Koryaksky

Koryaksky
Koryaksky volcano towers over Avacha Bay
Highest point
Elevation	3,456 m (11,339 ft)
Prominence	2,999 m (9,839 ft)  Ranked 91st
Isolation	199 kilometres (124 mi)
Listing	Ultra
Coordinates	53°19′15″N 158°42′45″E / 53.32083°N 158.71250°E / 53.32083; 158.71250Coordinates: 53°19′15″N 158°42′45″E / 53.32083°N 158.71250°E / 53.32083; 158.71250
Geography
Koryaksky Koryaksky in Russian Far East
Location	Kamchatka, Russia
Geology
Mountain type	Stratovolcano
Last eruption	2008 to 2009
Climbing
Easiest route	Basic rock/snow climb

Koryaksky or Koryakskaya Sopka (Russian: Коря́кская со́пка) is an active volcano on the Kamchatka Peninsula in the Russian Far East. It lies within sight of Kamchatka Krai's administrative center, Petropavlovsk-Kamchatsky. Together with neighbouring Avachinsky, it has been designated a Decade Volcano, worthy of particular study in light of its history of explosive eruptions and proximity to populated areas.

Koryaksky lies on the Pacific Ring of Fire, at a point where the Pacific Plate is sliding underneath the Eurasian Plate at about 80 mm/year. A wedge of mantle material lying between the subducting Pacific Plate and the overlying Eurasian Plate is the source of dynamic volcanism over the whole Kamchatka Peninsula.

The volcano has probably been active for tens of thousands of years. Geological records indicate that there have been three major eruptions in the last 10,000 years, at 5500 BC, 1950 BC and 1550 BC. These three eruptions seem to have been mainly effusive, generating extensive lava flows.

Koryaksky erupted for the first time in recorded history in 1890. The eruption was characterised by lava emissions from fissures that opened up on the volcano's southwestern flank, and by phreatic explosions. It was thought to have erupted again five years later, but it was later shown that no eruption had occurred; what was thought to be an eruption column was simply steam generated by strong fumarolic activity.

Another brief, moderately explosive eruption occurred in 1926, after which the volcano lay dormant until 1956. The 1956 eruption was more explosive than the previous known eruptions, with VEI=3, and generated pyroclastic flows and lahars. The eruption continued until June 1957.