Palestine

Palestine is a region at the eastern end of the Mediterranean, in the southern Levant. The name has been used for different territorial units over time, so this entry separates the historical region from the territory claimed by the State of Palestine. In present-day usage the term most often refers to the West Bank, including East Jerusalem, and the Gaza Strip, which together cover about 6,020 square kilometres and are separated from each other by Israeli territory. The landscape ranges from the coastal plain of Gaza and the central highlands of the West Bank down to the Jordan Rift Valley and the shore of the Dead Sea, the lowest land surface on Earth. Its Mediterranean climate in the west and arid conditions in the east shape water availability, farming, and settlement.

Geography matters for Palestine in ways that go beyond the physical landscape. The region sits at a crossroads of three Abrahamic religions, and its scarce water resources, dense population, and land use are closely tied to its history and economy. Its borders, its status in international law, and the status of Jerusalem remain subjects of dispute, and sources differ on some basic figures such as population and highest elevation. An encyclopedic treatment therefore has to separate measurable physical facts from contested political claims and report each with its source.

This entry moves from location, relief, climate, and water to ecology, land use, and population distribution. It then covers historical and political geography, the economy and infrastructure, cultural and religious geography, environmental pressures, the history of mapping and geographic research, and finally the unresolved questions and data discrepancies that affect how the territory is described.

Name and Definition

The English name Palestine derives through Latin Palaestina from Greek Palaistinē, conventionally associated with Peleshet, the Hebrew name for Philistia, the southern coastal territory inhabited by the Philistines. The name’s geographical application extended beyond that coastal territory. In the fifth century BCE, Herodotus used Palaistinē in his Histories for a district of Syria between Phoenicia and Egypt; in Book 7, chapter 89, he described Phoenicians and “Syrians of Palestine” among the naval forces of Xerxes. This classical geographical usage preceded the Roman provincial designation by several centuries and did not denote a state with modern boundaries. (courses.lsa.umich.edu)

Under the Roman Empire, the province previously called Judaea acquired the official name Syria Palaestina in the second century CE, following the suppression of the Bar Kokhba revolt in 135. In late Roman and Byzantine administration, the name appeared in three provincial designations: Palaestina Prima, Palaestina Secunda, and Palaestina Tertia, also called Salutaris. Their combined extent included territories beyond the present West Bank and Gaza Strip. Following the seventh-century Arab conquest, the Arabic form Filasṭīn became the name of a military-administrative district, Jund Filasṭīn, administered initially from Lydda and subsequently from Ramla. These successive administrative uses retained the name while changing its territorial extent. (courses.lsa.umich.edu)

In modern administrative terminology, Palestine became the name of the British-mandated territory established after World War I. The League of Nations approved the Mandate for Palestine on 24 July 1922. Article 25 provided for different application of the mandate’s provisions east of the Jordan, and a memorandum approved on 16 September 1922 established the corresponding arrangements for Transjordan. Consequently, the mandate’s legal framework must be distinguished from Palestine’s separately administered territory west of the Jordan. A League of Nations account published in 1945 listed Palestine and Transjordan separately, assigning them approximately 27,009 and 90,000 square kilometres respectively. This administrative distinction explains why references to the mandate can have different geographical meanings. (un.org)

As a historical or scholarly regional name, Palestine has no single boundary valid for every period. It commonly encompasses the land associated with present-day Israel and the Palestinian territories, while some historical definitions also include areas east of the Jordan. Religious usage often overlaps with the Holy Land, especially in discussions of the Bible, pilgrimage, and the life of Jesus. The Jewish designation Eretz Yisrael, or Land of Israel, likewise expresses historical and religious conceptions whose boundaries need not coincide with those of a modern state. Geographical, scriptural, imperial-administrative, and contemporary diplomatic definitions therefore identify different territorial objects rather than interchangeable borders. (cambridge.org)

The State of Palestine is a more specific political designation. On 15 November 1988, the Palestine National Council, meeting in Algiers, proclaimed its establishment “in the land of Palestine with its capital at Jerusalem.” The declaration invoked United Nations General Assembly resolution 181 of 1947, which had proposed partition into Arab and Jewish states, but did not itself delineate the new state’s borders. The accompanying political communiqué called for Israeli withdrawal from territories occupied since 1967, including Arab Jerusalem, and negotiations based on Security Council resolutions 242 and 338. The declaration’s broad historical wording must therefore be distinguished from the territorial reference articulated in its accompanying diplomatic programme. (un.org)

In United Nations documents, the Occupied Palestinian Territory, also abbreviated OPT or oPt, comprises the West Bank, including East Jerusalem, and the Gaza Strip. General Assembly resolution 67/19, adopted on 29 November 2012, accorded Palestine non-member observer State status and reaffirmed the Palestinian people’s right to an independent state in the Palestinian territory occupied since 1967. Accordingly, State of Palestine names the political entity, whereas Occupied Palestinian Territory identifies its territorial reference in the language of occupation; neither expression is synonymous with every historical use of Palestine. (documents.un.org)

Location, Boundaries, and Administrative Extent

Palestine’s territorial extent comprises two geographically separate units in Western Asia: the West Bank, including East Jerusalem, and the Gaza Strip. They occupy part of the southern Levant, between the eastern Mediterranean coast and the Jordan Valley. Representative geographical coordinates are approximately $32^\circ00^\prime\text{N},\,35^\circ15^\prime\text{E}$ for the West Bank and $31^\circ25^\prime\text{N},\,34^\circ20^\prime\text{E}$ for Gaza; these locate the territories generally rather than defining their boundaries. Gaza lies southwest of the West Bank, with roughly 40 km of Israeli territory separating their nearest margins. This separation is a distance between territorial edges, not a city-to-city distance or the length of a travel route. (en.wikipedia.org)

The West Bank is landlocked, bordering Israel on its northern, western, and southern sides and Jordan to the east, along the Jordan River and the Dead Sea. Its perimeter with Israel is conventionally represented by the 1949 Armistice Line, commonly called the Green Line. East Jerusalem forms part of the West Bank in United Nations geographical usage, although Israel’s expanded Jerusalem municipal boundary and the separation barrier introduce additional administrative and physical divisions. The barrier does not coincide with the Green Line: OCHA reported in September 2024 that approximately 85 per cent of its route runs within the West Bank. Consequently, maps depicting the barrier, municipal limits, or access restrictions show different kinds of boundaries and should not be read as interchangeable representations of the territory’s outer extent. (en.wikipedia.org)

Gaza is an elongated coastal territory bordered by Israel to the north and east, Egypt to the southwest, and the Mediterranean Sea to the west. Its Egyptian boundary lies in the Rafah area. UNRWA describes the strip as approximately 41 km long and between 6 and 12 km wide, with about 40 km of Mediterranean coastline. Gaza therefore provides the coastal component of Palestine, whereas the West Bank reaches the Jordan Valley but has no Mediterranean frontage. The two territories share neither a land boundary nor a continuous Palestinian land corridor. (unrwa.org)

The frequently cited area of approximately 6,020 km² derives from the Palestinian Central Bureau of Statistics’ figures of 5,655 km² for the West Bank and 365 km² for Gaza, listed with a 2016 reference year. On that basis, the West Bank constitutes about 94 per cent of the combined area and Gaza about 6 per cent. Another PCBS presentation gives 5,660 km² for the West Bank, which produces a combined figure of 6,025 km²; the UN’s SDG 6 data portal likewise records 6,025 km² of land area for 2023. These closely spaced estimates should retain their source and reference year rather than be presented as a single exact measurement. A separate distinction is necessary between land area and totals that include inland water: the CIA’s 2020 West Bank entry listed 5,860 km² overall, comprising 5,640 km² of land and 220 km² of water, with explicit qualifications concerning territorial coverage. (microdata.pcbs.gov.ps)

