The urban area ... a soft alluvial plainis ... composedof sand , silt , and clay , which are sediments prone to amplify seismic waves
moderately hard sedimentary rockcomposedof very fine - grained ( silt - sized ) particles and clay materials
the uncemented sand / shale rock physics modeldesignedto relate the velocity to porosity and clay content in soft clastic sediment
grain - scale propertiesinfluencingporosity and ultrasonic velocities in siliciclastic sediment
the factorsinfluencingthe water content and clay - particle fabric of clayey sediments
ditch bottom areato contributeclay and silt particles to its flow
sodium ... the sodiumcausesbreakdown of aggregates and dispersal of clay particles
which was formed by or in association with a glacial lake environmenttypically resultingin the deposition of sand- , silt- and clay - sized particles
The banding of the domes(passive) is caused byThe banding of the domes
the electrical conductivity and resistivity of the rocksinfluencethe electrical conductivity and resistivity of the rocks
part of the subdivision to break up and slide toward the ... Clay particles are very smallcausingpart of the subdivision to break up and slide toward the ... Clay particles are very small
part of the subdivision to break up and slide toward the baycausingpart of the subdivision to break up and slide toward the bay
to unacceptable levels of turbidityto leadto unacceptable levels of turbidity
orange and grey bands(passive) are caused byorange and grey bands
The Nile silt layer(passive) is composedThe Nile silt layer
of detrital components ( clay minerals , quartz , carbonates , and feldspars ) and endogenic / authigenic components ( carbonates , sulfides , and organic mattercomposedof detrital components ( clay minerals , quartz , carbonates , and feldspars ) and endogenic / authigenic components ( carbonates , sulfides , and organic matter
The Great Salt Lake Desert or basin(passive) was created byThe Great Salt Lake Desert or basin