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Shephelah
The Shephelah or Shfela, lit. "lowlands" ( hbo, הַשְּפֵלָה ''hašŠǝfēlā'', also Modern Hebrew: , ''Šǝfēlat Yəhūda'', the "Judaean foothills"), is a transitional region of soft-sloping rolling hills in south-central Israel stretching over between the Judaean Mountains and the Coastal Plain. The different use of the term "Judean Plain", as either defining just the Coastal Plain segment stretching along the Judaean Mountains, or also including, or only referring to, the Shfela, often creates grave confusion. Today the Shfela is largely rural with many farms, but the cities of Ashdod, Ashkelon, Rehovot, Beit Shemesh, and Kiryat Gat roughly surround it. The Bible assigned land in the Shfela to the tribes of Judah and Dan. Biblical references The Shfela is mentioned many times in the Hebrew Bible. (In the King James Version, the Hebrew term "Shfela" tends to be translated as "vale" or "valley.") The Shfela was the site of many biblical battles. During the Ba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
HaShfela
The Shephelah or Shfela, lit. "lowlands" ( hbo, הַשְּפֵלָה ''hašŠǝfēlā'', also Modern Hebrew: , ''Šǝfēlat Yəhūda'', the "Judaean foothills"), is a transitional region of soft-sloping rolling hills in south-central Israel stretching over between the Judaean Mountains and the Coastal Plain. The different use of the term "Judean Plain", as either defining just the Coastal Plain segment stretching along the Judaean Mountains, or also including, or only referring to, the Shfela, often creates grave confusion. Today the Shfela is largely rural with many farms, but the cities of Ashdod, Ashkelon, Rehovot, Beit Shemesh, and Kiryat Gat roughly surround it. The Bible assigned land in the Shfela to the tribes of Judah and Dan. Biblical references The Shfela is mentioned many times in the Hebrew Bible. (In the King James Version, the Hebrew term "Shfela" tends to be translated as "vale" or "valley.") The Shfela was the site of many biblical battles. During the Bar K ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tribe Of Judah
According to the Hebrew Bible, the tribe of Judah (, ''Shevet Yehudah'') was one of the twelve Tribes of Israel, named after Judah, the son of Jacob. Judah was the first tribe to take its place in the Land of Israel, occupying the southern part of the territory. Jesse and his sons, including King David, belonged to this tribe. Biblical account The tribe of Judah, its conquests, and the centrality of its capital in Jerusalem for the worship of the god Yahweh figure prominently in the Deuteronomistic history, encompassing the books of Deuteronomy through II Kings, which most scholars agree was reduced to written form, although subject to exilic and post-exilic alterations and emendations, during the reign of the Judahite reformer Josiah from 641–609 BCE. According to the account in the Book of Joshua, following a partial conquest of Canaan by the Israelite tribes (the Jebusites still held Jerusalem),Kitchen, Kenneth A. (2003), ''On the Reliability of the Old Testament'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Judaean Mountains
The Judaean Mountains, or Judaean Hills ( he, הרי יהודה, translit=Harei Yehuda) or the Hebron Mountains ( ar, تلال الخليل, translit=Tilal al-Khalīl, links=, lit=Hebron Mountains), is a mountain range in Palestine and Israel where Jerusalem, Hebron and several other biblical cities are located. The mountains reach a height of . The Judean Mountains can be separated to a number of sub-regions, including the Mount Hebron ridge, the Jerusalem ridge and the Judean slopes. The Judaean Mountains formed the heartland of the Kingdom of Judah (930-586 BCE), where the earliest Jewish settlements emerged, and from which Jews are generally descended. Geography The Judaean mountains are part of a more extended range that runs in a north-south direction. The ridge consists of the Samarian Hills in its northern part, and of the Judaean mountains in its southern part, the two segments meeting at the latitude of Ramallah. The westward descent from the hard limestone country of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tribe Of Dan
The Tribe of Dan (, "Judge") was one of the twelve tribes of Israel, according to the Torah. They were allocated a coastal portion of land when the people of Israel entered the Promised Land, later moving northwards. Biblical narrative In the Biblical census of the Book of Numbers, the tribe of Dan is portrayed as the second largest Israelite tribe (after Judah). Some textual scholars regard the census as being from the Priestly Source, dating it to around the 7th century BC, and more likely to reflect the biases of its authors.Richard Elliott Friedman, '' Who Wrote the Bible?'' (Harper San Francisco) (1987) In the ''Blessing of Moses'', which some textual scholars regard as dating from only slightly earlier than the deuteronomist, Dan is prophesied to "leap from Bashan"; scholars are uncertain why this should be since the tribe did not live in the Bashan plain, east of the Jordan River. Conquest and territory According to the biblical narrative, following the completion of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Israeli Coastal Plain