Palestinian administrative geography divides these territories into 16 governorates, eleven in the West Bank and five in Gaza. The Gaza governorates are North Gaza, Gaza, Deir al-Balah, Khan Yunis, and Rafah; West Bank units include Jerusalem, Hebron, Bethlehem, Nablus, and Ramallah and al-Bireh. Governorate boundaries serve a different purpose from the Oslo-era division of the West Bank into Areas A, B, and C: the former organize territorial administration and statistics, while the latter delineate differing administrative and security arrangements. Neither division replaces the combined West Bank–Gaza geographical extent used in the area figures. (aman-palestine.org)

Relief, Landforms, and Geological Structure

The Gaza Strip occupies a low coastal plain whose relief consists of sandy beaches, dunes, elongated sandstone ridges, and intervening depressions containing alluvial deposits. Its characteristic rock is kurkar, a calcareous sandstone formed from wind-deposited sand subsequently cemented by carbonate. Alternating kurkar and reddish buried soils, locally called hamra, record successive periods of dune accumulation and soil formation during the Pleistocene and Holocene. A 2012 geomorphological study identified three northeast–southwest ridges broadly parallel to the Mediterranean shoreline: Sheikh Ejlin, Al Montar, and Bait Hanon. Wadi Gaza cuts across this landscape south of Gaza City, extending approximately 9 km through the strip to the sea. Its seasonal channel receives storm runoff from a much larger drainage basin, exceeding 3,500 km², in the northern Negev and Hebron Mountains; meanders, alluvial sediments, and Pleistocene windblown silt distinguish the wadi corridor from the surrounding dune terrain. (sciencedirect.com)

The West Bank’s central highlands form a north–south mountain spine, commonly described in terms of the Nablus, Jerusalem–Ramallah, and Hebron mountain segments. Much of the ridge lies above 700 m, with several summits exceeding 1,000 m. Valleys dissect the highlands and carry drainage eastward toward the Jordan depression or westward toward the Mediterranean. The bedrock comprises limestone, dolomite, chalk, and marl, folded into a broad anticlinorium: a composite structure containing numerous smaller upward and downward folds. Its main axis approximately follows the mountain spine, but subsidiary folds and faults complicate the structure locally. Resistant carbonate beds and softer intervening strata produce an uneven landscape of ridges, slopes, and incised valleys rather than a continuous level plateau. (etheses.durham.ac.uk)

Stone-built terraces give many western highland slopes a stepped appearance superimposed on the natural relief. At Battir, southwest of Jerusalem, dry-stone walls convert parts of a deeply dissected valley landscape into cultivation surfaces, some supplied by spring-fed channels. The site illustrates how terracing has modified steep hillsides without removing the underlying valley-and-ridge pattern. Elevation figures require distinction between individual summits and territorial definitions. Tell Asur, also rendered Al-Arsour, is listed at about 1,016 m in the British administration’s A Survey of Palestine, prepared in 1945–1946. A 2007 local geographical account identifies Mount Nabi Yunis at Halhul, north of Hebron, as the West Bank’s highest summit at approximately 1,030 m. The historical region also includes the higher hills of Upper Galilee: the British survey gives Jebel Jarmaq, or Mount Meron, an elevation of 1,208 m. Those Galilean heights lie outside the West Bank and Gaza Strip. (whc.unesco.org)

East of the central ridge, the terrain descends toward the Jordan Valley and Dead Sea. The southeastern highlands extend into the Judean Desert, or Jerusalem Wilderness, where rugged cliffs, caves, and deeply incised valleys—including Wadi al-Qelt and the Kidron Valley—characterize the relief. The Dead Sea shoreline forms the lowest exposed land on Earth. Its elevation is often rounded to approximately 430 m below mean sea level, but it is not a fixed topographic datum: the lake surface changes seasonally and has declined over time. NASA reported an approximate elevation of 435 m below sea level in July 2019, illustrating why measurements from different years cannot be treated as interchangeable. (yplus.ps)

The Jordan depression belongs to the Dead Sea Transform, a major boundary separating the Arabian plate to the east from the Sinai subplate to the west. Although conventionally called a rift valley, its dominant tectonic movement is left-lateral strike-slip, with the crustal blocks moving horizontally past one another. Extension at offsets between fault segments also permits localized subsidence, producing pull-apart basins. The Dead Sea occupies one such basin, whose buried structural extent is considerably greater than that of the present lake. Geological and geophysical investigations describe a basin approximately 150 km long and mostly 8–10 km wide, bordered by zones of normal faulting. Horizontal displacement along the transform and vertical subsidence within these fault-bounded depressions together explain the sharp contrast between the central highlands and the exceptionally low valley floor. (pubs.usgs.gov)

Climate and Meteorology

Western Palestine has a predominantly Mediterranean climate, with hot, dry summers and a cooler, wetter winter season. This seasonal pattern extends across the Gaza coastal plain and much of the West Bank, but temperatures and rainfall differ substantially with elevation and exposure. The State of Palestine’s 2016 Initial National Communication distinguishes five climatic and agro-ecological zones: the Coastal Plain, Semi-Coastal Plain, Central Highlands, Eastern Slopes, and Jordan Valley. Gaza has relatively temperate maritime conditions, the highlands have cooler winters with occasional frost, snow, and hail, and the southern Jordan Valley is warm and very dry. Most winter rainfall occurs between November and March; summer is largely rainless. (unfccc.int)

Rainfall generally decreases southward, although topography modifies this gradient. In Gaza, roughly 400 mm annually is representative of the northern coastal zone rather than the entire strip: a 2015 study by Salem S. Gharbia, Adnan Aish, and Francesco Pilla describes average annual rainfall declining from about 400 mm in the north to approximately 200 mm in the south. It identifies October–March as the principal rainy period, including the autumn onset of the wet season. Station observations illustrate both the spatial gradient and departures from these averages. In 2020, the Palestinian Central Bureau of Statistics (PCBS), using Meteorological Directorate data, reported 640.1 mm at Jabaliya in North Gaza, 531.8 mm at Al-Rimmal in Gaza City, 402.0 mm at Deir al-Balah, and 247.8 mm at Rafah. These are individual-year totals, not long-term climatic normals. (researchgate.net)

Across the West Bank, the west–east rainfall contrast reflects the passage of moist Mediterranean air over the central hills. Air rising over the western slopes cools and releases precipitation; the eastern slopes and Jordan Valley lie in a rain shadow and receive considerably less rain. A 1995 UNCTAD environmental study explicitly describes this concentration of rainfall on the western slopes. The contrast remains evident in station records: in 2020, Nablus received 849.0 mm and Ramallah 846.4 mm, compared with 150.9 mm at Jericho. In 2021, the corresponding totals were 681.1, 500.4, and 116.9 mm. Thus, the dry eastern zone cannot be characterized adequately by an average calculated for the West Bank as a whole. (un.org)

Temperature differences are similarly pronounced between the highlands and the low-lying Jordan Valley. PCBS annual mean temperatures for 2011–2024 ranged from 15.5 to 17.8 °C at Ramallah, 15.8 to 17.8 °C at Hebron, and 24.4 to 26.0 °C at Jericho, excluding years without observations. In 2024, the annual means were 17.6 °C at Ramallah, 17.2 °C at Hebron, 19.5 °C at Nablus, and 26.0 °C at Jericho. These values describe annual averages rather than summer maxima or winter minima. The relatively mild Gaza coast contrasts with both the colder uplands and the hotter valley, while occasional highland snowfall is a feature of winter weather rather than a regular condition throughout Palestine. (pcbs.gov.ps)

Rainfall varies markedly between years as well as between stations. Nablus recorded only 291.0 mm in 2017, followed by 873.0 mm in 2018; Ramallah increased from 252.4 to 804.0 mm over the same interval, and Jericho from 45.8 to 213.0 mm. The timing of observations also matters: the PCBS series reports totals by calendar year, whereas a winter rainy season crosses two calendar years. Its Gaza figures for 2023 cover only the period through 30 September and therefore are not directly comparable with complete annual totals. These distinctions are important when interpreting unusually wet or dry years and comparing observations from different meteorological stations. (pcbs.gov.ps)

