Dead Sea in the context of Tributary


Dead Sea in the context of Tributary

Dead Sea Study page number 1 of 4

Play TriviaQuestions Online!

or

Skip to study material about Dead Sea in the context of "Tributary"


⭐ Core Definition: Dead Sea

The Dead Sea (Arabic: اَلْبَحْر الْمَيِّت, romanizedal-Baḥr al-Mayyit; or اَلْبَحْر الْمَيْت, al-Baḥr al-Mayt; Hebrew: יַם הַמֶּלַח, romanizedYam hamMelaḥ), also known by other names, is a landlocked salt lake bordered by Jordan to the east, the Israeli-occupied West Bank to the west and Israel to the southwest. It lies in the endorheic basin of the Jordan Rift Valley, and its main tributary is the Jordan River.

As of 2025, the lake's surface is 439.78 metres (1,443 ft) below sea level, making its shores the lowest land-based elevation on Earth. It is 304 m (997 ft) deep, the deepest hypersaline lake in the world. With a salinity of 342 g/kg, or 34.2% (in 2011), it is one of the world's saltiest bodies of water, 9.6 times as salty as the ocean—and has a density of 1.24 kg/litre, which makes swimming similar to floating. This salinity makes for a harsh environment in which plants and animals cannot flourish, hence its name. The Dead Sea's main, northern basin is 50 kilometres (31 mi) long and 15 kilometres (9 mi) wide at its widest point.

↓ Menu
HINT:

In this Dossier

Dead Sea in the context of Messinian salinity crisis

The Messinian salinity crisis (also referred to as the Messinian event, and in its latest stage as the Lago Mare event) was an event in which the Mediterranean Sea went into a cycle of partial or nearly complete desiccation (drying-up) throughout the latter part of the Messinian age of the Miocene epoch, from 5.96 to 5.33 Ma (million years ago). It ended with the Zanclean flood, when the Atlantic reclaimed the basin.

Sediment samples from below the deep seafloor of the Mediterranean Sea, which include evaporite minerals, soils, and fossil plants, show that the precursor of the Strait of Gibraltar closed about 5.96 million years ago, sealing the Mediterranean off from the Atlantic. This resulted in a period of partial desiccation of the Mediterranean Sea, the first of several such periods during the late Miocene. After the strait closed for the last time around 5.6 Ma, the region's generally dry climate at the time dried the Mediterranean basin out nearly completely within a thousand years. This massive desiccation left a deep dry basin, reaching 3 to 5 km (1.9 to 3.1 mi) deep below normal sea level, with a few hypersaline pockets similar to today's Dead Sea. Then, around 5.5 Ma, wetter climatic conditions resulted in the basin receiving more fresh water from rivers, progressively filling and diluting the hypersaline lakes into larger pockets of brackish water (much like today's Caspian Sea). The Messinian salinity crisis ended with the Strait of Gibraltar finally reopening 5.33 Ma, when the Atlantic rapidly filled up the Mediterranean basin in what is known as the Zanclean flood.

View the full Wikipedia page for Messinian salinity crisis
↑ Return to Menu

Dead Sea in the context of Israel

Israel, officially the State of Israel, is a country in the Southern Levant region of West Asia. It borders Lebanon to the north, Syria to the northeast, Jordan to the east and Egypt to the southwest. Israel occupies the Palestinian territories of the West Bank in the east and the Gaza Strip in the southwest, as well as the Syrian Golan Heights in the northeast. Israel's western coast lies on the Mediterranean Sea, the southern tip reaches the Red Sea, and the east includes the Earth's lowest point near the Dead Sea. Jerusalem is the government seat and proclaimed capital, while Tel Aviv is Israel's largest urban area and economic centre.

