Geography of Israel

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Geography of Israel
Topography Israel
Relief map of Israel
Area
Total 20,770 km2[1][2]
Water 430 km2[1]
Latitude 31°30' Nr574567
Longitude 34°45'E
Borders
Egypt 208 km[1]
Jordan 307 km[1]
Lebanon 81 km[1]
Syria 83 km[1]
West Bank 330 km[1]
Gaza Strip 59 km[1]
Coastlines 273 km[1]

The geography of Israel is very diverse, with desert conditions in the south, and snow-capped mountains in the north. Israel is located at Lua error in package.lua at line 80: module 'strict' not found. at the eastern end of the Mediterranean Sea in western Asia.[1] It 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.[1] To the west of Israel is the Mediterranean Sea, which makes up the majority of Israel's 273 km (170 mi) coastline[3] and the Gaza Strip. Israel has a small coastline on the Red Sea in the south.

Israel's area is approximately 20,770 km2 (8,019 sq mi), which includes 445 km2 (172 sq mi) of inland water.[1][2][3] Israel stretches 424 km (263 mi) from north to south, and its width ranges from 114 km (71 mi) to, at its narrowest point, 15 km (9.3 mi).[3] The Israeli-occupied territories include the West Bank, 5,879 km2 (2,270 sq mi), East Jerusalem, 70 km2 (27 sq mi) and the Golan Heights, 1,150 km2 (444 sq mi).[2] Geographical features in these territories will be noted as such.

Southern Israel is dominated by the Negev desert, covering some 16,000 square kilometres (6,178 sq mi), more than half of the country's total land area. The north of the Negev contains the Judean Desert, which, at its border with Jordan, contains the Dead Sea which, at −417 m (−1,368 ft) is the lowest point on Earth. The inland area of central Israel is dominated by the Judean Hills of the West Bank, whilst the central and northern coastline consists of the flat and fertile Israeli coastal plain. Inland, the northern region contains the Mount Carmel mountain range, which is followed inland by the fertile Jezreel Valley, and then the hilly Galilee region. The Sea of Galilee is located beyond this, and is bordered to the east by the Golan Heights, which contains the highest point under Israel's control, a peak in the Israeli-occupied Mount Hermon massif, at 2,224 meters (7,297 ft). The highest point in territory internationally recognized as Israeli is Mount Meron at 1,208 meters (3,963 ft).[1]

Location and boundaries

Israel on the world map

Israel lies to the north of the equator around 31°30' north latitude and 34°45' east longitude.[1] It measures 424 km (263 mi) from north to south and, at its widest point 114 km (71 mi), from east to west.[1] At its narrowest point, however, this is reduced to just 15 km (9 mi). It has a land frontier of 1,017 km (632 mi) and a coastline of 273 km (170 mi).[1] It is ranked 153 on the List of countries and outlying territories by total area.[1]

Prior to the establishment of the British Mandate for Palestine, there was no clear-cut definition of the geographical and territorial limits of the area known as "Palestine." On the eve of World War I it was described by Encyclopedia Britannica as a "nebulous geographical concept."[4] The Sykes-Picot Treaty in 1916 divided the region that later became Palestine into four political units.[5] 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.[6]

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.[1]

The statistics provided by the Israel Central Bureau of Statistics include the annexed East Jerusalem and Golan Heights, but exclude the West Bank and Gaza Strip. The population of Israel includes Israeli settlers in the West Bank. The route of the Israeli West Bank barrier incorporates some parts of the West Bank.