Water Resources and Hydrology

The Jordan River links the principal surface-water features of historical Palestine within a drainage basin shared by Israel, Jordan, Lebanon, Palestine, and Syria. Its upper course passes through the Huleh Valley and Lake Tiberias, also called the Sea of Galilee; below the lake, it receives the Yarmouk River and continues along the eastern side of the West Bank to the Dead Sea. Lake Tiberias is a freshwater storage body, whereas the Dead Sea is a saline terminal lake with no natural outlet, losing water through evaporation. Lake Tiberias and the former Huleh Lake lie outside the West Bank and Gaza Strip, but form part of their wider regional hydrological setting. Huleh Lake and its surrounding marshes were largely drained in the 1950s; the surviving nature reserve contains permanent and intermittent water bodies rather than the original lake system. (waterinventory.org)

Upstream abstraction, reservoirs, and diversions have substantially altered the lower Jordan’s flow. The 2013 inventory prepared by the United Nations Economic and Social Commission for Western Asia and Germany’s Federal Institute for Geosciences and Natural Resources estimated annual discharge into the Dead Sea at 20–200 million cubic metres, compared with a historical flow of approximately 1,300 million cubic metres. Consequently, proximity to the river does not imply access to a dependable freshwater supply: the same inventory recorded no Palestinian abstraction from the Jordan itself. The lower river also receives agricultural drainage, saline water, and wastewater, making its water quality markedly different from that of the upper reaches. (waterinventory.org)

Groundwater is the principal local water resource of the West Bank. The Mountain Aquifer is conventionally divided into western, northeastern, and eastern basins. Its limestone and dolomite formations transmit water through fractures and karst conduits, with rainfall infiltrating exposed rock in the highlands and groundwater subsequently moving toward springs and pumping areas. In the Western Aquifer Basin, the 2013 regional inventory estimated that approximately 73% of recharge occurred in the West Bank, although much of the groundwater flowed westward beneath Israel. It adopted a mean annual recharge of 385 million cubic metres for 1970–2006, while emphasizing substantial year-to-year variation. Wells supply municipal networks and irrigated land; springs provide additional local supplies, especially where water-bearing formations intersect valley slopes. (nora.nerc.ac.uk)

Gaza relies on the shallow Coastal Aquifer and supplementary supplies rather than a perennial river. Wadi Gaza carries seasonal runoff from its catchment through the strip to the Mediterranean, with freshwater flows concentrated in winter. According to the Palestinian Central Bureau of Statistics (PCBS), groundwater abstraction in Gaza reached 189.4 million cubic metres in 2022, against an estimated sustainable yield of 50–60 million cubic metres annually. Pumping depresses groundwater levels and encourages saltwater intrusion, reducing the usable freshwater resource. Desalination therefore supplements well water and purchases from Israeli suppliers. These pre-war supply patterns were subsequently disrupted: UNEP’s September 2025 assessment reported severely limited freshwater supplies and damage to piped water and sewage systems. (paduco.ps)

Water statistics distinguish total supplied quantities from household consumption and potable availability. PCBS recorded 445.7 million cubic metres of available water in 2022: 298.5 million from wells, 38.8 million from springs, 9.6 million from desalination, and 98.8 million purchased from Israeli water companies. Average domestic consumption was 85.7 litres per person per day—86.4 in the West Bank and 84.6 in Gaza. These figures include water of differing quality and are not measurements of renewable freshwater availability per person. The statistical coverage also excludes the parts of Jerusalem annexed by Israel in 1967. (pcbs.gov.ps)

Allocation and development of shared groundwater were addressed in Article 40 of the Israeli–Palestinian Interim Agreement of 28 September 1995. It recognized Palestinian water rights in the West Bank while deferring their final settlement to permanent-status negotiations, and estimated additional Palestinian needs at 70–80 million cubic metres annually. It established an equally constituted Joint Water Committee whose decisions required consensus, covering matters including wells, extraction, and water-system development. The agreement envisaged additional abstraction from the eastern basin and supplementary Israeli deliveries. This framework made supply development dependent on agreed extraction quantities and coordinated projects, rather than simply on the location of recharge within the West Bank; the World Bank’s 2018 assessment described negotiated abstraction and imported water as central determinants of Palestinian supply. (nad.ps)

Ecosystems and Biodiversity

The western slopes and central highlands of the West Bank support Mediterranean woodland and scrub, including evergreen Palestine oak (Quercus calliprinos), Aleppo pine (Pinus halepensis), carob (Ceratonia siliqua), and pistachio species. Dense, woody maquis alternates with lower, more open garrigue containing rockroses and aromatic plants such as Syrian oregano (Origanum syriacum). These communities often occur alongside old olive groves rather than forming continuous forest. Eastward, woodland gives way to the Irano-Turanian steppe belt, where rainfall of approximately 150–300 millimetres annually supports dwarf shrubs, thorny vegetation, and broom-like Retama raetam. Still drier desert communities occupy parts of the Jordan Valley and Dead Sea margins, while springs sustain localized vegetation otherwise absent from the surrounding arid terrain. (environment.ps)

Gaza’s Mediterranean shore contains sandy beaches, dunes, and the coastal wetlands at the mouth of Wadi Gaza. Surveys describe common reed, giant reed, and Nile tamarisk around the wetland, with little egrets, black-winged stilts, common snipe, and other waterbirds using its aquatic and shoreline habitats. Gaza’s position between Eurasia and Africa makes it a passage and stopover area for migrating storks, cranes, raptors, ducks, and waders. (mahmiyat.ps) The Huleh—or Hula—wetlands belong to the broader historical region’s ecological geography but lie in northern Israel, outside the West Bank and Gaza Strip. Their lake and marshes were largely drained during the 1950s; the retained wetland required an artificial water regime to preserve open water and associated wildlife. Ornithologist Amotz Zahavi was among those advocating conservation during the drainage project. (biu.ac.il)

Endemism must be distinguished from occurrence within present administrative boundaries. The Gilboa iris (Iris haynei), for example, is a restricted-range regional plant occurring in both the West Bank and Israel, rather than a species exclusive to the Palestinian territories. (environment.ps) Small freshwater habitats also support locally rare species: Palestine’s sixth national report to the Convention on Biological Diversity identified the seasonal pond at Jinsafut as the only known West Bank locality of the eastern spadefoot toad (Pelobates syriacus). Research by Bethlehem University’s Palestine Institute for Biodiversity and Sustainability informed work with the Environment Quality Authority to protect this pond within the Wadi Qana conservation area. Its importance derives from its seasonal inundation and breeding habitat, not its size. (cbd.int)

Habitat loss results from urban expansion, vegetation clearance, overgrazing, roads, and other land conversion. Fragmentation adds a distinct pressure: barriers between surviving patches restrict animal movement to food and breeding sites and can reduce genetic exchange between populations. The 2015 national biodiversity report identified settlement development, bypass roads, and the West Bank separation barrier among the sources of fragmentation. (environment.ps) In Gaza, conflict has added extensive physical damage to vegetation. A UNEP assessment reported that satellite analysis through May 2025 indicated damage to 95.1 per cent of shrubland and 89 per cent of grassland or fallow land. These are land-cover damage estimates, not direct measurements of species extinction or population decline. (un.org)

Protected-area designation does not necessarily mean effective ecological management. The sixth national biodiversity report, published in 2021, recorded 51 protected areas covering approximately 515 square kilometres, or about 9 per cent of the territory. It also reported that most reserves fell within Area C, under Israeli civil and military control, limiting Palestinian agencies’ ability to manage the network. (cbd.int) Wadi Gaza was declared a nature reserve in June 2000 and submitted to the UNESCO World Heritage Tentative List in April 2012; this submission did not constitute World Heritage inscription. Its catchment extends beyond Gaza into the Negev and southern Hebron hills, making upstream conditions relevant to downstream conservation. (whc.unesco.org) A UNDP natural-park and greenway master plan subsequently provided a framework for rehabilitation, but UNEP’s June 2024 assessment reported that the conflict had reversed investments in restoring the coastal wetland. (undp.org)

