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Sedimentary Geology Geos 240 – Chapter 7 Sediment Transport Processes. Dr. Tark Hamilton Readings from Sediments & Basins: (7:1-41) Camosun College. Crossbeds, Cretaceous Non-Marine NEBC. Hjulstrom Diagram: Caliber vs Velocity.
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Sedimentary GeologyGeos 240 – Chapter 7Sediment Transport Processes Dr. Tark Hamilton Readings from Sediments & Basins: (7:1-41) Camosun College
Turbulent Boundary LayerCauses Flow Separation:Tractive flow, Entrainment, Suspension
Turbidity Current in a Lab Flume:Dense, Turbulent, Sediment Underflow
Flume Observations Laminar Stable Flow Turbulent Flow
Variation in Ripple/Dune shapesVersus Shallowness & Velocity or
Gravel Dunes Haro Strait Real Gap, no bedforms Unstable turbulent transition
Standing Waves form Antidunes California Beach
ReversingTidal CurrentsFloodSlackwaterEbbSlackwater*(not all tides arepurely diurnal!)~basin shape
Symmetric - Tidal Foresets - Asymmetric Or Tidal Delta
New/Full Half
Wave Rippled Modern Beach South CarolinaInterference Patterns in Sandy RipplesFormed During Prior Flood TideBeing Modified in Ebb
Wave Rippled Ordovician Calcarenites, Ottawa Sandbars Herringbone Dolo-grainstones Calsiltites
HummockyCrossStratification(HCS)JurassicOld RedSandstoneYorkshire(domes &mounds)
Storm Driven – Coriolis ControlledDue to Flow in a Rotating Reference Frame
Modern Wind Ripples Climbing Dune Face Lighter Winds Channelled By Older Dunes
Permian Wind Fall Ripples AZ Note Rare Wind Ripple Foresets