place

Geulei Teiman

1948 establishments in IsraelHefer Valley Regional CouncilMoshavimPopulated places established in 1948Populated places in Central District (Israel)
Religious Israeli communitiesYemeni-Jewish culture in Israel
Ge'ule Teman haMeyasdim st 01
Ge'ule Teman haMeyasdim st 01

Geulei Teiman (Hebrew: גְּאֻלֵי תֵּימָן or גאולי תימן‎, lit. The Redeemed of Yemen) is a religious moshav in central Israel. Located near Hadera in the Sharon plain, it falls under the jurisdiction of Hefer Valley Regional Council. In 2021 it had a population of 358.

Excerpt from the Wikipedia article Geulei Teiman (License: CC BY-SA 3.0, Authors, Images).

Geulei Teiman
HaMeyasdim, Emek Hefer Regional Council

Geographical coordinates (GPS) Address Nearby Places
placeShow on map

Wikipedia: Geulei TeimanContinue reading on Wikipedia

Geographical coordinates (GPS)

Latitude Longitude
N 32.392222222222 ° E 34.901666666667 °
placeShow on map

Address

המייסדים

HaMeyasdim
4020000 Emek Hefer Regional Council
Center District, Israel
mapOpen on Google Maps

Ge'ule Teman haMeyasdim st 01
Ge'ule Teman haMeyasdim st 01
Share experience

Nearby Places

Sharon Escarpment
Sharon Escarpment

The Sharon Escarpment or Sharon Cliff is the escarpment in Israel that connects the level of the coastal plain with the level of the Mediterranean Sea beach and the continental shelf and stretches along the Sharon coastal ridge approximately between Giv'at Olga and Tel Aviv, i.e., along the Sharon plain.The escarpment is up to 45m in height, of steepness 75-90°. Both the ridge and the escarpment are composed of alternating layers of kurkar (the local variety of sandstone) and loose palaeosol. The escarpment gradually moves eastward due to collapsing and slumping seawards. The separated slabs of kurkar slide downwards and crumble completely into fans of sand, swashed away by waves. The catchment area of the escarpment is visibly eroded by runoff, but this erosion is negligible compared to rockslides and slumps.The escarpment is threatened by road building, sand quarrying, drainage, slope grading, and other uncontrolled tampering with the topography. Coastal erosion of the Israeli coastal plain endangers ancient cities, such as Ashkelon, Yavne-Yam, Jaffa, Apollonia–Arsuf, Caesarea, Atlit, Akko and Achziv.The ridge was formed during the Late Pleistocene and the cliff developed when at about 7,500 years Before Present (BP) the sea level reached the western edge of the current ridge. Now this edge is at about 8 m. below the sea level. Galil and Zviely suggest that over these 7,500 years the cliff retreated for about 730m, i.e., at the rate about 9.7 cm. per year.

Battle of Megiddo (1918)
Battle of Megiddo (1918)

The Battle of Megiddo was fought between 19 and 25 September 1918, on the Plain of Sharon, in front of Tulkarm, Tabsor and Arara in the Judean Hills as well as on the Esdralon Plain at Nazareth, Afulah, Beisan, Jenin and Samakh. Its name, which has been described as "perhaps misleading" since very limited fighting took place near Tel Megiddo, was chosen by British commander Edmund Allenby for its biblical and symbolic resonance. The battle was the final Allied offensive of the Sinai and Palestine Campaign of World War I. The contending forces were the Allied Egyptian Expeditionary Force, of three corps including one of mounted troops, and the Ottoman Yildirim Army Group which numbered three armies, each the strength of barely an Allied corps. The series of battles took place in what was then the central and northern parts of Ottoman Palestine and parts of present-day Israel, Syria and Jordan. After forces of the Arab Revolt attacked the Ottoman lines of communication, distracting the Ottomans, British and Indian infantry divisions attacked and broke through the Ottoman defensive lines in the sector adjacent to the coast in the set-piece Battle of Sharon. The Desert Mounted Corps rode through the breach and almost encircled the Ottoman Seventh and Eighth armies still fighting in the Judean Hills. The subsidiary Battle of Nablus was fought virtually simultaneously in the Judean Hills in front of Nablus and at crossings of the Jordan River. The Ottoman Fourth Army was subsequently attacked in the Hills of Moab at Es Salt and Amman. These battles resulted in many tens of thousands of prisoners and many miles of territory being captured by the Allies. Following the battles, Daraa was captured on 27 September, Damascus on 1 October and operations at Haritan, north of Aleppo, were still in progress when the Armistice of Mudros was signed ending hostilities between the Allies and Ottomans. The operations of General Edmund Allenby, the British commander of the Egyptian Expeditionary Force, achieved decisive results at comparatively little cost, in contrast to many offensives during the First World War. Allenby achieved this through the use of creeping barrages to cover set-piece infantry attacks to break a state of trench warfare and then use his mobile forces (cavalry, armoured cars and aircraft) to encircle the Ottoman armies' positions in the Judean Hills, cutting off their lines of retreat. The irregular forces of the Arab Revolt also played a part in this victory.