Israeli coastal plain ( he, מישור החוף, ''Mishor HaḤof'') is the coastal plain along Israel's Mediterranean Sea coast, extending north to south. It is a geographical region defined morphologically by the sea, in terms of topography and soil, and also in its climate, flora and fauna. It is narrow in the north and broadens considerably towards the south, and is continuous with the exception of the short section where Mount Carmel reaches almost all the way to the sea. The Coastal Plain is bordered to the east by – north to south – the topographically higher regions of the Galilee, the low and flat Jezreel Valley, the Carmel range, the mountains of Samaria, the hill country of Judea known as the Shephelah, and the Negev Mountains in the south. To the north it is separated from the coastal plain of Lebanon by the cliffs of Rosh HaNikra, which jut out into the sea from the Galilee mountains, but to the south it continues into the Egyptian Sinai Peninsula. The plain c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marl
Marl is an earthy material rich in carbonate minerals, clays, and silt. When hardened into rock, this becomes marlstone. It is formed in marine or freshwater environments, often through the activities of algae. Marl makes up the lower part of the cliffs of Dover, and the Channel Tunnel follows these marl layers between France and the United Kingdom. Marl is also a common sediment in post-glacial lakes, such as the marl ponds of the northeastern United States. Marl has been used as a soil conditioner and neutralizing agent for acid soil and in the manufacture of cement. Description Marl or marlstone is a carbonate-rich mud or mudstone which contains variable amounts of clays and silt. The term was originally loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions. These typically contain 35–65% clay and 65–35% carbonate. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calcrete
Caliche () is a sedimentary rock, a hardened natural cement of calcium carbonate that binds other materials—such as gravel, sand, clay, and silt. It occurs worldwide, in aridisol and mollisol soil orders—generally in arid or semiarid regions, including in central and western Australia, in the Kalahari Desert, in the High Plains of the western United States, in the Sonoran Desert, Chihuahuan Desert and Mojave Desert of North America, and in eastern Saudi Arabia at Al-Hasa. Caliche is also known as calcrete or kankar (in India). It belongs to the duricrusts. The term ''caliche'' is Spanish and is originally from the Latin ''calx'', meaning lime. Caliche is generally light-colored, but can range from white to light pink to reddish-brown, depending on the impurities present. It generally occurs on or near the surface, but can be found in deeper subsoil deposits, as well. Layers vary from a few inches to feet thick, and multiple layers can exist in a single location. A calich ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bar Kokhba Revolt
The Bar Kokhba revolt ( he, , links=yes, ''Mereḏ Bar Kōḵḇāʾ''), or the 'Jewish Expedition' as the Romans named it ( la, Expeditio Judaica), was a rebellion by the Jews of the Roman province of Judea, led by Simon bar Kokhba, against the Roman Empire. Fought CE, it was the last of three major Jewish–Roman wars, so it is also known as the Third Jewish–Roman War or, the Third Jewish Revolt. Some historians also refer to it as the Second Revolt of Judea, not counting the Kitos War (115–117 CE), which had only marginally been fought in Judea. The revolt erupted as a result of religious and political tensions in Judea following on the failed First Revolt in 66–73 CE. These tensions were related to the establishment of a large Roman military presence in Judea, changes in administrative life and the economy, together with the outbreak and suppression of Jewish revolts from Mesopotamia to Libya and Cyrenaica. The proximate reasons seem to be the constructi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', "dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope 13C in the atmosphere was exceptionally low in comparison with the more common isotope 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Siberia and in what is now Chesapeake Bay. As with other geologic periods, the strata that define the start ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now- extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
%2C_Western_Negev%2C_Israel.jpg "Click for more on -> Chalk")
