Hollow Land. Eyal Weizman

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      The Tunnel Road, Daniel Bauer, 2002.

       Interlude – 1967

      Israeli military strategy, conscious of the strategic limitations of Israel’s pre-1967 borders, was defined by an oxymoron coined by former military general and then Knesset member Yigal Allon in 1959: ‘pre-emptive counter-attack’.¹ According to a plan he drew up with Air Force Commander Ezer Weizman in the mid-1960s, Israel’s Air Force would provide volumetric – that is, aerial – compensation for Israel’s apparent inferiority on the ground.

      In May 1967, after several clashes between Israeli and Syrian troops, originating in earlier dispute over water sources, Egyptian President Gamal Abd al-Nasser honoured his country’s military pact with Syria and deployed ten divisions along the border to Israel, ordered UN observers to leave the Sinai and, on 23 May 1967, closed the Straits of Tiran to Israeli shipping. Israel formed a unity government, mobilized reserves and appointed, under popular pressure, the bellicose Moshe Dayan as Minister of Defence. In anxious anticipation of the war, sports grounds were consecrated as makeshift cemeteries and Israeli newspapers explicitly likened Nasser to Hitler. However, the Israeli Defence Force (IDF) under Chief of Staff Yitzhak Rabin, confident of its ability and seeing an opportunity to defeat the Arab armies, pressed – by some accounts even threatened – the hesitant government of Levy Eshkol into war. The 1967 war implemented Allon and Weizman’s strategy to the letter. On 5 June 1967 the IDF launched an air strike that incapacitated the Egyptian and Jordanian Air Forces. This allowed Israel’s ground forces to charge across the surface of the Sinai and the Gaza Strip. On 7 June the Old City of Jerusalem was surrounded and then occupied. The entire West Bank followed soon afterwards. On 9 June Israel attacked Syrian positions on the Golan Heights. By the end of the June 1967 war, Israeli soldiers were deployed behind clear territorial boundaries of mountain and water: the Suez Canal, the Jordan River on the Jordanian front and the line of volcanic mounts about 40 kilometres into the Syrian Golan Heights. The territory under Israeli control grew threefold, including the rest of former British Mandatory Palestine – the 365 square kilometres of the Gaza Strip and the 5,655 square kilometres of the West Bank.² A period of economic prosperity began, due in no small part to the cheap labor drawn from the newly occupied Palestinian population of more than a million people, about a third of them refugees who had either fled or had been expelled to the region during the 1948 War.³ On December 1967, the Israeli government decided to erase the internationally recognized 1949 Armistice Agreement’s Green Line, which separated Israel from the West Bank and Gaza, from all atlases, maps and textbooks it published. However, except for the area around Jerusalem, Israel did not annex the territories, and according to international law, their status remained that of ‘occupied territories’; in these territories, the Israeli military assumed legislative, executive and judicial powers.⁴

      The area occupied had distinct topographical characteristics. The mountain ranges of Palestine were formed by the fissure of the Great Rift Valley, a 5,000 kilometre tectonic crack running north to south, from the Golan Heights to the eastern shores of Africa, on the Indian Ocean. The West Bank occupies the central portion of this mountain range. Marking its eastern edge is the Jordan River which meanders through the Jordan Valley where the weather is hot, dry and delusionary. The Palestinian population of the area is mainly located around the city of Jericho, a desert oasis on the Jerusalem–Amman road, in small villages and semi-nomadic Bedouin encampments. West of the Rift Valley the ridges rise fast and steep, scorched by wadies, deep canyons and cliffs. The mountain range itself is corrugated with a repetitive sequence of wrinkles and folds, whose elevation ranges from 500 to 1,000 metres above sea level. The summits are barren, rocky and windswept, while the valleys between are fertile and often cultivated with field crops. The six most populous Palestinian cities of the West Bank – Jenin, Nablus, Ramallah, Jerusalem, Bethlehem and Hebron – are strung from north to south along the mountain range’s line-of-water-divide by the Mountain Road (now Road 60), the most important transport route in the West Bank. A few kilometres west of the line-of-water-divide are the western slopes of the West Bank – an area characterized by a benign landscape that slopes gently westwards, with fertile soil and plenty of water and a position close to and overlooking the main Israeli metropolitan centres on the coastal plain.

      The hydrological cycle of the Jordan Valley basin, of which Israel/Palestine and the surrounding states form part, is a system of cyclical flows that cuts through the area’s political and security borders. In winter the water evaporating off the surface of the Mediterranean Sea condenses into rain clouds. The clouds are blown eastwards over the Israeli coastal plains towards the West Bank mountains. There they break against their peaks in sudden bursts of violent rain. The rainwater runs into gullies and streams that drain westwards through the western slopes of the West Bank mountains and back through the Israeli coastal plain into the sea. Some of this rainwater filters through the porous limestone and drains into the soil. Depending on the porosity of the rocks, it may take decades for the water to filter through and collect in underground ‘storage areas’, trapped by a ‘floor’ and ‘ceiling’ of impenetrable rock. There, within the western slopes of the West Bank mountains, on both sides of the 1949 Green Line, the water of the mountain aquifer, can be easily pumped out.

      This hydrological condition asserts itself in the organization of habitation on the surface. The location of water-extraction points has determined the location of Palestinian towns and villages, СКАЧАТЬ