Land Use and Agriculture

Agricultural land use differs sharply between the predominantly rain-fed West Bank highlands and the more intensively irrigated Gaza coastal plain and Jordan Valley. The Palestinian Central Bureau of Statistics (PCBS) recorded 1,021.5 km² cultivated with permanent and temporary crops in the agricultural year 2020/2021: 937.4 km² in the West Bank and 84.1 km² in Gaza. Of this cultivated area, approximately 77.5% was rain-fed. Permanent crops occupied 676.9 km², substantially more than temporary crops, reflecting the importance of orchards in the agricultural landscape. These census figures describe cultivation before the extensive disruption of Gaza’s farming systems following October 2023. (pcbs.gov.ps)

Olives are the principal tree crop. The 2021 agricultural census recorded approximately 575.2 km² of olive cultivation, including 552.5 km² in the West Bank; Jenin alone accounted for about 151.9 km². Grapevines accompany olives in the highlands, while citrus and vegetables are associated with irrigated production. Soil conditions vary rather than forming a uniformly fertile agricultural zone: the western foothills contain alluvial and heavier terra-rossa soils, whereas much of the central highland terrain has shallow soils over rock. The drier eastern slopes are used extensively for grazing. In the Jordan Valley, sandy and calcareous soils, hot summers, and mild winters support irrigated vegetables and subtropical fruit production, including crops harvested outside the main highland growing season. (pcbs.gov.ps)

Terraced agriculture has historically made steep highland slopes cultivable. Stone retaining walls create comparatively level plots, retain soil, and interrupt runoff, limiting soil erosion during heavy rainfall. Their effectiveness depends on maintenance: damaged walls and uncontrolled drainage leave cultivated slopes exposed to soil loss. Battir, southwest of Jerusalem, provides a documented example of this land-use system. Its dry terraces support olives and vines, while irrigated terraces produce market-garden crops. Springs feed collection pools and channels, and village families distribute the water through a time-based rotation. UNESCO inscribed the Battir cultural landscape on the World Heritage List in 2014, recognizing a farming landscape in which terraces and water-distribution infrastructure remain functionally connected. (fao.org)

Irrigation and greenhouse cultivation concentrate production on smaller areas. In 2020/2021, approximately 85.7% of Gaza’s cultivated land was irrigated, compared with 16.9% in the West Bank; within Jericho and Al-Aghwar governorate, the proportion was approximately 95.9%. Greenhouses and plastic tunnels, combined with drip irrigation, permit protected vegetable cultivation. However, production depends on reliable water, pumping energy, and access to agricultural infrastructure. The World Bank reported in 2023 that only about 75% of estimated agricultural irrigation-water demand was available, identifying high energy costs and restrictions on infrastructure development in Area C as additional constraints. (pcbs.gov.ps)

Agriculture’s economic weight must be distinguished from the wider economy and dated explicitly. PCBS reported that agriculture, forestry, and fishing contributed 6.0% of Palestinian gross domestic product in 2024, measured at constant 2015 prices. The sector’s value added nevertheless fell by 21.0% from 2023, including a 90.8% decline in Gaza; its increased GDP share therefore did not indicate expanding production. A separate PCBS employment series placed agriculture, hunting, and fishing at 6.2% of total employment in 2022. Dependence on rainfall exposes orchards and field crops to seasonal variability: prolonged drought reduces olive fruit yield, oil production, and oil quality, and influences the alternation between heavier and lighter harvests. (pcbs.gov.ps)

Physical damage and restricted access have substantially altered Gaza’s agricultural land availability. An FAO–UNOSAT assessment published on August 18, 2026, using conditions assessed as of June 24, found that 4,091 hectares—27% of Gaza’s cropland—were accessible, but only 448 hectares, approximately 3% of the total, were both accessible and undamaged. Another 3,643 accessible hectares required rehabilitation. The assessment also identified shortages of seeds, fertilizers, irrigation equipment, fuel, and other inputs, illustrating why accessible land alone does not establish the capacity to resume cultivation. (fao.org)

Population and Settlement Patterns

The Palestinian Central Bureau of Statistics (PCBS) estimated the Palestinian population of the West Bank and Gaza Strip at 5.48 million in mid-2023, 5.49 million at the end of 2024, and 5.56 million at the end of 2025. The last figure comprised 3.43 million in the West Bank and 2.13 million in Gaza. These dated estimates should be distinguished from projections prepared before the war that began in October 2023: PCBS’s revised end-2025 Gaza estimate was approximately 254,000 below the previously projected population, reflecting deaths, departures, and reduced births. Using a territorial area of approximately 6,025 km², the end-2025 total implies an average density of about 923 persons per km². Gaza’s corresponding density was approximately 5,800 persons per km² across 365 km², although this territorial average conceals much higher concentrations in inhabited neighbourhoods and displacement sites. (microdata.pcbs.gov.ps)

The 2017 census classified 77% of the population as living in urban localities, 15% in rural localities, and 8% in refugee camps. These are statistical settlement categories rather than a simple distinction between built-up and unbuilt land: camps may adjoin or form part of urban agglomerations while remaining separately classified. Housing data illustrate differences in residential concentration. In 2017, average occupancy was 1.3 persons per room in the West Bank and 1.6 in Gaza; 5% of West Bank households and 12% of Gaza households occupied dwellings with at least three persons per room. The corresponding proportion in refugee camps was 13%. (microdata.pcbs.gov.ps)

Palestinian demography is characterized by a young age structure, with Gaza younger than the West Bank. PCBS’s 2023 estimates placed median age at 22.5 years in the West Bank and 19.5 in Gaza. Estimated crude birth rates for that year were respectively 26.6 and 32.0 births per 1,000 inhabitants; these were demographic estimates, not measurements of wartime birth patterns. Before the war, infant mortality also differed: PCBS reported 11.7 deaths per 1,000 live births in the West Bank and 12.7 in Gaza for 2019–2020. Revised end-2025 estimates still showed children under 15 constituting 35% of the West Bank population and 39% of Gaza’s; people aged 65 or older represented less than 4% of the combined population. (pcbs.gov.ps)

Internal migration and urbanization have reinforced concentrations around employment and service centres. UN-Habitat identifies the concentration of economic activity in major towns, together with comparatively limited rural investment, as drivers of rural-to-urban migration. Its State of Palestine: Cities Report 2016 describes the growth of the Ramallah–al-Bireh–Beitunia urban area through natural increase, migration from elsewhere in the West Bank, and the settlement of Palestinian returnees after the Oslo agreements. Expansion across neighbouring municipal boundaries has encouraged joint urban planning, while land scarcity and territorial fragmentation constrain where additional housing can be built. (unhabitat.org)

The United Nations Relief and Works Agency for Palestine Refugees in the Near East (UNRWA) recognizes 19 refugee camps in the West Bank and eight in Gaza. West Bank camps are distributed around centres including Jenin, Tulkarm, Nablus, Jerusalem, Bethlehem, Hebron, and Jericho. Gaza’s camps extend from Jabalia and Beach camp in the north through Nuseirat, Bureij, Maghazi, and Deir al-Balah to Khan Younis and Rafah. Refugee status does not imply camp residence: UNRWA reports that approximately one-quarter of registered refugees in the West Bank live in recognized camps. These established localities must also be distinguished from the emergency displacement sites created during the Gaza war. On 31 December 2024, the UN estimated that approximately 1.9 million people—about 90% of Gaza’s population—were internally displaced, many repeatedly; destruction of homes and Israeli-issued evacuation orders substantially altered the distribution of residents within the territory. (unrwa.org)

Historical Geography

Early settlement was closely associated with dependable water supplies and routes through the Jordan Valley and central highlands. At Tell es-Sultan, northwest of modern Jericho, the perennial spring of ‘Ain es-Sultan supported a sizeable permanent settlement by the ninth to eighth millennia BCE; surviving structures include a wall, ditch, and stone tower. Later Bronze Age occupation produced a fortified Canaanite city-state. In the highlands, Tell Balata, identified with ancient Shechem, occupied the passage between Mount Ebal and Mount Gerizim, where north–south and east–west routes intersected. Its Middle Bronze Age walls, monumental gates, and imported objects document both defensive organization and regional exchange. Gibeon’s rock-cut pools and spring tunnels illustrate how engineered water access sustained other highland settlements. (whc.unesco.org)

