География Израиля: границы, регионы и ландшафты

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Israel's area is approximately , which includes of inland water. The Sykes Picot Treaty in 1916 divided the region that later became Palestine into four political units. Under the British Mandate for Palestine, the first geo political framework was created that distinguished the area from the larger countries that surrounded it. The boundary demarcation at this time did not introduce geographical changes near the frontiers and both sides of the border were controlled by the British administration. Modern Israel is bounded to the north by Lebanon, the northeast by Syria, the east by Jordan and the West Bank, and to the southwest by Egypt. To the west of Israel is the Mediterranean Sea, which makes up the majority of Israel's 273 km (170 mi) coastline and the Gaza Strip. Israel has a small coastline on the Red Sea in the south. The southernmost settlement in Israel is the city of Eilat whilst the northernmost is the town of Metula. The territorial waters of Israel extend into the sea to a distance of twelve nautical miles measured from the appropriate baseline. | 6,674
| 100–120
| 7,129
| 225
| 20,918
|
| Seam Zone (West Bank)
| Area between the Green Line and the Israeli West Bank barrier. Occupied in 1967
| 188
| 7,359
| 115
| 375
| 25,233
| 2,686
| 4,238 It is about wide at Gaza and narrows toward the north to about at the Lebanese border. Geographically, the region is divided into five sub regions. The northernmost section lays between the Lebanese border, the Western Galilee to the east, and the sea. It stretches from Rosh HaNikra in the north and down to Haifa, Israel's third largest city. It is a fertile region, and off the coast there are many small islands. Along the Mount Carmel range is Hof HaCarmel, or the Carmel Coastal Plain. It stretches from the point where Mount Carmel almost touches the sea, at Haifa, and down to Nahal Taninim, a stream that marks the southern limit of the Carmel range. The Sharon Plain is the next section, running from Nahal Taninim (south of Zikhron Ya'akov) to Tel Aviv's Yarkon River. This area is Israel's most densely populated. South of this, running to Nahal Shikma, is the Central Coastal Plain, also known as the Western Negev. The last segment is the Southern Coastal Plain, which extends south around the Gaza Strip. It is divided into two – in the north, the Besor region, a savanna type area with a relatively large number of communities, and south of it the Agur Halutza region, which is very sparsely populated. The Negev is also sub divided into five different ecological regions: northern, western and central Negev, the high plateau and the Arabah Valley. The northern Negev receives of rain annually and has fairly fertile soils. The high plateau area of Ramat HaNegev stands between and above sea level with extreme temperatures in summer and winter. The numerous limestone and sandstone layers of the Israeli mountains serve as aquifers through which water flows from the west flank to the east. Several springs have formed along the Dead Sea, each an oasis, most notably the oases at Ein Gedi and Ein Bokek (Neve Zohar) where settlements have developed.

The Jordan Rift Valley is the result of tectonic movements within the Dead Sea Transform (DSF) fault system. The DSF forms the transform boundary between the African Plate to the west and the Arabian Plate to the east. The Golan Heights and all of Jordan are part of the Arabian Plate, while the Galilee, West Bank, Coastal Plain, and Negev along with the Sinai Peninsula are on the African Plate. This tectonic disposition leads to a relatively high seismic activity in the region. The entire Jordan Valley segment is thought to have ruptured repeatedly, for instance during the last two major earthquakes along this structure in 749 and 1033. The deficit in slip that has built up since the 1033 event is sufficient to cause an earthquake of ~7.4. The most catastrophic earthquakes occurred in 31 BCE, 363, 749, and 1033 CE, that is every ca. 400 years on average. Destructive earthquakes leading to serious loss of life strike about every 80 years. While stringent construction regulations are currently in place and recently built structures are earthquake safe, as of 2007 the majority of the buildings in Israel were older than these regulations and many public buildings as well as 50,000 residential buildings did not meet the new standards and were "expected to collapse" if exposed to a strong quake. The river flows south through the freshwater Sea of Galilee, and from there forms the boundary with the Kingdom of Jordan for much of its route, eventually emptying into the Dead Sea. South of the Kinneret lies the saltwater Dead Sea which forms the border between Israel and Jordan and is below sea level, making it the lowest water surface on Earth. The Dead Sea is long with a maximum width of and also makes up part of the Rift Valley.

The northern half of Israel, has a Mediterranean climate with long, hot, rainless summers and relatively short, mild to cool, rainy winters (Köppen climate classification Csa). Changing to hot semi arid (BSh) and hot desert (BWh) climates in the southern half. The climate is as such due to Israel's location between the subtropical aridity of the Sahara and the Arabian deserts, and the subtropical humidity of the Levant and Eastern Mediterranean. Heat waves are frequent. 2010 was the hottest year in the history of Israel with absolute record high in several places in August. The heat became stronger from August when temperatures were considerably above the average. October and November were also dry, and November was almost rainless when it was supposed to be rainy.

Unlike much of the Middle East which is rich in lucrative crude oil, Israel has limited natural resources. These include copper, phosphates, bromide, potash, clay, sand, sulfur, asphalt, and manganese.

Israel has a large number of environmental concerns ranging from natural hazards to man made issues both resulting from ancient times to modern development. Natural hazards facing the country include sandstorms which sometimes occur during spring in the desert south, droughts which are usually concentrated in summer months, flash floods which create great danger in the deserts due to their lack of notice, and regular earthquakes, most of which are small, although there is a constant risk due to Israel's location along the Jordan Rift Valley. Originally these were collective and cooperative settlements respectively.

As of 2013, the population of Israel is 8 million, 6,015,000 of them Jewish. For statistical purposes, the country has three metropolitan areas; Gush Dan Tel Aviv (population 3,150,000), Haifa (population 996,000), and Beersheba (population 531,600). Some argue that Jerusalem, Israel's largest city with a population of 763,600, and Nazareth, should also be classified as metropolitan areas. In total, Israel has 74 cities, 14 of which have populations of over 100,000. Other forms of local government in Israel are local councils of which there are 144 governing small municipalities generally over 2,000 in population, and regional councils of which there are 53, governing a group of small communities over a relatively large geographical area. Israel's population is diverse demographically; 76% Jewish, 20% Arab, and 4% unaffiliated. In terms of religion, 76% are Jewish, 16% Muslim, 2% Christian, 2% Druze, and 4% are unclassified by choice. 8% of Israeli Jews are haredi; 9% are "religious", 12% "religious traditionalists", 27% are "non religious traditionalists", and 43% are "secular". Other small, but notable groups in Israel, include Circassians of whom there are approximately 3,000 living mostly in two northern villages, 2,500 Lebanese, and 5,000 Armenians predominantly in Jerusalem.

Israel is ranked 34th in the world in terms of population density with, as noted, a climate of long, hot, rainless summers and relatively short, cool, rainy winters. ranked Israel as the third most dependent region in the World after Singapore and Kuwait.