Deep Sea Sedimentary Systems Flashcards

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Vocabulary flashcards covering the drivers, components, and physics of deep-sea sedimentary systems based on lecture notes.

Last updated 2:11 PM on 5/13/26
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15 Terms

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Grand Banks earthquake (1929)

An event that caused the severing of submarine telegraph cables up to 700km700\,km away, 1313 hours after the initial tremor, with recorded speeds reaching 7.7m/sec7.7\,m/sec.

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Turbidite systems

The systems through which most deep-sea sediment is supplied.

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Eustatic lowstand

A driver of slope sediment erosion tied to climatic changes or sea level drops.

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Autocyclic migration

The movement of sheet sands and channels that changes dispersal systems on the basin floor.

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Submarine canyons

Conduits for sediment deposition in the deep ocean, more commonly found on the steep slopes of active margins.

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Upwards formation (Submarine Canyons)

The creation of canyons caused by headward erosion of the continental slope by mass wasting and retrogressive slumping.

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Downwards formation (Submarine Canyons)

The creation of canyons through erosion by turbidity currents sourced from the continental shelf, often associated with riverine systems.

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Submarine fans

Accumulations of sediment deposited at the termini of land-to-deep-sea sediment routing systems, such as the Indus Fan or Bengal Fan.

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Slides

Mass movements involving large, intact blocks moving on a slippage plane.

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Slumps

Mass movements similar to slides but characterized by blocks that may break up into smaller pieces.

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Debris Flows

A type of mass movement where laminar flow leads to an unsorted deposit.

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Turbidity Currents

Submarine flows characterized by turbulent flow that leads to sorted deposits, known as Bouma Divisions.

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Reynolds Number (RR)

The ratio of viscous to inertial forces used to determine if a flow is turbulent or laminar.

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Laminar flow

A flow state that occurs when the Reynolds Number (RR) is small and viscous forces dominate.

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Turbulent flow

A flow state that occurs when the Reynolds Number (RR) is large and inertial forces dominate.