Oceanography

It is called a bathysphere. Horse Isle answer: bathysphere

An iceberg is a large piece of freshwater ice floating in the open ocean. It forms when chunks of ice break off from glaciers or ice shelves. The majority of an iceberg's mass is underwater, with only a small portion visible above the surface.

Some deep-sea fish use bioluminescent organs to produce their own light, attracting prey to them in the darkness of the deep ocean. This ability helps them hunt for food efficiently in the vast, dark environments they inhabit.

The phenomena of ocean waves lighting up at night is called bioluminescence. This occurs when certain marine organisms, such as phytoplankton or jellyfish, produce light through a chemical reaction within their bodies, creating a magical glowing effect in the water.

The deep-water zone is the region of the ocean that is located below the sunlight zone, extending from approximately 200 meters to the ocean floor. This zone is characterized by low temperatures, high pressure, and complete darkness, and is inhabited by different species of fish, cephalopods, and other deep-sea creatures. Seabed features such as abyssal plains, trenches, and hydrothermal vents can be found in the deep-water zone.

High tide times vary because they are influenced by factors such as the gravitational pull of the moon and sun, the shape of the coastline, the depth of the water, and the Earth's rotation. These factors create differences in the timing and height of tides at different locations around the world.

It graduly changes throughout the year. The only way to know is to get a pamplet showing what tides will hapen when. Hope it helps ;)

Sand heats up faster than dirt because it has a lower specific heat capacity, which means it requires less heat to increase its temperature. Additionally, sand is more porous and has less moisture content compared to dirt, allowing it to absorb and retain heat more effectively.

One estimate is that there are approximately 1.3 billion cubic kilometers of water on Earth (salt water and fresh water). This does not include the volume within hydrated minerals.

This is equal to about 1.3 x 1021 (1.3 billion trillion) liters of water of all kinds, including ice in ice sheets and glaciers. Of that, liquid fresh water is only about 0.6% of the total.

The most negatively charged ion dissolved in seawater is chloride. In fact, Cl- makes up 55 percent of the seawater's salinity.

Ocean waves form as wind blows across the surface of the water, creating friction and energy that transfers to the water. The energy causes the water to move in a circular motion, forming waves that travel across the ocean's surface. Factors such as wind speed, duration, and distance over which it blows determine the size and strength of the waves.

Seven Seas:

the Red Sea, the Mediterranean Sea, the Persian Gulf, the Black Sea, the Adriatic Sea, the Caspian Sea, and the Indian Ocean

Major Oceans:

the Arctic Ocean, the Atlantic Ocean, the Indian Ocean, the Pacific Ocean

The North Equatorial Current is important because it influences global climate patterns by transporting warm water towards higher latitudes, affecting weather and precipitation patterns. It also plays a crucial role in the ocean's ecosystem by redistributing nutrients and supporting diverse marine life, including commercially important fish species.

The oldest ocean, geologically, is the Panthalassa Ocean which was around 220 million years ago in the Triassic era.

It encompassed the whole Earth except the land mass Pangea.

See related link for more information.

The area between bulges of water in the ocean is known as a trough. This is the part of the water surface that is lower between two adjacent crests. Troughs are typically found in waves and result from the alternating rise and fall of the water.

Oceanographer Jacques Piccard died in Cully Switzerland in 2008.

Abiotic parts of the ocean include non-living elements like water, sunlight, temperature, salinity, oxygen, and minerals. These abiotic factors play a crucial role in shaping the marine environment and influencing the distribution and abundance of marine life.

The main features of a hurricane include strong winds that can exceed 74 mph, heavy rainfall leading to flooding, and a low-pressure center known as the eye. Hurricanes can also produce storm surges, which are large, dome-shaped coastal floods caused by the combination of high winds and low atmospheric pressure.

If you can centrifuge it and get something out of it then it is a mixture. If it is a solution it is a physical combination and not chemical reaction.
Yes i definatly can be. Its possible in some cases the minerals are not correctly combining. But for the most part, its a mixture.
yes because sea water is mixed with water and salt and other minerals and mixture is anything that you can combine

One good experiment to demonstrate why the ocean is salty involves using a simulation with a container filled with water and adding salt to it. As the water evaporates, the salt remains behind, showing how salt gets deposited in the ocean over time through processes like evaporation and erosion from rocks. This can help explain why the ocean is salty.

Ocean currents do not directly affect Las Vegas, as it is located inland and far from any major bodies of water. However, changes in ocean currents can influence weather patterns that may indirectly impact weather conditions in Las Vegas.

Dr. Robert Ballard utilized the Argo, which was a deep sea underwater craft. Going by what he found when he used the Argo to search for two sunken Navy submarines, he then used it to seach for a debris field. His belief is that Titanic imploded as it sank to the ocean floor. He eventually found the Titanic on September 1, 1985.

The two main types of tides are spring tides and neap tides. Spring tides occur when the sun, moon, and Earth are aligned, resulting in higher high tides and lower low tides. Neap tides occur when the sun and moon are at right angles to each other, resulting in less extreme tidal variations.

Quoting Guinness Book of Records: The slowest-moving fish are the sea horses (Syngnathidas), of which there are about 30 species. Some of the smaller species, such as the dwarf sea horse (Hippocampus zosterae), probably never attain speeds of more than 0.001 m.p.h.