Dead Sea

  • The Dead Sea is an endorheic, hypersaline lake located between Jordan, Israel and the West Bank.
  • Its high salinity prevents aquatic life; only bacteria and unicellular algae survive.
  • Its water volume is reduced annually due to the diversion of the Jordan River.
  • It is known for its therapeutic properties and mineral value, despite its low biodiversity.

One of the most famous seas in the world for its particularity is the Dead Sea. It is famous for several reasons. The first is its high amount of salt. This makes life in its waters unable to develop and favors that the rest of the objects can float in it. It is also often known as it is mentioned in various passages in the Bible. Although it is called by the name of the sea, it is an endorheic lake that does not have any kind of outlet.

In this article we are going to tell you about all the characteristics, geology and curiosities of the Dead Sea.

Key features

Dead Sea

The Dead Sea is an endorheic lake that is completely surrounded by land without any type of exit from the water to an open space. That is to say, It is a hypersaline lake with a high concentration of salts that exceeds that of any type of sea or ocean. It is located on the borders of Jordan, Israel and the West Bank. It is located at a depth of about 400 meters below sea level. This may be one of the reasons why it has such a high concentration of salt.

If we analyze it from a perspective, we can see that the Dead Sea is one of the lowest points on Earth. That is, it is the lowest body of water of all. It is divided into two basins separated by a land bridge. The entire basin sits on a depression created by a rift or fault known as the Jordan Valley. This is located between the Judean Hills and the Transjordanian Plateau.

The northern part of the Dead Sea is the largest and deepest. TIt has a length of about 50 kilometers and reaches up to 400 meters deepThe southern basin, on the other hand, is only 11 kilometers long and only 4 meters deep. The only river that flows into this lake is the Jordan River, which is the only continuous tributary of this sea. It typically discharges large amounts of freshwater, especially into the northern basin. If you're interested in the river's geography, you can read more at the history of the Jordan River.

In the southern part, it is usually fed by water from various streams. But this is not a significant contribution. This means that the Dead Sea level does not fluctuate throughout the year. The high salt content amounts to approximately 340 grams per liter. One of the factors that contributes to the high salt content is that the amount of fresh water it receives is less than the amount of water that evaporates. Furthermore, it is important to consider why seawater is salty, which is closely related to its mineral content.

In this case, we have very high seawater evaporation. This is due to the fact that it is located in an area with high temperatures and little rainfall. The salts found in this water are sodium chloride, magnesium chlorine, calcium chloride, potassium chloride, and magnesium bromide. It can be said that approximately 27% of the water in this sea is made up of solid substances.

Formation of the dead sea

biodiversity dead sea

As we mentioned before, the Dead Sea is located on a rift valley. That is, it is a depression bordered by parallel faults. This fault runs along the African and Arabian tectonic plates. Before this rift was created, the Mediterranean Sea was more extensive than now. It came to occupy all roads and Palestine during the jurassic period and the cretaceous. However, in the Miocene the Arabian plate collided with the northern part of the Eurasian plate. This is how the earth began to rise and the central mountain range of Palestine was formed. Little by little, over the years, the rift valley was gradually formed and filled with seawater.

Already in the Pleistocene, there was a large amount of land between the Mediterranean and the valley that was formed because of the crack between the tectonic plates. It was possible to raise several meters until the sea water was withdrawn. This caused the pit and the waters to be isolated. The Gulf of Aqaba was also isolated.

Biodiversity of the Dead Sea

float in the dead sea

As we have mentioned before, the salinity of the Dead Sea is very high. It becomes about 10 times the salinity of the ocean. This makes it practically a marine desert in which only some living beings are capable of inhabiting it. The only living beings capable of surviving in these extreme conditions are bacteria, protozoa, and single-celled algae.

Most of these algae belong to the genus Dunaliella. However, along the entire coastline of the Dead Sea we can find some halophyte plants. These plants are those that are adapted to soils with high concentrations of salinity or alkalinity. On the contrary, we cannot find any type of fish, reptiles, amphibians and much less mammals. On some occasions, some fish are dragged in the river currents and end up dying without any chance of survival.

For this reason, one cannot speak of biodiversity when we refer to the Dead Sea. However, it does not mean that this sea does not possess valuable resources. Thanks to its large amount of salinity, its salts can be extracted for therapeutic purposes. You can also apply the mud that is on the seabed in the body since it has great beneficial properties with its minerals.

Threats

Although this sea does not suffer from overexploitation of fishing, its size and volume has been reducing during the last decades. This is mainly due to the fact that the waters are diverted and there are large subsidences of land that cause some areas of the surroundings to end up collapsing. Since 1960 there has been a reduction in the total water volume. This began to happen when Israel established a pumping station on the shores of the Sea of ​​Galilee. This pumping station caused the Jordan River's waters to be diverted to other countries, which used it to supply water and irrigate their crops.

As a large amount of water is diverted from its main tributary and evaporation is occurring, the volume of water in this sea is decreasing. The water level is shrinking by about 1 meter per year. Due to this situation, you can read more about the effects of its disappearance in the article humanity and climate change.


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