Population (thousands) Area (km2)
Name Status Description Israelis (incl. Israeli Jews and Israeli Arabs in Israel proper, and incl. Israeli settlers in the Israeli-occupied territories) Cumulative Total Palestinians (incl. non-Israeli Palestinians residing legally in Israel) Cumulative Total Area Cumulative Total
Israel (Green Line) Area sovereign to Israel since 1948 6,674[7] 6,674[7] 100-120 [8] 100-120 [8] 20,582[7] 20,582[7]
East Jerusalem Occupied and subject to Israeli law since 1967. Formal legislation on 1980 (see Jerusalem Law) 455[9] 7,129[7] 225 (double counted)[10] 225[7] 336[11] 20,918[7]
Golan Heights Occupied since 1967, subject to Israeli law since 1981 (see Golan Heights Law) 42[12] 7,172[12] n.a. n.a. (Syrians) 1,154[13] 22,072[13]
Seam Zone (West Bank) Area between the Green Line and the Israeli West Bank barrier. Occupied in 1967 188[14] 7,359[7] 35[14] 260[7] 200[11] 22,272[7]
Other Israeli settlements and IDF Military Areas (West Bank Area C) Other Israeli settlements (not in East Jerusalem or the Seam Zone) and areas in the West Bank directly controlled by the IDF. Occupied in 1967 57[7] 7,473[12] 115[15] 375[7] 2,961[16] 25,233[7]
Palestinian civil control (West Bank Areas A+B) Palestinian National Authority civil controlled area. Subject to "joint" military control with the IDF. Occupied in 1967 0 7,473[7] 2,311[17] 2,686[7] 2,143[15] 27,376[7]
Gaza Strip Palestinian governed area. Israel controls airspace, maritime border and its own border with Gaza. Occupied in 1967, unilaterally disengaged in 2005, declared a foreign entity in 2007. 0 7,473[7] 1,552[18] 4,238[7] 360[18] 27,736[7]

Physiographic regions

Israel is divided into four physiographic regions: the Mediterranean coastal plain, the Central Hills, the Jordan Rift Valley and the Negev Desert.[1]

Coastal plain

Northern coast

The Israeli Coastal Plain stretches from the Lebanese border in the north to Gaza in the south, interrupted only by Cape Carmel at Haifa Bay.[19] It is about 40 kilometers (25 mi) wide at Gaza and narrows toward the north to about 5 kilometers (3.1 mi) at the Lebanese border.[19] The region is fertile and humid (historically malarial) and is known for its citrus orchards and viticulture.[19] The plain is traversed by several short streams. From north to south these are: the Kishon, the Hadera, the Alexander, the Poleg, and the Yarkon. All of these streams were badly polluted, but in the last ten years much work has been done to clean them up. Today the Kishon, Alexander and Yarkon again flow year round, and also have parks along their banks.[20]

The region is divided into five sub-regions. The Western Galilee stretches from Rosh HaNikra in the far north, down to Israel's third-largest city, Haifa. It is a fertile region containing with a coastline with many small islands off of it.[21] South of Haifa is the Hof HaCarmel region which runs to the town of Zikhron Ya'akov. The Sharon plain is the next stage down the Coastal Plain, running from 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. The southern region of the Coastal Plain is the Southern Coastal Plain (also known as the Shephelah, Plain of Judea, and Western Negev) and extends south to the Gaza Strip. It is divided into two. The Besor region, a savanna-type area with a relatively large number of communities, in the north, and the Agur-Halutsa region in the south which is very sparsely populated.[21]

Central hills

Judaean Mountains

Inland (east) of the coastal plain lies the central highland region.[19] In the north of this region lie the mountains and hills of Upper Galilee and Lower Galilee, which are generally 500 meters (1,640 ft) to 700 meters (2,297 ft) in height, although they reach a maximum height of 1,208 meters (3,963 ft) at Mount Meron.[19] South of the Galilee, in the West Bank, are the Samarian Hills with numerous small, fertile valleys rarely reaching the height of 800 meters (2,625 ft).[19] South of Jerusalem, also mainly within the West Bank, are the Judean Hills, including Mount Hebron.[19] The central highlands average 610 meters (2,001 ft) in height and reach their highest elevation at Har Meron, at 1,208 meters (3,963 ft), in Galilee near Safed.[19] Several valleys cut across the highlands roughly from east to west; the largest is the Jezreel Valley (also known as the Plain of Esdraelon), which stretches 48 kilometers (30 mi) from Haifa southeast to the valley of the Jordan River, and is 19 kilometers (12 mi) across at its widest point.[19]

