|
Mount Olivet
The Mount of Olives or Mount Olivet ( he, הַר הַזֵּיתִים, Har ha-Zeitim; ar, جبل الزيتون, Jabal az-Zaytūn; both lit. 'Mount of Olives'; in Arabic also , , 'the Mountain') is a mountain ridge east of and adjacent to Jerusalem's Old City. It is named for the olive groves that once covered its slopes. The southern part of the mount was the Silwan necropolis, attributed to the elite of the ancient Kingdom of Judah. The mount has been used as a Jewish cemetery for over 3,000 years and holds approximately 150,000 graves, making it central in the tradition of Jewish cemeteries. Several key events in the life of Jesus, as related in the Gospels, took place on the Mount of Olives, and in the Acts of the Apostles it is described as the place from which Jesus ascended to heaven. Because of its association with both Jesus and Mary, the mount has been a site of Christian worship since ancient times and is today a major site of pilgrimage for Catholics, the E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jerusalem
Jerusalem (; he, יְרוּשָׁלַיִם ; ar, القُدس ) (combining the Biblical and common usage Arabic names); grc, Ἱερουσαλήμ/Ἰεροσόλυμα, Hierousalḗm/Hierosóluma; hy, Երուսաղեմ, Erusałēm. is a city in Western Asia. Situated on a plateau in the Judaean Mountains between the Mediterranean Sea, Mediterranean and the Dead Sea, it is one of the List of oldest continuously inhabited cities, oldest cities in the world and is considered to be a holy city for the three major Abrahamic religions: Judaism, Christianity, and Islam. Both Israelis and Palestinians claim Jerusalem as their Capital city, capital, as Israel maintains its primary governmental institutions there and the State of Palestine ultimately foresees it as its seat of power. Because of this dispute, Status of Jerusalem, neither claim is widely recognized internationally. Throughout History of Jerusalem, its long history, Jerusalem has been destroyed at least twice, Sie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Jerusalem
East Jerusalem (, ; , ) is the sector of Jerusalem that was held by Jordan during the 1948 Arab–Israeli War, as opposed to the western sector of the city, West Jerusalem, which was held by Israel. Jerusalem was envisaged as a separate, international city under the 1947 United Nations partition plan. It was, however, divided by the 1948 war that followed Israel's declaration of independence. As a result of the 1949 Armistice Agreements, the city's western half came under Israeli control, while its eastern half, containing the famed Old City, fell under Jordanian control. Israel occupied East Jerusalem during the 1967 Six-Day War; since then, the entire city has been under Israeli control. The 1980 Jerusalem Law declared unified Jerusalem the capital of Israel, formalizing the effective annexation of East Jerusalem. Palestinians and many in the international community consider East Jerusalem to be the future capital of the State of Palestine. This includes (out of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock-cut Tombs In Ancient Israel
Rock-cut tombs were a form of burial and interment chamber used in ancient Israel. Cut into the landscapes surrounding ancient Judean cities, their design ranges from single chambered, with simple square or rectangular layouts, to multi-chambered with more complex designs. Almost all burial chambers contain a platform for primary burial and an ossuary or other receptacle for secondary burial. There is debate on if these tombs were originally intended for secondary burials, or if that practice arose later. The use of rock-cut cave tombs in the region began in the early Canaanite period, from 3100–2900 BCE. The custom lapsed a millennium, however, before re-emerging in the earliest Israelite tombs, dating to the 9th century BCE in Jerusalem. The use of rock-cut tombs reached its peak in the 7th and 8th centuries BCE, before rapidly declining and eventually falling out of use in the 6th century BCE in some regions. Use of the tombs has been recorded as recently as the late Roman ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quarry
A quarry is a type of open-pit mine in which dimension stone, rock, construction aggregate, riprap, sand, gravel, or slate is excavated from the ground. The operation of quarries is regulated in some jurisdictions to reduce their environmental impact. The word ''quarry'' can also include the underground quarrying for stone, such as Bath stone. Types of rock Types of rock extracted from quarries include: *Chalk *China clay *Cinder *Clay *Coal * Construction aggregate (sand and gravel) * Coquina * Diabase *Gabbro *Granite * Gritstone *Gypsum *Limestone *Marble *Ores *Phosphate rock *Quartz *Sandstone * Slate *Travertine Stone quarry Stone quarry is an outdated term for mining construction rocks (limestone, marble, granite, sandstone, etc.). There are open types (called quarries, or open-pit mines) and closed types ( mines and caves). For thousands of years, only hand tools had been used in quarries. In the 18th century, the use of drilling and blasting operatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flint
