The saltiest bodies of water on Earth is in fact contained in some hypersaline lakes of the McMurdo Dry Valleys in Antarctica (such as Don Juan Pond and perhaps Lake Vanda). I will also discuss other notable hypersaline lakes outside Antarctica. It is very important to note that the Dead Sea is often incorrectly considered the world's most saline lake.
Don Juan Pond
The salinity in Don Juan Pond is over 18 times the ocean's salinity: the salinity is high enough that it doesn't freeze even in winter. It has an estimated salinity of over 63%. Therefore, unlike other lakes and ponds in the dry valleys, it has no ice cover. It has been described as a groundwater discharge zone. The dominant ions in solution are calcium and chloride. The area around Don Juan Pond is covered with sodium chloride and calcium chloride salts that have been precipitated as the water evaporated. Unfortunately, in recent years the size of the pond has shrunk considerably. The maximum depth in 1993 was described as "a foot deep." In January 1997, it was approximately 10 cm deep; in December 1998 the pond was almost dry everywhere except for an area of a few tens of square meters. Most of the water that was left was restricted to depressions around large boulders in the pond.
Lake Vanda
Lake Vanda is a hypersaline lake with a salinity more than ten times that of seawater (salinity that exceeds 35%), which makes it technically world's most saline lake outside of Antarctica, although parts of Lake Vanda lie within Antarctica. Lake Vanda is also meromictic, which means that the deeper waters of the lake don't mix with the shallower waters, hence measurements are generally referring to the surface waters. Like Don Juan Pond, there are no fish in Lake Vanda. The only life is microorganisms. But unlike the pond, Lake Vanda actually freezes in the colder months, yielding a totally transparent clear ice, visible metres deep.
Lake Assal
Lake Assal is generally considered the most saline body of water on earth outside Antarctica, with up to 40% (at 20 m depth) salt concentration. Lake Assal is a crater lake in central Djibouti, located at the southern border of Tadjoura Region, touching Dikhil Region, some 120 km west of Djibouti city. It lies 155 m below sea level in the Afar Depression and its shores comprise the lowest point on land in Africa. It measures 19 by 7 km and has an area of 54 km2. The maximum depth is 40 m, whereas the mean depth is 7.4 m , which makes for a water volume of 400 million cubic metres. The catchment area measures 900 km2, and there is just a residual runoff of fresh water into the lake.
Garabogazköl
The salinity of this bay is about 35%. Because of the exceptionally high salinity it has practically no marine vegetation. The Garabogazköl (literally "mighty strait lake") is a shallow inundated depression in the northwestern corner of Turkmenistan. It forms a bay of the Caspian Sea with a surface area of about 18,000 km2. The water volume of the bay fluctuates seasonally with the Caspian Sea; at times it becomes a large bay of the Caspian Sea, while at other times its water level drops drastically.
The Dead Sea
The Dead Sea sits at about 33.7% salinity. It is notable as being 378 m deep: the deepest hypersaline lake in the world. It is not, as often cited, the saltiest body of water on Earth.
The saltiest bodies of water on Earth is in fact contained in some hypersaline lakes of the McMurdo Dry Valleys in Antarctica (such as Don Juan Pond and perhaps Lake Vanda). I will also discuss other notable hypersaline lakes outside Antarctica. It is very important to note that the Dead Sea is often incorrectly considered the world's most saline lake. Don Juan Pond: The salinity in Don Juan Pond is over 18 times the ocean's salinity: the salinity is high enough that it doesn't freeze even in winter. It has an estimated salinity of over 63%. Therefore, unlike other lakes and ponds in the dry valleys, it has no ice cover. It has been described as a groundwater discharge zone. The dominant ions in solution are calcium and chloride. The area around Don Juan Pond is covered with sodium chloride and calcium chloride salts that have been precipitated as the water evaporated. Unfortunately, in recent years the size of the pond has shrunk considerably. The maximum depth in 1993 was described as "a foot deep." In January 1997, it was approximately 10 cm deep; in December 1998 the pond was almost dry everywhere except for an area of a few tens of square meters. Most of the water that was left was restricted to depressions around large boulders in the pond. Lake Vanda: Lake Vanda is a hypersaline lake with a salinity more than ten times that of seawater (salinity that exceeds 35%), which makes it technically world's most saline lake outside of Antarctica, although parts of Lake Vanda lie within Antarctica. Lake Vanda is also meromictic, which means that the deeper waters of the lake don't mix with the shallower waters, hence measurements are generally referring to the surface waters. Like Don Juan Pond, there are no fish in Lake Vanda. The only life is microorganisms. But unlike the pond, Lake Vanda actually freezes in the colder months, yielding a totally transparent clear ice, visible metres deep. Lake Assal: Lake Assal is generally considered the most saline body of water on earth outside Antarctica, with up to 40% (at 20 m depth) salt concentration. Lake Assal is a crater lake in central Djibouti, located at the southern border of Tadjoura Region, touching Dikhil Region, some 120 km west of Djibouti city. It lies 155 m below sea level in the Afar Depression and its shores comprise the lowest point on land in Africa. It measures 19 by 7 km and has an area of 54 km2. The maximum depth is 40 m, whereas the mean depth is 7.4 m , which makes for a water volume of 400 million cubic metres. The catchment area measures 900 km2, and there is just a residual runoff of fresh water into the lake. Garabogazköl: The salinity of this bay is about 35%. Because of the exceptionally high salinity it has practically no marine vegetation. The Garabogazköl (literally "mighty strait lake") is a shallow inundated depression in the northwestern corner of Turkmenistan. It forms a bay of the Caspian Sea with a surface area of about 18,000 km2. The water volume of the bay fluctuates seasonally with the Caspian Sea; at times it becomes a large bay of the Caspian Sea, while at other times its water level drops drastically. The Dead Sea: The Dead Sea sits at about 33.7% salinity. It is notable as being 378 m deep: the deepest hypersaline lake in the world. It is not, as often cited, the saltiest body of water on Earth.
salt water is found in the sea. Saltwater can also be called brine.
No, the Atlantic ocean is the saltiest of the oceans.
Density. The saltier water is the heavier (per unit volume) it is. The saltiest water doesn't always sink though. Seawater density is dependent on temperature, salinity and pressure. Most often the effects of temperature are dominant in determining vertical stratification.
the most common thing on earth crust as well as in human body is water .
A lake in russia called Karymsky.
The ocean covers about 71% of Earth's surface, making it the largest landform on our planet.
Earth is the planet with the most body of water, with approximately 71% of its surface covered by oceans, seas, rivers, and lakes.
Most of the water on earth is salt water.
Ocean water is usually saltiest near the surface. High levels of evaporation at the surface cause a reduction in freshwater and thus create saltier water near the surface. This effect is most dominant in the warm tropical areas around the equator, thus these areas are saltier than in midlatitudes. Since high salinity implies denser, and thus heavier, water, one might suspect that the saltiest water sinks to the bottom. However, temperature effects tend to dominate the vertical stratification.
Most of earth's water is from oceans but its a 50% chance that it is glaciers that has most of earth's water.
Most of the water on earth is salt water.
from where did earth water most likly come