

ECO TOURISm
North Israel
WELCOME TO Golan Hights
Description and characterization of the
* The Golan Heights is located in the northeast of the state of Israel.
* Ref: 32.950364, 35.667509 [latitude and longitude].
* Drive: Car rental for travel from place to place.
* The trail is suitable for all ages - Difficulty easy-medium
Geographical background
The Golan Heights is a level flat located south of the Yarmouk River, north of Mount Hermon and the Sea of Galilee and the Hula Valley West.
The area is about 1,800 square kilometers, of which 1,200 square kilometers controlled by Israel.
Many rivers in the Golan Heights, which provide about a third from the Sea of Galilee.
The land is mostly basalt, due to the many volcanoes were active in the past.
history background
Geopolitical region, the Golan Heights is a territory Israel captured from Syria during the Six Day War, and applied it to Israeli law in 1981 enactment of the Golan Heights Law (Some call it "annexation"). This area includes two-thirds of the Golan Heights geology, and the Israeli part of Mount Hermon.
Use ground
Geysers
Average temperature is 19-21 degrees
Mshakim area: the most northern part of the region from 1300 to 1400 mm, and the southernmost part of the region reaches 500 mm
Agricultural 3% -5%
Industry and Construction Department 20% -25%
Commercial Services - 30%
40% Security
Following rifle basaltic soil volcanoes are active Bowhser but not a lot of time
Soil saturated with water so there's a lot of drainage basins, lakes and Margie ordinary water.
Also rich soil clay stones
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Geyser is a hot spring that erupts periodically, and up into the pillar of hot water and steam. Geysers are quite rare, because it takes a combination of unique geological conditions and climatic, which exists only in few locations in the world. Geyser's activity is caused by rainwater seeping into the ground until they hit a rock heated by magma. When geyser is filled, the top water cool, but because of the narrow canals, cooling water does not reach the lower layers. The cold water from the top click on the hot water below, like the lid of a pressure cooker, and allow the water reservoir to heat up beyond the boiling point while liquids. Eventually, the pressure near the bottom of the geyser comes to the point where it starts boiling. Steam bubbles rise to the top of the trenches. When these bubbles burst their way out through the geyser , some of the water skiers or splashes out, thus mitigating the canals and water weight, respectively, reducing the pressure on the lower layers. With this pressure id released, beyond the boiling point of water turns into steam, and burst wildly through the opening. Expanding foam produced by the steam and hot water sprayed out of a geyser. Eventually it cools off leaving water geyser below the boiling point and the eruption ends. Hot water underground begin to flow back into ditches geyser, and the cycle begins all over again.
ABOUT the area -"golan Hights"


