Volcano Type: Stratovolcano
Volcano Status: Radiocarbon
Last Known Eruption: 6880 BC ± 40 years
Summit Elevation: 3916 m 12,848 feet
Latitude: 38.52°N 38°31’0″N
Longitude: 35.48°E 35°29’0″E
Mount Erciyes is a massive stratovolcano located 25 km to the south of Kayseri in Turkey.
Erciyes is the highest mountain in central Anatolia, with its summit reaching 3,916 metres. It is considered to be an extension of the Taurus Mountains to the south and is generally regarded as the highest peak of this mountain range which belongs to the Alpide belt in Eurasia.
The volcano is heavily eroded, but may have erupted as recently as 253 BC, as may be depicted on Roman era coins.
Growth of the modern volcano began about 0.9 million years ago, following Pliocene caldera collapse of the Kocdag complex. Numerous parasitic cones and lava domes are found mostly on the north flank of the modern edifice, many along radial fissures. The youngest dated rock was from an 83,000-year-old dacitic lava flow, but rhyodacitic eruptions and lava dome growth occurred later at the Perikartin dome.
One of the latest documented events was an edifice collapse that produced a large debris avalanche that extended to the east. An early Holocene distal tephra layer in Lebanon was attributed to Erciyes Dagi. Uncertainty remains regarding reported historical eruptions of Erciyes Dagi and their possible depiction on Roman Cappadocian coins. Historical accounts possibly referring to eruptions could also be attributed to methane releases from a swamp in the Sultansazligi Basin.
Originally posted 2010-10-18 04:24:47.































