Ararat


          Mount Ararat or Ağrı Dağı is a snow-capped, dormant volcanic cone in Turkey. It has two peaks: Greater Ararat (the highest peak in Turkey with an elevation of 5,137 m/16,854 ft) and Lesser Ararat (with an elevation of 3,896 m/12,782 ft). The Ararat massif is about 40 km (25 mi) in diameter. The Iran-Turkey boundary skirts east of Lesser Ararat, the lower peak of the Ararat massif. It was in this area that, by the Tehran Convention of 1932, a border change was made in Turkey's favour, allowing it to occupy the eastern flank of Lesser Ararat. Mount Ararat in Judeo-Christian tradition is associated with the "Mountains of Ararat" where, according to the book of Genesis,Noah's ark came to rest. It also plays a significant role in Armenian culture and irredentism.

          Ararat is a stratovolcano, formed of lava flows and pyroclastic ejecta, with no volcanic crater. Above the height of 4,100 m (13,451 ft), the mountain mostly consists of igneous rocks covered by an ice cap. A smaller 3,896 m (12,782 ft) cone,Little Ararat, rises from the same base, southeast of the main peak. The lava plateau stretches out between the two pinnacles. The bases of these two mountains is approximately 1,000 km2 (386 sq mi). The formation of Ararat is hard to retrieve geologically, but the type of vulcanism and the position of the volcano raise the idea that subduction relation vulcanism occurred when the Tethys Ocean closed during the Neogene.

          An elevation of 5,165 m (16,946 ft) for Mount Ararat is still given by some authorities. However, a number of other sources, such as public domain and verifiable SRTM data and a 2007 GPS measurement show that the alternatively widespread figure of 5,137 m (16,854 ft) is probably more accurate, and that the true elevation may be even lower due to the thick layer of snow-covered ice cap which permanently remains on the top of the mountain. 5,137 m is also supported by numerous topographic maps.

          Dr. Friedrich Parrot, with the help of Khachatur Abovian, was the first explorer in modern times to reach the summit of Mount Ararat, subsequent to the onset of Russian rule in 1829. Abovian and Parrot crossed the Aras River and headed to the Armenian village of Agori situated on the northern slope of Ararat 4,000 feet above sea level. Following the advice of Harutiun Alamdarian of Tbilisi, they set up a base camp at the Monastery of Saint Jacob some 2,400 feet higher, at an elevation of 6,375 feet. Abovian was one of the last travelers to visit Agori and the monastery before a disastrous earthquake completely buried both in May 1840. Their first attempt to climb the mountain, using the northeastern slope, failed as a result of lack of warm clothing.

          Six days later, on the advice of Stepan Khojiants, the village chief of Agori, the ascent was attempted from the northwestern side. After reaching an elevation of 16,028 feet they turned back because they did not reach the summit before sundown. They reached the summit on their third attempt at 3:15 p.m. on October 9, 1829. Abovian dug a hole in the ice and erected a wooden cross facing north. Abovian also picked up a chunk of ice from the summit and carried it down with him in a bottle, considering the water holy. On November 8, Parrot and Abovian climbed up Lesser Ararat. Impressed with Abovian's thirst for knowledge, Parrot arranged for a Russian state scholarship for Abovian to study at the University of Dorpat in 1830. In 1845, the German mineralogist Otto Wilhelm Hermann von Abich climbed Ararat with Abovian. Abovian's third and last ascent to Ararat was with the Englishman Henry Danby Seymour in 1846.