brine pool

The island is named for brine pools in its interior at the north end.

Without mixing, oxygen from above can't get into the brine pool.

Under the right conditions, including favorable ocean floor topography, a brine pool may be created.

Deep sea brine pools often coincide with cold seep activity.

Deep sea and Antarctic brine pools can be toxic to marine animals.

This prevents the water in the brine pool from mixing with the 'normal' seawater above.

The most common bacteria in the brine pool was the Thiomicrospira arctica.

Brine pools are another seabed feature, usually connected to cold seeps.

A brine pool is a large area of brine on the ocean basin.

Brine pools are large areas of brine on the seabed.

These brine pools are completely without any oxygen (anoxic).

Sometimes these lakes are called brine pools.

Both countries recover the lithium from brine pools.

Bromine is found as bromide in the ocean and in brine pools.

It is built by halophilic (salt loving) bacteria, found in high-temperature brine pools.

However, some salt lakes have "trapped" brine pools beneath them with salinities up to ten times seawater.

The pool at Nantwich today dates back to 1935 and is possibly the only inland brine pool left in the country.

These are sometimes called brine lakes, but are more frequently referred to as brine pools.

In the United States lithium is recovered from brine pools in Nevada.

When submarines dive into brine pools, they float on the brine surface due to the high density.

Ocean explorers have discovered lakes and pools on the ocean floor that are known as brine pools.

The Orca Basin is a distinctive brine pool on the Louisiana continental shelf.

The largest of the Boroughs Pools and probably the only inland Brine Pool left in the country.

Lithium salts are extracted from the water in mineral springs, brine pools and brine deposits.

Iodine is found on Earth mainly as the highly water-soluble iodide I, which concentrates it in oceans and brine pools.