Jordan Rift Valley

Jordan Rift Valley

East of the central highlands lies the Jordan Rift Valley, which is a small part of the 6,500 kilometers (4,039 mi)-long Syrian-East African Rift.[19] In Israel the Rift Valley is dominated by the Jordan River, the Sea of Galilee (an important freshwater source also known as Lake Tiberias and Lake Kinneret), and the Dead Sea.[19] The Jordan, Israel's largest river (322 kilometers (200 mi)), originates in the Dan, Baniyas, and Hasbani rivers near Mount Hermon in the Anti-Lebanon Mountains and flows south through the drained Hula Basin into the freshwater Lake Tiberias. Lake Tiberias is 165 square kilometers (64 sq mi) in size and, depending on the season and rainfall, is at about 213 meters (699 ft) below sea level.[19] With a water capacity estimated at 3 cubic kilometers (0.72 cu mi), it serves as the principal reservoir of the National Water Carrier (also known as the Kinneret-Negev Conduit).[19] The Jordan River continues its course from the southern end of Lake Tiberias (forming the boundary between the West Bank and Jordan) to its terminus in the highly saline Dead Sea.[19] The Dead Sea is 1,020 square kilometers (394 sq mi) in size and, at 420 meters (1,378 ft) below sea level, is the lowest surface point on the earth.[19] South of the Dead Sea, the Rift Valley continues in the Nahal HaArava (Wadi al Arabah), which has no permanent water flow, for 170 kilometers (106 mi) to the Gulf of Eilat.[19]

Negev Desert

Acacia tree in Makhtesh Gadol

The Negev Desert comprises approximately 12,000 square kilometers (4,633 sq mi), more than half of Israel's total land area.[19] Geographically it is an extension of the Sinai Desert, forming a rough triangle with its base in the north near Beersheba, the Dead Sea, and the southern Judean Mountains, and it has its apex in the southern tip of the country at Eilat.[19] Topographically, it parallels the other regions of the country, with lowlands in the west, hills in the central portion, and the Arabah valley as its eastern border.[19]

Unique to the Negev region are the craterlike makhteshim cirques; Makhtesh Ramon, Makhtesh Gadol and Makhtesh Katan.[22] The Negev is also sub-divided into five different ecological regions: northern, western and central Negev, the high plateau and the Arabah Valley.[23] The northern Negev receives 300 millimeters (11.8 in) of rain annually and has fairly fertile soils.[23] The western Negev receives 250 millimeters (9.8 in) of rain per year, with light and partially sandy soils.[23] The central Negev has an annual precipitation of 200 millimeters (7.9 in) and is characterized by impervious soil, allowing minimum penetration of water with greater soil erosion and water runoff.[23] This can result in rare flash floods during heavy rains as water runs across the surface of the impervious desert soil.[24] The high plateau area of Ramat HaNegev stands between 370 meters (1,214 ft) and 520 meters (1,706 ft) above sea level with extreme temperatures in summer and winter.[23] The area gets 100 millimeters (3.9 in) of rain each year, with inferior and partially salty soils.[23] The Arabah Valley along the Jordanian border stretches 180 kilometers (112 mi) from Eilat in the south to the tip of the Dead Sea in the north and is very arid with barely 50 millimeters (1.97 in) of rain annually.[23]

Geology

Rosh HaNikra limestone grotto
Strata exposed by excavation in Jerusalem

Israel is divided east-west by a mountain range running north to south along the coast. Jerusalem sits on the top of this ridge, east of which lies the Dead Sea graben which is a pull-apart basin on the Dead Sea Transform fault.[25]

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.[25] Israel also has a number of areas of karst topography. Caves in the region have been used for thousands of years as shelter, storage rooms, barns and as places of public gatherings.[25]

The far northern coastline of the country has some chalk landscapes best seen at Rosh HaNikra, a chalk cliff into which a series of grottoes have been eroded.[26]

