This is the most common pelagic sediment by area, covering 48% of the world ocean's floor.

The composition of pelagic sediments is controlled by three main factors.

These pelagic sediments are typically bright red to chocolate brown in color.

Though slow by human standards, this rate is much faster than that for deep-sea pelagic sediments.

As the least common type of pelagic sediment, it covers only 15% of the ocean floor.

Pelagic sediments of red mud dominate the deeper regions.

Based upon the composition of the ooze are three main types of pelagic sediments.

The remainder of the sediment is composed chiefly of pelagic sediments.

The chalk was formed by pelagic sediments deposited along the eastern edge of the Mississippi embayment.

Such instrumentation includes acoustic mappers and a pelagic sediment profiler to produce maps of the sea floor.

Siliceous ooze is a soft siliceous pelagic sediment that covers large areas of the deep ocean floor.

These pelagic sediments also contain authegenic minerals that include zeolites, limonite and manganese oxides.

Hemipelagic sediments are those deposited slowly, but not as slowly as pelagic sediments.

Pelagic sediments, containing significant quantities of siliceous biogenic remains, are commonly referred to as siliceous ooze.

Trace amounts of meteoric dust and variable amounts of volcanic ash occur within pelagic sediments.

Diatoms calcium hydrogen carbonate skeletal material these things are probably ending up predominantly as deep sea sediments pelagic sediments, yeah, remember?

North of 50 south latitude, 86% of the main basin is covered by pelagic sediments, of which more than half is globigerina ooze.

Ooze is pelagic sediment that consists of at least 30% of microscopic remains of either calcareous or siliceous planktonic debris organisms.

In the western domain open towards the Atlantic, the pelagic sediments comprise ammonite-bearing limy marls very rich in filamentous microfossils (bryozoans).

The formation of the Cordillera Oriental covered the continental platform with pelagic sediments with Precambrian and Paleozoic metamorphic rocks bases.

Pelagic sediment or pelagite is a fine-grained sediment that has accumulated by the settling of particles through the water column to the ocean floor beneath the open ocean far from land.

The remainder of the sediment comprises chiefly dust (clay particles) blown out to sea from land, and the remains of small marine plants and animals which sink from the upper layer of the ocean, known as pelagic sediments.

Classic, low-density turbidites are characterized by graded bedding, current ripple marks, alternating sequences with pelagic sediments, distinct fauna changes between the turbidite and native pelagic sediments, sole markings, thick sediment sequences, regular bedding, and an absence of shallow-water features (Fairbridge, 1966).

This is the most common pelagic sediment by area, covering 48% of the world ocean's floor.

The composition of pelagic sediments is controlled by three main factors.

These pelagic sediments are typically bright red to chocolate brown in color.

Though slow by human standards, this rate is much faster than that for deep-sea pelagic sediments.

As the least common type of pelagic sediment, it covers only 15% of the ocean floor.

Pelagic sediments of red mud dominate the deeper regions.

Based upon the composition of the ooze are three main types of pelagic sediments.

The remainder of the sediment is composed chiefly of pelagic sediments.

The chalk was formed by pelagic sediments deposited along the eastern edge of the Mississippi embayment.

Such instrumentation includes acoustic mappers and a pelagic sediment profiler to produce maps of the sea floor.

Siliceous ooze is a soft siliceous pelagic sediment that covers large areas of the deep ocean floor.

These pelagic sediments also contain authegenic minerals that include zeolites, limonite and manganese oxides.

Hemipelagic sediments are those deposited slowly, but not as slowly as pelagic sediments.

Pelagic sediments, containing significant quantities of siliceous biogenic remains, are commonly referred to as siliceous ooze.

Trace amounts of meteoric dust and variable amounts of volcanic ash occur within pelagic sediments.

Diatoms calcium hydrogen carbonate skeletal material these things are probably ending up predominantly as deep sea sediments pelagic sediments, yeah, remember?

North of 50 south latitude, 86% of the main basin is covered by pelagic sediments, of which more than half is globigerina ooze.

Ooze is pelagic sediment that consists of at least 30% of microscopic remains of either calcareous or siliceous planktonic debris organisms.

In the western domain open towards the Atlantic, the pelagic sediments comprise ammonite-bearing limy marls very rich in filamentous microfossils (bryozoans).

The formation of the Cordillera Oriental covered the continental platform with pelagic sediments with Precambrian and Paleozoic metamorphic rocks bases.

Pelagic sediment or pelagite is a fine-grained sediment that has accumulated by the settling of particles through the water column to the ocean floor beneath the open ocean far from land.

The remainder of the sediment comprises chiefly dust (clay particles) blown out to sea from land, and the remains of small marine plants and animals which sink from the upper layer of the ocean, known as pelagic sediments.

Classic, low-density turbidites are characterized by graded bedding, current ripple marks, alternating sequences with pelagic sediments, distinct fauna changes between the turbidite and native pelagic sediments, sole markings, thick sediment sequences, regular bedding, and an absence of shallow-water features (Fairbridge, 1966).

Pelagic sediment or pelagite is a fine-grained sediment that has accumulated by the settling of particles through the water column to the ocean floor beneath the open ocean far from land.