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  1. The Golan Heights ( Arabic: هَضْبَةُ الْجَوْلَانِ, romanized : Haḍbatu l-Jawlān or مُرْتَفَعَاتُ الْجَوْلَانِ, Murtafaʻātu l-Jawlān; Hebrew: רמת הגולן, Ramat HaGolan, pronunciation ⓘ ), or simply the Golan, is a basaltic plateau at the southwest corner of Syria. It is bordered by the ...

  2. Jun 13, 2024 · Golan Heights. Golan Heights. Golan Heights, near the Syrian-Israeli border. Golan Heights, hilly area overlooking the upper Jordan River valley on the west. The area was part of extreme southwestern Syria until 1967, when it came under Israeli military occupation, and in December 1981 Israel unilaterally annexed the part of the Golan it held.

    • The Editors of Encyclopaedia Britannica
  3. Learn about the biblical and contemporary history of the Golan Heights, a strategic area that has been contested by Israel and Syria for centuries. See maps, photos and sources of the Golan Heights.

  4. Oct 11, 2023 · Here is a series of maps explaining why. ... East Jerusalem and most of the Syrian Golan Heights - effectively tripling the size of territory under Israel's control. Israel effectively annexed ...

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  5. Golan Heights. The Golan Heights is a rocky plateau at the southern end of the Anti-Lebanon Mountains, and straddles the borders of Syria and Israel. Israel holds about two-thirds of the territory, while Syria holds the other third. Photo: אסף.צ, CC BY-SA 3.0. Photo: Wikimedia, CC BY 2.5. Ukraine is facing shortages in its brave fight to ...

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  6. Aug 29, 2023 · Golan Heights profile. 29 August 2023. The Golan Heights is a rocky plateau in south-western Syria, about 60km (40 miles) south-west of Damascus and covers about 1,000 sq km. It has a political ...

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  8. The Golan Heights is composed of two geologically distinct areas divided by the Sa'ar River: the Golan Heights proper (approximately 1,070 sq. km.) and the slopes of the Mount Hermon range (approximately 100 sq. km.). While the Mt. Hermon range is mostly limestone, the Golan Heights proper is mostly basalt and other types of volcanic rock ...

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