Rivers and lakes

Israel's longest and most famous river is the Lua error in Module:Convert at line 272: attempt to index local 'cat' (a nil value). long River Jordan, which rises on the southern slopes of Mount Hermon in the Anti-Lebanon mountains.[27] 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.[27] The northern tributaries to the Jordan are the Dan, Banias, and Hasbani.[27] Only the Dan is within undisputed Israel; the Hasbani flows from Lebanon and the Banias from territory captured from Syria in the Six-Day War.[27]

Lake Kinneret

The Sea of Galilee (also called the Kinneret) is Israel's largest and most important freshwater lake, located in the northeast of the country. The pear-shaped lake is Lua error in Module:Convert at line 272: attempt to index local 'cat' (a nil value). long from north to south, with a maximum width of Lua error in Module:Convert at line 272: attempt to index local 'cat' (a nil value). in the north, covering 166 square kilometers (64 sq mi). The Kinneret lies 207 meters (679 ft) below sea level and reaches depths of 46 meters (151 ft). In a previous geological epoch the lake was part of a large inland sea which extended from the Hula marshes in northern Israel to 64 kilometers (40 mi) south of the Dead Sea. The bed of the lake forms part of the Jordan Rift Valley.[28]

South of the Kinneret lies the saltwater Dead Sea which forms the border between Israel and Jordan and is 418 meters (1,371 ft) below sea level, making it the lowest water surface on Earth.[29] The Dead Sea is 67 kilometers (42 mi) long with a maximum width of 16 kilometers (10 mi) and also makes up part of the Rift Valley.[29] A peninsula juts out into the lake from the eastern shore, south of which the lake is shallow, less than 6 meters (19.7 ft) deep. To the north is the lake's greatest depth.[29]

There are no navigable, artificial waterways in Israel, although the National Water Carrier, a conduit for drinking water, might be classified as such. The idea of a channel connecting the Mediterranean and Dead Seas or the Red and Dead Seas has been discussed.[30]

Selected elevations

Mount Tabor

The following are selected elevations of notable locations, from highest to lowest:[31]

Location Region Elevation (feet) Elevation (meters)
Mount Hermon Golan Heights (Israeli-occupied) 7,336 ft. 2,236 m.
Mount Meron Upper Galilee 3,964 ft. 1,208 m.
Mount Ramon Negev 3,396 ft. 1,035 m.
Mount of Olives East Jerusalem (Israeli-occupied) 2,739 ft. 835 m.
Mount Tabor Lower Galilee 1,930 ft. 588 m.
Mount Carmel Haifa 1,792 ft. 546 m.
Dead Sea Judean Desert  – 1,368 ft.  – 417 m.

Climate

Snow in Jerusalem
Flash flood at Ein Avdat

Israel has a Mediterranean climate with long, hot, rainless summers and relatively short, cool, rainy winters (Köppen climate classification Csa).[32] 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.[32] The climate conditions are highly variable within the state and modified locally by altitude, latitude, and the proximity to the Mediterranean.[32]

On average, January is the coldest month with average temperatures ranging from 6 to 15 °C (42.8 to 59.0 °F), and July and August are the hottest months at 22 to 33 °C (71.6 to 91.4 °F), on average across the country.[32] Summers are very humid along the Mediterranean coast but dry in the central highlands, the Rift Valley, and the Negev Desert. In Eilat, a desert city, summer daytime-temperatures are often the highest in the state, at times reaching 44 to 46 °C (111.2 to 114.8 °F). More than 70% of the average rainfall in Israel falls between November and March; June through September are usually rainless.[32] Rainfall is unevenly distributed, significantly lower in the south of the country.[32] In the extreme south, rainfall averages near 30 millimeters (1.18 in) annually; in the north, average annual rainfall exceeds 900 millimeters (35.4 in).[32] Rainfall varies from season to season and from year to year, particularly in the Negev Desert. Precipitation is often concentrated in violent storms, causing erosion and flash floods.[32] In winter, precipitation often takes the form of snow at the higher elevations of the central highlands, including Jerusalem.[32] Mount Hermon has seasonal snow which covers all three of its peaks for most of the year in winter and spring. In rare occasions, snow gets to the northern mountain peaks and only in extremely rare occasions even to the coast. The areas of the country most cultivated are those receiving more than 300 millimeters (11.8 in) of rainfall annually, making approximately one-third of the country cultivable.[32]

Thunderstorms and hail are common throughout the rainy season and waterspouts occasionally hit the Mediterranean coast, capable of causing only minor damage. However, supercell thunderstorms and a true F2 tornado hit the Western Galilee in April 2006, causing significant damage and 75 injuries.[33]

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.

