Nemrut (volcano) facts for kids
- Turkey also has a mountain called Nemrut
Quick facts for kids Nemrut Dağı |
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Satellite view from 2001
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| Highest point | |
| Elevation | 2,948 metres (9,672 feet) |
| Geography | |
| Location | Turkey |
| Geology | |
| Mountain type | Stratovolcano |
| Last eruption | 1692 |
Nemrut (Turkish: Nemrut Dağı, Armenian: Սարակն, «Mountain spring», scientific transliteration: Sarakn, Kurdish Çiyayê Nemrud) is a dormant volcano in Eastern Turkey, close to Lake Van, at 38°37′10″N 42°14′28″E / 38.61944°N 42.24111°E.
The volcano is named after King Nimrod who is said to have ruled this area in about 2100 BC.
Contents
Overview
Nemrut is a polygenic stratovolcano located in the collision zone of the Arabian and Eurasian tectonic plates, which determines the seismic and volcanic activity in the region. The collision of these plates began in the Middle Eocene and closed the stretch of water, which in the Mesozoic formed the Tethys Ocean.
Nemrut, along with three other extinct volcanoes of eastern Turkey: Ararat, Tendürek and Süphan, is located in the area of a complex fault, which runs along the boundary of the Arabian and Eurasian plates in the territory of the Armenian Highland.
It is the westernmost of these volcanoes, the only one that remains active, and generally the only volcano in Anatolia, which erupted in the historical period. Nemrut is located 10 km north of the city Tatvan, in the north-western shore of Lake Van.
Nemrut was probably formed in the early Quaternary Period, about 1 million years ago. It showed the greatest activity in the Pleistocene, with regular eruptions occurring in the Holocene. In the middle Pleistocene, about 250,000 years ago, a major eruption formed a lava flow over 60 km long, which blocked the water discharge from the Van basin and formed Lake Van, the world's largest alkali endorheic lake.
In the same period, the conical top of the volcano collapsed inward, forming an 8.3×7 km caldera. Later, the freshwater Lake Nemrut formed inside the caldera, becoming the world's second largest caldera lake. Subsequent eruptions separated a small lake Ilı from Lake Nemrut.
Nemrut volcano has an elliptical shape, its size at the base is 27×18 km, and its center contains 377.5 km3 of volcanic materials. The caldera of Nemrut is the largest in Turkey, the fourth largest in Europe and sixteenth largest in the world.
Etymology
Locals link the name of the volcano with the legendary ruler Nimrod, who is credited with the construction of the Tower of Babel.
Volcanic activity
Eruptions of Nemrut were mainly of Plinian type. Their products are mainly alkaline and include a wide range of lavas: from basalt to rhyolite and phonolite, as well as pyroclastic emissions and slag. Eruption of different periods were either effused or explosive. Nemrut is located on a fault that crosses the volcano from the north to the south and contains the main crater and a number of small craters, maars, hot springs and fumaroles.
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| View from space in winter | Caldera viewed from its south-eastern edge | Red line shows the Nemrut fault with arrows indicating directions of lava flows |
The volcanic activity of Nemrut occurred in three stages: the formation of a cone (pre-caldera stage), the post-caldera stage, and the late stage. Further, divisions are debatable and are based on different interpretations of the stratigraphic data.
Formation of volcanic cone
The formation of Nemrut and the first stage of eruptions began about 1 million years ago with fissure eruptions that later localized in separate vents separated by 5–10 km. These eruptions resulted in a strong (thicker than 50 m) layer of successive pyroclastic deposits consisting mainly of trachyte. Their products covered an area of 500 km2, forming a plateau that hid the continental deposits of the Miocene period.
The cone of Nemrut was further formed by mobile dark trachytic lavas, which gradually filled Bitlis gorge to a distance of 80 km from the volcanic center. Lava flows reached a width of 200 m and had a thickness of 5–30 meters. Consequent deposits from basalt and trachytic lavas finalized a pronounced cone with a height of about 4400-4500 m.
The next major eruption (volume 62.6 km3) created large voids inside the volcano, which led to the collapse of the apex and the formation of the caldera. Initially it was assumed that the caldera formed right after this eruption, about 310 thousand years ago; however, more recent studies suggest that the collapse happened with the next eruption, about 270 thousand years ago. The products of this eruption mostly consisted of ignimbrites (c. 58.2 km3). Thus the collapse of the cone occurred gradually, probably in three stages.
Post-caldera stage
After the formation of the caldera, eruptions were localized to its edge and formed more than ten of small craters, mostly on the northern edge. The products were dominated by viscous trachyte and rhyolite lavas. Pyroclastic flow deposits were accumulating on the bottom of the caldera, forming ignimbrites and obsidian, and sometimes slag pumice. A cone-shaped crater Göltepe (height 2,485 m above sea level) formed at the bottom of the caldera, on the fault line.
Late stage
At this stage, about 20 small craters and maars formed at the cracks located on the caldera floor, mostly along the central fault. A number of craters with a diameter of 10–100 m formed outside of the main cone, mainly in its northern part. They include Girigantepe (2433 m), Arizintepe (2445 m), Kayalitepe (2311 m), Mezarliktepe (2409 m), Atlitepe (2281 m), Amis (2166 m), Kevriağa (2087 m), Avuştepe and Sivritepe, which is the highest point of Nemrut. Basaltic lava of these craters are the youngest volcanic rocks within Nemrut. The last eruption took place on 13 April 1692. Since then only bursts of steam were observed at the bottom of the caldera, indicating fumarolic activity.