The Land of Israel is synonymous with Palestine or the Holy Land. In antiquity it was home to the Canaanites and later the kingdoms of Israel and Judah. Its location at a continental crossroads brought demographic shifts under various empires. Nineteenth-century European antisemitism fuelled the Zionist movement for a Jewish homeland. Britain endorsed this goal in the 1917 Balfour Declaration and ruled Mandatory Palestine from 1920. Jewish immigration and British policies intensified Arab-Jewish tensions, and the 1947 United Nations (UN) Partition Plan led to a civil war.

View the full Wikipedia page for Israel
↑ Return to Menu

Dead Sea in the context of Jordan

Jordan, officially the Hashemite Kingdom of Jordan, is a country in the Southern Levant region of West Asia. Jordan is bordered by Syria to the north, Iraq to the east, Saudi Arabia to the south, and both Israel and Palestine (West Bank) to the west. The Jordan River, flowing into the Dead Sea, is located along the country's western border within the Jordan Rift Valley. Jordan has a small coastline along the Red Sea in its southwest, separated by the Gulf of Aqaba from Egypt. Amman is the country's capital and largest city, as well as the most populous city in the Levant.

Inhabited by humans since the Paleolithic period, three kingdoms developed in Transjordan during the Iron Age: Ammon, Moab and Edom. In the third century BC, the Arab Nabataeans established their kingdom centered in Petra. The Greco-Roman period saw the establishment of several cities in Transjordan that comprised the Decapolis. After the end of Byzantine rule, the region became part of the Islamic caliphates of the Rashidun, Umayyad, Abbasid, and the Ottoman. Following the 1916 Great Arab Revolt during World War I, former Ottoman Syria was partitioned, leading to the establishment of the Emirate of Transjordan in 1921, which became a British protectorate. In 1946, Jordan gained independence and became officially known as the Hashemite Kingdom of Jordan. Jordan captured and annexed the West Bank during the 1948 Palestine war until it was occupied by Israel in 1967. Jordan renounced its claim to the territory to the Palestinians in 1988 and signed a peace treaty with Israel in 1994.

View the full Wikipedia page for Jordan
↑ Return to Menu

Dead Sea in the context of Jerusalem

Jerusalem is a city in the Southern Levant, on a plateau in the Judaean Mountains between the Mediterranean and the Dead Sea. It is one of the oldest cities in the world, and is considered holy to the three major Abrahamic religionsJudaism, Christianity and Islam. Both Israel and Palestine claim Jerusalem as their capital city; Israel maintains its primary governmental institutions there, while Palestine ultimately foresees it as its seat of power. Neither claim is widely recognised internationally.

Throughout its long history, Jerusalem has been destroyed at least twice, besieged 23 times, captured and recaptured 44 times, and attacked 52 times. The part of Jerusalem called the City of David shows first signs of settlement in the 4th millennium BCE, in the shape of encampments of nomadic shepherds. During the Canaanite period (14th century BCE) Jerusalem was named as Urusalim on ancient Egyptian tablets, probably meaning "City of Shalem" after a Canaanite deity. During the Israelite period, significant construction activity in Jerusalem began in the 10th century BCE (Iron Age II), and by the 9th century BCE the city had developed into the religious and administrative centre of the Kingdom of Judah. In 1538 the city walls were rebuilt for a last time around Jerusalem under Suleiman the Magnificent of the Ottoman Empire. Today those walls define the Old City, which since the 19th century has been divided into four quarters—the Armenian, Christian, Jewish and Muslim quarters. The Old City became a World Heritage Site in 1981, and is on the List of World Heritage in Danger. Since 1860 Jerusalem has grown far beyond the Old City's boundaries. In 2023 Jerusalem had a population of 1,028,366. In 2022 60% were Jews and almost 40% were Palestinians. In 2020 the population was 951,100, of which Jews comprised 570,100 (59.9%), Muslims 353,800 (37.2%), Christians 16,300 (1.7%) and 10,800 unclassified (1.1%).

