Palestine's geography: two territories, one ridge and one coast
1 996 words · 9 min · updated 2026-10-02
Two pieces of land that do not touch make up the territory the State of Palestine claims: a limestone upland west of the Jordan River and a sandy strip of coastal plain on the Mediterranean, with Israeli territory between them. Britannica measures the West Bank at about 5,660 square kilometres and the Gaza Strip at 363. One is hill country that drops into the Jordan rift, the other a plain of dunes and sandstone ridges a few kilometres wide, and in both the land that can be farmed is set by water more than by soil.
In short
- West Bank area
- about 5,660 km², Britannica
- Gaza Strip area
- about 363 km², Britannica
- Gaza Strip length
- 41 km, 6 to 12 km wide
- Gaza land borders
- Israel 51 km, Egypt 11 km
- West Bank land boundaries
- 404 km, landlocked
- Highest point in Gaza
- Abu 'Awdah, 105 m
- Area C share of the West Bank
- 60%, under Oslo II
- Rainfall
- over 685 mm in the north-west hills to under 100 mm by the Dead Sea
Why the two territories do not touch
The West Bank and the Gaza Strip are the two parts of mandate Palestine that stayed in Arab hands at the armistices of 1949, and the lines drawn then still define them. The West Bank is bordered by Jordan to the east, along the Jordan River and the Dead Sea, and by Israel to the north, west and south; it is landlocked, with land boundaries of 404 km. The Gaza Strip has the Mediterranean to the west, a border of 11 km with Egypt near Rafah and a border of 51 km with Israel on its northern and eastern sides. The shortest route between the two crosses Israel.
Both areas are measured slightly differently by different publishers. The West Bank article on Wikipedia gives 5,628 or 5,640 square kilometres, about 21.2% of mandate Palestine west of the Jordan, and counts 220 square kilometres of water, the north-western quarter of the Dead Sea. Britannica gives 5,660. For Gaza, Britannica gives 363 square kilometres and the Gaza Strip article 365, over a strip 41 km long and 6 to 12 km wide.
| West Bank | Gaza Strip | |
|---|---|---|
| Area | about 5,660 km², Britannica | about 363 km², Britannica |
| Land borders | Jordan, Israel; 404 km in all | Israel 51 km, Egypt 11 km |
| Coast | none; shore of the Dead Sea | Mediterranean, about 40 km |
| Terrain | limestone hills falling east to the Jordan rift | flat or rolling coastal plain, dunes near the sea |
| Climate | Mediterranean in the hills, desert in the east | hot semi-arid |
| Rainfall | over 685 mm in the north-west hills, under 100 mm by the Dead Sea | about 300 mm a year, Britannica |
| Governorates | 11 | 5 |
How the West Bank falls from ridge to rift
The West Bank is mostly north-south limestone hills, which Britannica calls the Samarian Hills north of Jerusalem and the Judaean Hills south of it, averaging 700 to 900 metres in height. Named summits include Mount Gerizim at 881 m, Nabi Samwil at 890 m and Mount Scopus at 826 m, and the highest point is Mount Nabi Yunis. The rock is marine sediment, limestone and dolomite.
Samaria, in the north, has wider and gentler basins than Judaea, such as the Arrabah plain and the basin around Nablus, and is approached from the Jordan by the Fari'ah valley. From Ramallah southward the high plateau of Judaea is, in Britannica's description, a rocky wilderness of limestone with rare patches of cultivation, as around al-Bireh and Hebron. On its eastern side the plateau falls abruptly into the Jordan Valley, reached with difficulty down wadis such as the Qelt.
The Jordan Valley is a rift between 2.5 and 22 km wide that descends to about 400 metres below sea level. It is a segment of the Dead Sea Transform, the fault that separates the African and Arabian plates.
The Geography of Palestine article lists destructive earthquakes along it in 31 BCE and in 363, 749 and 1033 CE. The valley is dry and hot, and cultivation is limited to irrigated land and oases such as Jericho, where UNESCO describes a perennial spring, Ain es-Sultan, beside a settlement mound already permanent by the 9th to 8th millennium BCE.
Not all of the West Bank drains to the Jordan, because streams rising on the higher western ground run west towards the Mediterranean, while wadis such as Wadi Fa'rah and Wadi Qelt run east into the river or the Dead Sea. The valley of Marj Sanur holds a seasonal lake.