Under the Roman Empire, urban foundations and provincial administration reorganized this settlement network. Emperor Vespasian founded Flavia Neapolis in 72 CE west of ancient Shechem; its name subsequently developed into Nablus. The Roman town therefore represents continuity within the same valley rather than uninterrupted occupation of one archaeological site. By the fifth century, under the Byzantine Empire, the region was divided into Palaestina Prima, broadly covering Judaea, Samaria, and the central coastal area; Palaestina Secunda, around Galilee and the upper Jordan; and Palaestina Tertia, encompassing southern territories including Idumaea and Moab. These units extended beyond the present West Bank and Gaza Strip. Christian patronage also strengthened pilgrimage centres: Bethlehem’s first Church of the Nativity was completed in 339, and its sixth-century replacement preserved elements of the earlier building. (getty.edu)

Following the Muslim conquests of the seventh century, military-administrative districts replaced Byzantine provinces. Jund Filastin covered much of southern Palestine, while Jund al-Urdunn incorporated northern areas. In the early eighth century, the governor Sulayman ibn Abd al-Malik established Ramla as Jund Filastin’s capital. Its planned mosque, palace, markets, and workshops created a new administrative and manufacturing centre near existing inland routes. Crusader rule subsequently organized territory around the Kingdom of Jerusalem and its ecclesiastical and lordship centres, linking coastal towns with inland religious destinations. Bethlehem’s surviving complex records this period through church embellishment and the development of convents around the Nativity church. (doria.fi)

The Ottoman Empire incorporated the region in 1516–1517, but its administrative boundaries changed repeatedly rather than forming a single enduring province of Palestine. In the late nineteenth century, Jerusalem constituted a separate district reporting directly to the imperial government; Nablus and Acre became districts of the Beirut province established in 1888. Highland towns retained commercial and religious functions across these reorganizations. Hebron stood at the intersection of caravan routes connecting southern Palestine, Sinai, eastern Jordan, and northern Arabia. Its old town preserves a predominantly Mamluk street and neighbourhood structure, extended during Ottoman rule through additional upper storeys and surrounding development. Together with Roman-origin Nablus and the successive church complexes of Bethlehem, it illustrates urban persistence through rebuilding and shifts in administrative authority. (palquest.org)

British rule after World War I replaced Ottoman districts with a mandate administration. The League of Nations approved the Mandate for Palestine on 24 July 1922; a memorandum approved on 16 September provided for separate administration in Transjordan, east of the Jordan–Dead Sea–Wadi Araba line. On 29 November 1947, the United Nations General Assembly recommended partition into Arab and Jewish states, with Jerusalem under an international regime. The ensuing war and the 1949 armistice arrangements produced a different territorial pattern: Israel controlled most of former Mandate Palestine west of the Jordan, Jordan controlled the West Bank and East Jerusalem, and Egypt administered the Gaza Strip. The war also displaced large numbers of Palestinians, reshaping settlement through refugee concentrations outside former home towns and villages. (digitallibrary.un.org)

In June 1967, Israel occupied the West Bank, including East Jerusalem, and the Gaza Strip. These two geographically separate territories consequently became the principal territorial reference for subsequent discussions of Palestinian statehood. Their outlines arose from twentieth-century warfare and armistice arrangements, not from the boundaries of Roman provinces, early Islamic districts, or Ottoman administrative units. Jerusalem’s division between 1948 and 1967, followed by Israeli occupation of its eastern sector, likewise altered access and administrative relationships within a historically interconnected highland urban network. (un.org)

Political Geography and International Status

On 15 November 1988, the Palestine National Council, meeting in Algiers, proclaimed the State of Palestine, with Jerusalem as its capital. The declaration invoked United Nations General Assembly Resolution 181 (II), the 1947 partition resolution, as an international basis for Palestinian statehood, but did not delimit precise borders. The accompanying political communiqué called for negotiations under Security Council Resolutions 242 and 338 and Israeli withdrawal from territories occupied in 1967. On 29 November 2012, General Assembly Resolution 67/19 accorded Palestine non-member observer State status by 138 votes to nine, with 41 abstentions. It reaffirmed the Palestinian right to independence in the territory occupied since 1967, including East Jerusalem; this territorial reference encompasses the West Bank and Gaza Strip rather than the whole historical region of Palestine. (un.org)

Diplomatic recognition is distinct from both UN membership and effective territorial control. By late September 2025, approximately 157 of the 193 UN member states recognized Palestine; recognitions announced that month included those of France, the United Kingdom, Canada, Australia and Portugal. The Holy See, which is not a UN member state, also recognizes Palestine, a position explicitly reflected in its comprehensive bilateral agreement signed on 26 June 2015. Recognition statements do not necessarily settle boundaries: the United Kingdom, for example, recognizes statehood over provisional borders based on the 1967 lines, subject to agreed land swaps and future negotiations. These lines therefore serve as a diplomatic reference rather than a mutually agreed final frontier. (en.wikipedia.org)

States withholding recognition have not adopted a single common position. In explaining its veto of Palestine’s UN membership application on 18 April 2024, the United States maintained that Palestinian statehood should emerge through direct negotiations with Israel. Israel opposed the application, with its representative arguing that the Palestinian Authority did not meet the requirements for statehood. The proposed Security Council recommendation received 12 affirmative votes, two abstentions and the American veto. On 10 May 2024, the General Assembly subsequently adopted Resolution ES-10/23, expanding Palestine’s participation rights, including introducing proposals and being seated alphabetically among member states. It expressly withheld a General Assembly vote and did not itself confer membership, which requires a Security Council recommendation. (press.un.org)

The Oslo arrangements created an interim administration rather than resolving sovereignty. The 1993 Declaration of Principles and subsequent agreements established the Palestinian Authority and transferred specified responsibilities from Israel. The agreement signed on 28 September 1995 divided the West Bank, excluding East Jerusalem, into Areas A, B and C. Following subsequent redeployments, their approximate shares became 18%, 22% and 60%, respectively. Area A has Palestinian civil administration and internal-security responsibilities; Area B combines Palestinian civil administration with divided Israeli–Palestinian security responsibilities; Israel retains extensive civil and security control in Area C, including planning and construction. The agreement reserved Jerusalem, settlements, borders and other permanent-status questions for later negotiations. These categories describe jurisdictional arrangements, not three separate sovereign territories. (un.org)

A further administrative division developed in June 2007. Following armed conflict between Hamas and Fatah, Hamas assumed control of Gaza by 15 June, while President Mahmoud Abbas declared a state of emergency and formed a separate Palestinian Authority government. Gaza consequently developed a Hamas-led de facto administration separate from the Authority’s administration in the West Bank. This political separation did not constitute an internationally recognized partition: UN resolutions continue to treat Gaza and the West Bank, including East Jerusalem, as the territorial components of Palestinian statehood. (un.org)

International legal assessments distinguish occupation from sovereign title. In its advisory opinion of 19 July 2024, the International Court of Justice treated the occupied Palestinian territory as a single territorial unit and concluded that Israel’s continued presence there was unlawful and should end as rapidly as possible. It held that occupation cannot transfer sovereignty to the occupying power and that the Oslo agreements did not authorize annexation. Israel’s assertion that East Jerusalem forms part of its sovereign capital contrasts with the Court’s treatment of it as occupied territory. The opinion was advisory rather than a binding judgment between litigating states; it neither negotiated a final border nor replaced the unresolved permanent-status arrangements. (icj-cij.org)

Economic Geography and Trade

Services dominate the Palestinian economy, although statistical classifications distinguish a narrow services category from commerce, transport, communications and other service-producing activities. The Palestinian Central Bureau of Statistics (PCBS), in its December 2022 preliminary assessment, estimated that the broad “services and other branches” grouping contributed 61.6% of gross domestic product (GDP), compared with 10.8% for industry and 4.6% for construction, at constant 2015 prices. The broad grouping included public administration, finance, wholesale and retail trade, transport and communications, as well as electricity and water supply. These figures describe the economy before the war beginning in October 2023; the underlying national accounts exclude the parts of Jerusalem annexed by Israel in 1967. (pcbs.gov.ps)

