Oceans and Seas

There's no country there. That point is in the south Pacific Ocean, and there aren't

too many places on Earth where you could be farther from any country or any land.

It's at least 1,300 miles from the nearest point on the coast of Antarctica, and

1,600 miles from the nearest point on the South American coast of Chile.

Places where sea water is evaporated to get salt are typically called salt pans or salt flats. These areas are created by allowing seawater to evaporate naturally, leaving behind salt deposits that can then be harvested.

Marine organisms are said to live in a "desert" because ocean waters, especially in open ocean regions, have low nutrient concentrations similar to those found in deserts. This makes it challenging for marine organisms to find food, just like how organisms in deserts struggle to find water. However, in contrast to deserts, the ocean is vast and teeming with life in certain areas.

The Salton Sea is located in a desert region with a hot desert climate characterized by high temperatures and low precipitation. The geography of the area consists of dry, arid landscapes with salt flats and agricultural fields surrounding the sea. The sea itself is a shallow, saline lake that is below sea level.

Canada is bordered by three oceans: the pacific, the atlantic, and the Arctic.

hurricane

The coastline of Libya is approximately 1,770 kilometers (1,100 miles) long.

Ocean crust is younger than landform crust. Oceanic crust is constantly being created at mid-ocean ridges through volcanic activity, making it much younger in comparison to the older landform crust found on continents.

True. Global warming causes the polar ice caps and glaciers to melt, leading to an increase in sea levels. This is due to the additional water from melted ice entering the oceans, contributing to sea level rise.

The salt water that covers about three-quarters of the Earth's surface is called the ocean.

Wyoming is a landlocked state, so it does not border the Pacific Ocean. The closest point to the Pacific Ocean from Wyoming would be in western Oregon, which is approximately 800 miles away.

The Mariana Trench was formed by the Pacific Plate subducting beneath the Mariana Plate. This subduction process created the deep trench in the western Pacific Ocean.

Mid-ocean ridges are caused by divergent plate boundaries, where tectonic plates move away from each other. This movement allows magma to rise to the surface, creating new crust and forming underwater mountain ranges.

Sea level rise can lead to increased flooding, erosion of coastlines, and saltwater intrusion into freshwater sources, affecting communities further inland. This can disrupt livelihoods, damage infrastructure, and pose risks to property and food security. Therefore, people living further away from the coast may still be impacted by the consequences of sea level rise.

Yes, the Pacific Ring of Fire and the Ring of Fire are the same thing. The Pacific Ring of Fire is a horseshoe-shaped area in the Pacific Ocean basin where many earthquakes and volcanic eruptions occur due to tectonic plate movements.

Life can exist on the mid-ocean ridge due to deep-sea hydrothermal vents that release mineral-rich, superheated water into the cold ocean, creating a unique ecosystem. Organisms such as tube worms, giant clams, and microbes thrive in these extreme conditions by utilizing chemosynthesis instead of photosynthesis to produce energy. The discovery of these ecosystems challenges our understanding of where life can exist on Earth.

due to scientists theory's yes, there is more salt. but the salt isn't actual table salt you would find, its a special kind of salt, mostly broken up coral and some other chemicals put together it contains Na (sodium) that's all i know.

Yes, a large trench known as the Mid-Atlantic Ridge runs down the middle of the Atlantic Ocean basin. This underwater mountain range is where tectonic plates are moving apart, causing new oceanic crust to form in the process.

Sediment closer to mid-ocean ridges is typically younger, coarser, and consists of more volcanic material compared to sediment farther away. This is because the closer proximity to the ridge results in a higher input of freshly erupted material from the underlying volcanic activity.

The North American Plate and the Eurasian Plate are separated by the Mid-Atlantic Ridge. The ridge is a divergent boundary where the two plates are moving away from each other, causing magma to rise and create new oceanic crust.

When ocean water freezes into sea ice, some of the salt is incorporated into the new ice. Thereafter, that salt drains as brine (salt plus water), causing the layer of water below to be of higher salinity.

The combination of salt water and fresh water is called brackish water.

The city where winds blow across an ocean can vary depending on the prevailing wind patterns. For example, cities like San Francisco, Cape Town, and Tokyo experience winds blowing across the ocean due to their coastal locations and prevailing wind directions.

Tides are created by the known and predictable gravitational pull of the sun and moon in their relationship to the earth. Tides are also affected by unpredictable forces of nature (winds, storms, river runs, atmospheric pressure changes). An understanding of the forces causing ocean tides is complex.

Generally, there will be 2 high tides and 2 low tides every 24 hours occuring approximately 50 minutes later each day. During periods of full moon or new moon high tides are usually higher than normal and low tides are usually lower than normal. During periods of the first quarter and last quarter the high tides and the low tides are usually less than normal.