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Harod Stream

Commons category link is locally definedRivers of Israel
Nahal Harod1
Nahal Harod1

The Harod Stream Hebrew: נחל חרוד, romanized: Nahal Harod, Arabic: نهر جالود, romanized: Wadi Jalud is a stream in Israel that flows west to east, from the Givat HaMoreh area via the Harod Valley and Beit She'an Valley into the Jordan River, about two kilometres (1.2 mi) north of Ma'oz Haim. It is the main drainage route of the Harod ValleyThe elevation is 500 metres (1,600 ft) above sea level at the source and 230 metres (750 ft) below sea level at the mouth (at 32.5144°N 35.5528°E / 32.5144; 35.5528). The drainage basin is 180 km2 (69 sq mi).The total length from the source to mouth is 31 km (19 mi), but the length of the non-intermittent flow is 20 to 22 km (12 to 14 mi). While the original sources of the water are karst springs, most of the stream's water comes from the discharge of numerous fish ponds, irrigation systems, and sewage. Rain floods are rare, and the upper flow of the stream is dry during most of the time. The network of the stream and its tributaries is mostly man-made, and natural riverbeds are preserved at the southern steep slopes of the valley.

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

Harod Stream
Gilboa Regional Council

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N 32.528531 ° E 35.444782 °
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מועצה אזורית גלבוע


Gilboa Regional Council
North District, Israel
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Nahal Harod1
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Harod Valley
Harod Valley

The Harod Valley (Hebrew: עמק חרוד, romanized: Emek Harod) is a valley in the Northern District of Israel. It is the eastern part of the Jezreel Valley,a transitional zone that extends to the Beit She'an Valley. From south it locked by Mount Gilboa and by the Issachar Plateau from north. It is named after the Ma'ayan Harod ("Spring of Harod", i.e., "Spring of Goliath") at the edge of the valley. It is naturally separated from the western part of the Jezreel valley by a watershed. While the Jezreel Valley is drained via the Kishon River to the Mediterranean Sea, the Harod Valley is drained through the Harod Stream ("Nahal Harod", "Wadi Jalud" in Arabic), which flows from Givat HaMoreh via Beit She'an Valley into the Jordan River. Ma'ayan Harod is the largest of the springs emerging on the northern slopes of Mount Gilboa. The source of the spring as well as other springs in the Beit She'an Valley to the east, comes from fresh rainwater that percolate into the limestone hills of Samaria and collect in an underground water reservoir beneath the areas of the Palestinian cities of Nablus and Jenin. The water emerges from the hills as they incline north towards the valleys. At this valley the waters emerge from a natural cave known as "Gideon's Cave".The valley covers about 40 sq.km. and is intensely cultivated. It is a corridor 18 km. long and 5 km. max wide. The exact border between the Harod Valley and the Beit She'an Valley depends on the conventions. For example, according to soil and precipitation parameters the border is the Sde Nahum - Beit Alfa line, while according to the climate, the border is defined by Kfar Yehezkel. The climate of the valley transitions from the Mediterranean climate of the western part of the Jezreel Valley to the arid dry-steppe climate of the Jordan Valley. There is a fault line between Mount Gilboa and the floor of the valley, with many spring along the line. Until the mid-20th century the valley was swamped, similarly to the Jordan Valley. Now the swamps are drained.