View the full Wikipedia page for Jerusalem
↑ Return to Menu

Dead Sea in the context of Evaporite

An evaporite (/ɪˈvæpəˌrt/) is a water-soluble sedimentary mineral deposit that results from concentration and crystallization by evaporation from an aqueous solution. There are two types of evaporite deposits: marine, which can also be described as ocean deposits, and non-marine, which are found in standing bodies of water such as lakes. Evaporites are considered sedimentary rocks and are formed by chemical sediments.

View the full Wikipedia page for Evaporite
↑ Return to Menu

Dead Sea in the context of Meander

A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank (cut bank or river cliff) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain.

The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.

View the full Wikipedia page for Meander
↑ Return to Menu

Dead Sea in the context of Southern Levant

The Southern Levant is a geographical region that corresponds approximately to present-day Israel, Palestine, and Jordan; some definitions also include southern Lebanon, southern Syria and the Sinai Peninsula. As a strictly geographical description, it is sometimes used by archaeologists and historians to avoid the religious and political connotations of other names for this area.

Like much of Southwestern Asia, the Southern Levant is an arid region consisting mostly of desert and dry steppe, with a thin strip of wetter, temperate climate along the Mediterranean coast. Geographically it is dominated by the Jordan Valley, a section of the Great Rift Valley bisecting the region from north to south, and containing the Sea of Galilee, the Jordan River and the Dead Sea—the lowest point on the Earth's land surface.

View the full Wikipedia page for Southern Levant
↑ Return to Menu

Dead Sea in the context of West Bank

The West Bank is on the western bank of the Jordan River and is the larger of the two Palestinian territories (the other being the Gaza Strip) that make up the State of Palestine. A landlocked territory near the coast of the Mediterranean Sea in West Asia's Levant region, it is bordered by Jordan and the Dead Sea to the east and by Israel (via the Green Line) to the south, west, and north. Since 1967, the territory has been under Israeli occupation, which has been regarded as illegal under the law of the international community.

The territory first emerged in the wake of the 1948 Arab–Israeli War as a region occupied and subsequently annexed by Jordan. Jordan ruled the territory until the 1967 Six-Day War, when it was occupied by Israel. Since then, Israel has administered the West Bank (except for East Jerusalem, which was effectively annexed in 1980) as the Judea and Samaria Area. Jordan continued to claim the territory as its own until 1988. The mid-1990s Oslo Accords split the West Bank into three regional levels of Palestinian sovereignty, via the Palestinian National Authority (PNA): Area A (PNA), Area B (PNA and Israel), and Area C (Israel, comprising 60% of the West Bank). The PNA exercises total or partial civil administration over 165 Palestinian enclaves across the three areas.

View the full Wikipedia page for West Bank
↑ Return to Menu

Dead Sea in the context of Jordan River

The Jordan River or River Jordan (Arabic: نَهْر الْأُرْدُنّ, Nahr al-ʾUrdunn; Hebrew: נְהַר הַיַּרְדֵּן, Nəhar hayYardēn), also known as Nahr Al-Sharieat (Arabic: نهر الشريعة), is a 251-kilometre-long (156 mi) endorheic river in the Levant that flows roughly north to south through the Sea of Galilee and drains to the Dead Sea. The river passes by or through Jordan, Syria, Israel, and the Palestinian territories.

Jordan and the Israeli-occupied Golan Heights border the river to the east, while Israel and the Israeli-occupied West Bank lie to its west. Both Jordan and the West Bank derive their names in relation to the river. The river holds major significance in Judaism and Christianity. According to the Bible, the Israelites crossed it into the Promised Land and Jesus of Nazareth was baptized by John the Baptist in it.

