temperature, current, and turbidity A+temperature, current, and turbidity
mixing with sediment
Turbidity refers to the cloudiness or haziness of a fluid. Turbidity current density results from water mixing with sediment particles.
An underwater avalanche is called a turbidity current. It is a fast-moving current of sediment and water that flows down a slope on the ocean floor, resembling an avalanche in terrestrial environments. Turbidity currents can be triggered by factors such as earthquakes, underwater landslides, or excess sediment supply.
Turbidity currents result from underwater landslides. These currents are caused by sediment-rich water rapidly moving downslope due to gravity, carrying sediment and debris with them. Turbidity currents can be powerful and can affect marine ecosystems and underwater infrastructure.
temperature, current, and turbidity A+temperature, current, and turbidity
"They move along the bottom."
turbidity currents...
mixing with sediment.
mixing with sediment
Turbidity refers to the cloudiness or haziness of a fluid. Turbidity current density results from water mixing with sediment particles.
A turbidity current is denser due to the sediment it carries, causing it to sink beneath the clearer, lighter water. This density difference results in the turbidity current flowing along the seafloor, transporting sediment and creating undersea canyons and deposits.
By mud slides
An underwater avalanche is called a turbidity current. It is a fast-moving current of sediment and water that flows down a slope on the ocean floor, resembling an avalanche in terrestrial environments. Turbidity currents can be triggered by factors such as earthquakes, underwater landslides, or excess sediment supply.
The type of deposit that results from a turbidity current is a sediment deposit, or a turbidite. This type of deposit makes the water denser, which makes it sink deeper while the clearer water rises.
An ancient turbidity current deposit found in a mountain may be recognized by characteristic sedimentary structures such as graded bedding, cross-bedding, and lamination. These deposits often consist of fine-grained sediments that settled out of a high-energy underwater current. Additionally, fossils or paleocurrent indicators within the deposit can provide further evidence of its origin as a turbidity current.
Turbidity currents