Mount Judi
Mount Judi
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Mount Judi

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Mount Judi

Mount Judi (Turkish: Cudi Dağı; Arabic: ٱلْجُودِيّ, romanizedAl-Jūdiyy; Armenian: Արարադ; Kurdish: Çiyayê Cûdîyê) is a mountain in Turkey. It was considered in antiquity to be Noah's apobaterion or "Place of Descent", the location where the Ark came to rest after the Great Flood, according to very early Christian and Islamic traditions (the latter based on the Quran, 11:44). The Quranic tradition is part of the Judeo-Christian-Islamic belief. The identification of biblical Ararat with Mount Judi as the landing site of the ark persisted in Syriac and Armenian tradition throughout Late Antiquity. Only during the Middle Ages was this identification abandoned in favour of another mountain, which had not until then been referred to by any of the native peoples as Mount Ararat (a double-peaked massif, today the highest mountain in Turkey and now generally known by that name).

Mount Judi is situated in Turkey's Şırnak Province, near the villages of Derebaşı and Boyunyaka, at latitude: 37°22'28.21" and longitude: 42°28'16.03".

It is a peak northeast of the town of Cizre in south-east Turkey, at the headwaters of the Tigris River, near the modern border with Syria and that of Iraq. A 10th-century historian placed it c. 32 miles (51 km)) from the Tigris.

The mountainous area that Mount Judi is part of, was known as Qardū (Syriac: ܩܪܕܘ) in Syriac texts, Gordyene by Greek and Roman writers, and Kordukh in Armenian.

Syriac, Islamic, and early Christian traditions identify Mount Judi or Qardu as a peak near or northeast of the town of Jazirat ibn 'Umar in (modern Cizre) Upper Mesopotamia, at the headwaters of the Tigris River. Arab historian Al-Masudi (d. 956), reported that the spot where the ark came to rest could be seen in his time, and that it was located at 80 parasangs (approximately 32 miles (51 km)) from the Tigris. The mountain was historically located in the province of Corduene, south of Lake Van.

The Arabic word al-Jūdiyy (ٱلْجُودِيّ), originates from the Syriac word Gudo (ܓܘܕܐ) meaning "Mounds" or "Elevations". The relation of some of the spellings is clear. The origin of Judi is less clear. It is usually interpreted as a corrupted version of the same name, via Al-Gurdi (Reynolds 2004). Since at least 697 BC, it was often held that after the ark came to rest on the mountain, Noah and the survivors of the flood (who were thought to have numbered 80) came down from it, and built this town to the south of the mountain, hence the name of Thamānīn (Arabic: ثَمَانِيْن, lit.'Eighty'). The proposal that the two names are ultimately the same was first advanced by the English Orientalist George Sale. In his commentary about the Quran (11:4; the verse that mentions the landing of Noah's ark upon Al-Judiy), the English Orientalist George Sale said:

This mountain [al-Judi] is one of those that divide Armenia on the south, from Mesopotamia, and that part of Assyria which is inhabited by the Kurds, from whom the mountains took the name Cardu, or Gardu, by the Greeks turned into Gordyae, and other names. ... Mount Al-Judi (which seems to be a corruption, though it be constantly so written by the Arabs, for Jordi, or Giordi) is also called Thamanin (Geogr. Nub. p. 202), probably from a town at the foot of it (D'Herbel. Bibl. Orient. p. 404 and 676, and Agathiam, 1. 14, p. 135), so named from the number of persons saved in the ark, the word thamanin signifying eighty, and overlooks the country of Diyar Rab ah, near the cities of Mawsel, Forda, and Jazirat Ebn Omar, which last place one affirms to be but four miles from the place of the ark, and says that a Mohammedan temple was built there with the remains of the vessel by the Khalif Omar Ebn Abd'alaziz, whom he by mistake calls Omar Ebn Khattab (Benjamin. Itiner. p. 61). ... The relics of the ark were also to be seen here in the time of Epiphanius, if we may believe him (Epiph. Haeres. 18); and we are told the emperor Heraclius went from the town of Thamanin up to the mountain Al-Judi, and saw the place of the ark (Elmacin. 1. 1. c. 1 ).

— George Sale, 1734; p. 214-215

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