Climate charts of different locations in Israel

Tel Aviv
Climate chart (explanation)
J F M A M J J A S O N D
 
 
127
 
 
17
9
 
 
90
 
 
18
10
 
 
61
 
 
19
12
 
 
18
 
 
23
14
 
 
2.6
 
 
25
17
 
 
0
 
 
28
21
 
 
0
 
 
29
23
 
 
0
 
 
30
24
 
 
0.4
 
 
29
23
 
 
26
 
 
27
19
 
 
79
 
 
23
15
 
 
126
 
 
19
11
Average max. and min. temperatures in °C
Precipitation totals in mm
Source: Israel Meteorological Service
Beit Dagan
Climate chart (explanation)
J F M A M J J A S O N D
 
 
141
 
 
18
7
 
 
97
 
 
18
7
 
 
66
 
 
20
9
 
 
18
 
 
25
12
 
 
2.2
 
 
27
15
 
 
0
 
 
29
18
 
 
0
 
 
31
21
 
 
0
 
 
31
21
 
 
0.4
 
 
30
19
 
 
20
 
 
28
16
 
 
76
 
 
24
12
 
 
130
 
 
20
9
Average max. and min. temperatures in °C
Precipitation totals in mm
Source: Israel Meteorological Service
Jerusalem
Climate chart (explanation)
J F M A M J J A S O N D
 
 
133
 
 
12
6
 
 
118
 
 
13
6
 
 
93
 
 
15
8
 
 
25
 
 
22
13
 
 
3.2
 
 
25
16
 
 
0
 
 
28
18
 
 
0
 
 
29
19
 
 
0
 
 
29
20
 
 
0.3
 
 
28
19
 
 
15
 
 
25
17
 
 
61
 
 
19
12
 
 
106
 
 
14
8
Average max. and min. temperatures in °C
Precipitation totals in mm
Source: Israel Meteorological Service
Haifa
Climate chart (explanation)
J F M A M J J A S O N D
 
 
125
 
 
17
9
 
 
92
 
 
18
9
 
 
53
 
 
20
11
 
 
24
 
 
24
14
 
 
2.7
 
 
26
17
 
 
0
 
 
29
21
 
 
0
 
 
31
23
 
 
0
 
 
31
24
 
 
1.2
 
 
30
22
 
 
28
 
 
28
19
 
 
77
 
 
24
14
 
 
136
 
 
19
10
Average max. and min. temperatures in °C
Precipitation totals in mm
Source: Israel Meteorological Service
Safed
Climate chart (explanation)
J F M A M J J A S O N D
 
 
159
 
 
9
5
 
 
130
 
 
10
4
 
 
95
 
 
13
6
 
 
43
 
 
20
11
 
 
5.7
 
 
25
14
 
 
0
 
 
28
17
 
 
0
 
 
30
19
 
 
0
 
 
30
19
 
 
1.5
 
 
28
18
 
 
25
 
 
24
15
 
 
86
 
 
17
10
 
 
136
 
 
12
6
Average max. and min. temperatures in °C
Precipitation totals in mm
Source: Israel Meteorological Service
Beersheba
Climate chart (explanation)
J F M A M J J A S O N D
 
 
50
 
 
17
8
 
 
40
 
 
18
8
 
 
31
 
 
20
9
 
 
13
 
 
26
13
 
 
2.7
 
 
29
15
 
 
0
 
 
31
18
 
 
0
 
 
33
21
 
 
0
 
 
33
21
 
 
0.4
 
 
31
20
 
 
5.8
 
 
29
17
 
 
20
 
 
24
13
 
 
42
 
 
19
9
Average max. and min. temperatures in °C
Precipitation totals in mm
Source: Israel Meteorological Service
Tiberias
Climate chart (explanation)
J F M A M J J A S O N D
 
