Mount Carmel
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Mount Carmel
Mount Carmel (; ), also known in Arabic as Mount Mar Elias (; ), is a coastal mountain range in northern Israel stretching from the Mediterranean Sea towards the southeast. The range is a UNESCO biosphere reserve. A number of towns are situated there, most notably Haifa, Israel's third largest city, located on the northern and western slopes. Etymology The word ''karmel'' ("garden-land") has been explained as a compound of ''kerem'' and ''el'' meaning "vineyard of El (deity), God" or a clipping of ''kar male,'' meaning "full kernel." Martin Jan Mulder suggested a third etymology, that of ''kerem + l'' with a lamed wiktionary:sufformative, sufformative, meaning only "vineyard", but this is considered unlikely as evidence for the existence of a lamed sufformative is weak. In Song of Songs 7:6, ''karmel'' is generally interpreted as a color, perhaps "crimson" or "yellow". suggests connecting it to the yellow "''karmel'' lily" mentioned by the Jerusalem Talmudy. Sukkah 3:6) in t ...
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Kibbutz
A kibbutz ( / , ; : kibbutzim / ) is an intentional community in Israel that was traditionally based on agriculture. The first kibbutz, established in 1910, was Degania Alef, Degania. Today, farming has been partly supplanted by other economic branches, including Factory, industrial plants and high-tech Business, enterprises. Kibbutzim began as utopian communities, a combination of socialism and Zionism. In recent decades, some kibbutzim have been Privatization, privatized and changes have been made in the communal lifestyle. A member of a kibbutz is called a ''kibbutznik'' ( / ; plural ''kibbutznikim'' or ''kibbutzniks''), the suffix ''-nik'' being of Slavic languages, Slavic origin. In 2010, there were 270 kibbutzim in Israel with a total population of 126,000. Their factories and farms account for 9% of Israel's industrial output, worth US$8 billion, and 40% of its agricultural output, worth over US$1.7 billion. Some kibbutzim had also developed substantial high-tech and mi ...
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Jerusalem Talmud
The Jerusalem Talmud (, often for short) or Palestinian Talmud, also known as the Talmud of the Land of Israel, is a collection of rabbinic notes on the second-century Jewish oral tradition known as the Mishnah. Naming this version of the Talmud after Palestine or the Land of Israelrather than Jerusalemis considered more accurate, as the text originated mainly from Galilee in Byzantine Palaestina Secunda rather than from Jerusalem, where no Jews were allowed to live at the time. The Jerusalem Talmud predates its counterpart, the Babylonian Talmud (known in Hebrew as the ), by about a century. It was written primarily in Galilean Aramaic. It was compiled between the late fourth century to the first half of the fifth century. Both versions of the Talmud have two parts, the Mishnah (of which there is only one version), which was finalized by Judah ha-Nasi around the year 200 CE, and either the Babylonian or the Jerusalem Gemara. The Gemara is what differentiates the Jerusalem ...
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Yokneam Illit
Yokneam Illit (), also Yoqne'am Illit, is a city in the Northern District of Israel. It is located in a hilly region of the Lower Galilee at the base of the Carmel Mountains, and overlooks the Jezreel Valley. It is from Haifa and from Tel Aviv. Yokneam Illit, known as Israel's "Startup Village", is home to a high-tech hub surrounded by forests and small communities. In it had a population of . Yokneam Illit was founded in 1950. It was recognized as a local council in 1967 and achieved city status in 2007. It is located on the route of Israel's major highways – Highway 70 and Highway 6. In 1989, after Simon Alfassi was elected mayor, Yokneam Illit began to attract high-tech companies looking for an alternative to Gush Dan. Over 100 high-tech companies now operate from Yokneam Illit, generating exports of approximately 5 billion US dollars annually. Although real estate prices are low relative to the Gush Dan area, the high rate of growth has pushed prices up faster ...
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Lauraceae
Lauraceae, or the laurels, is a plant Family (biology), family that includes the bay laurel, true laurel and its closest relatives. This family comprises about 2850 known species in about 45 genus (biology), genera worldwide. They are dicotyledons, and occur mainly in warm temperate and tropical regions, especially Southeast Asia and South America. Many are aromatic evergreen trees or shrubs, but some, such as ''Sassafras'', are deciduous, or include both deciduous and evergreen trees and shrubs, especially in tropical and temperate climates. The genus ''Cassytha'' is unique in the Lauraceae in that its members are parasite, parasitic vines. Most laurels are highly poisonous. Overview The family has a worldwide distribution in tropical and warm climates. The Lauraceae are important components of tropical forests ranging from low-lying to Montane forest, montane. In several forested regions, Lauraceae are among the top five families in terms of the number of species present. T ...