The West Bank and Gaza subsequently experienced markedly different contractions. PCBS’s Performance of the Palestinian Economy, 2024 reported preliminary real GDP declines of 17.0% in the West Bank and 83.2% in Gaza, producing a combined decline of 26.6%. Industrial value added—including manufacturing—fell by 21.7% and 92.7%, respectively. In the West Bank, industry still contributed 11.5% of GDP in 2024, and wholesale and retail trade contributed 19.3%; Gaza’s corresponding shares were only 3.2% and 4.0%. Gaza’s narrow “services and other branches” category accounted for 87.2% of its remaining GDP, reflecting the disproportionate collapse of other activities rather than service-sector expansion. These estimates were based on quarterly accounts and remained subject to revision. (pcbs.gov.ps)

The labour market combines local employment with substantial dependence on jobs in Israel and Israeli settlements. PCBS’s 2022 Labour Force Survey recorded 34.1% of employed people in services and other branches and 22.3% in commerce, hotels and restaurants. Employment in Israel and settlements represented 17.0% of total employment. Cross-border wages therefore transmit changes in access directly into household income and domestic demand: in the second quarter of 2025, the World Bank reported average daily wages of NIS243.4 for Palestinians working in Israel, against NIS134.8 in the West Bank. Its May 2026 economic monitor recorded a fall in employment in Israel and settlements from 177,400 workers in the third quarter of 2023 to 24,000 in the fourth quarter; numbers recovered to 51,800 by the fourth quarter of 2025, largely through workers without permits rather than a formal reopening of access. (pcbs.gov.ps)

Israel is also the principal market for registered merchandise exports and a major supplier of imports. PCBS’s December 2024 figures illustrate this concentration: Israel received 84% of exports and supplied 55% of imports that month. Total registered goods exports were US$164.2 million, compared with imports of US$598.6 million, leaving a monthly deficit of US$434.4 million. These are merchandise figures for a single month, not annual totals or a balance including services. Fiscal dependence accompanies commercial dependence: under the Paris Protocol, Israel collects import duties and much of the value-added tax on behalf of the Palestinian Authority, with monthly transfers prescribed after a 3% collection fee. Interruptions to those transfers affect public expenditure alongside disruptions to goods and labour flows. (pcbs.gov.ps)

Restrictions on movement, production inputs and resource access shape both operating costs and investment opportunities. UNCTAD’s January 2024 assessment described the restrictions on movement and goods trade imposed on Gaza, intensified after 2007, as effectively constituting a blockade. In the West Bank, the World Bank’s Area C and the Future of the Palestinian Economy estimated that removing constraints on Palestinian economic activity in Area C could generate approximately US$3.4 billion in additional annual output, including indirect effects—equivalent to 35% of Palestinian GDP in 2011. This was a counterfactual estimate, not a measured contemporary annual loss. The activities examined included agriculture, Dead Sea minerals, stone quarrying, construction, tourism and telecommunications, illustrating how access to land and resources limits diversification beyond services and trade. (unctad.org)

Cities, Transport, and Infrastructure

Ramallah, together with adjoining Al-Bireh, functions as the Palestinian Authority’s administrative centre and a major concentration of financial institutions, offices, and commercial services. Its importance is institutional rather than a consequence of being the largest city. Gaza City, Nablus, Hebron, and Bethlehem constitute other major urban centres. Infrastructure planning often treats these cities and their neighbouring municipalities as metropolitan areas rather than isolated municipal jurisdictions: in 2021, a World Bank programme supported all five urban areas with a US$5 million grant for joint planning, policies, and services. This approach addresses the extension of built-up areas across municipal boundaries and the resulting need to coordinate roads, drainage, and service networks. (en.wikipedia.org)

The West Bank road network combines routes serving Palestinian towns with roads connecting Israeli settlements to one another and to Israel. Road 60 is a principal north–south artery, but proximity to it does not necessarily provide unrestricted access: gates, blocked junctions, checkpoints, and permit requirements determine which routes travellers can use. OCHA’s September 2024 assessment identified at least 129 movement obstacles within a 300-metre buffer along 180 kilometres of this road. Such restrictions funnel traffic onto longer secondary routes and affect access to employment, hospitals, schools, and markets. A subsequent survey, conducted in December 2025 and published in April 2026, recorded 925 movement obstacles across the West Bank, including East Jerusalem; the total encompasses several kinds of physical obstruction, not simply staffed checkpoints. (ochaopt.org)

Electricity infrastructure depends heavily on external supply. A World Bank assessment published in 2025 reported that Israeli imports supplied more than 95 percent of West Bank electricity demand, which had reached nearly 1,300 megawatts. Before October 2023, Gaza’s demand routinely exceeded 500 megawatts, whereas available supply was generally only 180–200 megawatts. Its diesel-fired power plant had a nominal capacity of 140 megawatts but normally generated 60–80 megawatts because of fuel constraints; imports from Israel provided up to another 120 megawatts. These figures describe the pre-war supply structure, rather than subsequent operating conditions. Dependence on imported electricity and fuel links the functioning of the electrical grid to border access as well as to local generating and distribution capacity. (documents1.worldbank.org)

Water and sewage networks likewise require both physical investment and sustained operating finance. A February 2023 World Bank report recorded piped-water connections for more than 95 percent of the population, while noting that supply remained intermittent and dependence on purchases from Israel’s Mekorot water company was increasing. External funding has supported treatment facilities and their maintenance: in June 2020, the World Bank approved US$10 million for North Gaza wastewater operations, complemented by US$3.7 million from donor partners, with an estimated 400,000 beneficiaries. The infrastructure damage assessment released jointly by the World Bank, United Nations, and European Union in February 2025, covering October 2023–October 2024, estimated Gaza’s transport damage at approximately US$2.5 billion and reported damage or destruction affecting 81 percent of its classified primary, secondary, and tertiary road network. (documents1.worldbank.org)

External mobility is channelled through a limited number of crossings. The Allenby, or King Hussein, Bridge provides a route between the West Bank and Jordan. Gaza’s established gateways include Rafah towards Egypt and Erez and Kerem Shalom towards Israel, historically differentiated between passenger movement and freight. Their operating status and permitted uses have changed during hostilities. OCHA’s July 2025 account, for example, recorded Rafah as closed and identified Kerem Shalom and additional northern and southern entry points for goods. Consequently, an open crossing does not itself guarantee onward delivery: collection capacity, road access, and security conditions within Gaza also determine whether cargo reaches its destination. (gov.il)

Air and maritime infrastructure has not provided a durable alternative to these land gateways. Gaza International Airport opened on 24 November 1998, with Yasser Arafat presiding over its inauguration, but ceased operating in 2001; its subsequent destruction prompted condemnation by the International Civil Aviation Organization in March 2002. A proposed deep-water seaport south of Gaza City was intended to give Palestinian merchandise trade direct maritime access. UNCTAD’s 2003 transport study recorded that the project had been suspended following the outbreak of conflict in September 2000, leaving Palestinian overseas freight dependent on external ports and connecting land routes rather than the planned Gaza terminal. (en.wikipedia.org)

Religious and Cultural Geography

Jerusalem’s Old City concentrates sacred places of Islam, Christianity, and Judaism within a compact urban landscape: the Haram al-Sharif/Temple Mount precinct, with the Dome of the Rock and al-Aqsa Mosque; the Western Wall; and the Church of the Holy Sepulchre, associated in Christian tradition with Jesus’s crucifixion and burial. These sites connect worship to the city’s religious quarters and pedestrian routes. Bethlehem’s Church of the Nativity stands over the grotto traditionally identified as the birthplace of Jesus Christ. Its UNESCO-listed pilgrimage route follows Star Street toward Manger Square, incorporating streets used for Christmas processions into the everyday commercial and residential fabric. Custody of the church is shared by Greek Orthodox, Armenian, and Franciscan communities, making conservation dependent on cooperation among religious custodians and public authorities. (whc.unesco.org)

