Plain Of Esdraelon
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Plain Of Esdraelon
The Jezreel Valley (from the he, עמק יזרעאל, translit. ''ʿĒmeq Yīzrəʿēʿl''), or Marj Ibn Amir ( ar, مرج ابن عامر), also known as the Valley of Megiddo, is a large fertile plain and inland valley in the Northern District of Israel. It is bordered to the north by the highlands of the Lower Galilee region, to the south by the Samarian highlands, to the west and northwest by the Mount Carmel range, and to the east by the Jordan Valley, with Mount Gilboa marking its southern extent. The largest settlement in the valley is the city of Afula, which lies near its center. Etymology The Jezreel Valley takes its name from the ancient city of Jezreel (known in Hebrew as Yizre'el; ; known in Arabic as Zir'ēn, ) which was located on a low hill overlooking the southern edge of the valley. The word ''Jezreel'' comes from the Hebrew, and means "God sows" or " El sows".Cheyne and Black, ''Encyclopedia Biblica'' The phrase "valley of Jezreel" was sometimes used ...
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Tel Megiddo
Tel Megiddo ( he, תל מגידו; ar, مجیدو, Tell el- Mutesellim, ''lit.'' "Mound of the Governor"; gr, Μεγιδδώ, Megiddo) is the site of the ancient city of Megiddo, the remains of which form a tell (archaeological mound), situated in northern Israel near Kibbutz Megiddo, about 30 km south-east of Haifa. Megiddo is known for its historical, geographical, and theological importance, especially under its Greek name Armageddon. During the Bronze Age, Megiddo was an important Canaanite city-state and during the Iron Age, a royal city in the Kingdom of Israel. Megiddo drew much of its importance from its strategic location at the northern end of the Wadi Ara defile, which acts as a pass through the Carmel Ridge, and from its position overlooking the rich Jezreel Valley from the west. Excavations have unearthed 20 strata of ruins since the Neolithic phase, indicating a long period of settlement. The site is now protected as Megiddo National Park and is a Worl ...
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Midian
Midian (; he, מִדְיָן ''Mīḏyān'' ; ar, مَدْيَن, Madyan; grc-gre, Μαδιάμ, ''Madiam'') is a geographical place mentioned in the Hebrew Bible and Quran. William G. Dever states that biblical Midian was in the "northwest Arabian Peninsula, on the east shore of the Gulf of Aqaba on the Red Sea", an area which he notes was "never extensively settled until the 8th–7th century B.C." According to the Book of Genesis, the Midianites were the descendants of Midian, who was a son of Abraham and his wife Keturah: "Abraham took a wife, and her name was Keturah. And she bare him Zimran, and Jokshan, and Medan, and Midian, and Ishbak, and Shuah" (Genesis 25:1–2, King James Version). Neither Midian's nor the Midianites' existence are attested in antiquity outside of Biblical sources. Land or tribal league? Some scholars have suggested that the name "Midian" does not refer to geographic places or to a specific tribe, but to a confederation or "league" of tribes br ...
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Gideon
Gideon (; ) also named Jerubbaal and Jerubbesheth, was a military leader, judge and prophet whose calling and victory over the Midianites are recounted in of the Book of Judges in the Hebrew Bible. Gideon was the son of Joash, from the Abiezrite clan in the tribe of Manasseh and lived in Ephra (Ophrah). As a leader of the Israelites, he won a decisive victory over a Midianite army despite a vast numerical disadvantage, leading a troop of 300 "valiant" men. Archaeologists in southern Israel have found a 3,100-year-old fragment of a jug with five letters written in ink that appear to represent the name Jerubbaal, or Yeruba'al. Names The nineteenth-century Strong's Concordance derives the name "Jerubbaal" from "Baal will contend", in accordance with the folk etymology, given in . According to biblical scholar Lester Grabbe (2007), " udges6.32 gives a nonsensical etymology of his name; it means something like 'Let Baal be great. Likewise, where Strong gave the meaning "hewer" ...
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Israelites
The Israelites (; , , ) were a group of Semitic-speaking tribes in the ancient Near East who, during the Iron Age, inhabited a part of Canaan. The earliest recorded evidence of a people by the name of Israel appears in the Merneptah Stele of ancient Egypt, dated to about 1200 BCE. According to the modern archaeological account, the Israelites and their culture branched out of the Canaanite peoples and their cultures through the development of a distinct monolatristic—and later monotheistic—religion centred on the national god Yahweh.Mark Smith in "The Early History of God: Yahweh and Other Deities of Ancient Israel" states "Despite the long regnant model that the Canaanites and Israelites were people of fundamentally different culture, archaeological data now casts doubt on this view. The material culture of the region exhibits numerous common points between Israelites and Canaanites in the Iron I period (c. 1200–1000 BCE). The record would suggest that the Isra ...
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Hebrew Bible
The Hebrew Bible or Tanakh (;"Tanach"
''Random House Webster's Unabridged Dictionary''.