What the Gaza Strip is built of
The Gaza Strip sits on a relatively flat coastal plain. Three ridges run parallel to the shore, built of a wind-laid calcareous sandstone called kurkar, with red fine-grained soils called hamra between the layers, and wadis filled with alluvium separate them. Dunes line the coast. The highest point, Abu 'Awdah, stands 105 m above sea level.
Wadi Gaza is the strip's main watercourse, and a nature reserve around it protects the only coastal wetland in the territory.
The towns follow the coast and the ridges. Rafah lies on the Egyptian border, Khan Yunis 7 km north-east of it, Deir el-Balah on the coast between Khan Yunis and Gaza City, and Beit Lahia and Beit Hanoun beyond Gaza City in the north. The Israeli settlement bloc of Gush Katif stood on the dunes beside Rafah and Khan Yunis until 2005.
Where the rain falls and where it does not
Rain comes in the cool half of the year, from October to April, and decreases from north to south and from the coast inland. In the West Bank the north-western hills receive more than 685 mm a year, and the amount falls to under 100 mm along the Dead Sea in the south-east. The hills have a Mediterranean climate, slightly cooler with height; the eastern slopes, the Judaean Desert and the Dead Sea shore are dry and hot.
Gaza has a hot semi-arid climate, and Britannica puts its annual precipitation at about 300 mm, and the Gaza Strip article gives a range from 225 mm in the south to 400 mm in the north, almost all of it between November and February. Britannica gives average temperatures of about 13 °C in winter and the mid to upper 20s in summer; the Geography of Palestine article gives July and August as the hottest months, with an average high of 33 °C.
Who controls the water in the hills
The porosity of the limestone lets rain filter down to the impermeable layers that feed the aquifers, and the West Bank highlands are the main recharge area for the coastal aquifers on the Israeli side. Britannica notes that perennial rivers are few in the whole region and that this porosity makes the shortage worse. The division of groundwater was written into the Oslo II agreement of 1995, and Israel supplied the Palestinian territories with 52 million cubic metres in 2012 from its own and desalinated supply.
The Geography of Palestine article cites Friends of the Earth Middle East as reporting that up to 96% of the Jordan's fresh water is diverted by Israel, Jordan and Syria, while untreated sewage is discharged into the river. In Gaza the problems listed by the same article are salination of fresh water, depletion and contamination of the groundwater, and sewage. Between a third and a half of the water delivered in the Palestinian territories is lost in the distribution network.
What the ground holds besides farmland
The Dead Sea is the territory's mineral resource. Its muds and brines carry magnesium, potash and bromine, and the Geography of Palestine article records that these are worked by Israeli settlements; the Palestinian policy network Al-Shabaka estimated in 2015 that access to them could have added $918 million a year to the Palestinian economy.
Stone is the other: the West Bank article records that Israel licenses eleven settlement quarries that sell 94% of their output to Israel, while permits for most of the roughly 40 Palestinian-owned quarries at Beit Fajar are refused. The same article calculates that a further 275 quarries could open in Area C if the restrictions were lifted, and cites a World Bank estimate that the near ban on Palestinian quarry permits there costs the economy at least US$241 million a year.
Offshore, a gas field known as Gaza Marine was found in 2000 under a licence the Palestinian Authority granted to British Gas. It had not been developed by 2024.
Three terrestrial ecoregions are found in the territory: Eastern Mediterranean conifer, sclerophyllous and broadleaf forest, the Arabian Desert and the Mesopotamian shrub desert. The Palestine article divides the territory into five ecological zones, the Central Highlands, the Semi-coastal Region, the Eastern Slopes, the Jordan Rift Valley and the Coastal Region, and counts 373 bird species recorded in the occupied Palestinian areas. Forest and woodland cover about 1% of the West Bank.
How the land is farmed and divided
Water decides land use. Britannica describes the better-watered unirrigated hills, especially in Samaria, used for grazing sheep and for cereals, olives and fruit, and the irrigated land of the hills and the Jordan valley farmed intensively for fruit and vegetables. The West Bank article puts arable land at 27% of the area. At Battir, south-west of Jerusalem, UNESCO's World Heritage listing of 2014 describes valleys of stone terraces, some irrigated for vegetables and others dry and planted with vines and olives, fed by channels from underground springs and shared between the village's families by a traditional rota.