In Hebron, the Ibrahimi Mosque/Tomb of the Patriarchs encloses the place traditionally associated with the burial of Abraham and members of his family. The old town developed around this pilgrimage centre, with limestone houses, markets, and quarters organized partly by religious and occupational affiliation. Near Nablus, Mount Gerizim is the sacred mountain of the Samaritan community; ceremonial movement to and around its summit preserves a distinct religious geography overlooking the city and ancient Tell Balata. Samaritan worship should not be treated simply as a subdivision of the region’s Jewish population: it represents a separate living religious tradition centred on Gerizim rather than Jerusalem. (whc.unesco.org)

Religious population figures depend on the population and territory counted. The Palestinian Central Bureau of Statistics’ 2017 census religion table, excluding the J1 portion of Jerusalem, recorded 4,615,683 Muslims and 46,850 Christians—approximately 98.9% and 1.0%, respectively, of the 4,665,426 people tabulated. These figures describe the Palestinian census population, not everyone geographically resident in the West Bank. Israeli statistics separately recorded 455,700 Jews in the “Judea and Samaria Area,” excluding East Jerusalem, on 31 December 2021. That figure uses a population-group classification rather than a measure of religious observance and cannot be combined directly with the earlier Palestinian census to produce a single religious distribution. (database.ours.foundation)

Arabic is designated the official language in the Palestinian Basic Law. Arabic poetry also connects cultural identity with places extending beyond today’s administrative territories: Mahmoud Darwish (1941–2008), born in al-Birwa in Galilee, repeatedly explored homeland, displacement, and exile. Material traditions preserve more localized associations. Palestinian embroidery, inscribed on UNESCO’s Intangible Cultural Heritage Representative List in 2021, developed in rural communities and continues in towns, refugee camps, and the diaspora. Dress designs draw on surrounding environments and transmit skills between generations. Cuisine likewise has recognizable urban and agricultural associations: Nablus is particularly associated with knafeh, while musakhan combines chicken, onions, sumac, and taboon bread with the olive-oil-based food culture of the region. (tscc.pna.ps)

By October 2026, UNESCO listed six World Heritage properties under the State of Palestine: Bethlehem’s Nativity Church and pilgrimage route (2012), Battir’s cultural landscape (2014), Hebron’s old town (2017), Ancient Jericho/Tell es-Sultan (2023), Saint Hilarion Monastery/Tell Umm Amer in Gaza (2024), and Sebastia (2026). Jerusalem’s Old City and its Walls, inscribed in 1981 following a nomination by Jordan, appears separately. Battir illustrates heritage as a working landscape: spring-fed channels, pools, and cultivated terraces depend on continuing community maintenance. Nabulsi soap making, inscribed as intangible heritage in 2024, similarly links cultural practice to olive cultivation through the use of olive oil, water, and lye and the transmission of craft skills in families and workshops. (whc.unesco.org)

Heritage management combines national institutions, municipalities, religious custodians, and community organizations. Under the 2018 Tangible Cultural Heritage law, Hebron’s listed property is managed by the Ministry of Tourism and Antiquities in cooperation with the Ministry of Awqaf, municipality, Hebron Rehabilitation Committee, and local community. In Bethlehem, the Centre for Cultural Heritage Preservation works with municipal and ministerial bodies on conservation of the historic urban setting. The Palestinian Museum in Birzeit connects collections and exhibitions with landscape interpretation: its terraced architecture and gardens, designed by Lara Zureikat, present cultivated and wild plants as part of Palestine’s agricultural and cultural history. (whc.unesco.org)

Environmental Pressures and Climate Change

Water scarcity reflects both rising demand and deterioration of groundwater resources. In Gaza, population growth and withdrawals for domestic use and irrigation have placed sustained pressure on the shallow coastal aquifer. Pumping lowers groundwater levels, encouraging saltwater intrusion from the Mediterranean and the movement of deeper saline water into freshwater-bearing layers. Untreated sewage introduces additional contamination. In February 2020, the World Bank reported that 97% of the available groundwater was undrinkable; this was a dated assessment of groundwater quality, not a measure of all water subsequently supplied through desalination or imports. The same report identified over-pumping and sewage contamination as principal causes of deterioration. (documents1.worldbank.org)

Climate change adds pressure by altering rainfall, recharge, and the frequency of extreme heat. The World Bank’s 2023 West Bank and Gaza Country Climate and Development Report estimated that a 10% decline in average rainfall could reduce aquifer recharge by 14–24%, while a 15% decline could reduce it by 28–50%. Its projections indicated increasing numbers of days above 35°C across Palestinian cities and worsening drought, particularly in southern areas toward the end of the century. These changes threaten rain-fed agriculture and increase exposure among agricultural workers, other outdoor labourers, older people, and young children. Households without reliable electricity or cooling face additional difficulty managing extreme heat. The report distinguished between emissions scenarios: precipitation changes were less uniform than the projected warming, with some Gaza cities showing slight rainfall increases under a low-emissions pathway but decreases under higher-emissions pathways. (documents1.worldbank.org)

Flooding can occur despite chronic water scarcity. Intense rainfall generates rapid runoff where urban surfaces limit infiltration, while undersized drains and accumulations of waste restrict its discharge. Palestine’s 2016 National Adaptation Plan identified inadequate storm-water drainage and limited municipal resources as important contributors to urban flood vulnerability. A concrete example occurred in December 2013, when four days of torrential rain inundated parts of Gaza: UNICEF subsequently reported that approximately 10,000 people had been evacuated to temporary shelters or relatives’ homes. Displacement compounds exposure because makeshift shelters offer limited protection from rain and cold; UNICEF documented these conditions among displaced families in Gaza in December 2023. These events illustrate vulnerability to weather hazards without establishing that an individual storm was caused by climate change. (unfccc.int)

Gaza’s coastal environment combines long-standing wastewater pollution with risks from sea-level rise. In 2017, UNICEF reported that more than 108,000 cubic metres of raw or poorly treated sewage entered the Mediterranean each day amid electricity shortages. Conflict subsequently disrupted treatment much more extensively: UNEP’s assessment of 18 June 2024 reported that Gaza’s five wastewater treatment plants had shut down, with sewage contaminating beaches, coastal waters, soils, and freshwater. It also identified rubble, hazardous waste, and dust as major urban environmental pressures. UNEP distinguished these documented disruptions from possible chemical and heavy-metal contamination of the coastal aquifer, which required sampling to establish its extent. Separately, the World Bank’s climate assessment identified rising sea levels and saltwater intrusion as threats to Gaza’s groundwater quality. (unicef.org)

Adaptation planning addresses water, agriculture, drainage, buildings, and coastal management together. The National Adaptation Plan was approved by relevant Palestinian ministries in May 2016; the updated 2021 climate contribution subsequently set out internationally supported actions across twelve highly vulnerable sectors, including a conditional target for 50% of farms to apply climate-smart agriculture by 2040. International cooperation has also financed water-supply diversification: in February 2020, the World Bank and partners announced US$117 million for associated works within the Gaza Central Desalination Program, whose planned plant had an initial capacity of 55 million cubic metres annually. The programme linked desalination, purchased water, groundwater, reservoirs, and distribution networks rather than relying on a single source. Such plans depend on functioning infrastructure, finance, and operational coordination; the announced capacities and targets describe planned interventions, not verified post-conflict service levels. (unfccc.int)

History of Geographic Research and Mapping

Claudius Ptolemy’s second-century Geography placed Palestine within a coordinate-based description of the known world: Book V included a regional account of Palestine, while the work as a whole supplied latitude and longitude values and instructions for constructing map projections. Maps subsequently attributed to Ptolemy were often later cartographers’ reconstructions from these coordinates, rather than surviving drawings made by him. A different geographical tradition developed in Eusebius of Caesarea’s early-fourth-century Onomasticon, a gazetteer connecting biblical place-names with contemporary settlements, landmarks, and distances. Jerome’s Latin translation and revisions transmitted this material to western readers. The sixth-century Madaba mosaic map drew extensively on the Onomasticon, combining biblical identifications with representations of contemporary towns and religious sites. These sources preserve valuable geographical information, but their coordinate catalogues, textual descriptions, and pictorial conventions require different methods of interpretation. (penelope.uchicago.edu)