Hebrew: ''Tānāḵh''), also known in Hebrew as Miqra (; Hebrew: ''Mīqrā''), is the Biblical canon, canonical collection of Hebrew language, Hebrew scriptures, including the Torah, the Nevi'im, and the Ketuvim. Different branches of Judaism and Samaritanism have maintained different versions of the canon, including the 3rd-century Septuagint text used by Second-Temple Judaism, the Syriac language Peshitta, the Samaritan Torah, the Dead Sea Scrolls, and most recently the 10th century medieval Masoretic Text, Masoretic text created by the Masoretes currently used in modern Rabbinic Judaism. The terms "Hebrew Bible" or "Hebrew Canon" are frequently confused with the Masoretic text, however, this is a medieval version and one of several ...
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Fresh Water
Fresh water or freshwater is any naturally occurring liquid or frozen water containing low concentrations of dissolved salts and other total dissolved solids. Although the term specifically excludes seawater and brackish water, it does include non- salty mineral-rich waters such as chalybeate springs. Fresh water may encompass frozen and meltwater in ice sheets, ice caps, glaciers, snowfields and icebergs, natural precipitations such as rainfall, snowfall, hail/ sleet and graupel, and surface runoffs that form inland bodies of water such as wetlands, ponds, lakes, rivers, streams, as well as groundwater contained in aquifers, subterranean rivers and lakes. Fresh water is the water resource that is of the most and immediate use to humans. Water is critical to the survival of all living organisms. Many organisms can thrive on salt water, but the great majority of higher plants and most insects, amphibians, reptiles, mammals and birds need fresh water to survive. Fresh ...
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Salinity
Salinity () is the saltiness or amount of salt dissolved in a body of water, called saline water (see also soil salinity). It is usually measured in g/L or g/kg (grams of salt per liter/kilogram of water; the latter is dimensionless and equal to ‰). Salinity is an important factor in determining many aspects of the chemistry of natural waters and of biological processes within it, and is a thermodynamic state variable that, along with temperature and pressure, governs physical characteristics like the density and heat capacity of the water. A contour line of constant salinity is called an ''isohaline'', or sometimes ''isohale''. Definitions Salinity in rivers, lakes, and the ocean is conceptually simple, but technically challenging to define and measure precisely. Conceptually the salinity is the quantity of dissolved salt content of the water. Salts are compounds like sodium chloride, magnesium sulfate, potassium nitrate, and sodium bicarbonate which dissolve into ions ...
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Surface Water
Surface water is water located on top of land forming terrestrial (inland) waterbodies, and may also be referred to as ''blue water'', opposed to the seawater and waterbodies like the ocean. The vast majority of surface water is produced by precipitation. As the climate warms in the spring, snowmelt runs off towards nearby streams and rivers contributing towards a large portion of human drinking water. Levels of surface water lessen as a result of evaporation as well as water moving into the ground becoming ground-water. Alongside being used for drinking water, surface water is also used for irrigation, wastewater treatment, livestock, industrial uses, hydropower, and recreation. For USGS water-use reports, surface water is considered freshwater when it contains less than 1,000 milligrams per liter (mg/L) of dissolved solids. There are three major types of surface water. Permanent (perennial) surface waters are present year round, and includes lakes, rivers and wetlands (marshe ...
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Precipitation (meteorology)
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers. Moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condense ...
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Evaporation
Evaporation is a type of vaporization that occurs on the surface of a liquid as it changes into the gas phase. High concentration of the evaporating substance in the surrounding gas significantly slows down evaporation, such as when humidity affects rate of evaporation of water. When the molecules of the liquid collide, they transfer energy to each other based on how they collide. When a molecule near the surface absorbs enough energy to overcome the vapor pressure, it will escape and enter the surrounding air as a gas. When evaporation occurs, the energy removed from the vaporized liquid will reduce the temperature of the liquid, resulting in evaporative cooling. On average, only a fraction of the molecules in a liquid have enough heat energy to escape from the liquid. The evaporation will continue until an equilibrium is reached when the evaporation of the liquid is equal to its condensation. In an enclosed environment, a liquid will evaporate until the surrounding air is ...
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Jordan Rift Valley
The Jordan Rift Valley, also Jordan Valley ''Bīrʿāt haYardēn'', ar, الغور Al-Ghor or Al-Ghawr),, date=November 2022 also called the Syro-African Depression, is an elongated depression located in modern-day Israel, and Jordan. This geographic region includes the entire length of the Jordan River – from its sources, through the Hula Valley, the Korazim block, the Sea of Galilee, the (Lower) 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. History and physical features The Jordan Rift Valley was formed many millions of years ago in the Miocene epoch (23.8 – 5.3 Myr ago) when the Arabian Plate moved northward and then eastward away from Africa. One million years later, the land between the Mediterranean and the Jordan Rift Valley rose so that the sea water sto ...
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