In Gaza, Britannica describes nearly three-quarters of the land as cultivated, with citrus as the chief crop on irrigated land, followed by vegetables, wheat and olives.
The land is also divided by administration. Under Oslo II the West Bank was split into Area A, 18% of its area, under Palestinian civil and security control; Area B, 22%, under Palestinian civil control with joint security; and Area C, 60%, under Israeli control. The Palestine article on Wikipedia records that 81% of the designated protected areas lie in Area C. The Israeli barrier, begun on 23 June 2002 and 708 km long as approved, leaves 9% of the West Bank in a closed zone between the barrier and the 1949 line, by the West Bank article's count. In Gaza, a buffer zone along the Israeli border covered 14% of the strip and 30 to 55% of its arable land before the ceasefire of November 2012, by the Gaza Strip article's account.
Where people live on the land
The Palestinian Central Bureau of Statistics estimated 3,395,260 people in the West Bank and 2,349,301 in the Gaza Strip for 2025, figures prepared before October 2023; its revised estimate put Gaza at 2,114,301 in mid-2025, 10% below the earlier figure. Britannica adds about 750,000 Israelis living in the West Bank to its 2026 estimate for the territory, and gives Gaza a density of 6,024 people per square kilometre in 2023.
In the West Bank most people live along the mountain spine running north to south, in Jenin, Nablus, Ramallah, al-Bireh, Jerusalem, Bethlehem, Hebron and Yattah. Qalqilyah and Tulkarm lie in the low foothills on the western edge, and Jericho and Tubas in the Jordan Valley. East Jerusalem sits at the centre of the West Bank. Israel administers it as part of its own Jerusalem District, and the State of Palestine claims it as part of the Jerusalem Governorate; in 2010, of its 456,000 people, roughly 60% were Palestinian and 40% Israeli, by the Palestine article's figures.
The West Bank article counted over 450,000 Israeli settlers in 132 settlements in 2022, excluding East Jerusalem, and a further 220,000 in 12 settlements in East Jerusalem. The same article cites a European Union report of 2011: between 200,000 and 320,000 Palestinians lived in the Jordan Valley before 1967 and about 56,000 by 2011, most of them in Jericho, while the Jewish population of Area C grew from 1,200 to 310,000 over a similar period.
Britannica records that the first accurate census there, in September 1967, found nearly half of the population living in refugee camps, and the Gaza Strip article notes that the camps are managed by the United Nations Relief and Works Agency. The Palestinian Authority divides the territory into 16 governorates, 11 in the West Bank and 5 in the Gaza Strip.
Surroundings
Which countries border Palestine
Recorded as shared borders, which includes neighbours across water: Palestine has a coast, and the list reads accordingly. Hover a row to find the country on the map; the distance is capital to capital, in a straight line.
Common questions
Questions about Palestine
How far apart are the West Bank and the Gaza Strip?
They have no common border. Israeli territory lies between them, and travel from one to the other crosses Israel. Israel restricts that movement; the Gaza Strip article records that Gaza residents are typically refused permission to move to the West Bank, even those originally from there.
Does the West Bank have a coastline?
No. Its eastern edge runs down the Jordan River and the north-western shore of the Dead Sea, and its other borders are with Israel. The only coast the State of Palestine claims is the Gaza Strip's, about 40 km of Mediterranean shore.
Why is the Jordan Valley so dry?
It is a rift that descends to about 400 metres below sea level on the eastern side of the hills. Rainfall in the West Bank falls from over 685 mm in the north-western hills to under 100 mm along the Dead Sea, and Britannica records that cultivation in the valley is restricted to irrigated land and oases such as Jericho.
What is kurkar?
The Arabic name for the porous calcareous sandstone that makes up the three ridges running parallel to the Gaza coast. It was laid down by wind in the Pleistocene and Holocene, and red soils called hamra lie between its layers. The Geography of Palestine article notes that apart from kurkar there is no other rock on the Gaza plain.
How much of the West Bank is in Area C?
About 60%, under the Oslo II agreement of 1995, which left Area C, apart from East Jerusalem, under the Israeli Civil Administration. Area A, about 18%, is under Palestinian civil and security control, and Area B, about 22%, under Palestinian civil control with joint security. The Palestine article records that 81% of designated protected areas are in Area C.