 
90
 
 
18
10
 
 
73
 
 
19
9
 
 
57
 
 
23
11
 
 
20
 
 
28
14
 
 
4
 
 
33
18
 
 
0
 
 
36
20
 
 
0
 
 
38
23
 
 
0
 
 
38
23
 
 
0.6
 
 
36
22
 
 
14
 
 
32
19
 
 
50
 
 
26
15
 
 
81
 
 
20
11
Average max. and min. temperatures in °C
Precipitation totals in mm
Source: Israel Meteorological Service
Eilat
Climate chart (explanation)
J F M A M J J A S O N D
 
 
3.5
 
 
21
10
 
 
5.8
 
 
22
11
 
 
3.7
 
 
26
14
 
 
1.7
 
 
31
18
 
 
1
 
 
35
22
 
 
0
 
 
39
24
 
 
0
 
 
40
26
 
 
0
 
 
40
26
 
 
0
 
 
37
25
 
 
3.5
 
 
33
21
 
 
3.5
 
 
27
16
 
 
6
 
 
22
11
Average max. and min. temperatures in °C
Precipitation totals in mm
Source: Israel Meteorological Service

Natural resources

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.[1] Small amounts of natural gas and crude oil are present, often too little to merit commercial extraction.[1] In 2009, significant reserves of natural gas were discovered at the Tamar 1 offshore drilling site, 90 kilometers west of Haifa. It is the largest natural gas reserve ever discovered in Israel.[34]

Environmental concerns

Ashdod dunes
Formerly polluted Kishon River after clean-up, 2010

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.[1] Current environmental concerns include the lack of arable land and natural fresh water resources. Whilst measures have been taken to irrigate and grow in the desert, the amount of water needed here poses issues. Desertification is also a risk possible on the desert fringe, whilst air pollution from industrial and vehicle emissions and groundwater pollution from industrial and domestic waste are also issues facing the country.[1] Furthermore, the effects of the use of chemical fertilizers, and pesticides are issues facing the country.[1] Israel has signed many international environmental agreements and is party to:[1]

Signed but not ratified:

Rural settlements

View of Kibbutz Lotan

Israel's rural space includes several unique kinds of settlements, notably the moshav and the kibbutz.[35] Originally these were collective and cooperative settlements respectively.[35] Over time, the degree of cooperation in these settlements has decreased and in several of them the cooperative structure has been dismantled altogether.[35] All rural settlements and many small towns (some of which are dubbed "rurban settlements") are incorporated in regional councils. Land use in Israel is 17% arable land, 4% permanent crops, and 79% other uses.[1] As of 2003 1,940 square kilometers (749 sq mi) were irrigated.[1]

There are 242 Israeli settlements and civilian land use sites in the West Bank, 42 in the Golan Heights, and 29 in East Jerusalem.[1]

Islands

Israel currently has no offshore islands within its territorial waters. However, the Israeli government plans to build artificial islands off the coast to house an airport, a seaport, a desalination plant, a power plant, and a military testing base, as an answer to Israel's lack of space.[36][37]

Human geography

Israel and its current neighbors, with a rare dusting of snow over many areas. (December 17, 2013)[38]

As of 2013, the population of Israel is 8 million, 6,015,000 of them Jewish.[39]

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).[40] Some argue that Jerusalem, Israel's largest city with a population of 763,600,[41] and Nazareth,[42] 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,[43][44] and regional councils of which there are 53, governing a group of small communities over a relatively large geographical area.[43][45]

Israel's population is diverse demographically; 76% Jewish, 20% Arab, and 4% unaffiliated.[46] In terms of religion, 76% are Jewish, 16% Muslim, 2% Christian, 2% Druze, and 4% are unclassified by choice.[47] 8% of Israeli Jews are haredi; 9% are "religious", 12% "religious-traditionalists", 27% are "non-religious traditionalists", and 43% are "secular".[48] 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.[49][50]

Overshoot

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.[32] The Population Matters 2011 overshoot index[51] ranked Israel as the third most dependent region in the World after Singapore and Kuwait.