View the full Wikipedia page for Jordan River
↑ Return to Menu

Dead Sea in the context of Jordan Rift Valley

The Jordan Rift Valley, also Jordan Valley (Modern Hebrew: בקעת הירדן Bik'at Hayarden, Biblical Hebrew: בִּקְעָת הַיַרְדֵּן, romanized: Biqʿāṯ hay-Yardēn, Arabic: الغور, romanizedal-Ghawr), is an elongated endorheic basin located in modern-day Israel, Jordan, and Palestine. This geographic region includes the entire length of the Jordan River from its sources, through the Hula Valley, the Korazim Plateau, the Sea of Galilee, the Jordan Valley, all the way to the Dead Sea, the lowest land elevation on Earth – and then continues through the Arabah depression, the Gulf of Aqaba whose shorelines it incorporates, until finally reaching the Red Sea proper at the Straits of Tiran.

View the full Wikipedia page for Jordan Rift Valley
↑ Return to Menu

Dead Sea in the context of Moab

Moab (/ˈmæb/) was an ancient Levantine kingdom whose territory is today located in southern Jordan. The land is mountainous and lies alongside much of the eastern shore of the Dead Sea. The existence of the Kingdom of Moab is attested to by numerous archaeological findings, most notably the Mesha Stele, which describes the Moabite victory over an unnamed son of King Omri of Israel, an episode also noted in 2 Kings 3. The Moabite capital was Dibon. According to the Hebrew Bible, Moab was often in conflict with its Israelite neighbours to the west.
Cite error: There are <ref group=lower-alpha> tags or {{efn}} templates on this page, but the references will not show without a {{reflist|group=lower-alpha}} template or {{notelist}} template (see the help page).

View the full Wikipedia page for Moab
↑ Return to Menu

Dead Sea in the context of Sea level

Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datum – a standardised geodetic datum – that is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead a long-term average of tide gauge readings at a particular reference location.

The term above sea level generally refers to the height above mean sea level (AMSL). The term APSL means above present sea level, comparing sea levels in the past with the level today.

View the full Wikipedia page for Sea level
↑ Return to Menu

Dead Sea in the context of Kingdom of Judah

The Kingdom of Judah was an Israelite kingdom of the Southern Levant during the Iron Age. Centered in the highlands to the west of the Dead Sea, the kingdom's capital was Jerusalem. It was ruled by the Davidic line for four centuries. Jews are named after Judah, and primarily descend from people who lived in the region.

The Hebrew Bible depicts the Kingdom of Judah as one of the two successor states of the United Kingdom of Israel, a term denoting the united monarchy under biblical kings Saul, David, and Solomon and covering the territory of Judah and Israel. However, during the 1980s, some biblical scholars began to argue that the archaeological evidence for an extensive kingdom before the late 8th century BCE is too weak, and that the methodology used to obtain the evidence is flawed. In the 10th and early 9th centuries BCE, the territory of Judah might have been limitedly populated, comprising some fortified sites and many unfortified rural settlements. The Tel Dan Stele, discovered in 1993, shows that the kingdom existed in some form by the middle of the 9th century BCE, but it does not indicate the extent of its power. Recent excavations at Khirbet Qeiyafa, however, support the existence of a centrally organized and urbanized kingdom by the 10th century BCE, according to the excavators.

View the full Wikipedia page for Kingdom of Judah
↑ Return to Menu

Dead Sea in the context of Bitumen

Bitumen (UK: /ˈbɪʊmɪn/ BIH-chuum-in, US: /bɪˈtjmɪn, b-/ bih-TEW-min, by-) is an immensely viscous constituent of petroleum. Depending on its exact composition, it can be a sticky, black liquid or an apparently solid mass that behaves as a liquid over very large time scales. In American English, the material is commonly referred to as asphalt. Whether found in natural deposits or refined from petroleum, the substance is classed as a pitch. Prior to the 20th century, the term asphaltum was in general use. The word derives from the Ancient Greek word ἄσφαλτος (ásphaltos), which referred to natural bitumen or pitch. The largest natural deposit of bitumen in the world is the Pitch Lake of southwest Trinidad, which is estimated to contain 10 million tons.

About 70% of annual bitumen production is destined for road construction, its primary use. In this application, bitumen is used to bind aggregate particles like gravel and forms a substance referred to as asphalt concrete, which is colloquially termed asphalt. Its other main uses lie in bituminous waterproofing products, such as roofing felt and roof sealant.

