The Lower Galilee (; ) is a region within the Northern District of Israel. The Lower Galilee is bordered by the Jezreel Valley to the south; the Upper Galilee to the north, from which it is separated by the Beit HaKerem Valley; the Jordan Rift Valley with the Jordan River and the Sea of Galilee to the east; and to the west, a segment of the Northern Coastal Plain known as the Zvulun Valley (Zebulon Valley), stretching between the Mount Carmel and Acre. The Lower Galilee is the southern part of the Galilee. In Josephus' time, it was known to stretch in breadth from Xaloth (Iksal) to Bersabe, and in length from Cabul to Tiberias,[Josephus, The Jewish War 3.3.1 (3.35). In The Jewish War 3.3.1., the Greek word used for the city is Cabul (Gr. Χαβουλών), although in William Whiston's English translation the word is erroneously written as Zebulon. Cf. Josephus (1968), Jacob N. Simchoni (ed.), The History of the War of the Jews with the Romans (in Hebrew) (2 ed.), Ramat-Gan: Masada. p. 565.] a region that contains around 470 km2.[Erich M. Meyers, "Galilean Regionalism as a Factor in Historical Reconstruction," in: Bulletin of the American Schools of Oriental Research (No. 221, 1976), p. 95] It is called "Lower" since it is less mountainous than the Upper Galilee. The peaks of the Lower Galilee rise to above sea level. The tallest peaks are Mount Kamon () at the northern part of the Lower Galilee, and Mount Tabor () in the southern part.
Geography
The Lower Galilee consists of three different regions which differ in their geological structure:
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The western Lower Galilee
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The central Lower Galilee
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The high regions of the eastern Lower Galilee
The central Lower Galilee consists of low mountain ranges which extend from east to west with several valleys in between; south of the Beit Kerem (Šagor) Valley is the Shagor mountain range, then Sakhnin valley, Yodfat range, Beit Netofa Valley, Tur'an valley and range, Nazareth range, and Ksulot () valley. In the western part of the Lower Galilee there are several low hills (200–300 meters) covered with Oak tree forests, the central Lower Galilee region is more mountainous and the eastern Lower Galilee region turn into flat basalt mountainside reaching heights of 300 meters above sea level which extend from northeast to the southwest.
Although the landscape of the Lower Galilee is less dramatic than that of the Upper Galilee, it is , more peaceful and quiet. The Lower Galilee is more accessible to the majority of Israelis (less than a 2-hour drive from the Gush Dan). Much of the produce farms of Israel originates in the Lower Galilee, especially in the Jezreel Valley and the Beit She'an Valley.
Type of soil
The
soil of the Lower Galilee mainly consists of the following:
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Limestone - the lands in the central Lower Galilee region consists mainly of limestone which was created due to accumulation of shells and skeletons of marine life on the seabed.
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Brown Terra Rossa - the Lower Galilee region also have many areas which consists of this type of soil which has high amounts of minerals. The Terra Rossa is the basis for the development of forests in the Galilee because it has a large amount of mineral needed for the trees to grow.
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Basalt - the lands in the eastern Lower Galilee region (the area near the Golan Heights) consists mainly of basalt which is a type of rock that was created as a result of hot magma from erupted volcanoes which later cooled in temperature and became rock hard and impenetrable. The basalt areas also comprise very fertile soil.
Water resources
Until 1932 the settlements in the eastern Lower Galilee were based solely on
spring water which existed in proximity to the villages which were only enough for home use and therefore it was not possible to have irrigated agriculture in the Lower Galilee at the time. In 1932 the first
Well drilling was done in the Yavne'el Valley which supplied
irrigation water to Yavne'el. In 1942 a water pipeline was constructed from the Sea of Galilee to the village which as a result extended its amount of agricultural lands, which were based mainly on the new water sources, despite the relatively high cost of water at that time. During the first decade of the State of Israel the villages of the Lower Galilee were involved in a constant struggle with the government demanding that the government would solve their water problems. After several local Well drilling attempts made during those years failed water pipelines were laid from the Sea of Galilee to all villages in the Lower Galilee.
Historical overview
In the Iron Age II, Lower Galilee was part of the Kingdom of Israel, which fell to the Assyrian Empire in the 8th century BCE. The Assyrians expelled the local
Israelites population, leading to the region's depopulation. Archaeological evidence shows that the number of settlements in Lower Galilee plummeted from 60 before 733/732 BCE to zero, remaining uninhabited for centuries. It was only during the Persian period that the area was resettled, with 30 known settlements established.
[Zvi Gal, Lower Galilee during the Iron Age (American Schools of Oriental Research Dissertation Series 8; Winona Lake, Ind.: Eisenbrauns, 1992), p. 108][Jensen, M. H. (2014). The Political History in Galilee from the First Century BCE to the end of the Second Century CE. Galilee in the late Second Temple and Mishnaic periods. Volume 1. Life, culture and society, 51-77. "Gal’s survey has influenced a number of scholars to accept a break in the Israelite/Jewish presence in Galilee."]
Gallery
Image:Mount Tabor4.jpg|Mount Tabor
Image:Mount of transfiguration is.JPG|Church of the Transfiguration
Image:Almog IL2 Movil.jpg|Beit Netofa Valley
Image:PikiWiki Israel 8964 Geography of Israel.jpg|Nahal Amud
Image:Mount-Arbel-189.jpg|Mount Arbel
Image:Cipori142.jpg|Sepphoris ruins
Image:PikiWiki Israel 7674 Archeological sites of Israel.JPG|The "Mona Lisa of the Galilee" mosaic in Sepphoris
Image:View of Nazareth from El Kishleh neighborhood.jpg|Nazareth
See also