Historical role
Besides the legendary relationship of the volcano with King Nimrod, in 1990s scientists discovered that Nemrut played an important role in the life of the first civilizations. Despite the abundance of obsidian sources in Anatolia and Iran, Nemrut was the main source of obsidian – the most important material of the Stone Age – for all settlements in Mesopotamia and the settlements of the Mesolithic era around the Dead Sea. The analysis of obsidian products revealed that the population of those areas used obsidian from only two sources: Nemrut and the nearby dormant volcano Bingöl. An ancient center of obsidian processing and trade was found at Lake Van, which was part of one of the earliest trade routes.
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| Obsidian deposits at the bottom of Nemrut caldera | Obsidian arrowhead | Obsidian eye in an ancient sculpture |
Two eruptions of Nemrut were probably witnessed by people of Urartu, an ancient state located in the eastern Turkey. These eruptions occurred c. 787 BC (period of King Menua) and c. 657 BC (period of King Rusa II), and the latter eruption might cause the sudden disappearance of the city Uaiais located 30 km east of Süphan.
Present state
Volcanic activity
In the 1980s, Japanese volcanologists studied the evolution of gases inside the caldera of Nemrut. They found that the ratio of helium isotopes 3He/4He is 1.06×10−5, which indicates volcanic activity (most of the measured helium evolved from the mantle). More recent studies have confirmed these findings. The seismic activity in the region is high – in recent years there have been several earthquakes directly related to the Nemrut fault. Significant seismic events of the last 150 years that occurred within 30 km of Nemrut include the earthquakes of 18 May 1881 (magnitude 6.7), 29 March 1907 (5), 27 January 1913 (5), 14 February 1915 (6), and 3 November 1997 (5).
There is evidence that the nature of volcanism in the region may change due to the shift of stress at the boundary of the Arabian and Eurasian plates. The direction of pressure coming from the Arabian plate is gradually turning from South-North to the West-East, with a linear shift of 7.8–9 mm per year. Fumarolic activity and the presence of many hot springs are observed at the bottom of the caldera.
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| A fumarole of Nemrut on the bottom of the caldera | One of the hot springs that feed Lake Nemrut | |
Structure
The volcano has an elliptical shape and covers 486 km2. Its center contains 377.5 km3 of volcanic material, mainly 0.23–1.18 million years old lava. Nemrut has a distinct caldera with an area of 46.7 km2 and a volume of 32.9 km3; the maximum height of the edge of the caldera is 2,935 m (9,629 ft) above sea level (Sivritepe, on the northern edge of the caldera). The average height of the walls of the caldera, measuring from its bottom, is 600 m (2,000 ft). The lowest point of the caldera coincides with the deepest point of Lake Nemrut (2,071 m (6,795 ft) above sea level). There are three lakes at the bottom of the caldera: the larger Lake Nemrut and two smaller ones, Ilı and the so-called "Seasonal Lake".
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| Ilı, eastern view | Lake Nemrut, northeastern view | "Seasonal Lake" |
Lake Nemrut
Lake Nemrut (Turkish: Nemrut gölü) is located in the south-western part of the caldera and is now a freshwater lake. Similar to Lake Van, under the influence of volcanic processes it is gradually becoming a saline lake. The lake is fed by hot springs, which is why it is warmer at the bottom than at the surface and does not freeze in winter. The total area is 4.9×2.1 km, the average depth is 140 m, and the maximum depth is 176 m; the altitude of the lake is 2,247 m (7,372 ft) above the sea level.
Lake Ilı
Lake Ilı, "hot lake") was split from Lake Nemrut by an ancient lava flow. Ilı is located closer to the fault than Lake Nemrut; therefore it has a larger inflow of hot springs and a higher temperature. In the summer, it sometimes reaches 60 °C, and an average is 6–8 °C warmer than expected for a lake of its altitude. Nevertheless, it partly freezes in winter because of the small size and depth.
Risk of future eruptions
Recent studies note the danger of possible eruptions. Nemrut is located in close proximity to Tatvan (distance 10 km, population: 66,000), Bitlis (population 52,000), Ahlat (population 22,000), and a number of smaller settlements. In total, about 135,000 people live in the potential eruption zone. The presence of more than 1 km3 of water in the caldera adds a risk of flooding, which may destroy Güroymak, a town of 15,000 people.
Climate, flora and fauna of the caldera
The climate of the caldera is unique for the Armenian Highland. It is the only place in the region where deciduous trees grow at high altitudes, owing to the high temperature and humidity and the protection from winds by the caldera walls. The caldera also hosts a few flowers and trees unique to the region. Velvet scoters (Melanitta deglandi) and two species of gull live and breed on the shores of Lake Nemrut. Since ancient times the bottom of the caldera is used for grazing by the nearby villages.
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| Unusual for the region deciduous vegetation | Gull at Lake Nemrut | Flock of sheep on the banks of a seasonal hot spring |
Tourism
Nemrut is considered one of the most spectacular volcanoes in the region. Its caldera can be accessed in the summer on 4x4 vehicles from the south or east side. Nemrut is covered with snow five months per year, and therefore the Turkish authorities are building a mountain ski resort and a 2,517 m long ski track on the slopes of Nemrut.
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Left: unfinished elevator on the southern slope of Nemrut which will be part of a ski resort, right: a road to caldera on the south-eastern slope. |
Images for kids
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A 19th century map of the Nemrut area composed by a British traveler.
See also
In Spanish: Nemrut (volcán) para niños