See also

References

  1. ↑ 1.00 1.01 1.02 1.03 1.04 1.05 1.06 1.07 1.08 1.09 1.10 1.11 1.12 1.13 1.14 1.15 1.16 1.17 1.18 1.19 1.20 1.21 1.22 1.23 1.24 1.25 1.26 1.27 Lua error in package.lua at line 80: module 'strict' not found.
  2. ↑ 2.0 2.1 2.2 Lua error in package.lua at line 80: module 'strict' not found.
  3. ↑ 3.0 3.1 3.2 Lua error in package.lua at line 80: module 'strict' not found.
  4. ↑ An Empire in the Holy Land: Historical Geography of the British Administration in Palestine, 1917–1929, Gideon Biger, St. Martin's Press and Magnes Press, 1994, pp.40–41.
  5. ↑ An Empire in the Holy Land: Historical Geography of the British Administration in Palestine, 1917–1929, Gideon Biger, St. Martin's Press and Magnes Press, 1994, pp.46–52.
  6. ↑ An Empire in the Holy Land: Historical Geography of the British Administration in Palestine, 1917–1929, Gideon Biger, St. Martin's Press and Magnes Press, 1994, pp.67–69.
  7. ↑ 7.00 7.01 7.02 7.03 7.04 7.05 7.06 7.07 7.08 7.09 7.10 7.11 7.12 7.13 7.14 7.15 7.16 7.17 7.18 Figure calculated from other sourced figures in table
  8. ↑ 8.0 8.1 http://www.miftah.org/Display.cfm?DocId=14464&CategoryId=4
  9. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  10. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  11. ↑ 11.0 11.1 Lua error in package.lua at line 80: module 'strict' not found.
  12. ↑ 12.0 12.1 12.2 Lua error in package.lua at line 80: module 'strict' not found.
  13. ↑ 13.0 13.1 Lua error in package.lua at line 80: module 'strict' not found.
  14. ↑ 14.0 14.1 Lua error in package.lua at line 80: module 'strict' not found.
  15. ↑ 15.0 15.1 Lua error in package.lua at line 80: module 'strict' not found.
  16. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  17. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  18. ↑ 18.0 18.1 Lua error in package.lua at line 80: module 'strict' not found.
  19. ↑ 19.00 19.01 19.02 19.03 19.04 19.05 19.06 19.07 19.08 19.09 19.10 19.11 19.12 19.13 19.14 19.15 19.16 19.17 19.18 Lua error in package.lua at line 80: module 'strict' not found.
  20. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  21. ↑ 21.0 21.1 Lua error in package.lua at line 80: module 'strict' not found.
  22. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  23. ↑ 23.0 23.1 23.2 23.3 23.4 23.5 23.6 Lua error in package.lua at line 80: module 'strict' not found.
  24. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  25. ↑ 25.0 25.1 25.2 Lua error in package.lua at line 80: module 'strict' not found.
  26. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  27. ↑ 27.0 27.1 27.2 27.3 Lua error in package.lua at line 80: module 'strict' not found.
  28. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  29. ↑ 29.0 29.1 29.2 Lua error in package.lua at line 80: module 'strict' not found.
  30. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  31. ↑ Statistical Abstract of Israel, No. 58, 2007
  32. ↑ 32.00 32.01 32.02 32.03 32.04 32.05 32.06 32.07 32.08 32.09 32.10 Lua error in package.lua at line 80: module 'strict' not found.
  33. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  34. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  35. ↑ 35.0 35.1 35.2 Lua error in package.lua at line 80: module 'strict' not found.
  36. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  37. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  38. ↑ Rare Middle Eastern Snow - December 17, 2013
  39. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  40. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  41. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  42. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  43. ↑ 43.0 43.1 Lua error in package.lua at line 80: module 'strict' not found.
  44. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  45. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  46. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  47. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  48. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  49. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  50. ↑ Lua error in package.lua at line 80: module 'strict' not found.
  51. ↑ Lua error in package.lua at line 80: module 'strict' not found.

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