View the full Wikipedia page for Bitumen
↑ Return to Menu

Dead Sea in the context of Linen

Linen (/ˈlɪnən/) is a textile made from the fibers of the flax plant.

Linen is very strong and absorbent, and it dries faster than cotton. Because of these properties, linen is comfortable to wear in hot weather and is valued for use in garments. Linen textiles can be made from flax plant fiber, yarn, as well as woven and knitted. Linen also has other distinctive characteristics, such as its tendency to wrinkle. It takes significantly longer to harvest than a material like cotton, although both are natural fibers. It is also more difficult to weave than cotton.

View the full Wikipedia page for Linen
↑ Return to Menu

Dead Sea in the context of Below sea level

This is a list of places on land below mean sea level.

Places artificially created such as tunnels, mines, basements, and dug holes, or places under water, or existing temporarily as a result of ebbing of sea tide etc., are not included. Places where seawater and rainwater is pumped away are included. Fully natural places below sea level require a dry climate; otherwise, rain would exceed evaporation and fill the area.

View the full Wikipedia page for Below sea level
↑ Return to Menu

Dead Sea in the context of Dead Sea Scrolls

The Dead Sea Scrolls, in the narrow sense identical with the Qumran Caves Scrolls, are a set of ancient Jewish manuscripts from the Second Temple period. They were discovered over a period of ten years, between 1946 and 1956, at the Qumran Caves near Ein Feshkha in the West Bank, on the northern shore of the Dead Sea. Dating from the 3rd century BCE to the 1st century CE, the Dead Sea Scrolls include the oldest surviving manuscripts of entire books later included in the biblical canons, including deuterocanonical manuscripts from late Second Temple Judaism and extrabiblical books. At the same time, they cast new light on the emergence of Christianity and of Rabbinic Judaism. In the wider sense, the Dead Sea Scrolls also include similar findings from elsewhere in the Judaean Desert, of which some are from later centuries. Almost all of the 15,000 scrolls and scroll fragments are held in the Shrine of the Book at the Israel Museum located in Jerusalem.

The Israeli government's custody of the Dead Sea Scrolls is disputed by Jordan and the Palestinian Authority on territorial, legal, and humanitarian grounds—they were mostly discovered following the Jordanian annexation of the West Bank and were acquired by Israel after Jordan lost the 1967 Arab–Israeli War—whilst Israel's claims are primarily based on historical and religious grounds, given their significance in Jewish history and in the heritage of Judaism.

View the full Wikipedia page for Dead Sea Scrolls
↑ Return to Menu

Dead Sea in the context of Judaean Desert

The Judaean Desert or Judean Desert (Hebrew: מִדְבַּר יְהוּדָה, romanizedMidbar Yehuda, Arabic: برية الخليل, romanizedBariyat al-Khalil) is a desert in the West Bank and Israel that stretches east of the ridge of the Judaean Mountains and in their rain shadow, so east of Jerusalem, and descends to the Dead Sea.

The Judaean Desert has historically functioned as a place of refuge for rebels and displaced populations. According to the Hebrew Bible, David took shelter there while fleeing from King Saul. The Hasmonean rulers of Judaea, and their successor, Herod the Great, built several monumental fortresses in the region, including Herodium, Hyrcania, and Masada. In the period of the Jewish–Roman Wars, the desert became a key theater of conflict, with Roman forces besieging major strongholds. Caves in the area, such as the Cave of Letters and the Cave of Horrors, later served as hiding places for Jewish refugees, preserving personal documents, religious texts, skeletons, weapons, clothing, and household items—thanks to the region's arid climate. The desert also attracted religious sects, including the classical-era Jewish ascetics of Qumran (likely Essenes) and Byzantine-era Christian monks who practiced spiritual isolation in local lavras.

View the full Wikipedia page for Judaean Desert
↑ Return to Menu