Nineteenth-century research introduced systematic instrumental surveying. Pierre Jacotin’s maps, based on Napoleon’s 1799 campaign, provided an early triangulation-based representation at 1:100,000. The Palestine Exploration Fund, founded in 1865, subsequently sponsored the Survey of Western Palestine, whose principal surveyors included Royal Engineers officers Claude Reignier Conder and Horatio Herbert Kitchener. The project extended from 1871 to 1878, with the published map identifying field surveys undertaken in 1872–1877. Its 26 sheets appeared in 1880 at 1:63,360—one inch to one mile—and were accompanied by descriptive memoirs. Mapping brought settlements, roads, relief, water sources, and archaeological remains into a common topographical framework. Research comparing these maps with later surveys has also examined their positional accuracy and their usefulness for reconstructing historical settlement and landscape change. (sciencedirect.com)

During World War I, aerial photography became an important means of revising existing maps and producing more detailed military coverage. Photographic strips and mosaics supported map compilation at scales including 1:20,000 and 1:40,000. Under the British Mandate, the Survey of Palestine, established in 1920, introduced a new triangulation network and developed cadastral and topographical surveying. Its maps served distinct purposes: cadastral surveys documented land parcels for settlement and registration, whereas topographical sheets represented terrain, settlements, and communications. Surviving accounts show that aerial photographs were used at least for map revision, although the documentary record of that work is incomplete. Mandate-era sheets at scales up to 1:20,000 now provide detailed evidence of the landscape before 1948. (palestine-studies.org)

Digitization has made historical mapping usable within geographic information systems rather than solely as individual printed sheets. Palestine Open Maps, initiated in March 2018, combines hundreds of Mandate-era sheets into navigable layers and brings them together with the 1945 Village Statistics, historical aerial photographs, oral histories, and present-day spatial data. This enables comparison of former village locations, roads, property boundaries, and subsequent urban development. Historical GIS research has likewise evaluated successive maps against modern geographical references, distinguishing actual landscape change from discrepancies in the original surveys. The date, scale, coverage, and spatial accuracy of each source remain important when interpreting apparent changes between map layers. (palopenmaps.org)

Recent remote sensing research combines satellite observations with field and administrative data. A 2010 doctoral study by Adla Jamil Khalaf mapped West Bank groundwater recharge by integrating satellite-derived land cover, evapotranspiration, rainfall, and elevation information with hydrogeological data in a GIS model. Research at Palestine Polytechnic University has used Landsat and Sentinel multispectral imagery to classify land cover and detect urban change. Such approaches turn repeated observations into spatially comparable datasets, while water-resource estimates depend on the accompanying hydrogeological model rather than satellite imagery alone. (etheses.durham.ac.uk)

Satellite assessments also illustrate the importance of dated observations and explicit validation limits. In an assessment published on 1 May 2024, the United Nations Satellite Centre used 10-metre Sentinel-2 imagery and vegetation-index analysis to compare Gaza’s agricultural condition with preceding seasons. It reported substantially reduced crop health and density in approximately 45% of permanent crop fields and arable land in April 2024. The product also incorporated 50-centimetre WorldView-2 imagery, but explicitly described its findings as preliminary and not field-validated. These measurements document remotely detected vegetation change; their interpretation depends on the comparison period, classification method, image resolution, and availability of independent ground evidence. (unosat.org)

Disputes, Data Discrepancies, and Open Questions

Borders, Jerusalem, refugees, and resource allocation remain distinct questions rather than consequences automatically settled by recognition of Palestinian statehood. The Palestine Liberation Organization’s published negotiating position seeks a state in the West Bank and Gaza Strip, with East Jerusalem as its capital, based on the lines preceding June 1967; it allows consideration of minor, equitable, mutually agreed territorial exchanges. Israeli negotiating positions have varied between governments. At the opening of permanent-status negotiations on 8 November 1999, Prime Minister Ehud Barak’s guidelines rejected a return to the 1967 lines, retained a united Jerusalem as Israel’s capital, and sought incorporation of most settlements. These were negotiating positions, not agreed boundaries. Separately, the International Court of Justice concluded on 19 July 2024 that Israel’s continued presence in the occupied Palestinian territory was unlawful and should end as rapidly as possible; that advisory opinion did not draw a negotiated final border. (nad.ps)

Jerusalem and refugee claims involve different geographic reference points. The Palestinian claim concerns East Jerusalem as the national capital, whereas Israel’s claim encompasses the unified city. The United Nations Committee on the Exercise of the Inalienable Rights of the Palestinian People treats East Jerusalem as occupied territory and rejects recognition of its annexation. Palestinian proposals for refugees invoke General Assembly resolution 194 of 11 December 1948, seeking return and compensation; Israel’s 1999 negotiating guidelines explicitly excluded refugee return to Israeli territory. The distinction between return to original homes and settlement within a future Palestinian state is therefore substantive, not terminological: the destinations occupy different territories and imply different citizenship, property, and compensation arrangements. (un.org)

Water disputes similarly distinguish interim operational arrangements from permanent rights. Article 40 of the 1995 Israeli-Palestinian Interim Agreement recognized Palestinian water rights in the West Bank but deferred their settlement to permanent-status negotiations, while maintaining existing utilization and providing for additional supplies. The PLO seeks control over Palestinian resources and equitable and reasonable allocation of shared surface water and groundwater. In its 2009 response to a World Bank assessment, Israel maintained that it had fulfilled and exceeded its water-supply obligations under the interim agreement. These positions address partly different measures—allocation rights, supplied volumes, and development permissions—so an increase in purchased water does not itself resolve disagreement over access to shared aquifers. (nad.ps)

Population discrepancies can arise within the same statistical institution when projections are superseded by revised estimates. A Palestinian Central Bureau of Statistics (PCBS) table published in May 2021 projected 5,744,561 inhabitants for mid-2025. Its release of 31 December 2025 instead estimated 5.56 million inhabitants at year-end, comprising 3.43 million in the West Bank and 2.13 million in Gaza. PCBS attributed Gaza’s downward revision to deaths and departures during the war. The figures therefore differ in both reference date and assumptions; the older projection should not be treated as an independent census contradicting the revised estimate. The same release estimated 15.49 million Palestinians worldwide, a population category that includes the diaspora and is not interchangeable with residents of the State of Palestine. (microdata.pcbs.gov.ps)

Area and elevation figures require comparable definitions. PCBS reported approximately 6,020 km² for Palestine in its 2015 environmental release. The 2009 CIA World Factbook entry for the West Bank, reproduced in an online archive, distinguished 5,640 km² of land from 220 km² of water, yielding 5,860 km² altogether: adding an inland-water component changes the denominator used for density calculations. Elevation discrepancies may instead concern different summits: that entry named Tall Asur at 1,022 metres, whereas geographical references identify Nabi Yunis near Halhul at approximately 1,030 metres and commonly give Tall Asur as 1,016 metres. Identifying the summit and source is essential before interpreting the difference as measurement error. (pcbs.gov.ps)

Names also identify different objects. Following the 2012 observer-state decision, the United Nations adopted “State of Palestine” for documents and meeting nameplates, without abandoning “occupied Palestinian territory” as a territorial and legal description. “Historical Palestine,” by contrast, can encompass Israel as well as the West Bank and Gaza. Future arrangements leave practical geographic questions unresolved, including the route and jurisdiction of a West Bank–Gaza connection and Gaza’s maritime boundaries. The PLO’s published position calls for a permanent territorial link carrying people, goods, and utilities. Its negotiating maps illustrate settlements, transport routes, and groundwater resources; such layers can support proposals about territorial continuity and resource access, but their depiction does not establish agreed sovereignty. (un.org)

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85. World Bank Document: Water Supply in West Bank and Gazadocuments1.worldbank.org
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