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Olive
The olive, botanical name ''Olea europaea'' ("European olive"), is a species of Subtropics, subtropical evergreen tree in the Family (biology), family Oleaceae. Originating in Anatolia, Asia Minor, it is abundant throughout the Mediterranean Basin, with wild subspecies in Africa and western Asia; modern Cultivar, cultivars are traced primarily to the Near East, Aegean Sea, and Strait of Gibraltar. The olive is the type species for its genus, ''Olea'', and lends its name to the Oleaceae plant family, which includes species such as Syringa vulgaris, lilac, jasmine, forsythia, and Fraxinus, ash. The olive fruit is classed botanically as a drupe, similar to the cherry or peach. The term oil—now used to describe any Viscosity, viscous Hydrophobe, water-insoluble liquid—was virtually synonymous with olive oil, the Vegetable oil, liquid fat made from olives. The olive has deep historical, economic, and cultural significance in the Mediterranean; Georges Duhamel (author), George ...
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Pine
A pine is any conifer tree or shrub in the genus ''Pinus'' () of the family Pinaceae. ''Pinus'' is the sole genus in the subfamily Pinoideae. ''World Flora Online'' accepts 134 species-rank taxa (119 species and 15 nothospecies) of pines as current, with additional synonyms, and ''Plants of the World Online'' 126 species-rank taxa (113 species and 13 nothospecies), making it the largest genus among the conifers. The highest species diversity of pines is found in Mexico. Pines are widely species distribution, distributed in the Northern Hemisphere; they occupy large areas of boreal forest, but are found in many habitats, including the Mediterranean Basin, and dry tropical forests in southeast Asia and Central America. Wood from pine trees is one of the most extensively used types of timber, and some pines are widely used as Christmas trees. Description Pine trees are evergreen, coniferous resinous trees (or, rarely, shrubs) growing tall, with the majority of species reachin ...
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Pleistocene
The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek () 'most' and (; Latinized as ) 'new'. The aridification and cooling trends of the preceding Neogene were continued in the Pleistocene. The climate was strongly variable depending on the glacial cycle, oscillating between cold Glacial period, glacial periods and warmer Interglacial, int ...
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Early Cretaceous
The Early Cretaceous (geochronology, geochronological name) or the Lower Cretaceous (chronostratigraphy, chronostratigraphic name) is the earlier or lower of the two major divisions of the Cretaceous. It is usually considered to stretch from 143.1 Megaannum#SI prefix multipliers, Ma to 100.5 Ma. Geology Proposals for the exact age of the Barremian–Aptian boundary ranged from 126 to 117 Ma until recently (as of 2019), but based on drillholes in Svalbard the defining Anoxic event#Cretaceous, early Aptian Oceanic Anoxic Event 1a (OAE1a) was dated to 123.1±0.3 Ma, limiting the possible range for the boundary to c. 122–121 Ma. There is a possible link between this anoxic event and a series of Early Cretaceous large igneous provinces (LIP). The Ontong Java Plateau, Ontong Java-Manihiki Plateau, Manihiki-Hikurangi Plateau, Hikurangi large igneous province, emplaced in the South Pacific at c. 120 Ma, is by far the largest LIP in Earth's history. The Onto ...
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Late Cretaceous
The Late Cretaceous (100.5–66 Ma) is the more recent of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''creta'', the Latin word for the white limestone known as chalk. The chalk of northern France and the white cliffs of south-eastern England date from the Cretaceous Period. Climate During the Late Cretaceous, the climate was warmer than present, although throughout the period a cooling trend is evident. The tropics became restricted to equatorial regions and northern latitudes experienced markedly more seasonal climatic conditions. Geography Due to plate tectonics, the Americas were gradually moving westward, causing the Atlantic Ocean to expand. The Western Interior Seaway divided North America into eastern and western halves; Appalachia and Laramidia. India maintained a northward course towards Asia. In the Southern Hemisphere, Aus ...
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Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ...
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Jezreel Valley
The Jezreel Valley (from the ), or Marj Ibn Amir (), also known as the Valley of Megiddo, is a large fertile plain and inland valley in the Northern District (Israel), 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 (Middle East), 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. Name The Jezreel Valley takes its name from the ancient city of Jezreel (city), Jezreel (known in Hebrew as Yizre'el; ; known in Arabic as Zir'in, 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 (god), El sows".Cheyne and Black, ''Encyclopedia Biblica'' The Arabic name of the valley is Marj Bani Amir (), which ...
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Headland
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosio ...
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