|Harei Yehuda / Jibal Al Khalil|
|Elevation||1,026 m (3,366 ft)|
|Parent range||Great Rift Valley|
|Age of rock||Late Cretaceous|
|Type of rock||Terra rossa, limestone|
|Easiest route||Road of the Patriarchs (the ridge route)|
The Judaean Mountains, or Judaean Hills (Hebrew: הרי יהודה Harei Yehuda) or the Hebron Mountains (Arabic: جبال الخليل Jibal Al Khalil (lit. "The Khalil Mountains")), is a mountain range in Israel and the West Bank where Jerusalem and several other biblical cities are located. The mountains reach a height of 1,026 metres (3,366 ft). The Judean Mountains can be separated to a number of sub-regions, including the Mount Hebron ridge, the Jerusalem ridge and the Judean slopes. These mountains formed the heartland of the Kingdom of Judah, where the earliest Jewish settlements emerged.
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 the Judaean mountains towards the coastal plain is by way of a longitudinal trough of fosse cut through chalk, followed by the low, rolling soft limestone hills of the Shephelah, while eastwards the landscape falls steeply towards the Jordan Rift Valley. The southern end of the mountain range is at Beersheba in the northern part of the Negev, where the mountains slope down into the Beersheba-Arad valley. The average height of the Judaean mountains is of 900 metres (2,953 ft), and they encompass the cities of Ramallah, Jerusalem, Bethlehem and Hebron. The northern section of the Judaean mountains is referred to as Jerusalem Hills, and the southern one as Hebron Hills.
Geology and palaeonthology
The Judaean Mountains are the surface expression of a series of monoclinic folds which trend north-northwest through Israel. The folding is the central expression of the Syrian Arc belt of anticlinal folding that began in the Late Cretaceous Period in northeast Africa and southwest Asia. The Syrian Arc extends east-northeast across the Sinai, turns north-northeast through Israel and continues the east-northeast trend into Syria. The Israeli segment parallels the Dead Sea Transform which lies just to the east. The uplift events that created the mountain occurred in two phases one in the Late Eocene-Early Oligocene and second in the Early Miocene.
The range has karst topography including a stalactite cave in Nahal Sorek National Park between Jerusalem and Beit Shemesh and the area surrounding Ofra, where fossils of prehistoric flora and fauna were found.
An Israel Railways line, Jaffa-Jerusalem railway runs from Beit Shemesh along the Brook of Sorek and Valley of Rephaim into Jerusalem Malha Train Station. The line has since been largely replaced by Tel Aviv-Jerusalem railway, which utilizes tunnels and bridges through Judean Mountains, runs up to 160km/h (99 mph) between Ben Gurion Airport and Jerusalem-Yitzhak Navon railway station.
The Judean Hills viewed from the Dead Sea
View from hilltop overlooking Wadi es-Ṣur, an extension of the Elah Valley in Israel
View from Beit Meir in the Judaean Mountains
The ruined structure of an ancient house, near Neve Michael
- Judaean Desert, the arid area descending east of the Judaean Mountains towards the Jordan Rift Valley
- Peter N. Peregrine, Melvin Ember, ed. (2003-03-31). Encyclopedia of Prehistory: South and Southwest Asia. 8. ISBN 9780306462627. Retrieved 2012-02-13.
- Judaean_Mountains - Mapcarta
- Palestine: Land, Encyclopaedia Britannica
- Stone, Lawson G. (2016). Philip W. Comfort (ed.). Judges (Judges 13:1-25). Cornerstone Biblical Commentary: Joshua, Judges, Ruth. 3. Tyndale House. pp. 381–382. ISBN 9781414398792. Retrieved 11 December 2019.
- Jerusalem Hills - Mapcarta
- Arieh Singer (2007). The Soils of Israel. Springer. pp. 129, 143.
- Abd El-Motaal, Essam; Kusky, Timothy M. (2003). Tectonic Evolution of the Intraplate S-Shaped Syrian Arc Fold-Thrust Belt of the Middle East Region in the Context of Plate Tectonics (PDF). The third international conference on the geology of Africa, Vol.2, December 2003, Assiut, Egypt, pp. 139–157. Archived from the original (PDF) on 2016-03-03. Retrieved 2012-02-23.
- Flexer A. (1989). "Late Cretaceous evolution of the Judean Mountains as indicated by ostracodes". Terra Nova. 1 (4): 349–358. doi:10.1111/j.1365-3121.1989.tb00385.x.
- Bar, Oded; Zilberman, Ezra; Feinstein, Shimon; Calvo, Ran; Gvirtzman, Zohan (2016). "The uplift history of the Arabian Plateau as inferred from geomorphologic analysis of its northwestern edge". Tectonophysics. 671: 9–23. doi:10.1016/j.tecto.2016.01.004.
- "History of Jerusalem from Its Beginning to David". Biu.ac.il. 1997-03-06. Retrieved 2012-02-13.
- "Cambridge History of Judaism". Cambridge.org. p. 210. Retrieved 16 August 2011. "In both the Idumaean and the Ituraean alliances, and in the annexation of Samaria, the Judaeans had taken the leading role. They retained it. The whole political–military–religious league that now united the hill country of Palestine from Dan to Beersheba, whatever it called itself, was directed by, and soon came to be called by others, 'the Ioudaioi'"
- A History of the Jewish People, edited by Haim Hillel Ben-Sasson, page 226, "The name Judea no longer referred only to...."
|Wikivoyage has a travel guide for Judaean Mountains.|
- Media related to Judaean Mountains at Wikimedia Commons
- Judaean Mountains & Jerusalem
- Symbolism and Landscape: The Etzion Bloc in the Judaean Mountains, Yossi Katz and John C. Lehr