There are a number of processes that could fit this description including mud / debris flows and solifluction (both types of "mass wasting"). In pelagic / benthic (marine) settings turbidity currents would also fit this description.
Please see the related links.
There are a number of processes that could fit this description including mud / debris flows and solifluction (both types of "mass wasting"). In pelagic / benthic (marine) settings turbidity currents would also fit this description.
Please see the related links.
Sediment-laden water is known as a turbidity current, and is usually formed by the slumping of waterlogged sediment on the continental slope.
Turbidity currents.
Turbidity currents
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In the Mediterranean Sea the cool dense water sinks under less dense water which is called density current.
i dont know im doing science homewok and i need this answer this
low pressure. because warm air is less dense. so it's pressure is also low.( less dense because because of the heat( warm air = hot air) the molecules of the air is very active. so the the are not close to each other which means less dense)
More dense material is less buoyant in water than less dense material of equal volume. Sediment shape also plays a role in deposition sequence as material with angular irregular surfaces are more likely to be carried by water flow than smooth surfaces, due to friction with the water. Finally, the size of the sediment particle, particularly of rock material, may be most critical in the sequence of deposition; larger particles are the first to overcome the power of friction encountered in moving water, via gravity.
When it is heated it becomes less dense (i.e. lighter). The more dense (i.e. heavier) magma sinks while the less dense magma rises to the top. It will eventually cool again causing a convection current within the mantle.
Turbidity currents
Turbidity currents
The smallest, least dense particles.
Turbidity currents are caused by sand and mud on the continental shelf and slope that is dislodged and thrown into suspension. Turbidity currents themselves are downslope movements of dense, sediment-laden water. Source: I'm in a college level geology course.
A density current forms when more dense seawater moves toward less dense seawater.
Dense regular and dense irregular connective tissues
the answer to this question is a density current forms when more dense seawater sinks beneath less dense seawater
You would fine sediment in the benthic zone, or bottom, of a lake.
Density current
Water from the rain mixes with loose sediment, forming a dense slurry that can flow downhill.
In the Mediterranean Sea the cool dense water sinks under less dense water which is called density current.
In the Mediterranean Sea the cool dense water sinks under less dense water which is called density current.