Flint, occasionally flintstone, is a sedimentary cryptocrystalline form of the mineral quartz, categorized as the variety of chert that occurs in chalk or marly limestone. Flint was widely used historically to make stone tools and start fires. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones.''The Flints from Portsdown Hill'' Inside the nodule, flint is usually dark grey, black, green, white or brown in colour, and often has a glassy or waxy appearance. A thin layer on the outside of the nodules is usually different in colour, typically white and rough in texture. The nodules can often be found along s and |
Chalk
Chalk is a soft, white, porous, sedimentary carbonate rock. It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor. Chalk is common throughout Western Europe, where deposits underlie parts of France, and steep cliffs are often seen where they meet the sea in places such as the Dover cliffs on the Kent coast of the English Channel. Chalk is mined for use in industry, such as for quicklime, bricks and builder's putty, and in agriculture, for raising pH in soils with high acidity. It is also used for " blackboard chalk" for writing and drawing on various types of surfaces, although these can also be manufactured from other carbonate-based minerals, or gypsum. Description Chalk is a fine-textured, earthy type of limestone distinguished by its light color, softness, and high porosity. It is composed mostly of tiny fragments of the calcite shells or skeletons ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Late Cretaceous
The Late Cretaceous (100.5–66 Ma) is the younger 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, Australia and Ant ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Judean Desert
The Judaean Desert or Judean Desert ( he, מִדְבַּר יְהוּדָה, Midbar Yehuda}, both ''Desert of Judah'' or ''Judaean Desert''; ar, صحراء يهودا, Sahraa' Yahuda) is a desert in Palestine and Israel that lies east of Jerusalem and descends to the Dead Sea. Under the name El-Bariyah, it has been nominated to the Tentative List of World Heritage Sites in the State of Palestine, particularly for its monastic ruins. Etymology The term he, מִדְבַּר יְהוּדָה, , Desert of Judaea originates in the Hebrew Bible, and it is mentioned in Judges and Psalms. It is sometimes known as he2, יְשִׁימוֹן ''Yeshimon'', meaning ''desert'' or ''wildland'', or yet ''Wilderness of Judah'' or ''Wilderness of Judaea'', among others. Geography The Judaean Desert lies east of Jerusalem and descends to the Dead Sea. The Judaean Desert stretches from the northeastern Negev to the east of Beit El, and is marked by natural terraces with escarpments. It en ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Scopus
Mount Scopus ( he, הַר הַצּוֹפִים ', "Mount of the Watchmen/ Sentinels"; ar, جبل المشارف ', lit. "Mount Lookout", or ' "Mount of the Scene/Burial Site", or ) is a mountain (elevation: above sea level) in northeast Jerusalem. Between the 1948 Arab–Israeli War and the Six-Day War in 1967, the peak of Mount Scopus with the Hebrew University campus and Hadassah Hospital was a UN-protected Israeli exclave within Jordanian-administered territory. Today, Mount Scopus lies within the municipal boundaries of the city of Jerusalem. Name and identification The ridge of mountains east of ancient as well as modern Jerusalem offers the best views of the city, which it dominates. Since the main part of the ridge bears the name Mount of Olives, the name "lookout" was reserved for this peak to the northeast of the ancient city. Its name in many languages (Hebrew, Arabic, Greek and Latin) means "lookout." Scopus is a Latinisation of the Greek word for "watcher", ''s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley Of Josaphat
The Valley of Josaphat (variants: Valley of Jehoshaphat and Valley of Yehoshephat) is a Biblical place mentioned by name in the Book of Joel ( and ): "I will gather together all nations, and will bring them down into the valley of Josaphat: "Then I will enter into judgment with them there", on behalf of my people and for My inheritance Israel, whom they have scattered among the nations and they have divided up My land."; "Let the nations be roused; Let the nations be aroused And come up to the Valley of Jehoshaphat, for there I will sit to judge all the nations on every side". This location is also referred to as the Valley of Decision. Identification In the Judaean Desert near Teqo'a By one interpretation, this describes the place where, in the presence of Jehoshaphat (Josaphat), King of Judah, Yahweh annihilated the Gentile coalition of Moab, Ammon and Edom. This may have indicated an actual valley euphemistically called by the Jews ''êmêq Berâkâh'' ("valley of blessing"), s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
%2C_Western_Negev%2C_Israel.jpg "Click for more on -> Chalk")
