Sabalan

Sabalan(Savalan)
Mount Sabalan
Highest point
Elevation	4,811 m (15,784 ft) [1]
Prominence	3,283 m (10,771 ft) [1] Ranked 66th
Listing	Ultra
Coordinates	[ ⚑ ] : 38°16′01″N 47°50′13″E / 38.26694°N 47.83694°E / 38.26694; 47.83694 [1]
Geography
Sabalan(Savalan) Location in Iran
Location	Meshkinshahr, Iran.
Geology
Age of rock	5.6–1.4 million years
Mountain type	Stratovolcano
Last eruption	Unknown, possibly Holocene.
Climbing
Easiest route	hiking / scrambling

Sabalan or Savalan (native: ساوالان[sævæ'lɒːn])^[2] is an inactive stratovolcano in northwestern Iran located in ardabil province.

At 4,794 metres (15,728 ft) above sea level, it is the third-highest mountain in Iran. A permanent crater lake has formed at its summit. On one of its slopes around 3,600 metres (11,800 ft) there are large rock formations of eroded volcanic outcrops that resemble animals, birds, and insects.

Map of summit region and glaciers of Sabalan.

Mount Sabalan

Located in the extreme northwest of Iran, Sabalan is the country's third-highest peak after Damavand and Alam-Kuh. It is also slightly higher than Mont Blanc in the Alps.

The mountain offers many attractions throughout the year. On the slopes of the mountain, the mineral water from springs attracts large numbers of tourists each year, many of whom have faith in healing properties attributed to the springs. The nomadic people of the area live in small villages, with their round "Yurt" tents appealing to tourists. Sabalan has a ski resort (Alvares) and different tourist areas such as the Sarein spa. The mountain is known for its beautiful vistas, including the Shirvan gorge, where few climbers venture.

Geology

Sabalan is a large andesite stratovolcano in Meshgin Shahr, in Ardabil Province in Iran. It is the second-highest volcano after Mount Damavand. The volcano is quite old. Its first eruptions occurred in the Eocene and later in the Miocene. But the main volcanism happened in the Pliocene and the Pleistocene as some of its rocks have been dated to 5–1.4  million years. Some references state that volcanic activity continued into the Holocene, less than 10,000  years ago.

The summit region has several peaks exceeding 4,500 metres (14,800 ft), primarily along a southwest-northeast trending ridge. The highest point 4,791 metres (15,719 ft) is at the northeast end of the ridge and is separated from the 4,620 metres (15,160 ft)+ group of southwestern summits by a 4,190 m (13,750 ft) col.

The mountain is located in a continental climate with hot, dry summers and extremely cold, snowy winters. Precipitation falls primarily as snow in late autumn, winter, and spring, and is sufficient to sustain seven glaciers near the summit above 4,000 metres (13,000 ft). The largest of these were more than 1.5 kilometres (1 mi) in length as of the 1970s. There are also extensive rock glaciers, several of which are more than 3 km (2 mi) in length.

Climbing

The climbing surface includes rocks of various size (Class 2 scrambling), and a moderate degree of fitness is required to climb it. The climb from the base camp starts easy, becomes challenging midway, then eases in gradient near the top. The lake on the top remains frozen except for about four weeks in late July to early August.

Some climbers start by driving to hot springs of Meshgin Shahr, where they start their climb. This climb takes about two days, reaching the base camp on the first day. Others take a taxi to base camp early in the morning and climb the mountain in one day. In 2006, there was talk of improving the road to the base camp. If this is done, a regular car should be able to make it to the base camp during the climbing season. The road goes through multiple nomadic encampments of shepherds.

One or two days of acclimatization in Tehran or Ardabil may be advisable. Mountaineering has been popular among the youth in Iran. On a Friday during the climbing season (late June to mid-August), one may find hundreds of people on the mountain. Guides can also be found in Ardabil. Adequate climbing equipment can be purchased in Ardabil or Tehran.

Surrounding area

The area around Sabalan, particularly near Meshkin, sarab city and ardabil city,^[3] produces large quantities of grain, including wheat. Due to the microclimate produced by the mountain, Ardabil remains pleasantly cool in the summers.

There are numerous hot springs around the slopes of Sabalan, with the main concentration within Sareyn County.

There are skiing slopes, with snow even in near-summer. A ski resort named "Alvares" is within an hour's drive from Sareyn on the south ridge of Sabalan.

Mount Sabalan and Alvares ski piste seen from South

Gallery

• 

  Arshoq Castle in Meshgin Shahr in foreground, Sabalan in background

• 

  Shelter on Sabalan at 3,600 m

• 

  Crater lake of Sabalan

• 

  Sabalan landscape at 4,100 m

• 

  Igneous rock, Mr. Sabalan, Iran

See also

• List of mountains in Iran
• List of volcanoes in Iran
• List of Ultras of West Asia

References

• "Sabalan". Smithsonian Institution. https://volcano.si.edu/volcano.cfm?vn=232002. 
• Williams, Richard S. Jr, ed (1991). Satellite Image Atlas of Glaciers of the World -- Middle East and Africa. USGS Professional Paper 1386-G. pp. 37–39. http://pubs.usgs.gov/pp/p1386g/. 
• Peaklist.org: Iran Mountain Ultra-Prominence

Sources

• Chehabi, H. E. (1997). "Ardabil Becomes a Province: Center-Periphery Relations in Iran". International Journal of Middle East Studies 29 (2): 235–253. doi:10.1017/S0020743800064485.  (registration required)

External links

• Story of a climb to Mount Sabalan
• Hamed Tohidi's Blog about Mount Sabalan

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