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The Ocean's Memory: Sediment Distribution Patterns
00:41

The Ocean's Memory: Sediment Distribution Patterns

While sediments of all varieties can be found almost anywhere in the marine environment, there are some very distinct distribution patterns.

The Ocean's Memory: Sediments and Earth's Magnetic Field
02:03

The Ocean's Memory: Sediments and Earth's Magnetic Field

As with climate changes, there have been some unexplained aberrations in Earth's magnetic field during the recent past. Marine sediments provide important information that may help scientists better understand those aberrations.

The Ocean's Memory: Biogenous Sediments
01:12

The Ocean's Memory: Biogenous Sediments

While most sediments are terrigenous, there are other sediments that are also found in the marine environment. Biogenous sediments are those that form from the shells or skeletons of marine animals.

The Ocean's Memory: Terrigenous Sediments
02:10

The Ocean's Memory: Terrigenous Sediments

Sediment is the debris that accumulates on the surface of the Earth as the result of chemical, physical and biological processes. Most sediment, known as terrigenous sediment, forms when rain falls on soil and washes it into rivers, which then carry...

The Ocean's Memory: Obtaining and Analyzing Sediment Samples
06:22

The Ocean's Memory: Obtaining and Analyzing Sediment Samples

Despite its temporary nature, sediment remains uniquely valuable. As a result, oceanographers have worked hard to refine the process of obtaining and analyzing sediment samples.

The Ocean's Memory: Oil, Gas and Manganese Nodules
03:37

The Ocean's Memory: Oil, Gas and Manganese Nodules

Sediment is a uniquely valuable commodity within the marine environment. Oil, natural gas, coal, diamonds, gravel, sand, tin and titanium are all associated with marine sediment. Perhaps the most famous potential deep sea deposits are manganese nodu...

The Ocean's Memory: Sediments and Past Climate
05:09

The Ocean's Memory: Sediments and Past Climate

As sediments get laid down, they carry with them a record of the kind of environment in which they were formed. Scientists can read that record and learn valuable information about past climate and temperature change.